在常青草泥炭中硫的二氧化生成和煤炭中矿的起源
概括
减少硫的细菌通过消耗有机硫化合物,在有机丰富的沼泽中驱动皮里特的形成. 这一过程解释了煤炭和有机沉积物中的硫分布,包括化石组织中发现的矿.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 沉积物学的沉积物学
背景情况:
- 硫化合物在沼泽等有机丰富的环境中至关重要,影响地质过程.
- 了解硫的转化途径是解释沉积物记录的关键.
研究的目的:
- 为了阐明埃弗格莱德斯泥炭中矿形成的机制.
- 将微生物硫循环与煤炭和沉积物中硫化合物的原生成联系起来.
主要方法:
- 在埃弗格莱德斯盆地的泥炭样本中分析了硫的转化模式.
- 研究微生物异型呼吸过程.
主要成果:
- 矿的形成与微生物利用有机氧硫化合物直接相关.
- 这种微生物过程决定了低含硫煤和相关有机沉积物的硫物种分布.
- 该机制解释了化石组织中framboidal pyrite的存在.
结论:
- 减少硫的细菌对有机氧硫化合物的分散呼吸是有机丰富的沼泽中矿形成的主要驱动因素.
- 这种类型生成为硫化合物分布和煤炭,有机土壤和沉积物中矿的出现提供了统一的解释.
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