Palaeoclimate - Tree rings floating on ice cores

被引：2
|
作者：
Reimer, Paula J. [1 ]
Hughen, Konrad A. [2 ]
机构：
[1] Queens Univ Belfast, Sch Geog Archaeol & Palaeoecol, CHRONO Ctr Climate Environm & Chronol, Belfast B17 1NN, Antrim, North Ireland
[2] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA
来源：
NATURE GEOSCIENCE | 2008年 / 1卷 / 04期
关键词：
D O I：
10.1038/ngeo167
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
Because of difficulties in creating a radiocarbon calibration that covers the end of the last glaciation, defining the timing and duration of the Younger Dryas cold event has been a challenge. Linking related cosmogenic isotopes in tree rings and ice cores may provide new insights into abrupt climate changes.
引用
收藏
页码：218 / 219
页数：2
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