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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>Michael P. Carey</dc:contributor>
  <dc:contributor>Joshua C. Koch</dc:contributor>
  <dc:contributor>Xiaomei Xu</dc:contributor>
  <dc:contributor>Brett Poulin</dc:contributor>
  <dc:contributor>Jennifer Walker</dc:contributor>
  <dc:contributor>Christian E. Zimmerman</dc:contributor>
  <dc:creator>Jonathon A O'Donnell</dc:creator>
  <dc:date>2020</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Permafrost thaw in the Arctic is mobilizing old carbon (C) from soils to aquatic ecosystems and the atmosphere. Little is known, however, about the assimilation of old C by aquatic food webs in Arctic watersheds. Here, we used C isotopes (δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C, Δ&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;&lt;span&gt;C) to quantify C assimilation by biota across 12 streams in arctic Alaska. Streams spanned watersheds with varying permafrost hydrology, from ice-poor bedrock to ice-rich loess (that is, yedoma). We measured isotopic content of (1) C sources including dissolved organic C (DOC), dissolved inorganic C (DIC), and soil C, and (2) stream biota, including benthic biofilm and macroinvertebrates, and resident fish species (Arctic Grayling (&lt;/span&gt;&lt;i&gt;Thymallus arcticus&lt;/i&gt;&lt;span&gt;) and Dolly Varden (&lt;/span&gt;&lt;i&gt;Salvelinus malma&lt;/i&gt;&lt;span&gt;)). Findings document the assimilation of old C by stream biota, with depleted Δ&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;&lt;span&gt;C values observed at multiple trophic levels, including benthic biofilm (&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;&lt;span&gt;C ages = 5255 to 265&amp;nbsp;years before present (y BP)), macroinvertebrates (4490 y BP to modern), and fish (3195 y BP to modern). Mixing model results indicate that DOC and DIC contribute to benthic biofilm composition, with relative contributions differing across streams draining ice-poor and ice-rich terrain. DOC originates primarily from old terrestrial C sources, including deep peat horizons (39–47%; 530 y BP) and near-surface permafrost (12–19%; 5490 y BP). DOC also accounts for approximately half of fish isotopic composition. Analyses suggest that as the contribution of old C to fish increases, fish growth and nutritional status decline. We anticipate increases in old DOC delivery to streams under projected warming, which may further alter food web function in Arctic watersheds.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s10021-019-00413-6</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>Permafrost hydrology drives the assimilation of old carbon by stream food webs in the Arctic</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>