| Id | Number of occurences | Forms |
|---|---|---|
| 7279 | 1 | he structuring role of papuan karsts on groundwater and surface ichtyodiversité. dip integrates
|
| 7297 | 1 | ts electrochemical reactions. Amazonian soils and environments were rarely mentioned in the lit
|
| 7425 | 4 | nderstanding the overall functioning of agro-ecosystems. agro-ecosystems bordering conserved ar
overall functioning of agro-ecosystems. agro-ecosystems bordering conserved areas represent ide of new diseases. as such, the camargue agro- ecosystem seems remarkably well suited to this ty biodiversity plant virus present in the agroecosystem camargue. a mixed approach, combining hig |
| 7500 | 6 | some soils, said disease resistant, limit their particular m
genetic basis of the resistance of the soil, comparing different soil bacterial community, res stance of the soil, comparing different soil bacterial community, resistant or non- resistant. afeners already known in some resistant soils will be systematically included, and they will al tudied by quantitative pcr dna on total soil to validate the chip. this study will for the firs iological indicators to manage the pest soil quality |
| 7560 | 4 | s, they are especially important in the soil ecosystem. the structure of soil nematodes communi
in the soil ecosystem. the structure of soil nematodes community turns out to be a relevant ind of nematode species found in different agro-ecosystems selected. The objective of these studie ecular tool for comparative analysis of soil samples nématofaune. |
| 7609 | 2 | ria from the indigenous microflora of a soil having been genetically transformed by these molec
est of their properties inoculated into soil to speed up natural processes. the latest advances |
| 7612 | 1 | als. in france there are many sites and soils polluted by metals, mostly due to industrial acti
|
| 7614 | 3 | roject on the purifying capacity of the mangrove was supported as part of the tender ie2007, so
roach also enhances the preservation of mangroves as a natural property suitable for regulated not as a dumping ground, or an unwanted wetland. . . . pir 2009 ecological engineering |
| 10966 | 4 | e full system of climate - vegetation - groundwater - cave - speleothem. thus climate reconstru
ring the part of the system between the soil and the speleothem, using comprehensive measuremen y and oxygen isotopes in cave drips and soil water, plus the movement and composition of cave a composition of cave air, temperatures, soil and vegetation changes, and related these to amoun |
| 12585 | 1 | ecent years the emphasis has shifted to soil and water conservation, enhancement of carbon sequ
|
| 7633 | 1 | ed on the concept of inoculation in the soil of a bacterial strain specifically constructed to
|
| 11767 | 3 | e most fascinating yet least studied of terrestrial ecosystems. in terms of ecosystem science,
itter, woody debris, humic material and soil organic matter, by conducting a translocation expe where samples of litter, dead wood and soil with be swapped between different elevations along |
| 11791 | 2 | e most fascinating yet least studied of terrestrial ecosystems. in terms of ecosystem science,
where samples of litter, dead wood and soil with be swapped between different elevations along |
| 9983 | 3 | e most fascinating yet least studied of terrestrial ecosystems. in terms of ecosystem science,
itter, woody debris, humic material and soil organic matter, by conducting a translocation expe where samples of litter, dead wood and soil with be swapped between different elevations along |
| 13457 | 9 | impair the carbon sequestration in the soil and increase release of carbon to the atmosphere d
ible for carbon cycling in agricultural soils. global climate projections depend today on model ls that estimate the carbon fluxes from soils under land use and climate change. despite the kn change. despite the known importance of soil microorganisms we lack knowledge of the mechanisms y microbial actors of carbon cycling in soils. the aim of this project is to determine the func ffecting carbon cycling in agricultural soils. we propose here a way to develop and use cost ef ty of extracellular enzymes produced by soil microorganism. we will adopt the sequence capture echnology. we will apply the methods on soils from 25 farms in europe and sweden with varied ma sity and functions of microorganisms in soil communities. |
| 15083 | 2 | soil and litter are the reservoir of a huge number of m
ic fungi we will develop a study of the soil and litter hyphomycetes diversity. different geogr |
| 14715 | 2 | soil and litter are the reservoir of a huge number of m
ic fungi we will develop a study of the soil and litter hyphomycetes diversity. different geogr |
| 10883 | 1 | lecular biological methods, measure key soil chemistry parameters, and co-analyse these data ri
|
| 13742 | 4 | itat to sustain. preferred habitats are wetlands and non-cultivated grasslands. in a good stork
abitats are wetlands and non-cultivated grasslands. in a good stork habitat, a plethora of more the interest of the general public for wetland conservation issues, and its reintroduction may el will also be valuable for many other wetland organisms, and hence the model can be used to d |
| 13712 | 1 | lement and partly decrease the need for protected areas. it is today applied in production fore
|
| 14751 | 1 | sical-chemical properties attributes of soil quality.
|
| 9828 | 2 | ffects of long term tnt exposure on the soil microbial community structure, diversity and funct
igate the stability of tnt contaminated soil microbial communities when challenged with additio |
| 7189 | 1 | l the nitrogen flows across the coastal watershed, incorporating the constraints of livestock s
|
| 11330 | 1 | sphere exchange, and provide energy for chemosynthetic ecosystems. reconstructing the magmatic
|
| 10031 | 1 | summary peats and other organic soils provide a major global store of carbon could prov
|
| 11825 | 1 | peats and other organic soils provide a major global store of carbon could prov
|
| 1992 | 3 | g experiment of an unprecedented scale. urban habitat confronts animals, including humans, with
tic environment. some species thrive in urban settings, others perish, but we often have no clu no clue how or why. the great tit is an urban survivor, despite its dependence on acoustic sign |
| 10709 | 2 | ented and scattered across inhospitable urban and agricultural landscapes. because of this habi
scattered across inhospitable urban and agricultural landscapes. because of this habitat loss, |
| 12067 | 1 | complex ecosystems to more simple like agroecosystems. but if land-use practices yield key eco
|
| 13608 | 2 | ses, such as nutrient cycling in forest soils and tree growth. bacteria that enhance mycorrhiza
ns effect on nutrient cycling in forest soils, will lead to increased knowledge concerning how |
| 6843 | 9 | subject / introduction soil biodiversity is an intriguing facet of global biod
is that the biodiversity in the forest–soil is always higher than in arable fields. major func ts are released by decomposition in the soil and litter horizont. the decomposition process dri ocess drives complex food webs with the soil fauna. collembola are ubiquitous members of the so ollembola are ubiquitous members of the soil fauna, often reaching abundances on 100.000 or mor nw–hungary and in the hungarian–plain. soil samples will be taken from afforested monotonous a are their collembola diversity with the grassland’s and arable fields’ fauna. sampling methods arable fields’ fauna. sampling methods soil cores – 100 cm3 – will be removed from randomly se iametered steel corer will be used. the soil cores will be wrapped in plastic film for their sa |
| 7051 | 1 | changes in agroecosystem management affect the natural control of
|
| 10639 | 4 | ategy. the project will show if biochar soil treatment of uk soils is likely to lead to success
ll show if biochar soil treatment of uk soils is likely to lead to successful carbon sequestrat d the consequences for the stability of soil communities and the functions they underpin. this m processes by studying the response of soil biodiversity to a perturbation - addition of bioch |
| 7190 | 1 | bility, ie enhance the functionality of agro-ecosystems while maintaining adequate production l
|
| 13593 | 1 | t of three introduced macroalgae on the swedish coastal ecosystem.
|
| 12016 | 2 | h of processes involved in invasions of insular ecosystems. the biodiversity and the threats up
cies when introduced to or removed from island ecosystems. apart from its scientific outputs, t |
| 12037 | 2 | ions and ecosystem services provided by soils, tested for significant links among them. if sign
plants and 7 groups of terrestrial and soil animals. covariation among the 14 different tables |
| 12051 | 1 | the marine protected areas are means to protect essential habitats
|
| 15445 | 2 | of the genus must dig in very different soil conditions. it is known that although limbs are us
be due to variations in animal size and soil compactness, but also to phylogenetic reasons, sin |
| 12479 | 3 | the ecosystem services provided by the terrestrial ecosystems of england, such as woodlands, r
study will specifically concentrate on terrestrial ecosystems in england and will calculate th information to the context of england’s terrestrial ecosystems. it will employ a consultative a |
| 10444 | 1 | study the social behaviour of foxes in urban bristol. we will compare gps- and vhf-tracking da
|
| 11576 | 1 | oth wet evaporation from the canopy and soil surfaces and transpiration derived from within the
|
| 10650 | 1 | ns store as much as one-third of global soil carbon and represent a highly important global car
|
| 12327 | 1 | culty encountered by upland and lowland grassland farmers in entering els
|
| 13799 | 2 | analyze the role of different forms of urban green areas for biodiversity conservation and eco
dius of 20 km, centered in the national urban park. the major objectives are: . the social anal |
| 7689 | 1 | nt systems to keep them in a context of urban pressure and loss of agricultural activity. from
|
| 11726 | 2 | fluxes of energy, water and co2 over a mangrove forest using the eddy covariance technique. th
g of the fluxes of energy and mass in a mangrove ecosystem. this is an opportunity to understan |
| 14569 | 2 | trains and depend on the host plant and soil features. studies on its genetic and functional di
ontribution of the genetic diversity of soil microorganisms to the functioning of forest ecosys |
| 15143 | 2 | ts to the biodiversity conservation. in agricultural landscapes, loss of habitat diversity and
e effects that the habitat structure of agricultural landscapes has on its biological diversity |
| 13600 | 1 | o perform the studies in a shade coffee agroecosystem in the chiapas, mexico. first it provides
|
| 14366 | 5 | gh changes in land cover and underlying soil composition. results will be cross-validated with
ings. wp5 functional and multi-temporal urban development: the objective of this wp is to study ration, interaction and modeling of the urban, physical and archaeological environment: in this interactions and to asses the impact of urban development on the natural and cultural heritage tural heritage through the modelling of urban expansion and to assess the impact of environment |
| 15333 | 1 | d by agriculture, forestry, tourism, or urban development alter biodiversity at local, regional
|
| 10465 | 1 | are important members of most temperate terrestrial ecosystems, and include some of the most si
|
| 9887 | 1 | are important members of most temperate terrestrial ecosystems, and include some of the most si
|
| 15575 | 1 | ed agricultural production has modified agricultural landscapes, including destruction and frag
|
| 10103 | 1 | cialized associations with fungi in the soil. these fungi infect the germinating seeds and supp
|
| 12631 | 1 | grade alc land located near to existing urban areas. 3. study outputs from these elements of wo
|
| 7034 | 1 | terrestrial ecosystem models are designed to assess the
|
| 11022 | 1 | se, and the part that mammals played in mesozoic ecosystems is sketchy. exceptionally though, t
|
| 12490 | 2 | mmonia and ammonium; - acidification of soils through transformation of deposited ammonia to ni
es to reduce ammonia emissions from the soil to air could potentially lead to the nitrogen emer |
| 7035 | 1 | nic carbon that was initially stored in soils over extended periods become oxidized in streams
|
| 11636 | 14 | soil contains a complex and highly diverse community of
. these microorganisms are required for soil formation and for the many biologically-mediated, ycling processes that take place within soil. these processes are essential for maintenance of cesses are essential for maintenance of soil structure and for cycling of nutrients for plant g ients for plant growth. the majority of soil microorganisms cannot be readily cultivated in the chniques have been used to characterise soil microbial communities. typically, molecular analys lecular analysis involves extraction of soil dna or rna and amplification of genes that provide of considerable microbial diversity in soil and the existence of many groups with no cultivate re abundant and ubiquitous in temperate soils but, because none has ever been cultivated, we ha not possible to determine their role in soil processes or their ecosystem function. two recent quencing of large fragments of dna from soil and marine environments indicate a possible functi ounds. in addition, mrna extracted from soil will be analysed to determine whether the crenarch roorganisms contributes to an important soil ecosystem process, soil nitrification. to an important soil ecosystem process, soil nitrification. |
| 10070 | 1 | ing mineral nutrients captured from the soil for access to plant organic carbon. however, we kn
|
| 10429 | 2 | determine the relative contribution of andean ecosystems to the ch4 and n2o budgets for south
trols on ch4 and n2o fluxes from upland andean ecosystems will also help us evaluate whether ot |
| 10967 | 2 | determine the relative contribution of andean ecosystems to the ch4 and n2o budgets for south
trols on ch4 and n2o fluxes from upland andean ecosystems will also help us evaluate whether ot |
| 11699 | 2 | determine the relative contribution of andean ecosystems to the ch4 and n2o budgets for south
trols on ch4 and n2o fluxes from upland andean ecosystems will also help us evaluate whether ot |
| 14952 | 1 | using information on different types of soil use, recent fires and land-uses, models for the ex
|
| 12590 | 7 | a key requirement for reliable data on soil carbon on which evidence-based policy decisions ca
suggests that carbon is being lost from soils in england and wales, but the cause of this loss the belief of both policymakers and uk soil scientists that sufficient information already exi m a broad representative base of the uk soil community, was convened, through the auspices of p al and temporal properties of carbon in soils. • using the decision tool to define the ‘rules/i to define the ‘rules/inputs’ in running soil c flux models to deliver uk-wide estimates of soil models to deliver uk-wide estimates of soil c flux for several established land use and manage |
| 10163 | 1 | essure. in addition, the role of marine protected areas in altering the patterns of change in f
|
| 10973 | 1 | l be used to assess biodiversity within planktonic ecosystems in the southern ocean. following
|
| 13794 | 1 | regional model of the agricultural peri-urban region in southern quebec and its dynamics and re
|
| 14109 | 3 | environmental changes. in contemporary agricultural landscapes, field boundaries and other sem
, i will use a common self-incompatible wetland plant lychnis flos-cuculi as a model species re e to fragmentation, and ditch verges in agricultural landscapes as model systems. i will sample |
| 10156 | 1 | rldwide has tb, and over one fourth has soil transmitted helminths. importantly, these co-infec
|
| 11676 | 1 | rldwide has tb, and over one fourth has soil transmitted helminths. importantly, these co-infec
|
| 12615 | 1 | tial legacy of chemical contaminants in soil, mainly resulting from industrial pollution. gover
|
| 12295 | 3 | status/function/designation include: • urban – residential housing/commercial/industrial/trans
rial/transport networks/infrastructure/ urban greenspaces; • agricultural land – arable/horticu gricultural land – arable/horticultural/grassland; • land with designated status – aonbs/nation |
| 7370 | 1 | ch for evaluating the diversity of land agricultural landscape. this indicator will quantify th
|
| 7667 | 2 | and more recently on a very particular urban ecosystems. the assesment of ecosystem services o
assesment of ecosystem services of the urban biodiversity its a complementary step for the com |
| 7619 | 3 | s using the plant for the management of soil erosion. the french association of biological engi
gical engineering for the management of soil erosion. french position this association with a e plant technology for the management of soil erosion |
| 10191 | 2 | celia growing from woody resources into soil. the dearth of information available on these inte
ing of fungal community development and soil invertebrate population biology. such knowledge pr |
| 12608 | 2 | which aims to protect and enhance peat soils by reducing the volume of peat used by the hortic
defra has a target of 90% for the total soil improver and growing media market to be peat-free |
| 14784 | 10 | the high rate of mineralization of the soil organic matter, with the consequent decrease of th
er, with the consequent decrease of the soil fertility and productive capacity. in addition, in ave caused a sensible diminution in the soil biodiversity, because of the tillage systems and t of the quantity and the quality of the soil organic matter, as well as of the soil biochemical soil organic matter, as well as of the soil biochemical activity, is essential to understand t mical and biological characteristics of soil, and the relation with short and long-term product long-term productivity functions in the agroecosystem 4. construction of a soil bacterial genet the agroecosystem 4. construction of a soil bacterial genetic library, indicative of the diffe cator of agricultural sustainability in soils in olive agroecosystems. ltural sustainability in soils in olive agroecosystems. |
| 12595 | 1 | adopting a landscape-scale approach to wetland conservation such as the manchester mosslands.
|
| 12606 | 4 | cent research on practices for managing soil organic matter and lowland' agriculture in england
land, taking into account variations in soil type, agricultural systems and cropping/land use. or envelopes of normality for different soil/land use and rainfall areas. as well as identifyin o current cross compliance guidance for soil management or via incentivised environmental stewa |
| 14285 | 1 | icular on the structure and dynamics of coastal and shelf ecosystems in the perspective of glob
|
| 7249 | 2 | ich are strong diffuse contamination of urban environments. this project is part of the multi-y
metropolitan territory: reflections of urban development in ile de france network of r2ds. sis |
| 12044 | 2 | level would have on the biodiversity of agroecosystems at the plot and regional level. we will
mics and persistence of biodiversity in agroecosystems. this project is organised in four compl |
| 2493 | 1 | onservation management of exploited and pristine ecosystems in four european countries.
|
| 7104 | 2 | o main ways of managing biodiversity in agricultural landscapes - the first is to partition the
ent actual or potential contribution of urban agriculture in maintaining the ecological functio |
| 516 | 1 | methods for biodiversity management in agricultural landscapes: the first one consists in divi
|
| 11505 | 1 | anges of products within and beyond the watershed intensified, with fair trade and value-added
|
| 11619 | 2 | important quantitatively than others in soil biology, which may be important for understanding
derstanding the long-term health of the soil under modern methods of farming and forestry. |
| 10724 | 1 | assess the health and carbon budgets of soil and freshwater environments.
|
| 451 | 2 | the dispatching of biodiversity. marine protected areas of the republic of maldives: - which is
oral communities encountered within the protected areas of the maldives and outside is it neces |
| 6891 | 1 | an research centers of botany, zoology, soil science, and agro-environmental research we plan t
|
| 396 | 1 | dscape ecology. we will examine plants, soil animals, predatory insects, pollinators and two ec
|
| 14795 | 2 | one of the largest and most importants wetlands in europe. it is considered an unesco man and
rds. however, the microbial life in its soil is perfectly unknown. all these features make the |
| 521 | 1 | of biodiversity favouring practices in grassland areas which are the effects in terms of biodi
|
| 7674 | 3 | biodiversity conservation in protected areas is linked to ecological trade-offs betw
ar timeframe. simultaneously, ageing of groundwater will be conducted to assess whether recharg elephants and trees, in a large african protected area. |
| 7422 | 1 | c pesticides, and the simplification of agricultural landscapes resulting from the specializati
|
| 7281 | 1 | he implementation of the green and blue urban context. it documents the biodiversity areas, que
|
| 14821 | 2 | mediterranean coastal wetlands are considered ecosystems that deserve to be p
cies of tropical affinity to grow. this wetland is considered a refuge of biodiversity for its |
| 9933 | 1 | chness on a wider scale across european grasslands and to elucidate the mechanism responsible.w
|
| 1930 | 2 | especially in agricultural landscapes, space and finances must be div
nt functions in nature areas and in the agricultural landscape. |
| 14419 | 3 | . recent studies have demonstrated that flowering plants and insects ecosystems harbor vast unt
al parks are among the largest and most protected areas in europe. bulgarian parks host 250 end gically important properties from these bulgarian ecosystems. the research project will be acco |
| 7211 | 1 | essary to increase the extent of marine protected areas • how species richness of these sites d
|
| 429 | 1 | cient oak forests developped on neutral soils in the lorraine plateau, small as well as cannabi
|
| 14716 | 3 | the edaphic ecosystem is complex, scaresly studied, with a
pend on the productivity of natural and agricultural ecosystems. the isolation, identification improvement of enivronmental quality in land ecosystems |
| 10398 | 1 | used to identify the source of the deep groundwater, chemical analysis will define the geochemi
|
| 11782 | 5 | humans in the bark of oak trees and the soil around them. partly because sake, wine, beer and b
the world, they have also been found in soils from holland and finland, but they have not yet b ca discovered that pretreating bark and soil with alcohol and sugar led to the isolation of s. ven though their occurrence in bark and soil would otherwise rarely be noticed. the use of this n oaks. in this study, small amounts of soil, bark or grapes will be taken back to the lab and |
| 14115 | 1 | ogical indication methods in remote and urban areas. 3.to use bioindicational methods in evalua
|
| 7642 | 5 | ironments in which they live. secondly, soil invertebrates heavily involved in the operation of
eavily involved in the operation of the soil and thus to the provision of ecosystem services. b cal and ecological functional traits of soil invertebrates. originality of this project lies in ns in the macro- and meso- fauna of the soil and thus a wide spectrum of biological strategies. ing tools specific to the compartment ' soil ' ecosystems |
| 15074 | 1 | nces, autonomous communities, and rural-urban environments, justify the achievement of a geogra
|
| 15120 | 2 | nity structure in mediterranean shallow lentic ecosystems. the effects of the physical control
his objective we will study two shallow lentic ecosystems: temporary ponds, where the drought i |
| 10129 | 4 | tic warming on the emission of co2 from soil by investigating how soil biological and functiona
n of co2 from soil by investigating how soil biological and functional diversity carbon isotope ortant for constraining the response by soil respiration to climatic change and use our laborat a new understanding of the response by soil respiration to climatic warming and we will test h |
| 10417 | 4 | tic warming on the emission of co2 from soil by investigating how soil biological and functiona
n of co2 from soil by investigating how soil biological and functional diversity carbon isotope ortant for constraining the response by soil respiration to climatic change and use our laborat a new understanding of the response by soil respiration to climatic warming and we will test h |
| 11411 | 4 | tic warming on the emission of co2 from soil by investigating how soil biological and functiona
n of co2 from soil by investigating how soil biological and functional diversity carbon isotope ortant for constraining the response by soil respiration to climatic change and use our laborat a new understanding of the response by soil respiration to climatic warming and we will test h |
| 9891 | 4 | tic warming on the emission of co2 from soil by investigating how soil biological and functiona
n of co2 from soil by investigating how soil biological and functional diversity carbon isotope ortant for constraining the response by soil respiration to climatic change and use our laborat a new understanding of the response by soil respiration to climatic warming and we will test h |
| 14420 | 5 | wetlands on the flood plane of the lower danube concent
al parameters of the hydroecosystems of wetlands on the flood plane of the lower danube as a ba versity and the environmental status in wetlands will be obtained. clarification of the main me he ecological integrity of the riparian wetlands with different flooding regime is an expected rt the biodiversity and to optimize the wetland’s functions under intensive anthropogenic press |
| 15280 | 1 | as nitrificant chemoauto/mixo-trophs in soils and waters and efficiently competing with nitrifi
|
| 14494 | 10 | uch as sandy, degraded and low nutrient soils where commonly this species develops adaptative f
which could allow us to understand the soil fauna biology in that sort of environments. furthe f the surface of arid and poor nutrient soils where this species could stands for the main zoom rmation about their function in iberian soil, including agriculture ones where they are very of ies. must point out the interest of the soil fauna study in agrarian systems by its important r rarian systems by its important role in soil fertility, development of organic fertilizers, imp physical and chemical properties of the soil, mainly at the present time when the ecological fa , chemical and biological properties of soils, and their activity patterns depend on biological ation rate, water retention and loss of soil. on the biological properties the interest will be cycles. in a. caliginosa an d a. rosea soil selection, gut transit time, gut content and event |
| 14788 | 3 | sentinels of environmental pollution in soils. several authors suggested that slugs can be used
ors suggested that slugs can be used in soil health assessment in the manner that mussels and o ram based on the biomarker approach for soil pollution monitoring. |
| 14924 | 1 | ated the biomineralization ability of a soil bacterium: myxococcus xanthus. among this ability
|
| 15087 | 1 | hen decisions on population management, protected areas or endangered species must be taken. in
|
| 7613 | 1 | the water and sediment particles or the soil organic matter, and liquid / liquid interfaces for
|
| 14954 | 1 | udy will be performed with contaminated soils from a wood-treating creosote plant.
