The Evolution of Deep Ocean Chemistry and Respired Carbon in the Eastern Equatorial Pacific Over the Last Deglaciation

Fuente Maria; Calvo Eva; Skinner Luke; Pelejero Carles; Evans David; Müller Wolfgang; Povea Patricia; Cacho Isabel

摘要

Abstract > It has been shown that the deep Eastern Equatorial Pacific (EEP) region was poorly ventilated during the Last Glacial Maximum (LGM) relative to Holocene values. This finding suggests a more efficient biological pump, which indirectly supports the idea of increased carbon storage in the deep ocean contributing to lower atmospheric CO <sub>2</sub> during the last glacial. However, proxies related to respired carbon are needed in order to directly test this proposition. Here we present <fc> <fi>Cibicides wuellerstorfi</fi> </fc> B/Ca ratios from Ocean Drilling Program Site 1240 measured by laser ablation inductively coupled plasma mass spectrometry (LA‐ICPMS) as a proxy for deep water carbonate saturation state (Δ[CO <sub>3</sub> 2? ], and therefore [CO <sub>3</sub> 2? ]), along with δ 13 C measurements. In addition, the U/Ca ratio in foraminiferal coatings has been analyzed as an indicator of oxygenation changes. Our results show lower [CO <sub>3</sub> 2? ], δ 13 C, and [O <sub>2</sub> ] values during the LGM, which would be consistent with higher respired carbon levels in the deep EEP driven, at least in part, by reduced deep water ventilation. However, the difference between LGM and Holocene [CO <sub>3</sub> 2? ] observed at our site is relatively small, in accordance with other records from across the Pacific, suggesting that a “counteracting” mechanism, such as seafloor carbonate dissolution, also played a role. If so, this mechanism would have increased average ocean alkalinity, allowing even more atmospheric CO <sub>2</sub> to be “sequestered” by the ocean. T </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”> <title type =“main”>抽象</ title> >它已被证明在东部赤道太平洋（EEP）区域在最后冰川最大（LGM）相对于全新世。该发现表明了一种更有效的生物泵，它间接地支持在最后冰川期间贡献的深海中碳储存增加的想法。但是，需要与呼吸碳有关的代理，以便直接测试该命题。在这里，我们展示了通过激光烧蚀电感耦合等离子体质谱（La-ICPMS）测量的海洋钻井计划部位1240的<FC> <FI> Cibicides Wuellerstorfi </ Fi> </ Fi> B / Ca比作为深水碳酸盐的代理饱和状态（Δ[CO <sub> 3 </ sub> 2〜</ sup>]，因此[CO <sub> 3 </ sub> 2？</ sup>]） δ 13 </ sup> c测量。此外，已经分析了多胺涂层中的U / Ca比作为氧合变化的指示。我们的结果显示下[CO <sub> 3 </ sub> 2Δ</ sup>]，Δ 13 </ sup> c，以及[O <sub> 2 </ sub>]值LGM，这将与深EEP中的较高呼吸碳水平一致，至少部分地通过减少深水通气。然而，在我们的网站观察到的LGM和全新世（CO <Sub> 3 </ sub> 2？</ sup> 2？</ sup>]相对较小，符合来自周围的其他记录，表明a“抵消“机制，例如海底碳酸盐溶解，也发挥了作用。如果是这样，这种机制将增加平均海洋碱度，允许更多大气的CO <sub> 2 </ sub>“海洋”被螯合“。 T. </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12期</span><b style="margin: 0 2px;">|</b><span>共15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=Fuente Maria&option=202" target="_blank" rel="nofollow">Fuente Maria;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Calvo Eva&option=202" target="_blank" rel="nofollow">Calvo Eva;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Skinner Luke&option=202" target="_blank" rel="nofollow">Skinner Luke;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pelejero Carles&option=202" target="_blank" rel="nofollow">Pelejero Carles;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Evans David&option=202" target="_blank" rel="nofollow">Evans David;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller Wolfgang&option=202" target="_blank" rel="nofollow">Müller Wolfgang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Povea Patricia&option=202" target="_blank" rel="nofollow">Povea Patricia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cacho Isabel&option=202" target="_blank" rel="nofollow">Cacho Isabel;</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>Institut de Ciències del Mar CSICBarcelona Spain;</p> <p>Institut de Ciències del Mar CSICBarcelona Spain;</p> <p>Godwin Laboratory for Palaeoclimate Research Department of Earth SciencesUniversity of CambridgeCambridge UK;</p> <p>Institut de Ciències del Mar CSICBarcelona Spain;</p> <p>School of Earth and Environmental SciencesUniversity of St AndrewsSt Andrews UK;</p> <p>Department of Earth SciencesRoyal Holloway University of LondonLondon UK;</p> <p>Grup de Recerca Consolidat en Geociències Marines Departament de Dinàmica de la Terra i de l'OceàUniversitat de BarcelonaBarcelona Spain;</p> <p>Grup de Recerca Consolidat en Geociències Marines Departament de Dinàmica de la Terra i de l'OceàUniversitat de BarcelonaBarcelona Spain;</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=marine carbon cycle&option=203" rel="nofollow">marine carbon cycle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbonate chemistry&option=203" rel="nofollow">carbonate chemistry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean circulation&option=203" rel="nofollow">ocean circulation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glacial‐interglacial cycles&option=203" rel="nofollow">glacial‐interglacial cycles;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=soft‐tissue pump efficiency&option=203" rel="nofollow">soft‐tissue pump efficiency;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seafloor calcite dissolution&option=203" rel="nofollow">seafloor calcite dissolution;</a> </p> <div class="translation"> 机译：海洋碳循环;碳酸盐化学;海洋循环;冰川 - 中间峡循环;软组织泵效率;海底方解石溶解; </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/0704024380325.html">The Evolution of Deep Ocean Chemistry and Respired Carbon in the Eastern Equatorial Pacific Over the Last Deglaciation</a> <b>[J]</b> . <span> <a 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