CCPortal
DOI10.1126/science.274.5292.1504
The little ice age and medieval warm period in the Sargasso Sea
Keigwin L.D.
发表日期1996
ISSN0036-8075
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).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Keigwin L.D.]的文章
百度学术
百度学术中相似的文章
[Keigwin L.D.]的文章
必应学术
必应学术中相似的文章
[Keigwin L.D.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。