Department of Biology, University of Massachusetts, Amherst, MA, USA.
Integr Comp Biol. 2013 Aug;53(2):197-208. doi: 10.1093/icb/ict006. Epub 2013 Mar 22.
The origin of digit-bearing tetrapods in the Middle to Late Devonian (ca. 393-360 Mya) and their subsequent invasion of land represent a classic case of a major evolutionary radiation driven by new ecological opportunities. In this and other examples, exploration of new eco-space is hypothesized to correlate with functional innovation and adaptive divergence of phenotypes. Simultaneous changes in all morphofunctional systems are rare in major evolutionary transitions and may be non-existent. Here, we focus on the mandibles of early tetrapods and their kin as a model system to test whether shifts in functional innovation were coeval with some major events in tetrapod history. To this end, we quantified mechanical variation in the mandibles of tetrapodomorphs ranging in age from Early Devonian to earliest Permian. Biomechanical disparity is stable from the Devonian to the Early Pennsylvanian, even though the origin of weight-bearing, digited limbs, and the initial phases of the colonization of land occurred during this interval. An appreciable increase in functional variation is detected in the latest Pennsylvanian and earliest Permian, when stem and crown amniotes began to explore new regions of mechanical morphospace, a pattern partly attributable to the origin of herbivory. We find no difference in the rate of functional change between tetrapodomorph "fish" and early digited tetrapods, although two independent shifts are detected among Devonian stem tetrapods more crownward than Acanthostega. Instead, the most profound shifts in evolutionary rate are nested well within the tetrapod crown and are associated with amniotes (particularly diadectomorphs and some synapsids). The substantial temporal gap between the origin of postcranial features associated with terrestriality, such as limbs with functional elbow/knee and wrist/ankle joints capable of weight-bearing, and the onset of divergence in jaw biomechanics provides a compelling example of "functional modularity" during a major adaptive radiation.
中晚泥盆世(约 393-360 百万年前)出现带数字的四足动物起源及其随后向陆地的入侵代表了一个主要进化辐射的经典案例,这种辐射是由新的生态机会驱动的。在这个和其他例子中,探索新的生态空间被假设与表型的功能创新和适应性分化相关。在主要进化过渡中,所有形态功能系统的同时变化很少见,甚至可能不存在。在这里,我们专注于早期四足动物及其亲缘动物的下颚作为一个模型系统,以测试功能创新的转变是否与四足动物历史上的一些重大事件同时发生。为此,我们量化了从早泥盆世到最早二叠世年龄不等的四足形类动物下颚的力学变化。从泥盆纪到早宾夕法尼亚纪,生物力学差异是稳定的,尽管承重、有趾的四肢和陆地殖民的初始阶段都发生在这一时期。在最晚宾夕法尼亚纪和最早二叠纪,功能变异的显著增加被检测到,当时茎和冠羊膜动物开始探索机械形态空间的新区域,这种模式部分归因于草食性的起源。我们发现四足形类“鱼类”和早期有趾四足动物之间的功能变化率没有差异,尽管在比棘螈更向冠类的泥盆纪茎类四足动物中检测到了两个独立的转变。相反,进化率的最深刻转变嵌套在四足动物冠类内部,与羊膜动物(特别是合弓类和一些合踝类)有关。与陆地相关的后肢特征(如具有功能性肘/膝关节和能够承重的腕/踝关节)的起源与下颚生物力学差异的开始之间存在很大的时间差距,这为主要适应性辐射期间的“功能模块化”提供了一个令人信服的例子。