A New Seismic Stratigraphy in the Indian‐Atlantic Ocean Gateway Resembles Major Paleo‐Oceanographic Changes of the Last 7?Ma

Gruetzner Jens; Jiménez Espejo Francisco J.; Lathika Nambiyathodi; Uenzelmann‐Neben Gabriele; Hall Ian R.; Hemming Sidney R.; LeVay Leah J.; the Expedition 361 Scientists

摘要

Abstract >The exchange of water masses between the Indian Ocean and the Atlantic constitutes an integral interocean link in the global thermohaline circulation. Long‐term changes in deep water flow have been studied using seismic reflection profiles but the seismic stratigraphy was poorly constrained and not resolved for the time period from the late Miocene onward. Here we present results from International Ocean Discovery Program Site U1475 (Agulhas Plateau) located over a sediment drift proximal to the entrance of North Atlantic Deep Water into the Southern Ocean and South Indian Ocean. Site U1475 comprises a complete carbonate‐rich stratigraphic section of the last ~7?Ma that provides an archive of climate‐induced variations in ocean circulation. Six marker reflectors occurring in the upper 300?m of the drift are identified here for the first time. The formation of these reflectors is mainly due to density changes that are mostly caused by changes in biogenic versus terrigenous sediment deposition. Synthetic seismograms allow age assignments for the horizons based on biostratigraphy and magnetostratigraphy. Prominent reflectors are related to late Pleistocene glacial/interglacial variability, the middle and early Pleistocene transitions, and the onset of the northern hemisphere glaciation. A peculiar early Pliocene interval (~5.3–4.0?Ma) bounded by two reflectors is characterized by fourfold elevated sedimentation rates (10?cm/kyr) and the occurrence of sediment waves. We argue that this enhanced sediment transport to the Agulhas Plateau was caused by a reorganization of the bottom current circulation pattern due to maximized inflow of North Atlantic Deep Water. </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> >印度洋与大西洋之间的水群体构成全球热卤素循环中的整体互相环节。使用地震反射型材研究了深水流动的长期变化，但地震层层受到严重限制，而未在后期内科的时间段解析。在这里，我们呈现国际海洋发现计划网站U1475（Agulhas高原）的结果位于沉积物漂移到近端的沉积物漂移到北大西洋深水进入南海和南印度洋。站点U1475包括最后〜7？MA的完全碳酸盐的地层部分，提供了气候诱导的海洋循环变化的档案。在此漂移中发生在较高300Ωm中的六个标记反射器在此首次识别。这些反射器的形成主要是由于由于生物的变化与人造沉积物沉积而引起的密度变化。合成地震图允许基于生物数据和磁性数据的视野的年龄作业。突出的反射器与晚熟冰川/中间冰裂解，中期和早期渗透过渡，以及北半球冰川的发作相关。由两个反射器界定的特殊早期间隙（〜5.3-4.0〜mA）的特征在于四倍升高的沉降速率（＆ 10？cm / kyr）和沉积波的发生。我们认为这种增强的沉积物运输到Agulhas Plateau的沉积物运输是由于北大西洋深水最大流入的底部电流循环模式的重组引起的。</ 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1期</span><b style="margin: 0 2px;">|</b><span>共20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=Gruetzner Jens&option=202" target="_blank" rel="nofollow">Gruetzner Jens;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiménez Espejo Francisco J.&option=202" target="_blank" rel="nofollow">Jiménez Espejo Francisco J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lathika Nambiyathodi&option=202" target="_blank" rel="nofollow">Lathika Nambiyathodi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Uenzelmann‐Neben Gabriele&option=202" target="_blank" rel="nofollow">Uenzelmann‐Neben Gabriele;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hall Ian R.&option=202" target="_blank" rel="nofollow">Hall Ian R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hemming Sidney R.&option=202" target="_blank" rel="nofollow">Hemming Sidney R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LeVay Leah J.&option=202" target="_blank" rel="nofollow">LeVay Leah J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=the Expedition 361 Scientists&option=202" target="_blank" rel="nofollow">the Expedition 361 Scientists;</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>Alfred‐Wegener‐Institut Helmholtz‐Zentrum für Polar‐ und MeeresforschungBremerhaven Germany;</p> <p>Japan Agency for Marine‐Earth Science and Technology (JAMSTEC)Institute of BiogeosciencesYokosuka Japan;</p> <p>Ice Core LaboratoryNational Centre for Antarctic and Ocean Research (NCAOR)Vasco da Gama Goa India;</p> <p>Alfred‐Wegener‐Institut Helmholtz‐Zentrum für Polar‐ und MeeresforschungBremerhaven Germany;</p> <p>Department of Earth SciencesCardiff University Main CollegeCardiff UK;</p> <p>Lamont‐Doherty Earth ObservatoryColumbia UniversityPalisades NY USA;</p> <p>International Ocean Discovery ProgramTexas A&</p> <p>M UniversityCollege Station TX USA;</p> <p>See Appendix A2;</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=Agulhas Plateau&option=203" rel="nofollow">Agulhas Plateau;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic reflection method&option=203" rel="nofollow">seismic reflection method;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=contourites&option=203" rel="nofollow">contourites;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=physical properties&option=203" rel="nofollow">physical properties;</a> </p> <div class="translation"> 机译：Agulhas Plateau;地震反射方法;轮廓座;物理性质; </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/0704023360603.html">A New Seismic Stratigraphy in the Indian‐Atlantic Ocean Gateway Resembles Major Paleo‐Oceanographic Changes of the Last 7?Ma</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gruetzner Jens&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Gruetzner Jens,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiménez Espejo Francisco J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth 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NTO is used to generate energy from ocean currents, including a major floating body parallel to the direction of ocean currents.</a> <b>[P]</b> . <span> 外国专利：  CL2012000870A1 </span> <span> . 2012-12-14</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：洋流产生的能量的组合，包括一个主要的浮体，通过海流的方向定向，取决于浮体的转子介质，至少一条稳定器，锚固线;结晶。 NTO用于从洋流中产生能量，包括与洋流方向平行的主要漂浮体。 </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('0704023360603','4',7,2,1,'',this,24)" class="delivery" prompt="010401" 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