概括
碳酸炭球含有两种类型的碳,它们的碳-13和碳-12比率不同. 这表明沼泽沉和化石衍生的碳酸盐材料的混合.
科学领域:
- 地质化学 地质化学
- 古植物学是古植物学.
- 沉积物学的沉积物学
背景情况:
- 煤球是通过矿化保存的化石植物材料,通常是石或石.
- 了解煤球中的碳酸盐的起源对于解释它们的形成环境至关重要.
研究的目的:
- 为了研究不同类型的煤球中的碳酸盐的碳同位素组成 (C(13):C(12) 比率.
- 为了测试煤炭球含有authigenic和allogenic碳酸盐混合物的假设.
主要方法:
- 在碳酸盐中的碳同位素比率 (C(13):C(12) 的分析来自"正常"",野生"和"混合"的煤球.
- 对同位素特征进行比较,以识别不同的碳酸盐来源.
主要成果:
- 研究的煤球中的C13:C12比率与碳酸盐类型的混合物相一致.
- 一个成分显示了C(13) 的耗尽,这是现场沉碳酸盐的特征.
- 另一个成分被丰富了C(13),与外来化石碎片一致.
结论:
- 石灰质煤球由不同比例的沉碳酸盐和外来破碎物质组成.
- 同位素数据支持一个模型,包括早期的基因沉和化石碎片在煤沼环境中的结合.
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