概括
南非维特沃特斯兰德系统中的聚合碳化合物表明有机起源. 碳同位素分析表明,生物活动存在于215亿年前.
科学领域:
- 地质化学 地质化学
- 古生物学的古生物学
- 同位素地质学的同位素.
背景情况:
- 南非的维特沃特斯兰德系统中含有金集团.
- 这些聚合物中含有来源不明的聚合碳化合物.
研究的目的:
- 研究在维特沃特斯兰德系统中发现的聚合碳化合物的起源.
- 为了确定这些碳化合物是否有机或无机衍生.
主要方法:
- 在聚合碳化合物中分析碳同位素比率 (deltaC(13) .
- 同位素值与已知范围对沉积有机碳的比较.
主要成果:
- 德尔塔C(13) 值在每千米22.4至32.8之间.
- 这些同位素成分属于沉积性有机碳的典型范围.
结论:
- 同位素数据强烈表明碳化合物的有机起源.
- 这一发现支持了215亿年前的早期生物活动和有机进化模型.
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