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DOI | 10.1073/pnas.1917518117 |
Triple oxygen isotope insight into terrestrial pyrite oxidation | |
Hemingway J.D.; Olson H.; Turchyn A.V.; Tipper E.T.; Bickle M.J.; Johnston D.T. | |
发表日期 | 2020 |
ISSN | 0027-8424 |
起始页码 | 7650 |
结束页码 | 7657 |
卷号 | 117期号:14 |
英文摘要 | The mass-independent minor oxygen isotope compositions (∆0 17O) of atmospheric O2 and CO2 are primarily regulated by their relative partial pressures, pO2/pCO2. Pyrite oxidation during chemical weathering on land consumes O2 and generates sulfate that is carried to the ocean by rivers. The ∆0 17O values of marine sulfate deposits have thus been proposed to quantitatively track ancient atmospheric conditions. This proxy assumes direct O2 incorporation into terrestrial pyrite oxidation-derived sulfate, but a mechanistic understanding of pyrite oxidation-including oxygen sources-in weathering environments remains elusive. To address this issue, we present sulfate source estimates and ∆0 17O measurements from modern rivers transecting the Annapurna Himalaya, Nepal. Sulfate in high-elevation headwaters is quantitatively sourced by pyrite oxidation, but resulting ∆0 17O values imply no direct tropospheric O2 incorporation. Rather, our results necessitate incorporation of oxygen atoms from alternative, 17O-enriched sources such as reactive oxygen species. Sulfate ∆0 17O decreases significantly when moving into warm, low-elevation tributaries draining the same bedrock lithology. We interpret this to reflect overprinting of the pyrite oxidation-derived ∆0 17O anomaly by microbial sulfate reduction and reoxidation, consistent with previously described major sulfur and oxygen isotope relationships. The geologic application of sulfate ∆0 17O as a proxy for past pO2/pCO2 should consider both 1) alternative oxygen sources during pyrite oxidation and 2) secondary overprinting by microbial recycling. © 2020 National Academy of Sciences. All rights reserved. |
英文关键词 | Atmospheric O2; Chemical weathering; Himalayas; Sulfur cycle; ∆0 17O |
语种 | 英语 |
scopus关键词 | oxygen; pyrite; reactive oxygen metabolite; Article; atmosphere; chemical analysis; chemical reaction kinetics; concentration (parameter); geology; isotope analysis; Nepal; oxidation; precipitation; priority journal; river; seasonal variation; troposphere; weathering |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/159026 |
作者单位 | Hemingway, J.D., Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, United States; Olson, H., Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, United States; Turchyn, A.V., Department of Earth Sciences, Cambridge University, Cambridge, CB2 1TN, United Kingdom; Tipper, E.T., Department of Earth Sciences, Cambridge University, Cambridge, CB2 1TN, United Kingdom; Bickle, M.J., Department of Earth Sciences, Cambridge University, Cambridge, CB2 1TN, United Kingdom; Johnston, D.T., Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, United States |
推荐引用方式 GB/T 7714 | Hemingway J.D.,Olson H.,Turchyn A.V.,et al. Triple oxygen isotope insight into terrestrial pyrite oxidation[J],2020,117(14). |
APA | Hemingway J.D.,Olson H.,Turchyn A.V.,Tipper E.T.,Bickle M.J.,&Johnston D.T..(2020).Triple oxygen isotope insight into terrestrial pyrite oxidation.Proceedings of the National Academy of Sciences of the United States of America,117(14). |
MLA | Hemingway J.D.,et al."Triple oxygen isotope insight into terrestrial pyrite oxidation".Proceedings of the National Academy of Sciences of the United States of America 117.14(2020). |
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