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プレイストセーン中期の海循環危機を振り返る
Sophia K V Hines1, Christopher D Charles2, Aidan Starr3,4
1Department of Marine Chemistry & Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
まとめ
プレイストセンの中期移行 (MPT) は深海循環危機を伴わなかった. 私たちの研究では 氷河期深海の変動が一貫しており 気候変動の際に 炭素の貯蔵がわずかに変化しています
科学分野:
- 古代海洋学
- 気候科学
- 地化学
背景:
- プレイストセンの中期 (約125万年前から850万年前) の移行は,氷河期から氷河期間の気候サイクルに大きな変化をもたらした.
- 主要な仮説は,プレイストセンの中期の移行の原因として,約0.90万年前の深海の循環危機を提案した.
研究 の 目的:
- プレイストセンの中期の循環の変化の役割を調査する.
- 約0.90万年の循環"危機"の仮説を検証する.
主な方法:
- 高解像度ペア化されたネオジウム,炭素,酸素同位体のデータ分析.
- 南大西洋 (ケープ盆地) の過去の深海循環と炭素貯蔵の再構築
主要な成果:
- プレイストセンの中期にわたる深海循環の実質的な変化の証拠は見つかりませんでした.
- MPT前期と初期における氷河の深海変動は,最も最近の氷河周期を反映した.
- 深海層の形成は 炭素を貯蔵するために ほんのわずかな循環調整を 必要とした.
結論:
- 深海循環の根本的な変化や危機によって引き起こされたのではありません
- 海洋循環は安定しており 層分化による炭素貯蔵の増加に対応するわずかな調整があった.
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