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DOI | 10.1073/pnas.1112248109 |
Antarctic and Southern Ocean influences on Late Pliocene global cooling | |
McKay R.; Naish T.; Carter L.; Riesselman C.; Dunbar R.; Sjunneskog C.; Winter D.; Sangiorgi F.; Warren C.; Pagani M.; Schouten S.; Willmott V.; Levy R.; DeConto R.; Powell R.D. | |
发表日期 | 2012 |
ISSN | 0027-8424 |
起始页码 | 6423 |
结束页码 | 6428 |
卷号 | 109期号:17 |
英文摘要 | The influence of Antarctica and the Southern Ocean on Late Pliocene global climate reconstructions has remained ambiguous due to a lack of well-dated Antarctic-proximal, paleoenvironmental records. Here we present ice sheet, sea-surface temperature, and sea ice reconstructions from the ANDRILL AND-1B sediment core recovered from beneath the Ross Ice Shelf. We provide evidence for a major expansion of an ice sheet in the Ross Sea that began at ∼3.3 Ma, followed by a coastal sea surface temperature cooling of ∼2.5°C, a stepwise expansion of sea ice, and polynya-style deep mixing in the Ross Sea between 3.3 and 2.5 Ma. The intensification of Antarctic cooling resulted in strengthened westerly winds and invigorated ocean circulation. The associated northward migration of Southern Ocean fronts has been linked with reduced Atlantic Meridional Overturning Circulation by restricting surface water connectivity between the ocean basins, with implications for heat transport to the high latitudes of the North Atlantic. While our results do not exclude low-latitude mechanisms as drivers for Pliocene cooling, they indicate an additional role played by southern high-latitude cooling during development of the bipolar world. |
英文关键词 | Glacial history; Late Neogene; Paleoclimate; Paleooceanography; West Antarctic ice sheet |
语种 | 英语 |
scopus关键词 | article; cooling; latitude; oscillation; paleoclimate; Pliocene; priority journal; sea; sea ice; sea surface temperature; sea surface waters; sediment |
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/158937 |
作者单位 | McKay, R., Antarctic Research Centre, Victoria University of Wellington, PO Box 600, Wellington 6140, New Zealand; Naish, T., Antarctic Research Centre, Victoria University of Wellington, PO Box 600, Wellington 6140, New Zealand; Carter, L., Antarctic Research Centre, Victoria University of Wellington, PO Box 600, Wellington 6140, New Zealand; Riesselman, C., Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, United States, Eastern Geology and Paleoclimate Science Center, US Geological Survey, Reston, VA 20192, United States; Dunbar, R., Department of Environmental Earth Systems Science, Stanford University, Stanford, CA 94305, United States; Sjunneskog, C., Antarctic Marine Geology Research Facility, Florida State University, Tallahassee, FL 32306, United States; Winter, D., Rhithron Associates, Inc., Missoula, MT 59804, United States; Sangiorgi, F., Department of Earth Sciences, Faculty of Geosciences, Utrecht University, U3584 CD Utrecht, Netherlands; Warren, ... |
推荐引用方式 GB/T 7714 | McKay R.,Naish T.,Carter L.,et al. Antarctic and Southern Ocean influences on Late Pliocene global cooling[J],2012,109(17). |
APA | McKay R..,Naish T..,Carter L..,Riesselman C..,Dunbar R..,...&Powell R.D..(2012).Antarctic and Southern Ocean influences on Late Pliocene global cooling.Proceedings of the National Academy of Sciences of the United States of America,109(17). |
MLA | McKay R.,et al."Antarctic and Southern Ocean influences on Late Pliocene global cooling".Proceedings of the National Academy of Sciences of the United States of America 109.17(2012). |
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