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在古热带地区的陆地末纪大灭绝是海上灭绝之后的
Qiong Wu1,2, Hua Zhang3, Jahandar Ramezani4
1Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China.
Science advances
|January 31, 2024
概括
波斯纪末期的大规模灭绝.
科学领域:
- 古生物学的古生物学
- 地质时间学 (Geochronology)
- 气候科学 气候科学
背景情况:
- 波斯末期的大规模灭绝是最严重的Phanerozoic事件.
- 据推测,它在海洋和陆地生态系统中同时发生.
- 西伯利亚陷大火山区是可疑的触发因素.
研究的目的:
- 为了准确地确定卡泰西亚雨林的崩的日期.
- 调查陆地末波斯纪灭绝的时间和地理进展.
- 探索灭绝模式与环境变化之间的关系.
主要方法:
- 使用化学磨损-同位素稀释-热电离质谱的高精度体U-Pb地质年代学.
- 分析中国西南地区从陆地到过渡性沿海环境的.
- 与同期继承的高分辨率地质年代学集成.
主要成果:
- 卡泰西亚热带雨林的崩始于波斯末期海洋灭绝开始后.
- 陆地上的灭绝与度发生的时间是对称的,从高度开始,向热带发展.
- 这次灭绝事件持续了大约100万年.
结论:
- 在地球上,二叠纪末期的陆地灭绝并非在全球范围内同时发生.
- 灭绝的度年龄梯度表明了不同的环境影响,可能与表面变暖有关.
- 较高的度经历了更恶化的条件,导致更高的灭绝率.
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