新元古代重大地质事件及其与生物演化的耦合关系

叶云涛; 王华建; 翟俪娜; 周文喜; 王晓梅; 张水昌; 吴朝东

doi:10.14027/j.cnki.cjxb.2017.02.001

ISSN 1000-0550 CN 62-1038/P

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新元古代重大地质事件及其与生物演化的耦合关系

叶云涛, 王华建, 翟俪娜, 周文喜, 王晓梅, 张水昌, 吴朝东

文章导航 > 沉积学报 > 2017 > 35(2): 203-216

叶云涛, 王华建, 翟俪娜, 周文喜, 王晓梅, 张水昌, 吴朝东. 新元古代重大地质事件及其与生物演化的耦合关系[J]. 沉积学报, 2017, 35(2): 203-216. doi: 10.14027/j.cnki.cjxb.2017.02.001

引用本文:

YE YunTao, WANG HuaJian, ZHAI LiNa, ZHOU WenXi, WANG XiaoMei, ZHANG ShuiChang, WU ChaoDong. Geological Events and Their Biological Responses During the Neoproterozoic Era[J]. Acta Sedimentologica Sinica, 2017, 35(2): 203-216. doi: 10.14027/j.cnki.cjxb.2017.02.001

Citation:

YE YunTao, WANG HuaJian, ZHAI LiNa, ZHOU WenXi, WANG XiaoMei, ZHANG ShuiChang, WU ChaoDong. Geological Events and Their Biological Responses During the Neoproterozoic Era[J]. Acta Sedimentologica Sinica, 2017, 35(2): 203-216. doi: 10.14027/j.cnki.cjxb.2017.02.001

引用本文:

Citation:

YE YunTao, WANG HuaJian, ZHAI LiNa, ZHOU WenXi, WANG XiaoMei, ZHANG ShuiChang, WU ChaoDong. Geological Events and Their Biological Responses During the Neoproterozoic Era[J]. Acta Sedimentologica Sinica, 2017, 35(2): 203-216. doi: 10.14027/j.cnki.cjxb.2017.02.001

新元古代重大地质事件及其与生物演化的耦合关系

doi: 10.14027/j.cnki.cjxb.2017.02.001

叶云涛^1,2,3,
王华建³,
翟俪娜^1,2,3,
周文喜^3,4,
王晓梅³,
张水昌³,
吴朝东^1,2,

1.
北京大学地球与空间科学学院, 造山带与地壳演化教育部重点实验室, 北京 100871;
2.
北京大学石油与天然气研究中心, 北京 100871;
3.
中国石油勘探开发研究院油气地球化学重点实验室, 北京 100083;
4.
贵州大学资源与环境工程学院, 贵阳 550025

基金项目: 高等学校博士学科点专项科研基金资助课题（20120001110052）

详细信息

作者简介:
叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者:
吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

中图分类号: P534.3;P597

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文章访问数: 835
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Geological Events and Their Biological Responses During the Neoproterozoic Era

1.
Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;
2.
Institute of Oil & Gas, Peking University, Beijing 100871, China;
3.
Key Laboratory of Petroleum Geochemistry, Research Institute of Petroleum Exploration and Development, Beijing 100083, China;
4.
College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China

Funds: Specialized Research Fund for the Doctoral Program of Higher Education, No. 20120001110052

摘要

摘要: 新元古代的地球表层系统经历了超大陆裂解与重组、大规模冰期、古海洋氧化、埃迪卡拉生物群辐射与灭绝、后生动物兴起等一系列重大变革，这些地质事件与生物演化在时空上的耦合关系长期受多学科交叉研究领域的广泛关注。Rodinia超大陆的裂解伴随有超级地幔柱活动、古地磁真极移等复杂响应，裂解过程影响了大气圈和水圈中氧气和二氧化碳的循环，并可能直接导致了新元古代极端的气候条件。构造格局的变动对生物的影响主要体现在物质来源和生存环境的改变上，强上升洋流和强地表径流区域的富营养化促使生物大量繁盛。“雪球地球”期间巨大的选择压力为生物的多样化演变提供了可能，而其后冰川的快速消融则促进了生产力的爆发式增长及多种沉积矿产的形成。与此同时，大气-海洋氧气含量的增加和海水化学结构的改变使得多项元素及同位素指标发生了地质历史上最大幅度的波动，这种特殊的地质背景可能最终对生物演化产生了极为深刻的影响。
- 新元古代 /
- 超大陆事件 /
- 冰期事件 /
- 大气氧含量 /
- 生物演化
Abstract: The Neoproterozoic Era witnessed a series of geological and biological events which may have significantly changed the Earth's surface environment. These events are suspected to be linked and their temporal relationships have long been a focus of multidisciplinary studies. Superplume activity and true polar wander through the early Neoproterozoic led to the break-up of Rodinia supercontinent. Indeed, such a large perturbation of deep mantle dynamics exerted a crucial impact on the global cycles of O₂ and CO₂, thus further inducing the extraordinarily dramatic climate. Biological consequences of tectonic re-configuration are mainly reflected in nutrient availability and living conditions. The elevated upwelling and surface runoff could sustain persistent blooms of marine organisms. A Snowball Earth hypothesis has been proposed to explain the tropical glaciation. During times of widespread ice, there must be an intense environmental filter on the evolution of early life. Moreover, the subsequent rapid melting of glaciers may result in the explosion of productivity as well as the formation of major sedimentary minerals. Besides these geological and biological events, this period is also characterized by prominent fluctuations of geochemical proxies, which indicate great changes of atmosphere and ocean at this critical interval.
- Neoproterozoic /
- supercontinent /
- glaciation /
- atmospheric oxygen level /
- biological events

