Stable Oxygen Isotopes and Mg/Ca in Planktic Foraminifera From Modern Surface Sediments of the Western Pacific Warm Pool: Implications for Thermocline Reconstructions

Hollstein Martina; Mohtadi Mahyar; Rosenthal Yair; Moffa Sanchez Paola; Oppo Delia; Martínez Méndez Gema; Steinke Stephan; Hebbeln Dierk

摘要

Abstract > Mg/Ca and stable oxygen isotope compositions (δ 18 O) of planktic foraminifera tests are commonly used as proxies to reconstruct past ocean conditions including variations in the vertical water column structure. Accurate proxy calibrations require thorough regional studies, since parameters such as calcification depth and temperature of planktic foraminifera depend on local environmental conditions. Here we present radiocarbon‐dated, modern surface sediment samples and water column data (temperature, salinity, and seawater δ 18 O) from the Western Pacific Warm Pool. Seawater δ 18 O (δ 18 O <sub>SW</sub> ) and salinity are used to calculate individual regressions for western Pacific surface and thermocline waters (δ 18 O <sub>SW</sub> ?=?0.37?×? <fi>S</fi> ‐12.4 and δ 18 O <sub>SW</sub> ?=?0.33?×? <fi>S</fi> ‐11.0). We combine shell δ 18 O and Mg/Ca with water column data to estimate calcification depths of several planktic foraminifera and establish regional Mg/Ca‐temperature calibrations. <fi>Globigerinoides ruber</fi> , <fi>Globigerinoides elongatus</fi> , and <fi>Globigerinoides sacculifer</fi> reflect mixed layer conditions. <fi>Pulleniatina obliquiloculata</fi> and <fi>Neogloboquadrina dutertrei</fi> and <fi>Globorotalia tumida</fi> preserve upper and lower thermocline conditions, respectively. Our multispecies Mg/Ca‐temperature calibration (Mg/Ca?=?0.26exp0.097* <fi>T</fi> ) matches published regressions. Assuming the same temperature s </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</ title> > mg / ca和稳定的氧同位素组合物（Δ 18 </ sup> o ）综合体的Foraminifera测试通常用作重建过去的海洋条件的代理，包括垂直水柱结构的变化。精确的代理校准需要彻底的区域性研究，因为诸如钙化深度和塑料传染率的温度等参数取决于局部环境条件。在这里，我们从西太平洋温水池中呈现无线电金，现代表面沉积物样品（温度，盐度和海水δ 18）。海水δ 18（δ 18 </ sup> O <sum> sw </ sub>）和盐度用于计算西太平洋表面和热湿润水域的个体回归（Δ<sup > 18 </ sup> O <sum> sw </ sub>？Δ0.37？×α≤z/ fi> -12.4和δ 18 </ sup> o <sum> sw </ sub >？=？0.33？×1/1 / fi> -11.0）。我们将壳δ 18和Mg / sup> o和mg / ca与水柱数据相结合，以估计几种浮法面包素的钙化深度，并建立区域Mg / Ca温度校准。 <fi> globigerinoides ruber </ fi>，<fi> globigerinoides elongatus </ fi>，以及<fi> globigerinoides sacculifer </ fi>反射混合层条件。 <FI> Pulleniatina Obliquiloculata </ Fi>和<Fi> Neogloboquadrina dutertrei </ Fi>和<fi> Globorotalia tumida分别保留上层和下部热量下划线条件。我们的MUG / CA温度校准（MG / CA？=？0.26exp0.097 * <FI> T </ FI>）匹配已发布的回归。假设温度相同 </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-28889/'>《Paleoceanography》</a> <b style="margin: 0 2px;">|</b><span>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共21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=Hollstein Martina&option=202" target="_blank" rel="nofollow">Hollstein Martina;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mohtadi Mahyar&option=202" target="_blank" rel="nofollow">Mohtadi Mahyar;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rosenthal Yair&option=202" target="_blank" rel="nofollow">Rosenthal Yair;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moffa Sanchez Paola&option=202" target="_blank" rel="nofollow">Moffa Sanchez Paola;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oppo Delia&option=202" target="_blank" rel="nofollow">Oppo Delia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Martínez Méndez Gema&option=202" target="_blank" rel="nofollow">Martínez Méndez Gema;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Steinke Stephan&option=202" target="_blank" rel="nofollow">Steinke Stephan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hebbeln Dierk&option=202" target="_blank" rel="nofollow">Hebbeln Dierk;</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>MARUM–Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</p> <p>MARUM–Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</p> <p>Department of Marine and Coastal Sciences and Department of Earth and Planetary SciencesRutgers State University of New JerseyNew Brunswick NJ USA;</p> <p>School of Earth and Ocean SciencesCardiff UniversityCardiff UK;</p> <p>Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>MARUM–Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</p> <p>Department of Geological OceanographyXiamen UniversityXiamen China;</p> <p>MARUM–Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</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/166.html" title="海洋学">海洋学;</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=Western Pacific Warm Pool&option=203" rel="nofollow">Western Pacific Warm Pool;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mg/Ca calibration&option=203" rel="nofollow">Mg/Ca calibration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oxygen isotopes&option=203" rel="nofollow">oxygen isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=planktic foraminifera&option=203" rel="nofollow">planktic foraminifera;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermocline reconstruction&option=203" rel="nofollow">thermocline reconstruction;</a> </p> <div class="translation"> 机译：西太平洋暖池;Mg / CA校准;氧同位素;塑料Foraminifera;热控重建; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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/0704024380194.html">Stable Oxygen Isotopes and Mg/Ca in Planktic Foraminifera From Modern Surface Sediments of the Western Pacific Warm Pool: Implications for Thermocline Reconstructions</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hollstein Martina&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hollstein Martina,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mohtadi Mahyar&option=202" target="_blank" rel="nofollow" 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