Reef Carbonate Productivity During Quaternary Sea Level Oscillations

Husson L.; Pastier A.‐M.; Pedoja K.; Elliot M.; Paillard D.; Authemayou C.; Sarr A.‐C.; Schmitt A.; Cahyarini S. Y.

摘要

Abstract > Global variations in reef productivity during the Quaternary depend on external parameters that may alter the global chemical balance in the oceans and atmosphere. We designed a numerical model that simulates reef growth, erosion, and sedimentation on coastlines undergoing sea level oscillations, and uplift or subsidence. We further develop a probabilistic evaluation that accounts for variable vertical ground motion, erosion, and foundation morphologies. Absolute sea level change appears primordial, as productivity must have increased by an order of magnitude since the onset of the glacial cycles, ～2.6 Ma. But most important is relative sea level change, i.e., eustasy modulated by uplift or subsidence, that rejuvenates the accommodation space and exposes pristine domains of the shore to active reefs at each cycle. Integrated over the long‐term, vertical land motion sets the pace of reef growth: productivity in tectonically unstable domains is thus expected to be up to 10 times higher than in stable regions, if any. We quantify the global length of reef coasts and the probability density functions for slopes and uplift rates. Productivity waxes during transgressions to reach 2–8 <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21541:ggge21541-math-0001" wiley:location="equation/ggge21541-math-0001.png"> <mat:mrow> <mat:mtext>Gt</mat:mtext> <mat:mo>?</mat:mo> <mat:mo>?</mat:mo> <mat:msub> <mat:mrow> <mat:mtext>CaCO</mat:mtext> </mat:mrow> <mat:mn>3</mat:mn> </mat:msub> <mat:mo>/</mat:mo> <mat:mtext>yr</mat:mtext> </mat:mrow> </mat:math> and wanes during highstands, which may contribute to increase atmospheric p CO <sub>2</sub> by several tens of ppm during deglaciations. Over the last 1.5 Ma, reefs precipitated ～0.8 × 10 6 <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21541:ggge21541-math-0002" wiley:location="equation/ggge21541-math-0002.png"> <mat:mrow> <mat:mtext>Gt</mat:mtext> <mat:mo>?</mat:mo> <mat:mo>?</mat:mo> <mat:msub> <mat:mrow> <mat:mtext>CaCO</mat:mtext> </mat:mrow> <mat:mn>3</mat:mn> </mat:msub> </mat:mrow> </mat:math> (～500 × 10 3 km 3 ), the equivalent of a 1 m‐thick layer spread over the entire surface of the Earth. This production modulates the calcium budget, for it represents some 30% of the modern Ca flux in the ocean. </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”> <标题类型=“main”>抽象</ title> > 第四纪期间珊瑚礁生产率的全局变化取决于可能改变海洋和大气中的全球化学平衡的外部参数。我们设计了一种数值模型，模拟海底振荡和隆起或沉降的海岸线上的珊瑚礁生长，侵蚀和沉降。我们进一步开发了概率评估，占可变垂直地面运动，侵蚀和基础形态的概率评估。绝对</ i> 海平面变化出现原始，因为生产力必须增加，因为冰川周期发作，〜2.6 mA。但最重要的是相对</ i> 海平面变化，即通过隆起或沉降调节的泛果，可让住宿空间恢复活力，并将岸边的原始座位暴露于每个周期的活动珊瑚礁。在长期内集成，垂直陆运动设定了珊瑚礁的速度：由于任何情况，因此预期在根本上不稳定的域中的生产率高达10倍，如果有的话。我们量化了Reef海岸的全球长度以及斜坡和提升速率的概率密度函数。过渡期间的生产力蜡达到2-8 <mat：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：媒体：GGGE21541：GGGE21541-Math-0001”Wiley：Location =“等式/ GGGE21541-Math-0001.png”> <MAT：MROW> <mat：mtext> gt </ mat：mtext> <mat：mo>？</ mat：mo> <mat：mo>？</ mat：mo> <mat：msub> <MAT：MROW> <mat：mtext> caco </ mat：mtext> </ mat：MROW> <MAT：MN> 3 </ MAT：MN> </ mat：msub> <mat：mo> / </ mat：mo> <mat：mtext> Yr </ mat：mtext> </ mat：MROW> </ mat：math> 在高处理期间的徘徊，这可能有助于增加大气 p </ i> CO. <sub> 2 </ sub> 在下降期间在几十个ppm。在最后1.5 ma，珊瑚礁沉淀〜0.8×10 6 </ sup> <mat：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：媒体：GGGE21541：GGGE21541-Math-0002”Wiley：Location =“等式/ GGGE21541-Math-0002.png”> <MAT：MROW> <mat：mtext> gt </ mat：mtext> <mat：mo>？</ mat：mo> <mat：mo>？</ mat：mo> <mat：msub> <MAT：MROW> <mat：mtext> caco </ mat：mtext> </ mat：MROW> <MAT：MN> 3 </ MAT：MN> </ mat：msub> </ mat：MROW> </ mat：math> （〜500×10 3 </ sup> km. 3 </ sup> ），相当于1米厚的层在地球的整个表面上传播。这一生产调制了钙预算，因为它代表了海洋中现代CA通量的约30％。 </ p> </摘要> </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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共17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=Husson L.&option=202" target="_blank" rel="nofollow">Husson L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pastier A.‐M.&option=202" target="_blank" rel="nofollow">Pastier A.‐M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pedoja K.&option=202" target="_blank" rel="nofollow">Pedoja K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Elliot M.&option=202" target="_blank" rel="nofollow">Elliot M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Paillard D.&option=202" target="_blank" rel="nofollow">Paillard D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Authemayou C.&option=202" target="_blank" rel="nofollow">Authemayou C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sarr A.‐C.&option=202" target="_blank" rel="nofollow">Sarr A.‐C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmitt A.&option=202" target="_blank" rel="nofollow">Schmitt A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cahyarini S. Y.&option=202" target="_blank" rel="nofollow">Cahyarini S. Y.;</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>ISTerre CNRS Université Grenoble AlpesGrenoble France;</p> <p>Géosciences Rennes CNRS Université Rennes‐1Rennes France;</p> <p>M2C Caen CNRS Université de CaenCaen France;</p> <p>LPG Nantes CNRS Université NantesNantes France;</p> <p>LSCE CNRS CEAGif‐sur‐Yvette France;</p> <p>LGO CNRS IUEM Université de BrestPlouzané France;</p> <p>ISTerre CNRS Université Grenoble AlpesGrenoble France;</p> <p>LPG Nantes CNRS Université NantesNantes France;</p> <p>Research Center for Geotechnology Indonesian Institute of Sciences LIPIBandung Indonesia;</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/163.html" title="地球物理学">地球物理学;</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=coral reefs&option=203" rel="nofollow">coral reefs;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea level&option=203" rel="nofollow">sea level;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbonate&option=203" rel="nofollow">carbonate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=modeling&option=203" rel="nofollow">modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleoclimate&option=203" rel="nofollow">paleoclimate;</a> </p> <div class="translation"> 机译：珊瑚礁;海平面;碳酸盐;建模;古古典; </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/0704023360745.html">Reef Carbonate Productivity During Quaternary Sea Level Oscillations</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Husson L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Husson L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pastier A.