大気中の二酸化炭素濃度の変化が,初期ケノゾイク期の気候の主要な要因であった
Eleni Anagnostou1, Eleanor H John2, Kirsty M Edgar2,3
1Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK.
Nature
|April 26, 2016
まとめ
初期のエオセンの気候最適期は 6500万年で最も暖かい時期でした 新しい研究によると 二酸化炭素 (CO2) 濃度は 約1,400ppmで 温暖化と冷却を後押ししています
科学分野:
- 古代気候学
- 地化学
背景:
- 初期エオセンの気候最適期 (Early Eocene Climate Optimum, EECO) は過去6500万年で最も暖かい時期であり,工業化以前の水準より10°C以上暖かい時期でした.
- 地球の冷却はエオセーン時代に続き 南極の氷床の形成につながった.
- 以前のエオセンの大気中の二酸化炭素 (CO2) 濃度 (500〜3,000ppm) の推定値は精度が不足しており,炭素と気候の相互作用の理解を妨げていた.
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