大気中のCO2における氷河期間氷河期間の変化の塵による制御に反対する証拠
1Centre for Environmental Magnetism and Palaeomagnetism (CEMP) and Stable Isotope Laboratory, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK. b.maher@lancaster.ac.uk
Nature
|May 11, 2001
まとめ
大気中の塵による南洋の鉄の肥料化が,最後の脱氷期中に大気中のCO2レベルに重大な影響を及ぼさなかった. 北大西洋の塵のピークはCO2の変化と相関せず,この気候規制理論に異議を唱えた.
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
- 海洋学 海洋学 海洋学
- 地質化学 地質化学
背景:
- 氷河期には大気中のCO2濃度が低かったが,これは海洋の鉄の肥料化が増加したためかもしれない.
- 南洋の植物プランクトンは,鉄の堆積によって刺激された二酸化炭素の吸収を増加させた可能性がある.
- 南大洋の塵の流れは低いため,生産性に影響を与える遠隔鉄の源の仮説が提唱されている.
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