晚白时期的氨体表明,多样化的驱动因素在区域上是异质的
Joseph T Flannery-Sutherland1,2, Cameron D Crossan3, Corinne E Myers4
1School of Geography, Earth and Environmental Science, University of Birmingham, Birmingham, UK. j.t.flannerysutherland@bham.ac.uk.
Nature communications
|June 27, 2024
概括
全球生物多样性趋势在区域上是多样化的,而不是统一的. 氨类化石数据揭示了多样化的区域差异,挑战了它们在灭绝之前全球衰退的想法.
科学领域:
- 古生物学的古生物学
- 海洋生物学 海洋生物学
- 进化生物学 进化生物学
背景情况:
- 全球生物多样性趋势经常被假定,但化石记录显示区域异质性.
- 了解过去的多元化需要考虑空间和时间抽样偏差.
研究的目的:
- 分析不同地区的晚白时期氨体多样化动态.
- 调查区域起源和灭绝率及其驱动因素.
- 挑战全球氨菌生物数量下降的概念.
主要方法:
- 氨类化石记录的区域细分,以减轻空间采样偏差.
- 贝叶斯推断,以纠正时间采样偏差的区域起源和灭绝率.
- 对生物和非生物驱动因素的区域多样化率进行建模.
主要成果:
- 氨基体多样化和对多样性驱动因素的反应在区域上是异质的.
- 在白纪晚期,没有证据表明类动物在生态上普遍下降.
- 全球多元化模式受到区域抽样努力差异的重大影响.
结论:
- 过去的生物多样性信号是区域过程的马赛克,而不是全球趋势.
- 该研究质疑从空间偏差的化石记录中寻找全球多样性驱动因素的有效性.
- 在白纪-古纪的边界,氨类物种的灭绝并没有先于全球生态衰退.
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