埃迪亚卡拉人生活在陆地上
1Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403-1272, USA. gregr@uoregon.edu
Nature
|December 14, 2012
概括
在南澳大利亚古岩石中发现的埃迪亚卡拉化石表明它们是陆地生物,而不是海洋动物. 这些早期的生命形式很可能类似于凉爽干燥的环境中的土壤或.
科学领域:
- 古生物学的古生物学
- 地质地质地质地质地质地
- 环境科学 环境科学
背景情况:
- 埃迪亚卡拉 (635-542亿年前) 的化石一直被认为是早期动物祖先,海洋原生物或真菌.
- 以前的解释表明,埃迪亚卡拉层的湖-岩沉积.
研究的目的:
- 重新评估古老环境和埃迪亚卡拉化石的性质.
- 调查埃迪亚卡拉岩石的沉积环境,是罗恩斯利石英岩石的成员.
主要方法:
- 纪录古岩层和相关的沉积物特征.
- 对化石保存,土壤结构 (裂,结节) 和地质化学数据的分析.
- 基于土壤特征和同位素数据的古气候重建.
主要成果:
- 通过证据证实古岩的存在,例如非海洋面,土壤块和地化学差异化.
- 发现了埃迪亚卡的化石 (例如,Charniodiscus,Dickinsonia) 在古表面的生长位置上保存.
- 在南澳大利亚确定一个干燥,寒冷温和的埃迪亚卡拉古气候.
结论:
- 一些埃迪亚卡拉化石代表着生活在凉爽干燥的土壤上的大型式生物.
- 化石保存与生物土壤地 (,微生物殖民地) 一致,具有挑战性的海洋动物或原生体解释.
- 这一发现为早期的陆地生态系统和生命进化提供了新的视角.
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