在埃迪亚卡拉 - 坎布里亚过渡时期,有机壁微化石的形态持续变化
Kelly E Tingle1, Ross P Anderson2,3, Neil P Kelley1
1Department of Earth and Environmental Sciences, Vanderbilt University, Nashville, TN, USA.
Royal Society open science
|June 12, 2025
概括
欧核生物的进化受到了埃迪亚卡兰时期环境变化的影响. 微化石分析揭示了与舒拉姆游览和浮游生物真核生物的兴起相关的大小和形态的变化.
科学领域:
- 古生物学的古生物学
- 地质生物学 地质生物学
- 进化生物学 进化生物学
背景情况:
- 早期的真核生物进化是由Proterozoic Eon期间显著的环境转变所塑造的.
- 这些扰动可能影响了坎布里亚爆炸之前的原生态生物圈和地球系统.
- 了解真核生物对这些事件的反应,可以在关键的进化阶段了解地层-生物圈联系.
研究的目的:
- 分析整个埃迪亚卡拉 - 坎布里亚过渡时期有机壁的微化石大小和形态.
- 为了研究"舒拉姆"碳同位素外流对微化石特征的影响.
- 重建微生物真核生物对环境变化的进化反应.
主要方法:
- 对有机壁微化石大小 (囊泡直径) 和形态学的分析.
- 在微化石中对相对过程长度的量化.
- 检查与"舒拉姆"碳同位素外游有关的形态变化.
主要成果:
- 微化石囊直径的减少始于埃迪亚卡兰,在"舒拉姆"游览之后.
- 在整个埃迪亚卡-坎布里亚过渡时期观察到相对过程长度的增加.
- 在"Shuram"游览后,整个微化石形态的持续转变发生了.
结论:
- "舒拉姆"游览标志着微化石形态学的转折点,开始了尺寸缩小和形态变化.
- 环境变化和营养压力可能推动了这些形态适应.
- 微生物真核生物向浮游生物生活方式的扩张是建立现代海洋食物网的关键一步.
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