ホロセンの炭素サイクルにおける安定同位体制約は,南極の氷の核からの変化によるものです
Joachim Elsig1, Jochen Schmitt, Daiana Leuenberger
1Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
Nature
|September 26, 2009
まとめ
ホロセンの大気中のCO2の変化は,ホロセンの初期に陸地生物圏の炭素吸収と海洋の放出によって引き起こされた. 後のホロセンの増加は,主に海洋炭酸補償とサンゴ礁の形成によるものでした.
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
- 炭素循環に関する研究
- イソトープ地球化学 イソトープ地球化学
背景:
- 大気中のCO2濃度は,ホロセーン時代に大きく変動した.
- これらのCO2シフトを駆動する正確なメカニズムは不明である.
- 貯水池の間の炭素同位体シグネチャーは,CO2フルスダイナミクスのヒントを提供します.
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