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東部 の 熱帯 太平洋 の 酸素 の 欠乏 し た 海水 の 氷河 膨張
Babette A A Hoogakker1,2, Zunli Lu3,4, Natalie Umling5
1The Lyell Centre, Heriot-Watt University, Edinburgh, UK. b.hoogakker@hw.ac.uk.
Nature
|October 19, 2018
まとめ
氷河期における大気中の二酸化炭素の減少を 海洋の炭素貯蔵が説明するかもしれません 新しい研究によると 氷河太平洋の酸素の減少により 炭素の貯蔵量が増加しています
科学分野:
- 古代海洋学
- 海洋生物化学
- 気候科学
背景:
- 氷河期における大気中の二酸化炭素の減少のための提案されたメカニズムです.
- 以前の研究では 深海の酸素は低かったが 氷河太平洋の上部がより酸素に富んだと示唆されていた.
- この垂直の対比は 海洋の炭素貯蔵量の 微小な変化を示しています
研究 の 目的:
- 最後の氷河期以来の 低酸素水域の変化を再現する
- 氷河期の大気中の二酸化炭素の減少における太平洋の炭素貯蔵庫の役割を調査する.
主な方法:
- 上水柱と下水柱の酸素再構築を組み合わせた二重プロキシアプローチを使用しました.
- 呼吸する炭素貯蔵庫を推定するために,深海の量的な酸素データを適用した.
主要な成果:
- 最後の氷河期における 東太平洋の酸素の減少の 証拠です
- 氷河期中の上層水柱の酸素化が増加した兆候はない.
- 太平洋の氷河で 呼吸する炭素の貯蔵量が大幅に増加しました
結論:
- 太平洋の氷河は 酸素の枯渇を体験し 炭素の貯蔵量を増加させました
- 氷河期の間 大気中の二酸化炭素を 減少させる重要な要因でした
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