概括
对碳状混凝土的分析揭示了不同的碳同位素比率. 这些发现表明,这些石中的碳酸盐,剩余碳和一些有机化合物是土著的,为早期太阳系材料提供了洞察力.
科学领域:
- 宇宙化学 宇宙化学
- 天体生物学 天体生物学
- 地质化学 地质化学
背景情况:
- 碳状石是原始的石,为早期太阳系提供了关键的见解.
- 了解石中的有机化合物和碳酸盐的起源是天体生物学和行星科学的关键.
研究的目的:
- 分析碳的同位素组成在各种分数 (可溶性有机化合物,碳酸盐,剩余碳) 的七个碳酸.
- 确定石中这些含碳成分的起源 (内源与外源).
主要方法:
- 从石样本中化学提取可溶性有机化合物,碳酸盐和剩余碳.
- 碳-13/碳-12 (13C/12C) 同位素比率测量使用质谱学,相对于海洋碳酸盐标准.
主要成果:
- 同位素测量显示了每个分量的不同的范围:碳酸盐 (+40至+70‰),残碳 (-15至-17‰) 和可溶有机物质 (-17至-27‰,其中一个异常值为-5.5‰).
- 碳酸盐和剩余碳的观察到的13C/12C值与典型的外星有机物有显著的不同,这表明其起源是内源的.
结论:
- 同位素数据强烈表明,碳酸盐,剩余碳和一部分可溶性有机物是分析碳状地质的本地物质.
- 这一发现支持了复杂的有机化学和碳酸盐形成在这些石的母体中发生的假设.
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