<?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>Jason B. Fellman</dc:contributor>
  <dc:contributor>J. Ryan Bellmore</dc:contributor>
  <dc:contributor>Emily J. Whitney</dc:contributor>
  <dc:contributor>Eran Hood</dc:contributor>
  <dc:contributor>Kevin Fitzgerald</dc:contributor>
  <dc:contributor>Jeffrey A. Falke</dc:contributor>
  <dc:creator>Claire Delbecq</dc:creator>
  <dc:date>2024</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Riverine export of carbon (C) is an important part of the global C cycle; however, most riverine C budgets focus on individual forms of C and fail to comprehensively measure both organic and inorganic C species in concert. To address this knowledge gap, we conducted high frequency sampling of multiple C forms, including dissolved organic C (DOC), inorganic carbon (as alkalinity), particulate organic C (POC), coarse particulate organic C (CPOC), and invertebrate biomass C across the main run-off season in a predominantly rain-fed watershed in Southeast Alaska. Streamwater concentrations were used to model daily watershed C export from May through October. Concentration and modeled yield data indicated that DOC was the primary form of riverine C export (8708&amp;nbsp;kg C/km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;), except during low flow periods when alkalinity (3125&amp;nbsp;kg C/km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;) was the dominant form of C export. Relative to DOC and alkalinity, export of particulate organic C (POC: 992&amp;nbsp;kg C/km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;; CPOC: 313&amp;nbsp;kg C/km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;) and invertebrates (40&amp;nbsp;kg C/km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;) was small, but these forms of organic matter could disproportionately impact downstream food webs because of their higher quality, assessed via C to nitrogen ratios. These seasonal and flow driven changes to C form and export likely provide subsidies to downstream and nearshore ecosystems such that predicted shifts in regional hydroclimate could substantially impact C transfer and incorporation into aquatic food webs.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s10533-024-01175-7</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer Nature</dc:publisher>
  <dc:title>Seasonal patterns in riverine carbon form and export from a temperate forested watershed in Southeast Alaska</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>