生物标志物证明了沉积有机碳的主要保存途径
Y Hebting1, P Schaeffer, A Behrens
1Laboratoire de Géochimie Bioorganique, Unité Mixte de Recherche 7509 du CNRS, Université Louis Pasteur, Ecole de Chimie, Polymères, Matériaux de Strasbourg, 25 rue Becquerel, 67200 Strasbourg, France.
概括
早期的基因生成涉及生物分子的非生物化到化石生物标记物. 硫化 (H2S) 等硫物种作为捐赠物,在沉积物中保存有机碳.
科学领域:
- 地质化学 地质化学
- 有机地化学 有机地化学
- 沉积物学的沉积物学
背景情况:
- 将生物分子化为化石生物标志物对于无氧沉积物中的有机物质保存至关重要.
- 这些早期的代谢遗传过程仍然不太了解.
- 了解这些路径是解释岩石记录的关键.
研究的目的:
- 为了研究生物分子减少在早期diagenesis的机制.
- 确定参与减少生物标志物的形成的捐赠者.
- 为了阐明生物标志物基因生成中的非生物学途径.
主要方法:
- 在最近的沉积物中分析减少的胡卜素.
- 模拟基因条件的实验室实验.
- 确定硫物种作为气捐赠者.
主要成果:
- 在最近的沉积物中发现了减少的胡卜素,这表明早期的基因突变.
- 这些减少发生在没有结构或立体化学特异性的情况下,这表明非生物途径.
- 硫物种,特别是硫化 (H2S),在实验室实验中被证实是有效的捐赠者.
结论:
- 硫物种的非生物化是早期二代发生的一个关键过程.
- 这一途径有助于在沉积岩中保存丰富的有机碳.
- 这些发现为从生物分子中形成化石生物标记物提供了新的见解.
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