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古海洋微量元素地球化学演化: 对关键地质事件研究的启发
Geochemical Recycling of Trace Elements in Paleo-oceans: Implications to the Studies Associated with Key Geological Events

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邓倩 1,2   廖泽文 1 *   徐建兵 1,2   程斌 1   梁允干 1,2   韦志伟 1,2  
文摘 古海洋微量元素地球化学循环、沉积环境和生物发育之间发生着复杂的相互作用,对重要地质事件具有指示意义.为加深对这一领域的认识,本文综述了微量元素在古环境重建及在关键地质事件的地球化学应用研究进展.以我国华南地区震旦系-下寒武统为例,阐述了关键地质事件时期古海洋中微量元素变化、沉积环境演变和生物演化之间的协同机制.指出今后值得进一步从微量元素同位素以及不同盆地乃至全球尺度上对比探讨震旦系-早寒武世沉积地层中微量元素分布特征及其在寒武纪生物大爆发中的响应.
其他语种文摘 The complicated interactions among the geochemical recycling of trace elements,sedimentary environment,and biological development of paleo-oceans are of indicative significance to key geological events. In order to deepen the understanding of this topic,the research progress about the geochemical applications of trace elements for reconstructing paleoenvironment and for studying key geological events has been reviewed in this paper. Taking the Sinian-Lower Cambrian strata in South China as objectives of a case study,we have deeply discussed the co-evolution mechanisms among the trace elements distribution patterns,variation of sedimentary environments,and the biological development. The comparative study on distribution characteristics of trace elements and isotopes of the Sinian-Early Cambrian strata and their possible implications for studying the Cambrian Biomass Explosion from perspectives at a basin or even a global scale are worth to be further comprehensively undertaken in near future.
来源 矿物岩石地球化学通报 ,2019,38(3):587-594 【核心库】
DOI 10.19658/j.issn.1007-2802.2019.38.070
关键词 微量元素 ; 生物演化 ; 古沉积环境 ; 震旦-寒武纪 ; 黑色岩系
地址

1. 中国科学院广州地球化学研究所, 有机地球化学国家重点实验室, 广州, 510640  

2. 中国科学院大学, 北京, 100049

语种 中文
文献类型 研究性论文
ISSN 1007-2802
学科 海洋学
基金 国家自然科学基金项目 ;  国家“十三五”油气专项研究课题
文献收藏号 CSCD:6525116

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引证文献 5

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