新的罗纪早期四足动物组合约束了罗纪-罗纪四足动物灭绝事件
概括
最早的罗纪四足动物化石组合揭示了大多数罗纪-罗纪灭绝发生在赫塔尼亚时代之前. 这种模式表明,在特里亚斯纪-罗纪边界发生了全球灭绝事件,可能与马尼库阿根撞击有关.
科学领域:
- 古生物学的古生物学
- 地质时间学 (Geochronology)
- 灭绝事件研究 灭绝事件研究
背景情况:
- 三亚纪-罗纪灭绝事件标志着一个重要的生物周转.
- 以前的研究表明,在罗纪-罗纪边界发生了全球灭绝.
- 四足动物灭绝的确切时间和持续时间仍在争论中.
研究的目的:
- 重新评估三叠纪-罗纪四足动物灭绝事件的持续时间.
- 为了确定Fundy盆地最早的罗纪四足动物组合的精确年龄.
- 为了调查四足动物家族消失和引入的模式,跨越了三叠纪-罗纪的边界.
主要方法:
- 确定相关的最早的拉纪四足动物组合的发现和分析.
- 使用花粉和子的平流图相关性.
- 化石集合的放射测量和地化学测年.
- 动物构成与特里亚斯纪晚期和罗纪纪录的比较分析.
主要成果:
- 芬迪盆地组合代表了一个早期的赫坦格纪 (最早的罗纪) 时代.
- 该组合包括多种多样的四足动物:类似哺乳动物的爬行动物,恐龙,鱼类,虫类和鱼类.
- 所有构成家族都是从早期的地层中知道的,在这个最早的罗纪组合中没有新家族出现.
- 典型的三叠纪形式不存在,这表明灭绝发生在早期赫坦格纪之前.
结论:
- 大多数特里亚斯纪-罗纪四足动物的灭绝发生在赫坦格纪早期之前,没有引入新的家族.
- 这种模式支持在罗纪-罗纪边界发生的全球灭绝事件,与海洋无脊椎动物研究一致.
- 马尼库阿根撞击事件,大致可以追溯到三叠纪-罗纪边界,是灭绝的潜在因果因素.
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