School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK.
Proc Biol Sci. 2018 Feb 14;285(1872). doi: 10.1098/rspb.2017.2730.
The Carboniferous and early Permian were critical intervals in the diversification of early four-limbed vertebrates (tetrapods), yet the major patterns of diversity and biogeography during this time remain unresolved. Previous estimates suggest that global tetrapod diversity rose continuously across this interval and that habitat fragmentation following the 'Carboniferous rainforest collapse' (CRC) drove increased endemism among communities. However, previous work failed to adequately account for spatial and temporal biases in sampling. Here, we reassess early tetrapod diversity and biogeography with a new global species-level dataset using sampling standardization and network biogeography methods. Our results support a tight relationship between observed richness and sampling, particularly during the Carboniferous. We found that subsampled species richness initially increased into the late Carboniferous, then decreased substantially across the Carboniferous/Permian boundary before slowly recovering in the early Permian. Our analysis of biogeography does not support the hypothesis that the CRC drove endemism; instead, we found evidence for increased cosmopolitanism in the early Permian. While a changing environment may have played a role in reducing diversity in the earliest Permian, our results suggest that the CRC was followed by increased global connectivity between communities, possibly reflecting both reduced barriers to dispersal and the diversification of amniotes.
石炭纪和早二叠世是早期四足脊椎动物(四足动物)多样化的关键时期,但这一时期多样性和生物地理学的主要模式仍未解决。先前的估计表明,全球四足动物的多样性在此期间持续上升,而“石炭纪雨林崩塌”(CRC)后栖息地的破碎化导致了群落之间特有性的增加。然而,以前的工作未能充分考虑到采样的空间和时间偏差。在这里,我们使用新的全球种级数据集,通过采样标准化和网络生物地理学方法,重新评估早期四足动物的多样性和生物地理学。我们的结果支持观察到的丰富度与采样之间的紧密关系,特别是在石炭纪期间。我们发现,经过抽样的物种丰富度最初在石炭纪晚期增加,然后在石炭纪/二叠纪边界大幅下降,然后在早二叠世缓慢恢复。我们对生物地理学的分析不支持 CRC 驱动特有性的假设;相反,我们发现早二叠世有更多的世界性现象的证据。虽然不断变化的环境可能在最早的二叠纪降低了多样性,但我们的结果表明,CRC 之后,群落之间的全球连通性增加,这可能反映了扩散障碍的减少和羊膜动物的多样化。