エバーグレイドの泥炭における硫黄のダイアゲネシス,石炭におけるピライトの起源
まとめ
硫黄を減らすバクテリアは,有機硫黄化合物を消費することによって,有機豊富な沼地のピライト形成を駆動します. このプロセスは,化石化した組織に存在するピライトを含む石炭と有機堆積物における硫黄の分布を説明する.
科学分野:
- 地質化学 地質化学
- 微生物学 微生物学とは
- 堆積物学 堆積物学 堆積物学 堆積物学 堆積物学
背景:
- 硫黄化合物は,沼地などの有機に富んだ環境において極めて重要であり,地質学的過程に影響を与えます.
- 硫黄の変換経路を理解することは,堆積物記録の解釈の鍵です.
研究 の 目的:
- エバーグレーズでピライト形成のメカニズムを解明するため.
- 炭や沈殿物の硫黄化合物のパラゲネシスと微生物の硫黄循環を結びつける.
主な方法:
- エバーグレーズ流域の泥炭サンプルにおける硫黄変換パターンの分析.
- 微生物の似ていない呼吸過程の調査.
主要な成果:
- ピライトの形成は,有機酸化硫黄化合物の微生物利用と直接関連しています.
- この微生物のプロセスは,低硫黄炭および関連する有機堆積物における硫黄種の分布を決定する.
- このメカニズムは,化石化した組織の中にフランボイドのピライトの存在を説明する.
結論:
- 硫黄を還元するバクテリアによる有機酸化硫黄化合物の分散呼吸は,有機豊富な沼地のピライト形成の主な要因です.
- このパラゲネシスは,硫黄化合物の分布と石炭,有機土壌,堆積物におけるピライトの発生について統一された説明を提供します.
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