概括
三纪末期发生了多次撞击,意大利页岩床中发现的冲击石英颗粒证明了这一点. 这些影响与Rhaetavicula动物群的灭绝相吻合.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 行星科学 行星科学
背景情况:
- 特里亚斯纪末期的灭绝事件是一个重大的大规模灭绝事件.
- 了解这种灭绝的触发因素对于古气候和古环境重建至关重要.
研究的目的:
- 为了调查三叠纪 - 罗纪边界的潜在撞击事件.
- 为了分析意大利地质形成中的冲击石英.
主要方法:
- 用显微镜检查石英颗粒的平面变形特征.
- 在北方阿宁山脉的页岩床的平流图分析.
- 对冲石英的石岩学分析.
主要成果:
- 在三个不同的页岩层中发现的冲击变形石英颗粒.
- 在5-10%的石英颗粒中观察到平面变形特征.
- 冲击石英层的平流图位置与Rhaetavicula动植物终点相关.
结论:
- 有证据表明,在特里亚斯纪末期,至少有三次紧密相距的撞击事件发生.
- 这些影响可能导致了三叠纪-罗纪边界的环境变化.
- 需要进一步的研究来确认外星人的起源和撞击的精确时间.
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