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Updated: Jun 12, 2025

Conducting Miller-Urey Experiments
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石中常见的氨基酸诱导了粘土脱皮和非生物区间的形成

Orr Rose Bezaly1,2, Annemieke Petrignani1, Helen E King2,3

  • 1Molecular Photonics, Van 't Hoff Institute for Molecular Sciences, Faculty of Science, University of Amsterdam, Science Park 904, Amsterdam, 1098 XH The Netherlands.

Communications earth & environment
|June 9, 2025
PubMed
概括

石来源的玛-氨基黄油酸不可逆转地改变了蒙莫里隆石的粘土结构. 这种相互作用创造了纳米尺度的空洞,可能有助于前生物的细分,并提供新的纳米复合材料合成路径.

关键词:
天体生物学 天体生物学地质化学 地质化学矿物学是什么?矿物学是什么?生命的起源 生命的起源

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Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
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