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DOI10.1126/science.1116913
Paleontology: Transient floral change and rapid global warming at the Paleocene-Eocene boundary
Wing S.L.; Harrington G.J.; Smith F.A.; Bloch J.I.; Boyer D.M.; Freeman K.H.
发表日期2005
ISSN0036-8075
起始页码993
结束页码996
卷号310期号:5750
英文摘要Rapid global warming of 5° to 10°C during the Paleocene-Eocene Thermal Maximum (PETM) coincided with major turnover in vertebrate faunas, but previous studies have found little floral change. Plant fossils discovered in Wyoming, United States, show that PETM floras were a mixture of native and migrant lineages and that plant range shifts were large and rapid (occurring within 10,000 years). Floral composition and leaf shape and size suggest that climate warmed by ∼5°C during the PETM and that precipitation was low early in the event and increased later. Floral response to warming and/or increased atmospheric CO2 during the PETM was comparable in rate and magnitude to that seen in postglacial floras and to the predicted effects of anthropogenic carbon release and climate change on future vegetation.
英文关键词Climatology; Plants (botany); Precipitation (meteorology); Vegetation; Floral change; Paleocene-eocene thermal maximum (PETM); United States; Global warming; carbon; carbon dioxide; carbon; oxygen; rain; flora; global warming; Paleocene-Eocene boundary; paleoclimate; article; atmosphere; carbon dioxide measurement; chemical composition; climate change; environmental temperature; Eocene; flora; fossil; geology; greenhouse effect; nonhuman; Paleocene; plant; plant leaf; precipitation; prediction; priority journal; United States; vegetation; animal; biodiversity; classification; climate; ecosystem; fossil; growth, development and aging; histology; plant; sediment; temperature; time; Vertebrata; Animals; Biodiversity; Carbon Isotopes; Climate; Ecosystem; Fossils; Geologic Sediments; Greenhouse Effect; Oxygen Isotopes; Plant Leaves; Plants; Rain; Temperature; Time Factors; Wyoming
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/246047
作者单位Department of Paleobiology, Smithsonian Museum of Natural History, 10th St. and Constitution Avenue, NW, Washington, DC 20560, United States; Department of Geography, Earth, and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, United Kingdom; Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States; Division of Vertebrate Paleontology, Florida Museum of Natural History, 222 Dickinson Hall, Museum Road and Newell Drive, Gainesville, FL 32611, United States; Department of Anatomical Sciences, Stony Brook University, Stony Brook, NY 11794-8081, United States
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Wing S.L.,Harrington G.J.,Smith F.A.,et al. Paleontology: Transient floral change and rapid global warming at the Paleocene-Eocene boundary[J],2005,310(5750).
APA Wing S.L.,Harrington G.J.,Smith F.A.,Bloch J.I.,Boyer D.M.,&Freeman K.H..(2005).Paleontology: Transient floral change and rapid global warming at the Paleocene-Eocene boundary.Science,310(5750).
MLA Wing S.L.,et al."Paleontology: Transient floral change and rapid global warming at the Paleocene-Eocene boundary".Science 310.5750(2005).
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