THE YOUNGER-DRYAS COLD EVENT - WAS IT SYNCHRONOUS OVER THE NORTH-ATLANTIC REGION

被引：39

作者：

GOSLAR, T ^{[1
]}

ARNOLD, M ^{[1
]}

PAZDUR, MF ^{[1
]}

机构：

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

来源：

RADIOCARBON | 1995年 / 37卷 / 01期

关键词：

D O I：

10.1017/S003382220001479X

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Determined independently from annually laminated ice cores and lake sediments, and German pines, the calendar ages of Younger Dryas (YD) boundaries significantly disagree with one another. C-14 dates, plotted vs. calendar ages for samples from different sediments, also reveal distinct offsets. The adjustment of varve chronologies to synchronize the boundaries of the YD nearly cancels the discrepancies between C-14 data, and supports the synchronism of the YD cold period over the North Atlantic region. However, the exact timing of the event cannot be estimated in this way.

引用

页码：63 / 70

页数：8

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