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DOI | 10.1126/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 |
ISSN | 0036-8075 |
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
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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 |
推荐引用方式 GB/T 7714 | 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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