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首页> 外文期刊>Geochemistry, geophysics, geosystems >Incorporation of Mg, Sr, Ba, U, and B in High‐Mg Calcite Benthic Foraminifers Cultured Under Controlled pp CO 22
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Incorporation of Mg, Sr, Ba, U, and B in High‐Mg Calcite Benthic Foraminifers Cultured Under Controlled pp CO 22

机译：在受控培养的高镁角质石结石的花瓶中掺入Mg，Sr，Ba，U和B中的Bentminififers p p CO. 2 2

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Abstract > Measurement of elemental ratios (E/Ca) has been performed in two symbiont‐bearing species of high‐Mg calcite benthic foraminifers (hyaline, Baculogypsina sphaerulata and porcelaneous, Amphisorus hemprichii ), cultured under five p CO <sub>2</sub> levels, representing preindustrial, modern, and three predicted future values. E/Ca ratios were analyzed by Laser Ablation coupled with Inductively Coupled Plasma Mass Spectrometer (LA‐ICP‐MS). We measured several E/Ca, such as Mg/Ca, Sr/Ca, Ba/Ca, U/Ca, and B/Ca simultaneously. We observed that high‐Mg calcite benthic foraminifers possess higher E/Ca than low‐Mg calcite foraminifers, irrespective of their calcification mode (hyaline or porcelaneous). In both modes of calcification, Mg, Sr, Ba, U, and B incorporation could be controlled by Rayleigh fractionation. However, more data are needed to validate and quantify the relative importance of this process and closely investigate the presence/absence of other mechanism. Therefore, it highlights the need for a multielemental approach when looking at trace element incorporation. Finally, no significant relationship was observed between the different ratios and the p CO <sub>2</sub> of the water, suggesting that none of the Mg/Ca, Sr/Ca, Ba/Ca, U/Ca, and B/Ca is sensitive to bottom water p CO <sub>2</sub> or pH for these species. </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> > 元素比率（E / CA）的测量已在两种含两种含有High-Mg方解石底栖火炭的含量（Hyaline）（ Baculogypsina sphaerulata </ i> 和陶瓷， amphisorus hemprichii </ i> ），五下面培养 p </ i> CO. <sub> 2 </ sub> 级别，代表预工业，现代和三个预测的未来价值。通过与电感耦合等离子体质谱仪（La-ICP-MS）耦合的激光消融来分析E / CA比率。我们同时测量了几种E / Ca，例如Mg / Ca，Sr / Ca，Ba / Ca，U / Ca和B / Ca。我们观察到高Mg辅导底栖火细胞比低Mg辅导火花蛋白化物具有更高的E / Ca，而不管其钙化模式（透明或陶瓷）。在两种钙化模式中，可以通过瑞利分馏来控制Mg，Sr，Ba，U和B掺入。但是，需要更多的数据来验证和量化该过程的相对重要性，并密切研究其他机制的存在/不存在。因此，它突出了在查看跟踪元素结合时对多元首方法的需要。最后，在不同比率之间没有观察到显着的关系 p </ i> CO. <sub> 2 </ sub> 水，表明Mg / Ca，Sr / Ca，Ba / Ca，U / Ca和B / Ca都不是底水敏感 p </ i> CO. <sub> 2 </ sub> 或对这些物种的pH值。 </ 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1期</span><b style="margin: 0 2px;">|</b><span>共16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=Not C.&option=202" target="_blank" rel="nofollow">Not C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thibodeau B.&option=202" target="_blank" rel="nofollow">Thibodeau B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yokoyama Y.&option=202" target="_blank" rel="nofollow">Yokoyama 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>Department of Earth SciencesUniversity of Hong KongHong Kong;</p> <p>Department of Earth SciencesUniversity of Hong KongHong Kong;</p> <p>Atmosphere and Ocean Research Institute Department of Earth and Planetary SciencesUniversity of TokyoChiba Japan;</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=benthic foraminifer&option=203" rel="nofollow">benthic foraminifer;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=high‐Mg calcite&option=203" rel="nofollow">high‐Mg calcite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mg/Ca&option=203" rel="nofollow">Mg/Ca;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sr/Ca&option=203" rel="nofollow">Sr/Ca;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=U/Ca&option=203" rel="nofollow">U/Ca;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ba/Ca&option=203" rel="nofollow">Ba/Ca;</a> </p> <div class="translation"> 机译：Benthic foraminifer;高mg方解石;mg / ca;sr / ca;u / ca;ba / ca; 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