Segments of atmospheric 14C change as derived from late glacial and Early Holocene floating tree-ring series

被引：39
|
作者：
Kromer, B
Spurk, M
Remmele, S
Barbetti, M
机构：
[1] Heidelberg Acad Sci, Inst Environm Phys, D-69120 Heidelberg, Germany
[2] Univ Hohenheim, Inst Bot, D-70593 Stuttgart, Germany
[3] Univ Sydney, NWG Macintosh Ctr Quaternary Dating, Sydney, NSW 2006, Australia
来源：
RADIOCARBON | 1998年 / 40卷 / 01期
关键词：
D O I：
10.1017/S0033822200018221
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：
We present results of C-14 dating of several tree-ring series from the Late Glacial and Early Holocene, analyzed at the Heidelberg University radiocarbon laboratory. Although these are floating series, they contribute high-resolution information about the variability of atmospheric C-14 during those periods.
引用
收藏
页码：351 / 358
页数：8
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