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首页> 外文期刊>Geochemistry, geophysics, geosystems >Constraining the Timing and Amplitude of Early Serpukhovian Glacioeustasy With a Continuous Carbonate Record in Northern Spain
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Constraining the Timing and Amplitude of Early Serpukhovian Glacioeustasy With a Continuous Carbonate Record in Northern Spain

机译：利用北西班牙连续碳酸盐血液甘露甘露甘露糖的定时和幅度

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Abstract > During the Late Paleozoic Ice Age (LPIA, 345–260 Ma), an expansion of ice house conditions at ～330 Ma caused a nearly synchronous, global unconformity. Subaerially exposed paleotropical carbonates were dissolved by meteoric waters, mixed with the light terrestrial carbon, and recrystallized with overprinted, diagenetic <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21592:ggge21592-math-0001" wiley:location="equation/ggge21592-math-0001.png"> <mat:mrow> <mat:msup> <mat:mi>δ</mat:mi> <mat:mrow> <mat:mn>13</mat:mn> </mat:mrow> </mat:msup> </mat:mrow> </mat:math> C values. In Northern Spain, development of a rapidly subsiding foreland basin kept local sea level relatively high, allowing continuous carbonate deposition to record <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21592:ggge21592-math-0002" wiley:location="equation/ggge21592-math-0002.png"> <mat:mrow> <mat:msup> <mat:mi>δ</mat:mi> <mat:mrow> <mat:mn>13</mat:mn> </mat:mrow> </mat:msup> </mat:mrow> </mat:math> C without meteoric overprint. The Spanish sections show a 2‰ increase in <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21592:ggge21592-math-0003" wiley:location="equation/ggge21592-math-0003.png"> <mat:mrow> <mat:msup> <mat:mi>δ</mat:mi> <mat:mrow> <mat:mn>13</mat:mn> </mat:mrow> </mat:msup> </mat:mrow> </mat:math> C that can be modeled as the ocean's response to the creation of a significant light carbon sink through widespread meteoric diagenesis of marine carbonates during the near‐global hiatus. About 15–35 m of sea level fall would have exposed a large enough volume of carbonate to account for the positive excursion in <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21592:ggge21592-math-0004" wiley:location="equation/ggge21592-math-0004.png"> <mat:mrow> <mat:msup> <mat:mi>δ</mat:mi> <mat:mrow> <mat:mn>13</mat:mn> </mat:mrow> </mat:msup> </mat:mrow> </mat:math> C of oceanic DIC. Combining the <mat:math display="inline" altimg="urn:x-wiley:15252027:media:ggge21592:ggge21592-math-0005" wiley:location="equation/ggge21592-math-0005.png"> <mat:mrow> <mat:msup> <mat:mi>δ</mat:mi> <mat:mrow> <mat:mn>13</mat:mn> </mat:mrow> </mat:msup> </mat:mrow> </mat:math> C data with high resolution biostratigraphy and new ID‐TIMS U‐Pb zircon ages from interbedded tuffs, we calculate that the depositional hiatus and glacioeustatic fall caused by the early Serpukhovian phase of ice growth lasted for approximately 3.5 My. </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”> <标题类型=“main”>抽象</ title> > 在晚古生代冰河时代（LPIA，345-260 MA），〜330 mA的冰屋状况的扩展导致几乎同步，全球无关。将亚型暴露的古雌碳酸碳酸酯溶解在一起，与光陆碳混合，并用叠印重新结晶，呈重写，成岩 <mat：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：GGGE21592：GGGE21592-Math-0001”Wiley：Location =“等式/ GGGE21592-Math-0001.png”> <MAT：MROW> <mat：msup> <mat：mi>δ</ mat：mi> <MAT：MROW> <MAT：MN> 13 </ MAT：MN> </ mat：MROW> </ mat：msup> </ mat：MROW> </ mat：math> C值。在西班牙北部，迅速消退的前陆盆地的发展使当地海平面相对较高，允许连续碳酸盐沉积记录 <mat：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：GGGE21592：GGGE21592-Math-0002”Wiley：Location =“等式/ GGGE21592-Math-0002.png”> <MAT：MROW> <mat：msup> <mat：mi>δ</ mat：mi> <MAT：MROW> <MAT：MN> 13 </ MAT：MN> </ mat：MROW> </ mat：msup> </ mat：MROW> </ mat：math> c没有血流叠印。西班牙部分显示出2¼增加 <mat：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：媒体：GGGE21592：GGGE21592-Math-0003”Wiley：Location =“等式/ GGGE21592-Math-0003.png”> <MAT：MROW> <mat：msup> <mat：mi>δ</ mat：mi> <MAT：MROW> <MAT：MN> 13 </ MAT：MN> </ mat：MROW> </ mat：msup> </ mat：MROW> </ mat：math> C，可以通过在近全球性的中断期间通过海洋碳酸盐的广泛的Meaoric成岩作用来建模作为海洋对创建显着的轻碳沉没的反应。