气候变化领域集成服务门户(CCPortal): Climate records covering the last deglaciation

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DOI	10.1126/science.269.5221.210
	Climate records covering the last deglaciation
	Sowers T.; Bender M.
发表日期	1995
ISSN	0036-8075
起始页码	210
结束页码	214
卷号	269 期号:5221
英文摘要	The oxygen-18/oxygen-16 ratio of molecular oxygen trapped in ice cores provides a time-stratigraphic marker for transferring the absolute chronology for the Greenland Ice Sheet Project (GISP) II ice core to the Vostok and Byrd ice cores in Antarctica. Comparison of the climate records from these cores suggests that, near the beginning of the last deglaciation, warming in Antarctica began approximately 3000 years before the onset of the warm Bølling period in Greenland. Atmospheric carbon dioxide and methane concentrations began to rise 2000 to 3000 years before the warming began in Greenland and must have contributed to deglaciation and warming of temperate and boreal regions in the Northern Hemisphere.
英文关键词	carbon dioxide; climate warming; deglaciation; ice core; last deglaciation; methane; Antarctica; Greenland
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/245571
作者单位	Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, United States; Lamont-Doherty Earth Observatory, Palisades, NY 10964, United States
推荐引用方式 GB/T 7714	Sowers T.,Bender M.. Climate records covering the last deglaciation[J],1995,269(5221).
APA	Sowers T.,&Bender M..(1995).Climate records covering the last deglaciation.Science,269(5221).
MLA	Sowers T.,et al."Climate records covering the last deglaciation".Science 269.5221(1995).