|
| 1083 | 1 | changes are detectable and modelled in extant ecosystems, long-term variations in the biospher
|
| 2196 | 3 | biodiversity of blue mussel ecosystems: patterns and processes blue mus
sent an analysis of the main threats to mytilus ecosystems and the goods and services produced. include a comparison between baltic and west coast ecosystems. it is also expected that under t |
| 13572 | 2 | ng will be made on leaching of doc from soils under various scenarios of precipitation and vege
us scenarios of runoff, doc-losses from soils and in-lake doc processing. |
| 15430 | 1 | n important part of the biodiversity in land ecosystems with approximately 15000 species in the
|
| 15221 | 1 | ion and therefore in the fucntioning of terrestrial ecosystems. this decline is a component of
|
| 6916 | 1 | diagenetic processes will be assessed. soil parameters will be analysed. exact age of the fore
|
| 14764 | 1 | understand the mechanisms by which the terrestrial ecosystems work - maintenance and improveme
|
| 15290 | 11 | erow networks are characteristic of the agricultural landscapes. although its relative surface
ay a key role to the functioning of the agroecosystems as it has been recognised by the new cap and to the buffering of the n fluxes in agricultural landscapes. understanding hedgerow c seque lances -required by kyioto protocol- in agricultural landscapes. hedgerow vegetation can be mad erow vegetation can be made of forests, grasslands or ruderal. nevertheless, because of their v higher nutrient fluxes than forest and grasslands growing unconnectedly from the arable lands. t the same as in mature or successional grasslands or forests. c dynamics in hedgerows can be d will be monitored for two years in the soil plant systems of crop edges and hedgerows. finally study the forms of n recently fixed in soils by using densimetric fractionation techniques. th ute to establish the basis for managing soil c sequestration and n retention in agricultural la soil c sequestration and n retention in agricultural landscapes with contrasted intensification |
| 7025 | 1 | ii increasing contact between water and soil or sediment increases nitrogen retention and proce
|
| 13710 | 1 | and animals. shorebirds breeding on wet grasslands have particularly suffered from these change
|
| 11102 | 1 | ment, long-term survival of seed in the soil, and characterising habitat patches. we propose a
|
| 11670 | 1 | rbon entering the lake from surrounding soils. we therefore need to find a method whereby this
|
| 13777 | 1 | ows higher. this threatens species-rich riparian ecosystems, which depend on recurrent floods,
|
| 10045 | 1 | lts will be readily applied in existing protected areas. as a result we aim to create a bluepri
|
| 11162 | 1 | commitment to the management of coastal ecosystems through addressing both ecological a
|
| 7251 | 1 | ows carbon storage in plant biomass and soils. current carbon footprint models, in particular g
|
| 14612 | 5 | derstand and to predict the response of terrestrial ecosystems to climate change and to underst
ould be of particular risk for arid and semiarid ecosystems such as those in the province of al igate aspects related to vegetation and soil such as plant biomass, spatial variability, and ca rbon stocks. furthermore, we will study soil respiration and the response of soil respiration a dy soil respiration and the response of soil respiration and ecosystem fluxes to summer rainfal |
| 11204 | 5 | buscular mycorrhizal mycelium in upland grassland provides a major, rapid and distinct pathway
ay for the flux of plant-derived c into soil and supports specialized populations of soil micro and supports specialized populations of soil micro-organisms. novel soil-core systems controlli ulations of soil micro-organisms. novel soil-core systems controlling the presence and absence antify c flux from plants through am to soil bacteria and microarthropods by 14c and 13c labell |
| 7663 | 1 | lubilization of organic nitrogen in the soil water, by measuring the isotopic composition 15n a
|
| 14873 | 7 | limate and land-use changes interact on agro-pastoral ecosystems in the iberian peninsula at di
r ability to retain nutrients and store soil carbon. results from the previous project carbopas s in the interactions within the system soil-microorganism-plant-animal, affecting the c and n e the existing database on c content in grassland ecosystems through the use of altitudinal/cli nts, and b to use the existing plots on grasslands and legume-based forage swards linked to the mental systems where those processes of soil c accumulation will be analyzed in detail. the com . the results will be useful beyond the agro-pastoral ecosystems, which in this context would b |
| 14874 | 7 | limate and land-use changes interact on agro-pastoral ecosystems in the iberian peninsula at di
r ability to retain nutrients and store soil carbon. results from the previous project carbopas s in the interactions within the system soil-microorganism-plant-animal, affecting the c and n e the existing database on c content in grassland ecosystems through the use of altitudinal/cli nts, and b to use the existing plots on grasslands and legume-based forage swards linked to the mental systems where those processes of soil c accumulation will be analyzed in detail. the com . the results will be useful beyond the agro-pastoral ecosystems, which in this context would b |
| 10243 | 5 | incorporation of carbon at the sourhope soil biodiversity field site from atmospheric carbon di
atmospheric carbon dioxide, through the soil fauna, into soil organic matter. this will be achi n dioxide, through the soil fauna, into soil organic matter. this will be achieved through the ed by individual plant, mycorrhizal and soil faunal species in in situ c transfers at sourhope. ct to control the fate of carbon in the soil. the project will involve a multi-disciplinary con |
| 11005 | 5 | incorporation of carbon at the sourhope soil biodiversity field site from atmospheric carbon di
atmospheric carbon dioxide, through the soil fauna, into soil organic matter. this will be achi n dioxide, through the soil fauna, into soil organic matter. this will be achieved through the ed by individual plant, mycorrhizal and soil faunal species in in situ c transfers at sourhope. ct to control the fate of carbon in the soil. the project will involve a multi-disciplinary con |
| 11216 | 5 | incorporation of carbon at the sourhope soil biodiversity field site from atmospheric carbon di
atmospheric carbon dioxide, through the soil fauna, into soil organic matter. this will be achi n dioxide, through the soil fauna, into soil organic matter. this will be achieved through the ed by individual plant, mycorrhizal and soil faunal species in in situ c transfers at sourhope. ct to control the fate of carbon in the soil. the project will involve a multi-disciplinary con |
| 14118 | 6 | the changes in the size and quality of soil carbon and nitrogen pools after forest fires. the
ry timely since deeper understanding on soil carbon stocks and its underlying processes is urge m carbon cycle in the changing climate. soil is the largest stock of organic carbon, but the re bon, but the related processes changing soil organic matter quality and its pool distribution a odel to below-ground processes such as: soil organic matter decomposition, turnover of carbon c pounds of different chemical fractions, soil nitrogen/protein pools, root and rhizosphere respi |
| 10891 | 2 | od chain to affect herbivore, plant and soil microbe biomass. it will also test whether herbivo
for the management of insect species in agricultural ecosystems. |
| 12480 | 1 | ar case study area undergoing extensive urban regeneration and how best they can be evaluated w
|
| 14819 | 13 | soil degradation due to human activity affects the qual
man activity affects the quality of the terrestrial ecosystems and consequently, its biodiversi to evaluate the interrelations between soil quality and biodiversity and its implications on t interest are the studies that integrate soil genesis aspects, soil degradation and its use with es that integrate soil genesis aspects, soil degradation and its use with the biodiversity them by heavy metals and pesticides, and the soil biological activity. the kind of soil can be the p e soil biological activity. the kind of soil can be the primary factor that determines the biod consider that in order to rehabilitate soils that have lost a great part of their biodiversity tance persistence diminish directly the soil biodiversity and could affect the ecosystem functi s project is to study the effect of the soil degradation on the biodiversity loss on different ation, the pollution by heavy metals on agroecosystems with already known accumulation and the s use of the post-control substances on agroecosystems with intense agricultural activity are s tats loss and fragmentation: effects of soil degradation on ecosystem functioning and biodivers |
| 13749 | 5 | tter formation and nutrient turnover in soils under different scenarios of nitrogen sequestrati
ies on microbial communities in natural soils – to identify the microorganisms that carry out c isms that carry out c and n turnover in soils, characterize some of these processes at molecula ion and risks of nutrient leaching from soils. a centre for soil microbial ecology will be esta rient leaching from soils. a centre for soil microbial ecology will be established to accomplis |
| 15267 | 1 | re is an initiative to declare a marine protected area around el hierro.
|
| 10788 | 2 | to find out the importance in antarctic soils of specific forms of nitrogen. in addition, we wa
lter the nitrogen dynamics of antarctic soils. we hypothesize that our research may offer an ex |
| 10804 | 2 | to find out the importance in antarctic soils of specific forms of nitrogen. in addition, we wa
lter the nitrogen dynamics of antarctic soils. we hypothesize that our research may offer an ex |
| 1947 | 1 | mmunities on mesotrofic and oligotrofic soils is one of the key issues of the ecological main s
|
| 440 | 1 | ncluding worldwide bases of climate and soil properties. this will contribute to the emerging f
|
| 528 | 3 | ces and the methods used to exploit the soil request less and less the resources of open enviro
the last big sub-mediterranean area of grasslands and chalky moors, the region of the grands c environment closures. furthermore, the grasslands there are colonized by a small number of lig |
| 12656 | 1 | tion and abundance of breeding birds in urban and suburban housing areas in relation to surroun
|
| 11294 | 1 | take of c by plants and its transfer to soil, and then back to the atmopshere.
|
| 11305 | 1 | take of c by plants and its transfer to soil, and then back to the atmopshere.
|
| 14949 | 4 | decades, have on plant communities and soil. the short period of time since the treatments are
dress the effects of climatic change on soil microbes, particularly mycorrhiza and bacteria, wh the effects of precipitation changes on soil respiration and soil carbon accumulation, and rela itation changes on soil respiration and soil carbon accumulation, and relate these changes to m |
| 15388 | 1 | ecosystems is the role that biological soil crusts the intrinsic variability of the drying-rew
|
| 7150 | 2 | tions of sahelian countries like niger. agro ecosystems in this country are exposed to profound
ties, the cropping systems, climate and soil conditions and demographic, entries conducted to d |
| 10349 | 1 | ropical forest plots, integrate it with soil and climate data, then creatively use this data to
|
| 11786 | 1 | ropical forest plots, integrate it with soil and climate data, then creatively use this data to
|
| 11013 | 1 | f reactive carbon gases from plants and soil, and wind transport of primary carbonaceous partic
|
| 12514 | 1 | penetration of the organic market into urban versus rural areas will be investigated. a projec
|
| 10818 | 3 | soil usually possesses a microbiotic crust at the surfa
acteria. since these layers form at the soil surface, they have considerable importance in dete p provides interdisiplinary training in soil science, microbiology and the environmental chemis |
| 10743 | 1 | rce areas. input of organic n to forest soils will be measured in throughfall. the results will
|
| 11755 | 1 | rce areas. input of organic n to forest soils will be measured in throughfall. the results will
|
| 9974 | 1 | rce areas. input of organic n to forest soils will be measured in throughfall. the results will
|
| 12185 | 11 | defra have identified compaction in grasslands as an important issue that may threaten the
a need to improve our understanding of soil compaction in grasslands and to identify and evalu our understanding of soil compaction in grasslands and to identify and evaluate mitigation meth we will carry out a national survey of soil compaction in grasslands. we will identify and vis a national survey of soil compaction in grasslands. we will identify and visit 300 grassland fi sslands. we will identify and visit 300 grassland fields covering improved, semi-improved and u improved, semi-improved and unimproved grassland pastures and hay meadows; fields within and w ed in an interim report on the national grassland characterisation survey and a final report on roduction of a technical advice note on soil compaction and loosening and the establishment of and loosening and the establishment of grassland plant communities. in addition, results will e communicated through regionally based soil workshops for advisers and land managers via visit |
| 11625 | 2 | some success but the models of surface soil erodibility are very crude. the aim is to establis
ablish a physical basis between surface soil properties including roughness and bi-directional |
| 13359 | 4 | s to be grown very variable climate and soil conditions are required both rehabilitation of pas
as especially for providing nitrogen to soil, improving soil texture and supplying with high yi r providing nitrogen to soil, improving soil texture and supplying with high yield and quality ns and adapted salty and poorly drained soil. in this study the national collection at aegean a |
| 15181 | 1 | e have been reported in three important protected areas, while in other areas, we have not obse
|
| 7625 | 5 | ots increases the shear strength of the soil, but they do not take into account the architectur
of architectural traits of interest for soil reinforcement and integrate these effects in slope pproach is based on the embodiment 1 of soil shear tests reinforced by roots; 2- developing dig uantify the influence of root traits on soil resistance; 4- integration of these results in a s on between the root system of trees and soil |
| 14588 | 4 | the autochthonous olive orchard agroecosystem in extremadura must be protected because
because of the ecological importance in soils protection, as soils in many zones of extremadura ical importance in soils protection, as soils in many zones of extremadura are in precarious st in precarious state, due to low ph and soil development, under extreme temperature and drought |
| 157 | 1 | total flux of energy and matter of the coastal ecosystem. being a quite unique and small group
|
| 10316 | 1 | we propose an analysis of the chemosynthetic ecosystems in antarctica south of the po
|
| 10551 | 1 | we propose an analysis of the chemosynthetic ecosystems in antarctica south of the po
|
| 10781 | 1 | we propose an analysis of the chemosynthetic ecosystems in antarctica south of the po
|
| 11308 | 1 | we propose an analysis of the chemosynthetic ecosystems in antarctica south of the po
|
| 11568 | 1 | we propose an analysis of the chemosynthetic ecosystems in antarctica south of the po
|
| 11828 | 1 | we propose an analysis of the chemosynthetic ecosystems in antarctica south of the po
|
| 6752 | 3 | vestigate the fate of chromium polluted soil will be studied as well. the expected results of t
anding of forming chromium complexes in soils and its fate in the soil plant system. complexes in soils and its fate in the soil plant system. |
| 14157 | 4 | h project is a synthesised study of the urban environment and the environmental impact of urban
e especially acute due to the intensive urban sprawl in the light of multifunctional land use p quent extraordinary weather conditions, urban areas as sensitive places have to adapt and mitig on transport load and the condition of urban environment, also needs to be elaborated. the obj |
| 13615 | 2 | eding nematodes are major herbivores of grasslands. the goal of the proposed study is to examin
the biological control of nematodes in agro-ecosystems. |
| 1105 | 1 | st efficient systems for the storage of soil carbon in widespread agro-forestal systems in cent
|
| 10476 | 1 | life habitat with either agriculture or urban environments. not only does such development redu
|
| 12592 | 10 | change has been identified by the draft soil strategy for england as one of the key pressures l
the key pressures likely to affect our soils now and in the future, along with land-use practi limatic changes are likely to impact on soils and the soil biota, and potentially affect the ab s are likely to impact on soils and the soil biota, and potentially affect the ability of soils , and potentially affect the ability of soils to maintain delivery of the range of ecosystem go em goods and services required of them. soil organisms are directly involved in the provision o tem services, performing major roles in soil processes and functioning, including carbon and nu including carbon and nutrient cycling, soil structural dynamics, detoxifying pollutants and su nd supporting aboveground biodiversity. soil organisms are likely to be directly and indirectly und biodiversity and the ability of the soil to withstand and recover from perturbations. |
| 15005 | 1 | nt part of the biodiversity existing in terrestrial ecosystems corresponds to bryophytes, with
|
| 2109 | 3 | s. we will also use past vegetation and soil registrations for analysing the development of the
ue to a detailed mapping of vegetation, soil properties and timberline position in 1932-1936. t analysed with respect to vegetation and soil, and the information will be included in a digital |
| 12588 | 9 | current literature on the state of soil carbon levels in uk soils is equivocal. prediction
n the state of soil carbon levels in uk soils is equivocal. predictions of future changes in so vocal. predictions of future changes in soil carbon levels related to land use and climate chan uggested the need to collate uk data on soil carbon and the release of greenhouse gases in rela to be gained of the current state of uk soil carbon and the processes driving change, and infor ienced and recognised members of the uk soil science community who have the broad range of skil ailability and provenance of data on uk soil carbon stocks, fluxes and land use influences. 2. is project will be a brief review of uk soil carbon data sources and shortfalls in these data. vidence to policy makers in relation to soil carbon and land management. tasks for a second pha |
| 15028 | 3 | -as well as their relationships- on the coastal ecosystem have received little attention. never
ects over the exploited species and the coastal ecosystem. the objective of the current proposa ions and maintain the resiliency of the coastal ecosystems, the health of the fish stocks and t |
| 13386 | 1 | ion criteria and genotypes suitable for rangelands and/or hay production will be utilized in th
|
| 12146 | 2 | colony changes of vegetation, fungi and soil biota take place. nature and dynamics of these cha
chemical and biological composition of soil, structure of various groups of mycobiota, formati |
| 11836 | 2 | s are typical of either normal dry-land/wetland, or salinity stressed wetland ecosystems. follo
dry-land/wetland, or salinity stressed wetland ecosystems. following detailed anatomical descr |
| 10333 | 2 | scape ecology is possible using natural micro-ecosystems rather than experimentally assembled m
richness . here we propose to use this micro-ecosystem to test the effect of community disasse |
| 15499 | 1 | organisms, or to after-life effects on soil function through microbial use of leaf litter and
|
| 7662 | 2 | fects of representative contaminants in urban areas or the decline of the species if genotoxici
ronic low-dose chemical substance in an urban environment in a fresh water body model, the zebr |
| 2478 | 1 | arine resources require management in a broader ecosystem context. this proposal follows on fro
|
| 12617 | 12 | n predictions of future climate change. soil carbon dynamics are a key element of this because
amics are a key element of this because soils contain two or three times the amount of carbon a d published the results of the national soil inventory of england and wales for changes in soil ory of england and wales for changes in soil carbon during the 1980s and 90s. this showed gains 0s. this showed gains in carbon in some soils, but large losses in others and overall a net los d management, such as the conversion of grassland to crops after the war, and land drainage sch asons, such a large loss of carbon from soils has serious implications for the global carbon cy e possibility of sequestering carbon in soils, and for the ability of soils to perform other en carbon in soils, and for the ability of soils to perform other environmental and agricultural f and these fail to detect the changes in soil carbon observed in the nsi. the reaons for the dif eld and ceh. given that our datasets on soil carbon in england and wales are among the most com e results will inform the debate around soil protection for other environmental and agricultura |
| 517 | 1 | of result achievement: an innovation in grassland areas. the research question that we will dea
|
| 7490 | 12 | european soil biodiversity is pivotal for delivering food, fibre
he demand is greater than the amount of soil available, as production of bio-fuels competes wit moreover, intensified land use reduces soil biodiversity and the resulting ecosystem services. system services. soilservice will value soil biodiversity through the impact on ecosystem servi interdisciplinary empirical studies and soil biodiversity surveys to construct soil food web mo soil biodiversity surveys to construct soil food web models and determine effects of changing odels and determine effects of changing soil biodiversity on stability and resilience of carbon models to develop a system for valuing soil biodiversity in relation to ecosystem services. ob s. objectives: develop methods to value soil ecosystem services during different pressure of la ent pressure of land use and changes in soil biodiversity. field and modelling studies will det ine to what spatial and temporal scales soil biodiversity and soil ecosystem services are vulne d temporal scales soil biodiversity and soil ecosystem services are vulnerable to disturbance. |
| 7433 | 2 | ment and restoration of biodiversity in wetlands. it will: -d'établir levels of vulnerability o
ir levels of vulnerability of different wetland types in terms of genetic diversity, -to define |
| 13879 | 1 | iable populations of bee pollinators in agricultural landscapes.
|
| 7103 | 1 | ical / scientific one hand, and rural / urban secondly - that coexist and are in tension in str
|
| 11070 | 3 | a large component of soil co2 efflux is driven by autotrophic respiration; i
t groups of root-associated microbes in grassland are arbuscular mycorrhizal to provide the fir tion of arbuscular mycorrhizal fungi to soil co2 efflux in response to climate manipulation. |
| 10404 | 8 | rbon turnover in species-rich limestone grassland. moreover, we will additionally determine whe
d the extent to which it is mediated by soil conditions, such as physical and chemical properti cosms also have imposed on them defined soil treatments to mimic the variation that occurs in n . we will measure the carbon content of soil in a number of important physical fractions and re s and release of carbon as co2 from the soil surface. in addition, we will supply plants with a mount of carbon that plants allocate to soils. this will enable us to gain a more mechanistic u important for carbon turnover, and the soil factors that may regulate this. it will also provi on strategies of species-rich limestone grassland that target genotypic, as well as species div |
| 12714 | 5 | ssess the contribution of the brazilian protected areas for the national economy in order to he
ts of investing in the establishment of protected areas and conservation strategies more genera to assess the economic contribution of protected areas. significant effort has been put in pla s, on the creation and establishment of protected areas. during a time of growing demands on re ing the contribution that the brazilian protected areas make to the brazilian economy will help |
| 7515 | 1 | which two individuals that colonize the protected areas of the western mediterranean coasts 3 w
|
| 12598 | 2 | versity and carbon storage. peat use in soil improver materials has almost ceased but the growi
hip project to protect and enhance peat soils and the habitats they support. |
| 12667 | 2 | in broad habitats, landscape features, soil, vegetation and freshwaters. the survey is an impo
ion impacts, water framework directive, soil strategy and climate change programme. new methods |
| 7195 | 1 | ce of common birds are complex. indeed, agro-ecosystems are characterized by a scenario approac
|
| 515 | 1 | – policy/science on one hand and rural/urban on the other – that coexist in a strained relatio
|
| 7160 | 4 | a such as the opening of the landscape, urban sprawl of the agricultural landscape, agricultura
g of the landscape, urban sprawl of the agricultural landscape, agricultural decline, the closu e closure of the landscape, artificial, urban densification ... this approach will be complemen projections under scenarios of various urban development. the same type of approach will be us |
| 11036 | 1 | of spilled petroleum released to anoxic groundwater or sediments. there is even the possibility
|
| 2116 | 1 | tween farmers and geese foraging in the agricultural landscapes have intensified. finding optim
|
| 2542 | 1 | tain pastures to industrial farming and urban sprawls in order to ascertain how people diagnose
|
| 15522 | 1 | on stocks and net primary production of terrestrial ecosystems in peninsular spain, with a decl
|
| 10172 | 3 | tion and loss of viability of pollen in soils and this restricts understanding of its role in n
len of different species in contrasting soils, and when attacked by specific microorganisms and attacked by specific microorganisms and soil communities, and determine the period for pollen t |
| 12033 | 1 | biodiversity of chemosynthetic ecosystems in the deep ocean discovered
|
| 12460 | 1 | ically optimal level of exploitation of european ecosystems under changing climatic conditions
|
| 12465 | 1 | ically optimal level of exploitation of european ecosystems under changing climatic conditions,
|
| 12637 | 16 | soil protection is of strategic importance for protecti
nce for protecting uk food security, as soils are responsible for the national provision of foo o provide evidence on which to base its soil protection strategy. given defras aim of developin en defras aim of developing sustainable soil managment across the uk, and tackling soil degrada l managment across the uk, and tackling soil degradation threats by 2030, this project will pro ovide a synthesis of defra commissioned soils research to date, and provide a vision for future last 20 yrs will be assessed within the soil natural capital stocks and soil ecosystem services hin the soil natural capital stocks and soil ecosystem services framework, and the research con h conducted on threats that may degrade soils will be evaluated within this context. the threat within this context. the threats to uk soils are expensive with half of england’s farmers havi h half of england’s farmers having seen soil erosion on their land, which costs british agricul ver, the annual cost of flooding due to soil degradation has been conservatively estimated at b he cost of not sustainably managing our soils it is imperitive that research provides solutione s have developed plans to protect their soils, in order to ensure that they can be sustainably edge of the changes taking place in our soils, and the effects of these changes on the goods an s on the goods and services provided by soils. this synthesis will put the last 20 yrs of defra |
| 7672 | 5 | the world wide population will live in urban areas. while public, urban plannings are per se p
will live in urban areas. while public, urban plannings are per se predictable; their consequen ion and expected ecological services in urban soils and artificialized surfaces are poorly unde d expected ecological services in urban soils and artificialized surfaces are poorly understood aces are poorly understood. the project urban microorganism diversity . these comparisons will |
| 7105 | 1 | pecially agricultural areas, especially grasslands said surfaces
|
| 12626 | 13 | soil erosion in england and wales was not considered to
f these studies underline the fact that soil erosion rates may not be high, the consensus in th the consensus in the literature is that soil erosion in england and wales often occurs at an ac detrimental both to the quality of the soil . numerous different techniques have been used to ent techniques have been used to assess soil erosion in england and wales. these include: direc catchments to observe erosion, tracing soil erosion using geochemical and radionuclide analysi as the erosion from intensively-managed grasslands has best been captured via detailed monitori hesis of all the information describing soil erosion in england and wales and a framework that objectives to improve understanding of soil erosion in england and wales and to develop a way and to develop a way forward to monitor soil erosion. objective one will be to deliver an in-de y world-leading experts in the field of soil erosion, who have already contributed dozens of re ed dozens of research papers describing soil erosion in england and wales to the research liter a consensus as to how we should monitor soil erosion in the future. objective two will bring to |
| 12586 | 7 | ngoing which are raising the profile of soil protection and use. with this greater consideratio
use. with this greater consideration of soil comes the need to determine the state of uk soils s the need to determine the state of uk soils and to develop processes to monitor future change evelopment and implementation of future soil and environmental policy by providing evidence on y by providing evidence on the state of soils. this project forms part of the programme of work e of work funded and overseen by the uk soil inicators consortium and will, building on previou on previous uksic work, design a new uk soil monitoring scheme. the project is being managed by |
| 14538 | 2 | water redistribution between soil layers carried out by roots may have an important
e. such redistribution can be upwards , soil type, the organic matter content, the depth of wat |
| 13375 | 1 | accumulating plants grown in serpentine soils and cadmium resistant species collected from zinc
|
| 11779 | 19 | tion of the biodiversity and biomass in soils and consequently they play an essential role in m
y play an essential role in maintaining soil processes which, ultimately, regulate the function ultimately, regulate the functioning of terrestrial ecosystems. the use of molecular techniques dominant bacteria present in a range of soil types, though there is still a lack of understandi e controlling factors behind a range of soil processes, and in addition may provide a fundament future use of biological indicators of soil quality. recently it has been shown that ph is the ining the richness of bacterial taxa in soil communities, and additionally there is an emerging othesis that the nutrient status of the soil dictates the ratio of two abundant groups of soil tes the ratio of two abundant groups of soil taxa. we aim to disentangle this relationship in a this relationship in a diverse range of soil types. specifically we seek to firstly asses the r determining the identities of dominant soil bacteria, and then we will address how different n ditional environmental variables affect soil bacterial biodiversity. we will do this by assessi rsity. we will do this by assessing all soil samples taken as part of the countryside survey 20 t of the countryside survey 2007. these soil samples will be thoroughly characterised with resp horoughly characterised with respect to soil chemistry and overlying vegetation as a core eleme of the countryside survey. using these soils will allow us to correlate several key soil varia will allow us to correlate several key soil variables with specific changes in members of the undamental questions on the controls of soil bacterial community diversity, we also seek to que e usefulness of microbial indicators of soil functionality. therefore, once taxonomic relations |
| 12292 | 1 | rotations and inoculum build up in the soil as other important susceptible crops such as lettu
|
| 12645 | 1 | low for the legal designation of marine protected areas using the site-selection algorithm marx
|
| 11118 | 1 | riments, food web elucidation and plant-soil interactions.
