IdNumber of occurencesForms
7300 1                                     the pollination of flowering plants is mainly provided by i 
7500 1 iological indicators to manage the pest soil quality  
11864 4 ausing plant life to take over the lake carbon entering from surrounding land. this research is 
actices. the consumption of terrestrial carbon by species in the lake can also be affected by i 
ies in the lake can also be affected by invasive species such as the zebra mussel which voracio 
 which voraciously consumes within-lake carbon and is rapidly spreading through irish and u.k.  
10966 2 ring the part of the system between the soil and the speleothem, using comprehensive measuremen 
 composition of cave air, temperatures, soil and vegetation changes, and related these to amoun 
14360 1  which are most important for assessing habitat quality - most existing remote sensing methodol 
12585 3 ecent years the emphasis has shifted to soil and water conservation, enhancement of carbon sequ 
shifted to soil and water conservation, enhancement of carbon sequestration for climate change  
ation for climate change mitigation and flood protection goals. these changing objectives and a 
11767 1 uantify the the effects of temperature, litter quality and rainfall on the decay rates of leaf  
11791 1 ts quantify the effects of temperature, litter quality and rainfall on organic matter decay rat 
9983 1 uantify the the effects of temperature, litter quality and rainfall on the decay rates of leaf  
12596 7 ities of greenhouse gases, particularly carbon dioxide, thereby contributing to global warming. 
promoted as a means of restarting their carbon sink function so that they take up or sequester  
 so that they take up or sequester more carbon from the atmosphere in the form of carbon dioxid 
rbon from the atmosphere in the form of carbon dioxide than they release to it; that is, so tha 
release of methane from peatlands. like carbon dioxide, methane is a carbon gas, but it is much 
ands. like carbon dioxide, methane is a carbon gas, but it is much more potent as a greenhouse  
en the uncertain role of methane in the carbon balance of restored peatlands, this study aims t 
10072 1 ns, effecting how key elements, such as carbon and nitrogen, are cycled within aquatic environm 
13457 8 n intensified production may impair the carbon sequestration in the soil and increase release o 
 impair the carbon sequestration in the soil and increase release of carbon to the atmosphere d 
ion in the soil and increase release of carbon to the atmosphere due to actions by the microorg 
s by the microorganisms responsible for carbon cycling in agricultural soils. global climate pr 
epend today on models that estimate the carbon fluxes from soils under land use and climate cha 
identity of the key microbial actors of carbon cycling in soils. the aim of this project is to  
n gene level that is directly affecting carbon cycling in agricultural soils. we propose here a 
 involved in the degradation of complex carbon sources, that is up to 200 times faster and 100  
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 
15064 1 ersing individuals are crucial elements regulating population dynamics, trajectories, spatial a 
13742 1 white stork demands large areas of high quality habitat to sustain. preferred habitats are wetl 
12267 2 etation of the significance of biogenic carbon is key to drawing conclusions on the impacts of  
nge. many lca studies discount biogenic carbon as there is no net emission between its sequestr 
14751 1 sical-chemical properties attributes of soil quality.  
10280 1 to account for about half of the annual carbon fixation in seasonally stratified shelf seas, an 
10553 1 to account for about half of the annual carbon fixation in seasonally stratified shelf seas, an 
10522 7 d food, in supporting recreation and in protecting species diversity. however, the stability of 
rectives that set stringent targets for water quality and biodiversity. meeting these targets r 
ed to make such measurements, automatic water quality monitoring stations . however at present, 
nts. a few have other probes to measure water quality, but these are subject to biofouling whic 
he effect of meteorology on the fate of carbon within lakes: we will track pool and flux variab 
 pool and flux variability of dissolved carbon dioxide over daily to seasonal time scales. by r 
to define critical controls on the lake carbon cycle. dst3: the level of regional coherence in  
10752 7 d food, in supporting recreation and in protecting species diversity. however, the stability of 
rectives that set stringent targets for water quality and biodiversity. meeting these targets r 
ed to make such measurements, automatic water quality monitoring stations . however at present, 
nts. a few have other probes to measure water quality, but these are subject to biofouling whic 
he effect of meteorology on the fate of carbon within lakes: we will track pool and flux variab 
 pool and flux variability of dissolved carbon dioxide over daily to seasonal time scales. by r 
to define critical controls on the lake carbon cycle. dst3: the level of regional coherence in  
10756 7 d food, in supporting recreation and in protecting species diversity. however, the stability of 
rectives that set stringent targets for water quality and biodiversity. meeting these targets r 
ed to make such measurements, automatic water quality monitoring stations . however at present, 
nts. a few have other probes to measure water quality, but these are subject to biofouling whic 
he effect of meteorology on the fate of carbon within lakes: we will track pool and flux variab 
 pool and flux variability of dissolved carbon dioxide over daily to seasonal time scales. by r 
to define critical controls on the lake carbon cycle. dst3: the level of regional coherence in  
11807 7 d food, in supporting recreation and in protecting species diversity. however, the stability of 
rectives that set stringent targets for water quality and biodiversity. meeting these targets r 
ed to make such measurements, automatic water quality monitoring stations . however at present, 
nts. a few have other probes to measure water quality, but these are subject to biofouling whic 
he effect of meteorology on the fate of carbon within lakes: we will track pool and flux variab 
 pool and flux variability of dissolved carbon dioxide over daily to seasonal time scales. by r 
to define critical controls on the lake carbon cycle. dst3: the level of regional coherence in  
10264 1 he only consequence of rising levels of carbon dioxide in the atmosphere. because co2 is an aci 
10031 1 c soils provide a major global store of carbon could provide an enhanced sink for atmospheric c 
11825 1 c soils provide a major global store of carbon could provide an enhanced sink for atmospheric c 
211 1 of human-degraded ecosystems, and their habitat quality for threatened species, can be signific 
10053 1 ions are currently exposed to levels of carbon dioxide more than twice as high as those of the  
12148 1  project is to study the adaptations of invasive species and their impacts on the ecosystems of 
13737 1 ut vary in the waters levels of organic carbon and inorganic aluminium content, and in streams  
12067 1 tems makes them less prone to cope with invasive species . some of which are clearly detrimenta 
13362 1  the material will be evaluated as free pollination and hybrid variety or lines.  
6843 1 ts are released by decomposition in the soil and litter horizont. the decomposition process dri 
7051 6  in agroecosystem management affect the natural control of pests. the effects of agricultural c 
ffecting it remain to be understood. as biological control is effectively the product of networ 
food web interactions affect parasitoid aphid control. based on the fieldderived data, cage exp 
tity affect parasitoid interactions and pest control, complementing the field results. the work 
d here will take research on parasitoid aphid control one step further, as it will provide a cl 
s, allowing for further improvements in natural pest control.  
10639 2  calling for geo-engineering methods of carbon capture and sequestration . it brings together c 
k soils is likely to lead to successful carbon sequestration and the consequences for the stabi 
7417 1 era aphid natural enemies of aphids and pollinators, linked to the type of grass cover on the s 
13310 1 tal chemicals, biological invasions and pollinator loss in the context of current and future eu 
2522 1 op monitoring and action plans for this invasive species.  
12016 2 xt. we have studied the impact of alien invasive species in invaded communities, taking the rat 
ing of the complexity of the impacts of invasive species when introduced to or removed from isl 
13743 10  space and nutrients. however, although pollination is vital for reproductive success in about  
ms established between alien plants and native pollinators. first, a complete pollination netwo 
d native pollinators. first, a complete pollination network will be mapped in a habitat that ha 
ow alien plants integrate into a native plant pollination network. knowledge about the centrali 
en plants integrate into a native plant pollination network. knowledge about the centrality of  
iment will be performed to estimate how pollinator visitation, seed set and seed size is affect 
riment will be a subset from the mapped pollination network. to study the ability of invasive s 
nation network. to study the ability of invasive species to establish facilitative interactions 
to predict the effect of alien plant on pollination interactions whole pollination networks has 
alien plant on pollination interactions whole pollination networks has to be studied.  
12355 1 se - why is the r&d needed the food and environment protection act of defra and samples for ana 
10527 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
10774 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
11051 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
11574 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
11816 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
11817 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
11820 3 rgest reservoir of above-ground organic carbon and are exceptionally species rich. they are und 
iple constraint and mutually consistent carbon fluxes over the four-year measurement period. we 
rly constrained component of the global carbon cycle, based on a new understanding of the under 
11235 1 cines, rainfall regulation and a global carbon sink. internationally, there is an urgent need t 
10573 1  use change, which may trigger enhanced carbon losses, greenhouse gas emissions and habitat deg 
12479 1 , and services such as purifying water, pollinating crops and providing a natural defence again 
10650 10 ore as much as one-third of global soil carbon and represent a highly important global carbon d 
and represent a highly important global carbon dioxide sink, with an amount of stored carbon re 
 dioxide sink, with an amount of stored carbon representing 25-50% of current levels of atmosph 
 their ability to continue to sequester carbon dioxide and their botanical composition under fu 
ut research into their ability to store carbon during former periods of climate change can prov 
 been shown that changes in the rate of carbon accumulation during the medieval warm period and 
when investigating long-term records of carbon accumulation, but this, unfortunately is not alw 
its which contain millennial records of carbon accumulation rate changes, and in this way recon 
the spatial and temporal variability of carbon sequestration. this research seeks to redress th 
og deposits contain detailed records of carbon sequestration rate changes, and also provide pro 
10079 6                                         pollination ecology in now able to explain and predict  
logy in now able to explain and predict pollinator-mediated gene flow. the comprehensive model  
ey elements of our conventional view of pollination and offers a powerful understanding of a pr 
ies. the model can be applied to insect-pollinated crops and so yield predictions about the lev 
he model and three previously unstudied pollination processes that may affect the accuracy of i 
l in developing a full understanding of pollinator-mediated gene flow and thus supporting accur 
15038 3  further than the direct impacts by the invasive species, such as changes in species compositio 
dentifying special sensitive regions to invasive species and, with them specific communities. u 
cies is considered one of the 100 worst invasive species in europe and in the mediterranean sea 
14417 1 to be a wide field for biodiversity and environmental protection investigations. the resistance 
10344 1 p will study the supply of nitrogen and carbon to the bacteria and algae, how this is affected  
13786 1 for improving baculovirus efficiency in biological control. it can also give insights into anti 
15333 1 ispersal and subsequent recruitment, on pollination, and even on vertebrate fauna. ants are con 
15575 12 ices mediated by biodiversity are rare. biological pest control is one ecosystem service threat 
ut the mechanisms behind such landscape-pest control relationships. moreover, the relationship  
hip between natural enemy diversity and biological control is not straightforward. even though  
use and natural enemy diversity affects biological control. it has been shown that the structur 
ication with important implications for biological control. however, to date no study has explo 
 food web interactions and the value of biological control. our study system will be cereal aph 
fts in natural enemy communities affect biological control. using up-to-date molecular techniqu 
rent scales affects trophic linking and biological control. these data will feed into a model f 
. these data will feed into a model for biological control of cereal aphids, and facilitate val 
al aphids, and facilitate valuations of biological control through monetary and non-monetary me 
-monetary methods. finally, we will map biological control across landscapes in europe and test 
 and landscape structure will influence biological control.  
10103 5  seeds and supply the young plants with carbon and nutrients. this unique form of nutrition con 
ss spectrometer enabling the individual carbon and nitrogen containing compounds to be identifi 
f the composition and concentrations of carbon and nitrogen-containing compounds can be made in 
gal partner, in adjacent cells in which carbon is stored by the plant and the fungus excluded,  
ular tissue through which nutrients and carbon pass up into the shoots.  
7034 1 ed to assess the flux of energy, water, carbon and nitrogen corresponding to a given vegetation 
12490 3 ling due to ammonium sulphate aerosols; air quality management for ecosystem protection has pri 
tems approach with current conventional air quality management approaches to determine which as 
mentation of an ecosystems approach for air quality policy development at national level in the 
11045 1                                     the regulation of water transport is fundamental to the sur 
11057 1                                     the regulation of water transport is fundamental to the sur 
7035 6 in the landscape that transport organic carbon from the continents to the oceans. recent studie 
ystem metabolism on terrestrial organic carbon — in streams and rivers. obviously, these observ 
ons raise the question: how can organic carbon that was initially stored in soils over extended 
pended aggregates, are major drivers of carbon cycling in streams and large rivers. first, we w 
pine, tropical and arctic networks. the carbon cycle in these biomes is predicted to be particu 
formance to oxidize terrestrial organic carbon.  
10183 1  central to marine foodwebs, the global carbon cycle and represent a key life-stage of many ben 
11636 2  of considerable microbial diversity in soil and the existence of many groups with no cultivate 
quencing of large fragments of dna from soil and marine environments indicate a possible functi 
10070 1 om the soil for access to plant organic carbon. however, we know surprisingly little about how  
14540 2 ginal from america, which behaves as an invasive species, outcompeting the autochthonous artemi 
 as possible the presence of the exotic invasive species. the research on life span for specime 
13875 1 ar species, and the introduction of new invasive species. the project will test for quantittive 
12590 3 y requirement for reliable data on soil carbon on which evidence-based policy decisions can be  
 be made. recent evidence suggests that carbon is being lost from soils in england and wales, b 
 the spatial and temporal properties of carbon in soils. • using the decision tool to define th 
12291 5 nge. in the last 30 years, agricultural weed control has been dominated by the use of herbicide 
icides, in order to deliver sustainable control of weeds. a key objective of this research is t 
hanges in herbicide availability on the control of weeds in uk arable cropping rotations. as it 
incorporate more cultural, physical and biological weed control options. this modelling-based p 
ticular, the development of alternative weed control strategies will require research to better 
12550 2 agriculture and the environment through pollination: they also produce honey and wax. the honey 
 use of antibiotics to achieve improved disease control of efb. shook swarm involves transferri 
10156 3 se studies and, indeed, the majority of disease control programmes of humans and domestic anima 
sign of truly effective and sustainable disease control programs. if control approaches only co 
e a vital tool for developing long-term disease control strategies in other host species, such  
11676 3 se studies and, indeed, the majority of disease control programmes of humans and domestic anima 
sign of truly effective and sustainable disease control programs. if control approaches only co 
e a vital tool for developing long-term disease control strategies in other host species, such  
12615 1 r statutory duties under part 2a of the environmental protection act 1990, e.g. where sites whi 
12272 1 ncluding food security, climate change, environmental protection, uk and eu government policy,  
7457 2  a changing climate on the quantity and quality of water in mountain regions. modeling techniqu 
and the health implications of changing water quality. attention will also be devoted to the in 
12646 1 ce, and hence the effectiveness, of the environmental protection , through an assessment of wil 
13778 2  that are necessary for quantifying the carbon flux through this part of the pelagic community  
tion. by applying laboratory determined carbon budgets and vital rates to data on abundance, si 
10191 1 es an essential pointer to the possible biocontrol of some invertebrate forest pests. the work  
10002 2 gions directly influences the burial of carbon and nutrient cycling. long-term research has now 
, a significant input for ecosystem and carbon budget modelling. our effort will also have impa 
12595 1 r a range of ecosystem services such as carbon capture and other government requirements such a 
12606 1 ighlighted. additionally, the potential carbon storage achievable with each management option w 
7249 1  temporal variability of contamination, invasive species now widely present in temperate aquati 
12015 1                                     the protection of nature imposes the twin requirements of c 
7104 2 nsidered in the banal spaces, since the environmental protection strategies compete with other  
mpact on the natural environment versus environmental protection hampers economic and social de 
516 2 dered in ordinary areas, as soon as the environmental protection strategies enter into competit 
hropization on natural areas versus the protection of the environment, which compromise the eco 
11619 1                     in all environments carbon and nutrients are recycled by organisms that dec 
10724 2 ental agencies to assess the health and carbon budgets of soil and freshwater environments.  
assess the health and carbon budgets of soil and freshwater environments.  
14846 3 ammonia to nitrate and fixing inorganic carbon in the dark. in addition, they also seem to be a 
em to be an important source of organic carbon in the sediments of aquatic systems. the project 
e biodiversity and role in nitrogen and carbon biogeochemical cycling of this enigmatic group o 
14845 3 ammonia to nitrate and fixing inorganic carbon in the dark. in addition, they also seem to be a 
em to be an important source of organic carbon in the sediments of aquatic systems. the project 
e biodiversity and role in nitrogen and carbon biogeochemical cycling of this enigmatic group o 
1977 1 rophic prokaryotes obtaining energy and carbon from cold seeps e.g. via methane. benthic lander 
396 1 lants, soil animals, predatory insects, pollinators and two ecosystem services along a time-sin 
13729 1  contributes to ecosystem services like pollination and resilience in selected managed ecosyste 
13942 1 nity has the potential to transfer more carbon up the food chain. 3. a more diverse community b 
14821 2 park, as a first step to evaluating the water quality and the level of conservation of its aqua 
ose friendly methods for the control of environmental quality of transitional waters, which cou 
14419 1  they are primary drivers of the global carbon cycle and they belong to the most valuable micro 
7286 1 d reduce this risk by being a source of pollinators for fragmented populations and favorable re 
14716 2 ncy as an alternative technology in the biological control of the lepidoptera spodoptera littor 
roviding a base for tthe development of biocontrol agents which are environmentally, reducing e 
10561 2                                         carbon is one of the essential elements required for li 
ts of the earth s biosphere, cycling of carbon compounds beneath glaciers and ice sheets is poo 
12036 1 ario of invasion which applies to three invasive species considered: the invasive bridgehead sc 
7642 2 eavily involved in the operation of the soil and thus to the provision of ecosystem services. b 
ns in the macro- and meso- fauna of the soil and thus a wide spectrum of biological strategies. 
