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</ title> >估计多瑙河沉积物到达黑海的时间从Messinian到Pleistocene的时间;这条河流是最大的沉积物，供应88？ <FC> MT </ FC> / YR。我们在西南黑海中识别<FC> DSDP </ FC>位点380 / 380A的硅土出处敏感重型矿物丰富的两种变化。与现代河沉积物组成的比较表明，多瑙河提供571.5？MBSF（海底低于海底米）的硅灰石，而其他供应系统则采购低于651.0米以下的沉积物。 Palaeo-mangety， 40 </ sup> Ar / 39 </ sup> AR和生物数据库数据表明，西南黑海西南黑海的多瑙河供应沉积物的涌入在4.36？±0.19？ma和1？MA之前（Zanclean-Calabrian）。我们的结果为Pannonian和Dacian盆地的古地理重建提供了一个独立的时间限制，它充当上游沉积物沉积物，并表明在Messinian盐度之后，仅开始到达黑海的多瑙河供应沉积物。危机（5.971-5.33？ma）结束了。 </ p> </ 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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Timing of arrival of the Danube to the Black Sea: Provenance of sediments from DSDPDSDP site 380/380A

摘要