|
| 12245 | 1 | e and enhancing the biodiversity in the farm ecosystem. a number of ifm components in livestock
|
| 7678 | 1 | sphere is analogous to its influence on soils, but it can occur much more rapidly in response t
|
| 14336 | 1 | ropical ant communities to rainfall and soil conditions. the paraguay dry chaco, with little al
|
| 10040 | 1 | tes, but in pots so that we can control soil conditions and the densities of neighbouring indiv
|
| 12023 | 1 | ification of disturbance regimes and of soil fertility, or indirect, via changes in the structu
|
| 1936 | 2 | ty in dutch heathlands and species-rich grasslands have declined severely during the last decad
es of heathland and species-rich acidic grassland in relation to the distance to the nearest se |
| 7138 | 2 | ion of populations of various groups of soil invertebrates and litter invertebrates that separa
ais species to predict the responses of soil invertebrates to land use change. |
| 185 | 1 | his is a type of seminatural calcareous grasslands, nowadays occurring in a landscape as a netw
|
| 14675 | 3 | the presence of gypsum in the soil determines the development of a vegetation of grea
environments, with easily erosionables soils and arid and semiarid conditions, revegetation is development of plant species in gypsum soils. under this hypothesis, the initial aim of the pr |
| 10182 | 2 | their prey in the control and improved grassland treatments at sourhope. a molecular dietary a
al role of higher trophic levels in the soil at sourhope and their effects on the plant communi |
| 13468 | 8 | and species diversity within arable-to-grassland successions on öland and in s germany – in lo
ion satellite data in the monitoring of grassland quality. an earlier phase of the project indi s that are characteristic components of grasslands with a long historical continuity on öland a ve high frequencies in relatively young grasslands. we will explore the chronology of species-e fferent spatial scales within arable-to-grassland successional chronosequences. to what extent are alpha and beta diversity related to grassland age/successional stage do we need to change o management of species diversity in old grasslands to include the dynamics of species-populatio ecies-populations in early successional grasslands on a european scale, we will seek generaliti |
| 421 | 2 | ty and biodiversity also has impacts on soil communities, leading to an expected commensurate r
istory traits increasing the ability of soil fauna to disperse would be more prevalent in commu |
| 15065 | 1 | cobacteria are frequently isolated from soil, water, air and clinical samples. both bacterial g
|
| 13878 | 14 | soil communities are among the most species-rich commun
ove- and belowground organisms say that soil processes can function at low levels of species ri on at low levels of species richness in soil. this is due to a low degree of species specific l ee of species specific links within the soil food web that maintain a high redundancy in functi cific interactions between organisms in soil food web we propose the use of techniques that wil d a high resolution of the structure of soil food webs. we will: identify the direction and spe ngi and fungal feeding invertebrates in soil food webs. nested pcrs of dna extracts of soil ani od webs. nested pcrs of dna extracts of soil animals and soil will identify fungal dna sequence crs of dna extracts of soil animals and soil will identify fungal dna sequences to species. the thus the feeding specialization of the soil animals. we will: identify the structure of food w detecting stable 13c isotope ratios of soil organisms. analysis with gc-irms of signature plfa ysis with gc-irms of signature plfas of soil microorganims and of soil animals will determine t ture plfas of soil microorganims and of soil animals will determine their trophic levels in the etermine the structure and diversity of soil food webs under influence of different plant commu |
| 11874 | 1 | ooking in detail at competition between soil and plants for organic and inorganic nitrogen. ult
|
| 10034 | 5 | esponsible for nitrogen cycling in acid soils nitrification is essential to the cycling of nitr
nsequences. ammonium can be retained in soil, but after conversion to nitrate, it can be readil phere. approximately 30% of the world s soil can be considered acid . the findings will benefit n cycling in natural and managed acidic soil systems. the findings will also be important to re for the emission of nitrous oxide from soil. |
| 10255 | 4 | ion and store up to one-third of global soil carbon reserves. their stability under future atmo
the stability of current vegetation and soil microbial processes. sub-arctic heath systems are also investigate whether variations in soil temperature and moisture content will interact wit ract with the future capacity of arctic soils to retain sequestered c under future elevated co2 |
| 2022 | 4 | estuaries and bays harbouring mangroves and seagrass beds provide important food sour
if the higher densities of juveniles in mangroves/seagrass beds never reach the reef fish popul survival of juvenile fish is higher in mangroves/seagrass nurseries than on the reef, and whet lity depends on input of juveniles from mangrove/seagrass nurseries versus coral reef, and on t |
| 10817 | 1 | ir herbivores. there are many important grassland systems that support a wide range of herbivor
|
| 11049 | 1 | ir herbivores. there are many important grassland systems that support a wide range of herbivor
|
| 11562 | 1 | ir herbivores. there are many important grassland systems that support a wide range of herbivor
|
| 11829 | 1 | ir herbivores. there are many important grassland systems that support a wide range of herbivor
|
| 11441 | 1 | of utilisation of new and old carbon in soils and peats by the microbial biomass to be assessed
|
| 10211 | 2 | soils contain vast numbers of organisms, yet their dive
communities, saprotrophic bacteria and soil mesofauna, and to determine if c can regulate thei |
| 10944 | 8 | ery similar needs for a small number of soil resources, most notably for nitrogen, which until
take a variety of nitrogen forms in the soil, including many organic forms such as amino acids. ts may be able to avoid competition for soil nitrogen by using different forms of nitrogen that forms of nitrogen that are available in soil. there is a certain amount of evidence that this m ogen forms that commonly occur in these soils. we will also test whether plants have to compete itrogen limited ecosystems, notably the soil microbes that are know to be effective competitors ogen forms from each other, and whether soil microbes also use different nitrogen forms from th ity of their preferred nitrogen form in soil in other words, the most abundant plants preferent |
| 11492 | 2 | the c4 photosynthetic pathway dominate grassland ecosystems and cereal production in warm clim
ty and water-use in natural climate and soil conditions, using a sub-sample of the nadp-me c4 a |
| 14122 | 4 | acterized by the complex topography and soil distribution. although good spatial-correlations b
ial-correlations between vegetation and soil have been found, the extent of soil’s role on the and soil have been found, the extent of soil’s role on the long-term vegetation dynamics is lit term spatial dynamics of vegetation and soil, even though widely assumed but little known, is e |
| 7463 | 1 | hange, acid deposition, and land use on terrestrial ecosystems, and the resultant effects upon
|
| 14199 | 16 | biodiverse seminatural grasslands have practically disappeared from europe due
is increasing interest to restore those grassland communities and landscapes and in estonia the estoration management in dry calcareous grasslands. we aim to study calcareous grassland vegeta grasslands. we aim to study calcareous grassland vegetation dynamics under changing land use, y used, intensively used, and disturbed grasslands, and evaluate their ‘restoration potential’ ionally managed species-rich calcareous grasslands will serve as references. we shall also addr ular, we shall focus on the role of the soil seed bank as a potential source of plant diaspores in the establishment and performance of grassland plant species. because land use intensificati fungi in ecosystems, and overgrowth of grasslands by scotch pine may change the dominating sym l taxa may inhibit the establishment of grassland plant species even if diaspores are present. s in traditionally managed semi-natural grassland plant community composition and diversity und s in traditionally managed semi-natural grassland plant community composition and diversity und ects of changing land use on the viable soil seed bank what are the effects of changing land us i, present both as viable spores in the soil and functioning hyphae in plant roots is the estab in plant roots is the establishment of grassland plant species limited by the lack of appropri changes, as well as advice managers of grasslands. |
| 14691 | 1 | conditions. 2 to study the dynamics of soil processes, mainly mineralization and nutrient avai
|
| 14690 | 1 | know the importance of the dynamics of soil processes affecting plant regeneration. lastly, we
|
| 14689 | 1 | conditions. 2 to study the dynamics of soil processes affecting plant regeneration. 3 to study
|
| 7028 | 3 | ines plant diversity and functioning of grassland ecosystems is a major goal of contemporary ec
ity diversity and structure by creating soil microsites enriched in nutrients and/or amf. the l n and symbiosis and consequently affect grassland diversity and functioning. |
| 11723 | 2 | mangroves may provide nursery sites for commercially an
erature, salinity and delta 13c between mangrove, seagrass and coral reef biotopes. these three |
| 12601 | 2 | nd partners with a regional overview of soil resources, their extent and use and their key func
standing of the strategic importance of soil resources could help the regional assembly deliver |
| 13387 | 1 | he most frequent species in the natural grassland vegetation, e.g. festuca, agropyron, poa, bro
|
| 15530 | 3 | nk structural and functional changes in semiarid ecosystems, and identify critical points of de
project will focus on key functions in semiarid ecosystems such as water and soil conservation n semiarid ecosystems such as water and soil conservation, and plant productivity. the specifc |
| 12040 | 2 | patrimonial value similar to corals or mangroves in tropical areas. these forests are subject
ge needed for the delineation of marine protected areas and for sustainable management of marin |
| 7182 | 3 | radication through the seed bank in the soil. as soon as the carpobrotus spots have a large sur
er eradication of witch - claws lies in soil erosion phenomena that occur when the slope is ste in the biodiversity and functioning of coastal ecosystems invaded |
| 13466 | 1 | scale natural fires in modern times on soil and water chemistry as well as on biodiversity and
|
| 7635 | 4 | ustrial activities are causing a strong soil contamination by metal species. this is a very ser
s is a very serious problem because the soil performs essential functions that largely determin w interesting solutions to rehabilitate soil contaminated by heavy metals. it consists in cover avy metals. it consists in covering the soil with plant species tolerant to heavy metals, for i |
| 2502 | 2 | xperiment in unusually rapid selection. coastal ecosystems in general, and intertidal systems i
ive model of climate induced changes in coastal ecosystems and appropriate societal responses. |
| 14546 | 1 | planning and management of networks of protected areas, due to the possibility of appraising t
|
| 11410 | 1 | h parasite genetic diversity in shaping grassland community structure. the work will provide va
|
| 9964 | 1 | h parasite genetic diversity in shaping grassland community structure. the work will provide va
|
| 7688 | 2 | ese two scales is that our proposal. in agricultural landscapes we identify three main types of
he amount of structural continuities in agricultural landscapes relative to the amount of habit |
| 10722 | 2 | on can act by increasing the acidity of soil, because base cations such as calcium are released
the amount of available nitrogen in the soil, a process which is often referred to as eutrophic |
| 7603 | 6 | ecological services provided by living soil are essential. for which the Alps mountains, the P
ich the Alps mountains, the Protocol on Soil Protection to the Alpine Convention is a good stat cological functions and services of the soil, for their wise use. face this international, Euro al, European and national context where soils are mentioned as an essential resource for sustai y to promote the biological improvement soils affected by daily human activities and global cha ey element that can effectively control soil adaptability face of global change. it proposes to |
| 7636 | 4 | the study of urban ecosystems is a major environmental challenge. th
the first ring around paris. yet these urban ecosystems, including their soils have jusquici b these urban ecosystems, including their soils have jusquici been little studied from the perspe amental knowledge on the functioning of soils in general, magnified by the comparison of treatm |
| 15131 | 1 | solated from diverse habitats including soil, water and marine sediments. recently, strains of
|
| 11071 | 1 | ation to previously established natural protected areas.
|
| 7606 | 2 | gardening practices and architectural, urban and landscape forms that structure the gardens th
d gardens for ecological engineering in urban areas this research aims to provide answers to th |
| 2527 | 2 | xperiment in unusually rapid selection. coastal ecosystems in general, and intertidal systems i
ive model of climate induced changes in coastal ecosystems and appropriate societal responses. |
| 7198 | 2 | se systems alter the functioning of the agro-ecosystem and the ecological services: biomass pro
cological services: biomass production, soil conservation and biodiversity, and carbon storage, |
| 15294 | 17 | soil is a natural resource with a high socio-economic v
tic changes which are irreversible. the soil biota is an essential pillar for the development o the major causes of disturbance to the soil. discharges and wastes have a major impact on the ce of risk for heavy metal pollution to soil, air, surface water and groundwater. metals and me llution to soil, air, surface water and groundwater. metals and metalloids, commonly referred t cation and monitoring of its content in soil in order to develop risk assessment systems. the r is the reactivity of metal species with soil factors such as watering regime, ph, organic matte anisms assessing the level of metals in soil is the first step to determine risk level. however se diagnosis of the risk of toxicity in soil, and the extrapolation of the results requires val te the effect on the composition of the soil biota, to determine the bioaccumulation of metals etermine the concentration of metals in soil and assess your risk, carries a high budget for so ss your risk, carries a high budget for soil analysis and requires specialist taxonomists quali mists qualified to assess the effect on soil biota. in this sense the new technologies of molec r determining the presence of metals in soil samples, and the development of sensors capable of u, zn, ni, cd, pb, cr, hg, as and se in soil 2- to study the structure of the soil invertebrate n soil 2- to study the structure of the soil invertebrate community, assessing the effect of me and to assess metal transference in the soil food web 4- to design the methodology t |
| 15295 | 9 | until not long-time ago soils were considered a medium with an unlimited capabi
fects. it was in 1972 with the european soil act of the european council when it was recognized ean council when it was recognized that soils were a natural resource that needed a special pro s objective information in contaminated soils due to mining activities and specifically the pre f environment , arsenic and selenium in soils affected by mining activities 2. to evaluate the by mining activities 2. to evaluate the soil characteristics by means of basic physic and chemi mobility and disponibility of metals in soils 3. to analyse the spatial variability in the heav riability in the heavy metal content in soils, the available fraction and related edaphic param iques to evaluate relationships between soil and edaphic fauna in contaminated areas |
| 14230 | 1 | infrastructures, the rise in mobility, urban sprawl, agricultural practices and tourism are al
|
| 14807 | 6 | wetlands seem the only ecosystem type that has been lef
it of indicators that can be applied to wetlands, in general, and particularly to those located low to assess the ecological quality of wetlands in the most arid mediterranean regions, follow e aquatic and terrestrial phases of the wetlands, and on the relationships between them. this i . the validation of these indicators in wetlands from all around the iberian semiarid region , the ecological state of these peculiar wetlands. |
| 10062 | 1 | he presence of different substrates for soil development. such heterogeneity contributes to the
|
| 7661 | 6 | urban pigeon is an integral part of urban ecosystems wo
urban pigeon is an integral part of urban ecosystems worldwide. despite its pervasiveness i worldwide. despite its pervasiveness in urban areas and proximity to urban dwellers, there is l iveness in urban areas and proximity to urban dwellers, there is little known to scientists. ob rst is to better understand the role of urban pigeon as a reservoir and vector of diseases pote 1: epidemiology of diseases carried by urban pigeon 1- characterize the main pests potentially |
| 7203 | 4 | habitats that they all attend. european agro-ecosystems consist of a shifting mosaic of potenti
the ecology of plant- insect across the agricultural landscape puisquil conditions the possibil n between the different compartments of agroecosystem and the influence of the structure and co of the structure and composition of the agricultural landscape on the ecology of pests, pathoge |
| 214 | 1 | ce via host specificity and/or positive soil and litter feedback. through field expeditions and
|
| 6739 | 1 | nd cause serious economical damage. for soil animals the most likely mean of introduction is th
|
| 14124 | 3 | estoration of species rich semi-natural grasslands is considered one of the most important aims
the protection and management of these grasslands has been to protect rare or endangered speci of disturbances, created by traditional grassland management by mowing or grazing can be diamet |
| 12039 | 4 | the microbial biodiversity of french soils: an endangered patrimony to protect. title 1: cha
terization of the « beta » diversity of soil microbial communities on the scale of france soil bial communities on the scale of france soil is subjected to numerous environmental perturbatio e biological state and evolution of the soils. |
| 10720 | 6 | the grasslands in china are in a state of ecological crisis
l crisis. for example, about 33% of the grasslands on the qinghai-tibetan plateau, the largest he qinghai-tibetan plateau, the largest grassland unit on the eurasian continent, are degraded, of the original vegetation cover left. grassland degradation has important economic and enviro 80% of the rural poor in china live in grassland ecosystems and any further degradation of thi ew relevant policies and regulations on grassland management and poverty alleviation in china, |
| 15482 | 2 | ociation, facilitative interactions and soil degradation and how this, in turn, determines the
portance of plant-plant interaction and soil nutrients and runoff connectivity over a climatic |
| 10106 | 1 | s from n, to n+p, to p during long-term soil development. despite the important implications of
|
| 11402 | 9 | europe, extensively managed or restored grasslands are key elements of managed and natural land
for multifunctionality in semi-natural grasslands is missing. therefore, its translation into to guide policy and management of these agroecosystems, is limited. vital will test the general iple ecosystem services in semi-natural grasslands, and its vulnerability to changing managemen plained by the coupling among plant and soil microbial functional diversity, and its impacts on delivery. vital will focus on mountain grasslands where traditional livelihoods relying on mul he maintenance of fertility in mountain grasslands, how these are perceived to be affected by m plant species with different traits on soils from differently managed grasslands. wp4 will tes raits on soils from differently managed grasslands. wp4 will test the robustness of this model |
| 481 | 3 | he maintenance of fertility in mountain grasslands, how these are perceived to be affected by m
plant species with different traits on soils from intensively / extensively managed grasslands from intensively / extensively managed grasslands. analyses of realised plant and microbial fu |
| 13987 | 3 | d to an increasing interest in managing agricultural landscapes for enhanced multi-functionalit
ns among multiple ecosystem services in agricultural landscapes. the core hypothesis is that di pt and non-linear. we will focus on two agricultural landscapes, one in sweden and one in south |
| 7675 | 4 | use and climate change for the grenoble urban region in the french alps. we will capitalize on
al multi-criteria analysis. besides the urban region, we will focus on two case study sub-syste ty and a mixed landscape of forests and grasslands in a mountain range south of the city. as be . these scenarios will build on current urban planning exercises by public authorities, and dow |
| 7629 | 8 | studying the functioning of urban ecosystems and ecosystem services that they provi
major environmental challenge. indeed, urban areas are characterized by extreme human impacts describe the impact of threats to non - urban areas for decades, and propose appropriate manage in the ecosystem service of pollination urban. the results obtained and the analysis of the per the ecosystem service of pollination in urban and non-urban areas. the ever increasing impact o service of pollination in urban and non-urban areas. the ever increasing impact of human activi , more than ¾ of the population live in urban areas, which currently cover nearly 20 % of the t xotic species reach extreme values in urban areas. well, this denotes the cities as a new bio |
| 1092 | 1 | es of the terrestrial parts of the lake watershed will concentrate on classifying procedures fo
|
| 15116 | 1 | ructural and functional biodiversity of soil and the aboveground plant communities. the propose
|
| 15117 | 1 | ructural and functional biodiversity of soil and the aboveground plant communities. the propose
|
| 14946 | 4 | appears to have pioneered the chemical soil theory. it was not unexpected, then, that a contra
cted, then, that a contrasting physical soil theory would emerge. the conflict between these tw objective, the vegetal communities and soils of dolomite and peridotites outcrops will be comp ompared between them and with limestone soils and communities. 2. to elucidate the most adequat |
| 15269 | 2 | both sites the n content in leaves and soils will be measured, as well as the soil solution an
soils will be measured, as well as the soil solution and streamwaters draining the study sites |
| 7123 | 3 | atter, the possibility of alteration of soil minerals and soil transfer opportunities to the sh
lity of alteration of soil minerals and soil transfer opportunities to the shaft a set of proce lter the composition and functioning of soil microbial populations. so we are in the situation |
| 538 | 2 | ams in the disciplines of geochemistry, soil microbiology, genomics and ecosystem processes are
ress key scientific issues in microbial soil ecology. these include assessing the impact of env |
| 15289 | 2 | fields and field boundaries related to agricultural landscape intensification and management .
diversity conservation in mediterranean agricultural landscapes differing in their agrarian int |
| 7202 | 5 | bial ecology in agricultural and forest soils and environmental issues related to it. the soil
environmental issues related to it. the soil is one of larger reservoirs of microbial diversity ver, are poorly understood. quality and soil fertility and mineral nutrition of plants, however bacterial and fungal communities in the soil. the modes of management and agricultural and fore he structure, diversity and activity of soil microbial communities and thereby alter the microb |
| 12507 | 1 | en they give no direct economic return. soil nutrient management and improvement of fertility b
|
| 11669 | 1 | the carbonaria frequency cline between urban manufacturing areas in northwest england and adja
|
| 14814 | 1 | te the effects of abiotic stress on two terrestrial ecosystems ecosystem composition, structure
|
| 14754 | 1 | of natural populations, the sampling of soil, plants and seeds of different populations in the
|
| 15216 | 2 | represented by kermes oak thickets in a protected area in the center of the iberian peninsula s
ions with selected species of scrub and grassland understory. quantifying variables of the resp |
| 14920 | 3 | climate exerts a major influence on soil organic carbon content and, consequently, there is
er the feedback response of carbon-rich soils to increasing global atmospheric temperatures. re l sinks resulting in the stimulation of soil organic matter mineralization with associated rele |
| 15397 | 1 | iation of insectivorous birds living in wetlands and their implications in a climate change sce
|
| 15384 | 1 | try to determine whether any changes in soil mycorrhizal fungal communities might be associated
|
| 2139 | 4 | the organisms themselves. microbes and soil fauna use litter and soil organic matter as energy
microbes and soil fauna use litter and soil organic matter as energy, carbon and nutrient sour te an increase in the mineralisation of soil organic matter by microbes and microarthropods, wh s have been carried out. the ability of soil organisms to adapt to a changing environment will |
| 2005 | 2 | soil-borne micro-organisms are the greatest source of b
earth, and plants drive the dynamics of soil-borne microbial communinities via the quality and |
| 13967 | 2 | ollination service to forbs in marginal grassland habitats by combining large-scale field exper
imated in large continuous semi-natural grasslands and in road-verges at different distance fro |
| 14469 | 1 | threat for the biological diversity of terrestrial ecosystems. the fragmentation of habitats a
|
| 13488 | 1 | ffects on the vegetation by influencing soil temperature, nutrient turnover and competition bet
|
| 14900 | 1 | sal is to ascertain how revegetation in agricultural landscapes, passive or active, affects div
|
| 13739 | 1 | alternative stable states in lakes and wetlands and how these transitions affect biodiversity
|
| 12576 | 1 | the effects of heavy metal additions on soil fertility and agricultural productivity.
|
| 1088 | 2 | onditions, litter quality, decomposers, soil factors, pollution and global warming, but the rol
model the biogeochemical cycles in the soil. in particular, no such studies have been performe |
| 11869 | 1 | ineages indicate major domain shifts in planktonic ecosystems and by observing and interpreting
|
| 11393 | 1 | peat, through examination of changes in soil hydrology and water quality. 2. provide a better u
|
| 15161 | 5 | ively the water restoration capacity of constructed wetlands. this fact derives mainly from the
associated microorganisms in treatment wetlands remain only partly understood at a molecular l y to analyze the microbial diversity in wetlands and to promote the enrichment and isolation of y of microorganisms both in natural and constructed wetlands. second- to use the emergent veget organisms targeting the nitrogen cycle. wetlands constitute real repositories of an enormous di |
| 10734 | 2 | ates and other small animals present in soil, ponds and marine environments and then extract th
ample freshwater, estuarine, marine and soil environments across different seasons and geograph |
| 10597 | 20 | ensively we understand little about how soil develops after ice has retreated. about one third
a wet desert environment where denuded soils harbour scant vegetation. as such this is an isla from continental influences in terms of soil colonisation. in iceland, currently, there are two mmer, uniquely, at these two locations, soil that has been covered since the little ice age bio d to monitor biochemical changes in the soil. typically, molecular analysis involves extraction lecular analysis involves extraction of soil dna or rna and amplification of genes that provide d diversity of the community. in mature soils, molecular analysis has revealed the existence of of considerable microbial diversity in soil and the existence of many groups with no cultivate re abundant and ubiquitous in temperate soils but, because none has ever been cultivated, we ha hysiological characteristics. to assess soil function we will look at how these soils play a ro soil function we will look at how these soils play a role in the cycling of nitrogen. by using his material. we can then track how the soil processes the nitrogen from the plant litter. inst anisms we study the full process of the soil. if the process is effective then it may be conclu f mature systems can develop from these soils that have been contained the glacier. to place th to place the results in context, mature soil from neighbouring locations will also be sampled. g locations will also be sampled. these soils will also be examined using the same methods as d tional attributes have developed in the soil over time or if they were present from this seed o ve we are collaborating with a group of soil scientists in iceland who will assist in the field and in the setting up of the functional soil tests at their research facility near reykjavik. n correct weather conditions, but careful soil survey and robust sampling methods are essential t |
| 10661 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 10912 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 11158 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 11170 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 11420 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 11421 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 11701 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 11702 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 9896 | 1 | ins a mix of agricultural, forestry and urban land. it is the site of a community forest and th
|
| 12305 | 1 | rbon from cropping of high carbon stock soils. although co-products currently used in animal di
|
| 11747 | 2 | calcareous grasslands are among the most species-rich plant commun
lcicole species to thrive on calcareous soils will contribute to the development of strategies |
| 7037 | 5 | ften can be discerned from satellite as agricultural landscapes bear the signs of different adm
e from a complete analysis of the total agro-ecosystem in question. thus a whole seigniorial es ples where natural boundaries define an agro-ecosystem distinct from others under the same pers ary study on population, production and agro-ecosystem as the three basic factors of the develo of environmental matters such as water, soil and infrastructure, the environmental history data |
| 7306 | 4 | o manager of the aggregate structure of soil and its cultivability. moreover, globally, the dec
ity. moreover, globally, the decline in soil carbon stocks is likely to accelerate global warmi t farming systems on the functioning of agro-ecosystem. it is used for a number of indicators o agrosystem to limit air pollution, and groundwater. the aim is to assess how the proper functi |
| 15012 | 1 | ronments. the first includes the saline wetland of fuente de piedra and in the bay of cadiz. th
|
| 13319 | 1 | the effects of precipitation change on terrestrial ecosystems in order to bring together inter
|
| 7246 | 4 | ycle in its wastewater and rainwater in urban dimensions. more precisely, it is to achieve a de
scales * assessment of water flows and urban-background * impact of wastewater discharges and gical and hydrometeorological models in urban areas, and the development of aid to the understa ools, qualitatively and quantitatively, urban water to optimize the operation of sanitation sys |
| 6894 | 1 | only in agricultural fields but also in urban areas and national parks. special emphasis is giv
|
| 13322 | 1 | scientists to integrate river, lake and wetland ecosystem science at the catchment scale. it fo
|
| 14822 | 2 | valuate the performance of the existing protected areas networks in the iberian peninsula to co
analyze the performance of the iberian protected area network, and identify priority areas for |
| 7561 | 1 | of preservation of bacterial consortia soil extracts on different characteristic parameters of
|
| 14586 | 1 | ational programmes, a detailed study of soil-plants-hydromorphy interactions is proposed which
|
| 7415 | 1 | dly changed the functioning of european agro- ecosystems, causing significant erosion of all bi
|
| 12627 | 7 | .introduction a total of 98 out of 2666 soil cores taken for countryside survey in 2007 that: ‘
r countryside survey in 2007 that: ‘the soil ph data show an increase over time in the frequenc values approaching ph 9 in some plots. soil ph values in excess of 8.3 indicate that calcium c ate solubility is no longer controlling soil ph and there is an influence from sodium salts acc e from sodium salts accumulating in the soil. two of the sample points with the highest ph valu , there may be abundant sodium in these soils. the remaining sites are further west in oxfordsh can lead to sodium accumulation in the soil’ |
| 15079 | 1 | anspiration, water budget components of soil layer and water stress of land surface vegetation
|
| 13716 | 1 | n of biodiversity in different types of agricultural landscapes, e.g. intensively farmed plains
|
| 1103 | 2 | ivity will depend also on the continuum soil-plant-climate and this continuum has to be include
rowth and photosynthesis translocation, soil water fluxes and solute transport. with the conclu |
| 13978 | 1 | unuous forest landscapes and fragmented agricultural landscapes will be reared in the lab and t
|
| 13323 | 1 | to three major interacting elements of terrestrial ecosystems: trees, phytophagous insects and
|
| 7716 | 3 | stem functioning and the maintenance of soil fertility, our work should lead to be taken into a
aken into account in the legislation on soil protection, research in agronomy and plant breedin gn steering the ecological functions of soil ' and also the sub- axis draw new precision agricu |
| 14740 | 1 | subterranean ecosystems represent perfect natural labor
|
| 15293 | 2 | onary processes in chronically polluted soils, and contributes to the foundation of the paradig
es to the foundation of the paradigm of soil ecosystem health and its impairment by chemical po |
| 10470 | 1 | re less adaptable to living in polluted soils, and are less able to tolerate extreme environmen
|
| 11415 | 1 | re less adaptable to living in polluted soils, and are less able to tolerate extreme environmen
|
| 6784 | 2 | tional and ecological farming system on soil biological activity and yield. within the two farm
t of plant nutrition, crop rotation and soil amelioration and prove the authenticity of them. |
| 6947 | 1 | d monitoring of the most characteristic grasslands of the pannon eco-region and comparing them
|
| 6772 | 1 | plant and soil samples of heavy-metal load experiment in nagyhörc
|
| 12763 | 2 | sed project aims to further investigate urban badger behaviour and ecology in order to identify
sustainable solutions to problems that urban badgers cause. |
| 11537 | 1 | petition on plant performance along the soil moisture gradient. if hypothesis a is correct, the
|
| 15401 | 1 | remediation as a viable option to treat soil pollution by polycyclic aromatic hydrocarbons . th
|
| 10511 | 1 | henotypic and ecological consequence of soil pollution to be linked.