14743 2                                         invasive species can pose a major threat to the biotic  
establishment and eventual expansion of invasive species in aquatic systems are not well unders 
10129 2 oil biological and functional diversity carbon isotope and trace where that carbon is used and  
ity carbon isotope and trace where that carbon is used and emitted - ie how much labeled co2 is 
10417 2 oil biological and functional diversity carbon isotope and trace where that carbon is used and  
ity carbon isotope and trace where that carbon is used and emitted - ie how much labeled co2 is 
11411 2 oil biological and functional diversity carbon isotope and trace where that carbon is used and  
ity carbon isotope and trace where that carbon is used and emitted - ie how much labeled co2 is 
9891 2 oil biological and functional diversity carbon isotope and trace where that carbon is used and  
ity carbon isotope and trace where that carbon is used and emitted - ie how much labeled co2 is 
2550 2 ane, a potent greenhouse gas, as a sole carbon and energy source. methylacidiphilum kamchatkens 
so play a role in detoxification and/or carbon assimilation. the organelles will be purified fr 
14421 3  introduction and spread of the studied invasive species and their impact on the local biodiver 
 a book on the invasive and potentially invasive species in the bulgarian flora. 9. a web-site  
b-site for the invasive and potentially invasive species in the bulgarian flora. project result 
15280 1  of the impact of their activity in the carbon fluxes, and metagenomic and 454 pyrosequencing t 
11601 2 ridded biomass information suitable for carbon cycle and earth system models does not exist, no 
antify the terrestrial component of the carbon cycle and its links to the water cycle, will pro 
15126 2 n the future: the use of these fungi as water quality indicators. though aquatic insects are ro 
ns that could possibly be correlated to water quality standards.  
11456 3 iño events can switch the region from a carbon sink to a source. however, we do not understand  
g the 21st century, but measurements of carbon exchange by rain forest during an el niño do not 
e of this event to make measurements of carbon exchange at multiple scales at an e. amazonian s 
14117 2 nt from the reaction of common species. protected species as especially important and vulnerabl 
rtainment of the biology and ecology of protected species in order to bring the conservation st 
15221 2                          bumblebees are insect pollinators that play a particularly important r 
is decline is a component of the global pollination crisis. in principle, global change is held 
15290 2 al landscapes. understanding hedgerow c sequestration capacity will be crucial for the c balanc 
s in hedgerows can be determined by the organic matter quality associated to the vegetation typ 
7025 8  in the transport and transformation of carbon and nutrients. while material is being transport 
es regulate the cycling and transfer of carbon and nitrogen in river ecosystems: i the mode of  
ogen in river ecosystems: i the mode of carbon and nitrogen delivery affects ecosystem function 
nts that strongly influence pathways of carbon and nitrogen cycling. these three principles can 
ics and key ecosystem processes such as carbon and nutrient retention. in this context the obje 
estigate the regulation of nitrogen and carbon cycling and transfer at the sediment/water inter 
2 /n 2 0 ratio. h2: the mode of organic carbon supply to retention areas controls denitrificati 
trols denitrification potential because carbon availability directly affects microbial nitrogen 
11670 1 ake sediments is problematic due to old carbon entering the lake from surrounding soils. we the 
10045 8 ems - or their importance as a store of carbon, as they contain 60% of all carbon found on land 
e of carbon, as they contain 60% of all carbon found on land. however, we also hear about their 
tropical forests contributes 25% of all carbon dioxide emissions by humans. many attempts have  
cosystem services like biodiversity and carbon storage that tropical forests provide, it is pos 
able to sell the resulting reduction in carbon dioxide emissions on international carbon market 
rbon dioxide emissions on international carbon markets or through bilateral agreements. this id 
ate of tropical deforestation, conserve carbon stocks and biodiversity, and alleviate poverty t 
surround how to measure and monitor the carbon or biodiversity that a project claims to protect 
15422 1                    the proliferation of invasive species is, together with habitat destruction, 
7251 6 ct aims to better simulate the flow and carbon stocks in forest ecosystems at different scales. 
 an essential component of the earth 's carbon cycle by their surfaces and their life time whic 
rfaces and their life time which allows carbon storage in plant biomass and soils. current carb 
age in plant biomass and soils. current carbon footprint models, in particular global models li 
model used by orchid ipsl, simulate the carbon balance of forests relatively simply. indeed, th 
rminants of the temporal variability of carbon fluxes across europe; * creation of a forestry m 
14612 4  to understand their role in the global carbon cycle. two major aspects of climate change are t 
plant biomass, spatial variability, and carbon stocks. furthermore, we will study soil respirat 
 to describe the processes of water and carbon balances and to predict their response to change 
iables that reflect possible changes in carbon stocks and fluxes not only erosion factors.  
11204 1 ay for the flux of plant-derived c into soil and supports specialized populations of soil micro 
10939 1                       changes in global carbon pools and changes in palaeoredox will be investi 
11297 2 nutrient and element recycling. benthic carbon mineralization represents the biogeochemical and 
d environments in estimates for coastal carbon turn over.  
201 7 , to reduce co2 emission and to balance carbon budget in the atmosphere. for inhibiting the inc 
g of co2 emission but also to extensive carbon sequestration. for this reason, during the last  
 during the last decade accumulation of carbon in different ecosystems, including forests, has  
 estimation of the potential ability of carbon accumulation of forests in various regions, howe 
growing at fertile site proceeding from carbon accumulation capacity and to provide recommendat 
ledge about the role of birch stands in carbon accumulation. research findings associated with  
d development of birch stands and their carbon sequestration potential can be considered novel  
14873 1 lity to retain nutrients and store soil carbon. results from the previous project carbopas sugg 
14874 1 lity to retain nutrients and store soil carbon. results from the previous project carbopas sugg 
10243 3 study is to follow the incorporation of carbon at the sourhope soil biodiversity field site fro 
iodiversity field site from atmospheric carbon dioxide, through the soil fauna, into soil organ 
versity interact to control the fate of carbon in the soil. the project will involve a multi-di 
11005 3 study is to follow the incorporation of carbon at the sourhope soil biodiversity field site fro 
iodiversity field site from atmospheric carbon dioxide, through the soil fauna, into soil organ 
versity interact to control the fate of carbon in the soil. the project will involve a multi-di 
11216 3 study is to follow the incorporation of carbon at the sourhope soil biodiversity field site fro 
iodiversity field site from atmospheric carbon dioxide, through the soil fauna, into soil organ 
versity interact to control the fate of carbon in the soil. the project will involve a multi-di 
15527 1 important components of the continental carbon ; and numerical modeling in order to integrate t 
15528 1 important components of the continental carbon ; and numerical modeling in order to integrate t 
14118 11         changes in climate, atmospheric carbon dioxide concentration and disturbance regimes ha 
overy from there are important regional carbon storage because carbon lost in fires has a subst 
portant regional carbon storage because carbon lost in fires has a substantial contribution to  
 a substantial contribution to regional carbon budgets. the main aim of the study is to evaluat 
to evaluate the changes in the size and quality of soil carbon and nitrogen pools after forest  
changes in the size and quality of soil carbon and nitrogen pools after forest fires. the topic 
mely since deeper understanding on soil carbon stocks and its underlying processes is urgently  
 gaps of understanding on the ecosystem carbon cycle in the changing climate. soil is the large 
e. soil is the largest stock of organic carbon, but the related processes changing soil organic 
but the related processes changing soil organic matter quality and its pool distribution are st 
ganic matter decomposition, turnover of carbon compounds of different chemical fractions, soil  
2124 10 tive plant animal interactions, such as pollination, has received considerable attention with r 
is lack of attention to consequences of plant-pollinator interactions for levels beyond the rep 
surprising. on purely pragmatic grounds pollinators conceivably play a fundamental role for pla 
 and abundance of bumblebees within the pollinator assemblage may affect the frequency of polli 
 assemblage may affect the frequency of pollination-specialised plant species, particularly ada 
species, particularly adapted to bumble bee pollination, within communities. it is conceivable, 
 with the functional composition of the pollinator assemblage. a central methodology of this pr 
eral plant species adapted to bumblebee pollination and species with a more generalist pollinat 
tion and species with a more generalist pollination to this experimentally induced change of th 
is experimentally induced change of the pollinator assemblage.  
12481 2                                         natural resource protection is one of five strategic pr 
published in march 2005 also identified natural resource protection and environmental enhanceme 
12480 1 ater resource availability, flood risk, air quality, transport and biodiversity. however, there 
14928 3 them become invasive in the new region. invasive species may monopolize local resources and out 
plain the high propagation potential of invasive species, while less attention has been paid to 
s will be tested on a list of 100 alien invasive species of the iberian peninsula, while the re 
10687 1 of continental rocks, burial of organic carbon, and changes in the flora of the oceans and cont 
2085 1  winter, and inf1uences of climatic and habitat quality on fecundity are central processes in t 
14819 1  to evaluate the interrelations between soil quality and biodiversity and its implications on t 
14273 2 e in the global biogeochemical cycle of carbon and its perturbations. there remain, however, la 
 concerning the uptake of anthropogenic carbon by the ocean, mainly due to insufficient knowled 
13749 1 r in soils under different scenarios of nitrogen sequestration, and fertilization, including n  
12309 1 mphasised the importance of arable crop disease control for climate change mitigation .  
11294 1                            the issue of carbon field experiment at the moor house national natu 
11305 1                    summary the issue of carbon field experiment at the moor house national natu 
14949 1 on changes on soil respiration and soil carbon accumulation, and relate these changes to microb 
11062 1 alia or other related artefacts. stable carbon and nitrogen isotope signals for marine foods im 
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 2 tions between biogeochemical cycling of carbon and water in semi-arid regions of the western u. 
s is that biogenic emission of reactive carbon gases from plants and soil, and wind transport o 
10818 1 nes to assess the environmental fate of crop protection products the studentship provides inter 
13465 1 cultural production through its role in plant pollination. however, it is threatened by several 
14313 1 ts on surface albedo, aerosols, and the carbon cycle. these studies concluded that the impact o 
13615 1 ural ecosystems may help to improve the biological control of nematodes in agro-ecosystems.  
9835 1 ich there are established links between habitat quality and demography, as a model system with  
13785 3  proposed here, i will study host plant-pollinator-parasitoid interactions under different clim 
bitat change scenarios. i will focus on pollinating insects with well known ecology i.e. large  
 generality in the study systems. using pollinating insects in an ecological and evolutionary f 
1105 10 ficient systems for the storage of soil carbon in widespread agro-forestal systems in central a 
nsular italian mediterranean areas. the carbon balance will be studied following the dynamics o 
namics of the processes involved in the carbon cycle that carry out and control the carbon cycl 
on cycle that carry out and control the carbon cycle. a simulation model of the carbon cycle wi 
carbon cycle. a simulation model of the carbon cycle will be set up simultaneously in order to  
e selected agro-forestal systems on the carbon sink. new climatic scenarios, predicted by globa 
n the diversity of microorganism and on carbon dynamic and in the carbon cycle models, in order 
ganism and on carbon dynamic and in the carbon cycle models, in order to compare the data obtai 
e greenhouse effect via the increase in carbon storage for territorial planners and agricultura 
ctional diversity of microorganisms; 4. carbon sink and biogeochemical cycles.  
2000 7 ificant long-term sinks for atmospheric carbon dioxide. climatic change could bring about chang 
have important repercussions for global carbon cycling. experiments that have been carried out  
ve of the history of the vegetation and carbon sequestration. based on the sequence of plant re 
 vascular plant species composition and carbon sequestration in bogs;· to determine the long-te 
lar activity on species composition and carbon accumulation;· to analyse the relation between t 
elation between species composition and carbon sequestration;· to investigate the long-term eff 
change on plant species composition and carbon sequestration in bogs using a simulation model.  
12592 1 il processes and functioning, including carbon and nutrient cycling, soil structural dynamics,  
11758 2 lating the concentration of atmospheric carbon dioxide . in such environments, small changes in 
ironments, small changes in whole plant carbon balances may have important consequences for see 
9996 2 lating the concentration of atmospheric carbon dioxide . in such environments, small changes in 
ironments, small changes in whole plant carbon balances may have important consequences for see 
13587 1 project will be of great importance for water quality management in the face of climate change. 
1997 1 es national key-players in the field of water quality and water management. the anticipated res 
11439 3 seley linked to how we alter the global carbon cycle. the rate at which we are using fossil fue 
ering land use ; however, if we get the carbon cycle slightly out of balance the plants and ani 
, etc. are. exactly how delicate is the carbon cycle within a closed system the work we are pro 
12588 7 current literature on the state of soil carbon levels in uk soils is equivocal. predictions of  
. predictions of future changes in soil carbon levels related to land use and climate change ar 
ted the need to collate uk data on soil carbon and the release of greenhouse gases in relation  
 gained of the current state of uk soil carbon and the processes driving change, and inform mod 
ility and provenance of data on uk soil carbon stocks, fluxes and land use influences. 2. appra 
oject will be a brief review of uk soil carbon data sources and shortfalls in these data. this  
ce to policy makers in relation to soil carbon and land management. tasks for a second phase of 
10137 4  ions in the ocean, a form of dissolved carbon that is depleted in the acidification reaction w 
etter understanding of the modern ocean carbon cycle, which is essential to get right before wo 
ons about the range of changes in ocean carbon and nutrient cycles we can expect in the future  
g more or less greenhouse gases such as carbon dioxide and nitrous oxide.  
11019 4  ions in the ocean, a form of dissolved carbon that is depleted in the acidification reaction w 
etter understanding of the modern ocean carbon cycle, which is essential to get right before wo 
ons about the range of changes in ocean carbon and nutrient cycles we can expect in the future  
g more or less greenhouse gases such as carbon dioxide and nitrous oxide.  
14318 1  forest management actions that enhance carbon storage in forests, offering incentives for deve 
15339 11 n the detection of resources by diurnal pollinators. the anatomy of the eye, the nature of the  
ity of the visual system differ between insect pollinator groups. this suggests that each insec 
the visual system differ between insect pollinator groups. this suggests that each insect group 
 for the ecology and evolution of plant-pollinator networks. this is because the ability of pol 
etworks. this is because the ability of pollinators to detect different flowers affects their r 
d allow flowers some control over their pollinators. because the only insect pollinator for whi 
ver their pollinators. because the only insect pollinator for which the visual system has been  
 differences in perceptual abilities of pollinators can lead to resource partitioning. this inf 
ial to determine under which conditions pollinators will be able to detect flowers of different 
s can advertise their reward to certain pollinators while remaining relatively inconspicuous to 
ining relatively inconspicuous to other pollinator groups.  
14898 1 at ecological importance as herbivores, pollinators and food for insectivores. moreover, due to 
11119 1  plants use chemical signals to promote pollination, seed dispersal, and protection from herbiv 
9936 3        at present it is unclear whether carbon-flow pathways to ch4 in freshwater and marine sy 
archaeal lipids, to ecosystem function. carbon-flow pathways to ch4 in freshwater, marine and e 
xy model that is commonly used to study carbon-flow pathways in freshwater and marine environme 
10701 3        at present it is unclear whether carbon-flow pathways to ch4 in freshwater and marine sy 
archaeal lipids, to ecosystem function. carbon-flow pathways to ch4 in freshwater, marine and e 
xy model that is commonly used to study carbon-flow pathways in freshwater and marine environme 
7662 1 he zebra mussel. the zebra mussel is an invasive species widely distributed in temperate aquati 
12617 12 ween climate change and the terrestrial carbon cycle is one of the main uncertainties in predic 
dictions of future climate change. soil carbon dynamics are a key element of this because soils 
ontain two or three times the amount of carbon as in vegetation or the atmosphere. in 2005 cran 
f england and wales for changes in soil carbon during the 1980s and 90s. this showed gains in c 
the 1980s and 90s. this showed gains in carbon in some soils, but large losses in others and ov 
tever the reasons, such a large loss of carbon from soils has serious implications for the glob 
has serious implications for the global carbon cycle, for the possibility of sequestering carbo 
le, for the possibility of sequestering carbon in soils, and for the ability of soils to perfor 
hese fail to detect the changes in soil carbon observed in the nsi. the reaons for the differen 
tain about 2 thousand million tonnes of carbon, detecting a change of even 4 million tonnes is  
nd ceh. given that our datasets on soil carbon in england and wales are among the most comprehe 
e results will inform the debate around soil protection for other environmental and agricultura 
12685 1 ent of the level of compliance with the environmental protection , and a review of other applic 
11302 1 mplete picture of internal and external energy storage and transfer during arboreal bipedality. 
11309 1 mplete picture of internal and external energy storage and transfer during arboreal bipedality. 
11831 1 mplete picture of internal and external energy storage and transfer during arboreal bipedality. 
7490 3 elivering food, fibre and bio-fuels and carbon storage. however, the demand is greater than the 
iversity on stability and resilience of carbon, nitrogen and phosphorus cycling, as well as ass 
 consequences for outbreaks of pests or invasive species. soilservice will link ecological and  
13879 3    wild bees are important providers of pollination services to agriculture and should be a foc 
ation may contribute to the decrease in pollinator populations both by reducing the general ava 
sures to maintain viable populations of bee pollinators in agricultural landscapes.  
6959 1 een shown to provide protection against invasive species. the aim of this project is the evalua 
11070 1 totrophic respiration; i.e. the flux of carbon occurring directly from plant roots and indirect 
10404 12 tems perform, such as the rate at which carbon is recycled or stored. but biodiversity has many 
s the key factor in regulating rates of carbon turnover. however, a largely ignored component o 
trated that key plant traits related to carbon cycling are highly variable within species. thes 
s potentially important consequences on carbon turnover. this project therefore seeks to discov 
h plant intraspecific diversity affects carbon turnover in species-rich limestone grassland. mo 
t occurs in nature. we will measure the carbon content of soil in a number of important physica 
rtant physical fractions and release of carbon as co2 from the soil surface. in addition, we wi 
 - a natural and easily distinguishable carbon isotope - to enable us to quantify the amount of 
 to enable us to quantify the amount of carbon that plants allocate to soils. this will enable  
ng of how genotypic diversity regulates carbon turnover. the data will be analysed alongside th 
f intraspecific diversity in regulating carbon turnover. the work will further our understandin 
 of biodiversity that are important for carbon turnover, and the soil factors that may regulate 
7414 1 eral decades, a significant decrease in pollinating insects is observed. the honeybee is partic 
15224 1 gical groups that are a useful tool for mosquito control technicians.  
