深海におけるエオセーン/オリゴセーン境界イベント
まとめ
エオセノ/オリゴセノ境界線は,大量絶滅ではなく,微生物化石の漸進的な変化を示している. ボリド衝突ではなく,古代気候の変化が,古代時代後半の生物学的変化を引き起こした.
科学分野:
- パレオントロジー・パレオントロジー
- マイクロパレオンタロジーとは
- パレオセアノグラフィー
背景:
- エオセノ/オリゴセノ境界は,地球の歴史における重要な間隔である.
- 以前の仮説では,この境界で大災害,おそらくボリデ衝突が起きたと示唆されていた.
研究 の 目的:
- エオセン/オリゴセンの境界を越えた生物学的変化を分析する.
- 紀元後期における生物学的変化の原因を調査する.
主な方法:
- 石灰質の微生物化石の分析.
- シリケスの微生物化石の分析.
主要な成果:
- 生物学的変化が徐々に観察され,大規模な絶滅の証拠はありません.
- 変化する古気候と古海洋学的条件と相関する生物学的シフトを特定した.
- 壊滅的な生物学的イベントを引き起こすボライド衝突イベントの支持は見つかりませんでした.
結論:
- エオセノ/オリゴセノ間の生物学的変化は,環境の変化によって徐々に進み,環境変化によって引き起こされた.
- 紀元後期には,海洋生物に影響を及ぼした重要な古海洋学と古気候の変化を経験しました.
- このデータは,エオセーン/オリゴセーン境界におけるボリデ衝突による大量絶滅の仮説を否定している.
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