在全球海洋多样性中的生物转变
1Department of Geology, University of Cincinnati, OH 45221-0013, USA. arnold.miller@uc.edu
概括
在法内罗纪时期,海洋生物组成的变化是由物理干扰驱动的,而不仅仅是生物相互作用或大规模灭绝. 宏观进化过程在整个地质时间尺度上始终保持一致.
科学领域:
- 古生物学的古生物学
- 海洋生物学 海洋生物学
- 地球科学 地球科学 地球科学
背景情况:
- 长期的海洋生物组成的变化在Phanerozoic被归因于生物相互作用或大规模灭绝.
- 以前的模型提出了背景多样性变化与大规模灭绝事件的独特机制.
研究的目的:
- 为了调查长期海洋生物群过渡的潜在驱动因素在整个Phanerozoic.
- 调和生物相互作用,大规模灭绝和物理扰乱在塑造海洋生物多样性的作用.
主要方法:
- 分析跨不同时间尺度的宏观进化过程,包括背景和大规模灭绝时期.
- 检查各种地理尺度影响生物成分的物理扰动的证据.
主要成果:
- 在非灭绝时期的宏观进化过程与大规模灭绝期间的过程没有根本的不同.
- 跨多个尺度的物理扰动是决定法内罗纪多样性的长期轨迹的关键因素.
- 仅仅生物相互作用和大规模灭绝并不能完全解释长期生物多样性模式.
结论:
- 海洋生物长期演变是综合过程的产物,其中物理干扰起着至关重要的作用.
- 对宏观进化动态的统一观点,包括背景和灭绝事件,得到了新证据的支持.
- 了解罗纪的多样性需要考虑物理力量和生物反应在地质时间的相互作用.
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