Registration of Precession Signal in the Last Interglacial Paleosol (S        <sub >1</sub>1        ) on the Chinese Loess Plateau

Ma Long; Li Ying; Liu Xingxing; Sun Youbin

摘要

Abstract > Solar insolation plays an essential role in driving orbital‐scale East Asian Monsoon (EAM) variability. Unlike Chinese speleothem δ 18 O records characterized by dominant precessional cycles, many loess proxies from the Chinese Loess Plateau (CLP) usually display damped precessional‐scale variability. To reconcile the precessional monsoon variability recorded in two classic archives, it's critical to investigate which factor can significantly affect the sensitivity of loess proxies to precessional forcing. In this study, we synthesize grain size (GS) and magnetic susceptibility (χ) results of 18 paleosol (S <sub>1</sub> ) profiles over the CLP, with effort to evaluating the relative impacts of sedimentation rate (SR), and pedogenesis on the precessional signal intensity (PSI) during the last interglaciation. Based on unified grain‐size age models, amplitude contrast between normalized GS and χ variations of five substages of the last interglaciation is employed to infer the PSI. The results indicate that precessional signals are evident in the GS/χ records of the high‐SR loess profiles on the northern and western CLP. Comparison of the PSI variations with the SR and mean annual precipitation (MAP) changes suggests that the GS‐PSI is positively correlated to the SR changes, while the χ‐PSI is negatively/positively related to the SR/MAP changes. Our results confirm that distinct precessional cycles in high‐resolution loess proxies permit a plausible reconciliation of monsoon variability recorded in Chinese loess and speleothem. </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> > 太阳能缺失在驾驶轨道级东亚季风（EAM）变异方面发挥着重要作用。与中国孢子素δ不同 18 </ sup> o由占主导地位的前期循环为特征的记录，来自中国黄土高原（CLP）的许多黄土代理通常会显示阻尼的模尺规模可变性。为了调和在两个经典档案中记录的预算正常季风可变性，探讨哪个因素可能会显着影响黄土代理敏感性至前进的档案至关重要。在这项研究中，我们合成粒度（GS）和磁化率（χ）结果为18古溶胶（s <sub> 1 </ sub> ）通过CLP的简档，努力评估沉淀率（SR）的相对影响（SR），以及在最后一个中间的前进信号强度（PSI）上的基础上的相对影响。基于统一的晶粒尺寸模型，采用了正常化GS与最后一个中间的五个等相变的幅度对比度来推断PSI。结果表明，在北部和西部CLP的高级SR黄土概况的GS /χ记录中，模型信号是显而易见的。 PSI变化与SR和均值年降水（MAP）变化的比较表明，GS-PSI与SR变化呈正相关，而χ-PSI与SR / MAP改变产生负面/正相关。我们的结果证实，高分辨率黄土代理中的独特的生态周期允许在中国黄土和斯派内测量中记录的季风变异性的合理和解。 </ 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>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共12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 Long&option=202" target="_blank" rel="nofollow">Ma Long;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Ying&option=202" target="_blank" rel="nofollow">Li Ying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Xingxing&option=202" target="_blank" rel="nofollow">Liu Xingxing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sun Youbin&option=202" target="_blank" rel="nofollow">Sun Youbin;</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>State Key Laboratory of Loess and Quaternary GeologyInstitute of Earth Environment Chinese Academy of SciencesXi'an China;</p> <p>State Key Laboratory of Loess and Quaternary GeologyInstitute of Earth Environment Chinese Academy of SciencesXi'an China;</p> <p>State Key Laboratory of Loess and Quaternary GeologyInstitute of Earth Environment Chinese Academy of SciencesXi'an China;</p> <p>State Key Laboratory of Loess and Quaternary GeologyInstitute of Earth Environment Chinese Academy of SciencesXi'an China;</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=Chinese loess plateau&option=203" rel="nofollow">Chinese loess plateau;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=last interglacial paleosol (S 1 )&option=203" rel="nofollow">last interglacial paleosol (S 1 );</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=precessional signal intensity&option=203" rel="nofollow">precessional signal intensity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sedimentation rate&option=203" rel="nofollow">sedimentation rate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mean annual precipitation&option=203" rel="nofollow">mean annual precipitation;</a> </p> <div class="translation"> 机译：中国黄土高原;上一层古醇（S 1）;模型信号强度;沉降率;平均年降水量; </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/0704023360818.html">Registration of Precession Signal in the Last 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<span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . </a> <span> <a href="/journal-cn-9054/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 国内外香化信息 </a> </span> <span> . 2015</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_textile-auxiliaries_thesis/0201249044749.html">染料行业预注册基本结束正式注册号角吹响中国染料工业协会田利明秘书长在染料行业欧盟化学物质注册工作会议上的讲话</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . </a> <span> <a href="/journal-cn-9250/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 印染助剂 </a> </span> <span> . 2009</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" 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target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 彭凌帅</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120957450.html">用于对在叶片环的装在流体机械的环形槽中的第一个和最后一个叶片之间留下的中间空隙进行封闭的闭锁组件以及相应的流体机械</a> <b>[P]</b> . <span> 中国专利： CN101351620B </span> <span> . 2012.06.13</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120105548644.html">用于对在叶片环的装在流体机械的环形槽中的第一个和最后一个叶片之间留下的中间空隙进行封闭的封闭组件以及相应的流体机械</a> <b>[P]</b> . <span> 中国专利： CN101351620A </span> <span> . 2009-01-21</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130419277080.html">the loess plateau loess board and the wall body.</a> <b>[P]</b> . <span> 外国专利：  KR2004697380000Y1 </span> <span> . 2013-11-04</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：黄土高原黄土板和墙体。 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130416631438.html">in the loess plateau.</a> <b>[P]</b> . <span> 外国专利：  KR2004706930000Y1 </span> <span> . 2014-01-07</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：在黄土高原。 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130436755072.html">in the loess plateau</a> <b>[P]</b> . <span> 外国专利：  KR2004220310000Y1 </span> <span> . 2006-07-20</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：在黄土高原 </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> 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Registration of Precession Signal in the Last Interglacial Paleosol (S 11 ) on the Chinese Loess Plateau

摘要

Registration of Precession Signal in the Last Interglacial Paleosol (S ₁1 ) on the Chinese Loess Plateau