クレタ紀後半の北極海の高温
Hugh C Jenkyns1, Astrid Forster, Stefan Schouten
1Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK. hughj@earth.ox.ac.uk
Nature
|December 17, 2004
まとめ
北極海の水温は約15°Cで,暖かい極地気候を明らかにした. この研究では,新しいTEX86古熱計を使用して,古代の海面温度を再構築しました.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 地質化学 地質化学
背景:
- 紀元後期の気候の動態を理解するには,極の古気温に関する知識が必要です.
- 北極海の初期の古海洋学の歴史は,アクセスの難しさのためにほとんど理解されていません.
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