在白纪 - 古纪边界的德坎火山运动的状态转移,可能是由撞击引起的
Paul R Renne1, Courtney J Sprain2, Mark A Richards3
1Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA. Department of Earth and Planetary Science, University of California-Berkeley, Berkeley, CA 94720, USA. prenne@bgc.org.
概括
纪末期的大规模灭绝可能与石撞击和Deccan Traps洪水火山活动有关. 新的数据表明德坎陷
科学领域:
- 地质科学
- 古生物学
- 地质化学
背景情况:
- 末纪大灭绝被归因于两个主要假设:石撞击和洪水火山活动.
- 德坎陷是一个巨大的火山区,
- 了解这些事件之间的相互作用对于理解灭绝模式至关重要.
研究的目的:
- 调查奇克苏鲁布石撞击与德坎陷洪水火山之间的时间关系.
- 确定这两个主要的地质事件是否有遗传联系,并影响了末纪大灭绝.
- 评估火山活动对灭绝后生态系统恢复的影响.
主要方法:
- 使用高精度 (40) Ar / (39) Ar 地质年代学来测定Deccan Traps火山岩的年代.
- 用地化学分析来描述岩系统.
- 高精度年龄数据与奇克苏鲁布撞击事件的时间相关.
主要成果:
- 高精度 (40) Ar/(39) Ar数据显示了Deccan Traps岩系统的状态转变.
- 这种状态的转变大约与奇克苏鲁布撞击和末纪大灭绝相吻合.
- 大约70%的Deccan陷在撞击后的5万年内发生了更大规模和更频繁的喷发.
结论:
- 德坎陷的洪水火山活动和奇克苏鲁布撞击事件可能是遗传相关的.
- 撞击可能引发了Deccan Traps岩系统的重大变化,导致火山活动加速.
- 海洋生态系统的恢复可能会持续到火山活动加速衰退.
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