|
| 12196 | 4 | ensity grazing options for agricultural grassland that aim to deliver substantial benefits for
sts and complexity for farmers. grazing grassland less intensively should confer a range of wid ing reduced fertilizer inputs, improved soil structure, reduced soil erosion and run-off, enhan nputs, improved soil structure, reduced soil erosion and run-off, enhanced pollinator services |
| 12198 | 1 | grassland is the predominant habitat in the agri-enviro
|
| 14228 | 1 | on and colonization patterns in altered grassland habitats. original diversity consists of spec
|
| 14634 | 1 | ng winds, summer high radiation or high soil surface temperature. the combination of these fact
|
| 14201 | 1 | treeless calcareous grasslands in northern europe . we analyse the effect o
|
| 7548 | 1 | conducted in 1982 in a new collection. agroecosystem is studied creole garden, traditional sys
|
| 10294 | 8 | y by methanogenic bacteria in anaerobic soils and sediments much of which is oxidised at the ae
d at the aerobic-anaerobic interface in wetlands or overlying aerobic soils before it is releas erface in wetlands or overlying aerobic soils before it is released to the atmosphere, thereby issions of methane into the atmosphere. wetlands and soils are therefore important sinks for me thane into the atmosphere. wetlands and soils are therefore important sinks for methane, consum rophs, which appear to be widespread in wetlands and soils, regulate their methane oxidation sy appear to be widespread in wetlands and soils, regulate their methane oxidation systems and how tive methanotrophs in peat and landfill soils in order to address the hypothesis that in certai |
| 11660 | 2 | pplications for the management of other wetland sites throughout europe. the studentship aims t
star carr and for preservation at other wetland sites, particularly acidic sites, will be fully |
| 12511 | 17 | soil quality is an important consideration for the succ
ainable farming systems. traditionally, soil quality has been assessed primarily on physical an lowly over time, and may poorly predict soil functions. biological properties, which respond mo nsitive indicators with which to assess soil health, but are not widely considered. worldwide, and physical indicators when assessing soil health. for example when measuring potential impac s of heavy metals and pesticides on the soil biota. however, the approaches to use soil indicat l biota. however, the approaches to use soil indicators to assess soil health vary widely even oaches to use soil indicators to assess soil health vary widely even between regions within cou mical and physical indicators to assess soil health in farming and related systems. this will i iodiversity and function in relation to soil health, and soil health assessment in organic farm unction in relation to soil health, and soil health assessment in organic farming systems. the red. international approaches to manage soil health, such as the use of inoculants and changes cal, chemical or physical assessment of soil health in farming or other relevant systems is con l, chemical or physical contributors to soil health in the systems identified have been interpr view international approaches to manage soil health 4.compare the relative merits of internatio , chemical and physical contributors to soil health with current uk approaches based on functio and physical components to address the soil health concept in farming systems, including futur |
| 15577 | 2 | agricultural landscapes occupy 40% of the available lan
ns. previous work has demonstrated that agricultural landscapes which contain significant areas |
| 12600 | 11 | soil is the essential growing medium for our food, timb
in the disturbance of large volumes of soil resources annually. topsoils may be stripped and s compact and impermeable. any damage to soil quality affects the long-term functioning of the s ffects the long-term functioning of the soils and has an impact not only on ecological diversit r recharge and water quality. the first soil action plan for england, 2004-06 recognises that t ognises that there is a need to improve soil management practice on construction sites and iden pportunities for the sustainable use of soil material. consequently this project will: · review ect will: · review current practices of soil management on construction and development sites, , · identify constraints to sustainable soil use and re-use, whether economic or planning-relat endations on how to improve sustainable soil use at construction and development sites. much of uce a good practice note on sustainable soil use on construction and development sites. |
| 15042 | 7 | rrent knowledge of food web dynamics in terrestrial ecosystems is limited by the scarcity of st
generated by different shub species on soil characteristics and to relate their effects on soi eristics and to relate their effects on soil macroinvertebrate distribution, and b to experimen ave dealt with the effects of shrubs on soil properties and soil organisms in fertile islands, ffects of shrubs on soil properties and soil organisms in fertile islands, none of them have ta uires to consider the feedbacks between soil organisms their effects as ecosystem engineers inc n rates of water and nutrients into the soil. the obtained results will increase our knowledge |
| 12235 | 10 | ndations to be generated for individual grassland fields according to the intended management `
r, will not provide recommendations for grassland since these were not available in time. inclu cluding functionality to generate rb209 grassland recommendations will meet the following requi on and ‘validation of the new system of grassland recommendations, to test industry reaction an ements. coding and provision of the new grassland recommendations into planet is an essential s step/milestone in this process so that grassland recommendations can be widely and easily gene at the farm and field level. 2. the new grassland recommendations are complex, and ideally suit ed from new research. 3. the absence of grassland recommendations in planet v3 will significant significantly detract from its value to grassland farmers, the potential for obtaining feedback roving nutrient management practices on grassland farms. |
| 6876 | 1 | subordinate species in a wide range of grasslands. our comparative studies with specific trait
|
| 9931 | 3 | are largely restricted to nutrient-poor grasslands and are of significant conservation interest
to measure the vertical distribution in soil of mycelia. detailed mapping of fruitbodies of the f the various plot treatments and local soil variations at sourhope to be quantified. 15n-enric |
| 10529 | 5 | ve on the chemical forms of elements in soil. the proposal aims to determine the physiological
u building on results of these studies, soils collected from mod testing ranges at kirkcudbrigh cquisition of du from real contaminated soils. impacts of plant growth on du distribution and c istribution and chemical forms in these soils will be determined. in addition, key processes af ombining expertise in plant physiology, soil science and analytical chemistry to identify proce |
| 10457 | 1 | through river basins. in recent years, groundwater-fed rivers throughout lowland england have
|
| 15505 | 2 | ecosystem services through changing the soil environment. in this proposal it is intended to su
o survey the fire-induced shifts in the soil microbial genomes, biogeochemical functions and co |
| 13757 | 2 | l disturbance agency of many forest and grassland ecosystems that contributes to species dynami
e to foster biodiversity in three major european ecosystems. fireman will focus on fire-biodive |
| 9881 | 2 | l disturbance agency of many forest and grassland ecosystems that contributes to species dynami
e to foster biodiversity in three major european ecosystems. fireman will focus on fire-biodive |
| 473 | 2 | l disturbance agency of many forest and grassland ecosystems that contributes to species dynami
e to foster biodiversity in three major european ecosystems. fireman will focus on fire-biodive |
| 15569 | 2 | l disturbance agency of many forest and grassland ecosystems that contributes to species dynami
e to foster biodiversity in three major european ecosystems. fireman will focus on fire-biodive |
| 222 | 2 | ce 1930-ies, total area of semi-natural grasslands is decrease nearly ten fold, the agricultura
ill be described newly for species-rich grassland and forest communities. the change in their a |
| 10705 | 3 | into and through the components of the soil structure. this will be achieved by the innovative
hieved by the innovative combination of soil micromorphological analysis with laser ablation is different labelled c inputs within the soil structure to assist with the overall modelling of |
| 7620 | 1 | the lichen in winter. swedish forestry, soil preparation by following clearcutting, destroys th
|
| 210 | 1 | f pollinator abundance and diversity in agricultural landscapes of america, asia and europe giv
|
| 7145 | 2 | we showed that the former use of forest soils for agriculture engendered changes in the composi
l the very long -term sustainability of soil fertility changes induced by ancient custom, in a |
| 13464 | 1 | boreal forest soils are reservoirs of enormous biodiversity and conta
|
| 13459 | 1 | erally leads to short-term increases in soil nutrient availability followed by increased leachi
|
| 11691 | 1 | de mineral phase which forms in natural soils under reducing conditions. in addition, this mine
|
| 9942 | 1 | de mineral phase which forms in natural soils under reducing conditions. in addition, this mine
|
| 7710 | 2 | e respective shares of genetics and the soil in the composition of the aroma. we aim to improve
ical methods. we also wish to establish soil production potential indicators, especially after |
| 10009 | 1 | the hydrology, soils and ecology of moorland are vulnerable to local e
|
| 10773 | 1 | onal and international policy on marine protected areas for wide ranging marine mammals. potent
|
| 9872 | 1 | platforms and trackways and the use of wetlands in prehistory. research demonstrates that the
|
| 1945 | 4 | orms an empirical meta-evaluation using soils from biodiversity trials to investigate how plant
ersity, plant functional diversity, and soil amendments, influence soil suppressiveness against versity, and soil amendments, influence soil suppressiveness against below-aboveground inverteb wground crop protection by agricultural soil biodiversity measures in relation to farmers incom |
| 14136 | 1 | mbinations of plant and fungal species, soil- based and monoxenic culturing of am fungi, real-t
|
| 13939 | 7 | gely unknown. stratified mineral podzol soils exhibit a range of different soil conditions. pat
dzol soils exhibit a range of different soil conditions. patterns of species diversity in relat rns of species diversity in relation to soil horizon have been demonstrated for fungi colonisin ot tips and forming mycelia in a podzol soil. the aim of this project is to identify functional r the large diversity of these fungi in soil. field studies of the realised niche of different ribution at a spatial scale relevant to soil heterogeneity and mycelial size. experimental stud ring the realized niche of a species in soil with its potential niche in vitro will demonstrate |
| 7020 | 1 | n, the maintenance of water quality and soil fertility, carbon storage, the mitigation of the e
|
| 418 | 3 | dies have measured interactions between soil microorganisms and plant diversity. our purpose is
ities in fertilized versus unfertilized grasslands. the study was carried out in a permanent gr he study was carried out in a permanent grassland in northeastern france using the same agricul |
| 7135 | 5 | ch program aims to improve knowledge of grassland agro-ecosystems. the innovative approach of t
aims to improve knowledge of grassland agro-ecosystems. the innovative approach of this projec elationship between plant diversity and soil microbial diversity in permanent grassland undergo d soil microbial diversity in permanent grassland undergoing various systems of organic and min icrobial diversity will be in permanent grasslands undergoing four types of fertilization. func |
| 14943 | 1 | n parts, to trampling and to changes in soil nutrient levels. we also study several aspects of
|
| 12034 | 2 | processes of interest for sylviculture, soil conservation and ladscape management. main results
sed ability to mobilize phosphorus from soil organic matter under drought conditions. il also a |
| 12466 | 1 | isheries project; enforcement of marine protected areas nationally; development of marine manag
|
| 10253 | 1 | in that way high resolution maps of key soil and vegetation variables can be constructed. compu
|
| 10254 | 1 | in that way high resolution maps of key soil and vegetation variables can be constructed. compu
|
| 10754 | 1 | in that way high resolution maps of key soil and vegetation variables can be constructed. compu
|
| 11529 | 1 | in that way high resolution maps of key soil and vegetation variables can be constructed. compu
|
| 11533 | 1 | in that way high resolution maps of key soil and vegetation variables can be constructed. compu
|
| 9994 | 1 | in that way high resolution maps of key soil and vegetation variables can be constructed. compu
|
| 11015 | 1 | the study of cooperative behaviour, the soil dwelling social amoeba d. discoideum. under favour
|
| 9991 | 1 | the study of cooperative behaviour, the soil dwelling social amoeba d. discoideum. under favour
|
| 10923 | 2 | onwards. these activities gave rise to soils and the development of the complex terrestrial ec
oils and the development of the complex terrestrial ecosystem. both rhizoids and root hairs are |
| 11200 | 2 | l be obtained directly from bacteria in soils at the unique rothamsted broadbalk experiment whi
onmental differences on biodiversity of soil bacteria, at the levels of the genes, the processe |
| 2027 | 1 | odies. they are important in nearly all terrestrial ecosystems, and several insect species have
|
| 15478 | 1 | l geographic area with basic, lime-rich soils in mediterranean eastern spain. our previous rese
|
| 15498 | 1 | ciated to nutrient-poor, acid sandstone soils which harbours a large proportion of the endemic
|
| 12043 | 1 | activities to promote candidate marine protected areas. to date the most important threat on p
|
| 7212 | 8 | biological and functional diversity of soil engineers madagascar, a wildlife group that soil p
neers madagascar, a wildlife group that soil plays a particularly important role in the functio ly important role in the functioning of soil. the study of the diversity of madagascar soils, b he study of the diversity of madagascar soils, biodiversity that they contain and the role of a and the role of agencies, major players soil functioning, is of utmost importance for the devel and functions of wildlife in madagascar soils will also be conducted. this knowledge is a prere projects related to the functioning of soils and ecosystems. the results of this project could to build a database on the diversity of soil macrofauna in madagascar and conserve species desc |
| 452 | 8 | biological and functional diversity of soil engineers in madagascar, a group of soil fauna tha
oil engineers in madagascar, a group of soil fauna that plays a role that is particularly impor cularly important in the functioning of soil. the study of madagascars soil diversity, of the b oning of soil. the study of madagascars soil diversity, of the biodiversity it encloses and the isms, main actors in the functioning of soil, is of greatest importance for the development of will in particular study the effect of soil usage and climate changes on the abundance, the di up projects linked with the function of soils and ecosystems. the results of this project could atabase on the diversity of madagascars soil macro-fauna and preserving the identified species |
| 13750 | 1 | environments are included at each site. soil temperature loggers are deployed at all summits si
|
| 11405 | 3 | n of pathogen sources and receptors are urban populations more vulnerable to pathogens than rur
ture health risks from pathogens in the soil-water environment to respond to these challenges w processes of pathogen interactions with soil and water; catchment risk assessment; water resour |
| 11584 | 3 | n of pathogen sources and receptors are urban populations more vulnerable to pathogens than rur
ture health risks from pathogens in the soil-water environment to respond to these challenges w processes of pathogen interactions with soil and water; catchment risk assessment; water resour |
| 12157 | 1 | roduce abundant, large seeds on fertile soils but is rarely allowed to flower. in a small-scale
|
| 7250 | 3 | ural areas is still largely build. peri-urban areas of ile-de- france are strategic places of h
rritories teach that the inhabitants of urban areas not only give importance to landscape aspec ld first be performed. it would be peri-urban areas, located in the green belt. * a spatial app |
| 14773 | 1 | ic compounds from lolium rigidum affect soil microbial populations, especially those functional
|
| 12706 | 1 | es for creation of open green spaces in urban settings. it will be managed by ciria, with a con
|
| 12707 | 2 | scoping review of the implications for wetlands of energy generation and distribution activiti
to issues concerning climate change and wetlands, linking as appropriate to work done in relati |
| 2186 | 1 | reas forestry methods and efficiency of protected areas, but also to monitoring of population v
|
| 13602 | 1 | storation in sweden each year, e.g. for grasslands. surprisingly, strategies for directing rest
|
| 13798 | 3 | search and in habitat monitoring within agricultural landscapes. much of the biodiversity value
apes. much of the biodiversity value of agricultural landscapes depends on the preservation of rch and in biodiversity conservation in agricultural landscapes. |
| 10270 | 3 | overnment psa targets for biodiversity, soil and water protection in uplands. restoration is of
is of crucial importance to protect uk soil carbon stores, as more than 50% of uk soil carbon l carbon stores, as more than 50% of uk soil carbon is stored in peat and is rapidly lost. rest |
| 10898 | 4 | we know in general terms that in the uk salt marshes occur between the elevation that correspon
owever, on the complex coastlines where salt marshes occur the elevation that a high water reac r year and the occurrence of particular salt marsh species and communities. the uncertainties i . the uncertainties in where particular salt marsh communities and species occur are at the upp |
| 13341 | 1 | s diversification and conservation with watershed management priorities throughout the region.
|
| 7481 | 1 | s diversification and conservation with watershed management priorities throughout the region.
|
| 15195 | 2 | na marshes are an international reknown wetland. even though, the seasonal flood dynamics of th
nal aim of this project is to develop a wetlands monitoring system based on remote sensing tech |
| 14747 | 2 | ana marshes are an international renown wetland. even though, the seasonal flood dynamics of th
nal aim of this project is to develop a wetland monitoring system based on remote sensing techn |
| 10130 | 2 | including the atmospheric water balance soil moisture availability. although we are beginning t
strial climate change, to enable future soil conditions water resources to be predicted using c |
| 10416 | 2 | including the atmospheric water balance soil moisture availability. although we are beginning t
strial climate change, to enable future soil conditions water resources to be predicted using c |
| 11698 | 2 | including the atmospheric water balance soil moisture availability. although we are beginning t
strial climate change, to enable future soil conditions water resources to be predicted using c |
| 9889 | 2 | including the atmospheric water balance soil moisture availability. although we are beginning t
strial climate change, to enable future soil conditions water resources to be predicted using c |
| 10703 | 2 | in otherwise toxic mercury contaminated soils. we will exploit the short generation times, and
esponse to heavy metal contamination of soils. - our study is powerful because we will use an e |
| 11428 | 2 | in otherwise toxic mercury contaminated soils. we will exploit the short generation times, and
esponse to heavy metal contamination of soils. - our study is powerful because we will use an e |
| 13922 | 1 | ants are ecologically very important in terrestrial ecosystems: they are extremely abundant, ar
|
| 11132 | 2 | le for uptake by neighbours. in natural soils, there is the possibility of a direct transfer pr
or transfer of semiochemicals into bulk soil and to neighbouring plants uninfected by aphids, a |
| 10063 | 1 | d using an experimental model animal: a soil mite. this has a fast generation time and a small
|
| 11076 | 1 | d using an experimental model animal: a soil mite. this has a fast generation time and a small
|
| 12255 | 11 | as the benefits of potentially reducing soil erosion and halting or reversing declines in farml
ge from arable cropping to set-aside on soil organic matter and soil microbial biodiversity. so to set-aside on soil organic matter and soil microbial biodiversity. soil organic matter as the matter and soil microbial biodiversity. soil organic matter as they are an important group invo they are an important group involved in soil biogeochemical cycling and carbon flow and because ales over which improvements to som and soil biodiversity take place following change to set-as de other ecosystem services mediated by soil to be determined, particularly nutrient loss, and ence water quality. the extent to which soil properties and geographical location determines di of set-aside to cropping, on different soil types and regions in england and wales. furthermor judgements to be made on the utility of soil microbes as generic bioindicators of soil quality, il microbes as generic bioindicators of soil quality, and the extent to which geography should |
| 10965 | 1 | n flow is central to the functioning of grassland ecosystems but there is virtually no informat
|
| 13797 | 1 | n copepods as food. previous studies in coastal ecosystems showed that salinity is important fo
|
| 11401 | 4 | e ecosystem. termites do this by moving soil around, and eating large amounts of dead leaves, w
e amounts of dead leaves, wood and even soil. ants also move soil around, and also consume a wi ves, wood and even soil. ants also move soil around, and also consume a wide variety of animals e collections of ants and termites from soil cores taken in rain forest in gabon. the different |
| 10488 | 1 | ctions. similar comparisons with modern island ecosystems can also suggest whether we can ident
|
| 13342 | 1 | vation increasingly takes place outside protected areas in multiple-use landscapes. success in
|
| 7658 | 2 | ich are strong diffuse contamination of urban environments. this project is part of the multi-y
metropolitan territory: reflections of urban development in ile de france network of r2ds. sis |
| 7047 | 6 | e of the principal fungal components in soil playing a key role for soil health. many species o
mponents in soil playing a key role for soil health. many species of hypocrea/trichoderma have en carried out on species isolated from soil, little has been known about the biodiversity and iversity and ecology of the genus above soil level. hypocrea teleomorphs occur commonly on wood eeds the biodiversity of trichoderma in soil and it exceeds by far expectations regarding the n s and forest fires. only two studies on soil inhabiting trichoderma anamorphs from sardinia and |
| 10489 | 1 | groundwater / surface water interactions, and the contr
|
| 15402 | 1 | diation as a viable option for treating soils contaminated by polycyclic aromatic hydrocarbons
|
| 15480 | 1 | soil and litter are the reservoir of a huge number of m
|
| 7379 | 1 | ral weathering in nutrient- poor forest soils.
|
| 12279 | 1 | eaching of nitrogen and phosphorus from soils results in poor water quality. • there have been
|
| 15103 | 1 | oastal lagoon of s'albufera des grau, a pristine ecosystem with changes between macrophytic and
|
| 13886 | 1 | will be used. these will be located to riparian ecosystems. such systems have high natural val
|
| 11153 | 1 | own and attenuation of pahs in polluted soils and sediments. such insight is of fundamental imp
|
| 15343 | 3 | t pellets in the most important spanish wetlands, accompanied by high prevalences of lead shot
hot use was banned in protected spanish wetlands in 2001, spent lead shot remains unaltered for in many bird species even in protected wetlands. however, very little is known about the suble |
| 7634 | 3 | ent approaches have led to a decline in soil fertility and biodiversity in these environments.
estrial plants form root symbiosis with soil fungi that can access difficult access resources d ibute to structuring and maintenance of soil fertility through the protein excretion. . . final |
| 1084 | 2 | iver mouths forming coastal lagoons and wetlands, and delivering sediment load to the nearshore
ence, primarily alongside estuaries, of mangrove forests that have played a protective role and |
| 13890 | 4 | richness of vascular plants, ground and soil living invertebrates. also soil temperature and so
und and soil living invertebrates. also soil temperature and soil respiration rates have been a nvertebrates. also soil temperature and soil respiration rates have been affected. effect furth round living invertebrates, biochemical soil processes and microclimate. the results will also |
| 12225 | 1 | and for eblex and dairyco on forage and grassland. adas have also collated data for pgro on pul
|
| 7129 | 1 | eir distribution areas the dominance of terrestrial ecosystems by humans led to a major alterat
|
| 14183 | 1 | experiments, how host plants within the agro-ecosystem affect the population dynamics and pheno
|
| 14983 | 7 | the mediterranean coastal wetlands of spain are systems that show a great richnes
aspects, as: - global evolution of the wetlands area - morphologic changes undergone in these morphologic changes undergone in these wetlands and their relationship with human development cteristics - appearance and dynamics of soil sealing and waterproofing phenomena - changes in h pect to the erosive processes - loss of soils and waters quality this integrated study would to ctionality of the mediterranean coastal wetlands, and their mechanisms and response patterns un ecovery and protection of mediterranean wetlands in progressive deterioration process. |
| 14141 | 3 | he intensity of evapo-transpiration and soil moisture. lower transpiration at higher air humidi
chamber, where light, air humidity and soil moisture will be controlled. the monitored variabl ylem. the water and the nitrogen in the soil will be also monitored. pressure-volume and leaf d |
| 10305 | 5 | icrobial communities which exist in the soils receiving such applications. these communities ar
e essential for the healthy function of soils: they underpin the production of food and fibre, ter flowing through them, contribute to soil structural stability and it s ability to resist er oparticles on the normal functioning of soil communities is potentially very significant. this normal composition and function of the soil microbial community, using well established techni |
| 10940 | 3 | lar pores in mineral grains of podzolic soils has challenged conventional views on mineral weat
l views on mineral weathering in forest soils. it has been hypothesised that these micropores a . we propose to study lmwoa dynamics in soil columns with/without trees and mycorrhiza in which |
| 165 | 1 | hemical and physical characteristics of soil-root contiinuum will be estimated in natural condi
|
| 187 | 1 | evergreen plants growing in contrasting soil and latitude conditions. it is known that the leaf
|
| 10004 | 2 | will investigate how long they last in soils. we will carry out flow through reactor experimen
ssolution. we will also put granules in soil columns and monitor dissolution through the change |
| 7626 | 4 | hemical and biological qualities of the soil and encourage the installation of plants. it is ba
ct of organic matter input on plant and soil processes implemented and technically, by improvin veness of biological engineering works. soil erosion in certain situations justify the establis gineering can play an important role in soil protection against surface erosion at the recovery |
| 7128 | 2 | grasslands and rangelands currently hold almost a third
grasslands and rangelands currently hold almost a third of the nationa |
| 543 | 2 | nd grass species phenology in a montane grassland community respond to elevated temperature , s
ry productivity, microbial activity and soil respiration rates show no significant effects of c |
| 11433 | 1 | d with the preservation of species rich grasslands and the restoration of these systems from ag
|
| 10155 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 10414 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 10422 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 10758 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 10915 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 11423 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 11693 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 11706 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 9879 | 1 | ios on the biodiversity and function of coastal ecosystems. the consortium will also act as a f
|
| 7429 | 2 | ersity across the grain farm. . - other soil insects and overhead involved in functional biodiv
involved in functional biodiversity of agricultural ecosystems different working methods will |
| 15271 | 1 | the temporal dynamic of nitrogen in the soils of the studied area, in order to evaluate the pos
|
| 2054 | 1 | ed to measure density of birds, whereas soil and litter samples are used to sample snails and e
|
| 10032 | 14 | ve been described as simply outcrops of groundwater . many of the rivers in the uk are supplied
vers in the uk are supplied mainly from groundwater sources, especially during the summer month etween surface and subsurface waters in groundwater catchments. here, the mixing of groundwater ndwater catchments. here, the mixing of groundwater and surface water and the resulting biologi llutant attenuating properties by some. groundwater abstraction, effluent disposal and diffuse ed there will also be upward flows from groundwater through the hyporheic zone and into the riv ted in what happens to the chemistry of groundwater as it moves through the hyporheic zone. we to the proposition that the movement of groundwater through this zone will reduce the concentra m that the hyporheic zone can attenuate groundwater contaminants such as nitrate. we want to lo e carefully at the pattern of flow from groundwater through the hyporheic zone. we propose that ugh the hyporheic zone. we propose that groundwater flux is influenced by the permeability of t y of the riverbed is high and flux from groundwater towards the river is high, we will find dif be important controls on the ecology of groundwater-fed rivers because they either release or t ng the water quality in rivers that are groundwater-fed, we will be able to provide evidence th |
| 11842 | 14 | ve been described as simply outcrops of groundwater . many of the rivers in the uk are supplied
vers in the uk are supplied mainly from groundwater sources, especially during the summer month etween surface and subsurface waters in groundwater catchments. here, the mixing of groundwater ndwater catchments. here, the mixing of groundwater and surface water and the resulting biologi llutant attenuating properties by some. groundwater abstraction, effluent disposal and diffuse ed there will also be upward flows from groundwater through the hyporheic zone and into the riv ted in what happens to the chemistry of groundwater as it moves through the hyporheic zone. we to the proposition that the movement of groundwater through this zone will reduce the concentra m that the hyporheic zone can attenuate groundwater contaminants such as nitrate. we want to lo e carefully at the pattern of flow from groundwater through the hyporheic zone. we propose that ugh the hyporheic zone. we propose that groundwater flux is influenced by the permeability of t y of the riverbed is high and flux from groundwater towards the river is high, we will find dif be important controls on the ecology of groundwater-fed rivers because they either release or t ng the water quality in rivers that are groundwater-fed, we will be able to provide evidence th |
| 12274 | 2 | ture and use water and nutrients in the soil. as pressure increases on global food prices and s
eaching of nitrogen and phosphorus from soils results in poor water quality. breeding crops tha |
| 12239 | 1 | nding of annual dormancy cycling in the soil seedbank. 3. establish the link between applied pr
|
| 10084 | 1 | many legumes form a symbiosis with soil bacteria, which are housed in special organs calle
|
| 11249 | 1 | many legumes form a symbiosis with soil bacteria, which are housed in special organs calle
|
| 1090 | 1 | odland habitats and species thriving in grassland habitats will be studied. understanding of th
|
| 10789 | 1 | nsive fossil record and dominate modern terrestrial ecosystems. living seed plants represent fi
|
| 10407 | 1 | ods of peoples living in the forest and agricultural ecosystems in south asia. the consortium i
|
| 7101 | 1 | e last 10 years in the network of eight protected areas special of the poitou-charentes region.
