Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid‐Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)

Scaife J. D.; Ruhl M.; Dickson A. J.; Mather T. A.; Jenkyns H. C.; Percival L. M. E.; Hesselbo S. P.; Cartwright J.; Eldrett J. S.; Bergman S. C.; Minisini D.

摘要

Abstract >Oceanic Anoxic Event 2 (OAE 2), during the Cenomanian‐Turonian transition (～94 Ma), was the largest perturbation of the global carbon cycle in the mid‐Cretaceous and can be recognized by a positive carbon‐isotope excursion in sedimentary strata. Although OAE 2 has been linked to large‐scale volcanism, several large igneous provinces (LIPs) were active at this time (e.g., Caribbean, High Arctic, Madagascan, Ontong‐Java) and little clear evidence links OAE 2 to a specific LIP. The Mid‐Cenomanian Event (MCE, ～96 Ma), identified by a small, 1‰ positive carbon‐isotope excursion, is often referred to as a prelude to OAE 2. However, no underlying cause has yet been demonstrated and its relationship to OAE 2 is poorly constrained. Here we report sedimentary mercury (Hg) concentration data from four sites, three from the southern margin of the Western Interior Seaway and one from Demerara Rise, in the equatorial proto‐North Atlantic Ocean. We find that, in both areas, increases in mercury concentrations and Hg/TOC ratios coincide with the MCE and the OAE 2. However, the increases found in these sites are of a lower magnitude than those found in records of many other Mesozoic events, possibly characteristic of a marine rather than atmospheric dispersal of mercury for both events. Combined, the new mercury data presented here are consistent with an initial magmatic pulse at the time of the MCE, with a second, greater pulse at the onset of OAE 2, possibly related to the emplacement of LIPs in the Pacific Ocean and/or the High Arctic. </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> >海洋缺氧事件2（OAE 2），在CENOMANIAN-Turonian过渡（〜94 mA）期间，中白垩纪中全球碳循环的最大扰动，可以通过阳性碳 - 同位素偏移来识别沉积层。虽然OAE 2已经与大规模的火山有关，但此时几个大的火油省（嘴唇）是活跃的（例如，加勒比，高北极，马达加斯州，Ontong-Java）和少量清晰的证据将OAE 2链接到特定唇部。由小1‰阳性碳 - 同位素偏移鉴定的中肠道事件（MCE，〜96 mA）通常被称为OAE 2的前奏。然而，没有证明潜在的事业及其关系OAE 2受到严重受损。在这里，我们在赤道原始北大西洋中报告了来自西部内部海路的四个地点的沉积汞（Hg）浓度数据，其中三个地点，其中一个来自Demerara崛起的地点。我们发现，在这两个领域，汞浓度的增加和Hg / toc比率与MCE和OAE 2重合。然而，这些位点中发现的增加比在许多其他中生代事件的记录中发现的那些较低的数量较小，可能是海洋的特征，而不是两种事件的汞的大气分散。结合，这里呈现的新的汞数据与MCE时的初始岩浆脉冲一致，其在OAE 2的发作时具有第二，更大的脉冲，可能与太平洋嘴唇的施加有关和/或高北极。</ 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12期</span><b style="margin: 0 2px;">|</b><span>共23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=Scaife J. D.&option=202" target="_blank" rel="nofollow">Scaife J. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ruhl M.&option=202" target="_blank" rel="nofollow">Ruhl M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dickson A. J.&option=202" target="_blank" rel="nofollow">Dickson A. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mather T. A.&option=202" target="_blank" rel="nofollow">Mather T. A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jenkyns H. C.&option=202" target="_blank" rel="nofollow">Jenkyns H. C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Percival L. M. E.&option=202" target="_blank" rel="nofollow">Percival L. M. E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hesselbo S. P.&option=202" target="_blank" rel="nofollow">Hesselbo S. P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cartwright J.&option=202" target="_blank" rel="nofollow">Cartwright J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eldrett J. S.&option=202" target="_blank" rel="nofollow">Eldrett J. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bergman S. C.&option=202" target="_blank" rel="nofollow">Bergman S. C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Minisini D.&option=202" target="_blank" rel="nofollow">Minisini 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>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Camborne School of Mines and Environment and Sustainability InstituteUniversity of ExeterPenryn UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Shell International Exploration &</p> <p>Production B.VRijswijk GS the Netherlands;</p> <p>Now at Shell R&</p> <p>D HoustonVashon WA USA;</p> <p>Shell International Exploration and Production Inc.Houston TX USA;</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=ocean circulation&option=203" rel="nofollow">ocean circulation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oceanic Anoxic Event 2 (OAE 2)&option=203" rel="nofollow">Oceanic Anoxic Event 2 (OAE 2);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=global carbon‐cycle change&option=203" rel="nofollow">global carbon‐cycle change;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cenomanian‐Turonian&option=203" rel="nofollow">Cenomanian‐Turonian;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=large igneous province (LIP) volcanism&option=203" rel="nofollow">large igneous province (LIP) volcanism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcanic mercury enrichment&option=203" rel="nofollow">volcanic mercury enrichment;</a> </p> <div class="translation"> 机译：海洋循环;海洋缺氧事件2（OAE 2）;全球碳循环变化;CENOMANIANIAN-Turonian;大火植物（唇）火山岩;火山汞浓缩; </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/0704023360315.html">Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? 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