Apparent timescaling of fossil diversification rates is caused by sampling bias

Bouwe Rutger Reijenga, Roger Adam Close
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Abstract

Negative scaling relationships between both speciation and extinction rates on the one hand, and the age or duration of organismal groups on the other, are pervasive and recovered in both molecular phylogenetic and fossil time series. The consistency between molecular and fossil data hints at a universal cause, and potentially to incongruence between micro- and macroevolution. However, the existence of negative rate scaling in fossil time series has not undergone the same level of scrutiny as in molecular data. Here, we analyse the marine fossil record across the last ~535 Ma of the Phanerozoic to investigate the presence and strength of negative rate scaling. We find that negative rate scaling arises under commonly applied age range-based per-capita rates, which do not control for sampling bias, but are severely reduced or absent when metrics are used that do correct for sampling. We further show by simulation that even moderate incomplete sampling of species occurrences through time may induce rate scaling. We thus conclude that there are no significant scaling relationships present in these fossil clades, and that any apparent trend is caused by taxonomic practices and sampling artefacts. If rate scaling appears genuinely in molecular phylogenies, the absence of such a relationship in the fossil record will provide a valuable benchmark and constraint on what processes can cause it.
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化石多样化率的表面时间尺度是由取样偏差造成的
在分子系统发育和化石时间序列中,物种演化率和灭绝率与生物群体的年龄或持续时间之间普遍存在负比例关系。分子数据和化石数据之间的一致性暗示了一个普遍的原因,也可能暗示了微观进化和宏观进化之间的不一致性。然而,化石时间序列中存在的负速率缩放现象并没有像分子数据那样受到严格的审查。在这里,我们分析了新生代最后约 535 Ma 的海洋化石记录,以研究负速率缩放的存在和强度。我们发现,在通常应用的基于年龄范围的人均比率下,会出现负比率缩放,而这种比率并不控制采样偏差,但在使用校正采样的指标时,负比率缩放就会严重减少或消失。我们还通过模拟进一步证明,即使对物种出现的时间进行适度的不完全采样,也可能导致比率缩放。因此,我们得出结论,这些化石支系中并不存在显著的比例关系,任何明显的趋势都是由分类学实践和取样误差造成的。如果分子系统发生学中真的出现了速率缩放关系,那么化石记录中没有这种关系将提供一个有价值的基准,并对可能导致这种关系的过程加以限制。
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