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Disorders of Erythrocytes
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パレオセーン/エオセーン熱的最大期における亜熱帯北極海の温度
Appy Sluijs1, Stefan Schouten, Mark Pagani
1Palaeoecology, Institute of Environmental Biology, Utrecht University, Laboratory of Palaeobotany and Palynology, Budapestlaan 4, 3584 CD Utrecht, The Netherlands. a.sluijs@bio.uu.nl
Nature
|June 6, 2006
まとめ
パレオセーン/エオセンの熱極は,5500万年前に極度の北極温暖化を引き起こした. 北極海の気温は上昇し,氷がないことを示し,温室効果ガスやその他のフィードバックから放大された温暖化を示唆しました.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 気候科学 気候科学
- 海洋学 海洋学 海洋学
背景:
- パレオセーン/エオセーン熱最大 (PETM) は,大規模な温室効果ガスの放出に関連した極端な地球温暖化の期間でした.
- 以前の研究では,低緯度でのPETM環境変化が記録されていたが,北極のデータは欠けていた.
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