坎布里亚辐射物种化事件是由海平面和西伯利亚克拉顿的氧化回归变化驱动的
Andrey Yu Zhuravlev1, Rachel A Wood2, Fred T Bowyer2
1Department of Biological Evolution, Faculty of Biology, Lomonosov Moscow State University Leninskie Gory 1(12), Moscow 119234, Russia.
Science advances
|June 16, 2023
概括
坎布里亚时代的物种化是由海平面变化所带来的本土化和分散的增加所驱动的. 这些事件表明浅层海洋氧气扩张是坎布里亚辐射期间的关键进化驱动因素.
科学领域:
- 古生物学的古生物学
- 进化生物学 进化生物学
- 地质地质地质地质地质地
背景情况:
- 在坎布里亚辐射期间快速物种化的驱动因素尚未完全理解.
- 海洋氧化事件等潜在的外部因素需要进一步调查.
研究的目的:
- 为了研究在早期坎布里亚时期在西伯利亚地上考古生物海绵物种的时间和空间分布.
- 为了确定在此期间物种化事件的驱动因素.
主要方法:
- 化石分布的高分辨率分析.
- 变种事件与古海洋学条件的相关性.
主要成果:
- 品种形成的特点是,在521万年前到51450万年前,本地特有性增加.
- 这些物种化事件跟随着祖先物种的分散.
- 种类形成与主要的海平面低位相吻合.
结论:
- 海平面的振荡可能导致浅层海洋氧气扩张.
- 这种氧气扩张创造了分散走廊,并促进了新的社区形成.
- 海洋氧化,由海平面变化驱动,在坎布里亚辐射期间作为物种形成的进化驱动因素.
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