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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Jayne Belnap</dc:contributor>
  <dc:contributor>Sasha C. Reed</dc:contributor>
  <dc:creator>Timothy M. Wertin</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;p&gt;1. Drylands represent our planet's largest terrestrial biome and, due to their extensive area, maintain large stocks of carbon (C). Accordingly, understanding how dryland C cycling will respond to climate change is imperative for accurately forecasting global C cycling and future climate. However, it remains difficult to predict how increased temperature will affect dryland C cycling, as substantial uncertainties surround the potential responses of the two main C fluxes: plant photosynthesis and soil CO&lt;sub&gt;2&lt;/sub&gt; efflux. In addition to a need for an improved understanding of climate effects on individual dryland C fluxes, there is also notable uncertainty regarding how climate change may influence the relationship between these fluxes.&lt;/p&gt;&lt;p&gt;2. To address this important knowledge gap, we measured a growing season's &lt;i&gt;in situ&lt;/i&gt;photosynthesis, plant biomass accumulation, and soil CO&lt;sub&gt;2&lt;/sub&gt; efflux of mature &lt;i&gt;Achnatherum hymenoides&lt;/i&gt; (a common and ecologically important C&lt;sub&gt;3&lt;/sub&gt; bunchgrass growing throughout western North America) exposed to ambient or elevated temperature (+2°C above ambient, warmed via infrared lamps) for three years.&lt;/p&gt;&lt;p&gt;3. The 2°C increase in temperature caused a significant reduction in photosynthesis, plant growth, and soil CO&lt;sub&gt;2&lt;/sub&gt; efflux. Of important note, photosynthesis and soil respiration appeared tightly coupled and the relationship between these fluxes was not altered by the elevated temperature treatment, suggesting C fixation's strong control of both above-ground and below-ground dryland C cycling. Leaf water use efficiency was substantially increased in the elevated temperature treatment compared to the control treatment.&lt;/p&gt;&lt;p&gt;4. Taken together, our results suggest notable declines in photosynthesis with relatively subtle warming, reveal strong coupling between above- and below-ground C fluxes in this dryland, and highlight temperature's strong effect on fundamental components of dryland C and water cycles.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/1365-2435.12708</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>Experimental warming in a dryland community reduced plant photosynthesis and soil CO&lt;sub&gt;2&lt;/sub&gt; efflux although the relationship between the fluxes remained unchanged</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>