<?xml version='1.0' encoding='utf-8'?>
<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>Jeffery M. Warren</dc:contributor>
  <dc:contributor>Peter B. Reich</dc:contributor>
  <dc:contributor>Eric Ward</dc:contributor>
  <dc:contributor>Bridget K. Murphy</dc:contributor>
  <dc:contributor>Artur Stefanski</dc:contributor>
  <dc:contributor>Raimundo Bermudez</dc:contributor>
  <dc:contributor>Marisol Cruz</dc:contributor>
  <dc:contributor>David A. McLennan</dc:contributor>
  <dc:contributor>Anthony W. King</dc:contributor>
  <dc:contributor>Rebecca A. Montgomery</dc:contributor>
  <dc:contributor>Paul J. Hanson</dc:contributor>
  <dc:contributor>Danielle A. Way</dc:contributor>
  <dc:creator>Mirindi E. Dusenge</dc:creator>
  <dc:date>2023</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Warming shifts the thermal optimum of net photosynthesis (&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;optA&lt;/sub&gt;&lt;span&gt;) to higher temperatures. However, our knowledge of this shift is mainly derived from seedlings grown in greenhouses under ambient atmospheric carbon dioxide (CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;) conditions. It is unclear whether shifts in&amp;nbsp;&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;optA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;of field-grown trees will keep pace with the temperatures predicted for the 21&lt;/span&gt;&lt;sup&gt;st&lt;/sup&gt;&lt;span&gt;&amp;nbsp;century under elevated atmospheric CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;concentrations. Here, using a whole-ecosystem warming controlled experiment under either ambient or elevated CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;levels, we show that&amp;nbsp;&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;optA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;of mature boreal conifers increased with warming. However, shifts in&amp;nbsp;&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;optA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;did not keep pace with warming as&amp;nbsp;&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;optA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;only increased by 0.26–0.35 °C per 1 °C of warming. Net photosynthetic rates estimated at the mean growth temperature increased with warming in elevated CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;spruce, while remaining constant in ambient CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;spruce and in both ambient CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;and elevated CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;tamarack with warming. Although shifts in&amp;nbsp;&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;optA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;of these two species are insufficient to keep pace with warming, these boreal conifers can thermally acclimate photosynthesis to maintain carbon uptake in future air temperatures.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1038/s41467-023-40248-3</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Nature</dc:publisher>
  <dc:title>Boreal conifers maintain carbon uptake with warming despite failure to track optimal temperatures</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>