来自新墨西哥州的特里亚斯纪晚期恐龙形组合和恐龙的兴起
Randall B Irmis1, Sterling J Nesbitt, Kevin Padian
1Museum of Paleontology and Department of Integrative Biology, University of California, Berkeley, CA 94720-4780, USA. irmis@berkeley.edu
概括
从古老的特里亚斯纪晚期动物到早期恐龙的过渡是渐进的,而不是突然的灭绝. 化石表明这种恐龙多样化需要1500万到200万年的时间,并因地区而异.
科学领域:
- 古生物学的古生物学
- 在平流体学上,平流体学是平流体学.
- 进化生物学 进化生物学
背景情况:
- 主流理论认为,早期恐龙通过竞争性排斥或突然灭绝事件迅速取代了古老的三亚纪晚期动物.
- 来自上三叠纪形形成的化石证据为重新评估这一过渡提供了机会.
研究的目的:
- 为了研究三纪晚期动物过渡的性质,特别是恐龙的兴起.
- 为了确定古老的动物被恐龙所取代是突然的还是渐进的.
主要方法:
- 来自新墨西哥州上季亚纪金尔形成的海登采石场的化石组合的分析.
- 区域上三叠纪化石集团的比较分析.
主要成果:
- 来自海登采石场和周围的尔形成的化石表明逐渐的过渡,而不是快速的替代.
- 在Chinle组合中发现的恐龙亲属代表了以前仅从北美以外的旧层中知道的群体.
- 恐龙的兴起可能已经跨越了15到2000万年.
结论:
- 恐龙的兴起和古老的特里亚斯纪晚期动物群的衰退是一个漫长而渐进的过程.
- 这种过渡很可能是双时的,在各种古度的不同时间发生.
- 这些发现挑战了长期以来关于在特里亚斯纪末期恐龙迅速接管的观点.
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