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[1]	邓奇, 汪正江, 宁括步, 崔晓庄, 熊国庆, 任光明, 任飞. 扬子陆块西北缘旺苍地区火地垭群沉积时代、物源及构造意义——来自碎屑锆石U⁃Pb年代学的约束 . 沉积学报, 2024, 42(6): 1948-1957. doi: 10.14027/j.issn.1000-0550.2024.014
[2]	李夔洲, 侯明才, 赵子霖, 迟宇超, 黄志发. 扬子陆块北缘大洪山地区莲沱组物源分析——来自沉积学和碎屑锆石U⁃Pb年代学的证据 . 沉积学报, 2024, 42(6): 1958-1970. doi: 10.14027/j.issn.1000-0550.2023.095
[3]	李军勇, 王孝磊, 谷志东, 黄煜, 王国光. 华南新元古代多地体汇聚—拼贴与资源效应 . 沉积学报, 2024, 42(6): 1876-1889. doi: 10.14027/j.issn.1000-0550.2024.089
[4]	刘龙宇, 崔晓庄, 陈风霖, 龙训荣, 马志鑫, 孙志明. 川西金口河新元古代辉绿岩的时代、成因及构造意义 . 沉积学报, 2024, 42(6): 1890-1902. doi: DOI:10.14027/j.issn.1000-0550.2024.111
[5]	蔡欣豫, 王伟, 田洋. 江南造山带中段新元古代构造演化——来自碎屑锆石U⁃Pb和Lu⁃Hf同位素的启示 . 沉积学报, 2024, 42(6): 1986-2005. doi: 10.14027/j.issn.1000-0550.2024.036
[6]	刘龙宇, 崔晓庄, 陈风霖, 龙训荣, 马志鑫, 孙志明. 川西金口河新元古代辉绿岩的时代、成因及构造意义【“华南古大陆演化及其资源效应”专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.111
[7]	邹灏, 李峤昕, 陈安清, 肖斌, 蒋修未, 黄长成, 胡成辉, 李蝶. 新元古代“雪球地球”形成与消融及华南板块的记录 . 沉积学报, 2022, 40(4): 1043-1058. doi: 10.14027/j.issn.1000-0550.2021.019
[8]	. 滇中新元古代裂谷盆地充填序列及演化模式：对Rodinia超大陆裂解的响应 . 沉积学报, 2014, 32(3): 399-409.
[9]	冯东. 新元古代晚期盖帽碳酸盐岩的成因与“雪球地球”的终结机制 . 沉积学报, 2006, 24(2): 235-241.
[10]	柳永清, 高林志, 刘燕学. 苏皖辽地区新元古代微亮晶构造碳酸盐岩的沉积岩相与环境约束 . 沉积学报, 2005, 23(1): 49-59.