11144 1  such as fish stocks or failure to curb carbon emissions are obvious examples. an extensive the 
12598 1 of peat extraction for biodiversity and carbon storage. peat use in soil improver materials has 
12667 1  component of the evidence base for the natural resource protection programme and supports poli 
7195 1 tion of habitat loss and degradation of habitat quality. the interactions between types and int 
15522 5                           estimation of carbon pools and net primary production at a higher spa 
e, land cover changes and management on carbon stocks and net primary production of vegetation  
ake it very suitable for characterizing carbon patterns of vegetation: large climatic and topog 
management have a synergistic effect on carbon stocks and net primary production of terrestrial 
s in peninsular spain, with a declining carbon stock due to reduced water availability owed to  
15056 1 s with different characteristics and/or water quality. our previous studies on cyanobacterial d 
10302 1  furthermore, radiocarbon can only date carbon based pigments, and the majority of early rock p 
13788 1 gal decay rates. this has relevance for carbon dynamics in managed boreal forests, and may incr 
7302 1 ve strongly suffered from the impact of invasive species. this project, which includes the cons 
12637 2                                         soil protection is of strategic importance for protecti 
o provide evidence on which to base its soil protection strategy. given defras aim of developin 
11113 1 estigating benthic-pelagic coupling and carbon fluxes in both temperate and tropical coastal sy 
11328 1 tions . it also has strong relevance to water quality monitoring in freshwater environments, wh 
11594 1 tions . it also has strong relevance to water quality monitoring in freshwater environments, wh 
12586 2 ngoing which are raising the profile of soil protection and use. with this greater consideratio 
evelopment and implementation of future soil and environmental policy by providing evidence on  
12770 3                                european protected species are strictly protected because of con 
fe legislation. in the case of european protected species, licences are issued in pursuance of  
measures and good practice for european protected species affected by roads. e. improving mitig 
15128 1 ructure and composition of the two-mode plant-pollinator network in different fragments of high 
12762 1 t they are an essential tool needed for pest control. previous investigations into snare use .  
11779 3 functions such as the mineralization of carbon. such knowledge is essential to improving our un 
 future use of biological indicators of soil quality. recently it has been shown that ph is the 
rial composition/diversity, and measure carbon mineralization rates to determine whether commun 
10770 3 e between the deep oceanic reservoir of carbon and the atmosphere. the balance between the co2  
dictates the content in the atmospheric carbon dioxide, which has implication on the climate on 
are responsible for a large part of the carbon drawdown to the seafloor. these micro-organisms  
10420 1 on summary for the linked proposals the carbon isotopes in protein that survives in archaeologi 
11389 1                                     the carbon isotopes in protein that survives in archaeologi 
12528 1 cales of the epidemic so as to optimise disease control and management • how do intervention st 
12551 1 agriculture and the environment through pollination: they also produce honey and wax . attracta 
11118 1 ces of the stable isotopes of hydrogen, carbon, nitrogen and oxygen of individual compounds can 
11134 1 ource pollution on river, estuarine and coastal water quality and particularly with regard to n 
14600 1 aking process related to: need to adopt sediment quality remediation measures in harbours and w 
14330 1 so above-ground biomass and underground carbon measurements.the insights obtained in this proje 
6960 1 urvey, 4. maize pistil faunula test, 5. pollinator distribution, 6. resistance to invasive weed 
7678 1  and bacteria, include plant pathogens, bio-control agents of plant pests and diseases, and org 
10006 1 s that provide advice and licensing for protected species; local authorities responsible for pl 
11536 1 s that provide advice and licensing for protected species; local authorities responsible for pl 
7702 1 t of more intensive production and high environmental quality is a challenge, involving at once 
1962 1 ral ecosystems and the compatibility of pest control strategies.  
10474 1 uction of oxygen and the consumption of carbon dioxide approach specifically targeted at the pp 
9905 1 uction of oxygen and the consumption of carbon dioxide approach specifically targeted at the pp 
9807 5 a bright advertisement to attract these pollinating animals. the majority of plant species prod 
n to make the petals more attractive to pollinators. it is not surprising, then, that most peta 
sult in increased seed set because more pollinating bees visit the flowers, when compared to mu 
ant families which have shown shifts in pollinators, and investigate whether there is any relat 
of the co-evolution of plants and their pollinators during their evolutionary history.  
2479 2 nked among the world's most detrimental invasive species, was first observed in northern europe 
succession in pelagic ecosystems due to invasive species and/or increased numbers of gelatinous 
2480 1  also have a major impact on the global carbon balance and on climate forcing, and toxins may c 
10182 1  that there are fast and slow routes of carbon transfer into the higher trophic levels. a manip 
9919 2 research involving all life stages, and biocontrol. the potential for automation of dna data ac 
ther insects and therefore are used for biocontrol, to demonstrate the principles of a combined 
11874 1 ooking in detail at competition between soil and plants for organic and inorganic nitrogen. ult 
10255 2  this change by sequestering additional carbon. key to our understanding and evaluation of thes 
nd store up to one-third of global soil carbon reserves. their stability under future atmospher 
11464 2 e community structure e.g. reduction in water quality due to pollution. we will use our model t 
to test whether lake trophic status and water quality are linked to the species abundance distr 
11799 2 e community structure e.g. reduction in water quality due to pollution. we will use our model t 
to test whether lake trophic status and water quality are linked to the species abundance distr 
10189 1 e introducing natural enemies can be an effective biological control strategy. because mutualis 
11335 1 his project is to develop a sustainable biological control system for vine weevil .  
10817 1 changes in the herbivore s food plants. food quality is not thought to respond to herbivory in  
11049 1 changes in the herbivore s food plants. food quality is not thought to respond to herbivory in  
11562 1 changes in the herbivore s food plants. food quality is not thought to respond to herbivory in  
11829 1 changes in the herbivore s food plants. food quality is not thought to respond to herbivory in  
11441 1 he degree of utilisation of new and old carbon in soils and peats by the microbial biomass to b 
10211 1 that regulate it are poorly understood. carbon fungi are a dominant group of microorganisms tha 
13790 1 tent and growth rate can be affected by food quality and that fast growing species have higher  
11870 1  hold wider-reach training workshops in carbon cycle science in each country at the start and e 
2169 3 r threats in the near future. these are invasive species. the project focuses on terrestrial ve 
ces for ecosystem services, focusing on pollination. for this purpose we have assembled a resea 
ts in palaeoecology, community ecology, pollination, forest ecology, cultural-landscape ecology 
10693 1 phytoplankton play a role in the global carbon cycle, which is of great importance for global w 
7553 1  also include a study of the biology of pollination. agricultural practices and their impact on 
14199 1 i, present both as viable spores in the soil and functioning hyphae in plant roots is the estab 
7261 1 ation process in the mediterranean this invasive species complex. for this we will develop a ne 
14319 1 greatly depend on the amount of organic carbon transiting through the microbial food web, known 
11723 2  of fish. stable isotopes of oxygen and carbon deposited in otolith cores and peripheries will  
or confounding effects of metabolism on carbon isotope balances.  
15530 1 resistance and resilience functions and carbon sequestration potential in dry-subhumid mediterr 
12040 1 liable early warning systems for marine invasive species.  
519 1 development of territorial policies for protection of biodiversity and the ecological assets. e 
7182 1 h frequency, the very important role of pollinators, dissemination fruit / seeds of mammals - a 
10152 1 ory birds requires a system in which 1. habitat quality has been identified, 2. changes in rang 
11496 1 ory birds requires a system in which 1. habitat quality has been identified, 2. changes in rang 
13466 1  scale natural fires in modern times on soil and water chemistry as well as on biodiversity and 
7635 1 pir ecological engineering products and quality of water. moreover, the"heavy metals"are among  
15205 2  distinct and frequent floral visitors, pollinators and nectar robbers, in the variation of flo 
sure opposite to the one exerted by the pollinators over the floral traits.  
9859 1                                         invasive species are a major threat to global biodivers 
12346 1  accrue from using dredged material for coastal protection and habitat conservation and will en 
7688 1 ich is characterized by its role in the biological regulation department. these approaches allo 
7603 1 ich the Alps mountains, the Protocol on Soil Protection to the Alpine Convention is a good stat 
7632 1  a changing world. habitat destruction, invasive species and climate change are the most import 
15318 5 core participants. in the case of plant-pollinator systems, pollination success is not determin 
n the case of plant-pollinator systems, pollination success is not determined by the interactio 
t determined by the interaction between plants and pollinators alone, but also by the direct an 
tion frequency and foraging behavior of animal pollinators, as well as aspects related to the p 
l-pollinated plants, including maternal pollination success, fruit set, seed size, outcrossing  
15209 1 e effect of game management, especially predator control, on the composition of carnivore commu 
7198 1 soil conservation and biodiversity, and carbon storage, without however, that the scope of thes 
15294 1 etermine the concentration of metals in soil and assess your risk, carries a high budget for so 
15295 1 iques to evaluate relationships between soil and edaphic fauna in contaminated areas  
14770 3 nsidering the fast deterioration of the water quality of the andean rivers and the scarce water 
 ecological status, developed under the regulation of water framework directive of the european 
 agencies to improve and increase their water quality control and management of the andean wate 
214 1 ce via host specificity and/or positive soil and litter feedback. through field expeditions and 
14124 1 evitable part of activities, focused on biodiversity protection. the results from our previous  
15033 1 with current trends of climatic change, invasive species are predicted to become more numerous  
14988 1  problems fishes are vectors of organic carbon transport between algal assemblages and seagrass 
14989 1  problems fishes are vectors of organic carbon transport between algal assemblages and seagrass 
11402 4 d to provide ecosystem services such as carbon storage and protection of water quality, along w 
tem services such as carbon storage and protection of water quality, along with biodiversity co 
unctional diversity, and its impacts on carbon and nitrogen turnover. vital aims to address thi 
s that respond to management and affect carbon and nitrogen turnover. wp3 will then build multi 
481 1 s that respond to management and affect carbon and nitrogen turnover. wp3 will then build multi 
7629 2  exotic floral species in the ecosystem service of pollination urban. the results obtained and  
pose measures to preserve the ecosystem service of pollination in urban and non-urban areas. th 
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 
2068 5 examines how plant species interact for pollination through pollinator attraction and heterospe 
pecies interact for pollination through pollinator attraction and heterospesific pollination. m 
ollinator attraction and heterospesific pollination. moreover the effects of such interaction f 
experiment where the composition of the pollinator fauna is altered is conducted to examine if  
 conducted to examine if a shift in the pollinator fauna will have impacts on the plant species 
2002 2 etween sphagnum species and the rate of carbon sequestration. the project will focus on four si 
position and the accumulated amounts of carbon will be measured. experiments will be performed  
14920 5 xerts a major influence on soil organic carbon content and, consequently, there is increasing c 
g concern over the feedback response of carbon-rich soils to increasing global atmospheric temp 
ures have been offsetting absorption of carbon by these terrestrial sinks resulting in the stim 
ed release of co2 and dissolved organic carbon describing the possible mechanisms involved and  
ch would allow to link biodiversity and carbon cycle. these three aims will provide a better un 
2139 1 tter and soil organic matter as energy, carbon and nutrient sources for biomass production and  
10526 1 ses in the concentration of atmospheric carbon dioxide , one of the centres of excellence for m 
2005 1 inities via the quality and quantity of carbon source inputs into the system. fot rerestrial ec 
13967 6 ffects of fragmentation and invasion on pollination service to forbs in marginal grassland habi 
ield experiments, focal observations of pollinator behavior and monitoring of pollinator abunda 
f pollinator behavior and monitoring of pollinator abundance. pollination service will be estim 
and monitoring of pollinator abundance. pollination service will be estimated in large continuo 
ad-verges, will be studied by comparing pollination success in experimentally invaded and non-i 
invaded and non-invaded sites. decay in pollination service will be indicated by increased poll 
15245 4  loss, fragmentation and restoration on plant and pollinator communities and on interactions be 
dered to be one of the major drivers of pollinator diversity loss, but the processes through wh 
ded in relation to species persistence. plant-pollinator interactions will also be surveyed to  
ndscape change on the topology of plant-pollinator networks.  
13830 1 roject is to evaluate the importance of habitat quality and quantity for the recruitment potent 
12177 1 ervation, stock management, shelter and erosion control. the hedgerow network may also play an  
14741 1  river has recently suffered changes in water quality, trophic structure and composition of the 
14184 3 mpt to avoid usage of harmful synthetic plant protection products. pest management by any plant 
ection products. pest management by any plant protection product is costly, which is why it is  
fic grounds for the pesticides using in plant protection.  
13488 2 lant community composition, dynamics of carbon and nitrogen and the regeneration and survival o 
 combined with mathematical modeling of carbon and nitrogen dynamics. results from these theore 
1088 2 ion in recent years. several studies on carbon cycling and decomposition have been done on sing 
these processes by climatic conditions, litter quality, decomposers, soil factors, pollution an 
15446 1 tion, by its repercussion on the global carbon cycle, as warming can enhance decomposition rate 
15385 1 ute to determine the characteristics of carbon global cycle. competitive equilibria between eve 
11869 1 uction of oxygen and the consumption of carbon dioxide by very small, single celled organisms,  
11393 3  through examination of changes in soil hydrology and water quality. 2. provide a better unders 
fluence of changes in stream hydrology, water quality and sediment fluxes on stream ecosystems  
ive of peat hydrology, chemistry, river water quantity and quality, and stream ecosystems, thus 
10597 2  of considerable microbial diversity in soil and the existence of many groups with no cultivate 
enous microorganisms will use this as a carbon substrate and break down this material. we can t 
14655 1 ect aims to study the variations in the energy storage levels of aquatic insects living under d 
10661 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
10912 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
11158 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
11170 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
11420 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
11421 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
11701 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
11702 1 tion of nutrients, and water supply and water quality, the creation of opportunities for recrea 
9896 1 gulation of nutrients, water supply and water quality, the creation of opportunities for recrea 
12305 2 hange and, specifically, the release of carbon from cropping of high carbon stock soils. althou 
release of carbon from cropping of high carbon stock soils. although co-products currently used 
11161 1              summary global atmospheric carbon dioxide levels .  
11853 3 ces in food availability that depend on habitat quality. traits closely related to fitness, suc 
less discriminatory. i will look at how local habitat quality influences sexual selection using 
ifferent mates before choosing how does habitat quality influence a male s likelihood of gainin 
7701 3 omies is very important. . energy flow, carbon and nitrogen can provide interesting indicators  
development. by focusing on the flow of carbon and energy in livestock farming of ruminants and 
ation models of the emission of ges and carbon stock and 3 - stream nitrogen, to develop energy 
7037 1 of environmental matters such as water, soil and infrastructure, the environmental history data 
14971 1 al conditions. objetive 3: to model the carbon balance of beech seedlings in response to hydric 
10945 1  the relative importance of abiotic and biotic control of prey defences.  
10592 2 e monooxygenase is important in cycling carbon in environments where there are high concentrati 
nooxygenases, key enzymes in the global carbon cycle.  
7306 2 o manager of the aggregate structure of soil and its cultivability. moreover, globally, the dec 
moreover, globally, the decline in soil carbon stocks is likely to accelerate global warming. - 
12536 1 ems. the aim of any non-native invasive weed control programme should be eradication. for this  
14375 4 dous value, e.g. water purification and carbon sequestration. in 1997, the work by defined the  
s are required, particularly concerning regulating services. two key challenges of ecosystem se 
osystem services primary production and climate regulation, more specifically: carbon sequestra 
 climate regulation, more specifically: carbon sequestration in ecosystems  
11399 3 ime, to understand the development of a carbon cycle in newly formed rocks and the early proces 
olcanic rocks, which account for 30% of carbon dioxide drawdown from the atmosphere each year t 
ce of events for the establishment of a carbon cycle and active microbial communities on volcan 
7246 1 ity and quality of wastewater and storm water quality of natural areas will be shared. from sit 
9875 1 nt ecosystem services, including higher pollinator abundance and cleaner waterways. many studie 
6894 3 ing environmentally friendly integrated plant protection methods and introducing them into ever 
y focused to the most important current plant protection problems of hungary. thus, top priorit 
ut the project environmentally friendly plant protection methods are favoured, such as resistan 
2516 2                                     one-carbon compounds such as methane and methanol are attra 
l are attractive, non-food and low-cost carbon and energy sources for microbial bioprocesses, w 
10354 5  will continue to rise, and atmospheric carbon dioxide concentrations will reach levels unprece 
ill surviving tropical forests remain a carbon sink - currently equivalent to ~15% of global ca 
 currently equivalent to ~15% of global carbon dioxide emissions from fossil fuel use - or will 
nd other changes cause them to become a carbon source with the potential to increase the rate a 
nd where changes in the composition and carbon balance of tropical forests are occurring will p 
10336 1 ed, the reefs are important not only in coastal protection but also in promotion of tourism. no 
10358 2 tion of pesticides, the introduction of biocontrol agents, or by artificially inducing the plan 
the need for use of pesticides or other biocontrol agents. current data indicate this method pr 
15158 2 variability reflects adaptation through pollinators, there is increasing evidence that other fa 
out the importance of selection through pollinators as opposed to other factors in the evolutio 
13752 1 as broad-scale processes such as global carbon cycles.  
14776 4  to increase interactions with the most efficient pollinators, and is expressed both at the mic 
pe by quantifying the selective role of pollinators, and determine the spatial variation in sel 
ios provoked by a concomitant change in pollinator fauna. second, we will explore the effect of 
 will explore the effect of a change in pollinator fauna and the potential for selective diverg 
15170 3 the origin and evolution of specialized pollination systems constitutes a major paradigm in pla 
igm in plant ecology. among specialized pollination interactions, nursery pollination systems a 
lized pollination interactions, nursery pollination systems as selective agents of flower trait 
14867 1 rstand these introgressive processes in invasive species and its putative role in speciation. e 
13323 1 dopted by the ministerial conference on protection of forests in europe.  
