Timing of arrival of the Danube to the Black Sea: Provenance of sediments from        <fc xmlns='http://www.wiley.com/namespaces/wiley'>DSDP</fc>DSDP        site 380/380A

Leeuw Arjan; Morton Andrew; Baak Christiaan G. C.; Vincent Stephen J.

摘要

Abstract > Estimates for the timing of the arrival of Danube sediment to the Black Sea range from Messinian to Pleistocene; the river is currently the largest sediment contributor, supplying 88? <fc>MT</fc> /yr. We identify two changes in siltstone provenance‐sensitive heavy mineral abundances at <fc>DSDP</fc> site 380/380A in the southwest Black Sea. Comparison with modern river sediment compositions indicates that siltstones above 571.5?mbsf (metres below sea floor) were supplied by the Danube, while sediments below 651.0?m were sourced by other supply systems. Palaeo‐magnetic, 40 Ar/ 39 Ar and biostratigraphic data reveal that the influx of Danube‐supplied sediment to the southwest Black Sea began between 4.36?±?0.19?Ma and 1?Ma ago (Zanclean–Calabrian). Our results provide an independent time constraint on palaeogeographic reconstructions of the Pannonian and Dacian basins, which acted as upstream sediment sinks, and suggest that significant volumes of Danube‐supplied sediment only started to reach the Black Sea at least 1?Ma after the Messinian Salinity Crisis (5.971–5.33?Ma) had ended. </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:id=“ter12314-abs-0001”xml:lang=“en”><title type=“main”“>摘要>对多瑙河沉积物到达黑海的时间从墨西尼安期到更新世的估计；多瑙河目前是最大的沉积物贡献者，每年供应88？<fc>MT</fc>。我们确定了两个变化，即黑海西南部。与现代河流沉积物成分的比较表明，571.5？以上的粉砂岩？mbsf（海底以下米）由多瑙河供应，而651.0以下的沉积物？m来自其他供应系统。古地磁、40Ar/39Ar和生物地层学数据显示，多瑙河供应的沉积物流入黑海西南部始于4.36？±?0.19?妈和1？Ma ago（Zanclean–卡拉布里亚）。我们的结果为Pannonian和Dacian盆地的古地理重建提供了独立的时间限制，这两个盆地充当了上游沉积物汇，并表明大量多瑙河供应的沉积物仅开始到达黑海至少1？在墨西哥人盐度危机（5.971–5.33？Ma）结束后 </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-30393/'>《Terra Nova》</a> <b style="margin: 0 2px;">|</b><span>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共11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=Leeuw Arjan&option=202" target="_blank" rel="nofollow">Leeuw Arjan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Morton Andrew&option=202" target="_blank" rel="nofollow">Morton Andrew;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Baak Christiaan G. C.&option=202" target="_blank" rel="nofollow">Baak Christiaan G. C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vincent Stephen J.&option=202" target="_blank" rel="nofollow">Vincent Stephen J.;</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>CASPCambridge UK;</p> <p>CASPCambridge UK;</p> <p>Paleomagnetic Laboratory “Fort Hoofddijk”Utrecht UniversityUtrecht The Netherlands;</p> <p>CASPCambridge UK;</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/14.html" title="天文学、地球科学">天文学、地球科学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> </p> </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024722652.html">Timing of arrival of the Danube to the Black Sea: Provenance of sediments from <fc xmlns="http://www.wiley.com/namespaces/wiley">DSDP</fc>DSDP site 380/380A</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leeuw Arjan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Leeuw Arjan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Morton Andrew&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Morton Andrew,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Baak Christiaan G. 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C.,</a> <a href="/journal-foreign-30393/" target="_blank" rel="nofollow" class="tuijian_authcolor">Terra Nova .</a> <span>2018</span><span>,第2期</span> </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：多瑙河到黑海的时间：<FC XMLNS =“http://www.wiley.com/namespaces/wiley”> dsdp </ fc> DSDP站点380/380a的沉积物来源</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704029088303.html"><fc xmlns="http://www.wiley.com/namespaces/wiley">Z</fc>Z ygomatic <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A rch <fc xmlns="http://www.wiley.com/namespaces/wiley">C</fc>C ortical <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A rea and <fc xmlns="http://www.wiley.com/namespaces/wiley">D</fc>D iet in <fc xmlns="http://www.wiley.com/namespaces/wiley">H</fc>H aplorhines</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Edmonds Hallie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Edmonds Hallie </a> <a href="/journal-foreign-30476/" target="_blank" rel="nofollow" class="tuijian_authcolor">The anatomical record: advances in integrative anatomy and evolutionary biology .</a> <span>2016</span><span>,第12期</span> </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：<fc xmlns =“http://www.wiley.com/namespaces/wiley”> z </ fc> z ygomic <fc xmlns =“http://www.wiley.com/namespaces/wiley”> a </ FC> RCH <FC XMLNS =“http://www.wiley.com/namespaces/wiley”> c </ fc> c Ortical <fc xmlns =“http://www.wiley.com/namespaces/wiley” > a </ fc> rea和<fc xmlns =“http://www.wiley.com/namespaces/wiley”> d </ fc> d iet在<fc xmlns =“http：//www.wiley中。 com /命名空间/ wiley“> h </ fc> h aplorhines</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024745020.html"><fc xmlns="http://www.wiley.com/namespaces/wiley">Z</fc>Z ygomatic <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A rch <fc xmlns="http://www.wiley.com/namespaces/wiley">C</fc>C ortical <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A rea and <fc xmlns="http://www.wiley.com/namespaces/wiley">D</fc>D iet in <fc xmlns="http://www.wiley.com/namespaces/wiley">H</fc>H aplorhines</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Edmonds Hallie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Edmonds Hallie </a> <a href="/journal-foreign-30476/" target="_blank" rel="nofollow" class="tuijian_authcolor">The anatomical record: advances in integrative anatomy and evolutionary biology .</a> <span>2016</span><span>,第12期</span> </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：<fc xmlns =“http://www.wiley.com/namespaces/wiley”> z </ fc> z ygomic <fc xmlns =“http://www.wiley.com/namespaces/wiley”> a </ FC> RCH <FC XMLNS =“http://www.wiley.com/namespaces/wiley”> c </ fc> c Ortical <fc xmlns =“http://www.wiley.com/namespaces/wiley” > a </ fc> rea和<fc xmlns =“http://www.wiley.com/namespaces/wiley”> d </ fc> d iet在<fc xmlns =“http：//www.wiley中。 com /命名空间/ wiley“> h </ fc> h aplorhines</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000124695778.html">Timing of arrival of the Danube to the Black Sea: Provenance of sediments from DSDP site 380/380A</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arjan de Leeuw&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Arjan de Leeuw,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Andrew Morton&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Andrew Morton,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Christiaan G. 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Timing of arrival of the Danube to the Black Sea: Provenance of sediments from DSDPDSDP site 380/380A

摘要