概括
来自南哈萨克斯坦的Vendian (晚期前剑桥纪) Conophyton化石揭示了多样化的蓝藻和真核藻类. 这些微生物,与他们形成的树岩不同,在前坎布里亚-坎布里亚灭绝事件中幸存下来.
科学领域:
- 古生物学的古生物学
- 微生物学 微生物学
- 地质地质地质地质地质地
背景情况:
- 纪 (晚期的甲纪) 时期对于理解早期生命演变至关重要.
- 包括Conophyton在内的斯特罗马托石是古代微生物生态系统的关键指标.
- 前坎布里亚-坎布里亚时期的边界标志着地球历史上一个重要的灭绝事件.
研究的目的:
- 为了研究Conophyton gaubitza stromatolites的微生物组成.
- 为了确定这些古老结构中存在的藻类类型.
- 为了确定前坎布里亚时代以外的构建 stromatolite 的微生物的生存.
主要方法:
- 来自南哈萨克斯坦的化科诺菲顿高比扎标本的分析.
- 显微镜检查用于识别和分类保存的微生物.
- 微生物群的存活率与藻类灭绝模式的比较.
主要成果:
- 在Conophyton中发现了一种保存良好的多样化的蓝藻和真核藻类组合.
- 这代表了苏联首次报告的树枝状微生物群.
- 已识别的微生物并没有在前剑桥纪末期灭绝.
结论:
- Conophyton gaubitza stromatolites提供了一个复杂的微生物社区.
- 这些 stromatolites 的建造者表现出比以前想象的更大的弹性.
- 这一发现挑战了前坎布里亚-坎布里亚微生物灭绝事件的现有模型.
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