显生宙大规模岩浆活动对温室期发育的制约  

Large-scale magmatic activities and their constraints on genesis of greenhouse during Phanerozoic Eon

作　　者：张少华 纪伟强[1] 陈厚彬 徐强 吴福元[1,2] ZHANG Shao-hua;JI Wei-qiang;CHEN Hou-bin;XU Qiang;WU Fu-yuan(State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Bejing 100029,China;College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Bejing 100049,China)

机构地区：[1]中国科学院地质与地球物理研究所,岩石圈演化国家重点实验室,北京100029 [2]中国科学院大学地球与行星科学学院,北京100049

出　　处：《矿物岩石地球化学通报》2023年第5期1042-1061,I0002,I0005,共22页Bulletin of Mineralogy, Petrology and Geochemistry

基　　金：国家重点研发计划项目(2022YFF0800800);国家自然科学基金资助项目(41888101,42072078)。

摘　　要：大规模岩浆活动对宜居环境的影响是地球科学研究的前沿领域之一。显生宙是地质历史上记录保存最完整的时期,为研究板块构造尺度下构造、岩浆、古生物和古气候演化等重大科学问题提供了有效的载体。本文系统概述了显生宙主要温室期发育的时间和温度等基本信息,结合近年来岩浆活动与深部碳循环的研究进展,进一步讨论了显生宙温室期发育与大规模岩浆活动之间的成因联系,旨在为正在加剧的全球变暖事件的预测和应对提供更多的研究支撑。The influence of large-scale magmatic activity on habitable environment is one of the research frontiers of earth sciences.The Phanerozoic Eon is the most well-documented period in geological history.It provides effective carriers for us to explore important scientific questions including the tectonic,magmatic,paleontological and paleoclimate evolution at the plate tectonic scale.In this paper,we have systematically summarized basic information including the developing times and temperatures of the major Phanerozoic greenhouse periods,and have further discussed the genetic relationship between Phanerozoic greenhouses and large-scale magmatisms based on the combined recent advances in researches on the magmat-ic activity and deep carbon cycling,in order to provide more research supports for predicting and responsing the increasing global warming events.

关 键 词：显生宙 温室期 岩浆活动 脱碳 

分 类 号：P532[天文地球—古生物学与地层学] P588.11[天文地球—地质学]