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DOI10.1126/science.1201182
Latitudinal gradients in greenhouse seawater δ18O: Evidence from eocene sirenian tooth enamel
Clementz M.T.; Sewall J.O.
发表日期2011
ISSN0036-8075
起始页码455
结束页码458
卷号332期号:6028
英文摘要The Eocene greenhouse climate state has been linked to a more vigorous hydrologic cycle at mid- and high latitudes; similar information on precipitation levels at low latitudes is, however, limited. Oxygen isotopic fluxes track moisture fluxes and, thus, the δ18O values of ocean surface waters can provide insight into hydrologic cycle changes. The offset between tropical δ18O values from sampled Eocene sirenian tooth enamel and modern surface waters is greater than the expected 1.0 per mil increase due to increased continental ice volume. This increased offset could result from suppression of surface-water δ18O values by a tropical, annual moisture balance substantially wetter than that of today. Results from an atmospheric general circulation model support this interpretation and suggest that Eocene low latitudes were extremely wet.
英文关键词oxygen 18; atmospheric general circulation model; enamel; Eocene; greenhouse effect; hydrological cycle; latitudinal gradient; moisture flux; oxygen isotope; paleoclimate; precipitation (climatology); seawater; sirenian; surface water; article; atmosphere; climate; continental ice; enamel; Eocene; fossil; greenhouse; latitude; moisture; precipitation; priority journal; sea surface waters; water cycle; Animals; Dental Enamel; Dugong; Fossils; Geography; Greenhouse Effect; Humidity; Oceans and Seas; Oxygen Isotopes; Seawater; Steam; Temperature; Trichechus; Tropical Climate; Water Cycle; Sirenia
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/243347
作者单位Department of Geology and Geophysics, University of Wyoming, Laramie, WY 82071, United States; Program in Ecology, University of Wyoming, Laramie, WY 82071, United States; Department of Physical Sciences, Kutztown University, Kutztown, PA 19530, United States
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Clementz M.T.,Sewall J.O.. Latitudinal gradients in greenhouse seawater δ18O: Evidence from eocene sirenian tooth enamel[J],2011,332(6028).
APA Clementz M.T.,&Sewall J.O..(2011).Latitudinal gradients in greenhouse seawater δ18O: Evidence from eocene sirenian tooth enamel.Science,332(6028).
MLA Clementz M.T.,et al."Latitudinal gradients in greenhouse seawater δ18O: Evidence from eocene sirenian tooth enamel".Science 332.6028(2011).
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