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新元古代重大地质事件及其与生物演化的耦合关系

doi: 10.14027/j.cnki.cjxb.2017.02.001

1. 北京大学地球与空间科学学院, 造山带与地壳演化教育部重点实验室, 北京 100871;

2. 北京大学石油与天然气研究中心, 北京 100871;

3. 中国石油勘探开发研究院油气地球化学重点实验室, 北京 100083;

4. 贵州大学资源与环境工程学院, 贵阳 550025

基金项目: 高等学校博士学科点专项科研基金资助课题（20120001110052）

作者简介:
叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者: 吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

收稿日期: 2016-04-08
修回日期: 2016-04-28
刊出日期: 2017-04-10

中图分类号: P534.3;P597

关键词:

摘要: 新元古代的地球表层系统经历了超大陆裂解与重组、大规模冰期、古海洋氧化、埃迪卡拉生物群辐射与灭绝、后生动物兴起等一系列重大变革，这些地质事件与生物演化在时空上的耦合关系长期受多学科交叉研究领域的广泛关注。Rodinia超大陆的裂解伴随有超级地幔柱活动、古地磁真极移等复杂响应，裂解过程影响了大气圈和水圈中氧气和二氧化碳的循环，并可能直接导致了新元古代极端的气候条件。构造格局的变动对生物的影响主要体现在物质来源和生存环境的改变上，强上升洋流和强地表径流区域的富营养化促使生物大量繁盛。“雪球地球”期间巨大的选择压力为生物的多样化演变提供了可能，而其后冰川的快速消融则促进了生产力的爆发式增长及多种沉积矿产的形成。与此同时，大气-海洋氧气含量的增加和海水化学结构的改变使得多项元素及同位素指标发生了地质历史上最大幅度的波动，这种特殊的地质背景可能最终对生物演化产生了极为深刻的影响。

English Abstract

Geological Events and Their Biological Responses During the Neoproterozoic Era

1. Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;

2. Institute of Oil & Gas, Peking University, Beijing 100871, China;

3. Key Laboratory of Petroleum Geochemistry, Research Institute of Petroleum Exploration and Development, Beijing 100083, China;

4. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China

Funds: Specialized Research Fund for the Doctoral Program of Higher Education, No. 20120001110052

Received Date: 2016-04-08
Rev Recd Date: 2016-04-28
Publish Date: 2017-04-10

Keywords:

Abstract: The Neoproterozoic Era witnessed a series of geological and biological events which may have significantly changed the Earth's surface environment. These events are suspected to be linked and their temporal relationships have long been a focus of multidisciplinary studies. Superplume activity and true polar wander through the early Neoproterozoic led to the break-up of Rodinia supercontinent. Indeed, such a large perturbation of deep mantle dynamics exerted a crucial impact on the global cycles of O₂ and CO₂, thus further inducing the extraordinarily dramatic climate. Biological consequences of tectonic re-configuration are mainly reflected in nutrient availability and living conditions. The elevated upwelling and surface runoff could sustain persistent blooms of marine organisms. A Snowball Earth hypothesis has been proposed to explain the tropical glaciation. During times of widespread ice, there must be an intense environmental filter on the evolution of early life. Moreover, the subsequent rapid melting of glaciers may result in the explosion of productivity as well as the formation of major sedimentary minerals. Besides these geological and biological events, this period is also characterized by prominent fluctuations of geochemical proxies, which indicate great changes of atmosphere and ocean at this critical interval.

引用本文:

Citation:

YE YunTao, WANG HuaJian, ZHAI LiNa, ZHOU WenXi, WANG XiaoMei, ZHANG ShuiChang, WU ChaoDong. Geological Events and Their Biological Responses During the Neoproterozoic Era[J]. Acta Sedimentologica Sinica, 2017, 35(2): 203-216. doi: 10.14027/j.cnki.cjxb.2017.02.001

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新元古代重大地质事件及其与生物演化的耦合关系

doi: 10.14027/j.cnki.cjxb.2017.02.001

作者简介:
叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者:
吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

计量

Geological Events and Their Biological Responses During the Neoproterozoic Era

计量

目录

新元古代重大地质事件及其与生物演化的耦合关系

doi: 10.14027/j.cnki.cjxb.2017.02.001

作者简介:
叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者: 吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

English Abstract

Geological Events and Their Biological Responses During the Neoproterozoic Era

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新元古代重大地质事件及其与生物演化的耦合关系

doi: 10.14027/j.cnki.cjxb.2017.02.001

作者简介: 叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者: 吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

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出版历程

Geological Events and Their Biological Responses During the Neoproterozoic Era

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出版历程

目录

新元古代重大地质事件及其与生物演化的耦合关系

doi: 10.14027/j.cnki.cjxb.2017.02.001

作者简介: 叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者: 吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

English Abstract

Geological Events and Their Biological Responses During the Neoproterozoic Era

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn

通讯作者:
吴朝东,男,教授,E-mail:cdwu@pku.edu.cn

作者简介:
叶云涛,男,1991年出生,博士,地质学(石油地质学),E-mail:yeyuntao@pku.edu.cn