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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>J. Renee Brooks</dc:contributor>
  <dc:contributor>Frederick C. Meinzer</dc:contributor>
  <dc:contributor>Rebecca Anderson</dc:contributor>
  <dc:contributor>Martin K.-F. Bader</dc:contributor>
  <dc:contributor>Giovanna Battipaglia</dc:contributor>
  <dc:contributor>Katie M. Becklin</dc:contributor>
  <dc:contributor>David Beerling</dc:contributor>
  <dc:contributor>Didier Bert</dc:contributor>
  <dc:contributor>Julio L. Betancourt</dc:contributor>
  <dc:contributor>Todd E. Dawson</dc:contributor>
  <dc:contributor>Jean-Christophe Domec</dc:contributor>
  <dc:contributor>Richard P. Guyette</dc:contributor>
  <dc:contributor>Christian Korner</dc:contributor>
  <dc:contributor>Steven W. Leavitt</dc:contributor>
  <dc:contributor>Sune Linder</dc:contributor>
  <dc:contributor>John D. Marshall</dc:contributor>
  <dc:contributor>Manuel Mildner</dc:contributor>
  <dc:contributor>Jerome Ogee</dc:contributor>
  <dc:contributor>Irina P. Panyushkina</dc:contributor>
  <dc:contributor>Heather J. Plumpton</dc:contributor>
  <dc:contributor>Kurt S. Pregitzer</dc:contributor>
  <dc:contributor>Matthias Saurer</dc:contributor>
  <dc:contributor>Andrew R. Smith</dc:contributor>
  <dc:contributor>Rolf T.W. Siegwolf</dc:contributor>
  <dc:contributor>Michael C. Stambaugh</dc:contributor>
  <dc:contributor>Alan F. Talhelm</dc:contributor>
  <dc:contributor>Jacques C. Tardif</dc:contributor>
  <dc:contributor>Peter K. Van De Water</dc:contributor>
  <dc:contributor>Joy K. Ward</dc:contributor>
  <dc:contributor>Lisa Wingate</dc:contributor>
  <dc:creator>Steven L. Voelker</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Rising atmospheric [CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;], &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;, is expected to affect stomatal regulation of leaf gas-exchange of woody plants, thus influencing energy fluxes as well as carbon (C), water, and nutrient cycling of forests. Researchers have proposed various strategies for stomatal regulation of leaf gas-exchange that include maintaining a constant leaf internal [CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;], &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt;, a constant drawdown in CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;(&lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;&amp;nbsp;−&amp;nbsp;&lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt;), and a constant &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt;/&lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;. These strategies can result in drastically different consequences for leaf gas-exchange. The accuracy of Earth systems models depends in part on assumptions about generalizable patterns in leaf gas-exchange responses to varying &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;. The concept of optimal stomatal behavior, exemplified by woody plants shifting along a continuum of these strategies, provides a unifying framework for understanding leaf gas-exchange responses to &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;. To assess leaf gas-exchange regulation strategies, we analyzed patterns in &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt; inferred from studies reporting C stable isotope ratios (δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C) or photosynthetic discrimination (∆) in woody angiosperms and gymnosperms that grew across a range of &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt; spanning at least 100&amp;nbsp;ppm. Our results suggest that much of the &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;-induced changes in &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt;/&lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt; occurred across &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt; spanning 200 to 400&amp;nbsp;ppm. These patterns imply that &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;&amp;nbsp;−&amp;nbsp;&lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt; will eventually approach a constant level at high &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt; because assimilation rates will reach a maximum and stomatal conductance of each species should be constrained to some minimum level. These analyses are not consistent with canalization toward any single strategy, particularly maintaining a constant &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;i&lt;/sub&gt;&lt;span&gt;. Rather, the results are consistent with the existence of a broadly conserved pattern of stomatal optimization in woody angiosperms and gymnosperms. This results in trees being profligate water users at low &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;, when additional water loss is small for each unit of C gain, and increasingly water-conservative at high &lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;sub&gt;a&lt;/sub&gt;&lt;span&gt;, when photosystems are saturated and water loss is large for each unit C gain.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/gcb.13102</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Blackwell Science</dc:publisher>
  <dc:title>A dynamic leaf gas-exchange strategy is conserved in woody plants under changing ambient CO&lt;sub&gt;2&lt;/sub&gt;: evidence from carbon isotope discrimination in paleo and CO&lt;sub&gt;2&lt;/sub&gt; enrichment studies</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>