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DOI | 10.1126/science.274.5292.1504 |
The little ice age and medieval warm period in the Sargasso Sea | |
Keigwin L.D. | |
发表日期 | 1996 |
ISSN | 0036-8075 |
起始页码 | 1504 |
结束页码 | 1508 |
卷号 | 274期号:5292 |
英文摘要 | Sea surface temperature (SST), salinity, and flux of terrigenous material oscillated on millennial time scales in the Pleistocene North Atlantic, but there are few records of Holocene variability. Because of high rates of sediment accumulation, Holocene oscillations are well documented in the northern Sargasso Sea. Results from a radiocarbon-dated box core show that SST was ~ 1°C cooler than today 400 years ago (the Little Ice Age) and 1700 years ago, and 1°C warmer than today 1000 years ago (the Medieval Warm Period). Thus, at least some of the warming since the Little Ice Age appears to be part of a natural oscillation. |
英文关键词 | carbon 14; sodium chloride; article; climate; geology; mass spectrometry; oscillation; priority journal; sea; sediment; temperature; Holocene; Holocene climate; Little Ice Age; Medieval Warm Period; palaeoclimate; sea surface temperature; sediment accumulation; Atlantic, Sargasso Sea |
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/244243 |
作者单位 | Woods Hole Oceanographic Institution, Woods Hole, MA 02543, United States |
推荐引用方式 GB/T 7714 | Keigwin L.D.. The little ice age and medieval warm period in the Sargasso Sea[J],1996,274(5292). |
APA | Keigwin L.D..(1996).The little ice age and medieval warm period in the Sargasso Sea.Science,274(5292). |
MLA | Keigwin L.D.."The little ice age and medieval warm period in the Sargasso Sea".Science 274.5292(1996). |
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