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末次冰消期倒数第二阶段,在休恩半岛记录到的海平面快速波动。

Rapid fluctuations in sea level recorded at huon peninsula during the penultimate deglaciation.

作者信息

Esat TM, McCulloch MT, Chappell J, Pillans B, Omura A

机构信息

T. 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.

出版信息

Science. 1999 Jan 8;283(5399):197-201. doi: 10.1126/science.283.5399.197.

Abstract

About 140,000 years ago, the breakup of large continental ice sheets initiated the Last Interglacial period. Sea level rose and peaked around 135,000 years ago about 14 meters below present levels. A record of Last Interglacial sea levels between 116,000 years to 136, 000 years ago is preserved at reef VII of the uplifted coral terraces of Huon Peninsula in Papua New Guinea. However, corals from a cave situated about 90 meters below the crest of reef VII are 130, 000 +/- 2000 years old and appear to have grown in conditions that were 6 degreesC cooler than those at present. These observations imply a drop in sea level of 60 to 80 meters. After 130,000 years, sea level began rising again in response to the major insolation maximum at 126,000 to 128,000 years ago. The early (about 140,000 years ago) start of the penultimate deglaciation, well before the peak in insolation, is consistent with the Devils Hole chronology.

摘要

约14万年前,大型大陆冰盖的解体开启了末次间冰期。海平面上升,并在约13.5万年前达到峰值,比当前海平面低约14米。新几内亚岛胡恩半岛隆起珊瑚台地的礁VII保存了11.6万至13.6万年前末次间冰期海平面的记录。然而,位于礁VII顶部以下约90米处一个洞穴中的珊瑚有130000±2000年历史,它们似乎生长在比当前温度低6摄氏度的环境中。这些观察结果意味着海平面下降了60至80米。13万年之后,由于12.6万至12.8万年前的主要日照最大值,海平面再次开始上升。倒数第二次冰消期在约14万年前很早就开始了,远早于日照峰值,这与魔鬼洞年代学一致。

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