Quantitative Models for Distinguishing Punctuated and Continuous-Time Models of Character Evolution and Their Implications for Macroevolutionary Theory

April M Wright, Peter J. Wagner
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Abstract

The recent proliferation of quantitative models for assessing anatomical character evolution all assume that character change happens continuously through time. However, punctuated equilibrium model posits that character change should be coincide with cladogenetic events, and thus should be tied to origination rates. Rates of cladogenesis are important to quantitative phylogenetics, but typically only for establishing prior probabilities of phylogenetic topologies. Here, we modify existing character likelihood models to use the local cladogenesis rates from Bayesian analyses to generate the amounts of character change over time dependent on origination rates, as expected under the punctuated equilibrium model. In the case of strophomenoid brachiopods strop from the Ordovician, we find that Bayesian analyses strongly favor punctuated models over continuous-time models, with elevated rates of cladogenesis early in the clade's history inducing frequencies of change despite constant rates of change per speciation event. This corroborates prior work proposing that the early burst in strophomenoid disparity reflects simply elevated speciation rates, which in turn has implications for seemingly unrelated macroevolutionary theory about whether early bursts reflect shifts in intrinsic constraints or empty ecospace. Future development of punctuated character evolution models should account for the full durations of species, which will provide a test of continuous change rates. Ultimately, continuous change vs. punctuated change should become part of phylogenetic paleobiology in the same way that other tests of character evolution currently are.
区分特征进化的定时模型和连续时间模型的定量模型及其对宏观进化理论的影响
近年来,用于评估解剖特征进化的定量模型层出不穷,这些模型都假定特征变化是随着时间的推移而不断发生的。然而,点状平衡模型认为,特征变化应与支系发生事件相吻合,因此应与起源率挂钩。支系发生率对定量系统发生学非常重要,但通常只用于确定系统发生拓扑的先验概率。在这里,我们修改了现有的特征似然模型,利用贝叶斯分析得出的局部谱系发生率来产生随时间变化的特征变化量,这种变化量取决于起源率,正如在点状平衡模型下所预期的那样。以奥陶纪的腕足动物栉水母纲为例,我们发现贝叶斯分析结果强烈倾向于点状模型而非连续时间模型,尽管每次物种分化的变化率不变,但在该支系历史的早期,克隆发生率的升高会诱发变化的频率。这印证了之前的研究,即石龙子差异的早期爆发仅仅反映了物种分化率的升高,这反过来又对看似无关的宏观进化理论产生了影响,即早期爆发是反映了内在约束的变化还是反映了空旷的生态空间。点状特征进化模型的未来发展应该考虑物种的全部持续时间,这将为连续变化率提供一个检验标准。最终,连续变化与点状变化应该像目前对特征进化的其他检验一样,成为系统发育古生物学的一部分。
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