|
| 1095 | 4 | the dynamics of native and semi-natural grasslands in marginal alpine and apennine areas, and i
eas, and ii to evaluate the attitude of grassland users towards the conservation of such vegeta f great interest in the conservation of grasslands at an evolutional state defined in the frame tion of local communities, tourists and grassland users to the management of marginal areas and |
| 14499 | 3 | nmental interest behavior of c and n in soil. our simulation model allows the evolutions of dif
utions of different pools of c and n in soil and makes possible a holistic interpretation of th uctural similarity that also appears in soil and composting processes. our simulations will act |
| 11037 | 1 | meerkats; and laboratory populations of soil mites. these systems have been chosen because prev
|
| 11566 | 1 | meerkats; and laboratory populations of soil mites. these systems have been chosen because prev
|
| 15338 | 2 | ts to the biodiversity conservation. in agricultural landscapes, habitat diversity loss and com
e effects that the habitat structure of agricultural landscapes has on its biological diversity |
| 14171 | 1 | tors of interest include precipitation, soil water potential, air humidity, air temperature and
|
| 224 | 3 | oral components in nutrient dynamics of coastal ecosystem. macroalgae and phytoplankton compete
an modify internal nutrient dynamics of coastal ecosystem. in order to assess the effect that e , the model can assist in assessment of coastal ecosystem response to eutrophication. |
| 11631 | 5 | is the primary interface with the bulk soil and is therefore the main conduit through which re
hich recent plant assimilate enters the soil. despite the importance of the external mycelium, n em fungi and other groups of abundant soil organisms for c cycling. using both radioactive an gical pathways of c flux from plants to soils to be determined in situ. it will also address ho ites, three numerically dominant forest soil invertebrates, disrupt c flux to em fungal myceliu |
| 14982 | 9 | wetlands constitute one of the richest and more product
50 years, more than 60 % of the coastal wetlands have disappeared in spain pressed by developme or the fullfilment of this project, two wetlands characteristic of the mediterranean area have ntative ecosystems of a large number of wetlands and supercial lagoons in europe. these systems d by different official figures such as wetlands of international importance will be compiled i ometry, which will be applied to water, soil, natural vegetation and crops, will be one of the inants and their relation ship with the urban, agricultural and industrial pressure. geo-statis talish the fragil points between water, soil and native vegetation and crops. finally, a global d regeneration of coastal mediterranean wetlands against the different anthropic pressures. |
| 12219 | 4 | ch to enable business led innovation in grassland management. the enhancement of the biodiversi
nhancement of the biodiversity value of grassland and other grazed habitats through informing t ntated research. in addition to work on grassland flora and grazing, wider research in support d grazing, wider research in support of grassland related biodiversity outcomes ranges from res |
| 7483 | 1 | has a negative environmental impact on groundwater . the eu seeks to stimulate measures that i
|
| 13728 | 1 | . sylvestris and r. raphanistrum in the agricultural landscape while s. arvensis is abundant. t
|
| 454 | 4 | t in order to increase the fertility of soil - the improvement of the microbial soil flora thro
soil - the improvement of the microbial soil flora through endemic hyper-mycosis species in ord the mycorrhizan potential in cultivated soil - the identification of bacterium of the rhizosphe ish the stock of parasite grains in the soil this research for targeted control methods will in |
| 7214 | 4 | ion of inorganic amendments to increase soil fertility; - enhancement of the microbial flora of
hancement of the microbial flora of the soil by endemic species hypermycotrophes to increase th rease the mycorrhizal potential of crop soils; - identification of bacteria in the rhizosphere to reduce the parasite seed bank in the soil; this research targeted control methods will be ba |
| 14444 | 1 | ity to fix atmospheric nitrogen in most agricultural ecosystems. they are able to form speciali
|
| 1104 | 1 | sk 3. sustainability of river, lake and agricultural ecosystems and hydrological stress. task 4
|
| 10649 | 29 | many problems in environmental and soils research require techniques that quantify the soi
ch require techniques that quantify the soil micro-environment. it has become increasingly appa ement other techniques that often study soils at spatial scales that are too coarse. at the mic o coarse. at the microscopic scale in a soil, bacteria and their food source or oxygen supply, emical, and biological heterogeneity of soils, which combined with modelling techniques, enable s us to make sense of the complexity of soil systems. soil physics and soil chemistry are highl ense of the complexity of soil systems. soil physics and soil chemistry are highly interdepende exity of soil systems. soil physics and soil chemistry are highly interdependent, with the spat eously distributed and intertwined with soil structure. examples include the role of metal comp on and stabilization of aggregates, the soil organic mineral interactions in gley soils and gle il organic mineral interactions in gley soils and gleyic features in poorly drained soils, or s s and gleyic features in poorly drained soils, or soils contaminated with metals. the opacity o ic features in poorly drained soils, or soils contaminated with metals. the opacity of soil has ontaminated with metals. the opacity of soil has hampered progress in our understanding of phys anding of physico-chemical processes in soils. to date, our understanding of the soil micro-env oils. to date, our understanding of the soil micro-environment relies heavily on the concept of onment relies heavily on the concept of soil aggregates. advances in the use of x-ray ct, howev tification of the internal structure of soils at microscopic scales without physical disruption ace after homogenizing relatively large soil samples. even studies with small samples of soils les. even studies with small samples of soils are effectively bulk analyses and a mechanistic u art x-ray ct facilities to quantify the soil structure in situ at a resolution of 8 micrometres of 8 micrometres. we will then prepare soil sections to obtain 2-d spatial maps of the distrib he distribution of elements in the same soil samples using sem-edx. first we will make horizont we will make horizontal slices through soil to obtain sequential 2-d maps that are quantified planes. we will apply the techniques to soils amended with black carbon and kaolinte, keeping s ocesses involved in c sequestration and soil structural dynamics and may provide means to test ation of macro- and micro-aggregates in soil and the stability of biochar. this will be importa e important for studies of c storage in soils and how this will be affected by climate change a will be affected by climate change and soil management. |
| 1942 | 2 | ological and economic information about wetland biodiversity is necessary for the development a
spatially disaggregated, for promoting wetland biodiversity and capturing associated values; 2 |
| 7209 | 1 | the other hand, bioindication tools of soil operating states
|
| 9882 | 1 | onservation management of exploited and pristine ecosystems in the face of global change. these
|
| 2494 | 1 | dic populations inhabiting these desert rangelands. the seemingly counterintuitive question doe
|
| 13865 | 9 | most of the natural wetlands in agricultural landscapes have been drained t
most of the natural wetlands in agricultural landscapes have been drained to gain arabl aken to counteract this by creating new wetlands in the agricultural areas. this project is des and biodiversity be optimised in these wetlands plant and macroinvertebrate species compositio obial diversity, are investigated in 36 constructed wetlands of similar morphology and nutrient ill also be followed in 18 experimental wetlands. ecosystem functioning and underlying biogeoch rocesses will be studied in some of the constructed wetlands as well as in the experimental wet wetlands as well as in the experimental wetlands. the obtained data will be analysed for intera d ecosystem functioning. guidelines for wetland construction and management will be developed b |
| 11561 | 1 | tions in other terrestrial sediment and soil environments, as well as subsurface environments o
|
| 15089 | 1 | saproxylic insects, the most diverse in terrestrial ecosystems, acting in the degradation and i
|
| 12151 | 1 | the junction zone of aquatic and terrestrial ecosystems is forming a specific habitat co
|
| 7243 | 1 | ical study of users and stakeholders in urban environmental management and their uses and their
|
| 15331 | 1 | n the functions of affected aquatic and terrestrial ecosystems. particularly, we aim to analyse
|
| 7018 | 2 | of the principal components of fungi in soil. studies of this genus are therefore mainly carrie
carried out with material isolated from soil. teleomorphs of this genus belong to the genus hyp |
| 12477 | 2 | se for assessing the state of england’s terrestrial ecosystems using an ecosystem approach. the
se for assessing the state of england’s terrestrial ecosystems using an ecosystem approach 2 re |
| 2481 | 2 | northern coastal ecosystems are experiencing environmental pertu
to spatial and temporal variability in coastal ecosystems. |
| 13876 | 1 | g plants and decomposers. in the study, soil samples will be taken from each island to estimate
|
| 12633 | 3 | most soil surveys and classifications are based on soil geom
urveys and classifications are based on soil geomorphic, physical and chemical properties. the properties. the microbial properties or soil biological quality indicators distributed across g |
| 10126 | 3 | production of nitrous oxide soil inoculated with aob and nob strains from objective
ains from objective 1, and in a natural soil community adopting a combination of 15n-isotopomer techniques, as well as a wide range of soil physical and chemical analyses. the student will o |
| 10798 | 2 | the soil microbial process of denitrification produces nitr
erived c flow drives denitrification in soils of different som contents, and management histori |
| 6941 | 2 | hytraeids are an important saprophagous soil mesofauna family with a worldwide distribution. du
reatened lowland woodlands and adjacent grasslands. the project is expected to produce internat |
| 11695 | 1 | the management of selected coastal and terrestrial ecosystems in china, india and central afri
|
| 14907 | 1 | f factors such as rainfall variability, soil resource availability for plants, and herbivory at
|
| 7219 | 2 | o meet these degradations, a network of protected areas was created and mayotte is planned on t
ros nor the relevance of the network of protected areas nont assessed on other groups that the |
| 459 | 2 | to face these degradations a network of protected areas has been set up in mayotte and is at pl
ro, nor the relevance of the network of protected areas have been evaluated other than on other |
| 7259 | 2 | rt on exogenous organic inputs from the watershed. it comes to sales, in a rich and diverse aqu
used by the species in the course of a watershed heavily modified by man will be |
| 2471 | 1 | sy are probably several, like e.g. like urban/rural, local/outsider, traditionalist/modernist.
|
| 2519 | 1 | regional parks and local management of protected areas in mountain regions in norway. the case
|
| 2544 | 5 | ent of norwegian management regimes for protected areas. another part of the project will addre
ct will address internationalization of protected areas, ranging from the consequences of assig igning formal international status to a protected area to the increasing international interest erest in and relevance of management of protected areas. while this part of the project will an the project will analyze management of protected areas from the perspective of international i |
| 13571 | 1 | ally changed species composition in the agricultural landscape. however, little is known about
|
| 12638 | 5 | spatial data infrastructure containing soil data and spatial and descriptive semantic soil pro
ta and spatial and descriptive semantic soil property data for england and wales, in addition t of related agro-meteorological and peri-soil thematic datasets. these data are used widely by a r national strategic issues relating to soil and the environment. this includes information con uality and potential use of the nations soils. the maintenance of the landis reference site is |
| 13723 | 4 | h species diversity. rationalization of agricultural landscapes leads to fragmentation and loss
n and loss of species-rich semi-natural grasslands. sustainable approaches to landscape managem pe structure and the history of present grassland fragments over the last 300 years. within thi on different scales within present-day grassland fragments; explore associations between prese |
| 439 | 1 | adows but no value was selected for the urban area. the validation stage shows that the migrati
|
| 10411 | 9 | the underlying biophysical capacity of agricultural ecosystems. this research focuses on a cri
the productivity and sustainability of agricultural ecosystems. these es are often provided by cape. the flows of these es rely on how agricultural ecosystems are managed at the site scale a ndscape structure. managing land use in agricultural landscapes to provide sufficient es offers impoverishment of modern high intensity agricultural landscapes. results of these studies highl gement strategies from the field to the agricultural landscape. as new evidence begins to emerg urces for beneficial insects within the agricultural landscapes. the overall goal of this propo based decisions on managing land use in agricultural landscapes that explicitly account for the ntrated in its rural population and the agricultural ecosystems face the challenge of improving |
| 14935 | 3 | t pellets in the most important spanish wetlands, accompanied by high prevalences of lead shot
hot use was banned in protected spanish wetlands in 2001, spent lead shot remains unaltered for rd, and such grit is commonly scarce in wetlands containing fine particle size sediments. the a |
| 14159 | 2 | n changing conditions in a semi-natural grassland; second involves comparison of disturbed and
servation in management of diversity in grasslands and in control of invasive alien plants. |
| 12228 | 1 | weed biology, ecology and adaptation in agroecosystems is a basic requirement for integrated we
|
| 7194 | 4 | in agro- ecosystems, functioning of biogeochemical cycles.
process of mos, microbial component of soil nest still regarded today as a functional black bo fficult to transpose to a wide range of agro-ecosystems. in this context, this project is part er manage the biogeochemical cycle c in agro-ecosystems. this project should also enable the de |
| 14692 | 1 | tion to understand food web dynamics in terrestrial ecosystems, there are currently no field st
|
| 2026 | 6 | ding multitrophic community. in natural grasslands, i will study aboveground and belowground co
dy the relationship between vegetation, soil biodiversity and aboveground invertebrates, and in ng plant community, and carry out plant-soil feedback studies to determine the effects of plant ruct quantitative interaction foodwebs. soil organisms will be identified using novel molecular de reliable information on abundance of soil microorganisms such as nematodes, bacteria and fun ng of multitrophic interactions between soil organisms, plants and aboveground invertebrates as |
| 11404 | 1 | tify their role in ammonia oxidation in soil, to compare the impact of environmental factors on
|
| 1975 | 1 | ng on above-ground systems, whereas the soil was viewed as a black box. much of the early resea
|
| 11763 | 3 | fferent processes to n2o emissions from soil, addressing current uncertainties associated with
tion to functional diversity and active soil microbial populations. this will be achieved using be used to quantify n2o emissions from soils, coupled with molecular techniques to determine f |
| 15104 | 1 | at gradient and intensively in selected wetland habitats. the results will be validated at habi
|
| 14721 | 2 | levels. the functional biodiversity of soil through the determination of different biological
onservation of nature. in this way, the protected areas will contribute to the conservation of |
| 14581 | 2 | s. thus, the functional biodiversity of soil through enzyme activity and the structural biodive
onservation of nature. in this way, the protected areas will contribute to the conservation of |
| 14582 | 2 | s. thus, the functional biodiversity of soil through enzyme activity and the structural biodive
onservation of nature. in this way, the protected areas will contribute to the conservation of |
| 14722 | 2 | levels. the functional biodiversity of soil through the determination of different biological
onservation of nature. in this way, the protected areas will contribute to the conservation of |
| 9957 | 2 | tance to poor groups, namely woodlands, grasslands and wetlands these three ecosystems potentia
roups, namely woodlands, grasslands and wetlands these three ecosystems potentially provide poo |
| 14944 | 1 | ild pear seeds to physical and chemical soil characteristics. our approach shows two novel qual
|
| 7406 | 2 | ed with phenological traits measured on urban and non-urban populations
ogical traits measured on urban and non-urban populations |
| 14548 | 4 | terns of biological diversity on gypsum soils have fascinated ecologist and evolutionary biolog
lutionary biologist for decades. gypsum soils which occurs patchily are high in calcium and low s essential macronutrients. these harsh soils exclude most plants found in surrounding nongypsu with near 50 taxa restricted to gypsum soils. species-area relationships have been of interest |
| 7038 | 4 | e managers to eco-systematic processes. soil and weather are the central conditions in determin
terpretation and reaction of farmers to soil and climate are in close connection with specific f farmers and other local experts about soil and weather in the regions of osttirol and pinzgau stions: - which type of knowledge about soil and weather is available, - to which values and at |
| 7709 | 1 | roecological to analyze the dynamics of grassland communities and their adaptation to drought,
|
| 12165 | 1 | l sites will be identified on different soil types, containing populations of uncommon arable p
|
| 12580 | 4 | udge, with different metal contents, on soil microorganisms and how they function within the so
anisms and how they function within the soil. the experiments were carried out at nine sites ac est the effects of individual metals on soil microbial activity and long term soil fertility. t n soil microbial activity and long term soil fertility. this project will give an independent e |
| 11849 | 1 | of greenhouse gases in their trees and soils. the brazilian amazon accounts for 40% of all the
|
| 7046 | 2 | s a key, and growing, threat to shallow coastal ecosystems. it will put an ecological framework
determining the location and borders of protected areas. finally, mariculture enterprises in sl |
| 12332 | 2 | , 10% of lyme bay was declared a marine protected area and permanently closed off to scallop dr
d to assess the effectiveness of marine protected areas in achieving conservation objectives; t |
| 7181 | 1 | ion, it should continue to monitor some protected areas but the risk appears limited impact out
|
| 183 | 1 | actical nature conservation in planning protected areas at the global and regional scale. we sh
|
| 6737 | 1 | n arm of the danube and in the adjacent wetland areas. majority of available records are severa
|
| 10716 | 1 | ll do these experiments on mud from the salt marshes of north norfolk. these are home to the gr
|
| 11704 | 1 | ll do these experiments on mud from the salt marshes of north norfolk. these are home to the gr
|
| 14632 | 1 | o the changes occurred in mediterranean wetlands. the loss and fragmentation of habitat may aff
|
| 7617 | 1 | s by installing i oaks directly on bare soil but with accompanying vegetation and ii in shrubla
|
| 13808 | 1 | sessment of qualities of the forests by urban people are studied. knowledge about effects by ma
|
| 15244 | 3 | es for natural mycorrhization of gypsum soils endemic plants, with the final goal of recovering
physical, chemical and microbiological soil properties. 2. implement methods for reproduction mycorrhizal fungi inoculum from gypsum soils. 2.1. try different types of substrates and plant |
| 15243 | 3 | es for natural mycorrhization of gypsum soils endemic plants, with the final goal of recovering
physical, chemical and microbiological soil properties. 2. implement methods for reproduction mycorrhizal fungi inoculum from gypsum soils. 2.1. try different types of substrates and plant |
| 12156 | 2 | of breeding wading birds on lowland wet grassland in uk and elsewhere in europe. these declines
such as drainage and intensification of grassland management. whilst there is clear evidence th |
| 12187 | 2 | g , increases the sequestration of c in grassland soils and brings additional benefits for the
ses the sequestration of c in grassland soils and brings additional benefits for the delivery o |
| 11231 | 3 | es that help to store organic carbon in soils and vegetation are becoming increasingly popular.
ays in which they are measured for both soil and vegetation; b identify the livelihood activiti it by assessing organic carbon in both soil and vegetation and link this with social and econo |
| 13764 | 1 | stal areas. the aim of a no-take marine protected area is twofold. from a commercial perspectiv
|
| 1923 | 4 | ary production, evapo-transpiration and soil nutrient turnover. but recent studies also show th
reach the target area. especially, many soil organisms have extremely limited dispersal capacit paid to effects of the introduction of soil organisms or small above-ground herbivores on plan the diversity of the various groups of soil organisms. subsequently, we will test whether the |
| 12343 | 1 | ed as part of the designation of marine protected areas under the marine and coastal access bil
|
| 10128 | 1 | marine coastal ecosystems are among the most productive and di
|
| 10245 | 2 | fundamental modelling approaches to the planktonic ecosystem, with the aim of clarifying what w
development of a module to simulate the coastal ecosystems, but useable in global ocean biogeoc |
| 10512 | 2 | fundamental modelling approaches to the planktonic ecosystem, with the aim of clarifying what w
development of a module to simulate the coastal ecosystems, but useable in global ocean biogeoc |
| 11471 | 2 | fundamental modelling approaches to the planktonic ecosystem, with the aim of clarifying what w
development of a module to simulate the coastal ecosystems, but useable in global ocean biogeoc |
| 11520 | 2 | fundamental modelling approaches to the planktonic ecosystem, with the aim of clarifying what w
development of a module to simulate the coastal ecosystems, but useable in global ocean biogeoc |
| 11796 | 2 | fundamental modelling approaches to the planktonic ecosystem, with the aim of clarifying what w
development of a module to simulate the coastal ecosystems, but useable in global ocean biogeoc |
| 9981 | 2 | fundamental modelling approaches to the planktonic ecosystem, with the aim of clarifying what w
development of a module to simulate the coastal ecosystems, but useable in global ocean biogeoc |
| 12408 | 1 | rements such as the formation of marine protected areas under the marine strategy directive. ke
|
| 2469 | 1 | develop conservation schemes and marine protected areas.
|
| 10941 | 1 | nd, or of putting bells on cats to warn urban sparrows, that are suggested by our research may
|
| 1974 | 6 | many soil bacteria produce chitinases and other lytic enzyme
ycoparasitism that is known for certain soil fungi. however, so far no information is available ollimonas, can grow on living hyphae in soil microcosms. the collimonas bacteria are dominant a nolytic bacteria in acidic, fungal rich soils indicating the potential importance of bacterial be used to develop a protocol to screen soil bacteria for mycoparasitic potential. the major go he mycoparasitic growth potential among soil bacteria. |
| 218 | 1 | n west- and north-estonia on calcareous soils, while m. sativa arrived in estonia at the break
|
| 7707 | 1 | eir land. . . a characterization of the soils will be established by a synthetic typology and q
|
| 14834 | 3 | of forest fires and prescribed fires on soils. for this purpose, these research tasks are based
al project we implement fire effects on soil microbiology, as well as we want to include a soil iology, as well as we want to include a soil quality index developed by us in the previous proj |
| 14835 | 3 | of forest fires and prescribed fires on soils. for this purpose, these research tasks are based
al project we implement fire effects on soil microbiology, as well as we want to include a soil iology, as well as we want to include a soil quality index developed by us in the previous proj |
| 14165 | 8 | our ability to estimate the health of soils and to identify key soil properties which can ser
the health of soils and to identify key soil properties which can serve as indicators of soil h erties which can serve as indicators of soil health has become a major issue for food and timbe estoration success is the return of the soil microbial biomass. soil fauna cross a range of tro e return of the soil microbial biomass. soil fauna cross a range of trophic levels and in soil cross a range of trophic levels and in soil food webs they are often allocated to functional g ing habit. the knowledge of food web in soil of post-mining and reclaimed areas is important fo as for bioindication of contaminants in soil. the aim of the project is to examine the specific |
| 14885 | 2 | urface of the roots and the surrounding soil areas . we are also interested in the detection of
rhizosphere of heavy metal contaminated soils and their relationships with the plants. |
| 10554 | 1 | ineages indicate major domain shifts in planktonic ecosystems and by observing and interpreting
|
| 10558 | 1 | ineages indicate major domain shifts in planktonic ecosystems and by observing and interpreting
|
| 12591 | 1 | cts of changing the maximum permissible soil metal concentrations.
