Organic carbon preservation in        <fc >S</fc>S        outheastern        <fc >A</fc>A        rabian        <fc >S</fc>S        ea sediments since mid‐        <fc >H</fc>H        olocene:        <fc >I</fc>I        mplications to        <fc >S</fc>S        outh        <fc >A</fc>A        sian        <fc >S</fc>S        ummer        <fc >M</fc>M        onsoon variability

Nagoji Siddhesh S.; Tiwari Manish

摘要

Abstract > The earlier studies show a contrasting long‐term trend of the South Asian Summer Monsoon (SASM) after attaining the precessional forcing induced mid‐Holocene maximum. The increasing total organic carbon (TOC) concentration of marine sediments in the Southeastern Arabian Sea (SEAS) has been interpreted to imply strengthening SASM since mid‐Holocene by a few studies. However, TOC concentration is also influenced by redox conditions, sedimentation rate, and an influx of terrigenous matter depending on the regional settings. So, it needs to be ascertained whether the TOC concentration of the sediments in the SEAS is a signal of productivity related to the SASM strength or preservation. Therefore, we studied multiple proxies (TOC, total nitrogen, atomic C/N, δ 13 C <sub>org</sub> , CaCO <sub>3</sub> , and major and trace elements concentration) for determining the productivity, redox conditions, detrital supply, and provenance in a sediment core from the upper continental slope of the SEAS spanning the past ～4700 years at centennial scale resolution. The present study shows that the observed increase in the TOC values since the mid‐Holocene is a result of better preservation caused by increased sedimentation rate and enhanced reducing conditions. We further show that the SASM has been declining since mid‐Holocene after attaining a precession‐forced maximum, which corroborates the earlier model ensemble studies. </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> > 早期的研究表明，南亚夏季季风（SASM）达到了对中全新世纪中期中期的生育迫使后的鲜明对比的长期趋势。在东南阿拉伯海（SEA）的海洋沉积物中越来越多的有机碳（TOC）浓度被解释为少数研究以来暗示加强SASM。然而，根据区域环境，TOC浓度也受氧化还原条件，沉降率和灌区涌入的影响。因此，需要确定海洋中沉积物的TOC浓度是否是与痉挛强度或保存相关的生产率的信号。因此，我们研究了多个代理（TOC，总氮，原子C / N，δ 13 </ sup> C <sub> org </ sub> ，椰子 <sub> 3 </ sub> 和主要和微量元素浓度）用于在百年大约4700年的海域的上大陆坡中确定生产力，氧化还原条件，脱墨供应和沉积物核心中的沉积物核心。本研究表明，由于中全新世以来，观察到的TOC值的增加是由增加沉降率和增强的还原条件引起的更好保存的结果。我们进一步表明，在获得了强制性最大值之后，SASM已被下降，这使得先前的模型集合研究得到了解决。 </ 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14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=Nagoji Siddhesh S.&option=202" target="_blank" rel="nofollow">Nagoji Siddhesh S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tiwari Manish&option=202" target="_blank" rel="nofollow">Tiwari Manish;</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>National Centre for Antarctic and Ocean ResearchVasco‐da‐Gama Goa India;</p> <p>National Centre for Antarctic and Ocean ResearchVasco‐da‐Gama Goa India;</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=monsoon&option=203" rel="nofollow">monsoon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arabian Sea&option=203" rel="nofollow">Arabian Sea;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=TOC&option=203" rel="nofollow">TOC;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=redox&option=203" rel="nofollow">redox;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=trace elements&option=203" rel="nofollow">trace elements;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=precession&option=203" rel="nofollow">precession;</a> </p> <div class="translation"> 机译：季风;阿拉伯海;TOC;氧化还原;微量元素;进展; 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href="/patent-detail/06120104161833.html">浅层电气保护器件(GFCI、AFCI和AFCI/GFCI)系统和方法</a> <b>[P]</b> . <span> 中国专利： CN111492540A </span> <span> . 