冰芯
格陵兰冰盖
冰原
海洋学
地质学
氧同位素
自然地理学
格罗恩兰迪亚
古气候学
气候学
δ18O
稳定同位素比值
气候变化
地理
地球化学
量子力学
物理
作者
W. Dansgaard,S. J. Johnsen,Jakob J. Møller,Chester C. Langway
出处
期刊:Science
[American Association for the Advancement of Science]
日期:1969-10-17
卷期号:166 (3903): 377-381
被引量:475
标识
DOI:10.1126/science.166.3903.377
摘要
A correlation of time with depth has been evaluated for the Camp Century, Greenland, 1390 meter deep ice core. Oxygen isotopes in approximately 1600 samples throughout the core have been analyzed. Long-term variations in the isotopic composition of the ice reflect the climatic changes during the past nearly 100,000 years. Climatic oscillations with periods of 120, 940, and 13,000 years are observed.
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