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DOI | 10.1126/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 |
ISSN | 0036-8075 |
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 |
推荐引用方式 GB/T 7714 | 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). |
条目包含的文件 | 条目无相关文件。 |
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