在古老生态时期灭绝的环境趋势
1Department of the Geophysical Sciences, University of Chicago, IL 60637, USA.
概括
古生代海洋群落在海上灭绝的增加,而单个属的灭绝在陆上更高. 这种模式反映了环境稳定影响不同种类的灭绝率.
科学领域:
- 古生物学的古生物学
- 海洋生态海洋生态学
- 在平流体学上,平流体学是平流体学.
背景情况:
- 灭绝模式对于理解海洋社区的动态和演变至关重要.
- 环境因素,如靠近岸边,可以显著影响物种的生存.
- 之前的研究表明,不同分类群体的灭绝敏感性各不相同.
研究的目的:
- 通过环境梯度,研究古世海洋组合中的灭绝强度模式.
- 为了确定社区层面的灭绝趋势是否与个人分类学类别的趋势有所不同.
- 为了将灭绝模式与环境的可预测性和稳定性相关联.
主要方法:
- 分析了505个古世海洋化石集团的灭绝强度.
- 集群的分类为六个不同的环境区和40个层级间隔.
- 在社区和分类阶级层面对灭绝率进行比较.
主要成果:
- 整个海洋社区表现出越来越多的灭绝率,离岸移动.
- 个别分类学类内的基因在近岸环境中表现出更高的灭绝率.
- 观察到的社区层面的趋势归因于近海地区的种群分布,其灭绝率较低.
结论:
- 环境稳定性在海洋灭绝动态中起着关键作用.
- 在可预测的稳定环境 (离岸) 中的生物体的灭绝率低于在波动的近岸环境中的生物体.
- 灭绝模式依赖于规模,在整个社区和个别分类群体之间存在差异.
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