まとめ
底流はタスマン流域の深海沈殿物を侵食し,大きな不一致を明らかにした. この侵食は,気候の冷却と南極の氷河化に関連した南極底水の速度の増加によって引き起こされた可能性が高い.
科学分野:
- 海洋地質学 海洋地質学
- パレオセアノグラフィー
- 堆積地質学 堆積地質学とは
背景:
- 深海の沈殿物は,地球の歴史を記録しています.
- 海流は,堆積物の移動と堆積に重要な役割を果たします.
- タスマン流域は,南大洋の動態を理解するための重要な地域です.
研究 の 目的:
- 南タスマンの盆地における堆積物の浸食と堆積のパターンを調査する.
- 重要な堆積物不一致の年齢と範囲を決定する.
- 強化された底流動活動の古海洋学的要因を理解するために.
主な方法:
- 堆積物核の古磁気分析 堆積物核の古磁気分析 堆積物核の古磁気分析
- 堆積物の中のマイクロ化石の微古生物学的な年代測定.
- 海底の地質的地図作成により,浸食特性を特定する.
主要な成果:
- 南タスマン盆地では,大規模な堆積物浸食地域が特定されました.
- 初期のプレオセンのような古い堆積物が侵食されています.
- 侵食表面は,主要な堆積物不一致を表しています.
結論:
- 南極の底水の速度の増加は,観測された侵食の主な原因です.
- この速度の上昇は,ケノゾイク期後半の気候の冷却と関連している可能性が高い.
- 強化された南極氷河は,底流の強化に寄与している可能性があります.
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