相关实验视频
Updated: Jul 19, 2026

04:41
Dissection and Grading of Ovarian Development in Wild-Type Female Insects
Published on: July 14, 2023
恐龙的起与在纪-纪边界的异常有关
概括
大型热足类恐龙在特里亚斯纪-罗纪灭绝事件后迅速多样化,这可能是由一个巨星撞击造成的. 这一事件建立了由恐龙主导的生态系统,持续了1.35亿年.
科学领域:
- 古生物学的古生物学
- 地质地质地质地质地质地
- 恐龙古生物学 恐龙古生物学
背景情况:
- 三叠纪-罗纪 (T-J) 边界标志着一个重要的灭绝和动物周转时期.
- 了解恐龙出现的时间和驱动因素对于理解中生代生态系统至关重要.
研究的目的:
- 分析大型热足类恐龙出现和T-J大灭绝之间的时间关系.
- 调查潜在的外星撞击作为这种灭绝事件的原因.
主要方法:
- 来自北美70多个地区的四足动物足迹和骨材料的分析.
- 对异常进行地质化学分析.
- 帕林学分析 (子计数) 用于检测环境变化.
主要成果:
- 大型热足类恐龙出现在T-J边界<10,000年后,在最后的三叠纪类别之后<30,000年后.
- 这种快速的周转与陆地大规模灭绝,异常和胞峰相吻合.
- 恐龙的多样性稳定在100,000年后边界,建立恐龙的统治地位.
结论:
- 强烈建议一个波利德撞击是T-J大灭绝和随后的热足动物辐射的原因.
- T-J边界事件导致在北美东部建立了长期存在的恐龙主导的生态系统.
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