|
| 10887 | 1 | that the original source of methane in groundwater fed rivers is both a subsidy to the system
|
| 12020 | 2 | the microbes project studied soil ecosystem services, in particular the decompositio
intaining or improving the diversity of soil biological components. the microbes program did no |
| 13523 | 3 | relations among microbes, plants, and soil function are complex and poorly understood. studie
y use of biomarkers , revealed that the soil c/n ratio explained as much, or more, of the varia the different functional groups in the soil. molecular methods will provide information about |
| 11761 | 2 | luding bacteria and fungi living in the soil. the aim of this research project is to determine
o determine which organisms live in the soils of the different sites, how they live together in |
| 2486 | 3 | arctic soil contains large amounts of stored organic carbon wh
the genomic and functional diversity of soil microbial communities, with emphasis on key functi expected to contribute to more reliable soil-atmosphere models for high latitude ecosystems and |
| 7041 | 1 | esents a unique starting point to study terrestrial ecosystem changes in the context of geodyna
|
| 2003 | 1 | backs between vegetation, hydrology and soil. we recently developed a process-based model descr
|
| 438 | 2 | activities, while the second refers to protected areas for the preservation and sustainability
g in poitevin marsh, size of the marine protected area in new-caledonia. |
| 10408 | 1 | the role that hydrological systems and watershed management play in regulating flows of provis
|
| 11413 | 1 | the role that hydrological systems and watershed management play in regulating flows of provis
|
| 10543 | 1 | or marine resources, such as a range of protected areas and a greater emphasis on regional mana
|
| 7277 | 1 | location of existing and future marine protected areas
|
| 11838 | 2 | s underlain by coarse and fine-textured soils in both high and low rainfall areas, with recent
for isolating the effects of rainfall, soil properties and disturbance on savanna tree demogra |
| 7676 | 1 | in agricultural landscapes, weeds are the main constituent
|
| 10828 | 1 | g with derivatives of elevation models, soil maps and land cover data. the comparison of these
|
| 13763 | 2 | future. in historical rural landscapes grasslands were large, and livestock and people contrib
lants creating high species-richness in grasslands. recent land-cover and land use changes thre |
| 12593 | 14 | vities are highly dependent on suitable soil functioning and properties, and are often adapted
nd are often adapted to the present day soil conditions. under climate change, the anticipated luence the structure and functioning of soils, making the local soil environment less suitable functioning of soils, making the local soil environment less suitable for some forms of activi nd more suitable for others. changes in soil conditions may also have other effects. changes in rage and transmission properties of the soil. the incidence of landslips and soil cracking may he soil. the incidence of landslips and soil cracking may also change, with consequences to hou ocesses typically respond to changes in soil moisture and temperature. of particular interest i interest is the possible change in the soil carbon budget, for example by increased rates of n insofar as the quantitative response of soil processes to temperature and water budget changes ntified changes in water storage in the soil, or the rate of biochemical processes such as mine ate simulations of changes in important soil properties under the climate change scenarios gene nd precipitation: 1. erosion 2. loss of soil organic matter 3. compaction 4. contamination 5. s up from process representation based on soil physics. biodiversity models will be empirical and |
| 12260 | 3 | enhancing or retaining biodiversity in agricultural ecosystems is a key priority within the uk
rity within the uk. the biodiversity of agricultural landscapes is determined by the spatial ar ent factors, affect biodiversity within agroecosystems, with a focus on how economic incentives |
| 10493 | 2 | impacts. recent uk work has shown that groundwater-dominated river catchments exhibit a long-t
erm. this will allow the rates at which groundwater nutrient transport can make land to river t |
| 7154 | 1 | directives; the effectiveness of marine protected areas for the conservation of populations and
|
| 11299 | 1 | onii epidemics on algal populations and coastal ecosystems. however, many unresolved biological
|
| 11540 | 1 | onii epidemics on algal populations and coastal ecosystems. however, many unresolved biological
|
| 10463 | 2 | ts of n deposition, and its removal, on soil nitrifier populations at upland sites will indicat
e information for mechanistic models of soil n cycling. |
| 7494 | 1 | of non cultivability more than 99 % of soil bacteria, alternative techniques have been develop
|
| 10104 | 1 | d from habitats ranging from intertidal mangrove mud to hydrothermal vents.
|
| 10352 | 4 | owth, but most of the sulfur in natural soil is present in a bound form that can be utilized by
h the amount of sulfonate-sulfur in the soil in which the plants are grown, and the ability of ur transformations at the plant-microbe-soil interface, but will also be of immense practical v promote sulfur bio-availability in the soil, and increase plant productivity. |
| 15024 | 2 | tiative gloria that leave zones of bare soil among them. with regard to the characterization of
l as the edaphic characteristics of the soils under the above described vegetation and also bar |
| 14967 | 2 | the soil is a reservoir of a huge number and variety of mic
erform the first world monograph of the soil-borne ascomycetes. approximately 150-200 genera an |
| 13814 | 1 | much of the biodiversity value of agricultural landscapes is dependent on the preservatio
|
| 7265 | 1 | rt us about that man inflicts damage to terrestrial ecosystems. by studying the knowledge and p
|
| 12483 | 1 | the current level of understanding of a protected area and to demonstrate a prioritisation fram
|
| 14712 | 1 | forest masses alternate with scrub and grassland zones, next to cultivated areas conforming as
|
| 11745 | 2 | mustard gas contaminated soil contains a toxic micture of mustard and its deriva
ttle over decades of contamination. the soil contains indigenous bacteria that have adapted to |
| 11096 | 1 | forest, contains around 35% of all c in terrestrial ecosystems and is the world s major source
|
| 6827 | 1 | tter and grain yields, n applied to the soil, and total n taken into the aboveground plant. the
|
| 11579 | 2 | ll see how the nzvi particles behave in soil by using an electron microscope. also, we will app
at nzvi agglomeration in an undisturbed soil situation. |
| 12604 | 1 | entially be used in the context of a uk soil monitoring network. the final report is available
|
| 10367 | 2 | d today. a complete picture of mesozoic terrestrial ecosystem function could not be assembled u
tomological data to understand mesozoic terrestrial ecosystems and how they survived global ext |
| 10287 | 4 | organic nitrogen for plant nutrition in terrestrial ecosystems has taken centre stage. recent s
xisiting plant species to partition the soil n pool based on chemical forms of n, is greatest i vity ecosystems where don dominates the soil n pool. we will take a holistic, field based appro haracterised and ubiquitous gradient of grassland productivity, coupled with non-destructive st |
| 10298 | 4 | organic nitrogen for plant nutrition in terrestrial ecosystems has taken centre stage. recent s
xisiting plant species to partition the soil n pool based on chemical forms of n, is greatest i vity ecosystems where don dominates the soil n pool. we will take a holistic, field based appro haracterised and ubiquitous gradient of grassland productivity, coupled with non-destructive st |
| 12242 | 3 | nmentally and economically sustainable. grassland represents more than 70% of the uks agricultu
f this need is to be met. new roles for grasslands have also been identified including the prot al and physiological traits that affect soil hydrology. genotypes will also be selected for inc |
| 14229 | 3 | estimate the effect of atmospheric and soil conditions , also their dependency on trees season
on well-watered trees in deficiency of soil mineral nutrients. 2. the hydraulic conductivity o stem scale depending on atmospheric and soil conditions. the fertilizing and moistening experim |
| 13613 | 1 | and increasing carbon storage in stable soil pools. therefore, understanding specific mechanism
|
| 7607 | 1 | up of an operation original transfer of soil per inoculation, developed in 2008
|
| 10291 | 2 | aller than photosynthesis, meaning that terrestrial ecosystems are thought to be a sink for atm
erature: currently our global models of terrestrial ecosystems make large assumptions about thi |
| 11285 | 1 | aller than photosynthesis, meaning that terrestrial ecosystems are thought to be a sink for atm
|
| 12512 | 1 | strategies for sustainable, low input, grassland-based, conventional and organic dairy farmers
|
| 13776 | 1 | e resilience, dynamics and integrity of swedish coastal ecosystems. this can, in turn, inform f
|
| 14987 | 1 | , specially, of the natural heritage of protected areas.
|
| 6768 | 1 | ing processes and of the development of terrestrial ecosystems during earth history is palaeobo
|
| 13601 | 1 | representing structure and function of riparian ecosystems. i will do this by comparing reache
|
| 15285 | 1 | f primary producers. this effect on the soil biota structure and composition, will in turn affe
|
| 15286 | 1 | f primary producers. this effect on the soil biota structure and composition, will in turn affe
|
| 14872 | 6 | soils can be source and sink of carbon, then soils cont
can be source and sink of carbon, then soils contribute to carbon cycle regulation and their c quences on climate change. land use and soil management influence soil organic carbon content a land use and soil management influence soil organic carbon content and its flux to the atmosph hich occur in forest ecosystems involve soil degradation that can be reversible. the use of org he amount of sequestrated carbon by the soil, its productivity and biodiversity. the present pr |
| 11465 | 4 | and emit more ch4 in gut communities of soil-feeding as opposed to wood-feeding termites. we pr
ogenic archaea in guts, faeces and food-soil of the soil-feeding termite cubitermes fungifaber ea in guts, faeces and food-soil of the soil-feeding termite cubitermes fungifaber sampled acro ether gut methanogens are ingested with soil as the animal forages, or vertically inherited as |
| 12531 | 1 | ist in the environment, particularly in soil, pathways and watercourses, and evidence is starti
|
| 14414 | 1 | ort tools to aid adaptive governance of agro-ecosystems. our aim is to understand how land-use
|
| 14757 | 1 | nertia, resilience and vulnerability of terrestrial ecosystems an adequate role in interpreting
|
| 12070 | 2 | e resilience of the contaminated marine coastal ecosystems over time. long term surveys suggest
resilience and the stability of marine coastal ecosystems. |
| 13841 | 2 | ion, landuse change and habitat loss in grassland and small grassland habitats. based on the ge
and habitat loss in grassland and small grassland habitats. based on the geographical data futu |
| 2187 | 1 | -natural and cultivated pastures in the agricultural landscape. we evaluate consequences for sp
|
| 14164 | 1 | ated by a few recent studies in oceanic coastal ecosystems, while there is no available data fr
|
| 10409 | 1 | iations between vegetation richness and soil microbial diversity, and how these are affected by
|
| 13611 | 2 | pally as elevated levels of nitrogen in soil solution and rising concentrations of greenhouse g
iations between vegetation richness and soil microbial diversity, and how these are affected by |
| 15571 | 2 | pally as elevated levels of nitrogen in soil solution and rising concentrations of greenhouse g
iations between vegetation richness and soil microbial diversity, and how these are affected by |
| 7199 | 2 | efficiency in use of resources and n p soil. . the complementary concepts of ecological niches
the n in resource use efficiency and p soil. this assessment combines bio- technical approache |
| 10301 | 3 | e environmental status of uk rivers. in groundwater-fed rivers, processes operating in the hypo
e controls in relation to p dynamics in groundwater-fed rivers.the focus in on understanding of oral variation in nutrient processes in groundwater-fed rivers. |
| 15454 | 7 | is fundamental to our understanding of terrestrial ecosystem functioning. litter decomposition
decomposition is the primary source of soil nutrients and it is also a fundamental component o of the global carbon cycle. litter and soil organic matter pools contain important amounts of contain important amounts of carbon in terrestrial ecosystems and their relative fast turnover main process of litter decomposition in semiarid ecosystems. it is a process by which solar rad ere without being incorporated into the soil organic matter pool. however, few studies have qua the contribution of photodegradation to soil respiration, standing mass decomposition will be d |
| 15512 | 1 | hat correspond to environments in which soil and climatic conditions are unfavorable, such as c
|
| 14503 | 1 | in plants widely represented in spanish terrestrial ecosystems, and to improve the parametrizat
|
| 15203 | 2 | use the recent restoration of a coastal wetland with water bodies of different trophic status t
be very useful for making decisions in wetland conservation, creation and restoration. the mai |
| 7026 | 2 | tional groups on food chains within the soil subsystem and the density and diversity of soil or
system and the density and diversity of soil organisms of different trophic levels is urgently |
| 7014 | 3 | iversity and community structure at the grassland sites and their link to c fluxes, - the devel
osystem c fluxes in differently managed grasslands the proposed project will answer questions a ort-term controls on c-sequestration of grasslands and contribute to an understanding of feedba |
| 15506 | 1 | ecosystem services through changing the soil environment. in this proposal it is intended to su
|
| 14212 | 4 | be fully understood without considering soil biota. soil pathogens and root symbionts are gener
erstood without considering soil biota. soil pathogens and root symbionts are generally host-sp mbionts are generally host-specific and soil microbial composition has been shown to change rap , and the function of root exudates and soil biota as mediators of plant responses to neighbour |
| 7682 | 3 | plays a key role in the maintenance of grassland areas with high biodiversity, especially in m
necessary step to predict the future of grassland biodiversity in the face of global change, an nts and insects in semi-natural managed grasslands. in these models, farming activities as well |
| 14662 | 6 | f ecosystems as well as changes in some soil properties relevant to soil resistance to erosion
ges in some soil properties relevant to soil resistance to erosion processes. these changes lea morphological and functional traits and soil characteristics related to plant colonization and to establish functions of variation of soil physical, chemical and hydrological characteristic able to identify and validate a set of soil indicators of the state and trend of both processe over to identify critical thresholds of soil properties that might be limiting for the differen |
| 2185 | 3 | uating policy measures for qualities of agricultural landscapes, c to evaluate alternative poli
of policies to improve the qualities of agricultural landscapes from a conservation standpoint. y measures for preserving the values of agricultural landscapes in terms of efficiency, fairnes |
| 1931 | 2 | in agricultural landscapes, values for nature conservation
nditions to increase biodiversity in an agricultural landscape. |
| 475 | 2 | pally as elevated levels of nitrogen in soil solution and rising concentrations of greenhouse g
iations between vegetation richness and soil microbial diversity, and how these are affected by |
| 14820 | 1 | nalysing the relative importance of the soil seed bank and of the yearly production of seeds. t
|
| 13835 | 3 | during the last century, semi-natural grasslands have become reduced by almost 90% in sweden.
l stages of degradation of semi-natural grasslands. the aim is to study local and regional dyna ecies living in fragmented semi-natural grasslands. how does the dynamics at the patch scale re |
| 6745 | 1 | ster is a characteristic species of the agricultural landscape and the steppe of the hungarian
|
| 12243 | 2 | i-permanent and permanent conversion to grassland. opportunites and constraints to further use
where needed, to enable application of grassland-based technologies. |
| 11073 | 2 | en causes changes to the vegetation and soil. the arctic tundra receives such air pollution fro
s damaged. critical load values for all european ecosystems were taken into account in the deve |
| 12612 | 1 | ders: concentrations of contaminants in soil, water and air associated with the site; potential
|
| 11163 | 1 | nmental problems. there is accelerating soil erosion on the hilly lands; deteriorating water qu
|
| 10714 | 1 | have pronounced effects in aquatic and terrestrial ecosystems. these effects will appear at di
|
| 9851 | 1 | s to adapt. pollination networks on its grassland reserves are already being studied by dr mich
|
| 13884 | 1 | em i will mainly work with old trees in agricultural landscapes. in that landscape, the beetle
|
| 1939 | 3 | om abiotic environmental factor such as soil moisture, ph and nutrients. indeed these factors c
from some species may be present in the soil; many species, however, have to recolonize the tar ding the established vegetation and the soil seed bank. moreover, lists of target species will |
| 2190 | 1 | reas of interest for the study are peri-urban areas of the stockholm region where there is an i
|
| 1956 | 1 | nd associated reproductive success in a soil-inhabiting predatory mite . in this way the geneti
|
| 13862 | 1 | plant community species composition and soil n turnover.
|
| 14617 | 2 | the re-colonization of alpine grassland with woody species as a result of vegetation
l pyrennes. disturbance value of alpine grassland. |
| 12160 | 1 | n independent programme manager for the grasslands assessment unit and its constituent projects
|
| 12161 | 1 | by acting as programme adviser for the grasslands assessment unit and its constituent projects
|
| 2140 | 2 | earth and are essential for structuring terrestrial ecosystems. this project represents the fir
mpare arthropod species richness in the soil and understorey vs. canopy habitats of a tropical |
| 2076 | 1 | he holistic approach to both marine and terrestrial ecosystems is expressed in the latest envir
|
| 11145 | 6 | methods for extraction of proteins from soils. the project will lead to an understanding of the
an understanding of the influence that soil protein have in determining the hydrophobicity of n determining the hydrophobicity of the soil around them and the manner in which hydrophobicity prediction of occurrence and effects of soil hydrophobicity, especially the transitions between ural resource management strategies for soil system functioning. the project is particularly re spread development of hydrophobicity in soils, which in turn reduces infiltration and water sto |
| 11484 | 1 | specially adapted dna extraction method soil will be sampled from three treatment regimes for p
|
| 9858 | 2 | important ecosystem services within the urban environment from biodiversity, climate change ada
auge, vaisala portable weather station, soil moisture theta probe. the student will also have a |
| 11850 | 1 | . the issue is particularly relevant in urban areas, where planners increasingly speculate on t
|
| 11020 | 3 | ance of earthworms in the processing of soil organic matter of carbon and nitrogen from organic
bon and nitrogen from organic matter in soils. overall, this research will add a new dimension nt of carbon and nitrogen stored in the soil. |
| 11141 | 6 | ed dry, so when the roof is constructed soil invertebrates are likely to be absent and the micr
hed. our hypothesis is that the lack of soil biota is one of the main reasons why plant establi are to 1 characterise the community of soil invertebrates and microbes in roofs of different a s are present, and 2 to add mixtures of soil bacteria and fungi, to determine if a sustainable technique that is culture-independent. soil invertebrates and we will also construct a new roo nalytical principles and the linking of soil ecology to the construction industry. finding a wa |
| 10779 | 1 | will use other techniques using fossil soils to get independent estimates of past carbon dioxi
|
| 11871 | 1 | and important components of almost all land ecosystems and show extremely specialised social b
|
| 14800 | 5 | matic changes and the regression of the wetlands where the mosquitoes thrive. for that reason i
for that reason it is possible that the wetlands act as a link between the climatic changes and es where the climate changes affect the wetlands, where the vectors of malaria thrive, a signif disease in those zones where the direct wetlands-climatic change relationship would not exist. works about the historical reduction of wetlands where the transmitting vector of malaria thriv |
| 14871 | 8 | ecological restoration of forest soils after fire could be improved by the addition of o
f organic amendments such as compost of urban refuse. the introduction of exogenous organic mat n nutrients, to increase the content of soil organic carbon and favouring the restoration of th on and favouring the restoration of the soil trophic web, and at the same time, reuses a subpro t the same time, reuses a subproduct of urban waste treatment with some difficulties for their t on the different organic fractions of soil carbon and its contribution to establish their tro long term of sequestering of carbon in soil, the activity of soil microbial biomass, its metab ring of carbon in soil, the activity of soil microbial biomass, its metabolic and functional di |
| 13348 | 2 | trategies needed to protect aquatic and riparian ecosystems. the future status of freshwater ec
th respect to lowland rivers, lakes and wetlands because these often pose the most difficult pr |
| 15587 | 5 | european marginal grasslands are biodiversity hot spots owing to ecologic
sms underpinning resilience of marginal grassland systems to global environmental and social ch , including extremes, and management on grassland ecosystems 2 how does coupled above-belowgrou functional diversity buffer or amplify grassland ecosystem responses to combined changes in cl ll address these questions for mountain grassland sites in austria, france and norway, where co |
| 7462 | 12 | soil and land information is needed for a wide range of
ct addresses the felt need for a global soil and terrain database. as the european contribution s the european contribution to a global soil observing system, it will deliver a web-based regi ude: quantitative mapping of landforms; soil parent material and soil attribute characterizatio of landforms; soil parent material and soil attribute characterization and pattern recognition ndardization of methods and measures of soil attributes to convert legacy data. two major resea ed existing parent material/geology and soil information, making use of advanced statistical pr d remote sensing, and remote sensing of soil attributes. advances beyond the state of the art i that address threats defined in the eu soil thematic strategy and comparing the results with c -scale soter databases, and an enhanced soil and terrain database at scale 1:1 million for the ced remote sensing techniques to obtain soil attribute data; 5 validation and uncertainty propa pplications related to major threats to soil quality and performance. |
| 11488 | 1 | ineages indicate major domain shifts in planktonic ecosystems and by observing and interpreting
|
| 1935 | 3 | h wet heaths and nardo-galion saxatllis grasslands were once wide spread and locations of hot s
these species-rich ecosystems on sandy soils were restricted to oligotrophic, but weakly buffe o oligotrophic, but weakly buffered wet soil conditions, mostly originating from seepage with b |
| 7621 | 2 | e project systemo the carbon content of soils while ensuring plant productivity. understand how
orm of"spots"affects the functioning of agro- ecosystems and study the fate of mo when amended |
| 7416 | 1 | exploitation it has problems of"fatigue"soil but also for beekeepers, providing high school nor
|
| 11531 | 1 | critical process to the functioning of terrestrial ecosystems. this process is largely driven
|
| 15382 | 9 | n biogeochemical cycles and the role of wetlands as green filters: effects of eutrophication, p
iversity such as semiarid mediterranean wetlands. the initial hypothesis, based on the results cycles and therefore the role of these wetlands as green filter perhaps may not be entirely co sequestration of semiarid mediterranean wetlands affected by the role of green filters played b es of carbon and nutrients in the plant-soil-water system of wetlands affected by eutrophicated ients in the plant-soil-water system of wetlands affected by eutrophicated waters, in order to s ocurr; 2. determine in what extent of soil microbial activity related to the carbon cycle is n, nitrogen and phosphorus in the plant-soil system from these wetlands and to ascertain what e rus in the plant-soil system from these wetlands and to ascertain what extent this effect may b |
| 162 | 5 | that may be connected with impoverished soil biota caused by ceased economical management and o
the wader species feed predominately on soil invertebrates, especially earthworms and insects, f the project, the relationship between soil biota and the numbers, territorial distribution an constitution, abundance and biomass of soil invertebrates communities. at the same time, we as ping methods, will also be carried out. soil invertebrates and microbial communities will be st |
| 13374 | 6 | tents were determined by icp-oes in the soil. maximum amount of cadmium in the soil samples was
soil. maximum amount of cadmium in the soil samples was 39 mg kg-1. the highest amount of cadm read and perfectly grows throughout the soil with zinc mines potentially having high cadmium co rally high amount of cadmium containing soils by setting up preliminary trials with the seeds c on capacity of sinapis alba l. grown in soil containing different doses of cadmium were also ex acid applications determined to improve soil organic matter. |
| 11859 | 2 | depth understanding of the link between wetland hydrology, developmental topography, biodiversi
ously and efficiently monitoring global wetland resources. |
| 12753 | 2 | the red requirements, their coverage of grasslands and their compatibility with the ieep approa
roach to dealing with highly biodiverse grasslands. |
| 10642 | 1 | rtant in an eastern african setting, as soil conditions are generally acidic and bone of does n
|
| 12181 | 1 | ngaged with resource protection such as soil and water and the enhancement of biodiversity, the
|
| 12415 | 1 | nt policy drivers including; ospar, the urban waste water treatment directive and the nitrates
|
| 13759 | 2 | due to anthropogenic pressures, coastal ecosystems are being rapidly degraded and can u
level are crucial for the resilience of coastal ecosystems, and that ecology and management the |
| 10500 | 1 | h has demonstrated that the capacity of soil to eliminate pollutants is greatly improved after
|
| 10740 | 1 | h has demonstrated that the capacity of soil to eliminate pollutants is greatly improved after
|
| 11622 | 1 | h has demonstrated that the capacity of soil to eliminate pollutants is greatly improved after
|
| 15151 | 3 | tructure and functioning of the regions terrestrial ecosystems. adaptation of ecosystems to the
ughts. our attention will be focused on soil respiration, also a function of the microbial comm age, as well as of the root systems and soil characteristics. |
| 14528 | 1 | iversity in planktonic organisms.in the wetlands sediments we can found the summary of process
|
| 12199 | 2 | the hedgerow herbaceous plant flora and soil properties, the effect of hedge management on thes
species occur, including field margins, grassland and woodland. restoration techniques with mos |
| 12192 | 1 | mical conditions, including topography, soils and hydrology under which existing fen, purple mo
|
| 1934 | 3 | nt decades dry heaths and nutrient-poor grasslands have been affected in the netherlands by soi
ave been affected in the netherlands by soil acidification and eutrophication as a result of at es of the acidic nardo-galion saxatllis grasslands, and the related species-rich dry heathlands |
| 13928 | 1 | ion land-use of agri-, silviculture and urban areas. the working hypothesis is that the dynamic
|
| 13531 | 1 | ion land-use of agri-, silviculture and urban areas. the working hypothesis is that the dynamic
|
| 12589 | 2 | eatlands are the most widespread of all wetland types on a global scale. as ecosystems they pro
e the uk with significant areas of peat soils and, in particular, temperate peatlands. it will |
| 12152 | 1 | slopes. it is defined by its deep peat soils, which depend on rainfall for water supply and ar
|
| 12240 | 2 | on systems, and reduce the incidence of soil-borne pests and disease. crop rotation and its ass
crobial and invertebrate species in the soil, through host alternation and physical disturbance |
| 12602 | 1 | road-testing soil-net in hampshire schools
|
| 10216 | 1 | times faster in marine in comparison to terrestrial ecosystems. this highlights that grazing by
|
| 10925 | 1 | times faster in marine in comparison to terrestrial ecosystems. this highlights that grazing by
|
| 10790 | 3 | strains and types, and in isolates from soils with different native cu conditions. from this in
s discovered, final experiments on real soils will be carried out to calibrate cu availability m defined mineral sources and different soils collected from natural systems. the ultimate goal |
| 14485 | 1 | been recorded, including both river and urban systems, as well as considering the main mediterr
|
| 7715 | 4 | ot traits depending on the depth of the soil will be examined at the level of individuals and p
plant communities. the fate of C in the soil profile will be drawn by isotope chemistry. isotop clarified through experiments cohesive soil and aggregate stability, analysis of root traits a f numerical models integrating the root-soil relationships, will quantify ecosystem services an |
| 11474 | 1 | wastewater treatment to productivity of soil, seas through to freshwater and disease. however,
|
| 13349 | 1 | . this framework focuses on networks of protected areas and regional connectivity. this framewo
|
| 13860 | 1 | ainly relate to issues of regeneration, soil and water; biodiversity aspects are largely lackin
|
| 14710 | 4 | e efficiency of a strategy for riverine wetlands restoration based on combining the flood poten
models, the efficiency of re-connecting wetlands and the practice of planting vs. auto-organiza nting vs. auto-organization of riverine wetlands. the results will be useful to be applied as s egies for the ecological restoration of wetlands at large scale in floodplains of regulated riv |
| 12584 | 7 | quirements of the inter-departmental uk soil indicators consortium to develop a set of policy r
and scientifically robust indicators of soil quality. sqid phase ii . the data derived from cs2 biological indicator to national-scale soil monitoring; the robustness of the different type o ing on ecological processes and the key soil functions. this information can be used by uk-sic iological indicators for national-scale soil monitoring and for other policy-related soil issue monitoring and for other policy-related soil issues. the information will also be invaluable to ecologically-relevant components of the soil community. |
| 12708 | 2 | scoping review of the implications for wetlands of energy generation and distribution activiti
to issues concerning climate change and wetlands, linking as appropriate to work done in relati |
| 12183 | 8 | soils in the moist regions of england are especially vu
ds of the year. under enclosed and open grassland, farm traffic and heavy grazing are the princ al causes of compaction. traditionally, soil compaction has been seen solely as a cause of redu of reduced grass productivity. however soil compaction, in its various forms, also impacts on so potential remediation techniques for soil compaction. the study will be of relevance to defr ntain a range of management options for grassland farmers. in many instances, farmers who have ptions that may influence the extent of soil compaction. this project will seek to elaborate an ny synergies and conflicts between good soil management and the environmental stewardship schem |
| 12180 | 2 | crop cover, and phosphate losses due to soil erosion. in order to assess whether agri-environme
