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DOI10.1126/science.290.5490.325
The last glacial-holocene transition in southern Chile
Bennett K.D.; Haberle S.G.; Lumley S.H.
发表日期2000
ISSN0036-8075
起始页码325
结束页码328
卷号290期号:5490
英文摘要Warming at the last glacial termination in the North Atlantic region was interrupted by a period of renewed glacial activity during the Younger Dryas chronozone (YDC). The underlying mechanism of this cooling remains elusive, but hypotheses turn on whether it was a global or a North Atlantic phenomenon. Chronological, sedimentological, and palaeoecological records from sediments of small lakes in oceanic southern Chile demonstrate that there was no YDC cooling in southern Chile. It is therefore likely that there was little or no cooling in southern Pacific surface waters and hence that YDC cooling in the North Atlantic was a regional, rather than global, phenomenon.
英文关键词carbon 14; climate change; glaciation; Holocene; Last Glacial; paleoclimate; paleoenvironment; Pleistocene; Younger Dryas; altitude; article; Atlantic Ocean; Chile; climate; geography; greenhouse effect; lake; Pacific Ocean; priority journal; sediment; South America; Chile
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/243018
作者单位Quaternary Geology, Department of Earth Sciences, Uppsala University, Villavagen 16, S-752 36 Uppsala, Sweden
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Bennett K.D.,Haberle S.G.,Lumley S.H.. The last glacial-holocene transition in southern Chile[J],2000,290(5490).
APA Bennett K.D.,Haberle S.G.,&Lumley S.H..(2000).The last glacial-holocene transition in southern Chile.Science,290(5490).
MLA Bennett K.D.,et al."The last glacial-holocene transition in southern Chile".Science 290.5490(2000).
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