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DOI | 10.1073/pnas.1513868113 |
Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation | |
Bauska T.K.; Baggenstos D.; Brook E.J.; Mix A.C.; Marcott S.A.; Petrenko V.V.; Schaefer H.; Severinghaus J.P.; Lee J.E.; Thiemens M.H. | |
发表日期 | 2016 |
ISSN | 0027-8424 |
起始页码 | 3465 |
结束页码 | 3470 |
卷号 | 113期号:13 |
英文摘要 | An understanding of the mechanisms that control CO2 change during glacial-interglacial cycles remains elusive. Here we help to constrain changing sources with a high-precision, high-resolution deglacial record of the stable isotopic composition of carbon in CO2 (δ13C-CO2) in air extracted from ice samples from Taylor Glacier, Antarctica. During the initial rise in atmospheric CO2 from 17.6 to 15.5 ka, these data demarcate a decrease in δ13C-CO2, likely due to a weakened oceanic biological pump. From 15.5 to 11.5 ka, the continued atmospheric CO2 rise of 40 ppm is associated with small changes in δ13C-CO2, consistent with a nearly equal contribution from a further weakening of the biological pump and rising ocean temperature. These two trends, related to marine sources, are punctuated at 16.3 and 12.9 ka with abrupt, century-scale perturbations in δ13C-CO2 that suggest rapid oxidation of organic land carbon or enhanced air-sea gas exchange in the Southern Ocean. Additional century-scale increases in atmospheric CO2 coincident with increases in atmospheric CH4 and Northern Hemisphere temperature at the onset of the BØlling (14.6-14.3 ka) and Holocene (11.6-11.4 ka) intervals are associated with small changes in δ13C-CO2, suggesting a combination of sources that included rising surface ocean temperature. |
英文关键词 | Atmospheric CO2; Carbon cycle; Ice cores; Last deglaciation; Paleoclimate |
语种 | 英语 |
scopus关键词 | carbon; carbon dioxide; ice; air; Antarctica; Article; atmosphere; deglaciation; gas exchange; Holocene; Northern Hemisphere; oxidation; priority journal; sea; temperature; trend study |
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/159078 |
作者单位 | Bauska, T.K., College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States, Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, United Kingdom; Baggenstos, D., Scripps Institution of Oceanography, University of California, San Diego, San Diego, CA 92093, United States; Brook, E.J., College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States; Mix, A.C., College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States; Marcott, S.A., Department of Geoscience, University of Wisconsin-Madison, Madison, WI 53706, United States; Petrenko, V.V., Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, United States; Schaefer, H., Climate and Atmosphere Center, National Institute of Water, Atmospheric Research Ltd., Wellington, 6023, New Zealand; Severinghaus, J.P., Scripps Institution of Oceanography, U... |
推荐引用方式 GB/T 7714 | Bauska T.K.,Baggenstos D.,Brook E.J.,et al. Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation[J],2016,113(13). |
APA | Bauska T.K..,Baggenstos D..,Brook E.J..,Mix A.C..,Marcott S.A..,...&Thiemens M.H..(2016).Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation.Proceedings of the National Academy of Sciences of the United States of America,113(13). |
MLA | Bauska T.K.,et al."Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation".Proceedings of the National Academy of Sciences of the United States of America 113.13(2016). |
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