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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>Gregory B. Noe</dc:contributor>
  <dc:contributor>Jamie A. Duberstein</dc:contributor>
  <dc:contributor>William H. Conner</dc:contributor>
  <dc:contributor>Camille L. Stagg</dc:contributor>
  <dc:contributor>Nicole Cormier</dc:contributor>
  <dc:contributor>Miriam C. Jones</dc:contributor>
  <dc:contributor>Christopher E. Bernhardt</dc:contributor>
  <dc:contributor>B. Graeme Lockaby</dc:contributor>
  <dc:contributor>Andrew S. From</dc:contributor>
  <dc:contributor>Thomas W. Doyle</dc:contributor>
  <dc:contributor>Richard H. Day</dc:contributor>
  <dc:contributor>Scott H. Ensign</dc:contributor>
  <dc:contributor>Katherine N. Pierfelice</dc:contributor>
  <dc:contributor>Cliff R. Hupp</dc:contributor>
  <dc:contributor>Alex T. Chow</dc:contributor>
  <dc:contributor>Julie L. Whitbeck</dc:contributor>
  <dc:creator>Ken W. Krauss</dc:creator>
  <dc:date>2018</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Carbon (C) standing stocks, C mass balance, and soil C burial in tidal freshwater forested wetlands (TFFW) and TFFW transitioning to low‐salinity marshes along the upper estuary are not typically included in “blue carbon” accounting, but may represent a significant C sink. Results from two salinity transects along the tidal Waccamaw and Savannah rivers of the US Atlantic Coast show total C standing stocks were 321‐1264 Mg C ha&lt;/span&gt;&lt;sup&gt;‐1&lt;/sup&gt;&lt;span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;among all sites, generally shifting to greater soil storage as salinity increased. Carbon mass balance inputs (litterfall, woody growth, herbaceous growth, root growth, surface accumulation) minus C outputs (surface litter and root decomposition, gaseous C) over a period of up to 11 years were 340‐900 g C m&lt;/span&gt;&lt;sup&gt;‐2&lt;/sup&gt;&lt;span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;yr&lt;/span&gt;&lt;sup&gt;‐1&lt;/sup&gt;&lt;span&gt;. Soil C burial was variable (7‐337 g C m&lt;/span&gt;&lt;sup&gt;‐2&lt;/sup&gt;&lt;span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;yr&lt;/span&gt;&lt;sup&gt;‐1&lt;/sup&gt;&lt;span&gt;), and lateral C export was estimated as C mass balance minus soil C burial as 267‐849 g C m&lt;/span&gt;&lt;sup&gt;‐2&lt;/sup&gt;&lt;span&gt;yr&lt;/span&gt;&lt;sup&gt;‐1&lt;/sup&gt;&lt;span&gt;. This represents a large amount of C export to support aquatic biogeochemical transformations. Despite reduced C persistence within emergent vegetation, decomposition of organic matter, and higher lateral C export, total C storage increased as forests converted to marsh with salinization. These tidal river wetlands exhibited high N mineralization in salinity‐stressed forested sites and considerable P mineralization in low salinity marshes. Large C standing stocks and rates of C sequestration suggest that TFFW and oligohaline marshes are considerably important globally to coastal C dynamics and in facilitating energy transformations in areas of the world in which they occur.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2018GB005897</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>AGU</dc:publisher>
  <dc:title>The role of the upper tidal estuary in wetland blue carbon storage and flux</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>