7716 1 aken into account in the legislation on soil protection, research in agronomy and plant breedin 
12767 1 ment is placing increasing pressures on protected species and their habitats in the uk. when a  
11258 1 rk will be supplemented with studies of carbon and sulphur isotopes from the limestones which w 
11391 1 rk will be supplemented with studies of carbon and sulphur isotopes from the limestones which w 
15401 1  the final goal is therefore to improve environmental quality by reaching lower bioremediation  
10203 1 house gas, second in importance only to carbon dioxide. most methane is produced by microorgani 
2107 2 ve also shown that kelp is an important carbon source for many animals in these areas. however, 
tly on the kelp plants which means that carbon from kelp mainly enters food webs through pom .  
12196 2 ture, reduced soil erosion and run-off, enhanced pollinator services and increased resilience o 
uced soil erosion and run-off, enhanced pollinator services and increased resilience of biodive 
7301 1 ite the importance of this scenario for pollinator conservation and the introduction of parasit 
10958 1 ian/cenomanian oaeld. stable oxygen and carbon isotope analyses on individual species will prov 
10294 3  bacteria which grow on methane as sole carbon source have been obtained from many environments 
hs which grow on both methane and multi-carbon compounds such as acetate now make it imperative 
 methane cycle. we propose to study the environmental regulation of methane oxidation in a mode 
12511 2                                         soil quality is an important consideration for the succ 
ainable farming systems. traditionally, soil quality has been assessed primarily on physical an 
15577 2 by providing ecosystem services such as crop pollination and biological control of crop pests.  
m services such as crop pollination and biological control of crop pests. in many regions farm  
12600 3  compact and impermeable. any damage to soil quality affects the long-term functioning of the s 
gical diversity and the performance and visual quality of the vegetated areas but can have impa 
ch as on flooding, aquifer recharge and water quality. the first soil action plan for england,  
12217 2 feasibility study into the potential of crop pollinators to act as delivery agents of entomopat 
entomopathogenic fungi for invertebrate pest control  
13769 1 ms to assess feeding characteristics of invasive species and to find out if species with wide f 
14303 1 broadleaved forests on biodiversity and environmental quality, study of the attitude of forest  
215 1 e role of fine roots in ecosystem-level carbon and nutrient cycling. the determination, in spuc 
11327 3 jor component of the marine-atmospheric carbon cycle is the precipitation and dissolution of ca 
tant to our understanding of the global carbon cycle, and to the earth system as a whole. this  
r understanding of the marine inorganic carbon budget. large amounts of calcium carbonate are p 
15585 1 ve effects on biodiversity by hindering invasive species dispersal and providing refuges in iso 
15447 2 ers offer nectar as the main reward for pollinators. numerous studies indicate that the nectar  
is independent of the commonest type of pollinator on its flowers .  
10705 1 lling of the effects of biodiversity on carbon fluxes.  
15177 1 ry context, if the preferences shown by pollinators and herbivores are likely to affect the mai 
9990 1 for making high quality measurements of carbon dioxide .  
12329 2 n because the impact of many options on water quality depends on their location. this proposal  
 estimating the impact of els uptake on water quality.  
13604 1 webs and are crucial for the cycling of carbon and nutrients. microbial populations are control 
14828 3 en postulated as the main mechanisms of population regulation for territorial birds. combined u 
under the traditional density-dependent population regulation theory, these scenarios predict t 
 hunter-killed ungulate availability in population regulation of the golden eagle and to discus 
210 9      general and widespread shortage of pollinator abundance and diversity in agricultural land 
ope gives cause for alarm. reduction of pollination service threatens not only the quantity and 
 in regulating the species richness and abundance of pollinators in these habitats. the aims of 
egies to protect both wild and domestic pollinators and help develop more effective agri-enviro 
nvironment schemes that aim to conserve pollinators. provision of adequate pollination services 
erve pollinators. provision of adequate pollination services will help achieve more reliable cr 
e more reliable crop yields from insect-pollinated crops as well as sustain populations of nati 
ulations of native flora, which in turn benefit pollinator populations.  
 of native flora, which in turn benefit pollinator populations.  
11877 1 nd quantification of the risk of forest carbon loss, and investor s confidence in forest invest 
13464 1 nt nutrients to their tree hosts and to sequestration of carbon. however the biodiversity of th 
13459 1  catchments and minimize its affects on water quality and planktonic biostructure in boreal lak 
10009 1  erosion and flooding, and degraded the water quality and biodiversity of streams. whilst much  
14603 1 tween dissolved and particulate organic carbon has ecological sense because poc goes down by gr 
11115 1 those charged with a responsibility for environmental protection. funding, totalling £114,293,  
11592 2 processes such as forest growth and the carbon cycle. traditional direct measurements of import 
er interpretation of data obtained from carbon flux measurement towers. knowledge gained from t 
10263 2 ponsible for 25% of primary fixation of carbon dioxide, which is as much as all tropical rain f 
 are virtually the sole source of fixed carbon for higher trophical levels in ice-covered water 
1945 5 gens and increase the need for chemical crop protection. eu-legislation stimulates plant-specie 
hey improve both above- and belowground crop protection. the aim of the present proposal is to  
 agricultural biodiversity measures for crop protection against above- and belowground pests an 
ta-analysis of postdoc 1 in relation to crop protection. with plant research international, end 
asibility of enhanced above-belowground crop protection by agricultural soil biodiversity measu 
7020 2 to humans, such as food production, the maintenance of water quality and soil fertility, carbon 
ce of water quality and soil fertility, carbon storage, the mitigation of the effects of greenh 
7135 1 ased on their biology and their rate of carbon and nitrogen compounds will be related to those  
14573 1 ication of the phenotypic plasticity of invasive species. the work plan of objective 1 includes 
11079 8 ly, forests contain a vast reservoir of carbon, approximately 30% of that in the biosphere, muc 
is balance is crucial for understanding carbon cycling, and for predicting carbon cycle respons 
ding carbon cycling, and for predicting carbon cycle responses to global climate changes. recyc 
cetes. thus, these fungi are central to carbon and nutrient cycling, and yet we still have rela 
te these dynamics into global models of carbon cycling. the majority of decay takes place in fa 
ect on the rates of wood decay and thus carbon cycling. we have a general understanding of fact 
ies affect decay rate, provide data for carbon cycling models, and possibly form the basis for  
tions of fungal communities to optimise carbon cycling.  
10832 6 ualistic relationship with their hosts, protecting plants against attack through their chemical 
t resources then they might compete for carbon in the plant, thereby reducing the growth of the 
uld lead to many novel forms of pest or weed control. if at least some of the chemicals in plan 
ons for the use of endophytes as insect biological control agents. we could inoculate the fungi 
s to use insects or pathogenic fungi as biological control agents of it have failed. we think t 
o manipulate fungal occurrence, so that biological control agents stand a better chance of succ 
10187 1 against parasites they could be used in biological control of plant disease.  
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 
10651 1 environment. this may guide tactics for pest control in a changing climate, and may even sugges 
7437 1 nce of the habitat to the dispersion of pollinators. assistance requested focuses on the recrui 
15305 1                                      as invasive species spread through a new environment they  
10704 1 sed in three environments which vary in food quality. it is possible that the environmental var 
11414 1 sed in three environments which vary in food quality. it is possible that the environmental var 
14781 1 l in the establishment and expansion of invasive species.  
220 1 iable than the restricted, annual, self-pollinating species. however, many exceptions, where ra 
2111 1  a sustainable context is how to ensure environmental protection and at the same time achieve e 
15183 1              freshwater colonization by invasive species has huge ecologic and economic consequ 
10286 6 re kilometres - and store about as much carbon as do the living plants in tropical rainforests. 
ts living on peatlands have been fixing carbon dioxide from the atmosphere and storing it as de 
nd possibly drier, climate, this stored carbon could be respired back to the atmosphere or leac 
fall lead to rapid loss of the peatland carbon store if so, then the extra carbon released from 
land carbon store if so, then the extra carbon released from peatlands could enhance greenhouse 
ill help us to predict how the peatland carbon store will fare in the face of future climate ch 
10539 6 re kilometres - and store about as much carbon as do the living plants in tropical rainforests. 
ts living on peatlands have been fixing carbon dioxide from the atmosphere and storing it as de 
nd possibly drier, climate, this stored carbon could be respired back to the atmosphere or leac 
fall lead to rapid loss of the peatland carbon store if so, then the extra carbon released from 
land carbon store if so, then the extra carbon released from peatlands could enhance greenhouse 
ill help us to predict how the peatland carbon store will fare in the face of future climate ch 
11043 6 re kilometres - and store about as much carbon as do the living plants in tropical rainforests. 
ts living on peatlands have been fixing carbon dioxide from the atmosphere and storing it as de 
nd possibly drier, climate, this stored carbon could be respired back to the atmosphere or leac 
fall lead to rapid loss of the peatland carbon store if so, then the extra carbon released from 
land carbon store if so, then the extra carbon released from peatlands could enhance greenhouse 
ill help us to predict how the peatland carbon store will fare in the face of future climate ch 
15416 2 re with implications for the cycling of carbon and nitrogen of ecosystems. during the last 3 de 
reen vs deciduous species and native vs invasive species.  
9950 1 anges in the atmosphere, such as rising carbon dioxide concentrations , and the climatic change 
11405 1 processes of pathogen interactions with soil and water; catchment risk assessment; water resour 
11584 1 processes of pathogen interactions with soil and water; catchment risk assessment; water resour 
12623 11 s hold the uk`s largest single store of carbon. in good condition, they can contribute to attem 
 addition, peatlands `leak` some of the carbon they hold into the rivers that drain them, as di 
s that drain them, as dissolved organic carbon , the amount of carbon released can increase if  
issolved organic carbon , the amount of carbon released can increase if peatlands become unstab 
t present, we do not know where all the carbon transported from peatlands into rivers goes. if  
s or coastal waters, this relocation of carbon from one secure store to another will not affect 
stablishing how much of the total river carbon flux is converted into greenhouse gases, we hope 
. to determine the fate of the riverine carbon released from peatlands, we will study how the d 
 study how the different forms of river carbon are processed at a range of critical locations w 
inking water treatment works where this carbon is removed by a variety of methods. the approach 
at proportion of each of these forms of carbon is ultimately emitted to the atmosphere as green 
7311 2 ling of physical phenomena of concern - carbon cycle and climate - also agrees satisfactorily w 
ic balance of short-term. it may be the carbon cycle, the whole climate system, a technical mod 
12706 1  of brown filed sites, with emphasis on protecting biodiversity, recognising the priority habit 
2186 2 lf-sustained there. the presence in low quality habitat can be the overflow of individuals prod 
so contribute to the development of the environmental quality objective healthy forest. the pro 
13602 2 on plant and insect communities, and on pollination which is an important ecosystem function pr 
 stressors such as land use conversion, invasive species and climate change.  
15139 2 us to take into consideration that most invasive species are not in equilibrium with the enviro 
will alos generate distribution maps of invasive species for current conditions but also for fu 
13325 1  genetic resources, global relevance to carbon cycling and possible susceptibility to global ch 
10270 6 nds offer vital ecosystem services from carbon storage, biodiversity, water provision, flood pr 
storage, biodiversity, water provision, flood protection, aesthetic/recreational value, to econ 
overnment psa targets for biodiversity, soil and water protection in uplands. restoration is of 
 psa targets for biodiversity, soil and water protection in uplands. restoration is of crucial  
f crucial importance to protect uk soil carbon stores, as more than 50% of uk soil carbon is st 
bon stores, as more than 50% of uk soil carbon is stored in peat and is rapidly lost. restorati 
15004 1 of the trophic line that influences the biological control of aphids and psyllids that can beco 
11132 1 or transfer of semiochemicals into bulk soil and to neighbouring plants uninfected by aphids, a 
12255 3 lved in soil biogeochemical cycling and carbon flow and because methods for assessing their pop 
, particularly nutrient loss, and hence water quality. the extent to which soil properties and  
il microbes as generic bioindicators of soil quality, and the extent to which geography should  
10965 4                             rhizosphere carbon flow is central to the functioning of grassland  
nship between the processes involved in carbon flow and the diversity, community structure and  
this project aims to assess rhizosphere carbon flow following input of a 13c pulse and simultan 
sity will determine whether rhizosphere carbon flow drives diversity.  
10911 3 tes use light for energy but cannot use carbon dioxide as their sole carbon source and conseque 
cannot use carbon dioxide as their sole carbon source and consequently use organic molecules fr 
s from the environment to satisfy their carbon requirements. despite considerable advances in t 
10980 3 tes use light for energy but cannot use carbon dioxide as their sole carbon source and conseque 
cannot use carbon dioxide as their sole carbon source and consequently use organic molecules fr 
s from the environment to satisfy their carbon requirements. despite considerable advances in t 
11401 1 f food, the prevention of flooding, and carbon sequestration. however, they are increasingly un 
10970 1 pply man with honey and provide a vital pollination service. however, recently a large number o 
7721 1 istance genes prove an effective way of controlling pests of plants and can significantly reduc 
7658 1  temporal variability of contamination, invasive species now widely present in temperate aquati 
7047 2 s sources of industrial enzymes, and as biological control agents of plant pathogenic fungi, bu 
eeds the biodiversity of trichoderma in soil and it exceeds by far expectations regarding the n 
15402 1 e ultimate goal is therefore to improve environmental quality by achieving after bioremediation 
15480 1                                         soil and litter are the reservoir of a huge number of m 
7218 1 ssment relevant to institute to achieve coastal protection and especially sustainable developme 
12279 1 en and phosphorus from soils results in poor water quality. • there have been steep increases i 
15103 1 cological approach. we will analyse the carbon and nitrogen isotope composition in organic matt 
12613 1 ion. these included the submission poor quality land contamination reports for planning approva 
12227 2 ative impacts on local environments and water quality, and the energy required and carbon dioxi 
er quality, and the energy required and carbon dioxide evolved in their production and use, wil 
10514 4 gists, climatologists as well as forest carbon and remote sensing experts in order to provide a 
ght, the extent of forest fires and the carbon losses associated with this event. working as a  
vey to quantify the impacts of fires on carbon stocks and the functioning of the fire-affected  
ht-induced fire impact on the amazonian carbon stocks by integrating the previous data. due to  
15343 1 n reported in many bird species even in protected wetlands. however, very little is known about 
10776 1  play a vital role in nitrogen cycling, water quality and ecosystem functioning and are sensiti 
10567 1 gauge what effect these factors have on carbon sequestration. we have considerable experience w 
12435 1 h to issues in fisheries management and environment protection.  
7129 2 petition if the increase of co2 promote invasive species over native species in terms of phenol 
kely deterioration in the efficiency of biological control because of the alteration of the che 
2149 1 odels in order to predict the impact of water quality on stocks and populations of wild atlanti 
13592 1 ct effect leading to the degradation of water quality in nursery grounds. we will use a combina 
14183 2  aim of finding innovative solutions to pest control in estonia that minimise pesticide use, ma 
or integrated pest management enhancing conservation biocontrol. postgraduate training, technol 
11140 3                          as atmospheric carbon dioxide continues to rise the ph of seawater wil 
r study here, e.g. on rates of man-made carbon dioxide uptake by the oceans and calculation of  
 trace gases for particle formation and air quality. what is proposed here would add an additio 
187 2 evergreen plants growing in contrasting soil and latitude conditions. it is known that the leaf 
ter leaf longevity enables higher total carbon gain in conditions where resources are limited.  
11818 9                   production of organic carbon by phytoplankton in the surface ocean, followed  
ed by transport of some of this organic carbon on sinking particulate matter from the surface o 
ean into underlying sediments, extracts carbon dioxide from and injects oxygen into the atmosph 
hat changes in the magnitude of organic-carbon deposition in deep-sea sediments can influence t 
 composition of the atmosphere. organic-carbon burial in deep-sea sediments must, therefore, be 
 the mechanisms controlling the flux of carbon from the oceanic water column into underlying se 
 underlying sediments and the burial of carbon in the sediments is of crucial importance. a num 
 a number of possible controls on these carbon fluxes into deep-sea sediments have been studied 
w do different tidal forcings influence carbon dynamics at kilometre-scale seafloor elevations  
7626 2 hemical and biological qualities of the soil and encourage the installation of plants. it is ba 
gineering can play an important role in soil protection against surface erosion at the recovery 
2054 2  as birds, would most likely respond to habitat quality at stand level and to compositional cha 
ed to measure density of birds, whereas soil and litter samples are used to sample snails and e 
10032 4 ions, may exert a lot of control on the water quality of the river and also its ecology: so muc 
 of the hyporheic zone to influence the water quality of a river. although quite a few research 
acceptors other than oxygen for organic carbon oxidation as the amount of oxygen in the riverbe 
he hyporheic zone is in influencing the water quality in rivers that are groundwater-fed, we wi 
11842 4 ions, may exert a lot of control on the water quality of the river and also its ecology: so muc 
 of the hyporheic zone to influence the water quality of a river. although quite a few research 
acceptors other than oxygen for organic carbon oxidation as the amount of oxygen in the riverbe 
he hyporheic zone is in influencing the water quality in rivers that are groundwater-fed, we wi 
13885 1 ocus management actions. in addition to invasive species, the results can be applied to conserv 
12274 2 . nitrogen inputs are a major source of carbon dioxide emissions and leaching of nitrogen and p 
en and phosphorus from soils results in poor water quality. breeding crops that require less fe 
12768 2                             as european protected species, bats are strictly protected under eu 
when bats move roosts. we will quantify habitat quality around churches used as roosts by using 
1090 1 through either autogamous or allogamous pollination.  
15049 1 roject will have an important impact on biological control of insects because they will represe 
10407 2 l examine a range of services including carbon sequestration, flood hazard and water regulation 
 carbon sequestration, flood hazard and water regulation, and the provision of food, materials  
14499 2 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 
7188 2 ctly for its ecological effects against invasive species may have evolutionary effects exactly  
 operations targeting mechanisms of the invasive species in order to place it on an "evolutiona 
13577 1 her concentrations of dissolved organic carbon , and changed light climate and hydrography. suc 
15400 1 tion, progressive isolation, changes in habitat quality and the increase of their permeability  
7705 1  of crops by pests and amplification of biological control by natural enemies. in this context, 
11631 2 ve a key role in the global terrestrial carbon cycle. the external mycelium of em fungi is of p 
 is the primary interface with the bulk soil and is therefore the main conduit through which re 
10962 1 fect upon ecosystem function and global carbon biogeochemistry. we propose to investigate the e 
14982 1 talish the fragil points between water, soil and native vegetation and crops. finally, a global 
2177 1 t policy will need to consider both the protection of forests, and management of the matrix.  
