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  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 中国科学院矿产资源研究重点实验室
Chromium isotope systematics and the diagenesis of marine carbonates

文献类型：期刊论文

作者Wang, Changle5,6,7,8; Reinhard, Christopher T.4; Rybacki, Kyle S.3,4; Hardisty, Dalton S.9; Ossa, Frantz Ossa1,10; Wang, Xiangli11,12; Hofmann, Axel1; Asael, Dan8; Robbins, Leslie J.2,8; Zhang, Lianchang5,6,7
刊名EARTH AND PLANETARY SCIENCE LETTERS
出版日期2021-05-15
卷号562页码:13
关键词chromium isotope diagenesis marine carbonates Cenozoic and Archean atmospheric oxygen abundance
ISSN号0012-821X
DOI10.1016/j.epsl.2021.116824
英文摘要Stable chromium (Cr) isotopes have emerged as a new tool for tracking broad-scale changes in Earth's surface oxygen levels. Carbonates are one proposed sedimentary Cr isotope archive. In order to contribute to the development of a robust framework for interpreting carbonate Cr isotopic compositions and evaluating their ability to record the global redox state, we explored Cr isotope systematics of modern and Archean carbonate successions-representing end member oxic and anoxic Earth system states. We generated new data from carbonate platform sediments from the Great Bahama Bank with variable post-depositional histories to better understand the effects of diagenetic alteration on carbonate-bound Cr and its isotopic composition in a modern well-oxygenated ocean-atmosphere system. More specifically, we investigated the effects of dolomitization and aragonite-to-calcite neomorphism in marine and meteoric fluids. We also present delta Cr-53 values from three carbonate successions, the similar to 3.0Ga Chobeni Formation (South Africa), similar to 2.8Ga Mosher Carbonate Formation (Canada), and similar to 2.65 Ga Cheshire Formation (Zimbabwe), that were deposited under an anoxic atmosphere. We find that modern Bahamian carbonates have a large range of almost exclusively positive delta Cr-53 values (from -0.04 to 2.88 parts per thousand). The delta Cr-53 values appear to be altered during both meteoric diagenesis and dolomitization but there may also be instances of rock-buffered conditions that may best preserve depositional delta Cr-53 values. These observations provide a baseline for carbonate Cr isotope behavior in a well-oxygenated ocean-atmosphere system. Our Archean carbonate successions contain both positively fractionated and crustal delta Cr-53 values, ranging between -0.37 and 0.89 parts per thousand. The Cr isotope fractionation observed in Archean strata is most plausibly linked to either non-redox dependent Cr isotope fractionation, local Cr redox cycling, late-stage diagenetic alteration, or some combination thereof. Given the significant effects of post-depositional alteration on the isotopic composition of carbonate-bound Cr, we suggest that Cr isotope values from ancient carbonate sediments should be generally interpreted with caution and cannot be straightforwardly linked to changes in atmospheric oxygen abundance. (C) 2021 Elsevier B.V. All rights reserved.
资助项目National Natural Science Foundation of China[41872087] ; National Natural Science Foundation of China[41890833] ; Key Research Program of the Institute of Geology and Geophysics, CAS[IGGCAS-201905] ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; China Scholarship Council ; Packard Foundation ; NSF-ELT program
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000636736200007
出版者ELSEVIER
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Packard Foundation ; Packard Foundation ; Packard Foundation ; Packard Foundation ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Packard Foundation ; Packard Foundation ; Packard Foundation ; Packard Foundation ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Packard Foundation ; Packard Foundation ; Packard Foundation ; Packard Foundation ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; Youth Innovation Promotion Association, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Packard Foundation ; Packard Foundation ; Packard Foundation ; Packard Foundation ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program ; NSF-ELT program
源URL[http://ir.iggcas.ac.cn/handle/132A11/101119]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Wang, Changle
作者单位1.Univ Johannesburg, Dept Geol, Johannesburg, South Africa
2.Univ Regina, Dept Geol, Regina, SK, Canada
3.Bur Land Management, Phoenix, AZ USA
4.Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA
5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China
6.Univ Chinese Acad Sci, Beijing, Peoples R China
7.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
8.Yale Univ, Dept Earth & Planetary Sci, New Haven, CT USA
9.Michigan State Univ, Dept Earth & Environm Sci, E Lansing, MI 48824 USA
10.Univ Tubingen, Dept Geosci, Tubingen, Germany
推荐引用方式
GB/T 7714		 Wang, Changle,Reinhard, Christopher T.,Rybacki, Kyle S.,et al. Chromium isotope systematics and the diagenesis of marine carbonates[J]. EARTH AND PLANETARY SCIENCE LETTERS,2021,562:13.
APA Wang, Changle.,Reinhard, Christopher T..,Rybacki, Kyle S..,Hardisty, Dalton S..,Ossa, Frantz Ossa.,...&Planavsky, Noah J..(2021).Chromium isotope systematics and the diagenesis of marine carbonates.EARTH AND PLANETARY SCIENCE LETTERS,562,13.
MLA Wang, Changle,et al."Chromium isotope systematics and the diagenesis of marine carbonates".EARTH AND PLANETARY SCIENCE LETTERS 562(2021):13.

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来源：地质与地球物理研究所

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