古代気候学: 古代の古土と古代の空気
1Department of Geophysics, Stanford University, Stanford, California 94305, USA. norm@pangea.stanford.edu
Nature
|December 8, 2004
まとめ
古代の土壌におけるシデライトの存在は,大気中の二酸化炭素濃度を示し,以前の仮定に異議を唱える. この発見は,初期の地球を理解するために極めて重要です.
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
背景:
- 鉄炭酸,鉱物シデライトは,アルカイア時代の古土石に含まれています.
- 以前の研究によると,シデライトの存在は,アルカイア期の大気中の二酸化炭素に関する限られた洞察を与えてくれると示唆されていた.
関連する概念動画
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