Late Holocene changes in vegetation and atmospheric circulation at Lake Uddelermeer (The Netherlands) reconstructed using lipid biomarkers and compound‐specific δD analysis

van den Bos V.; Engels S.; Bohncke S. J. P.; Cerli C.; Jansen B.; Kalbitz K.; Peterse F.; Renssen H.; Sachse D.

摘要

ABSTRACT <section xml:id="jqs3006-sec-0001"> > We reconstructed middle to late Holocene changes in atmospheric circulation patterns and vegetation in north‐west Europe by applying novel geochemical techniques to the sediment record of Lake Uddelermeer (The Netherlands). A comparison of higher plant‐derived leaf wax n ‐alkane distributions archived in the lake sediments with those in living plant material, combined with palynological analysis, indicates that the vegetation immediately surrounding the lake became more open at 3150?cal?a <sc>?BP</sc> , while the regional vegetation responded more gradually and ～650 years later. Our record of the hydrogen isotopic composition of plant leaf waxes (δD <sub>wax</sub> ) shows a deuterium enrichment starting from 3500?cal?a? <sc>BP</sc> , which we interpret as a change in atmospheric circulation. A similar δD <sub>wax</sub> record from nearby Meerfelder Maar (Germany) shows an opposite trend around this time, which could be explained by a change in sea‐level pressure resembling a negative North Atlantic Oscillation phase. This could account for depleted δD values of precipitation at Meerfelder Maar, while confounding factors related to the more maritime position of Uddelermeer cause the opposite shift there. </section> </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 XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”xml：lang =“en”> <title type =“main”>抽象</ title> <section XML：ID =“JQS3006-SEC-0001”> <P>我们通过将新的地球化学技术应用于UddeLermeer（荷兰）的沉积物记录，将中北部的大气循环模式和植被中的中间到后期全新世。比较高等植物衍生的叶片蜡 n </ i> - 链团分布在湖泊沉积物中，与生物植物材料中的沉积物，结合腭学分析，表明湖泊周围的植被在3150时变得更加开放？Cal？a <sc>？bp </ sc>，而区域植被逐渐响应〜650年。我们对植物叶蜡的氢同位素组成的记录（ΔD<sub> wax </ sub>）显示从3500？cal开始的氘富集？a？ <sc> bp </ sc>，我们将其解释为大气循环的变化。来自Meerfelder Maar（德国）附近的类似Δd<sub>蜡</ sub>记录围绕此时的相反趋势，可以通过类似于负北大西洋振荡阶段的海平压力的变化来解释。这可能考虑在Meerfelder Maar的耗尽ΔD值，而与UddeLermeer的更多海上位置相关的混淆因素导致相反的换档。 </ p> </ section> </ abstract> </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-35770/'>《Journal of quaternary science: JQS 》</a> <b style="margin: 0 2px;">|</b><span>2018年第1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=van den Bos V.&option=202" target="_blank" rel="nofollow">van den Bos V.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Engels S.&option=202" target="_blank" rel="nofollow">Engels S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bohncke S. J. P.&option=202" target="_blank" rel="nofollow">Bohncke S. J. P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cerli C.&option=202" target="_blank" rel="nofollow">Cerli C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jansen B.&option=202" target="_blank" rel="nofollow">Jansen B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kalbitz K.&option=202" target="_blank" rel="nofollow">Kalbitz K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peterse F.&option=202" target="_blank" rel="nofollow">Peterse F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Renssen H.&option=202" target="_blank" rel="nofollow">Renssen H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sachse D.&option=202" target="_blank" rel="nofollow">Sachse D.;</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>Institute for Biodiversity and Ecosystem DynamicsUniversity of AmsterdamAmsterdam The Netherlands;</p> <p>Institute for Biodiversity and Ecosystem DynamicsUniversity of AmsterdamAmsterdam The Netherlands;</p> <p>Department of Earth SciencesVU University AmsterdamAmsterdam The Netherlands;</p> <p>Institute for Biodiversity and Ecosystem DynamicsUniversity of AmsterdamAmsterdam The Netherlands;</p> <p>Institute for Biodiversity and Ecosystem DynamicsUniversity of AmsterdamAmsterdam The Netherlands;</p> <p>Institute for Biodiversity and Ecosystem DynamicsUniversity of AmsterdamAmsterdam The Netherlands;</p> <p>Department of Earth SciencesUtrecht UniversityUtrecht The Netherlands;</p> <p>Department of Earth SciencesVU University AmsterdamAmsterdam The Netherlands;</p> <p>Helmholtz Centre PotsdamGFZ German Research Centre for GeosciencesSection 5.1 Geomorphology Potsdam Germany;</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/27341.html" title="第四纪（系）">第四纪（系） ;</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=atmospheric circulation&option=203" rel="nofollow">atmospheric circulation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=compound‐specific δD analysis&option=203" rel="nofollow">compound‐specific δD analysis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lipid biomarkers&option=203" rel="nofollow">lipid biomarkers;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=North Atlantic Oscillation&option=203" rel="nofollow">North Atlantic Oscillation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=north‐west Europe&option=203" rel="nofollow">north‐west Europe;</a> </p> <div class="translation"> 机译：大气循环;特定于复合ΔD分析;脂质生物标志物;北大西洋振荡;西北欧洲; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025842344.html">Late Holocene changes in vegetation and atmospheric circulation at Lake Uddelermeer (The Netherlands) reconstructed using lipid biomarkers and compound‐specific δD analysis</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=van den Bos V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">van den Bos V.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Engels S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Engels S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bohncke S. 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