‐M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pastier A.‐M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pedoja K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pedoja K.,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第4期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：第四纪海平面振荡期间珊瑚礁碳酸盐生产率</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070405625396.html">Late Holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Harris Daniel L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Harris Daniel L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Webster Jody M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Webster Jody M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vila-Concejo Ana&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Vila-Concejo Ana,</a> <a href="/journal-foreign-23447/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geology .</a> <span>2015</span><span>,第2期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：全新世晚期海平面下降和礁石扁平碳酸盐岩生产的关闭：重新思考桶装和珊瑚礁生长模型</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704010825610.html">Comment on Hearty, PJ and O'Leary, MJ, 2008. 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NaiduPD</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=丰全会&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,丰全会</a> <span> <a href="/journal-cn-51619/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋地质动态 </a> </span> <span> . 2000</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201294624425.html">迎接我国珊瑚礁学科发展的春天——中国第四纪科学研究会珊瑚礁专业委员会2016年度学术会议</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=余克服&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 余克服</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵焕庭&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵焕庭</a> <span> <a href="/journal-cn-56877/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 热带地理 </a> </span> <span> . 2016</span><span>,第1期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201292064372.html">西沙群岛琛航岛全新世珊瑚礁的起始发育时间及其海平面指示意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=覃业曼&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 覃业曼</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=余克服&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,余克服</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王瑞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王瑞</a> <span> <a href="/journal-cn-56877/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 热带地理 </a> </span> <span> . 2019</span><span>,第3期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201293514725.html">未来海平面上升对涠洲岛珊瑚礁的可能影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=汤超莲&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 汤超莲</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周雄&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,周雄</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑兆勇&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑兆勇</a> <span> <a href="/journal-cn-56877/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 热带地理 </a> </span> <span> . 2013</span><span>,第2期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-5112_thesis/020221284551.html">未来海平面上升对涠洲岛珊瑚礁的可能影响</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tang Chao-Lian&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . Tang Chao-Lian</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=汤超莲&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,汤超莲</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhou Xiong&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Zhou Xiong</a> <span> <a href="/conference-cn-5112/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第六届海洋强国战略论坛 </a> <span> <span> . 2013</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020316362208.html">西沙群岛琛航岛全新世珊瑚礁的发育过程及其记录的海平面变化</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=覃业曼&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 覃业曼</a> <span> . 2019</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061204068674.html">一种小样品量的第四纪土壤碳酸盐的定年方法</a> <b>[P]</b> . <span> 中国专利： CN111398469B </span> <span> . 2020.10.27</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120103992760.html">一种小样品量的第四纪土壤碳酸盐的定年方法</a> <b>[P]</b> . <span> 中国专利： CN111398469A </span> <span> . 2020-07-10</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130406687874.html">Composition for maintaining stable elemental levels in seawater of artificial reef systems</a> <b>[P]</b> . <span> 外国专利：  IL254489D0 </span> <span> . 2017-11-30</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：用于维持人造礁石系统海水中元素水平稳定的组合物 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130412215805.html">3. The process of improving fishery productivity, including the introduction of a bioavailable iron compound into the marine environment near fish migration areas and areas without abnormal sea level known as "vortices".</a> <b>[P]</b> . <span> 外国专利：  CL2014003349A1 </span> <span> . 2016-09-02</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：3.提高渔业生产率的过程，包括将生物可利用的铁化合物引入鱼类迁徙区域和没有异常海平面的区域（称为“漩涡”）附近的海洋环境中。 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130440485442.html">Methods for selecting and producing animals having a predicted level of immune response, disease resistance or susceptibility, and/or productivity</a> <b>[P]</b> . <span> 外国专利：  US2004235061A1 </span> <span> . 2004-11-25</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：选择和生产具有预期免疫应答，疾病抵抗力或易感性和/或生产力的动物的方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360745','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p class="current">目前支持订阅全部北京大学中文核心（2020）期刊目录。</p> <div style="display: flex;margin-top: 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