气候变化领域集成服务门户(CCPortal): Mechanisms of climate warming at the end of the Paleocene

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DOI	10.1126/science.285.5428.724
	Mechanisms of climate warming at the end of the Paleocene
	Bains S.; Corfield R.M.; Norris R.D.
发表日期	1999
ISSN	0036-8075
起始页码	724
结束页码	727
卷号	285 期号:5428
英文摘要	An abrupt episode of global warming marked the end of the Paleocene epoch. Oxygen and carbon isotope records from two widely separated sites support the notion that degassing of biogenic methane hydrate may have been an important factor in altering Earth's climate. The data show evidence for multiple injections of methane, separated by intervals in which the carbon cycle was in stasis. Correlations between the two sites suggest that even these small-scale events were global in nature.
英文关键词	biogas; carbon; methane; oxygen; carbon; climate change; isotopic composition; oxygen; Paleocene; paleoclimate; article; carbon dioxide fixation; geology; global climate; greenhouse effect; isotope labeling; priority journal
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/242928
作者单位	Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, United Kingdom; Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, United States
推荐引用方式 GB/T 7714	Bains S.,Corfield R.M.,Norris R.D.. Mechanisms of climate warming at the end of the Paleocene[J],1999,285(5428).
APA	Bains S.,Corfield R.M.,&Norris R.D..(1999).Mechanisms of climate warming at the end of the Paleocene.Science,285(5428).
MLA	Bains S.,et al."Mechanisms of climate warming at the end of the Paleocene".Science 285.5428(1999).