南洋の塵と気候の結合は,過去400万年にわたって続いている
Alfredo Martínez-Garcia1, Antoni Rosell-Melé, Samuel L Jaccard
1Geological Institute, ETH Zürich, Zürich 8092, Switzerland. alfredo.martinez-garcia@erdw.ethz.ch
Nature
|August 5, 2011
まとめ
南大洋への塵の供給は,約125万年前に大幅に増加し,主要な氷河期の始まりと一致しました. この発見は,大気中の塵の増加を地球と結びつける.
科学分野:
- 古代気候学と地球システム科学
- 海洋地化学と沈殿物学について
- クォーターナー期気候ダイナミクス
背景:
- 大気中の塵は,放射能のバランスを変化させ,鉄のような海洋微量栄養素を提供することで,地球温暖化に影響を与えます.
- 南洋の塵の堆積と関連する"鉄の肥料化"は,氷河期間の大気中の二酸化炭素の減少に関与しています.
- プレイストセンの氷河周期における南洋の塵の長期的役割は,未だに十分に理解されていない.
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