概括
迄今为止发现的最古老的宏观环,可以追溯到低坎布里亚时期,揭示了大型内石生物在硬部位动物进化后不久就存在.
科学领域:
- 古生物学的古生物学
- 这种技术是什么?
- 珊瑚礁的地质学
背景情况:
- 巨型的化石记录,证明有机体钻入硬基板的证据,对于了解早期动物行为和生态相互作用至关重要.
- 以前最古老的巨型矿石已知来自下奥尔多维纪时期.
研究的目的:
- 报告发现了新的,非常古老的宏观矿物.
- 扩大已知的宏观生物的时间范围.
主要方法:
- 在拉布拉多南部进行实地勘探和地质测绘.
- 在Forteau形成的archaeocyathid珊瑚石灰岩中识别和分析痕迹化石 (钻孔).
主要成果:
- 许多归因于特里帕尼特的钻石在考古学的骨架和石灰岩中被鉴定出来.
- 这些钻石代表了迄今为止发现的最古老的宏观钻石,起源于下坎布里亚.
结论:
- 这一发现将已知的大型内石生物的记录推迟了大约1亿年.
- 自从坎布里亚早期以来,内石生物一直是珊瑚礁形成的组成部分,与硬骨动物的出现相吻合.
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