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二叠纪-三叠纪野火间断事件对生物灭绝的响应--以浙江煤山剖面为例

沈文杰 钟莉莉 林杨挺 孙永革 张华 杨志军 周永章

中山大学学报(自然科学版)Issue(6):19-26,8.
中山大学学报(自然科学版)Issue(6):19-26,8.

二叠纪-三叠纪野火间断事件对生物灭绝的响应--以浙江煤山剖面为例

Permian-Triassic Wildfire Gap Responses to the Mass Extinction-An Example Study in the Meishan Section,Zhejiang Province

沈文杰 1钟莉莉 2林杨挺 1孙永革 3张华 4杨志军 5周永章1

作者信息

  • 1. 中山大学地球科学与地质工程学院,广东 广州510275
  • 2. 广东省地质过程与矿产资源探查重点实验室,广东 广州510275
  • 3. 中国科学院地质与地球物理研究所,北京 100029
  • 4. 浙江大学地球科学系,浙江 杭州310027
  • 5. 南京地质古生物所,江苏 南京210008
  • 折叠

摘要

Abstract

Great changes occurred in the earth’s surrounding environments during the Permian-Triassic (P-Tr)transition and resulted in the collapse of land and marine ecosystems.Thus,the most severe mass extinction in the earth’s history appeared across the P-Tr boundary.Wildfire,as a key ecosystem driver and climate change indicator,is seldom reported in the documents of the pre-Quaternary researches.In this study,a 521 ka record of wildfire during the P-Tr mass extinction was recurred through the black car-bon (BC)and combustion-derived polycyclic aromatic hydrocarbons (PAHs)records in the GSSP section of Meishan.There were frequent wildfires in the 163 ka of history just before the P-Tr mass extinction and the most intensive one occurred in the mass extinction event beds.No combustion records were found in the beds above mass extinction line and a wildfire gap (lasting 358 ka)was recognized in the Early Trias-sic.Wildfire gap may be not a local phenomenon,but a response of global climatic and environmental changes.Wildfire would vanish accompanied by the destruction of land vegetation and abrupt drop of at-mospheric oxygen.Therefore,Meishan P-Tr wildfire gap can be used as an indicator of the mass extinc-tion.

关键词

二叠纪-三叠纪/大火间断/生物灭绝/煤山剖面

Key words

Permian-Triassic/wildfire gap/mass extinction/meishan section

分类

地质学

引用本文复制引用

沈文杰,钟莉莉,林杨挺,孙永革,张华,杨志军,周永章..二叠纪-三叠纪野火间断事件对生物灭绝的响应--以浙江煤山剖面为例[J].中山大学学报(自然科学版),2014,(6):19-26,8.

基金项目

国家自然科学基金资助项目(40803014);高校基本科研业务费资助项目(32110-3161324);海洋公益性科研资助项目 ()

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