南極の底水:オーストラリアと南極の間のケノゾイク期後半の速度の大変化

Science (New York, N.Y.)
|August 27, 1971
PubMed
まとめ

底流はタスマン流域の深海沈殿物を侵食し,大きな不一致を明らかにした. この侵食は,気候の冷却と南極の氷河化に関連した南極底水の速度の増加によって引き起こされた可能性が高い.

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