New evidence of sea‐level lowstands and paleoenvironment during MIS 6 and 4 in the Cantabrian coastal karst: the Cobiheru cave (North Iberia)

机译：在坎巴琳沿海喀斯特喀斯特喀斯特第6和4段期间海拔地区和古环境的新证据：Cobiheru Cave（North Iberia）

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Abstract > The geomorphological evolution of the Cobiheru Cave shows the influence of the non‐carbonate coastal mountain ranges on coastal karst evolution, as well as the temporal distribution of the cold‐adapted fauna sites in the Cantabrian Coast. Geomorphological observation and uranium/thorium (U/Th) dating lead to the construction of an evolution model. The model comprises two episodes of cave deposition occurring at c. 60–70 and 130–150?ka, linked to cold climate conditions, global sea‐level lowstands and the erosion of alluvial fans that covered the karst. Moreover, the comparison between the Cobiheru record and some raised beaches identified in previous studies sets the beginning of the sea‐level lowering in the Cantabrian Sea during the marine isotope stages (MIS) 5–4 transition. Two palaeoenvironments are inferred based on finding Equus ferus and Elona quimperiana . A wet deciduous forest would have developed on the emerged marine terrace of the Cobiheru Cave since at least the Middle Pleistocene, and an open landscape with scarce vegetation would have been present at c. 65?ka. The erosional event identified in the Cobiheru Cave helps to understand the temporal distribution of cold‐adapted mammals located in the Asturias region. The probable sites of cold‐adapted fauna developed in caves and alluvial fans would have disappeared after 65?ka. Therefore, palaeontological and palaeoclimate research based on cold‐adapted mammals suggests the occurrence of an hiatus in the palaeontological record prior to 50?ka. Copyright ? 2017 John Wiley & Sons, Ltd. </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”> <title type =“main”>抽象</ title> > Cobiheru洞穴的地貌演变显示非碳酸盐沿海山脉对沿海喀斯特演进的影响，以及坎塔布里亚海岸的冷适应动物区网站的时间分布。地貌观察和铀/钍（U / T）约会导致进化模型的构建。该模型包括在 c中发生的两集裂解沉积。</ i> 60-70和130-150？Ka，与寒冷的气候条件，全球海平面低位和覆盖喀斯特覆盖的冲积球迷的侵蚀相关联。此外，在先前研究中确定的Cobiheru记录和一些凸起的海滩之间的比较设定了在海洋同位素阶段（MIS）过渡期间Cantabrian海中的海平面的开头。基于发现 equus ferus </ i>和elona quimperiana </ i>，推断出两个古环境。湿落叶林将在雪氏洞穴的出现的海洋露台上开发，因为至少是中间人世代，以及缺乏植被的开放景观将存在于 c。</ i> 65？ka。 Cobiheru洞穴中鉴定的侵蚀事件有助于了解位于阿斯图里亚斯区的冷适应哺乳动物的时间分布。在洞穴和冲积球迷中发育的冷适应的动物的可能性位点在65岁后会消失。因此，基于冷适应哺乳动物的古生物学和古爱罗长研究表明，在50℃之前的古生物学记录中的发生发生。版权？ 2017年John Wiley＆amp; SONS，LTD。</ 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-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共13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=Ballesteros Daniel&option=202" target="_blank" rel="nofollow">Ballesteros Daniel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rodríguez‐Rodríguez Laura&option=202" target="_blank" rel="nofollow">Rodríguez‐Rodríguez Laura;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=González‐Lemos Saúl&option=202" target="_blank" rel="nofollow">González‐Lemos Saúl;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Giralt Santiago&option=202" target="_blank" rel="nofollow">Giralt Santiago;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=álvarez‐Lao Diego Jaime&option=202" target="_blank" rel="nofollow">álvarez‐Lao Diego Jaime;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Adrados Luna&option=202" target="_blank" rel="nofollow">Adrados Luna;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiménez‐Sánchez Montserrat&option=202" target="_blank" rel="nofollow">Jiménez‐Sánchez Montserrat;</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>GeologyUniversity of OviedoOviedo Spain;</p> <p>GeologyUniversity of OviedoOviedo Spain;</p> <p>GeologyUniversity of OviedoOviedo Spain;</p> <p>Environmental Geology and GeohazardsInstituto de Ciencias de la Tierra Jaume AlmeraBarcelona Spain;</p> <p>GeologyUniversity of OviedoOviedo Spain;</p> <p>Turismo geológico GEOLAGOviedo Spain;</p> <p>GeologyUniversity of OviedoOviedo 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=coastal karst&option=203" rel="nofollow">coastal karst;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Equus ferus&option=203" rel="nofollow">Equus ferus;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Elona quimperiana&option=203" rel="nofollow">Elona quimperiana;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=palaeoenvironment&option=203" rel="nofollow">palaeoenvironment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea level lowstand&option=203" rel="nofollow">sea level lowstand;</a> </p> <div class="translation"> 机译：沿海喀斯特;Equus ferus;elona quimperiana;Palaeenvironment;海平面; </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 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