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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>Daniel E. Winkler</dc:contributor>
  <dc:contributor>Robin H. Reibold</dc:contributor>
  <dc:contributor>Brooke Bossert Osborne</dc:contributor>
  <dc:contributor>Sasha C. Reed</dc:contributor>
  <dc:creator>Michala Lee Phillips</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;div id="Abs1-section" class="c-article-section"&gt;&lt;div id="Abs1-content" class="c-article-section__content"&gt;&lt;p&gt;Anthropogenic nitrogen (N) deposition is significantly altering both community structure and ecosystem processes in terrestrial ecosystems across the globe. However, our understanding of the consequences of N deposition in dryland systems remains relatively poor, despite evidence that drylands may be particularly vulnerable to increasing N inputs. In this study, we investigated the influence of 7 years of multiple levels of simulated N deposition (0, 2, 5, and 8&amp;nbsp;kg&amp;nbsp;N&amp;nbsp;ha&lt;sup&gt;−1&lt;/sup&gt;&amp;nbsp;year&lt;sup&gt;−1&lt;/sup&gt;) on plant community structure and biological soil crust (biocrust) cover at three semi-arid grassland sites spanning a soil texture gradient. Biocrusts are a surface community of mosses, lichens, cyanobacteria, and/or algae, and have been shown to be sensitive to N inputs. We hypothesized that N additions would decrease plant diversity, increase abundance of the invasive annual grass&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Bromus tectorum,&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;and decrease biocrust cover. Contrary to our expectations, we found that N additions did not affect plant diversity or&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;B. tectorum&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;abundance. In partial support of our hypotheses, N additions negatively affected biocrust cover in some years, perhaps driven in part by inter-annual differences in precipitation. Soil inorganic N concentrations showed rapid but ephemeral responses to N additions and plant foliar N concentrations showed no response, indicating that the magnitude of plant and biocrust responses to N fertilization may be buffered by endogenous N cycling. More work is needed to determine N critical load thresholds for plant community and biocrust dynamics in semi-arid systems and the factors that determine the fate of N inputs.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;div id="cobranding-and-download-availability-text" class="note test-pdf-link"&gt;&lt;br&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s00442-020-04841-3</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>Muted responses to chronic experimental nitrogen deposition on the Colorado Plateau</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>