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オリゴセーン/ミオセンの境界にある東南極氷床の軌道による振動

T R Naish1, K J Woolfe, P J Barrett

  • 1Institute of Geological and Nuclear Sciences, PO Box 30368, Lower Hutt, New Zealand. t.naish@gns.cri.nz

Nature
|October 19, 2001
PubMed
まとめ

南極の氷床は,オリゴセーン/ミオセンの移行期に軌道サイクルによって変動した. 堆積物核は,東南極の氷床の間の直接的なつながりを明らかにしています.

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