Upper Ordovician continuous lithological succession in outer‐shelf facies, Yangtze Platform, South China: Facies changes and oceanographic reconstruction up to the Late Ordovician Hirnantian glaciation

Yu Shenyang; Chen Qing; Kershaw Stephen; Li Yue; Li Chao

摘要

Abstract > Ordovician sequences at Huanghuachang, northern Yichang City of Hubei Province, Central China, are representative of an outer‐shelf setting of the Yangtze epicontinental sea, South China Block. Continuous drill cores of the Well Yihuang 1 penetrated the Upper Ordovician units of the Miaopo, Pagoda, Linhsiang, Wufeng, and Kuanyinchiao Formations in ascending order. Such a continuous succession gives valuable insights into environmental changes and an extinction event through Late Ordovician time. Results suggest that sluggish circulation and oligotrophic conditions were characteristic of the region from Sandbian to early Hirnantian Epochs of the Late Ordovician. Thin‐bedded limestones within the Miaopo Formation shales and nodular limestones of the Pagoda and Linhsiang Formations are mainly wackestones and mudstones with sparse and fine‐grained trilobite, cephalopod, gastropod, ostracod, and crinoid bioclasts with rare brachiopod and bivalve bioclasts, further showing gradual decreasing in abundance and grain size upwards through the succession. Such biological and lithological changes are interpreted as a trend towards a deeper and calmer seafloor below storm wave‐base. The Kwangsian Orogeny of the late Katian Epoch altered the geography of the region, creating a large embayment in the area of the Well Yihuang 1 core. Thus the sequence developed upwards to the Wufeng Formation graptolitic black shales consistent with formation in a dysoxic and stagnant embayment that excluded carbonate production and benthic biota, but ideal for preservation of planktic graptolite fossils. Bioclastic packstone and quartz grain lenses interlayered with the black shales are occasionally sourced from southeastward shallow submarine highs closed to the Cathaysian Land. Change from this interpreted sluggish ocean circulation affecting the ocean floor was delayed to the early Hirnantia </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 Type =“Main”> HuanghuaChang，中国中部湖北省北部北部北部北部的黄花岗奥陶凡科序列是代表南方南部长江综合大海的外壳设置。连续钻井井y煌1穿过莫博，塔帕，临革，武力的上奥陶涅迪师单位，按升序升序。这种持续的继承使有价值的见解对环境变化以及通过延迟奥陶器时间的灭绝事项。结果表明，缓慢的循环和寡营性条件是桑太地区的特征，从后期奥陶诺维安的早期河流初中。莫泛形成中的薄层石灰岩和庞达和临革地层的结节石灰岩主要是疣罐和泥石，含有稀疏和细粒度的三叶虫，头部和细胞泡，蛇蛇族，雌激素生物燃料，具有罕见的Brachiopod和双抗体生物燃料，进一步展现了渐进的通过连续逐渐减少丰富和粒度。这种生物和岩性变化被解释为朝向暴风波底部下方更深和平静的海底的趋势。 Kwangsian Orogeny的歌舞屋纪元改变了该地区的地理位置，在益气1核心的井中创造了一个大的压力。因此，序列向上发射到武力地层甘龙龙黑色的Shales一致，与碳酸盐生产和底栖生物群的替代品和停滞的倒置中的形成一致，但适当的是保存浮躁鹰石体化石。与黑色神话中夹层的生物塑化包装和石英纹理镜片偶尔是从东南浅潜高度源于封闭的天使土地。从这种解释的缓慢的海洋循环发生变化，影响海底被推迟到六年早期 </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-30952/'>《The island arc》</a> <b style="margin: 0 2px;">|</b><span>2018年第5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=Yu Shenyang&option=202" target="_blank" rel="nofollow">Yu Shenyang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Qing&option=202" target="_blank" rel="nofollow">Chen Qing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kershaw Stephen&option=202" target="_blank" rel="nofollow">Kershaw Stephen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Yue&option=202" target="_blank" rel="nofollow">Li Yue;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Chao&option=202" target="_blank" rel="nofollow">Li Chao;</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>Key Laboratory of Economic Stratigraphy and Palaeogeography Nanjing Institute of Geology and PaleontologyChinese Academy of Sciences39 East Beijing Road Nanjing 210008 China;</p> <p>Key Laboratory of Economic Stratigraphy and Palaeogeography Nanjing Institute of Geology and PaleontologyChinese Academy of Sciences39 East Beijing Road Nanjing 210008 China;</p> <p>Department of Life Sciences Halsbury BuildingBrunel UniversityUxbridge UB8 3PH UK;</p> <p>Key Laboratory of Economic Stratigraphy and Palaeogeography Nanjing Institute of Geology and PaleontologyChinese Academy of Sciences39 East Beijing Road Nanjing 210008 China;</p> <p>Key Laboratory of Economic Stratigraphy and Palaeogeography Nanjing Institute of Geology and PaleontologyChinese Academy of Sciences39 East Beijing Road Nanjing 210008 China;</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>P313.7; </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=environmental parameters&option=203" rel="nofollow">environmental parameters;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=microfacies&option=203" rel="nofollow">microfacies;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=outer‐shelf of the Yangtze epicontinental sea&option=203" rel="nofollow">outer‐shelf of the Yangtze epicontinental sea;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South China block&option=203" rel="nofollow">South China block;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Upper Ordovician&option=203" rel="nofollow">Upper Ordovician;</a> </p> <div class="translation"> 机译：环境参数;Microfacies;长江外壳;华南区块;上奥陶省; 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