在白纪 - 古纪边界周围发生的关键事件的时间尺度
Paul R Renne1, Alan L Deino, Frederik J Hilgen
1Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA. prenne@bgc.org
概括
奇克苏鲁布撞击与白纪-古世大规模灭绝相吻合,引发了快速的生态系统转变. 有证据表明,大气中的碳循环在不到5000年内恢复,比海洋盆地快得多.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 地球科学 地球科学 地球科学
背景情况:
- 大量灭绝代表了地球历史上关键的进化转折点.
- 甲纪 - 古世 (K-Pg) 边界标志着生物周转的一个重要时期.
- 奇克苏鲁布玻利德撞击是K-Pg大灭绝事件的主要假设.
研究的目的:
- 为了确定奇克苏鲁布撞击和K-Pg大灭绝事件之间的时间同步.
- 调查大气碳循环扰乱的持续时间和恢复时间.
- 评估撞击事件后哺乳动物动物的持续性.
主要方法:
- 使用阿贡-阿贡 ((40) Ar / ((39) Ar) 地质年代测定.
- 分析与白纪 - 古纪边界相关的地质层.
- 检查西威利斯顿盆地哺乳动物动物的化石记录.
主要成果:
- 奇克苏鲁布撞击和K-Pg大灭绝之间的同步是在32,000年内确立的.
- 大气碳循环的扰动持续不到5000年,并迅速恢复.
- 低多样性的哺乳动物群在撞击后持续了大约2万年.
结论:
- 奇克苏鲁布撞击可能引发了关键的生态系统状态转变.
- 碳循环的快速恢复表明,弹性机制被压倒了.
- K-Pg大灭绝与奇克苏鲁布撞击密切相关,具有深刻的生物后果.
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