泛热纪地球系统演化和海洋生物多样性
Bjarte Hannisdal1, Shanan E Peters
1Department of Earth Science, Centre for Geobiology, University of Bergen, Allégaten 41, Bergen, Norway. bjarte.hannisdal@geo.uib.no
概括
化石海洋动物的多样性跟踪沉积岩,但这种共变性不仅仅是采样偏差. 地球系统的相互作用,包括大陆洪水和海洋化学,驱动生物多样性模式独立于岩石数量.
科学领域:
- 古生物学的古生物学
- 地质地质地质地质地质地
- 宏观进化是如何发生的
背景情况:
- 化石记录中的海洋动物多样性似乎与海洋沉积岩的丰富性有关.
- 这种相关性反映了地质采样偏差的程度尚不清楚.
研究的目的:
- 调查海洋动物多样性模式是否受到地质采样偏差之外的因素的影响.
- 探索地球系统过程与法内罗纪海洋生物多样性之间的关系.
主要方法:
- 对海水化学和大陆洪水的Phanerozoic记录的分析.
- 统计检查环境变量与化石多样性数据之间的共变量.
- 在地质,化学和生物数据集之间的长期相互作用的审问.
主要成果:
- 海洋动物多样性数据包含了独立于沉积岩量和采样的信息.
- 他们确定了大陆洪水,硫和碳循环以及宏观进化之间的长期相互作用.
- 相互作用的地球系统中的相互反应,而不是采样偏差,解释了观察到的大部分协同变量.
结论:
- 泛热纪沉积和化石生物多样性的模式主要是由相互作用的地球系统驱动的.
- 生物多样性的变化与反映生物对海洋氧化还原条件和海平面波动的生物反应的环境记录有关.
- 板块构造驱动的海平面变化和海洋化学变化是宏观进化模式的关键驱动因素.
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