チェルツのシリコンイソトープに基づいたプレカンブリア海の古気温曲線
François Robert1, Marc Chaussidon
1Muséum National d'Histoire Naturelle, CNRS LEME NanoAnalyses, UMS 2679, 57 rue Cuvier, 75005 Paris, France. robert@mnhn.fr
Nature
|October 27, 2006
まとめ
カンブリア以前の海は,古代の桜のシリコン同位体分析によると,70°Cから20°Cに大幅に冷却された. この新しい方法は,長期の海洋冷却の傾向を確認し,気候データの信頼性に関する以前の議論を解決します.
科学分野:
- 地質化学 地質化学
- 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
- 堆積地質学 堆積地質学とは
背景:
- プレカンブリア気候記録は,極端な暑さから地球規模の氷河化まで,劇的な気温変動を明らかにしています.
- チェルツの酸素同位体比は,過去の海面温度を推論するために使用されてきたが,その信頼性は,堆積後の潜在的な変化のために議論されている.
関連する概念動画
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