Link between        <fc >I</fc>I        ndian monsoon rainfall and physical erosion in the        <fc >H</fc>H        imalayan system during the        <fc >H</fc>H        olocene

Joussain Ronan; Liu Zhifei; Colin Christophe; Duchamp‐Alphonse Stéphanie; Yu Zhaojie; Moréno Eva; Fournier Léa; Zaragosi Sébastien; Dapoigny Arnaud; Meynadier Laure; Bassinot Franck

摘要

Abstract >Mineralogical and geochemical analyses conducted on cores located on the active channel‐levee system of the northern Bengal Fan are used to establish changes in the weathering pattern and the sediment transport of the Himalayan system, and evaluate the effect of Indian summer monsoon rainfall during the Holocene. Our data indicate that during the Holocene, sediments from the northern Bengal Fan originate mainly from the G‐B river system without any significant changes in the relative contribution of these rivers. From 9.8 to around 6 ka, relatively low smectite/(illite+chlorite) ratios and relatively high K/Si* ratios indicate high physical denudation rates of the Himalayan highlands together with a rapid transfer of the detrital material to the Bengal Fan. The period between 9.2 and 7 ka is associated to lower values of K/Si* and corresponds to the maximum of Indian monsoon rainfall which indicates a more important chemical weathering material that rapidly transits by the G‐B river system without a long storage in the Indo‐Gangetic plain. From 6.0 ka to present day, higher smectite/(illite+chlorite) ratio and lower K/Si* ratio document a gradual increase of sediments originated from the Indo‐Gangetic plain, characterized by higher degree of chemical weathering. During the last 2.5 ka, the drastic increase in the smectite/(illite+chlorite) ratio could be associated to enhanced alteration of the plain soils due to anthropogenic activity. The comparison of mineralogical and geochemical data with previous reconstructions of the Indian monsoon dynamic indicates a rapid response of erosion and sediment transfer of the G‐B river system to changes of monsoon rainfall intensity. </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> >位于北孟加拉风扇有效通道 - 堤坝系统上的矿物质和地球化学分析用于建立风化图案的变化和喜马拉雅系统的沉积物运输，评价印度夏季季风降雨的影响在全新世期间。我们的数据表明，在全新世期间，北孟加拉粉的沉积物主要来自G-B河流系统，没有这些河流的相对贡献的任何重大变化。从9.8到大约6ka，相对低的蒙脱石/（illite +氯酸盐）比率和相对高的K / Si *比率表示喜马拉雅高地的高度身体剥削率，以及快速转移损伤材料到孟加拉风扇。 9.2和7 KA之间的周期与k / si *的值较低，对应于印度季风降雨的最大值，表示更重要的化学风化材料，可通过G-B河系统迅速运输，而无需长时间存储印度突然平原。从6.0 ka到现今，较高的蒙脱石/（illite +氯酸盐）比和较低的k / si *比例文件逐渐增加沉积物的沉积物源自印刷平原，其特征在于更高程度的化学风化。在最后2.5 ka期间，蒙脱石/（illite +亚氯酸盐）比的激烈增加可能与由于人为活性而增强普通土壤的改变。与先前的印度季风动态重建的矿物学和地球化学数据的比较表明G-B河流系统对季风降雨强度的变化的侵蚀和沉积物转移的快速响应。</ 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9期</span><b style="margin: 0 2px;">|</b><span>共18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=Joussain Ronan&option=202" target="_blank" rel="nofollow">Joussain Ronan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Zhifei&option=202" target="_blank" rel="nofollow">Liu Zhifei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Colin Christophe&option=202" target="_blank" rel="nofollow">Colin Christophe;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Duchamp‐Alphonse Stéphanie&option=202" target="_blank" rel="nofollow">Duchamp‐Alphonse Stéphanie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Zhaojie&option=202" target="_blank" rel="nofollow">Yu Zhaojie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moréno Eva&option=202" target="_blank" rel="nofollow">Moréno Eva;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fournier Léa&option=202" target="_blank" rel="nofollow">Fournier Léa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zaragosi Sébastien&option=202" target="_blank" rel="nofollow">Zaragosi Sébastien;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dapoigny Arnaud&option=202" target="_blank" rel="nofollow">Dapoigny Arnaud;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meynadier Laure&option=202" target="_blank" rel="nofollow">Meynadier Laure;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bassinot Franck&option=202" target="_blank" rel="nofollow">Bassinot Franck;</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>Laboratoire GEOsciences Paris‐Sud UMR 8148 CNRS‐Université de Paris‐Sud Université Paris‐SaclayOrsay Cedex France;</p> <p>State Key Laboratory of Marine GeologyTongji UniversityShanghai China;</p> <p>Laboratoire GEOsciences Paris‐Sud UMR 8148 CNRS‐Université de Paris‐Sud Université Paris‐SaclayOrsay Cedex France;</p> <p>Laboratoire GEOsciences Paris‐Sud UMR 8148 CNRS‐Université de Paris‐Sud Université Paris‐SaclayOrsay Cedex France;</p> <p>Laboratoire GEOsciences Paris‐Sud UMR 8148 CNRS‐Université de Paris‐Sud Université Paris‐SaclayOrsay Cedex France;</p> <p>Muséum National d'Histoire Naturelle UMR 7207Paris Cedex 05 France;</p> <p>UMR CNRS 5805 EPOC Université de BordeauxPessac Cedex France;</p> <p>UMR CNRS 5805 EPOC Université de BordeauxPessac Cedex France;</p> <p>Laboratoire des Sciences du Climat et de l'Environnement LSCE/IPSL CEA‐CNRS‐UVSQ Université Paris‐SaclayGif‐sur‐Yvette France;</p> <p>Equipe de Géochimie et Cosmochimie Institut de Physique du Globe de Paris – Sorbonne Paris Cité UMR 7154 Université Paris DiderotParis France;</p> <p>Laboratoire des Sciences du Climat et de l'Environnement LSCE/IPSL CEA‐CNRS‐UVSQ Université Paris‐SaclayGif‐sur‐Yvette France;</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=Bengal Fan&option=203" rel="nofollow">Bengal Fan;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=chemical weathering&option=203" rel="nofollow">chemical weathering;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sr and Nd isotopic compositions&option=203" rel="nofollow">Sr and Nd isotopic compositions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=physical erosion&option=203" rel="nofollow">physical erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=clay mineralogy&option=203" rel="nofollow">clay mineralogy;</a> </p> <div class="translation"> 机译：孟加拉风扇;化学风化;SR和ND同位素组成;物理侵蚀;粘土矿物学; </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/0704023360819.html">Link between <fc >I</fc>I ndian monsoon rainfall and physical erosion in the <fc >H</fc>H imalayan system during the <fc >H</fc>H olocene</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Joussain Ronan&option=202" 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Link between II ndian monsoon rainfall and physical erosion in the HH imalayan system during the HH olocene

摘要