パレオセノ・エオセノ熱極期における大規模な海洋脱酸素化
Weiqi Yao1, Adina Paytan2, Ulrich G Wortmann3
1Department of Earth Sciences, University of Toronto, Toronto, Ontario, M5S 3B1, Canada. weiqi.yao@mail.utoronto.ca.
まとめ
地球温暖化によって 海洋の酸素が失われ 深海の生態系は 居住不可能になります パレオセーヌ・エオセーヌ熱最大値 (PETM) 研究では 硫化状態が海洋生物と漁業に 影響を及ぼしていることが示されています
科学分野:
- 古代海洋学
- 海洋生物学
- 気候科学
背景:
- 地球温暖化が漁業に与える影響は不明です
- 地質学的記録は 炭素循環の変化と 海洋の脱酸素化を結びつけています
- パレオセーヌ・エオセーヌ熱最大値 (PETM) は,気候変動の関連アナログを提供します.
研究 の 目的:
- 海洋の酸素の減少を調査する
- 深海での硫化物汚染の可能性を評価する.
- 海洋生態系と漁業への影響を理解する
主な方法:
- PETMからの硫黄同位体データの分析
- 環境条件をシミュレートするために海洋モデリング.
主要な成果:
- PETMでは,硫黄同位体の出所が1ミリ単位で陽性であった.
- 海洋の大部分が硫化物になったことを示しています
- 硫化水素の毒性は,メソペラジックとバチペラジックゾーンを脅かします.
結論:
- PETMは海の大量の脱酸素と硫化状態を経験しました.
- 深海の生態系は硫化水素の毒性から深刻な脅威に直面しています
- 将来の温暖化シナリオは 海洋生物の生息地の大幅な喪失につながる可能性があります
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