揭示了整个罗纪海洋生物多样性的驱动因素
Alexis Balembois1, Alexandre Pohl2, Bertrand Lefebvre3
1Univ. Littoral Côte d'Opale, CNRS, Univ. Lille, UMR 8187 LOG, Wimereux, France. alexis.balembois@univ-littoral.fr.
Nature communications
|September 26, 2025
概括
超过5.41亿年的海洋生物多样性模式是由利基环境相互作用和气候所塑造的. 然而,古地理学,包括陆地结构和浅水区域,是生物多样性长期变化的基本驱动因素.
科学领域:
- 古生物学的古生物学
- 生物地理学 生物地理学 生物地理学
- 宏观生态学 宏观生态学
背景情况:
- 了解空间时间生物多样性模式在生物地理学和古生物学中至关重要.
- 现有30多个假设,但尚未就像度生物多样性梯度这样的主要驱动因素达成共识.
研究的目的:
- 为了调查全球海洋生物多样性变化和法内罗纪时代空间模式的驱动因素.
- 测试利基环境相互作用和古地理演变的作用.
主要方法:
- 将宏观生态模型与全球气候模拟相结合.
- 分析了过去5.41亿年的海洋生物多样性模式 (Phanerozoic).
主要成果:
- 利基环境相互作用通过设定承载能力和空间限制,定义度梯度来影响海洋生物多样性.
- 气候调节了这些相互作用,但古地理演变 (例如,浅水区,大陆构造) 是长期生物多样性趋势的基本驱动因素.
结论:
- 多种相互作用机制,包括利基环境相互作用和古地理学,平衡以推动海洋生物多样性轨迹.
- 古地理进化在地质时间尺度上塑造大规模海洋生物多样性模式方面发挥了关键作用.
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