质疑地球上最古老化石的证据
Martin D Brasier1, Owen R Green, Andrew P Jephcoat
1Earth Sciences Department, University of Oxford, Parks Road, Oxford OX1 3PR, UK. martinb@earth.ox.ac.uk
Nature
|March 8, 2002
概括
西澳大利亚的古老微化石样结构被重新解释为非生物文物. 这项研究挑战了生产氧气的光合作用和地球上的生命的早期证据,建议非生物起源.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 天体生物学 天体生物学
背景情况:
- 来自西澳大利亚的Apex chert微化石 (3.465亿年前) 被认为是最古老的生命和早期氧化光合作用的形态证据.
- 之前已经确定了11种丝状 prokaryote 物种,满足了真正的古老微化石的标准.
- 这些发现早于其他关于蓝藻菌和氧气大气层的证据近10亿年.
研究的目的:
- 重新评估阿佩克斯研究所所谓的微化石的生物起源.
- 研究这些古老结构的地质和化学背景.
- 为了确定这些结构是否代表了生命早期或非生物过程.
主要方法:
- 微观分析 (光学和电子显微镜)
- 地质化学技术 (微型拉曼光谱)
- 数字图像分析和地质样本的绘制.
主要成果:
- 以前被认定为微化石的结构被重新解释为二次文物.
- 这些文物是由水热脉和火山玻璃中的无形石墨形成的.
- 新的研究没有支持任何主要的生物形态学.
结论:
- 地球上生命的最古老的形态证据,基于Apex chert微化石,被驳斥了.
- 这些结构不支持早期的氧气生成光合作用.
- 对于早期的热水系统,已经推断出了包括费舍尔-托普施类型合成在内的非生物过程.
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