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DOI | 10.1126/science.aar5372 |
Late inception of a resiliently oxygenated upper ocean | |
Lu W.; Ridgwell A.; Thomas E.; Hardisty D.S.; Luo G.; Algeo T.J.; Saltzman M.R.; Gill B.C.; Shen Y.; Ling H.-F.; Edwards C.T.; Whalen M.T.; Zhou X.; Gutchess K.M.; Jin L.; Rickaby R.E.M.; Jenkyns H.C.; Lyons T.W.; Lenton T.M.; Kump L.R.; Lu Z. | |
发表日期 | 2018 |
ISSN | 0036-8075 |
起始页码 | 174 |
结束页码 | 177 |
卷号 | 361期号:6398 |
英文摘要 | Rising oceanic and atmospheric oxygen levels through time have been crucial to enhanced habitability of surface Earth environments. Few redox proxies can track secular variations in dissolved oxygen concentrations around threshold levels for metazoan survival in the upper ocean. We present an extensive compilation of iodine-to-calcium ratios (I/Ca) in marine carbonates. Our record supports a major rise in the partial pressure of oxygen in the atmosphere at ~400 million years (Ma) ago and reveals a step change in the oxygenation of the upper ocean to relatively sustainable near-modern conditions at ~200 Ma ago. An Earth system model demonstrates that a shift in organic matter remineralization to greater depths, which may have been due to increasing size and biomineralization of eukaryotic plankton, likely drove the I/Ca signals at ~200 Ma ago. 2017 © The Authors. |
英文关键词 | carbonic acid; organic matter; calcium; carbonic acid; iodine; oxygen; biomineralization; concentration (composition); dissolved oxygen; eukaryote; metazoan; oxygenation; paleoceanography; paleoenvironment; plankton; redox conditions; remineralization; survival; upper ocean; Article; astronomy; atmosphere; biomineralization; chemical parameters; ecosystem resilience; environmental sustainability; evolution; geological time; iodine to calcium ratio; marine environment; nonhuman; oxidation reduction state; oxygen concentration; oxygen tension; oxygenation; plankton; priority journal; sea; signal transduction; chemistry; evolution; plankton; sea; Eukaryota; Metazoa; Atmosphere; Biological Evolution; Calcium; Carbonates; Iodine; Oceans and Seas; Oxygen; Plankton |
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/244585 |
作者单位 | Department of Earth Sciences, Syracuse University, Syracuse, NY, United States; Department of Earth Sciences, University of California, Riverside, Riverside, CA, United States; School of Geographical Sciences, University of Bristol, Bristol, United Kingdom; Department of Geology and Geophysics, Yale University, New Haven, CT, United States; Department of Earth and Environmental Sciences, Wesleyan University, Middletown, CT, United States; Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, United States; State Key Laboratory of Biogeology and Environmental Geology, School of Earth Science, China University of Geosciences, Wuhan, China; State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, China; Department of Geology, University of Cincinnati, Cincinnati, OH, United States; School of Earth Sciences, Ohio State University, Columbus, OH, United States; Department of Geosciences, Virginia Polytechnic and State Univ... |
推荐引用方式 GB/T 7714 | Lu W.,Ridgwell A.,Thomas E.,et al. Late inception of a resiliently oxygenated upper ocean[J],2018,361(6398). |
APA | Lu W..,Ridgwell A..,Thomas E..,Hardisty D.S..,Luo G..,...&Lu Z..(2018).Late inception of a resiliently oxygenated upper ocean.Science,361(6398). |
MLA | Lu W.,et al."Late inception of a resiliently oxygenated upper ocean".Science 361.6398(2018). |
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