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オリゴトロフィーと窒素固定は,地中海東部のサプロペルのイベント中に発生します
1Department of Environmental Science, Barnard College, Columbia University, 3009 Broadway, New York, NY 10027, USA. Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
まとめ
化石クロロフィルの窒素同位体データは,地中海におけるプレイストセンの終わりのサプロペル形成の間に栄養素が欠乏した表面水と高い窒素固定を示しています. これは,特殊な植物プランクトンの咲きを示唆し,ユートロフィケーションではなく,サプロペルの堆積を助長した.
科学分野:
- パレオセアノグラフィー
- マリン・ジオケミストリー 海洋地化学
- バイオジオケミストリー バイオジオケミストリー
背景:
- 地中海東部のプレイストセンの後半のサプロペルは,生産性が高い時期を示唆しています.
- 以前の研究では,栄養素の濃縮や循環の変化の可能性が示されていた.
- サプロペルの形成を駆動する正確なメカニズムについては,依然として議論されている.
研究 の 目的:
- プレイストセンの後半のサプロペル形成における有機物質の源泉と栄養素の条件を調査する.
- 地化学的証拠と地中海のサプロペル堆積の既存のモデルを調和させる.
- ユートロフィケーションと循環パターンに関する仮説を検証する.
主な方法:
- 化石クロロフィルの窒素同位体の測定.
- 地中海東部の有機に富んだ堆積物核 (サプロペル) の分析.
- 古代海洋学モデルの文脈における同位体データの地球化学的解釈.
主要な成果:
- 窒素同位体データは,層分化され,栄養素が欠乏した地表水を示しています.
- 微生物による窒素固定が有意であることを示す証拠があります.
- サプロペルの形成は,特殊な植物プランクトンの開花と大量沈没イベントと関連しています.
- 結果は,広範囲にわたる優太化や循環の逆転を裏付けるものではない.
結論:
- サプロペルの形成は,分層化され,栄養素が少ない条件に適応したユニークな植物プランクトンコミュニティによって推進されました.
- 窒素固定は,この生態系を支える上で重要な役割を果たしました.
- この発見は,河川の流入量の増加や主要な循環のシフトが主な要因であるという以前の解釈に異議を唱えている.
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