The Northern Gulf of Mexico During OAE2 and the Relationship Between Water Depth and Black Shale Development

Lowery Christopher M.; Cunningham Robert; Barrie Craig D.; Bralower Timothy; Snedden John W.

摘要

Abstract >Despite their name, Oceanic Anoxic Events (OAEs) are not periods of uniform anoxia and black shale deposition in ancient oceans. Shelf environments account for the majority of productivity and organic carbon burial in the modern ocean, and this was likely true in the Cretaceous as well. However, it is unlikely that the mechanisms for such an increase were uniform across all shelf environments. Some, like the northwest margin of Africa, were characterized by strong upwelling, but what might drive enhanced productivity on shelves not geographically suited for upwelling? To address this, we use micropaleontology, carbon isotopes, and sedimentology to present the first record of Oceanic Anoxic Event 2 (OAE2) from the northern Gulf of Mexico shelf. Here OAE2 occurred during the deposition of the well‐oxygenated, inner neritic/lower estuarine Lower Tuscaloosa Sandstone. The overlying organic‐rich oxygen‐poor Marine Tuscaloosa Shale is entirely Turonian in age. We trace organic matter enrichment from the Spinks Core into the deepwater Gulf of Mexico, where wireline log calculations and public geochemical data indicate organic enrichment and anoxia throughout the Cenomanian‐Turonian boundary interval. Redox change and organic matter preservation across the Gulf of Mexico shelf were driven by sea level rise prior to the early Turonian highstand, which caused the advection of nutrient‐rich, oxygen‐poor waters onto the shelf. This results in organic matter mass accumulation rates 1–2 orders of magnitude lower than upwelling sites like the NW African margin, but it likely occurred over a much larger geographic area, suggesting that sea level rise was an important component of the overall increase in carbon burial during OAE2. </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”xml：lang =“en”> <title类型=“main”>抽象</ title> >尽管他们的名字，海洋缺氧事件（OAES）不是均匀缺氧和黑色页岩的时期沉积在古代海洋。货架环境占现代海洋中大部分生产力和有机碳的埋葬，这也很可能在白垩纪中真实。然而，在所有货架环境中，这种增加的机制不太可能是均匀的。一些，如非洲西北边缘，以强烈的升值为特征，但是什么可能引发了在不适合上升的货架上提高生产力？为了解决这一点，我们使用微博口，碳同位素和沉积学，从墨西哥北部的北部北部的海洋缺氧事件2（OAE2）的第一次记录。这里发生OAE2在沉积良好的内核/下乙酸碱的豆油酸盐砂岩期间发生。覆盖的有机富含氧气贫困的海洋托斯卡罗萨斯（Tuscaloosa Sheale）在时代完全是Turonian。我们将烟囱核心追溯到墨西哥深水海湾的有机物富集，其中有线日志计算和公共地球化学数据表明了整个临曼诺县 - 涡轮界边界间隔的有机富集和贫血。墨西哥湾海湾的氧化还原变化和有机物质保存是在早期的涡轮增长前的海平面上升驱动，这导致营养丰富的氧气不良水的平流在架子上。这导致有机物质质量积累率1-2级数量级低于NW非洲边缘的上升网站，但它可能发生在更大的地理区域上，这表明海平面上升是碳总体增加的重要组成部分在OAE2期间埋葬。</ 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-28889/'>《Paleoceanography》</a> <b style="margin: 0 2px;">|</b><span>2017年第12期</span><b style="margin: 0 2px;">|</b><span>共20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=Lowery Christopher M.&option=202" target="_blank" rel="nofollow">Lowery Christopher M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cunningham Robert&option=202" target="_blank" rel="nofollow">Cunningham Robert;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barrie Craig D.&option=202" target="_blank" rel="nofollow">Barrie Craig D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bralower Timothy&option=202" target="_blank" rel="nofollow">Bralower Timothy;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Snedden John W.&option=202" target="_blank" rel="nofollow">Snedden John W.;</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>University of Texas Institute for GeophysicsAustin TX USA;</p> <p>ChargeSearch LLCLlano TX USA;</p> <p>GeoMark Research Ltd.Houston TX USA;</p> <p>Department of GeosciencesPennsylvania State UniversityUniversity Park PA USA;</p> <p>University of Texas Institute for GeophysicsAustin 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/166.html" title="海洋学">海洋学;</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=Cretaceous&option=203" rel="nofollow">Cretaceous;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oceanic Anoxic Events&option=203" rel="nofollow">Oceanic Anoxic Events;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleoredox&option=203" rel="nofollow">paleoredox;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gulf of Mexico&option=203" rel="nofollow">Gulf of Mexico;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=black shales&option=203" rel="nofollow">black shales;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea level&option=203" rel="nofollow">sea level;</a> </p> <div class="translation"> 机译：白垩纪;海洋缺氧事件;古罗统兴;墨西哥湾;黑色页岩;海平面; 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