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南极冰盖在米奥世早期的千年级变化

Nicholas B Sullivan1, Stephen R Meyers1, Richard H Levy2,3

  • 1Department of Geoscience, University of Wisconsin-Madison, Madison, WI 53706.

Proceedings of the National Academy of Sciences of the United States of America
|September 18, 2023
PubMed
概括

东南极洲米奥森早期的千年级冰盖变化是由天文强迫驱动的. 这揭示了冰盖动态响应轨道周期,即使在温暖的气候,影响未来的气候变化理解.

关键词:
在米奥琴时期,冰层是一个冰层.循环平面绘图 (cyclostratigraphy) 是一种循环平面绘图.古代气候是一种古气候.

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