t losses in relation to factors such as soil type, topography, land use. |
| 12289 | 1 | ture and use water and nutrients in the soil. as pressure increases on global food prices and s
|
| 7466 | 1 | . this framework focuses on networks of protected areas and regional connectivity. this framewo
|
| 228 | 1 | ll be performed on seeds picked up from soil after a period of time to test if the non-germinat
|
| 10762 | 2 | soil respiration research programme in peru. the new in
c resources supplied to us to perform a soil translocation study at our field site. |
| 10054 | 1 | and impact in a conspicuously important soil-dwelling macroinvertebrate. by exploiting informat
|
| 11582 | 1 | and impact in a conspicuously important soil-dwelling macroinvertebrate. by exploiting informat
|
| 12191 | 7 | ats, including several types of lowland grassland. species-rich lowland grasslands are the prod
lowland grassland. species-rich lowland grasslands are the product of farming and are dependent odologies and the current definition of grassland types. from this review, a provisional rapid her a particular site achieves priority grassland status. the provisional assessment methodolog setting and take account of a range of grassland types and starting conditions. the primary us ver, a greater understanding of desired grassland attributes and the timescales for their devel storation sites and ‘wildlife value for grassland creation sites within agri-environment scheme |
| 15166 | 1 | to demonstrate that only the number of soil-borne species that exist is of from 3.5 to 5.1 mil
|
| 14174 | 3 | soil biota , by management of land-use and by working o
strategies of meadows recolonization by soil invertebrates and the spatial structure of soil co ertebrates and the spatial structure of soil communities are necessary to take into account. |
| 12620 | 11 | soils contain far more carbon than vegetation or the at
climate are sensitive to any changes in soil carbon. the amount of soil carbon is itself sensit y changes in soil carbon. the amount of soil carbon is itself sensitive to the way the land is is managed, and there is evidence that soils across england and elsewhere have been losing car y to increase carbon storage in english soils. four sub-projects are addressed within the proje centrates on knowledge gaps relating to soil carbon and how it may change with management pract s for accurate routine determination of soil carbon. the overall project will be co-ordinated b limate and land management practices on soil carbon and greenhouse gas emissions. soil carbon u il carbon and greenhouse gas emissions. soil carbon underlying the topsoil and its interactions ampling and laboratory determination of soil carbon will be standardised for soil monitoring sc of soil carbon will be standardised for soil monitoring schemes in the future. |
| 15148 | 8 | the thematic strategy for soil protection related to the soil organic carbon cycl
tegy for soil protection related to the soil organic carbon cycle this overall objective can be oloxidase and lacasse in olive orchards soils. 2. to develop proteomics techniques for determin oloxidase and lacasse in olive orchards soils. 3. to evaluate the effect of different agricultu oloxidase and lacasse in olive orchards soils. 4. to study the relationship between agricultura practices and agricultural systems and soil organic carbon balance. to determine the soil comp rganic carbon balance. to determine the soil compartments where the mineralization is smaller a le sinks of carbon in the mediterranean soils. |
| 6994 | 1 | . we have great experience in studying soil ciliates and my laboratory is in this respect uniq
|
| 227 | 15 | cultural grasslands are usually found on less fertile soils, suc
lands are usually found on less fertile soils, such leptosols and arenosols, and on wet soils, uch leptosols and arenosols, and on wet soils, such gleisols and histosols. on wet soils the ot ls, such gleisols and histosols. on wet soils the other agricultural activities are limited due agrotechnical bear capability of those soils. however, intensive management of grasslands, suc soils. however, intensive management of grasslands, such repeated cutting, high fertilization r e but heavy machinery, are proceeded on grasslands to get high quality fodder. in subject of so get high quality fodder. in subject of soil compaction research, the main attention is paid on paid on the cultivated land and less on grasslands. how are changing the soil properties during ess on grasslands. how are changing the soil properties during intensive management, in which l es the regeneration ability of roots of grassland cultures and thereby the nutrition and produc nts, is slightly known. however, as the grassland cultures with their extensive root system may system may reduce the harmful effect of soil compaction and improve the soil properties at diff fect of soil compaction and improve the soil properties at different fertilization rates will b th the institute of plant nutrition and soil science of christan albrechts university in kiel i |
| 13867 | 4 | in south swedish habitats and determine soil disturbance influence on am fungal communities; di
s and spore production. disturbed sandy grasslands in south east sweden will be studied and the goals: 1. to determine the influence of soil disturbance on the diversity, species composition, surveying the spore populations in the soil that provides a signature for am fungi, its measur |
| 13988 | 13 | in tropical soil the organic matter content decreases and the soil
rganic matter content decreases and the soil structure deteriorates faster than in temperate ar e. at the same time the biodiversity of soil organismsl decreases. knowledge of these structura ral and functitonal changes in tropical soil and their importance for soil processes is far fro tropical soil and their importance for soil processes is far from complete. in this project we g questions: how are the communities of soil fauna in tropical agriculture affected by amounts affected by amounts and quantity of of soil organic matter and different crops and different i fferent crops and different intesity of soil cultivation - is the soil food web more stable and t intesity of soil cultivation - is the soil food web more stable and recilient in soil with hi l food web more stable and recilient in soil with high organic matter content and high biodiver and high biodiversity than in degraded soils - to what extent are different taxonomic and func rent taxonomic and functional groups of soil animals feeding on the growing crop and on microor basic food source the structure of the soil fauna community will be studied by sampling in all |
| 12632 | 20 | ledge, explore potential ways to manage soils in a sustainable manner and identify gaps in the
the evidence base for defra relating to soil functions, quality and degradation. the five princ d support for the implementation of the soil strategy for england. the objectives of the four s are: objective a: to review the role of soil biota in soil fertility and quality, and explore a a: to review the role of soil biota in soil fertility and quality, and explore approaches to i , and explore approaches to influencing soil communities to enhance delivery of these functions objective b: to address the effects of soil degradation on the ability of soils to function an s of soil degradation on the ability of soils to function and identify gaps in the evidence bas eview the overall costs and benefits of soil erosion measures and to identify cost-effective mi dge on the impacts of climate change on soil processes, functions and its relevance to england carried out by internationally-leading soil scientists from cranfield university, the cross-in sity, the cross-institute programme for soils , lancaster university and nri, greenwich univers d evidence gaps into the context of the soil strategy for england. the principal benefits arisi work will be to: identify the ways that soil biota may be managed to potentially increase soil may be managed to potentially increase soil fertility and reduce external inputs; explore evid uts; explore evidence on the impacts of soil degradation on soil functions; review the costs an e on the impacts of soil degradation on soil functions; review the costs and benefits of mitiga s of mitigation measures used to reduce soil erosion; and review the potential impacts of clima potential impacts of climate change on soil processes, functions and biota. the outputs will b ustness and likely effectiveness of the soil strategy for england. |
| 14490 | 5 | the dynamics of soil seed banks in four threatened halophytes . the fat
eeds, if existing, will be assessed.the soil seed bank will be periodically sampled throughout les to analyze the fate of seeds in the soil. it will allow us to guess the seed output by agin to the moment they are removed from the soil seed bank, on causes producing seed bank output, a he time that seeds remain viable in the soil. such approach will give crucial information on th |
| 7477 | 10 | poses to develop an integrated model of soil processes that describes key soil functions. these
el of soil processes that describes key soil functions. these functions are defined in the ec s . these functions are defined in the ec soil thematic strategy as essential ecosystem services es, computational models that integrate soil erosion, solute transport, carbon dynamics and foo ototype simulator at eu-scale to assess soil threats and evaluate approaches to mitigation. thi advance of this project is to quantify soil stocks, their formation, loss and functions within ibe key stages within the life cycle of soil formation, its productive use and degradation. exi ets to validate the integrated model of soil processes. these process studies will be integrate usa and chinese field sites to compare soil processes and rates as they vary with lithology, c nd guidance of international leaders in soil sustainability. |
| 13350 | 16 | european soil biodiversity is pivotal for delivering food, fiber
he demand is greater than the amount of soil available, as production of biofuels competes with moreover, intensified land use reduces soil biodiversity and the resulting ecosystem services. system services. soilservice will value soil biodiversity through the impact on ecosystem servi interdisciplinary empirical studies and soil biodiversity surveys to construct soil food web mo soil biodiversity surveys to construct soil food web models and determine effects of changing odels and determine effects of changing soil biodiversity on stability and resilience of carbon models to develop a system for valuing soil biodiversity in relation to ecosystem services. ob objectives: • develop methods to value soil ecosystem services during different pressure of la ent pressure of land use and changes in soil biodiversity. • field and modelling studies will d ine to what spatial and temporal scales soil biodiversity and soil ecosystem services are vulne d temporal scales soil biodiversity and soil ecosystem services are vulnerable to disturbance. tion and land abandonment can influence soil biodiversity and ecosystem services over european are at threat and mitigating changes in soil biodiversity to achieve a sustainable use of soils versity to achieve a sustainable use of soils. our results contribute to a european knowledge-b economy and to a future eu directive on soils. |
| 14909 | 1 | because of its adaptations to semiarid soils favoured by the climatic change.
|
| 13536 | 4 | n effect on species diversity in nearby grasslands. wild flower strips are sown by farmers in s
le species pool and abundance in nearby grasslands, environmental factors as pesticide use, and influences species diversity in nearby grasslands in the context of metacommunity research. th rflies and bumblebees in the strips and grasslands in the study area, observing insect behaviou |
| 1941 | 1 | wetlands host a large amount of characteristic biologic
|
| 13559 | 1 | entory of ferns as indicator species of soil characteristics, in combination with remote sensin
|
| 1940 | 2 | biodiversity in the semi-natura1 dutch wetlands is influenced by a complex of factors, ranging
he influence of economic development of wetland areas. |
| 15016 | 3 | important reservoir of biodiversity in terrestrial ecosystems partly because the range of envi
catastrophic shifts. on the other side, semiarid ecosystems present a slow response, and their going from the central pyrenees to the semiarid ecosystems of the middle ebro valley. our prio |
| 14539 | 2 | water redistribution between soil layers carried out by roots may have an important
e. such redistribution can be upwards , soil type, the organic matter content, the depth of wat |
| 10308 | 1 | cal rainforests; even a metre square of grassland on a derbyshire hillside in the uk can hold o
|
| 11406 | 1 | cal rainforests; even a metre square of grassland on a derbyshire hillside in the uk can hold o
|
| 2207 | 1 | aluate the potential role of harvest in protected areas given a certain size. • evaluate the ap
|
| 15169 | 4 | spatio-temporal patterns of soil seed banks and their consequences in the regenerat
environmental conditions, particularly soil properties, are responsible for change patterns ra teppes, another habitat with particular soil properties as well. studies will be carried out in l. studies will be carried out in three protected area in castilla-la mancha. results may be of |
| 13574 | 7 | most studies of grassland plant diversity have focused on the spatial p
of habitat fragments within the modern agricultural landscape. however, it is increasingly cle stainable management of species-diverse grasslands need to be based on an understanding of inte stical approaches to the description of grassland connectivity. we will assess the extent to wh al and composite dispersal profiles for grassland species and species assemblages. we will then ofiles to species-presence/diversity in grassland patches in the modern landscape. finally, we es-occurrences and species diversity in grassland fragments. |
| 11765 | 2 | s a crucial role in nutrient cycling in terrestrial ecosystems. i will evaluate changes in spec
valuate the effect of climate change on terrestrial ecosystems as a function of changes in the |
| 2503 | 1 | on berried females, and no-take marine protected areas . in addition, we plan to perform an ev
|
| 6721 | 4 | ocuses both the native components /rock grasslands/ and a man made component /austrian pine pla
ration processes. stability of the rock grasslands will be studied by using permanent plot meth native trees. the regeneration of rock grassland communities following pine forest burning wil kew gardens. the impact of fire on the soil structure and element composition will be monitore |
| 7244 | 2 | d determine carbon sequestration in the soil c. the project overall objective is to study the r
sms on the storage of organic matter in soils, and in situ experiments. three specific objectiv |
| 7023 | 1 | n, the maintenance of water quality and soil fertility, carbon storage, the mitigation of the e
|
| 10897 | 1 | itiatives by the government of india on watershed management, national action plan on climate c
|
| 7121 | 3 | permanent grassland natural and semi-natural are carriers of both
scribing the characteristics of natural grassland and their evolution in order to reason with t e and manage the multi-functionality of grasslands: what descriptors for what functions |
| 14207 | 4 | pesticides can lead to the toxicity to soils, vegetables and contamination to aqueous systems
ined could be applied when constructing wetlands to enhance wetland function. the real-pcr anal d when constructing wetlands to enhance wetland function. the real-pcr analysis and the pyroseq ies in pesticide-influenced constructed wetland ecosystems. |
| 12628 | 10 | develop a cost curve for mitigation of soil compaction on agricultural land the use of heavy m
ng by livestock can cause compaction of soil; a greater mass of minerals and less space for air olume. in contrast to some of the other soil degradation threats, the costs associated with soi tion threats, the costs associated with soil compaction across europe cannot currently be estim the top seven threats to our use of the soil across england and wales. the degree of compaction he degree of compaction in agricultural soil largely depends on the which type of impact the so depends on the which type of impact the soil is exposed to we propose to use computerised x ray to examine how bulk density of mineral soils varies with depth, and the implications of this f ble to identify a protocol to determine soil bulk density which is efficient and adequate for o ble levels of error in our estimates of soil carbon stock. as a result we will have confidence |
| 12635 | 22 | ledge, explore potential ways to manage soils in a sustainable manner and identify gaps in the
the evidence base for defra relating to soil carbon, soil management, urban soils and soil resi base for defra relating to soil carbon, soil management, urban soils and soil resilience in rel lating to soil carbon, soil management, urban soils and soil resilience in relation to climate to soil carbon, soil management, urban soils and soil resilience in relation to climate change arbon, soil management, urban soils and soil resilience in relation to climate change. the rela imate change. the relationships between soil pollutants and food will also be reviewed, and soi nts and food will also be reviewed, and soil quality indicators pertinent to policy reporting c d support for the implementation of the soil strategy for england. the objectives of the six su logies for increasing carbon storage in soil to mitigate climate change. objective b: to determ ship between best practice for managing soils to protect the environment with that for increase ent of the impacts of climate change on soils in the urban environment, addressing the potentia pacts of climate change on soils in the urban environment, addressing the potential impact to t review the evidence of what makes some soils more resilient to change, to evaluate what this m change, to evaluate what this means for soils in england and wales, and to provide an initial a to which resilience can be conferred to soils. objective e: to review the literature on the con on the concentrations of pollutants in soils that lead to significant concentrations of pollut etting of outcome focused indicators of soil quality that can be reported on within policy repo carried out by internationally-leading soil scientists from cranfield university, the cross-in sity, the cross-institute programme for soils , adas consulting ltd and the british geological d evidence gaps into the context of the soil strategy for england. the tangible benefits arisin ustness and likely effectiveness of the soil strategy for england. |
| 7253 | 4 | anisms at the origin of biodiversity in urban areas has been neglected. it requires an interdis
social-geographical factors influencing urban gene flow. these issues will be discussed from si that influence the flow of genes recent urban. the questions are: 1- highly fragmented urban la the questions are: 1- highly fragmented urban landscapes she allows what-2 gene flow are the pr |
| 14626 | 3 | the most important structural pests in urban environments in terms of physical damage to struc
is increasing. as a consequence of the urban organisation of cities and villages in spain, the kill termites quickly; as a result, the urban environment and human health will be benefit. |
| 7241 | 3 | n²o the emission from the agricultural landscape in france is an important part o
by agricultural practices, humidity and soil drainage. objectives the subject is to finely stud in the continuum formed by agricultural soils, runoff and drainage and waterways, along a trans |
| 12501 | 1 | y english heritage in 2008 focussing on urban commons indicates the wide and varied pastimes an
|
| 15336 | 1 | to define a coherent network of marine protected areas in accordance with the requisites of na
|
| 15239 | 4 | the autochtonous olive orchard agroecosystem in extremadura must be protected because
because of the ecological importance in soils protection, as soils in many zones of extremadura ical importance in soils protection, as soils in many zones of extremadura are in precarious st in precarious state, due to low ph and soil development, under exteme temperature and drought. |
| 7377 | 1 | intra-specific diversity of spontaneous grassland species planted in landscapes with high agric
|
| 7431 | 1 | cooperation with the agency for marine protected areas is responsible for the program the mari
|
| 12546 | 1 | strengthen risk management methods for soil phases of invertebrate pest groups or species of s
|
| 6794 | 1 | iding vegetation-units, will be created soil ph examinations too. the distribution of vegetatio
|
| 14501 | 2 | n of a complex set of information about soil, fodder offer, nourishing value of vegetation, and
ating to the information about level of soil with tools for analysis , we will be liable to mak |
| 7713 | 2 | ms of governance and management of peri-urban territories in the perspective of sustainable dev
anean coastal plains where the focus of urban pressure on scarce agricultural land, fragile and |
| 12766 | 3 | •review problems with wild deer in the urban and peri-urban environment. •the project will dra
ms with wild deer in the urban and peri-urban environment. •the project will draw on experience ations for a strategy for management of urban deer populations and how this could be administer |
| 12159 | 1 | ng, by cattle, to maintain species rich grassland, and to quantify the impact of grazing on inv
|
| 12164 | 6 | nements to existing uk agri-environment soil conditions. prior to liming the soil ph was in the
nt soil conditions. prior to liming the soil ph was in the range 4.9-5.8 across the study sites ross the study sites. liming effects on soil base status can take between one and two years to years to fully develop. the botanical, soil microbial and agronomic responses to the combinati , is known to have a negative effect on grassland plant diversity. therefore any effects of the rms of plant diversity maintenance. the soil microbial community response to the different fert |
| 11688 | 9 | r livelihoods and security; for example mangrove forests provide them with firewood, fish, medi
stal erosion. despite the importance of mangroves they are suffering high rates of destruction. ys of studying, evaluating and managing mangroves, and will communicate the lessons learnt to g s working in other types of ecosystems. mangrove forests are highly productive and efficient at ing payments for carbon credits to help mangrove conservation and to bring revenue for local pe ent and organisation of the gazi womens mangrove boardwalk committee. a kenyan sociology studen d benefit, on how the management of the mangrove resource works and on how this project can inf ts for ecosystem services. the value of mangrove ecosystems to local people, and particularly t ites, but this approach is untested for mangroves and may lead to large errors. we will test th |
| 10822 | 1 | wetland lake systems can exist in alternative states of
|
| 13850 | 1 | their forming a vital component of the wetland fauna. we propose systematic and taxonomic rese
|
| 15102 | 1 | the potential vegetation of ravines and salt marshes of semiarid territories, a kind of plant c
|
| 15573 | 1 | w translating landscapes or networks of protected areas into functional connectivity. tenlamas
|
| 11350 | 1 | articulate carbon sources on and within soil across scales of cm to metres. the project will ad
|
| 14214 | 2 | estonian species-poor and species-rich grassland communities as model systems, to find evidenc
with artificial as well as semi-natural grassland communities will be used to test the hypothes |
| 10421 | 1 | ermine the structure and functioning of planktonic ecosystems in relation to physical and atmos
|
| 10663 | 1 | ermine the structure and functioning of planktonic ecosystems in relation to physical and atmos
|
| 10685 | 1 | ermine the structure and functioning of planktonic ecosystems in relation to physical and atmos
|
| 10914 | 1 | ermine the structure and functioning of planktonic ecosystems in relation to physical and atmos
|
| 11692 | 1 | ermine the structure and functioning of planktonic ecosystems in relation to physical and atmos
|
| 9897 | 1 | ermine the structure and functioning of planktonic ecosystems in relation to physical and atmos
|
| 6982 | 2 | ole of specific elaterid species in the soil food web in a correct way. furthermore this knowle
on/diet of the wireworms with humus and soil moisture content of the sites, conclusions can be |
| 174 | 1 | for variation in forest age structure, soil environment and light climate. due to the present-
|
| 10600 | 4 | ecently been detached at high levels in soil using molecular techniques, but no representative
nd we are ignorant of their function in soil ecosystems. this project aims to determine their a abolic activity in a well-characterised soil site , to assess the effects of soil management pr ed soil site , to assess the effects of soil management practices on their community structure, |
| 11481 | 9 | on, such as plant and/or fungal growth, soil factors or indeed chance. the formation of a mycor
. in this case we would expect external soil properties to have much less effect. to test this both in plant and fungal species and in soil properties. hetchell wood, near leeds uk, is an id e the limestone cap has eroded away the soil is much more acid, and a striking transition from striking transition from acid to basic soil can occur over the space of a few metres. this res es. this results in a high diversity of soil and vegetation in a restricted area. we need to kn populations, and the properties of the soil in which they are growing. the most effective way so that a map of the plants, fungi and soil properties can be constructed. the testing of the re important than growth in response to soil environment in determining observed patterns of am |
| 143 | 1 | o light availability, but plasticity to soil fertility will also be considered. the project wil
|
| 11865 | 3 | nly been isolated twice before. further soil and sediment isolates harboured novel chlamydia an
seeks to investigate human pathogens in soil and aquatic sediments associated with protozoa, an compare this to their diversity in bulk soil / sediment. previous work in this area is highly f |
| 177 | 2 | es. absorbing roots adapt to changes in soil conditions by differentiating their anatomical and
adaptation of short roots to different soil conditions to be assessed, and will, in addition i |
| 15141 | 1 | d for monitoring conservation status of terrestrial ecosystems in the meditteranean basin. they
|
| 14167 | 2 | on manor parks, which are scattered in agricultural landscape. woodland parts of these old man
spersal ability. we will study parks in agricultural landscapes and forest landscape around the |
| 14161 | 11 | l’s needs and manure helps preserve the soil fertility. generally in the mixed farms the closed
is managed by wearing of the reserve of soil mineral usually. in crop rotation the leguminous t act does the organic tillage has to the soil fertility comparing with conventional tillage does organic farming maintain or improve the soil fertility or is the decreasing of the soil fertili l fertility or is the decreasing of the soil fertility unavoidable •which are the soil agro-phy il fertility unavoidable •which are the soil agro-physical properties, microbiological activiti properties, microbiological activities, soil biota and other soil health indicators in the case ogical activities, soil biota and other soil health indicators in the case of different organic nt is defined. to observe the change of soil fertility, the soil ph, organic matter and the con serve the change of soil fertility, the soil ph, organic matter and the content of macro- and m o nutrients are measured regularly. the soil microorganisms and microbiological activity is mea |
| 12587 | 3 | l increase the carbon content of arable soils under english and welsh conditions. the 2006 uk c
of sequestering carbon in agricultural soils. however, a defra-funded review of the potential or carbon sequestration in agricultural soils , including new data from field experiments in en |
| 2153 | 1 | erent trophic levels in both marine and terrestrial ecosystem components on svalbard and in the
|
| 11025 | 1 | er implications for studies of mesozoic terrestrial ecosystems and extinctions.
|
| 10337 | 1 | ing on this character in uncontaminated soils. the mineral nutrition of this species and its cr
|
| 11580 | 27 | carbon dioxide to a range of different soils. we will then track the fate of the label in the
then track the fate of the label in the soil, to calculate what proportion of the carbon from c the carbon from ch4 is retained in the soil. we can also link the 13c-labelled ch4 to other so also link the 13c-labelled ch4 to other soil microorganisms that utilise the carbon from methan od, and build up a picture of the wider soil microbial food web. three different soil environme oil microbial food web. three different soil environments are going to be studied in this work. opment work will study a landfill cover soil and focus on establishing a range of new analytica range of new analytical techniques. the soil that overlays a landfill site contains extremely h eates out to the atmosphere through the soil that covers the site. it is well known that bacter own that bacteria in the landfill cover soils oxidise a large proportion of this methane but th . the fate of methane carbon in natural wetlands will also be studied. natural wetlands include wetlands will also be studied. natural wetlands include environments such as peat bogs, fens, e environments such as peat bogs, fens, salt marshes and tropical swamps. natural wetlands have lt marshes and tropical swamps. natural wetlands have organic rich soils that release methane i mps. natural wetlands have organic rich soils that release methane in a similar way to landfill similar way to landfill sites when the soil organic matter degrades. we are going to study the ption by methanotrophic bacteria in the soil. the final type of soils that will be used to asse bacteria in the soil. the final type of soils that will be used to assess the fate of carbon fr sess the fate of carbon from methane in soils are a range of soil chronosequences. a soil chron on from methane in soils are a range of soil chronosequences. a soil chronosequence is a relate are a range of soil chronosequences. a soil chronosequence is a related set of soils that form soil chronosequence is a related set of soils that formed under similar conditions of vegetatio mate. the length of time over which the soils have developed is the only difference between the oped is the only difference between the soils in the chronosequence. this will allow us to asse w us to assess the relationship between soil development and the soil processes involved in car onship between soil development and the soil processes involved in carbon sequestration. overal as it is utilised and dispersed by the soil microbial community. |
| 6746 | 1 | considerable part of the region became protected area some years ago but we have just a few of
|
| 15340 | 2 | erranean vegetation, which included two protected areas, the parque natural de cabo de gata nij
rvation and management of ecosystems of protected areas and in the valuation of his ecosistem s |
| 11575 | 1 | in such changing environments. for one soil-dwelling nematode worm we have investigated how it
|
| 14759 | 1 | l: establish to what extent the natural protected areas of spain and europe are contributing to
|
| 10205 | 2 | south asia, whether they were based on wetland paddy cultivation or dryland cultivation, and h
rice ecosystems, whether or wild type, wetland paddy type or dry, rainfed type using both arch |
| 12618 | 2 | the soil strategy for england, safeguarding our soils the l
strategy for england, safeguarding our soils the land use climate change report to the welsh a |
| 12249 | 2 | ated plantings of osr seeds in the same soil. a time course will be used to determine the perio
and land management on biodiversity and soil protection, and policy on climate change through s |
| 13791 | 1 | origins and environmental responses of soil co2 efflux. despite their large biomass, the contr
|
| 11077 | 4 | mmunities differ in plant productivity, soil co2 efflux, fungal biomass and nitrogen and carbon
higher organisms can be translated into soil fungi, and will increase our understanding of the nding of the functional significance of soil biodiversity in boreal and northern temperate fore es to better manage the biodiversity of soil. |
| 11772 | 1 | gate the characteristics of yeasts from urban and industrial sites exposed to some common man-m
|
| 13975 | 1 | on ecosystem functioning has come from terrestrial ecosystems and has focused on single trophi
|
| 13881 | 1 | other indicators of biodiversity in the agricultural landscape.