12554 13                                         insect pollinators initiative insects including honeybe 
butterflies and moths are vital for the pollination of many cultivated and wild plants. they pl 
 plants. having a healthy population of pollinators is also essential to maintain biodiversity  
ain biodiversity in natural ecosystems. pollinating insects are vulnerable to pests, diseases a 
ion set to reach 9 billion by 2050. the insect pollinators initiative is a fund of up to £10m t 
e causes and consequences of threats to insect pollinators and to inform the development of app 
nd approaches to reverse the decline in pollinator insects. researchers funded under the initia 
other organisations with an interest in insect pollinators to ensure a strong network to apply  
ctor causing the problem. the causes of pollinator declines are likely to be complex and involv 
omplex and involve interactions between pollinators, the environment and the pests and diseases 
hese insects. because of the vital role pollinating insects play – insects pollinate at least o 
he decline. some factors may affect all pollinating insects, others only one or two species and 
ng, alongside existing expertise in the pollinator research community.  
403 1 pletely replace the use of chemicals in pest control operations, many chemicals will continue t 
14768 1 ce, can be regarded as bio-indicator of habitat quality at larger scale.  
10252 1 st products, hydrological services, and carbon sequestration and biodiversity. we will seek to  
11167 1 ral to research into climate change and air quality. the description of chemistry in these mode 
10649 2  techniques to soils amended with black carbon and kaolinte, keeping selected applications in m 
ation of macro- and micro-aggregates in soil and the stability of biochar. this will be importa 
533 1 ipally approached from the viewpoint of nature protection policy  
7209 1  hand the sustainability of methods for controlling pests and auxiliaries by integrating a bett 
2494 1 ions. further, acacia will apply stable carbon and oxygen isotopic analysis combined with 14c d 
14153 1  can not be higher, than allowed by net carbon uptake by the tree. decrease in tree photosynthe 
13800 1 ctive is to evaluate the possibility of biological control of phytophagous insects on willows b 
10777 1  many benefits for the ability of bt to control pests. preliminary data in my laboratory sugges 
11165 1  many benefits for the ability of bt to control pests. preliminary data in my laboratory sugges 
15322 3 y mechanistic processes that may enable invasive species to establish in the face of novel envi 
eir introduction. the ongoing spread of invasive species in aquatic ecosystems calls for an urg 
will measure the response of native and invasive species, both in terms of survival and in diff 
7564 1 the introduction by man parasitoids for biological control, and will aim to understand the gene 
7176 1 an approach which assigns, rightly, the invasive species qualifier aboriginal and especially th 
7180 2 he management of these two species, and invasive species in general what their words and attitu 
at the public knows or does not know of invasive species our sociological research is based on  
13594 1 ing the recreational value of lakes and water quality. despite being classified as a nuisance a 
15316 2                                         invasive species can pose a major threat to the biotic  
establishment and eventual expansion of invasive species in aquatic systems are not well unders 
15331 1                                  exotic invasive species assessing the impacts of exotic trees  
7162 1 ry of endemism. tags: drosophila model, invasive species, ecological intraspecific divergence,  
14841 2  next years. the population genetics of invasive species has been relatively unexplored, even t 
 identify dispersal routes used by this invasive species. 3- to assess the effect of hydrologic 
14840 1                                         invasive species are the second threat to diversity aft 
7018 1 s of pharmaceuticals and mycotoxins, as biological control agents of plant pathogenic fungi, an 
10491 1 the sun s energy to combine atmospheric carbon dioxide habitats as these are considered to be t 
12622 4           peatlands are large stores of carbon to see which restoration measures are best at re 
tre for ecology and hydrology for their carbon catchments programme. the rigorously designed fi 
on, meteorological variables, dissolved carbon fluxes and detailed identification of the mechan 
its in terms of conserving the peatland carbon store and minimising ghg emissions. we will also 
12633 1 properties. the microbial properties or soil biological quality indicators distributed across g 
10396 1 cture can be modified to provide useful environmental protection. these results will also be in 
10406 1  producers, i.e. they convert inorganic carbon on the most likely predators of these cyanobacte 
7015 1 tic systems, with on average 40% of the carbon fixed through primary production flowing through 
14599 2 enor . the specific steps to ensure the trophic control of the mar menor should start from a de 
r menor, as in hydrodynamic aspects and water quality as in trophic aspects, using the wide inf 
10033 2 alth of information, both as records of carbon cycling in the environment and as a basis for al 
nderstanding past changes in the global carbon cycle. the project will also contribute to hypot 
10783 2 alth of information, both as records of carbon cycling in the environment and as a basis for al 
nderstanding past changes in the global carbon cycle. the project will also contribute to hypot 
11559 2 alth of information, both as records of carbon cycling in the environment and as a basis for al 
nderstanding past changes in the global carbon cycle. the project will also contribute to hypot 
7259 2 aquatic environment, the role played by carbon from terrestrial sources in the diet of species  
tions and the first results obtained on carbon sources used by the species in the course of a w 
13984 4 ng insects by comparing processes along regulated rivers with those along free-flowing ones . d 
lants. whether blackflies contribute to pollination will also be investigated. bilberries are i 
roducers that attract blackflies. their pollinators, bumblebees, might be forced to visit many  
blackflies are massive and then enhance pollination.  
2520 1 gnificance of red deer migration for an invasive species, the tick, and vice versa at the altit 
13571 1 ing damage, but also seed predation and pollination intensity. we will conduct field experiment 
12638 1 r national strategic issues relating to soil and the environment. this includes information con 
13723 1 an understanding of the mechanisms that control biodiversity. theory predicts that habitat frag 
10411 2 d upon a wide variety of supporting and regulating services that determine the underlying bioph 
cluding pest and disease regulation and pollination that are important for maintaining the prod 
2036 2  developing and maintaining a fisheries/nature protection management strategy in the wadden sea 
fishery that must take the needs of the protected species of birds into account.  
10725 2 en estuaries and the ocean across which carbon, nutrients, sediments and contaminants are excha 
r months. the exchange of nutrients and carbon across these critical interfaces of stratified f 
11084 1 ut europe, to increase biodiversity and environmental quality by restoring lowland rivers and f 
14935 1 pplementation has been effective in the control of diseases in other birds species, and ducks a 
2474 1 ver-exploitation and give incentive for protection of biodiversity. there is uncertainty about  
14797 2 nvolved in plant growth promotion or as biocontrol agents still remains unexplored. consequentl 
ntial and may play an important role in crop protection. in the present research proposal, we i 
14159 1 ement of diversity in grasslands and in control of invasive alien plants.  
11722 1  appear to recover from periods of poor food quality or quantity experienced in early developme 
15396 1 at the southern edge of the species the habitat quality is dropping below the lower limit, and  
12228 5 er crop pest and vast sums are spent on weed control annually, often with a significant cost to 
. in the last 30-40 years, agricultural weed control has been dominated by herbicides. more rec 
ance are limiting herbicide options for weed control, leading to calls for a more integrated an 
icide options with advances in physical weed control and a greater emphasis on cultural weed ma 
 weed management. chemical and physical weed control methods are predominantly technology-led a 
11724 1  cohort age as the progeny of non-local pollination are selected out.  
2485 3 provision of clean water is inadequate, storage of water for domestic use is crucial. fecal con 
 health risks associated with household water storage by identifying relationships between hous 
ill assist in development of integrated disease control strategies appropriate for the southeas 
10469 1 iceland, together with analysis of hand-pollination data to determine the plants incompatibilit 
11404 1  transformation of nutrients, including carbon and nitrogen, in the environment. however, our u 
10085 5 mall flowers: , and the average size of pollinator increases with flower size. the mobility of  
with flower size. the mobility of these insect pollinators is important, because their foraging 
er size and flower number are linked to pollinator size and mobility, the dispersal of pollen a 
licability to any plant community where competition for pollinators might underlie the evolutio 
ented tropical forest communities where plant-pollinator interactions are disrupted by changes  
2023 1 in a range of coastal marine sediments. carbon degradation in sediments covers the most importa 
15104 1                    floodplains of large regulated rivers with impacts of global changes extensi 
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 
10148 1 actions between nutrient deposition and carbon cycling are also important for understanding bio 
10908 1 actions between nutrient deposition and carbon cycling are also important for understanding bio 
11751 1 actions between nutrient deposition and carbon cycling are also important for understanding bio 
12165 2  assess the effectiveness of a range of weed control methods in the presence of uncommon arable 
cious weeds. proposals will be made for weed control treatments, such as cultural methods, herb 
14670 2 exes used by individuals when assessing habitat quality to subsequently choose an habitat. this 
 characters as possible cues indicating habitat quality.  
13804 9 tions of natural habitats have caused a pollinator decline, and as a result pollination interac 
d a pollinator decline, and as a result pollination interactions may be at risk. the impact of  
eractions may be at risk. the impact of pollinator loss on plant communities is, among other th 
o depend on degree of specialization of plant-pollinator interactions. this project will invest 
tigate the effect of loss of functional pollinator groups on reproductive success in plant spec 
flower morphology. extinctions of large pollinators will be simulated in a field experiment on  
ls and individuals subjected to natural pollination, and differences in degree of response will 
ized flowers. differences in functional pollinator diversity between species with specialized a 
ts of heterospecific pollen on arriving pollinators and on stigmas. specialization has been sug 
12282 8 of this scoping study is to explore the carbon components of key production steps within conven 
techniques that could contribute to low carbon farming. this should identify where reductions i 
his should identify where reductions in carbon inputs could be achieved without compromising yi 
ality and inform the development of low carbon production systems which are resilient and adapt 
principally from the perspective of its carbon burden. information on current production practi 
ovide a baseline for the assessments of carbon and water use. this will be obtained from standa 
provide a structure for quantifying the carbon inputs at every stage of production and identify 
techniques that could contribute to low carbon farming will be identified and key positive and  
15242 1 a mechanism that and depict the role of pollinators in those pollen transfer patterns  
7163 1 sms invasive processes and characterize invasive species as well as the most invaded areas. the 
10716 2  use forms of dms and dmsp in which the carbon atoms have an atomic weight of 13, not the more  
igests such a heavy molecule, the heavy carbon is incorporated into its molecules, including dn 
11704 2  use forms of dms and dmsp in which the carbon atoms have an atomic weight of 13, not the more  
igests such a heavy molecule, the heavy carbon is incorporated into its molecules, including dn 
12156 1 ator abundance can be reduced by lethal predator control but this is not a cost-effective long- 
10902 1 ave been shown to enhance services like pollination to levels where they have a direct economic 
10986 1 ave been shown to enhance services like pollination to levels where they have a direct economic 
12187 1 vices, including nutrient retention and pollination. this will be mainly tested using selected  
11231 12 therefore vital in determining how much carbon is stored or released into the atmosphere. payme 
nt practices that help to store organic carbon in soils and vegetation are becoming increasingl 
he risks and gains of managing land for carbon is an urgent challenge that requires the coopera 
ideas on the topic of managing land for carbon . we will focus on study areas in namibia, botsw 
will: a review current understanding of carbon stores and losses and the ways in which they are 
ays in which they are measured for both soil and vegetation; b identify the livelihood activiti 
s associated with managing the land for carbon; c identify the current environmental status of  
 to assessing how managing the land for carbon could alter these wider services; and d evaluate 
lopment of community-based payments for carbon storage projects. the novelty of our project lie 
 yet, we extend it by assessing organic carbon in both soil and vegetation and link this with s 
 it by assessing organic carbon in both soil and vegetation and link this with social and econo 
uthern africa while also increasing the carbon stored in the environment. in pursuing these act 
14277 2 parently linked with improvement of the water quality. the huge production of biomass can cause 
 development, based on criteria such as flood protection, amenity value and biodiversity preser 
10732 5 as an important influence on the global carbon cycling by affecting vegetation structure, chang 
ffecting vegetation structure, changing carbon pools and fluxes, and causing feedbacks to the a 
n will be available for calculating the carbon budget of amazonian forests, taking into account 
 uptake, release and the net balance of carbon in fire-affected forest sites in recent years, t 
onent processes that determine this net carbon balance and to understand how climate variation  
10810 5 as an important influence on the global carbon cycling by affecting vegetation structure, chang 
ffecting vegetation structure, changing carbon pools and fluxes, and causing feedbacks to the a 
n will be available for calculating the carbon budget of amazonian forests, taking into account 
 uptake, release and the net balance of carbon in fire-affected forest sites in recent years, t 
onent processes that determine this net carbon balance and to understand how climate variation  
9823 1 arshore marine environments occurs when coastal protection schemes, such as artificial reefs, a 
10128 2 hin marine ecosystems are important for regulating climate, nutrient cycling and the food chain 
en, as well as absorbing gases, such as carbon dioxide , and therefore to identify those combin 
10245 1 omponents of the sink for anthropogenic carbon dioxide. we will also make best estimates of the 
10512 1 omponents of the sink for anthropogenic carbon dioxide. we will also make best estimates of the 
11471 1 omponents of the sink for anthropogenic carbon dioxide. we will also make best estimates of the 
11520 1 omponents of the sink for anthropogenic carbon dioxide. we will also make best estimates of the 
11796 1 omponents of the sink for anthropogenic carbon dioxide. we will also make best estimates of the 
9981 1 omponents of the sink for anthropogenic carbon dioxide. we will also make best estimates of the 
12437 1 an`s capacity to provide food, maintain water quality, and recover from perturbations, and that 
2178 2  stoichiometry, biogeochemical cycling, food quality and energy/carbon flow through ecosystems  
emical cycling, food quality and energy/carbon flow through ecosystems from inorganic chemistry 
10335 1 ur group, employing a compound-specific carbon isotope approach, revealed a new marine dietary  
2467 1 ue to the major role of these oceans in carbon cycling and the global climate, and because thei 
12607 2  bleaklow plateau of greenhouse gas and carbon fluxes of peat in different conditions. the over 
toration on the bleaklow plateau on the carbon balance of the system.  
7707 1 anean eco- agro- systems by focusing on quality landscapes, guarantee sustainable development a 
14834 1 iology, as well as we want to include a soil quality index developed by us in the previous proj 
14835 1 iology, as well as we want to include a soil quality index developed by us in the previous proj 
11146 1                                     the carbon cycle in freshwater lake systems comprises two m 
10554 1 uction of oxygen and the consumption of carbon dioxide by very small, single celled organisms,  
10558 1 uction of oxygen and the consumption of carbon dioxide by very small, single celled organisms,  
10019 1 on is that climate change itself alters habitat quality and quantity, by changing the availabil 
11572 1 on is that climate change itself alters habitat quality and quantity, by changing the availabil 
10887 2 lly be the case. we measured the stable carbon isotope values of common aquatic invertebrates . 
ate is made up in part by 100+ year old carbon, then this would change our perception of the ec 
10719 3 driven by primary production of organic carbon made by non-photosythetic bacteria in the cave.  
d cells the heavy, 13c from methane and carbon dioxide that we fed the cells using the raman mi 
er time we can follow the course of the carbon through the microbial food web in movile cave.  
