南极地底水:在澳大利亚和南极洲之间的晚代代纪期间,速度的重大变化

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

底流侵蚀了塔斯曼盆地的深海沉积物,揭示了主要的不一致性. 这种侵蚀很可能是由于与气候冷却和南极冰川化相关的南极地底水速度增加造成的.

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