ボロンイソトープの証拠は,最後の脱氷期中に大洋の二酸化炭素が漏れた証拠である
M A Martínez-Botí1, G Marino2, G L Foster1
1Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK.
Nature
|February 13, 2015
まとめ
大気中の二酸化炭素 (CO2) 濃度は,氷河期に大きく変動した. この研究は,南大洋が脱氷期に二酸化炭素を放出し,地球の気候を調節する役割を支えていることを明らかにしています.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 海洋学 海洋学とは
背景:
- 氷河期と氷河期間の大気中の二酸化炭素の変動を理解することは,気候システム研究にとって極めて重要です.
- 仮説によると,南洋のプロセスに影響を受けた深海の炭素貯蔵の変化が,これらのCO2の変動を誘発している.
- 過去の海洋炭酸塩系の変化を再構築することは,限られたプロキシデータが限られているため,困難です.
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