2486 2 ontains large amounts of stored organic carbon which constitute a source for release of climate 
f climate gases. degradation of organic carbon involves a consortium of microbial phyla represe 
12061 1 es from extinction, either by improving habitat quality or by facilitating the colonization of  
2003 3 ibing the plant species composition and carbon accumulation of peat bogs in relation to changes 
on the historic species composition and carbon accumulation, supplied by project 1, will be use 
change on plant species composition and carbon sequestration in bogs, both in the past and in t 
7192 1 esticides. but the current practices of crop protection raise complex issues largely detailed i 
13767 3 roup of ecosystem services, for example carbon sequestration, without consideration of how chan 
ly of other ecosystem services, such as water quality or pollination. the proposed research pro 
stem services, such as water quality or pollination. the proposed research proposes to develop  
11838 3  contributing ~15% to the annual global carbon sink. climate change, particularly altered preci 
 sustainability or their role as global carbon sinks. despite decades of research, factors regu 
nfluence the structure and above-ground carbon sequestration potential of different savannas, a 
15234 1 ity. we will deepen in the study of the carbon cycle by analysing the production and decomposit 
14227 2 e microbial loop. to assess the flow of carbon and nutrients through the ecosystem, we will qua 
 data of dissolved oxygen. the internal carbon cycle of võrtsjärv is modelled and its climate s 
12593 3 al regime, by, for example altering the water storage and transmission properties of the soil.  
rest is the possible change in the soil carbon budget, for example by increased rates of net lo 
be such things as quantified changes in water storage in the soil, or the rate of biochemical p 
10493 6 riparian biodiversity, lowered drinking water quality and, in some places, increased occurrence 
r human impact on riverine nutrient and carbon fluxes by large-scale land-use and management ch 
 suggested to be of potentially greater water quality significance than projected climate chang 
ecords to construct the world s longest water quality time series comprising monthly average ni 
sent. this allows a unique insight into water quality changes affected by direct human influenc 
ange impacts will be as big a threat to water quality as large-scale changes in land use. this  
11344 2                                     the carbon cycle in freshwater lake systems comprises two m 
c phytoplankton biomass, principally to carbon dioxide and methane. in the environment, anaerob 
10074 1 al functions of the oceans not just the carbon cycle, it is necessary that for models to adequa 
14926 6 iosperms is the adaptation of plants to animal pollinators. the significance of animal pollinat 
animal pollinators. the significance of animal pollinator as a directional force can be appreci 
ce can be appreciated in the convergent pollination syndromes observed in flowers of quite diff 
as a result of adaptacion to particular pollinators. nor is it known to what extent convergence 
 it known to what extent convergence in pollination syndromes reflects convergence at the molec 
mental pathways leading to a particular pollination syndromes. our working hypothesis allows tw 
15045 6 iosperms is the adaptation of plants to animal pollinators. the significance of animal pollinat 
animal pollinators. the significance of animal pollinator as a directional force can be appreci 
ce can be appreciated in the convergent pollination syndromes observed in flowers of quite diff 
as a result of adaptation to particular pollinators. nor is it known to what extent convergence 
 it known to what extent convergence in pollination syndromes reflects convergence at the molec 
mental pathways leading to a particular pollination syndrome. my working hypothesis allows two  
14210 1 h play a central role in the regulation carbon dioxide uptake at minimal loss of water. this is 
14523 1 ing an advancement in the monitoring of air quality with moss, by using biotests. for this it w 
15110 1 as well as long-term gradual changes in water quality of g. sesquipedale. complementary field e 
7031 1 ae . practitioners, for example, in the water quality management, need not waste a lot of time  
13814 1 r threatened species and as refuges for pollinators and natural enemies of crop pests, and to e 
11254 1 uction of oxygen and the consumption of carbon dioxide by small photosynthetic plants called ph 
11494 1 uction of oxygen and the consumption of carbon dioxide by small photosynthetic plants called ph 
11029 1 ankton , and their photosynthesis draws carbon dioxide are bringing great advances, but we stil 
13974 2 c basidiomycetes, including widely used biocontrol agent phlebiopsis gigantea and endangered sp 
aprotrophic fungi on sites treated with biocontrol agent of p. gigantea and also determine impa 
15355 1 cquired ecological knowledge to improve pest control and crop productivity. the project aims to 
542 3 o strongly contrasting systems—fig/wasp pollination mutualisms and ant-plant protection mutuali 
fig/wasp pollination mutualisms and ant-plant protection mutualisms—we aim to characterize the  
 impact of climatic fluctuations on ant/plant protection mutualisms: species-distribution patte 
11096 5  this is exciting because it means that carbon fixed in photosynthesis by the trees might be us 
e it would alter the way we think about carbon and nutrient cycling in boreal forest, affect ou 
t systems. we will then use isotopes of carbon, nitrogen and phosphorus to confirm that carbon  
nitrogen and phosphorus to confirm that carbon moves from the host to the fungus and nutrients  
 can investigate how much of the fungus carbon is derived from each host, and how that influenc 
13887 2 resistance change over time. initially, invasive species may reach very high population densiti 
itude of negative ecological effects of invasive species. despite this, little is known about h 
10934 1 s, with emphasis on ag, a metal with no environmental quality standards in the uk despite being 
14452 1 joint projects in the field of ecology, environment protection, and the application of new mode 
12242 3 have also been identified including the protection of land and water quality and their potentia 
ed including the protection of land and water quality and their potential for carbon sequestrat 
d water quality and their potential for carbon sequestration. their genetic diversity also prov 
10560 1 early earth through an array of organic-carbon-rich samples available to us via existing and pr 
14229 1 n roots hydraulic conductivity and on a regulation of water transfer between roots and foliage. 
13613 1 , reducing productivity, and increasing carbon storage in stable soil pools. therefore, underst 
13936 1 ntribution to the primary production of carbon and nitrogen in the baltic sea. the results of t 
12313 3 he eu the first major advance in rodent pest control since the registration of the second gener 
animal welfare. the new chemistries and pest control products that emerge will be shaped by eur 
ompound has already been registered for predator control in new zealand. if successful there wi 
10291 4 rature on plant tissue respiration. the carbon balance of an organism and of an ecosystem is st 
re thought to be a sink for atmospheric carbon dioxide, slowing the continual rise in carbon di 
 dioxide, slowing the continual rise in carbon dioxide concentration in the atmosphere. about 8 
limits plant respiration, and hence the carbon balance. we also know only a little about how pl 
11285 3 rature on plant tissue respiration. the carbon balance of an organism and of an ecosystem is st 
re thought to be a sink for atmospheric carbon dioxide, slowing the continual rise in carbon di 
 dioxide, slowing the continual rise in carbon dioxide concentration in the atmosphere. a large 
10667 1  all the quality data relevant to ocean carbon uptake and ph. estimation of change will be set  
10916 1  all the quality data relevant to ocean carbon uptake, and from which ph trends can be derived. 
11174 1  all the quality data relevant to ocean carbon uptake, and from which ph trends can be derived. 
11403 1  all the quality data relevant to ocean carbon uptake, and from which ph trends can be derived. 
146 1 enopterous parasitoids is increasing in plant protection.  
13776 1                        rising levels of carbon dioxide in the atmosphere are making the oceans  
10894 1 s is releasing vast quantities of extra carbon dioxide to the earth s atmosphere. much of this  
10003 1 s is releasing vast quantities of extra carbon dioxide to the earth s atmosphere. much of this  
10153 1 s is releasing vast quantities of extra carbon dioxide to the earth s atmosphere. much of this  
11687 1 s is releasing vast quantities of extra carbon dioxide to the earth s atmosphere. much of this  
14987 3 therefore, the study of the dynamics of invasive species, their interaccions with other key org 
y. the project propose the study of the invasive species oculina patagonica aspects of its auto 
tribute to determine the impact of this invasive species on natural and human altered communiti 
7303 1 ican and lizard ruins, recently arrived invasive species on the island. a second part concerns  
2058 1 rthern svalbard shelf through different carbon sources and in different years. ultimately, the  
11334 4 ar in relation to nutrients, minimising carbon footprint, and at the same time, minimising capi 
esilience but also to reduce associated carbon and economic costs. therefore, the water industr 
but is also embedding the importance of carbon footprint in waste water treatment process optim 
ptimise pollutant removal at the lowest carbon cost.  
14872 4         soils can be source and sink of carbon, then soils contribute to carbon cycle regulatio 
ink of carbon, then soils contribute to carbon cycle regulation and their consequences on clima 
 soil management influence soil organic carbon content and its flux to the atmosphere. the nume 
 to increase the amount of sequestrated carbon by the soil, its productivity and biodiversity.  
11843 2 by actively removing individuals of the invasive species. removing the last individual however  
necessary to continue controlling those invasive species for the foreseeable future. this is ex 
10037 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
10039 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
10293 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
10296 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
11055 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
11306 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
11570 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
11834 1 ling studies of chemical processes in a protected forest area of sabah, east malaysia, to bette 
13481 1 we will do this by documenting plankton food quality and follow the transfer to fish during eig 
6885 1  which helps to infer trophic level and water quality. comparison between recent and ancient cr 
10647 2 ove models of how zooplankton transport carbon, through their faecal material, to depth. unders 
 sea ice might alter changes in the way carbon is captured and stored in the productive arctic  
12070 1  sediment is an inflating parameter: an invasive species becoming rapidly a recurrent problem i 
10782 1 iologically important elements, such as carbon situations. data describing changes in growth an 
11318 1 iologically important elements, such as carbon situations. data describing changes in growth an 
13841 1 provide relevant conservation plans for protecting species diversity in a landscape context for 
10265 1 agriculture, humans have been releasing carbon dioxide . atmospheric co2 is predicted to steadi 
10791 1 agriculture, humans have been releasing carbon dioxide . atmospheric co2 is predicted to steadi 
2187 1 project will give insight into how both habitat quality and landscape structure affect viabilit 
10409 4 thern europe are major global sinks for carbon and support a unique biological community. clima 
spread summer drying, thus reducing net carbon sequestration. this project aims to understand h 
te to accelerated rates of nitrogen and carbon cycling. this will result in increased losses of 
ult in increased losses of nitrogen and carbon to the environment, seen principally as elevated 
13611 5 thern europe are major global sinks for carbon and support a unique biological community. clima 
spread summer drying, thus reducing net carbon sequestration. this project aims to understand t 
te to accelerated rates of nitrogen and carbon cycling. this will result in increased losses of 
ult in increased losses of nitrogen and carbon to the environment, seen principally as elevated 
o a breakdown in the ecosystem and mass carbon and nitrogen loss. to address these concerns, we 
15571 5 thern europe are major global sinks for carbon and support a unique biological community. clima 
spread summer drying, thus reducing net carbon sequestration. this project aims to understand t 
te to accelerated rates of nitrogen and carbon cycling. this will result in increased losses of 
ult in increased losses of nitrogen and carbon to the environment, seen principally as elevated 
o a breakdown in the ecosystem and mass carbon and nitrogen loss. to address these concerns, we 
15426 1 roduction time and weak constraints for pollination. in addition, an adaptive divergence in rel 
15454 8 o a fundamental component of the global carbon cycle. litter and soil organic matter pools cont 
tter pools contain important amounts of carbon in terrestrial ecosystems and their relative fas 
e most dynamic components of the global carbon cycle. litter decomposition is controlled mainly 
r decomposition is controlled mainly by litter quality, temperature and precipitation. however, 
ng co2 and thus, it is a direct loss of carbon from the ecosystem to the atmosphere without bei 
s and its contribution to the ecosystem carbon balance as well as its response to climate chang 
on of photodegradation to the ecosystem carbon balance in a mediterranean shrubland site where  
semiarid ecosytems and to the ecosystem carbon balance. another part of the project will test t 
6940 1 ervation management of the area and the protected species. the examination of chytrid fungus wi 
15512 1 hat correspond to environments in which soil and climatic conditions are unfavorable, such as c 
14503 1  advance with potential applications on plant protection and the environmental monitoring in th 
15203 2                           mankind needs good quality water. however, at present, many aquatic e 
r restoration initiative that guarantee good water quality is welcome. the fact that some aquat 
2513 3 in the global biogeochemical cycling of carbon and other key elements . the overall ecological  
etermines the efficiency by which fixed carbon is transferred to higher trophic levels and into 
nd into the deep ocean- and sedimentary carbon reservoirs. concern is growing that rising tempe 
10381 1 . the review and assessment of london s air quality confirms that oxides of n from traffic exce 
14211 2              understanding factors that control species coexistence and diversity is crucial to 
hreatened species and to combat harmful invasive species or deceases. the most prevalent theory 
14212 1 nt species that naturally co-occur with invasive species in their native ranges show little res 
14662 1 on of species or plant types useful for erosion control in a scenario of climatic change. 3. to 
14889 1  of allergic asthma during or after the pollination period. various sub-micronic particles may  
14887 3 portance to exactly know the moments of pollination, and the factors that most influences polle 
ses for them provoked. likewise, during pollination and its previous periods, the expression an 
rains, as before as during or after the pollination period, leads us to carry out the study of  
14849 2 his project new ways of study regarding air quality are proposed, by using the methodology deve 
re only a few researches focused in the air quality evaluation regarding to biological particle 
14850 2 his project new ways of study regarding air quality are proposed, by using the methodology deve 
re only a few researches focused in the air quality evaluation regarding to biological particle 
14851 2 his project new ways of study regarding air quality are proposed, by using the methodology deve 
re only a few researches focused in the air quality evaluation regarding to biological particle 
14886 1 n of flowering plants is initiated with pollination when the desiccated pollen grains land on t 
15027 3 tial for the levels of pollen flow than pollination system of the species we propose to evaluat 
es, the effective number o fathers, the pollination area neigbourhood, and the inbreeding and b 
ing rates. 4. to address changes in the pollination biology of the studied species in relation  
2067 5  flowering plants produce seeds through pollination interactions with animals, and therefore th 
rently, there is growing awareness of a pollination crisis whereby the diversity of pollinators 
ess of a pollination crisis whereby the diversity of pollinators is declined due to human inter 
. to truly assess any consequences of a pollination crisis for natural ecosystems, there is an  
tantial and complete knowledge of plant-pollinator relationships and interactions, and the cons 
11445 6 hallenges this notion in the context of pollination biology. the provocative idea is that a pla 
splay striking specialisation to a less efficient pollinator, provided that such specialisation 
ere with the benefits conferred by more efficient pollinators. in other words, plants may be cr 
edictions of adaptation to a particular pollinator type. we found an ideal model system to stud 
wers, which appear to be specialised to bird pollination. yet there are no to tackle this quest 
entify the relative values of different pollinators for these flowers.  
14941 3 effect of predators on the behaviour of pollinators will depend on the amount of nectar that po 
ill depend on the amount of nectar that pollinators can expect to obtain at flowers. flower col 
ecause they affect the probability that pollinators detect ambushing predators and the probabil 
7418 1 into account the problems of farmers on pollinators. second, to organize a national day of awar 
475 5 thern europe are major global sinks for carbon and support a unique biological community. clima 
spread summer drying, thus reducing net carbon sequestration. this project aims to understand t 
te to accelerated rates of nitrogen and carbon cycling. this will result in increased losses of 
ult in increased losses of nitrogen and carbon to the environment, seen principally as elevated 
o a breakdown in the ecosystem and mass carbon and nitrogen loss. to address these concerns, we 
11149 1 st to the government regulatory bodies, environment protection groups, industry and the wider p 
11696 1 st to the government regulatory bodies, environment protection groups, industry and the wider p 
6745 1 e will able to give suggestions for the plant protection experts. we also hope that the researc 
12612 1                          part 2a of the environmental protection act 1990 came into force in en 
11163 2  negative consequences for food supply, water quality, biodiversity and other aspects of the en 
osion on the hilly lands; deteriorating water quality in irrigation channels, rivers and lakes; 
9945 1 ost alarmingly, key global cycles which control climate have been altered. however, how the pro 
9851 4 ons, and between these plants and their pollinators. these mismatches could substantially reduc 
 and the ecological resilience of plant-pollinator networks. attempts to predict such effects a 
tionary change in flower morphology and pollinator visitation. the case partner, the avon wildl 
mise the capacity for species to adapt. pollination networks on its grassland reserves are alre 
10108 1 s climate change, genetic modification, invasive species and the loss of biodiversity, mean tha 
14123 1           biogenic volatile compound on air quality under climate change and provides relevant  
2105 1 te change impacts on forest management, carbon sequestration, and income/employment in the fore 
14555 1 onmental factors, such as abundance and quality of food resources or demographic parameters, su 
2140 1 mpare arthropod species richness in the soil and understorey vs. canopy habitats of a tropical  
12560 3  want to minimise pesticide use and the carbon footprint of farming while maintaining food prod 
tify areas of fields needing mechanical weed control thereby reducing both carbon footprints an 
ical weed control thereby reducing both carbon footprints and also damage to crops by, for exam 
11145 1  which in turn reduces infiltration and water storage and may increase the number of flooding e 
10261 1 anisms effect how key elements, such as carbon and nitrogen, are cycled on a global scale. ther 
12189 7 n from ecosystems, such as clean water, flood control, storage of greenhouse gases and pollinat 
ontrol, storage of greenhouse gases and pollination of crops. they also include cultural servic 
conserve wildlife; maintain and enhance landscape quality and character; protect the historic e 
of land management on processes such as carbon storage and water flow to determine how combinat 
, greenhouse gas storage and emissions, water quality in terms of nitrogen phosphorus and sedim 
ms of nitrogen phosphorus and sediment, pollination of crops, biodiversity, and stakeholders’ u 
ntal stewardship activities will affect water quantity and quality and greenhouse gas storage o 
15451 2 . it will give us a global image of the water quality. 3 succession assessment of the pseudomon 
 risk assessment of the bacteriological water quality for the patient in hemodialysis with chro 
12540 1  will be written and made available for plant protection organizations across europe. in additi 
12544 1 ds are the first tools used by national plant protection organisations  
11183 3 al to research councils energy program: carbon capture and storage / potential ecosystem impact 
tential ecosystem impacts of geological carbon storage call. quantifying and monitoring potenti 
tential ecosystem impacts of geological carbon storage to a small scale tightly controlled arti 
9858 2 iodiversity, climate change adaptation, air quality management, environmental performance of bu 
 and biodiversity strategies and the gm air quality action plan, and this has provided the moti 
10166 1  as wind, wave and solar renewables and carbon capture and storage to a small scale tightly con 
10215 3 al to research councils energy program: carbon capture and storage / potential ecosystem impact 
tential ecosystem impacts of geological carbon storage call. quantifying and monitoring potenti 
tential ecosystem impacts of geological carbon storage to a small scale tightly controlled arti 
10415 1  as wind, wave and solar renewables and carbon capture and storage to a small scale tightly con 
10671 1  as wind, wave and solar renewables and carbon capture and storage to a small scale tightly con 
10931 3 al to research councils energy program: carbon capture and storage / potential ecosystem impact 
tential ecosystem impacts of geological carbon storage call. quantifying and monitoring potenti 
tential ecosystem impacts of geological carbon storage to a small scale tightly controlled arti 
11719 3 al to research councils energy program: carbon capture and storage / potential ecosystem impact 
tential ecosystem impacts of geological carbon storage call. quantifying and monitoring potenti 
tential ecosystem impacts of geological carbon storage to a small scale tightly controlled arti 
11182 1  as wind, wave and solar renewables and carbon capture and storage to a small scale tightly con 
10319 2  basis, are some of the world s densest carbon stores. discovering and quantifying the carbon s 
stores. discovering and quantifying the carbon stored in such peatlands, and the environmental  
10274 1 nd so provide less food and absorb less carbon dioxide changes. more broadly, these records of  
11020 2 he processing of soil organic matter of carbon and nitrogen from organic matter in soils. overa 
ty increases or decreases the amount of carbon and nitrogen stored in the soil.  
