Calibration of lacustrine sediment ages using the relationship between 14C levels in lake waters and in the atmosphere:: The case of Lake Linneret

被引：0

作者：

Stiller, M ^{[1
]}

Kaufman, A ^{[1
]}

Carmi, I ^{[1
]}

Mintz, G ^{[1
]}

机构：

[1] Weizmann Inst Sci, Dept Environm Sci & Energy Res, IL-76100 Rehovot, Israel

来源：

RADIOCARBON | 2001年 / 43卷 / 2B期

关键词：

D O I：

暂无

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：

The source of endogenic organic and inorganic carbon in lacustrine sediments is the dissolved inorganic carbon (DIC) in the lake water. The relation between the radiocarbon levels of DIC in Lake Kinneret and of CO2 in the atmosphere has been investigated. The ratio of the former to the latter was found to be 0.814 +/- 0.013. This ratio is used for calibrating the age of the sediment according to the natural fluctuations in the atmospheric levels of C-14 that occurred during the past 10,000 years.

引用

页码：821 / 830

页数：10

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