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DOI10.1073/pnas.2003197117
The seawater carbon inventory at the Paleocene-Eocene Thermal Maximum
Haynes L.L.; Hönisch B.
发表日期2020
ISSN0027-8424
起始页码24088
结束页码24095
卷号117期号:39
英文摘要The Paleocene-Eocene Thermal Maximum (PETM) (55.6 Mya) was a geologically rapid carbon-release event that is considered the closest natural analog to anthropogenic CO2 emissions. Recent work has used boron-based proxies in planktic foraminifera to characterize the extent of surface-ocean acidification that occurred during the event. However, seawater acidity alone provides an incomplete constraint on the nature and source of carbon release. Here, we apply previously undescribed culture calibrations for the B/Ca proxy in planktic foraminifera and use them to calculate relative changes in seawater-dissolved inorganic carbon (DIC) concentration, surmising that Pacific surface-ocean DIC increased by +1, 010+ 1,415-646 μmol/kg during the peak-PETM. Making reasonable assumptions for the pre-PETM oceanic DIC inventory, we provide a fully data-driven estimate of the PETM carbon source. Our reconstruction yields a mean source carbon δ13C of −10% and a mean increase in the oceanic C inventory of +14,900 petagrams of carbon (PgC), pointing to volcanic CO2 emissions as the main carbon source responsible for PETM warming. © 2020 National Academy of Sciences. All rights reserved.
英文关键词Boron proxies; Dissolved inorganic carbon; Foraminifera; Ocean acidification; Paleocene-Eocene Thermal Maximum
语种英语
scopus关键词boron; organic carbon; organic matter; sea water; Acarinina soldadoensis; acidification; alkalinity; Article; carbon footprint; carbon source; climate warming; concentration (parameter); controlled study; dissolution; Eocene; foraminifer; measurement error; Monte Carlo method; Morozovella velascoensis; nonhuman; Orbulina universa; Paleocene; pH; priority journal; Trilobatus sacculifer; weathering
来源期刊Proceedings of the National Academy of Sciences of the United States of America
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/160788
作者单位Haynes, L.L., Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027, United States, Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, United States; Hönisch, B., Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027, United States, Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, United States
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Haynes L.L.,Hönisch B.. The seawater carbon inventory at the Paleocene-Eocene Thermal Maximum[J],2020,117(39).
APA Haynes L.L.,&Hönisch B..(2020).The seawater carbon inventory at the Paleocene-Eocene Thermal Maximum.Proceedings of the National Academy of Sciences of the United States of America,117(39).
MLA Haynes L.L.,et al."The seawater carbon inventory at the Paleocene-Eocene Thermal Maximum".Proceedings of the National Academy of Sciences of the United States of America 117.39(2020).
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