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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>Stefan F. Hupperts</dc:contributor>
  <dc:contributor>Sandra Jämtgård</dc:contributor>
  <dc:contributor>Lars Östlund</dc:contributor>
  <dc:contributor>Jonas Fridman</dc:contributor>
  <dc:contributor>Steven S. Perakis</dc:contributor>
  <dc:contributor>Michael J. Gundale</dc:contributor>
  <dc:creator>Kelley R. Bassett</dc:creator>
  <dc:date>2026</dc:date>
  <dc:description>&lt;p&gt;Anthropogenic nitrogen (N) pollution has been emphasized as a cause of eutrophication globally. However, several recent datasets have suggested widespread oligotrophication may be occurring in some ecosystems, which is suggested to be a response to rising atmospheric carbon dioxide (eCO&lt;sub&gt;2&lt;/sub&gt;). Plant δ&lt;sup&gt;15&lt;/sup&gt;N chronologies have served as primary evidence for oligotrophication, however, there has been wide disagreement whether eCO&lt;sub&gt;2 &lt;/sub&gt;or temporal changes in N deposition explain these patterns. We constructed δ&lt;sup&gt;15&lt;/sup&gt;N tree ring chronologies across Sweden’s 23.5 million hectare productive forest area from the 1950s to 2010s. The study area spans a 1500 km latitudinal distance where N deposition varies four-fold, but where eCO&lt;sub&gt;2&lt;/sub&gt; is spatially uniform. Our data revealed negative δ&lt;sup&gt;15&lt;/sup&gt;N chronologies throughout Sweden, including forests in the far north where atmospheric N deposition rates are very low. Linear mixed effects models showed that eCO&lt;sub&gt;2&lt;/sub&gt; was by far the strongest predictor of δ&lt;sup&gt;15&lt;/sup&gt;N values, whereas N deposition variables, temperature, and forest basal area had much lower explanatory power. Our results clarify debates on the interpretation of previous δ&lt;sup&gt;15&lt;/sup&gt;N chronologies, and provide clear evidence that eCO&lt;sub&gt;2&lt;/sub&gt; is causing oligotrophication in boreal forests, which has implications for predicting their future role as sinks in the global carbon cycle.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1038/s41586-025-10039-5</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer Nature</dc:publisher>
  <dc:title>Rising atmospheric CO2 reduces nitrogen availability in boreal forests</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>