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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>Siyuan Ye</dc:contributor>
  <dc:contributor>Liujuan Xie</dc:contributor>
  <dc:contributor>Ken Krauss</dc:contributor>
  <dc:contributor>Lixin Pei</dc:contributor>
  <dc:contributor>Samantha K. Chapman</dc:contributor>
  <dc:contributor>Hans Brix</dc:contributor>
  <dc:contributor>Edward A. Laws</dc:contributor>
  <dc:contributor>Hongming Yuan</dc:contributor>
  <dc:contributor>Shixiong Yang</dc:contributor>
  <dc:contributor>Xigui Ding</dc:contributor>
  <dc:contributor>Shucheng Xie</dc:contributor>
  <dc:creator>Pan Zhou</dc:creator>
  <dc:date>2023</dc:date>
  <dc:description>&lt;h3 class="c-article__sub-heading" data-test="abstract-sub-heading"&gt;Aims&lt;/h3&gt;&lt;p&gt;Coastal salt marshes are productive ecosystems that are highly efficient carbon sinks, but there is uncertainty regarding the interactions among climate warming, plant species, and tidal restriction on C cycling.&lt;/p&gt;&lt;h3 class="c-article__sub-heading" data-test="abstract-sub-heading"&gt;Methods&lt;/h3&gt;&lt;p&gt;Open-top chambers (OTCs) were deployed at two coastal wetlands in Yancheng, China, where native&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Phragmites australis&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;(&lt;i&gt;Phragmites&lt;/i&gt;) and invasive&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Spartina alterniflora&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;(&lt;i&gt;Spartina&lt;/i&gt;) were dominant, respectively. Two study locations were set up in each area based on difference in tidal action. The OTCs achieved an increase of average daytime air temperature of ~ 1.11–1.55&amp;nbsp;°C. Net ecosystem CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;exchange (NEE), ecosystem respiration (&lt;i&gt;R&lt;/i&gt;&lt;sub&gt;&lt;i&gt;eco&lt;/i&gt;&lt;/sub&gt;), CH&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;fluxes, aboveground biomass and other abiotic factors were monitored over three years.&lt;/p&gt;&lt;h3 class="c-article__sub-heading" data-test="abstract-sub-heading"&gt;Results&lt;/h3&gt;&lt;p&gt;Warming reduced the magnitude of the radiative balance of native&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Phragmites&lt;/i&gt;, which was determined to still be a consistent C sink. In contrast, warming or tidal flooding presumably transform the&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Spartina&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;into a weak C source, because either warming-induced high salinity reduced the magnitude of NEE by 19% or flooding increased CH&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;emissions by 789%. Remarkably, native&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Phragmites&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;affected by tidal restrictions appeared to be a consistent C source with the radiative balance of 7.11–9.64&amp;nbsp;kg CO&lt;sub&gt;2&lt;/sub&gt;-eq m&lt;sup&gt;–2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;yr&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;because of a reduction in the magnitude of NEE and increase of CH&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;fluxes.&lt;/p&gt;&lt;h3 class="c-article__sub-heading" data-test="abstract-sub-heading"&gt;Conclusions&lt;/h3&gt;&lt;p&gt;Tidal restrictions that disconnect the tidal hydrologic connection between the ocean and land may transform coastal wetlands from C sinks to C sources. This transformation may potentially be an even greater threat to coastal carbon sequestration than climate warming or invasive plant species in isolation.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s11104-023-06160-x</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>Tidal restriction likely has greater impact on the carbon sink of coastal wetland than climate warming and invasive plant</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>