10359 1 ely studied in north america using both carbon and oxygen isotopes. in this proposal the mammal 
11141 2 roviding habitats for declining plants, pollinating insects and birds. all new developments in  
 quality of life in our cities, through carbon absorption, pollutant reduction, biodiversity en 
10047 2  importance of weathering on the global carbon cycle and its affect on the earth s climate. man 
 of the atmospheric partial pressure of carbon dioxide, and thus influence on the greenhouse ef 
11408 2  importance of weathering on the global carbon cycle and its affect on the earth s climate. man 
 of the atmospheric partial pressure of carbon dioxide, and thus influence on the greenhouse ef 
10779 5 stomata. stomata allow plants to absorb carbon dioxide. studies have shown that the more carbon 
oxide. studies have shown that the more carbon dioxide there is the air, the less stomata plant 
eaves allow us to detect changes in the carbon dioxide levels. as carbon dioxide is an importan 
hanges in the carbon dioxide levels. as carbon dioxide is an important greenhouse gas, changes  
ls to get independent estimates of past carbon dioxide levels. together we will put together a  
2001 1  climate change on the biodiversity and carbon accumulation in bogs during the last ca 400 year 
14871 3 to increase the content of soil organic carbon and favouring the restoration of the soil trophi 
the different organic fractions of soil carbon and its contribution to establish their trophic  
medium and long term of sequestering of carbon in soil, the activity of soil microbial biomass, 
7164 1 to explore the conditions under which a biotic control with parasitoids would be more effective 
11180 1  associated with climate change such as carbon dioxide. there are currently, however, large gap 
12207 1 work will aim to achieve high levels of weed control with the minimum risk of crop damage and r 
2012 4  response to gradual changes in organic carbon loading. thus, the effects of increased organic  
 thus, the effects of increased organic carbon loading on microbial abundance, microbial degrad 
functioning and its response to organic carbon loading. the experimental research will be condu 
g of their response to changing organic carbon loadings is imperative.  
7462 4                                         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 
-scale soter databases, and an enhanced soil and terrain database at scale 1:1 million for the  
pplications related to major threats to soil quality and performance.  
11488 1 uction of oxygen and the consumption of carbon dioxide by very small, single celled organisms,  
7621 1 2008 as part of the project systemo the carbon content of soils while ensuring plant productivi 
15382 11  species and the season of the year for carbon sequestration. according to a specific citation  
ophication will be studied jointly with carbon sequestration in environments of high diversity  
e entirely compatible with an effective carbon sequestration them, this may be influenced by ve 
following question: is the capacity for carbon sequestration of semiarid mediterranean wetlands 
chemical processes related to cycles of carbon and nutrients in the plant-soil-water system of  
e ability of these systems to sequester carbon and act at the same time as green filters. speci 
rogen, phosphorus and dissolved organic carbon contents in eutrophicated waters and if this is  
 soil microbial activity related to the carbon cycle is influenced by the type of litter and by 
rogen, phosphorus and dissolved organic carbon contents in eutrophicated waters and if this is  
rogen, phosphorus and dissolved organic carbon contents in eutrophicated waters and if this is  
trophic water on the balance of organic carbon, nitrogen and phosphorus in the plant-soil syste 
162 1 ducted mainly by the researchers of the environmental protection institute, but several other t 
13460 1 ity management and research, especially invasive species surveys.  
11859 5 wland raised bogs to absorb atmospheric carbon dioxide through photosynthesis means that they p 
at bogs contain around one third of the carbon stored in the terrestrial biosphere. climate cha 
, which will in turn, have an effect on carbon storage. this is because degraded peatlands rele 
tlands release greenhouse gases such as carbon dioxide, instead of absorbing them. human distur 
at cutting and draining may also affect carbon storage. as a result, there is a research impera 
12753 1 oach to the assessment of the other six protected land uses specified in the red. ultimately th 
14614 1 the low quantity of offspring got after self-pollination.  
12181 1 ngaged with resource protection such as soil and water and the enhancement of biodiversity, the 
6925 1 l estimations, the yearly extra cost of plant protection of wheat is at least 110 million eur i 
10256 1 y variable densities, such as pests and invasive species. identifying the conditions that favou 
11267 1 y variable densities, such as pests and invasive species. identifying the conditions that favou 
12142 1 rder to mitigate the negative impact of invasive species.  
7207 1 tion landscape management scenarios and crop protection  
11500 1 sts. this has economic implications for carbon markets and mined-land rehabilitation.the propos 
13877 1 onnected to biodiversity monitoring and forest carbon sequestration potential. the new q-land s 
12589 1 er resources, surface water management, carbon storage and sequestration, and paleo-environment 
14198 1 he role of rhizosphere processes in the carbon and presented in international conferences. the  
11276 1  increased efficiency of the biological carbon pump and thereby contributed to the onset of the 
7640 1 ties generated a sharp deterioration in water quality. in the context of sustainable developmen 
7715 2  impact on the amount of complex forest carbon. these systems will be chosen from different pro 
 clarified through experiments cohesive soil and aggregate stability, analysis of root traits a 
2541 3 o identify appropriate policy means for biodiversity protection in an interdisciplinary context 
s to biodiversity, and the policies for biodiversity protection. a major challenge will be to e 
in open lowland. for forest a model for carbon sequestration will be developed and expressed in 
10855 1  associated with climate change such as carbon dioxide. accurate determinations of iron are the 
7480 1  and pstn networks and with a perceived visual quality equal or better than h.263. this will in 
13860 1 ainly relate to issues of regeneration, soil and water; biodiversity aspects are largely lackin 
14711 1 /chemical reaction terms, the resulting water quality model depends on a set of parameters not  
14710 1 tlands at large scale in floodplains of regulated rivers.  
12584 1 and scientifically robust indicators of soil quality. sqid phase ii . the data derived from cs2 
12183 1  as the maintenance of biodiversity and environmental quality are cornerstones and main objecti 
12289 1 directly to defras policy objectives on water quality.  
11105 1 t decisions, and their implications for population regulation, in black-tailed godwits, a migra 
11434 1 t decisions, and their implications for population regulation, in black-tailed godwits, a migra 
11780 1 ganisms which are involve in processing carbon. the extra neutron in heavy 13c provides a uniqu 
14613 1 n in order to help the establishment of biological control programs of some plagues of hemipter 
14728 2 ariation in plants where animals act as pollinators and seed dispersers is markedly structured  
genetic markers and their dependence on animal pollinator and seed dispersers for successful re 
11578 1 e to captive breeding programmes and in biological control schemes by highlighting the link bet 
11830 1 e to captive breeding programmes and in biological control schemes by highlighting the link bet 
10762 1 t important elements of the terrestrial carbon cycle. the project will also develop a measureme 
13333 1 nd mitigation of climate change through carbon sequestration in water and sediments. the innova 
13334 1 in. the more purely social dimension of protection of biodiversity and ecosystems is still some 
12620 12                  soils contain far more carbon than vegetation or the atmosphere, and the conce 
he atmosphere, and the concentration of carbon dioxide in the atmosphere and hence the climate  
te are sensitive to any changes in soil carbon. the amount of soil carbon is itself sensitive t 
nges in soil carbon. the amount of soil carbon is itself sensitive to the way the land is manag 
 england and elsewhere have been losing carbon as a result of past changes in land management.  
his problem and potentially to increase carbon storage in english soils. four sub-projects are  
ates on knowledge gaps relating to soil carbon and how it may change with management practices  
 accurate routine determination of soil carbon. the overall project will be co-ordinated by skm 
e and land management practices on soil carbon and greenhouse gas emissions. soil carbon underl 
rbon and greenhouse gas emissions. soil carbon underlying the topsoil and its interactions with 
ace horizon will be explored to improve carbon storage and sampling and laboratory determinatio 
ng and laboratory determination of soil carbon will be standardised for soil monitoring schemes 
15148 4               the thematic strategy for soil protection related to the soil organic carbon cycl 
 protection related to the soil organic carbon cycle this overall objective can be broken down  
d agricultural systems and soil organic carbon balance. to determine the soil compartments wher 
in order to establish possible sinks of carbon in the mediterranean soils.  
13988 1 ral and functitonal changes in tropical soil and their importance for soil processes is far fro 
7477 1 tegrate soil erosion, solute transport, carbon dynamics and food web dynamics within an open-so 
13350 3 delivering food, fiber and biofuels and carbon storage. however, the demand is greater than the 
iversity on stability and resilience of carbon, nitrogen and phosphorus cycling, as well as ass 
 consequences for outbreaks of pests or invasive species. soilservice will link ecological and  
11246 2 g from rapidly rising concentrations of carbon dioxide and other greenhouse gases in our atmosp 
as emissions at or above current rates, carbon dioxide will reach nearly triple the pre-industr 
10541 1 f individuals are forced to occupy poor quality habitat as a population grows, thereby driving  
15531 2 st disturbances, and will also evaluate carbon sequestration potential through the analyses of  
ation potential through the analyses of carbon budgets in the experimental areas. the specifc o 
2128 2       the movement and establishment of invasive species in new habitats is a global economic a 
as a part of the competence building on invasive species. the final results will include recomm 
15222 1 valuate its tranferibility to perform a habitat quality assessment for reptiles. 6. with the co 
15266 1 r understand fractionation processes of carbon and nitrogen isotopes and to explore the use of  
11778 1 sentangle. the proposal brings together environmental regulators, managers, civil servants and  
7317 6                                         pollinators form a key component of european biodiversi 
 declines in both wild and domesticated pollinators, and parallel declines in plants relying up 
sk, develop a red list of some european pollinator groups, in particular bees and lay the groun 
 bees and lay the groundwork for future pollinator monitoring programmes. we will also assess t 
gical and economic impacts of declining pollinator services and floral resources, including eff 
and potential mitigation of declines in pollinator services at local, national, continental and 
13352 6                                         pollinators form a key component of european biodiversi 
 declines in both wild and domesticated pollinators, and parallel declines in plants relying up 
sk, develop a red list of some european pollinator groups, in particular bees and lay the groun 
 bees and lay the groundwork for future pollinator monitoring programmes. we will also assess t 
gical and economic impacts of declining pollinator services and floral resources, including eff 
and potential mitigation of declines in pollinator services at local, national, continental and 
7244 1 coming and outgoing flows and determine carbon sequestration in the soil c. the project overall 
12357 1 mmary objective as part of the food and environment protection act 1985 , nine offshore wind fa 
12250 1 eturn, interception of light energy and carbon capture by green tissues creates dry matter from 
7023 2 to humans, such as food production, the maintenance of water quality and soil fertility, carbon 
ce of water quality and soil fertility, carbon storage, the mitigation of the effects of greenh 
10897 1  such as a toolkit for the valuation of regulating services, and decision support systems. comp 
14207 1  have been used in large quantities for controlling pests and weeds, and thus greatly improve f 
14915 1 to interact with native supergeneralist pollinators than with others that visit with only a few 
14610 11 ed food web methodology to the study of plant-pollinator interactions. these studies have revea 
reme specialists than expected if plant-pollinator relationships were randomly structured. thes 
is to describe the structure of a plant-pollinator web and study some of its properties. we wil 
ral structure of the web. in surveys of plant-pollinator interactions, rare species appear nece 
ng pollen grains from the bodies of the pollinators, which will allow us to cover a longer segm 
pared to direct of observation of plant-pollinator contacts. we will also incorporate measures  
fectiveness as a crude estimate of each pollinators contribution to the fitness of the plant sp 
certain ecological factors to the plant-pollinator structure observed. first, we will analyze s 
ip to explain a substantial part of the pollination web structure. finally, we will test whethe 
ith the principle of the most effective pollinator, plants with complex floral morphologies exh 
d receive a smaller proportion from non-effective pollinators.  
15124 12 ir role in the ecology and evolution of pollination systems. generalization has been traditiona 
f in the selective pressures exerted by pollinators. however, contrary to the theoretical expec 
ralization is quite frequent in natural pollination systems and vary at population and individu 
at population and individual levels. in pollination generalist systems, all plant genotypes in  
ract with random subsets of the overall pollinator pool. we think that the generalization degre 
ctors would attract different subset of pollinators, and plants showing different values of tho 
traits would share similar subgroups of pollinators. these inter-individual differences could p 
 of interaction among the plant and its pollinators, a phenomenon that we call structured gener 
in generalization and the intraspecific pollination and mating networks at population level are 
 in subgroups of plants sharing similar pollinators . the main aim of this project is to explor 
project is to explore the occurrence of pollinator-mediated structured generalization, the fact 
structure and clustering pattern of the pollination and mating intraspecific networks emerging  
12628 1 evels of error in our estimates of soil carbon stock. as a result we will have confidence that  
12635 4 vidence base for defra relating to soil carbon, soil management, urban soils and soil resilienc 
nts and food will also be reviewed, and soil quality indicators pertinent to policy reporting c 
otential of technologies for increasing carbon storage in soil to mitigate climate change. obje 
etting of outcome focused indicators of soil quality that can be reported on within policy repo 
7628 2 the use of integrate for monitoring the quality of water that envisages the development of biom 
quences. surveillance and monitoring of water quality are hot topics. monitoring of aquatic env 
15031 1 he use of these species has extended to air quality monitoring networks in dozens of countries  
7431 1 howing the evolution of exploitable and invasive species, information that will be taken over b 
14368 1 pdated satellite derived information on environmental quality in east-africa and to lower the b 
11412 5 irds of our major food plants depend on pollinators, and honey and beeswax produced by wild and 
s around the world, suggesting that the pollination and food services provided by pollinators m 
llination and food services provided by pollinators might be under threat. indeed recent eviden 
 suggests that the expansion in area of pollinator-dependent crops is outstripping the availabi 
ops is outstripping the availability of pollinators. while in developed areas, we can diversify 
11495 5 irds of our major food plants depend on pollinators, and honey and beeswax produced by wild and 
s around the world, suggesting that the pollination and food services provided by pollinators m 
llination and food services provided by pollinators might be under threat. indeed recent eviden 
 suggests that the expansion in area of pollinator-dependent crops is outstripping the availabi 
ops is outstripping the availability of pollinators. while in developed areas, we can diversify 
7555 1 ll be studied in the analysis of stable carbon isotope and cuticular hydrocarbons potentially.  
11688 3 them with firewood, fish, medicines and protection from floods and coastal erosion. despite the 
y productive and efficient at capturing carbon, much of which ends up buried below ground and c 
up possibilities for using payments for carbon credits to help mangrove conservation and to bri 
11617 1  across habitat boundaries. for example carbon flow between terrestrial and freshwater systems  
12139 1 e the adaptation capacity of baltic sea invasive species prorocentrum minimum to adverse biotic 
15429 1 of the trophic line that influences the biological control of aphids and psyllids that can beco 
11862 1 tools to exploit beneficial insects and control pests. the conference is themed to promote the  
14574 1 neotropical. some of them are useful in weed control, meanwhile others are pests but most of th 
15405 1  through its repercussion on the global carbon cycle, because warming can enhance decomposition 
15406 1 tion, by its repercussion on the global carbon cycle, as warming can enhance decomposition rate 
11350 1 se populations of dispersed particulate carbon sources on and within soil across scales of cm t 
10026 1 enescence rates associated with sex and environmental quality. in order to test the roles of th 
10363 3 articles. we will use cfd to study wind pollination in oilseed rape, whose flowers appear suite 
ed rape, whose flowers appear suited to insect pollination. we will determine the likelihood th 
oral architecture is optimised for wind pollination. wind tunnel experiments will be used to va 
10421 1 fect, directly or indirectly, the ocean carbon cycle. a range of new technologies will be appli 
10663 1 fect, directly or indirectly, the ocean carbon cycle. a range of new technologies will be appli 
10685 1 fect, directly or indirectly, the ocean carbon cycle. a range of new technologies will be appli 
10914 1 fect, directly or indirectly, the ocean carbon cycle. a range of new technologies will be appli 
11692 1 fect, directly or indirectly, the ocean carbon cycle. a range of new technologies will be appli 
9897 1 fect, directly or indirectly, the ocean carbon cycle. a range of new technologies will be appli 
9821 1 the variations in organic molecules and carbon isotopes which tell us more about the climate at 
15344 1 rs measured are useful as indicators of environmental quality in addressing conservation measur 
174 1 t instructions for the studied rare and protected species.  
14135 1 cteria in different nutrient and labile carbon gradients and grazing pressure by zooplankton.  
10013 1                  the issue of ecosystem carbon , eriophorum sp. sphagnum sp. and other bryophyt 
11481 1 es. this results in a high diversity of soil and vegetation in a restricted area. we need to kn 
10975 5  degradation, atmospheric pollution and carbon emission. in this proposal we will focus attenti 
 fire ignition and spread, quantify the carbon emissions and recovery times associated with spe 
2009-2011. 3. measuring the biomass and carbon stocks in unburned and burned forests 4. install 
d and burned forests 4. installing some carbon plots in forests prior to burn, and visiting the 
g calibrated satellite data to estimate carbon emissions from fires across the tropical andes  
11865 2 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 
11683 9 bal production of oxygen and removal of carbon dioxide from the atmosphere each year. due to th 
is an accurate measure of the amount of carbon they take up. phytoplankton carbon fixation can  
t of carbon they take up. phytoplankton carbon fixation can be reasonably well approximated as  
a simplistic treatment of phytoplankton carbon fixation simply as pigment multiplied by light i 
kton convert the light they absorb into carbon varies hugely in the oceans. much of this variab 
nto our best estimates of the amount of carbon fixed each year. the current study aims to addre 
ankton light absorption and the rate of carbon fixation. at the same time we will measure a num 
ty in the ratio of light absorption and carbon fixation. by performing this work we will not on 
current best estimates of phytoplankton carbon fixation.  
