| 赫南特冰期古海洋环境转变及其成因机制研究现状 |
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| 引用本文： | 杨向荣,严德天,张利伟,张宝,徐翰文,刘文慧,郧嘉琳.赫南特冰期古海洋环境转变及其成因机制研究现状[J].沉积学报,2018,36(2):319-332. |
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| 作者姓名： | 杨向荣 严德天 张利伟 张宝 徐翰文 刘文慧 郧嘉琳 |
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| 作者单位： | 中国地质大学(武汉)构造与油气资源教育部重点实验室, 武汉 430070 |
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| 基金项目： | 国家自然科学基金项目，National Natural Science Foundation of China |
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| 摘 要： | 奥陶纪-志留纪转折期是地质历史时期一个重要的时间节点，形成了广为人知的赫南特冰期。该冰期的形成不仅诱发了显生宙第二大的两幕生物绝灭事件，同样使海水中的地球化学元素循环受到强烈的影响，如海洋碳酸盐与大气CO2的循环受到扰动，全球海平面的降低促使水体逐渐富氧化，进而导致海洋水体Mo、S、U等同位素值出现波动，而冈瓦纳大陆被冰雪大面积覆盖则削弱了铝硅酸盐岩的风化作用，并限制了陆壳放射性187Os、87Sr同位素向海水的运移。赫南特冰期的成因一直是学界探讨的热点，被归结于风化作用、火山活动的增强或有机碳的大量埋藏等因素，但对冰期的成因机制与持续时间仍具有较多的争论，其原因很多，比如缺乏独立的生物地层单元同时能够控制浅水碳酸盐岩及深水泥页岩区，缺少转折界限处高精度的地球化学信息与全球等时地层格架下的对比，以及未能排除风化作用、成岩作用和构造热事件对古海洋与古气候重建时的扰动等。
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| 关 键 词： | 赫南特冰期 古海洋环境 晚奥陶世 生物灭绝 |
| 收稿时间： | 2017-06-10 |
The Genesis of Hirnantian Glaciation and Paleo-Ocean Environment During Ordovician-Silurian Transition |
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| YANG XiangRong,YAN DeTian,ZHANG LiWei,ZHANG Bao,XU HanWen,LIU WenHui,YUN JiaLin.The Genesis of Hirnantian Glaciation and Paleo-Ocean Environment During Ordovician-Silurian Transition[J].Acta Sedimentologica Sinica,2018,36(2):319-332. |
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| Authors: | YANG XiangRong YAN DeTian ZHANG LiWei ZHANG Bao XU HanWen LIU WenHui YUN JiaLin |
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| Institution: | Key Laboratory of Tectonics and Petroleum Resources Ministry of Education, China University of Geosciences, Wuhan 430070, China |
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| Abstract: | The Ordovician-Silurian transition was an interval which revealed major changes in the Earth's biotic,cli-matic,and environmental systems,triggering the Hirnantian glaciation and end-Ordovician mass extinctions.The pa-leo-ocean environment experienced intense shift and exerted a crucial impact on the global cycles of carbon,molybde-num and sulfur during O-S transition.In addition,the weakness of continental weathering reduced 187Os and 87Sr flux, resulting in positive δ187Os and δ87Sr excursions.This first ice age,since the late Neoproterozoic,was the culmination of a cooling trend that had begun in the early or middle Ordovician,and was linked to some combination of reduced volcanic arc outgassing,enhanced silicate weathering, increased organic carbon burial and so on.There exist many problems about the genesis of Hirnantian glaciation,such as lacking in individual biostratigraphy which can control the carbonate platform in shallow water and mudstone in deep water simultaneously,as well as the high-precision analysis based on geochemical proxies and isochronous stratigraphic correlation.Meanwhile diagenesis,weathering and tecton-ic-thermal events also exerted an important impact on reconstruction of Hirnantian glaciation, resulting in inaccurate interpretation. |
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