重新评估最早生命痕迹的证据
Mark A van Zuilen1, Aivo Lepland, Gustaf Arrhenius
1Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093-0236, USA. mvanzuil@ucsd.edu
Nature
|August 9, 2002
概括
古代岩石中的石墨可能不表明早期生命. 新的研究表明,这种石墨是由二次静脉中的非生物过程形成的,需要重新评估早期生命证据.
科学领域:
- 地质化学 地质化学
- 天体生物学 天体生物学
- 早期地球的条件.
背景情况:
- 石墨的同位素成分是古老的转化岩石中的关键生物标志物.
- 之前对伊沙亚上皮带 (ISB) 石墨的研究表明,早期的阿基亚微生物生命.
- 由于新的发现,这种解释需要仔细重新审查.
研究的目的:
- 为了调查石墨在伊沙沙上皮带 (ISB) 的起源.
- 重新评估石墨在早期阿尔盖岩石中的生物学意义.
- 挑战现有的早期生命生物标志物.
主要方法:
- 对ISB岩石进行地质测绘和岩石分析.
- 石墨和相关矿物质的现场化学分析.
- 石墨形成反应的热力学建模.
主要成果:
- 石墨在ISB中的二次碳酸盐脉中非常丰富.
- 这些静脉是通过在深处注射热液体而形成的.
- 石墨起源于铁碳酸盐的高温不成比例,这是一个非生物过程.
结论:
- 石墨在ISB碳酸盐脉中的存在并不支持一个庞大的微生物生态系统.
- 从碳酸盐中形成的甲体质石墨提供了一个替代的非生物解释.
- 以往基于ISB石墨的早期生命证据需要重新评估.
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