10268 3                                         invasive species have been identified by the iucn as th 
owever, the precise mechanisms by which invasive species impact native biodiversity are often p 
sponsibility for uk islands, and to the invasive species community, both within the wider uk an 
13820 3 formance of natural enemies and improve biological control of pests. however, no studies have t 
ld impact on the theory and practise of conservation biological control – and challenge some ex 
s and on insect community structure and biological control at different spatial scales. in the  
12587 4 rganic matter returns will increase the carbon content of arable soils under english and welsh  
een promoted as a means of sequestering carbon in agricultural soils. however, a defra-funded r 
efra-funded review of the potential for carbon sequestration in agricultural soils , including  
efra to develop a clear line on whether carbon sequestration by changed land management practic 
10121 1 terest in the use of such parasites for biological control. sex ratio distortion has evolved in 
11048 1 terest in the use of such parasites for biological control. sex ratio distortion has evolved in 
11567 1 terest in the use of such parasites for biological control. sex ratio distortion has evolved in 
14925 1  applied field of conservation biology. invasive species are nothing more than species that in  
10853 1 volutionary rate generated from the ams carbon-dated specimens, and related to known paleoecolo 
11580 13 fossil fuel burning of large amounts of carbon that has been buried underground for millions of 
years. once back in the atmosphere, the carbon-containing compounds absorb infrared radiation,  
lobal warming is through the removal of carbon containing compounds, such as carbon dioxide to  
of carbon containing compounds, such as carbon dioxide to a range of different soils. we will t 
il, to calculate what proportion of the carbon from ch4 is retained in the soil. we can also li 
er soil microorganisms that utilise the carbon from methane as a source of food, and build up a 
opment work will study a landfill cover soil and focus on establishing a range of new analytica 
s methane but the ultimate fate of this carbon they consume is unknown. the fate of methane car 
consume is unknown. the fate of methane carbon in natural wetlands will also be studied. natura 
ades. we are going to study the fate of carbon from this methane following consumption by metha 
that will be used to assess the fate of carbon from methane in soils are a range of soil chrono 
ment and the soil processes involved in carbon sequestration. overall, the research will add a  
ension our understanding of the fate of carbon from one of the major green house gases as it is 
195 1 managers to learn to recognize the true quality of habitats from the point of view of animals,  
10698 7  the emission of greenhouse gases, like carbon dioxide and methane, are changing global tempera 
atterns. the strong rise in atmospheric carbon dioxide concentrations over the last 100 years i 
lobal storage reservoir for atmospheric carbon dioxide. however, the transfer of this gas from  
on, play an important role in taking up carbon dioxide. upon their death, a part of their popul 
aters and sediments, and hence transfer carbon dioxide from the atmosphere to deep ocean enviro 
ean environments. in the deep ocean the carbon will remain for a long period of time, and there 
eanic organisms play in the exchange of carbon dioxide between the atmosphere and the ocean, an 
10921 1 ospheric constituents and gases such as carbon dioxide, methane, nitrous oxide and dimethylsulp 
11054 1 ospheric constituents and gases such as carbon dioxide, methane, nitrous oxide and dimethylsulp 
11797 1 ospheric constituents and gases such as carbon dioxide, methane, nitrous oxide and dimethylsulp 
11293 3 verall impact of clouds and aerosols on carbon sequestration and evapotranspiration at the vege 
since the 1990s, on global and regional carbon, water and energy exchange. the feasibility stud 
mming exerts a comparable impact on the carbon cycle as that associated with human-induced foss 
12145 2 ight the eutrophication and improve the water quality in natural water reservoirs. there is nei 
ight the eutrophication and improve the water quality.  
11612 1 . this burning of fossil fuels produces carbon dioxide and the whole marine ecosystem. this pro 
12686 1 he need for control of this potentially invasive species, in the context of the emerging policy 
12249 2 ic and international targets, potential air quality benefits, the diversification of the fuel s 
and land management on biodiversity and soil protection, and policy on climate change through s 
12569 1  inform decisions on the development of water quality monitoring programmes that will provide t 
13791 3 ests play a critical role in the global carbon cycle, being considered an important carbon sink 
on cycle, being considered an important carbon sink. yet their net carbon exchange response to  
an important carbon sink. yet their net carbon exchange response to environmental change is a m 
11077 1 efflux, fungal biomass and nitrogen and carbon leaching. this project will establish the extent 
1954 1 n patches that offer a larger reward to pollinators. on the total population level, plants with 
15516 1 lizards, with the contribution of these pollination and seed-dispersal vectors varying greatly  
13458 1 ernatives to traditional pesticides for control of insect pests. tons of synthetic pheromones a 
12579 1 he continued development of policies on soil protection where heavy metals are applied to agric 
12578 1 he continued development of policies on soil protection where sludge is being applied to agricu 
10888 6 n and storm surges. mangroves also trap carbon from the atmosphere in the form of peat, which i 
agement should ensure that below-ground carbon stocks are maintained and that the emission of g 
th focused on a better understanding of carbon cycling and greenhouse gas emissions in mangrove 
hat has started again in kenya, affects carbon stored below the ground and greenhouse gas emiss 
ve there. 2 to determine the sources of carbon dioxide and other greenhouse gases that are lost 
ow quickly such roots can grow and trap carbon. in addition to these main aims, we will also be 
7282 1 , the mechanisms in place to ensure the protection of biodiversity, the institutions in which t 
6999 1 or else, do we have to figure out a new carbon pathway in the sediment system. the proposed stu 
10317 1 nd the major contributors to the global carbon cycle, have already altered their calcification  
11039 2 s the burning of fossil fuels releasing carbon that has been stored for centuries back into the 
l of ceh, parameterising water, energy, carbon and greenhouse gas balances for these bioenergy  
10035 2 s the burning of fossil fuels releasing carbon that has been stored for centuries back into the 
l of ceh, parameterising water, energy, carbon and greenhouse gas balances for these bioenergy  
203 1 he best hybrid aspen clones in estonian soil and climate conditions. the results from the proje 
10484 3 jor component of the marine-atmospheric carbon cycle is the precipitation and dissolution of ca 
tant to our understanding of the global carbon cycle, and to the earth system as a whole. this  
r understanding of the marine inorganic carbon budget. large amounts of calcium carbonate are p 
9959 3 ing the generation of electricity using carbon-based fossil fuels such as oil and gas. in parti 
els such as oil and gas. in particular, carbon dioxide emissions from the deforestation of trop 
eventing the emission of biomass-stored carbon dioxide emissions into the atmosphere. these inc 
11879 3 ion of two ecosystem services, those of pollination and pest control. collaborations between ac 
stem services, those of pollination and pest control. collaborations between academics and prac 
llows and a £1.3 million grant on urban pollinators led by memmott. at the somerset wildlife tr 
14148 1 a knowledge base for better planning of habitat protection and a more accurate determination of 
14217 5                                         plant-pollinator interactions are crucial in the functi 
 by altering plant traits important for pollinators, and consequently, how these effects are tr 
lative effects of floral herbivores and pollinators on individual plant fitness and quantify th 
ctive pressure by floral herbivores and pollinators on flower traits. based on simultaneous ana 
servation strategies for rare plant and pollinator species.  
11023 2 ave a different impact on the amount of carbon dioxide removed from the atmosphere and locked u 
different amount of resources including carbon and nutrients . subsequently the kinds of pigmen 
11277 12 st ice age large amounts of atmospheric carbon dioxide have been slowly locked up in peat soils 
lant remains. if this huge reservoir of carbon was to be released back in to the atmosphere it  
re it would cause a significant rise in carbon dioxide and release methane and result in furthe 
ms that control the losses and gains of carbon from this large area of the earth s surface. pea 
route to connect the large reservoir of carbon stored in peats to peatland pools and streams, a 
ms, and may act as pathways along which carbon can leak away. we aim to investigate how pipes c 
how pipes control the loss of water and carbon from peatlands. most of the research work, which 
 a catchment that has been designated a carbon study catchment by the centre for ecology and hy 
uring the concentrations and amounts of carbon and water flowing in pipes and streams. we will  
at allow us to determine the age of the carbon being released and therefore where in the peat t 
sed and therefore where in the peat the carbon is coming from. the overall aim of our work is t 
h affect this important global store of carbon.  
11301 12 st ice age large amounts of atmospheric carbon dioxide have been slowly locked up in peat soils 
lant remains. if this huge reservoir of carbon was to be released back in to the atmosphere it  
re it would cause a significant rise in carbon dioxide and release methane and result in furthe 
ms that control the losses and gains of carbon from this large area of the earth s surface. pea 
route to connect the large reservoir of carbon stored in peats to peatland pools and streams, a 
ms, and may act as pathways along which carbon can leak away. we aim to investigate how pipes c 
how pipes control the loss of water and carbon from peatlands. most of the research work, which 
 a catchment that has been designated a carbon study catchment by the centre for ecology and hy 
uring the concentrations and amounts of carbon and water flowing in pipes and streams. we will  
at allow us to determine the age of the carbon being released and therefore where in the peat t 
sed and therefore where in the peat the carbon is coming from. the overall aim of our work is t 
h affect this important global store of carbon.  
11837 12 st ice age large amounts of atmospheric carbon dioxide have been slowly locked up in peat soils 
lant remains. if this huge reservoir of carbon was to be released back in to the atmosphere it  
re it would cause a significant rise in carbon dioxide and release methane and result in furthe 
ms that control the losses and gains of carbon from this large area of the earth s surface. pea 
route to connect the large reservoir of carbon stored in peats to peatland pools and streams, a 
ms, and may act as pathways along which carbon can leak away. we aim to investigate how pipes c 
how pipes control the loss of water and carbon from peatlands. most of the research work, which 
 a catchment that has been designated a carbon study catchment by the centre for ecology and hy 
uring the concentrations and amounts of carbon and water flowing in pipes and streams. we will  
at allow us to determine the age of the carbon being released and therefore where in the peat t 
sed and therefore where in the peat the carbon is coming from. the overall aim of our work is t 
h affect this important global store of carbon.  
9801 1 w, plants use light to turn atmospheric carbon dioxide into sugars, in a process called photosy 
14877 2  this project is to study the effect of pollinator shifts on morphological variations of flower 
d with an increase of the efficiency of pollinators in pollen transfer between stylar morphs.  
14878 2  this project is to study the effect of pollinator shifts on morphological variations of flower 
ies, or even due to the virtual lack of pollinators.  
13981 1 g term changes in conditions related to soil and climate may impact on these habitats. two basi 
10631 2 ntribute almost a half of annual global carbon fixation. the phytoplankton can be divided into  
e is an important parameter in terms of carbon turnover, nutrient uptake and efficiency of trop 
10606 2 dification and resource productivity on pollinator-parasite community structure will be studied 
ood webs of flowering plants, bumblebee pollinators and their parasites will be constructed for 
12529 1 agriculture and the environment through pollination: they also produce honey and wax and also p 
10874 2 years. the importance of bumblebees for crop pollination means their declines are of economic a 
om continental europe each year for the pollination of greenhouse crops, and these potentially  
12636 1  according to the thematic strategy for soil protection . we will explore options for stratifyi 
15313 1                            biochar is a carbon-rich product obtained by thermal decomposition o 
15066 1 iterranean.presence of a.franciscana as invasive species. implications, supported by mec for th 
13858 1 types. to meet the overall objective of disease control, research will be directed to the follo 
11298 6 northern hermisphere and act as a major carbon sink, currently storing some 11% of the earth s  
rrently storing some 11% of the earth s carbon, locked away in the organic soils and peat of ar 
 determine the balance, and exchange of carbon between land surface and atmosphere so as to bet 
is is particularly the case in terms of carbon in the form of methane. methane is a powerful gr 
ay an important dual role in the global carbon cycle, being both the largest natural methane so 
 natural methane source and a large net carbon sink . key strengths of the current proposal are 
11112 3 bal oceanic productivity and/or organic carbon preservation potential oaes are hence important  
 in regulating the short- and long-term carbon cycle, and subsequently co2 levels in the oceans 
and their subsequent role in the global carbon cycle.  
15168 1 imilar to spanish ones, and most of the invasive species are associated with this cultural scen 
13720 2 system composition, and ultimately e.g. water quality, fisheries productivity and biological ri 
ystems, that may determine e.g. shallow lake water quality, productivity and species compositio 
11288 1 ations, bacteria can use sulphur to fix carbon for energy. this is known as chemosynthesis and  
14467 1  management practice and control of the water quality in bulgaria.  
10157 2 cal rainforests are a major terrestrial carbon store and are currently estimated to account for 
r around half of the global terrestrial carbon sink. although rainfall is a key determinant aff 
10174 2 cal rainforests are a major terrestrial carbon store and are currently estimated to account for 
r around half of the global terrestrial carbon sink. although rainfall is a key determinant aff 
10426 2 cal rainforests are a major terrestrial carbon store and are currently estimated to account for 
r around half of the global terrestrial carbon sink. although rainfall is a key determinant aff 
11426 2 cal rainforests are a major terrestrial carbon store and are currently estimated to account for 
r around half of the global terrestrial carbon sink. although rainfall is a key determinant aff 
11711 2 cal rainforests are a major terrestrial carbon store and are currently estimated to account for 
r around half of the global terrestrial carbon sink. although rainfall is a key determinant aff 
11712 2 cal rainforests are a major terrestrial carbon store and are currently estimated to account for 
r around half of the global terrestrial carbon sink. although rainfall is a key determinant aff 
10351 4                 the unstable isotope of carbon, 14c or radiocarbon, is produced via the interac 
sphere and ocean, a dynamic terrestrial carbon cycle, and a detailed representation of the ocea 
 a detailed representation of the ocean carbon cycle, and is capable of multi-millennial simula 
rstanding of the changes in climate and carbon cycling.  
10831 1 f tropospheric o3 that will help tackle air quality problems and perhaps minimize its role in f 
10133 1  of breeding seabirds who fertilise the soil and disturb the vegetation through burrowing and t 
13770 1 iated with fragmentation, isolation and habitat quality at a landscape scale. the project also  
10624 5 ntial for ecm fungi to influence forest carbon cycles has become clear. they play a fundamental 
cing both sequestration and emission of carbon from soil. ecm species are likely to respond dif 
in the way they partition plant-derived carbon between biomass and respiration. changes in ecm  
al mycelium produced, may influence the carbon balance of forest ecosystems and have important  
acks on nutrient capture. we will study carbon partitioning of ecm fungi with contrasting ecolo 
11292 4 ng in response to increased atmospheric carbon dioxide from the burning of fossil fuels. such r 
of carbonate, bicarbonate and dissolved carbon dioxide and ph in the surface ocean, which is ch 
quence of rapid increase in atmospheric carbon dioxide. organisms which produce external calciu 
patterns in relation to ocean inorganic carbon chemistry and will allow us to construct better  
11586 6 ority of these cases the plant supplies carbon, which it has fixed through photosynthesis, to t 
 the fungus supplies both nutrients and carbon to the young plants without any obvious benefit  
ctions between orchid and fungus. using carbon, nitrogen and phosphorus sources enriched with s 
een orchids behave in this way, how the carbon and nutrients are transferred between plant and  
ungus and whether being able to acquire carbon from a fungus has enabled some adult orchids to  
ons where they are unable to fix enough carbon into sugars to meet their needs and effectively  
10065 1     the rate of increase in atmospheric carbon dioxide programmes.  
11599 7  releases significant amounts of fossil carbon and can have a profound effect on total uk emmis 
s and a potential imbalance between the carbon lost from burnt vegetation and that which can be 
mate, fire frequency, fire severity and carbon fluxes from peatlands. for this reason there is  
th regards to moorland biodiversity and carbon stores. this research will play an important rol 
everities on the above and below ground carbon balance and ecosystem functioning of moorlands.  
l make estimates of the total amount of carbon lost from the system due to combustion and asses 
ferences in vegetation regeneration and carbon fluxes from peat in burnt and unburnt plots. by  
15330 1 lants, an improved understanding of the carbon balance of plants and of phloem transport and th 
15526 1 communities, including the dominance of invasive species and their biotic integrity. the findin 
13744 1  and community structure in relation to local habitat quality and matrix quality at multiple sc 
11770 1 occurs as a result of fishing. for such species protection in marine reserves, which will maint 
9958 1 m altered rates of nutrient cycling and carbon storage to changes in plant community compositio 
7248 1 epth, the deeper horizons are richer in carbon stable. more test closeaux involving a change of 
7252 2 tted to an emission reduction schedule. carbon dioxide is particularly referred. its main produ 
mal feed, fish, food, soil improvement, crop protection,.... by selected applications, addition 
153 2 itat. 4. what are the relations between pollinators and the composition of plant communities an 
tween the environmental requirements of pollinators and landscape structure. as the result of t 
2161 1 xperiment addressing the possibility of biocontrol by predator enhancement. ecological impacts  
1106 3 face; - to improve the understanding of carbon cycle processes, that are affected by global cha 
garding the behaviour of the ocean like carbon sink; - to provide data on the role of national  
he role of national seas in relation to carbon stocks usable for international negotiations. ne 
12293 1 d identifying osr-infecting isolates in soil and in planta. identification of infection can be  
2463 1 uction, plays a critical role in global carbon cycling. mechanisms that control their mortality 
10601 1 oplankton are central players in global carbon fixation, nutrient cycling and energy transfer.  
15574 1 s that respond to management and affect carbon and nitrogen turnover. wp3 will then build multi 
12583 4 soils will be reviewed of the potential carbon that could be removed from the atmosphere and st 
d from the atmosphere and stored by the soil and the reduction in carbon losses that could be p 
stored by the soil and the reduction in carbon losses that could be possible through mitigation 
 provide guidance on the most promising soil protection schemes in the uk.  
10145 1 s living in river basins, providing for flood storage and waste disposal. river basin landscape 
10979 1 s living in river basins, providing for flood storage and waste disposal. river basin landscape 
10870 1 nowledge to integrate the management of water quality and quantity in the environment. this gra 
14859 1 ch as canadian thistle, one of the most invasive species in dryland crops.  
11732 1 recently established that the fluxes of carbon and water from tropical rain forests exhibit str 
11860 2 ing their growth and role in the marine carbon cycle. the aim of this project is to address the 
phore ecology, their role in the marine carbon cycle and their future in a changing climate.  
10014 1 t will determine the influence of plant carbon flow on the location of production of nitrous ox 
10658 1  to 70 years. a marked deterioration in water quality has been observed in the last 10 to 15 ye 
9901 1  to 70 years. a marked deterioration in water quality has been observed in the last 10 to 15 ye 
10122 2 phores plays a major role in the global carbon cycle and climate change may have a significant  
isition of nutrients and as a source of carbon for photosynthesis, but definitive evidence for  
10355 2  change and their potential as sinks of carbon dioxide. we have recently discovered that mature 
es, but have to spend higher amounts of carbon on respiration, or allocate more to fine roots,  
10747 2  change and their potential as sinks of carbon dioxide. we have recently discovered that mature 
es, but have to spend higher amounts of carbon on respiration, or allocate more to fine roots,  
9976 2  change and their potential as sinks of carbon dioxide. we have recently discovered that mature 
es, but have to spend higher amounts of carbon on respiration, or allocate more to fine roots,  
12162 1 ed with entry level stewardship address natural resource protection such as the integrity and h