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The Role of the Upper Tidal Estuary in Wetland Blue Carbon Storage and Flux

机译：上潮气在湿地蓝碳储存和助焊剂中的作用

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Abstract > 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 U.S. Atlantic Coast show that total C standing stocks were 322–1,264?Mg C/ha among all sites, generally shifting to greater soil storage as salinity increased. Carbon mass balance inputs (litterfall, woody growth, herbaceous growth, root growth, and 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 ?2 ?·?year ?1 . Soil C burial was variable (7–337?g C?·?m ?2 ?·?year ?1 ), and lateral C export was estimated as C mass balance minus soil C burial as 267–849?g C?·?m ?2 ?·?year ?1 . 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. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>摘要</标题> >碳（c）碳（c）常规股，C质量平衡和土壤C埋藏在潮汐淡水森林中湿地（TFFW）和TFFW沿着上部河口的低盐度沼泽沼泽通常不包括在“蓝碳”会计中，但可能代表一个重要的C水槽。来自潮汐WACCAMAW的两个盐度横断面的结果，美国大西洋海岸的萨凡纳河流展示，所有网站中的C总股322-1,264？MG C / HA，一般转化为盐度的更大的土壤储存增加。碳质量平衡投入（落叶，木质生长，草本生长，根生长和表面积累）减去C输出（表面凋落物和根部分解，气态C）在达11岁以下的时间内为340-900？G C？ ·？m ？2 </ sup>？·？年？1 </ sup>。土壤c埋葬是可变的（7-337？g c？··m ？2 </ sup>？·？年？1 </ sup>），并且横向C导出估计为C质量平衡减去土壤c埋葬为267-849？g c？·m ？2 </ sup>？·？年？1 </ sup>。这代表了大量的C导出，以支持水生生物地质化化学转变。尽管在紧急植被中减少了C持续性，有机物的分解和较高的侧外出口，但由于森林转化为盐渍化的森林，C总储存增加。这些潮汐河湿地在盐度强调森林植物位点上表现出高N矿化，并且在低盐度沼泽中具有相当大的P矿化。大型C常规股票和C封存的速率表明，TFFW和Oligohaline Marshes在全球范围内具有很大的重要性，以沿海C动态以及促进他们发生的世界领域的能量转换。 </ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23728/'>《Global Biogeochemical Cycles》</a> <b style="margin: 0 2px;">|</b><span>2018年第5期</span><b style="margin: 0 2px;">|</b><span>共23页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krauss Ken W.&option=202" target="_blank" rel="nofollow">Krauss Ken W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Noe Gregory B.&option=202" target="_blank" rel="nofollow">Noe Gregory B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Duberstein Jamie A.&option=202" target="_blank" rel="nofollow">Duberstein Jamie A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Conner William H.&option=202" target="_blank" rel="nofollow">Conner William H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stagg Camille L.&option=202" target="_blank" rel="nofollow">Stagg Camille L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cormier Nicole&option=202" target="_blank" rel="nofollow">Cormier Nicole;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jones Miriam C.&option=202" target="_blank" rel="nofollow">Jones Miriam C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bernhardt Christopher E.&option=202" target="_blank" rel="nofollow">Bernhardt Christopher E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Graeme Lockaby B.&option=202" target="_blank" rel="nofollow">Graeme Lockaby B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=From Andrew S.&option=202" target="_blank" rel="nofollow">From Andrew S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doyle Thomas W.&option=202" target="_blank" rel="nofollow">Doyle Thomas W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Day Richard H.&option=202" target="_blank" rel="nofollow">Day Richard H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ensign Scott H.&option=202" target="_blank" rel="nofollow">Ensign Scott H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pierfelice Katherine N.&option=202" target="_blank" rel="nofollow">Pierfelice Katherine N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hupp Cliff R.&option=202" target="_blank" rel="nofollow">Hupp Cliff R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chow Alex T.&option=202" target="_blank" rel="nofollow">Chow Alex T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Whitbeck Julie L.&option=202" target="_blank" rel="nofollow">Whitbeck Julie L.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Wetland and Aquatic Research CenterU.S. Geological SurveyLafayette LA USA;</p> <p>Hydrological‐Ecological Interactions BranchU.S. Geological SurveyReston VA USA;</p> <p>Baruch Institute of Coastal Ecology and Forest ScienceClemson UniversityGeorgetown SC USA;</p> <p>Baruch Institute of Coastal Ecology and Forest ScienceClemson UniversityGeorgetown SC USA;</p> <p>Wetland and Aquatic Research CenterU.S. Geological SurveyLafayette LA USA;</p> <p>Wetland and Aquatic Research CenterU.S. Geological SurveyLafayette LA USA;</p> <p>Eastern Geology and Paleoclimate Science CenterU.S. Geological SurveyReston VA USA;</p> <p>Eastern Geology and Paleoclimate Science CenterU.S. Geological SurveyReston VA USA;</p> <p>School of Forestry and Wildlife SciencesAuburn UniversityAuburn AL USA;</p> <p>Wetland and Aquatic Research CenterU.S. Geological SurveyLafayette LA USA;</p> <p>Wetland and Aquatic Research CenterU.S. Geological SurveyLafayette LA USA;</p> <p>Wetland and Aquatic Research CenterU.S. Geological SurveyLafayette LA USA;</p> <p>Hydrological‐Ecological Interactions BranchU.S. Geological SurveyReston VA USA;</p> <p>School of Forestry and Wildlife SciencesAuburn UniversityAuburn AL USA;</p> <p>Hydrological‐Ecological Interactions BranchU.S. Geological SurveyReston VA USA;</p> <p>Baruch Institute of Coastal Ecology and Forest ScienceClemson UniversityGeorgetown SC USA;</p> <p>Jean Lafitte National Historical Park and PreserveNational Park ServiceNew Orleans LA USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/165.html" title="地质学">地质学;</a><a href="https://www.zhangqiaokeyan.com/clc/5109.html" title="生物地球化学、气体地球化学">生物地球化学、气体地球化学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wetland&option=203" rel="nofollow">Wetland;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Swamp forest&option=203" rel="nofollow">Swamp forest;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tide&option=203" rel="nofollow">Tide;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carbon budget&option=203" rel="nofollow">Carbon budget;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marsh&option=203" rel="nofollow">Marsh;</a> </p> <div class="translation"> 机译：湿地;沼泽森林;潮;碳预算;沼泽; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023423887.html">The 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