2020-08-04</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/061201972078.html">PFC信号生成电路、使用PFC信号生成电路的PFC控制系统以及PFC控制方法</a> <b>[P]</b> . <span> 中国专利： CN103503295B </span> <span> . 2016.03.09</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130446818066.html">n - acetyl - (l) - (4) - tsu00fcanofenu00fcu00fclalaniini ac - (l) - (4 - ((cn) phe - oh and n - acetyl - (l) - p - amidinofenu00fcu00fclalaniintsu00fckloheksu00fcu00fclglu00fctsiin - beta - (3) - n - metu00fcu00fclpu00fcridiinium) alanine ac - (l) - paph - chg - palme (3) - nh2 valmistamismeetod</a> <b>[P]</b> . <span> 外国专利：  EE03698B1 </span> <span> . 2002-04-15</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：n-乙酰-（l）-（4）-ts u00fcanofen u00fc u00fclalaniini ac-（l）-（4-（（cn）phe-oh和n-乙酰-（l）-p-amidinofen u00fc u00fclalaniints u00fckloheks u00fc u00fclgl u00fctsiin-beta-（3）-n-met u00fc u00fclp u00fcridiinium）丙氨酸ac-（l）-paph-chg-palme（3）-nh2 valmistamism </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130415182869.html">"process for separating a mixture comprising hf and hfc-1234ze, process for separating an e-hfc-1234ze from a mixture including hydrogen fluoride and said e-hfc-1234ze, process for separating" of hydrogen fluoride from a mixture containing hydrogen fluoride and e-hfc-1234ze, process for purifying an e-hfc-1234ze from a mixture of e-hfc-1234ze and hf, process for purifying hf from a mixture comprising e-hfc-1234ze and hf, process for separating e-hfc-1234ze from a mixture of e-hfc-1234ze, hf and at least one of hfc-245fa or hfc-245eb and process for hfc-1234yf separation from hfc-1234ze "</a> <b>[P]</b> . <span> 外国专利：  BRPI0906015A2 </span> <span> . 2015-06-30</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：从包含氟化氢的混合物中分离氟化氢的“分离包含hf和hfc-1234ze的混合物的方法，从包含氟化氢和所述e-hfc-1234ze的混合物中分离e-hfc-1234ze的过程，分离方法”。 e-hfc-1234ze，从e-hfc-1234ze和hf的混合物中纯化e-hfc-1234ze的方法，从包含e-hfc-1234ze和hf的混合物中纯化hf的方法，分离e-hfc-从e-hfc-1234ze，hf和hfc-245fa或hfc-245eb中至少一种的混合物中提取1234ze，以及从hfc-1234ze中分离hfc-1234yf的方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130415182870.html">Separation process of a mixture comprising HF and HFC - 1234yf, separation process of HFC - 1234yf a mixture comprising hydrogen fluoride and the mentioned this 1234yf, separation process of hydrogen fluoride in a mixture comprising hydrogen fluoride and HF. C - 1234yf, purification process of HFC - 1234yf from a mixture comprising HFCS - 1234yf and HF.Purification process of HF from a mixture comprising an HFC - 1234yf and HF, separation of a mixture of HFC - 1234yf HFC - 1234yf, HF and at least one of HFC - 245cb or HFCS - 245eb and separation process of a mixture comprising HF HFC - 1234yf, HF and at least u M of HFC - 245cb or HFCS - 245eb</a> <b>[P]</b> . <span> 外国专利：  BRPI0906014A2 </span> <span> . 2015-06-30</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：包含HF和HFC的混合物的分离过程-1234yf，HFC-1234yf的分离过程，包含氟化氢和上述的1234yf的混合物，包含氟化氢和HF的混合物中的氟化氢的分离过程。 C-1234yf，从包含HFCS-1234yf和HF的混合物中纯化HFC-1234yf的过程。从HFC-1234yf和HF的混合物中纯化HF，分离HFC-1234yf的混合物HFC-1234yf，HF和HFC-245cb或HFCS-245eb中的至少一种以及包含HF HFC-1234yf，HF和至少1 M的HFC-245cb或HFCS-245eb的混合物的分离方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" 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Organic carbon preservation in SS outheastern AA rabian SS ea sediments since mid‐ HH olocene: II mplications to SS outh AA sian SS ummer MM onsoon variability

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