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DOI | 10.1126/science.1135274 |
Paleocene-Eocene thermal maximum and the opening of the northeast Atlantic | |
Storey M.; Duncan R.A.; Swisher III C.C. | |
发表日期 | 2007 |
ISSN | 0036-8075 |
起始页码 | 587 |
结束页码 | 589 |
卷号 | 316期号:5824 |
英文摘要 | The Paleocene-Eocene thermal maximum (PETM) has been attributed to a sudden release of carbon dioxide and/or methane. 40Ar/39Ar age determinations show that the Danish Ash-17 deposit, which overlies the PETM by about 450,000 years in the Atlantic, and the Skraenterne Formation Tuff, representing the end of 1 ± 0.5 million years of massive volcanism in East Greenland, are coeval. The relative age of Danish Ash-17 thus places the PETM onset after the beginning of massive flood basalt volcanism at 56.1 ± 0.4 million years ago but within error of the estimated continental breakup time of 55.5 ± 0.3 million years ago, marked by the eruption of mid-ocean ridge basalt-like flows. These correlations support the view that the PETM was triggered by greenhouse gas release during magma interaction with basin-filling carbon-rich sedimentary rocks proximal to the embryonic plate boundary between Greenland and Europe. |
英文关键词 | argon 39; argon 40; carbon dioxide; isotope; methane; unclassified drug; age determination; argon-argon dating; carbon dioxide; continental breakup; explosive volcanism; flood basalt; greenhouse gas; magma; methane; mid-ocean ridge; Paleocene-Eocene boundary; plate boundary; sedimentary rock; temperature profile; article; Atlantic islands; Denmark; Eocene; Europe; greenhouse gas; Greenland; Paleocene; priority journal; rock; sea; volcano; Arctic; Atlantic Ocean; Atlantic Ocean (Northeast); East Greenland; Eurasia; Europe; Greenland |
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/245639 |
作者单位 | Quaternary Dating Laboratory, Department of Environment, Society and Spatial Change, Roskilde University Centre, Post Office Box 260, 4000 Roskilde, Denmark; College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States; Department of Geological Sciences, Rutgers University, Piscataway, NJ 08854-8066, United States |
推荐引用方式 GB/T 7714 | Storey M.,Duncan R.A.,Swisher III C.C.. Paleocene-Eocene thermal maximum and the opening of the northeast Atlantic[J],2007,316(5824). |
APA | Storey M.,Duncan R.A.,&Swisher III C.C..(2007).Paleocene-Eocene thermal maximum and the opening of the northeast Atlantic.Science,316(5824). |
MLA | Storey M.,et al."Paleocene-Eocene thermal maximum and the opening of the northeast Atlantic".Science 316.5824(2007). |
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