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DOI10.1126/science.aan8086
Titanium isotopic evidence for felsic crust and plate tectonics 3.5 billion years ago
Greber N.D.; Dauphas N.; Bekker A.; Ptáček M.P.; Bindeman I.N.; Hofmann A.
发表日期2017
ISSN0036-8075
起始页码1271
结束页码1274
卷号357期号:6357
英文摘要Earth exhibits a dichotomy in elevation and chemical composition between the continents and ocean floor. Reconstructing when this dichotomy arose is important for understanding when plate tectonics started and how the supply of nutrients to the oceans changed through time. We measured the titanium isotopic composition of shales to constrain the chemical composition of the continental crust exposed to weathering and found that shales of all ages have a uniform isotopic composition. This can only be explained if the emerged crust was predominantly felsic (silica-rich) since 3.5 billion years ago, requiring an early initiation of plate tectonics. We also observed a change in the abundance of biologically important nutrients phosphorus and nickel across the Archean-Proterozoic boundary, which might have helped trigger the rise in atmospheric oxygen. © 2017, American Association for the Advancement of Science. All rights reserved.
英文关键词isotope; nickel; oxygen; phosphorus; silicon dioxide; titanium; Archean; chemical weathering; continental crust; felsic rock; isotopic analysis; isotopic composition; Proterozoic; reconstruction; shale; titanium; Archean; Article; chemical composition; geology; priority journal; Proterozoic; rock; sediment; weathering
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/243864
作者单位Origins Laboratory, Department of the Geophysical Sciences, Enrico Fermi Institute, University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60615, United States; Department of Earth Sciences, University of California, Riverside, CA 92521, United States; Department of Geology, University of Johannesburg, Post Office Box 524, Auckland Park, 2006, South Africa; Department of Geological Sciences, 1272 University of Oregon, Eugene, OR 97403, United States; Department of Earth Sciences, University of Geneva, Rue des Maraîchers 13, Geneva, 1205, Switzerland
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Greber N.D.,Dauphas N.,Bekker A.,et al. Titanium isotopic evidence for felsic crust and plate tectonics 3.5 billion years ago[J],2017,357(6357).
APA Greber N.D.,Dauphas N.,Bekker A.,Ptáček M.P.,Bindeman I.N.,&Hofmann A..(2017).Titanium isotopic evidence for felsic crust and plate tectonics 3.5 billion years ago.Science,357(6357).
MLA Greber N.D.,et al."Titanium isotopic evidence for felsic crust and plate tectonics 3.5 billion years ago".Science 357.6357(2017).
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