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Changes in Intermediate Circulation in the Bay of Bengal Since the Last Glacial Maximum as Inferred From Benthic Foraminifera Assemblages and Geochemical Proxies

机译：孟加拉湾中间循环的变化自最近冰川最大值，从底栖传染媒体组合和地球化学代理推断出

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Abstract > Benthic foraminiferal assemblages and geochemical tracers (δ 18 O, δ 13 C and 14 C) have been analyzed on benthic and planktonic foraminifera from core MD77‐176, located in the northern Bay of Bengal, in order to reconstruct the evolution of intermediate circulation in the northern Indian Ocean since the last glaciation. Results indicate that during the Last Glacial Maximum (LGM), Southern Sourced Water masses were dominant at the core site. A high relative abundance of intermediate and deep infaunal species during the LGM reflects low oxygen concentration and/or mesotropic to eutrophic deep water conditions, associated with depleted benthic δ 13 C values. During the Holocene, benthic foraminiferal assemblages indicate an oligotropic to mesotrophic environment with well‐ventilated bottom water conditions compared with LGM. Higher values for benthic foraminifera δ 13 C and B‐P 14 C age offsets suggest an increased contribution of North Atlantic Deep Water to the northern Bay of Bengal during the Late Holocene compared to the LGM. Millennial‐scale events punctuated the last deglaciation, with a shift in the δ 13 C and the ? <sub>Nd</sub> values coincident with low B‐P 14 C age offsets, providing strong evidence for an increased contribution of Antarctic Intermediate Water at the studied site. This was associated with enhanced upwelling in the Southern Ocean, reflecting a strong sea‐atmospheric CO <sub>2</sub> exchange through Southern Ocean ventilation during the last deglaciation. </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”>抽象</ title> > 底栖的传染率集装配和地球化学示踪剂（δ 18 </ sup> o，δ 13 </ sup> C和 14 </ sup> c）从位于孟加拉北部的核心MD77-176核心MD77-176上分析了Benthic和Planktonic Foraminifera，以重建自上次冰川以来北方印度洋中间循环的演变。结果表明，在上次冰川最大（LGM）期间，南方源水群体在核心部位占主导地位。 LGM期间的高相对丰富的中间和深鉴定性物种反映了与耗尽的膨化剂δ相关的低氧浓度和/或半渗透性，与富营养的深水条件相关 13 </ sup> C值。在全新世期间，底栖的多氨酰胺机组合指示具有良好通风的底部水条件的植物营养环境的寡核苷酸，与LGM相比。 Benthic foraminiferaδ更高的值 13 </ sup> c和b-p 14 </ sup> C年龄抵消表明，与LGM相比，北大西洋深水北大西洋深水对孟加尔末期的北部湾。千禧年的尺度事件点击最后一个渐变，在δ中的偏移 13 </ sup> C和这一点 ？</ i> <sub> nd </ sub> 用低B-p重合的值 14 </ sup> C年龄抵消，提供了强有力的证据，以增加南极中间水在研究现场的贡献。这与南海中增强的升值有关，反映了强大的海洋大气合作 <sub> 2 </ sub> 在最后的谴责期间通过南海通风交流。 </ 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>2019年第3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=Ma Ruifang&option=202" target="_blank" rel="nofollow">Ma Ruifang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sépulcre Sophie&option=202" target="_blank" rel="nofollow">Sépulcre Sophie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Licari Laetitia&option=202" target="_blank" rel="nofollow">Licari Laetitia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bassinot Franck&option=202" target="_blank" rel="nofollow">Bassinot Franck;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Zhifei&option=202" target="_blank" rel="nofollow">Liu Zhifei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tisnérat‐Laborde Nadine&option=202" target="_blank" rel="nofollow">Tisnérat‐Laborde Nadine;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kallel Nejib&option=202" target="_blank" rel="nofollow">Kallel Nejib;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Zhaojie&option=202" target="_blank" rel="nofollow">Yu Zhaojie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Colin Christophe&option=202" target="_blank" rel="nofollow">Colin Christophe;</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>GEOPS Université Paris‐Sud CNRS Université Paris‐SaclayOrsay France;</p> <p>GEOPS Université Paris‐Sud CNRS Université Paris‐SaclayOrsay France;</p> <p>CEREGE Aix‐Marseille Université‐Europole de l'Arbois‐BP80Aix‐en‐Provence France;</p> <p>LSCE/IPSL CEA CNRS UVSQ UMR 8212Gif Sur Yvette France;</p> <p>State Key Laboratory of Marine GeologyTongji UniversityShanghai China;</p> <p>LSCE/IPSL CEA CNRS UVSQ UMR 8212Gif Sur Yvette France;</p> <p>Laboratoire Georessources Matériaux Environnements et Changements Globaux LR13ES23 Faculté des Sciences de SfaxUniversité de SfaxSfax Tunisia;</p> <p>Key Laboratory of Marine Geology and Environment Institute of OceanologyChinese Academy of SciencesQingdao China;</p> <p>GEOPS Université Paris‐Sud CNRS Université Paris‐SaclayOrsay France;</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=Bay of Bengal&option=203" rel="nofollow">Bay of Bengal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=intermediate water masses&option=203" rel="nofollow">intermediate water masses;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glacial Holocene&option=203" rel="nofollow">glacial Holocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=benthic foraminiferal assemblages&option=203" rel="nofollow">benthic foraminiferal assemblages;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbon and oxygen stable isotopes&option=203" rel="nofollow">carbon and oxygen stable isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=B‐P 14 C age&option=203" rel="nofollow">B‐P 14 C age;</a> </p> <div class="translation"> 机译：孟加拉湾;中间水群;冰川全新世;底栖多氨基纤维组合;碳和氧稳定同位素;B-P 14 C年龄; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 03:07:56</span> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div 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