<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/10.1007/s10021-010-9363-0">
    <dct:isReferencedBy>IMPACT4SOIL</dct:isReferencedBy>
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    <dct:isPartOf>Ecosystems</dct:isPartOf>
    <dct:license>Closed Access</dct:license>
    <dct:created>2010-07-22</dct:created>
    <dct:available>2020-05-30</dct:available>
    <dc:description>Future climate scenarios predict simultaneous changes in environmental conditions, but the impacts of multiple climate change drivers on ecosystem structure and function remain unclear. We used a novel experimental approach to examine the responses of an upland grassland ecosystem to the 2080 climate scenario predicted for the study area (3.5A degrees C temperature increase, 20% reduction in summer precipitation, atmospheric CO2 levels of 600 ppm) over three growing seasons. We also assessed whether patterns of grassland response to a combination of climate change treatments could be forecast by ecosystem responses to single climate change drivers. Effects of climate change on aboveground production showed considerable seasonal and interannual variation; April biomass increased in response to both warming and the simultaneous application of warming, summer drought, and CO2 enrichment, whereas October biomass responses were either non-significant or negative depending on the year. Negative impacts of summer drought on production were only observed in combination with a below-average rainfall regime, and showed lagged effects on spring biomass. Elevated CO2 had no significant effect on aboveground biomass during this study. Both warming and the 2080 climate change scenario were associated with a significant advance in flowering time for the dominant grass species studied. However, flowering phenology showed no significant response to either summer drought or elevated CO2. Species diversity and equitability showed no response to climate change treatments throughout this study. Overall, our data suggest that single-factor warming experiments may provide valuable information for projections of future ecosystem changes in cool temperate grasslands.</dc:description>
    <dc:subject>free air CO2 enrichment</dc:subject>
    <dc:subject>0106 biological sciences</dc:subject>
    <dc:subject>2. Zero hunger</dc:subject>
    <dc:subject>interannual variation</dc:subject>
    <dc:subject>vegetation dynamics</dc:subject>
    <dc:subject>[SDV]Life Sciences [q-bio]</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>01 natural sciences</dc:subject>
    <dc:subject>6. Clean water</dc:subject>
    <dc:subject>[SDV] Life Sciences [q-bio]</dc:subject>
    <dc:subject>climate change</dc:subject>
    <dc:subject>13. Climate action</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>grassland productivity</dc:subject>
    <dc:subject>biodiversity</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-8668-1323"/>
    <dc:creator>Bloor, Juliette, Pichon, Patrick, Falcimagne, Robert, Leadley, Paul, Soussana, Jean-Fran&#231;ois, </dc:creator>
    <dc:date>2010-07-23</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>Future climate scenarios predict simultaneous changes in environmental conditions, but the impacts of multiple climate change drivers on ecosystem structure and function remain unclear. We used a novel experimental approach to examine the responses of an upland grassland ecosystem to the 2080 climate scenario predicted for the study area (3.5A degrees C temperature increase, 20% reduction in summer precipitation, atmospheric CO2 levels of 600 ppm) over three growing seasons. We also assessed whether patterns of grassland response to a combination of climate change treatments could be forecast by ecosystem responses to single climate change drivers. Effects of climate change on aboveground production showed considerable seasonal and interannual variation; April biomass increased in response to both warming and the simultaneous application of warming, summer drought, and CO2 enrichment, whereas October biomass responses were either non-significant or negative depending on the year. Negative impacts of summer drought on production were only observed in combination with a below-average rainfall regime, and showed lagged effects on spring biomass. Elevated CO2 had no significant effect on aboveground biomass during this study. Both warming and the 2080 climate change scenario were associated with a significant advance in flowering time for the dominant grass species studied. However, flowering phenology showed no significant response to either summer drought or elevated CO2. Species diversity and equitability showed no response to climate change treatments throughout this study. Overall, our data suggest that single-factor warming experiments may provide valuable information for projections of future ecosystem changes in cool temperate grasslands.</dct:abstract>
    <dc:title>Effects Of Warming, Summer Drought, And Co2 Enrichment On Aboveground Biomass Production, Flowering Phenology, And Community Structure In An Upland Grassland Ecosystem</dc:title>
    <dc:identifier>10.1007/s10021-010-9363-0</dc:identifier>
    <dct:references>https://doi.org/10.1007/s10021-010-9363-0</dct:references>
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