大约15-35米的海平面秋季将暴露足够大量的碳酸盐，以解释积极的偏移 <MAT：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：媒体：GGGE21592：GGGE21592-Math-0004”Wiley：Location =“等式/ GGGE21592-Math-0004.png”> <MAT：MROW> <mat：msup> <mat：mi>δ</ mat：mi> <MAT：MROW> <MAT：MN> 13 </ MAT：MN> </ mat：MROW> </ mat：msup> </ mat：MROW> </ mat：math> 海洋DIC的C.结合了 <mat：数学显示=“内联”Altimg =“URN：X-Wiley：15252027：媒体：GGGE21592：GGGE21592-Math-0005”Wiley：Location =“等式/ GGGE21592-Math-0005.png”> <MAT：MROW> <mat：msup> <mat：mi>δ</ mat：mi> <MAT：MROW> <MAT：MN> 13 </ MAT：MN> </ mat：MROW> </ mat：msup> </ mat：MROW> </ mat：math> C数据具有高分辨率生物数据和新的ID-TIMS U-PB锆锆，我们从腹部凝固中衰减，我们计算沉积的中断和由早期Serpukhovian的冰增长阶段持续约3.5。 </ 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>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共14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=Campion Alison&option=202" target="_blank" rel="nofollow">Campion Alison;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Maloof Adam&option=202" target="_blank" rel="nofollow">Maloof Adam;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schoene Blair&option=202" target="_blank" rel="nofollow">Schoene Blair;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oleynik Sergey&option=202" target="_blank" rel="nofollow">Oleynik Sergey;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sanz‐López Javier&option=202" target="_blank" rel="nofollow">Sanz‐López Javier;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Blanco‐Ferrera Silvia&option=202" target="_blank" rel="nofollow">Blanco‐Ferrera Silvia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Merino‐Tomé Oscar&option=202" target="_blank" rel="nofollow">Merino‐Tomé Oscar;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bahamonde Juan Ramón&option=202" target="_blank" rel="nofollow">Bahamonde Juan Ramón;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fernández Luis Pedro&option=202" target="_blank" rel="nofollow">Fernández Luis Pedro;</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 GeosciencesPrinceton UniversityPrinceton NJ USA;</p> <p>Department of GeosciencesPrinceton UniversityPrinceton NJ USA;</p> <p>Department of GeosciencesPrinceton UniversityPrinceton NJ USA;</p> <p>Department of GeosciencesPrinceton UniversityPrinceton NJ USA;</p> <p>Departmento de GeologiaUniversidad de Oviedo c/Jesús Arias de Velasco s/nOviedo Spain;</p> <p>Departmento de GeologiaUniversidad de Oviedo c/Jesús Arias de Velasco s/nOviedo Spain;</p> <p>Departmento de GeologiaUniversidad de Oviedo c/Jesús Arias de Velasco s/nOviedo Spain;</p> <p>Departmento de GeologiaUniversidad de Oviedo c/Jesús Arias de Velasco s/nOviedo Spain;</p> <p>Departmento de GeologiaUniversidad de Oviedo c/Jesús Arias de Velasco s/nOviedo Spain;</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=Carboniferous&option=203" rel="nofollow">Carboniferous;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=meteoric diagenesis&option=203" rel="nofollow">meteoric diagenesis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Glacioeustasy&option=203" rel="nofollow">Glacioeustasy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=CA‐ID‐TIMS U‐Pb analyses&option=203" rel="nofollow">CA‐ID‐TIMS U‐Pb analyses;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Late Paleozoic Ice Age&option=203" rel="nofollow">Late Paleozoic Ice Age;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cantabrian Zone&option=203" rel="nofollow">Cantabrian Zone;</a> </p> <div class="translation"> 机译：石炭系;嗜睡;冰川般的;CA-ID-TIMS U-PB分析;晚古生代冰河时代;坎塔布里亚区; </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> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360477.html">Constraining the Timing and Amplitude of Early Serpukhovian Glacioeustasy With a Continuous Carbonate Record in Northern Spain</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Campion Alison&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Campion Alison,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Maloof Adam&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Maloof Adam,</a> <a 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