|
| 14193 | 2 | ical and chemical properties of organic soils and thereby the growth of plant species in bog ec
ant stress tolerances and plant-organic soil interactions in specific habitat conditions. the r |
| 7172 | 1 | ly open habitats such as wasteland, dry grasslands, pastures, dry crops and ruderal environment
|
| 10076 | 1 | the proposed massive plant killing and soil wash-off at the beginning of the triassic how did
|
| 12579 | 2 | he continued development of policies on soil protection where heavy metals are applied to agric
ects of heavy metal additions per se on soil fertility and agricultural productivity. |
| 12578 | 2 | he continued development of policies on soil protection where sludge is being applied to agricu
the effects of heavy metal additions on soil fertility and agricultural productivity. |
| 10888 | 14 | introduction mangroves are tropical forests that grow in salty water
against shore erosion and storm surges. mangroves also trap carbon from the atmosphere in the f ooking at better ways of managing their mangrove resources, such as allowing controlled cutting cycling and greenhouse gas emissions in mangroves: 1 to examine how controlled cutting, which r ther factors of importance to a healthy mangrove ecosystem such as the communities of fish and greenhouse gases that are lost from the soil in mangrove ecosystems - for example, whether this se gases that are lost from the soil in mangrove ecosystems - for example, whether this is comi decomposition of organic matter in the soil. we will also determine the productivity of mangro will also determine the productivity of mangrove roots, allowing us to estimate how quickly suc al women s group and school children in mangrove education and restoration events. field site t al reef, and contains seagrass beds and mangrove forests. gazi village next to the bay is home ay is home to 1000 people who use their mangroves for a wide range of products. methods using a communities, and on the ability of the mangrove forests to trap sediment and to retain a stabl and women s group will participate in a mangrove day of replanting and education. |
| 11515 | 1 | will also study the mineral phases and groundwater composition using state of the art mineralo
|
| 9862 | 1 | will also study the mineral phases and groundwater composition using state of the art mineralo
|
| 6983 | 2 | of plants. several site parameters like soil ph, total and plant available p content, soil wate
h, total and plant available p content, soil water content, bulk density and plant p content ar |
| 14673 | 1 | chr ||assessment and the management of protected areas.
|
| 13463 | 1 | tor treatment effects on communities of soil fungi, using high throughput sequencing of marker
|
| 518 | 1 | ys a central role in the functioning of agro-ecosystems having a strong natural value due to it
|
| 203 | 4 | ng hybrid aspen will be assessed. plant-soil interactions will be studied in even-aged monocult
ent demand of hybrid aspen on different soils will be clarified. the limiting factors for bioma ion of the trees, to monitor changes in soil fertility and vegetation cover and to assess the p he best hybrid aspen clones in estonian soil and climate conditions. the results from the proje |
| 12657 | 2 | rch is designed to assess the effect of urban development and number of visitors on the distrib
n of nightjar and woodlark numbers with urban development in dorset is replicated in the thames |
| 11879 | 1 | rch fellows and a £1.3 million grant on urban pollinators led by memmott. at the somerset wildl
|
| 10771 | 1 | istic understanding of the responses of grassland communities to environmental changes at the l
|
| 2057 | 1 | rther on svalbard and other high arctic terrestrial ecosystems.
|
| 11178 | 2 | ented and scattered across inhospitable urban and agricultural landscapes. because of this huma
scattered across inhospitable urban and agricultural landscapes. because of this human-induced |
| 11398 | 2 | ented and scattered across inhospitable urban and agricultural landscapes. because of this huma
scattered across inhospitable urban and agricultural landscapes. because of this human-induced |
| 14148 | 1 | on and a more accurate determination of protected areas and thereby support the overall effecti
|
| 14217 | 1 | are crucial in the functioning of most terrestrial ecosystems. nevertheless, it is poorly know
|
| 14176 | 1 | indirect mechanisms by which plant and soil microbial community interactions can influence the
|
| 13923 | 1 | l aid in the development of sustainable agro-ecosystems and develop solutions aiming at reducin
|
| 11277 | 3 | xide have been slowly locked up in peat soils in the cool, wet, northern regions of the world a
large area of the earth s surface. peat soils, which can be up to 5 m or more in thickness, con k. although it has been known that peat soils contain large numbers of pipes to streams. peat p |
| 11301 | 3 | xide have been slowly locked up in peat soils in the cool, wet, northern regions of the world a
large area of the earth s surface. peat soils, which can be up to 5 m or more in thickness, con k. although it has been known that peat soils contain large numbers of pipes to streams. peat p |
| 11837 | 3 | xide have been slowly locked up in peat soils in the cool, wet, northern regions of the world a
large area of the earth s surface. peat soils, which can be up to 5 m or more in thickness, con k. although it has been known that peat soils contain large numbers of pipes to streams. peat p |
| 15477 | 3 | the study of plant-soil feedbacks and their role as determinants of the st
within the framework of the response of terrestrial ecosystems to global change. the growing in of the interactions among the plant and soil community is largely due to the awareness that the |
| 9801 | 2 | trients they need are obtained from the soil, being taken up by the roots. to obtain these nutr
and they form the major food source for soil microbes. in return, the bacteria and fungi play a |
| 13981 | 3 | high conservation values, semi-natural grasslands and species-rich deciduous forests. in the p
g term changes in conditions related to soil and climate may impact on these habitats. two basi l gradients in community composition of grasslands and deciduous forest, and examine the niche |
| 11238 | 1 | lders. the focus will be on the role of protected areas within conservation strategies. the pro
|
| 2181 | 1 | ecological effects of climate change on terrestrial ecosystems . this project will provide a ne
|
| 166 | 1 | f suspension feeding communities in the coastal ecosystems.
|
| 6877 | 1 | enomenon characterizes first of all the soil fauna and it is the main subject of our researches
|
| 14772 | 1 | spatial variation, as well as to their soil characterization and geomorphology. remote sensing
|
| 14762 | 1 | directive to spain requires knowing the wetlands in our country as comprehensively as possible.
|
| 1925 | 17 | nitrogen and other nutrient losses from soil are important policy objectives. there are strong
s. there are strong indications that in terrestrial ecosystems the occurrence of plant diseases related to the diversity of vegetation. soil-borne diseases are rare in natural ecosystems with al hypothesis that high biodiversity in terrestrial ecosystems confers high soil suppressive ne in terrestrial ecosystems confers high soil suppressive ness against diseases and high nutrien diseases and high nutrient retention in soil. this follows from the working hypothesis that the poser subsystem, i.e. the heterotrophic soil community, is a key feature in terrestrial ecosyst hic soil community, is a key feature in terrestrial ecosystem functioning. permanent grassland strial ecosystem functioning. permanent grassland and agricultural fields, derived from the sam icultural fields, derived from the same grassland 20 years ago, will be compared in terms of ab lant biomass and litter, in relation to soil suppressive ness and nutrient fluxes. part of the e ness and nutrient fluxes. part of the grassland will be turned into agriculture. in addition relationships between biodiversity and soil suppressive ness and nutrient retention and the ch ication of the ecosystem. the degree of soil suppressive ness will be experimentally tested by sitive test plants and the potential of soils to reduce the development of plant pathogen popul itrogen turnover in the food web in the soil-plant system will be measured and simulated in ord e relationship between biodiversity and soil suppressive ness and nutrient retention will allow |
| 1924 | 17 | nitrogen and other nutrient losses from soil are important policy objectives. there are strong
s. there are strong indications that in terrestrial ecosystems the occurrence of plant diseases related to the diversity of vegetation. soil-borne diseases are rare in natural ecosystems with al hypothesis that high biodiversity in terrestrial ecosystems confers high soil suppressive ne in terrestrial ecosystems confers high soil suppressive ness against diseases and high nutrien diseases and high nutrient retention in soil. this follows from the working hypothesis that the poser subsystem, i.e. the heterotrophic soil community, is a key feature in terrestrial ecosyst hic soil community, is a key feature in terrestrial ecosystem functioning. permanent grassland strial ecosystem functioning. permanent grassland and agricultural fields, derived from the sam icultural fields, derived from the same grassland 20 years ago, will be compared in terms of ab lant biomass and litter, in relation to soil suppressive ness and nutrient fluxes. part of the e ness and nutrient fluxes. part of the grassland will be turned into agriculture. in addition relationships between biodiversity and soil suppressive ness and nutrient retention and the ch ication of the ecosystem. the degree of soil suppressive ness will be experimentally tested by sitive test plants and the potential of soils to reduce the development of plant pathogen popul itrogen turnover in the food web in the soil-plant system will be measured and simulated in ord e relationship between biodiversity and soil suppressive ness and nutrient retention will allow |
| 14932 | 4 | eans that inhabit exclusively temporary wetlands. many temporary wetlands are threatened by ant
vely temporary wetlands. many temporary wetlands are threatened by anthropogenic pressure assoc f ecologically hardly studied temporary wetland species. they survive in diapausing resting sta stages during dry periods, and once the wetlands fill after precipitation events, they grow ver |
| 12636 | 9 | the role played by soils in providing wellbeing to society has been clearl
been clearly articulated in the recent soil strategy for england. the continued provision of b ontinued provision of benefits from the soil to society is dependent on the physical, chemical, mical, and biological properties of the soil being maintained. however, much evidence suggests d. however, much evidence suggests that soil degradation, associated with the loss of integrity ted with the loss of integrity in these soil properties, results in significant costs, not only t costs, not only to immediate users of soils but also to society as a whole, now and into the according to the thematic strategy for soil protection . we will explore options for stratifyi d wales into a small number of distinct soil/ ecosystem types and adopt one of these typologies |
| 11740 | 5 | ation and bacterial activity, such that wetlands could expand and associated methane emissions
c biomarkers for bacterial processes in wetlands to provide a better understanding of the contr epresent a spatially averaged signal of wetland extent. from the biomarker abundance records, w not a significant expansion of tropical wetlands occurred coincidentally with the increase in m rovide crucial insight into the role of wetlands - and by comparison, that of clathrates - as a |
| 471 | 1 | w translating landscapes or networks of protected areas into functional connectivity. tenlamas
|
| 13801 | 4 | eveloping knowledge about how secondary grassland habitats, grazed forests and grazed former ar
diversity associated with semi-natural grasslands of high conservation value, under conditions e, under conditions where the secondary grasslands are located close, or adjacent, to the semi- close, or adjacent, to the semi-natural grasslands. the main objectives of the programme are to |
| 12263 | 2 | ll disease and / or ability to restrict soil inoculum build up in 1st wheat situations - introg
the interconnections between the three soil based traits - archiving of grain at low temperatu |
| 10903 | 1 | tion water depends strongly on mountain wetland management, and is potentially threatened by gl
|
| 11801 | 1 | tion water depends strongly on mountain wetland management, and is potentially threatened by gl
|
| 11298 | 2 | th s carbon, locked away in the organic soils and peat of arctic tundra and extensive mire syte
e forcing since the pre-industrial era. wetlands play an important dual role in the global carb |
| 13977 | 3 | gi are very sensitive to changes in the soil environment and most are negatively affected by th
ely affected by the increased levels of soil n resulting from forest fertilisation. we are slow potential for the fungi to acidify the soil during nitrate uptake was recently highlighted and |
| 10043 | 2 | the agro-ecosystems of the semi-arid west africa provide th
tem productivity will effect on-and off-farm ecosystem resources. this proposal aims to begin d |
| 209 | 9 | ophyte and vascular plant vegetation of wetland communities. study communities are fens, floodp
nities are fens, floodplain and coastal grasslands. the prolonged inundation periods have forme lant and bryophyte species diversity in wetland communities and what is the role of bryophytes phytes in restoring species richness of wetlands. study sites are located in floodplain grassla . study sites are located in floodplain grasslands at alam-pedja and endla nature reserves, and ng the project: 1 specific hydrology of wetlands has different influence on vascular plants and as management cessation in semi-natural wetland communities has long-term influence on species rict ecological demands can be found in wetlands due to their specific ecological conditions, 5 their specific ecological conditions, 5 wetland communities have long-lived bryophyte diaspore |
| 13440 | 10 | 008-2009 where food web structure among soil fauna, mainly collembola, acari and other small ar
we plan to extend the studies to other soil fauna groups and to microorganisms to get a holist icture. we ask the questions: - how are soil organism communities in tropical agriculture influ rops and cultivation intensity - is the soil organism food web more stable and resilient in agr re stable and resilient in agricultural soils with high levels of organic matter than in deplet vels of organic matter than in depleted soil - which species and groups get their nourishment d d organic matter the composition of the soil fauna will be analyzed by sampling of soil, extrac l fauna will be analyzed by sampling of soil, extraction and determination. microorganisms will sotope ration of 13c/12c and 15n/14n in soil animals and in fatty acids that are markers of dif s of organic fertilizer application and soil cultivation the crop will be labeled with 13c and |
| 14517 | 1 | intense interaction between aquatic and terrestrial ecosystems. riparian vegetation, among othe
|
| 10157 | 2 | ve distributions, other factors such as soil conditions, fire and disturbances such as grazing
local collaborators to examine climate/soil/disturbance associations in key hot spot rainfores |
| 10174 | 2 | ve distributions, other factors such as soil conditions, fire and disturbances such as grazing
local collaborators to examine climate/soil/disturbance associations in key hot spot rainfores |
| 10426 | 2 | ve distributions, other factors such as soil conditions, fire and disturbances such as grazing
local collaborators to examine climate/soil/disturbance associations in key hot spot rainfores |
| 11426 | 2 | ve distributions, other factors such as soil conditions, fire and disturbances such as grazing
local collaborators to examine climate/soil/disturbance associations in key hot spot rainfores |
| 11711 | 2 | ve distributions, other factors such as soil conditions, fire and disturbances such as grazing
local collaborators to examine climate/soil/disturbance associations in key hot spot rainfores |
| 11712 | 2 | ve distributions, other factors such as soil conditions, fire and disturbances such as grazing
local collaborators to examine climate/soil/disturbance associations in key hot spot rainfores |
| 12052 | 2 | disciplinary approach: botany, ecology, soil science, geochemistry, genetic, molecular biology
developed to evaluate the importance of soil constraints associated to ultramafism possible in |
| 11627 | 1 | , rainfall forecasting, atmospheric and groundwater transport, and the impacts of land use and
|
| 12262 | 2 | nmentally and economically sustainable. grassland represents more than 70% of the uk`s agricult
he need for environmentally sustainable grassland agriculture. |
| 10223 | 5 | nition, management and valuation of the watershed services that support ecosystems and people h
of water for these demands by improving watershed management has become increasingly important, stion, we seek to better understand how watershed processes function in landscapes that are sha nto the ways in which understandings of watershed processes - both scientific and local - influ practices could contribute to equitable watershed management in andean countries. |
| 11694 | 5 | nition, management and valuation of the watershed services that support ecosystems and people h
of water for these demands by improving watershed management has become increasingly important, stion, we seek to better understand how watershed processes function in landscapes that are sha nto the ways in which understandings of watershed processes - both scientific and local - influ practices could contribute to equitable watershed management in andean countries. |
| 15533 | 1 | alter nitrogen cycling in the riparian soil, and nitrogen exchanges with the stream, through p
|
| 15534 | 1 | alter nitrogen cycling in the riparian soil, and nitrogen exchanges with the stream, through p
|
| 10133 | 3 | s suddenly become invasive, taking over island ecosystems and thereby suppressing ground breedi
of breeding seabirds who fertilise the soil and disturb the vegetation through burrowing and t es and from which they gradually invade island ecosystems. the problem occurs not only in scotl |
| 7668 | 6 | coastal ecosystems host high human population densities
roughout coastal asia, deforestation of mangrove for intensive shrimp farming has had ecologica ing incidence of large disturbances the mangrove ecosystems in indonesia represent one fourth o sia represent one fourth of the world’s mangroves. on both sides of the malacca strait, two con years of sustainable management of the mangroves has resulted in a resilient socio-ecosystem. socio-ecosystem. across the strait, the mangroves in north sumatra have been transformed for aq |
| 13770 | 4 | sh plant diversity is associated to the agricultural landscape, especially traditionally manage
ally traditionally managed semi-natural grasslands. the most common way of studying landscapes andscape matrix, including semi-natural grasslands as well as secondary grasslands and new past natural grasslands as well as secondary grasslands and new pastures . by examining different pa |
| 10624 | 1 | questration and emission of carbon from soil. ecm species are likely to respond differently to
|
| 11586 | 1 | urn for mineral nutrients taken up from soil. this is a mutualistic symbiosis where both partne
|
| 11599 | 4 | t led to flammable vegetation, dry peat soils and the potential for severe ecological impacts.
uk emmissions. smoulering and extensive soil heating also destroys belowground plant structures stroys belowground plant structures and soil seedbanks leading to fundamental changes in patter environmental impacts such as increased soil erosion. despite the serious environmental consequ |
| 12603 | 1 | evidence on a the causes of c loss from soils and b the fate of the lost c. the purpose of this
|
| 6809 | 1 | vertebrate remains, - study the fossil soils for paleoclimate and water budget, - sedimentolog
|
| 11725 | 15 | urban areas are often regarded as being of little impor
ng directed at rural habitats. however, urban habitats are occupied by many species, some of wh despite the potential importance of the urban environment for wildlife, our knowledge of urban ironment for wildlife, our knowledge of urban ecology is surprisingly poor; furthermore, we kno sition from being a rural species to an urban one. the aim of this project is to investigate ho project is to investigate how a typical urban bird, the blackbird, has become such a familiar s detail the blackbird s colonisation of urban areas across europe since the earliest records in n dna samples from blackbirds in paired urban and rural samples along a transect from the earli st areas of colonisation to areas where urban occupation is currently occurring; we will then t similarity of blackbird populations in urban and rural habitats. results of these analyses wil ses will enable us to determine whether urban blackbirds: have a single origin, with subsequent igin, with subsequent spread into other urban areas by the dispersal of urban-adapted blackbird o other urban areas by the dispersal of urban-adapted blackbirds from one city to another acros ird objective is to investigate whether urban blackbirds differ from rural ones in either their nd blood parasites. differences between urban and rural populations will be assessed in order t |
| 13744 | 5 | urban nature is often severely fragmented and only smal
nswer questions about factors affecting urban biodiversity. birds will be surveyed from may to be surveyed from may to august in >500 urban parks distributed over 36 cities. these data will city level, in the proportional area of urban forest fragments. we will also examine species ri ing birds will be investigated along an urban to rural gradient, and across forest ecotones, to |
| 15581 | 17 | 75% in europe.the understanding of how urban ecosystems work, how they change, and what limits
tion. ecosystems provide flexibility in urban landscapes and help build adaptive capacity to co flooding. to address these challenges, urban social-ecological systems analyses represent an e sustainable planet that is increasingly urban. recent literature indicate that urban biodiversi urban. recent literature indicate that urban biodiversity contributes to multiple es of very l rtance for the citizens’ well-being and urban biodiversity may also be part of decreasing the e ium will focus on functional diversity, urban ecosystem services, institutions, economics and r ed to promote sustainable management of urban biodiversity and ecosystem service generation and s to important stakeholders. cluster i: urban biodiversity and ecosystem services what are the the drivers behind loss/enhancement of urban ecosystem services and how do they interact acros use change on ecosystem functioning and urban ecosystem services what are the roles of species functional diversity for generation of urban ecosystem services cluster ii. valuation of biodi diversity and ecosystem services in the urban landscape how can monetary and non-monetary ecosy system services and facilitating needed urban transformations cluster iv communication and trai s cluster iv communication and training urban europe has entered a critical development stage w tural resource shortage and patterns of urban growth and decline linked to demographic and econ nmental, social and economic balance of urban societies already in the near future. therefore, |
| 10542 | 5 | s of high landscape and cultural value. grassland species richness declines where the soils are
and species richness declines where the soils are enriched in phosphorus. a balanced phosphorus nalysing the phosphorus status of their soils, trapping flood sediments for phosphorus analysis of sediments immediately downstream of urban areas compared to previously collected winter sam e sediments deposited at ten floodplain grassland sites . the samples will be analysed for thei |
| 11770 | 1 | nd habitats. marine reserves, or marine protected areas and other fragile bottom animals agains
|
| 9958 | 4 | hanges in the structure and function of terrestrial ecosystems. human activities are also respo
in the activity and composition of the soil microbial community, and storage of additional nut st-fire microbial community dynamics in soils of contrasting composition, and its link with soi trasting composition, and its link with soil nutrients. in addition, we will obtain extremely v |
| 12055 | 2 | this pine forest pest is turning to an urban sanitary threat. breaking with a traditionally ap
t- and long- term management methods in urban areas, including the mapping of the areas at sani |
| 7248 | 4 | the objectives of soil organic matter and is interested in the evolution
compartments tetraethers on a reference soil. quantitative and qualitative comparison between t on of previously developed at different soil horizons method of ore"meadow"and the site of clos sition of individual tetraethers in the soil closeaux. demonstration of the influence of the ch |
| 7252 | 1 | ered priority: animal feed, fish, food, soil improvement, crop protection,.... by selected appl
|
| 14786 | 7 | nsformation making heavy metal polluted soils a major environmental concern and a health hazard
hat can be used to clean metal polluted soils are complex and expensive processes both from an ed as a system to clean up contaminated soils and to immobilise toxic elements. mycorrhiza are mobilise toxic elements. mycorrhiza are soil organisms that provide a unique link between the s that provide a unique link between the soil system and the plant, and can therefore be of impo ed. fungi from heavy metal rich natural soils or contaminated soils will be isolated and charac etal rich natural soils or contaminated soils will be isolated and characterised. the effects o |
| 13812 | 4 | semi-natural grasslands have the highest species-richness in the rur
iversity in the future. as many typical grasslands species are dispersal-limited the present ma this have, and will affect dispersal of grassland species. the results will lead to recommendat n for managing rural landscape not only grasslands. methods are: 1. historical sources will be |
| 12197 | 1 | ensity grazing options for agricultural grassland that aim to deliver substantial benefits for
|
| 10900 | 2 | h state and federal laws. 5. whilst the urban and peri-urban poor might not be affected directl
eral laws. 5. whilst the urban and peri-urban poor might not be affected directly by deforestat |
| 12293 | 4 | d identifying osr-infecting isolates in soil and in planta. identification of infection can be
to rapidly quantitate the fungus in the soil will enable us to study risk factors and predict d tive diagnostics will potentially allow soil-testing services which will allow growers to ident ead is it; how long does it last in the soil; how serious is yield loss in our wetter climate 4 |
| 15574 | 3 | he maintenance of fertility in mountain grasslands, how these are perceived to be affected by m
plant species with different traits on soils from intensively / extensively managed grasslands from intensively / extensively managed grasslands. analyses of realised plant and microbial fu |
| 7247 | 1 | oals it is to study the reaction of the soil-water -plant system as a result of diffuse metal p
|
| 12583 | 7 | scribe the potential threats to organic soils in england & wales, estimate their likely magnitu
in order to assess the state of organic soils and their potential vulnerability to future manag hreats. the causes and types of organic soil degradation will be identified and prioritised for and and wales. the functions of organic soils will be reviewed of the potential carbon that cou d from the atmosphere and stored by the soil and the reduction in carbon losses that could be p mining the economic benefits of organic soil conservation and prioritise future research needs provide guidance on the most promising soil protection schemes in the uk. |
| 10145 | 3 | pes, through changes to river flows and soil moisture levels which radically change patterns of
t they both contain large and important wetlands, which thus provide the opportunity to study t cle and other ecosystem services of the wetlands. both basins are important geographic and poli |
| 10979 | 3 | pes, through changes to river flows and soil moisture levels which radically change patterns of
t they both contain large and important wetlands, which thus provide the opportunity to study t cle and other ecosystem services of the wetlands. both basins are important geographic and poli |
| 13854 | 5 | half of the world´s population lives in urban areas. the urbanization process poses significant
the project fauna in urbanising areas - wetlands and small waters , the conference is a good op gated in 64 ponds and small lakes in an urban-rural gradient in and around stockholm. as explan bles and spatially explicit, quantified urban disturbances like density of human population, re improved by incorporating landscape and urban disturbance variables. |
| 14859 | 1 | sity in mediterranean dryland extensive agroecosystems. the project compares two contrasted mod
|
| 12719 | 1 | d livestock from existing and potential wetlands, consider whether there are any common themes
|
| 7424 | 1 | mproving the production biodiversity in agricultural landscapes. are they effective they cost t
|
| 11732 | 2 | ot known how much each component of the soil-plant continuum contributes to this seasonality. w
easurements will be used to calibrate a soil-plant-atmosphere model, which will be used to scal |
| 10014 | 1 | aberdeen, as well as in a wide range of soil physical and chemical analyses.
|
| 413 | 3 | ation, along the renewed cleavage lines urban-rural and centre-periphery does empirical support
politicisation along the cleavage lines urban – rural and centre – periphery may be of importan n have about the cleavage lines rural – urban and centre – periphery. this is a multidisciplina |
| 10355 | 4 | that the rate of growth seems driven by soil fertility, and, surprisingly, not by climate. this
d forest plots on fertile and infertile soils, with experiment design duplicated in two regions t to measure nutrient demand within the soil, to explore which soil nutrient may be limiting. emand within the soil, to explore which soil nutrient may be limiting. |
| 10747 | 4 | that the rate of growth seems driven by soil fertility, and, surprisingly, not by climate. this
d forest plots on fertile and infertile soils, with experiment design duplicated in two regions t to measure nutrient demand within the soil, to explore which soil nutrient may be limiting. emand within the soil, to explore which soil nutrient may be limiting. |
| 9976 | 4 | that the rate of growth seems driven by soil fertility, and, surprisingly, not by climate. this
d forest plots on fertile and infertile soils, with experiment design duplicated in two regions t to measure nutrient demand within the soil, to explore which soil nutrient may be limiting. emand within the soil, to explore which soil nutrient may be limiting. |
| 13560 | 3 | nitrogen levels of soil moisture. during succession humus depth increases
umus depth increases and this increases soil moisture retention; we will determine the response determine the response of n fixation to soil moisture status. by investigating these three fact |
| 12162 | 4 | grassland is the predominant habitat in the agri-enviro
ion such as the integrity and health of soil resource. there is therefore a need to identify op n deliver a range of benefits including grassland faunal diversity and abundance enhancement, s al diversity and abundance enhancement, soil structural amelioration and nutrient retention and |