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Updated: Aug 13, 2026

Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod
06:06

Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod

Published on: August 17, 2016

海面の急速な変動は,前回の脱氷期にフオン半島で記録された

Esat1, McCulloch, Chappell

  • 1T. M. Esat, M. T. McCulloch, J. Chappell, B. Pillans, Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia. A. Omura, Kanazawa University, Kanazawa, Ishikawa 920, Japan.

Science (New York, N.Y.)
|January 8, 1999
PubMed
まとめ

最後の氷河間期には,海面が大きく変化し,寒い洞窟のサンゴの成長により,海面が著しく低下した. 海面が再び上昇し始めたのは,約13万年前.

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