LATE QUATERNARY PALEOCEANOGRAPHY IN THE SOUTHERN BARENTS SEA

被引：0

作者：

HALD, M ^{[1
]}

LABEYRIE, LD ^{[1
]}

POOLE, DAR ^{[1
]}

STEINSUND, PI ^{[1
]}

VORREN, TO ^{[1
]}

机构：

[1] CNRS,CTR FAIBLES RADIOACTIVITES,F-91198 GIF SUR YVETTE,FRANCE

来源：

NORSK GEOLOGISK TIDSSKRIFT | 1991年 / 71卷 / 03期

关键词：

D O I：

暂无

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The paleoclimatic evolution of the Barents Sea and continental slope occurred in three main steps: Prior to 13-12 kyr BP the area suffered from cold temperatures and the salinity of the upper water masses was reduced by glacial meltwater. After 12 kyr BP the salinity reduction was smaller and at 10 kyr BP oceanic paleoclimatic conditions similar to those of the present were established and have been fairly stable since.

引用

页码：141 / 144

页数：4

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