Tracing the formation and differentiation of the Earth by non-traditional stable isotopes  

作　　者：Fangzhen TENG Shuijiong WANG Frédéric MOYNIER 

机构地区：[1]Isotope Laboratory,Department of Earth and Space Sciences,University of Washington,Seattle,WA 98195-1310,USA [2]State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China [3]Institut de Physique du Globe de Paris,Universite de Paris,Paris 75238,France [4]Institut Universitaire de France,Paris 75231,France [5]State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Sciences,China University of Geosciences,Wuhan 430074,China

出　　处：《Science China Earth Sciences》2019年第11期1702-1715,共14页中国科学（地球科学英文版）

基　　金：financially supported by the National Natural Science Foundation of China (Grant No. 41729001);the National Science Foundation (Grant No. EAR-1747706);the European Research Council under the H2020 framework program/ERC grant agreement (Grant No. #637503-Pristine);the UnivEarthS Labex program at Sorbonne Paris Cité (Grant Nos. #ANR-10-LABX-0023 and #ANR-11-IDEX-0005-02);the ANR through a chaire d’excellence Sorbonne Paris Cité

摘　　要：The Earth has grown from chaotically mixed small dusts and gases to its present highly differentiated layered structure over the past 4.567 billion years. This differentiation has led to the formation of the atmosphere, hydrosphere,biosphere, crust, mantle, and core. The timing and mechanism for the formation and evolution of these different layers are still subjects of intense debate. This review brings together recent advances in using non-traditional stable isotopes to constrain major events and processes leading to the formation and differentiation of the Earth, including the Moon-forming giant impact, crustmantle interactions, evolution of life, the rise of atmospheric oxygen, extreme paleoclimate changes, and cooling rate of magmas.The Earth has grown from chaotically mixed small dusts and gases to its present highly differentiated layered structure over the past 4.567 billion years. This differentiation has led to the formation of the atmosphere, hydrosphere,biosphere, crust, mantle, and core. The timing and mechanism for the formation and evolution of these different layers are still subjects of intense debate. This review brings together recent advances in using non-traditional stable isotopes to constrain major events and processes leading to the formation and differentiation of the Earth, including the Moon-forming giant impact, crustmantle interactions, evolution of life, the rise of atmospheric oxygen, extreme paleoclimate changes, and cooling rate of magmas.

关 键 词：Non-traditional stable isotopes Differentiation of the EARTH CRUST-MANTLE interactions Atmospheric evolution SNOWBALL EARTH Mass extinction 

分 类 号：O57[理学—粒子物理与原子核物理]