大気中のCO2の氷河期間の変化に対するフォアミニフェラルカルシフィケーション反応
Stephen Barker1, Henry Elderfield
1Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. sbar98@esc.cam.ac.uk
まとめ
海洋フォラミニフェラの殻の重さは,過去の二酸化炭素レベルを明らかにします. 大気中のCO2濃度の上昇は,海洋の化に直接影響を及ぼし,地球的な炭素循環と古海洋学的プロキシアプリケーションに影響を与えます.
科学分野:
- パレオセアノグラフィー
- 海洋地化学は,海洋地化学である.
- 気候科学 気候科学
背景:
- フォラミニフェラは重要な海洋カルシファーです.
- 海水の炭酸イオン濃度は殻形成に影響する.
- 大気中のCO2レベルは,氷河期と氷河間周期の間に変動します.
研究 の 目的:
- 表面海水の二酸化炭素記録を再構築する.
- 大気中のCO2が海洋の化に及ぼす影響を調査する.
- 海洋の化と大気中のCO2の間のフィードバックメカニズムを評価する.
主な方法:
- ターミネーションI.の全域でフォラミニフェラル殻の重量を分析する.
- 殻の重量と海水の炭酸イオン濃度の相関.
- 過去の表面海水のCO2濃度を再構築する.
主要な成果:
- Foraminiferal貝殻の重量記録は,海水の炭酸イオン濃度を追跡しています.
- 再構築された地表海水のCO2記録は,大気記録と一致しています.
- 大気中のCO2の上昇は,海洋の化の変化と直接相関しています.
結論:
- 海洋の石灰化は大気中のCO2レベルに敏感です.
- この感受性は,大気中のCO2に負のフィードバックを与える.
- この発見は,古海洋学的なプロキシを解釈し,気候の動態を理解するために極めて重要です.
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