在白纪末期大规模灭绝的零点处迅速恢复生命
Christopher M Lowery1, Timothy J Bralower2, Jeremy D Owens3
1Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA. cmlowery@utexas.edu.
Nature
|June 1, 2018
概括
在白纪/古纪大灭绝后,海洋生态系统的恢复在奇克苏鲁布撞击坑附近迅速. 这表明生态因素,而不是与影响相关的环境控制,推动了初级生产率的恢复.
科学领域:
- 古生物学的古生物学
- 海洋生态海洋生态学
- 地质化学 地质化学
背景情况:
- 由奇克苏鲁布小行星撞击引发的白纪/古纪大灭绝事件造成了海洋物种的大量丧失.
- 通过初级生产力来衡量灭绝后的海洋生态系统恢复,表现出地理异质性,在墨西哥湾等地区观察到的恢复速度较慢.
研究的目的:
- 为了调查接近奇克苏鲁布撞击坑是否延迟了海洋生态系统的恢复.
- 为了确定与影响相关的环境因素是否控制了灭绝后的恢复率.
- 了解生态过程在恢复海洋生产力的作用.
主要方法:
- 从奇克苏鲁布火山口内对类植物和石灰质的纳米浮游生物进行分析.
- 对痕迹化石和元素丰度数据的检查.
- 样品的约会时间为古世时期的前20万年.
主要成果:
- 撞击后几年内,奇克苏鲁布盆地的海洋生物重新出现.
- 一个高生产率的生态系统是在3万年内建立的.
- 接近撞击坑的回收率并不慢,反驳了与撞击有关的环境控制.
结论:
- 靠近奇克苏鲁布撞击并没有延迟海洋生态系统的恢复.
- 生态因素,如热带相互作用和竞争排斥,可能会治理恢复.
- 这些发现对预测人类干扰生态系统的恢复模式有影响.
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