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プレイストセンの半ばの気候移行を通して,海洋温度と氷の量の進化

H Elderfield1, P Ferretti, M Greaves

  • 1Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK. he101@cam.ac.uk

Science (New York, N.Y.)
|August 11, 2012
PubMed
まとめ

プレイストセーン中期の移行期 (MPT) は,地球の気候サイクルを10万年というより長い周期に移した. この変化は,90万年前に南極の氷の量が急増したことで引き起こされた.

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