MacLaren Jamie A, Anderson Philip S L, Barrett Paul M, Rayfield Emily J
Department of Biology , Universiteit Antwerpen , Campus Drie Eiken , Universiteitsplein , Wilrijk , Antwerp , 2610 , Belgium.
Department of Animal Biology , University of Illinois at Urbana-Champaign , 515 Morrill Hall , 505 S. Goodwin Ave. , Urbana , Illinois 61801 , U.S.A.
Paleobiology. 2017 Feb;43(1):15-33. doi: 10.1017/pab.2016.31. Epub 2016 Dec 15.
Morphological responses of nonmammalian herbivores to external ecological drivers have not been quantified over extended timescales. Herbivorous nonavian dinosaurs are an ideal group to test for such responses, because they dominated terrestrial ecosystems for more than 155 Myr and included the largest herbivores that ever existed. The radiation of dinosaurs was punctuated by several ecologically important events, including extinctions at the Triassic/Jurassic (Tr/J) and Jurassic/Cretaceous (J/K) boundaries, the decline of cycadophytes, and the origin of angiosperms, all of which may have had profound consequences for herbivore communities. Here we present the first analysis of morphological and biomechanical disparity for sauropodomorph and ornithischian dinosaurs in order to investigate patterns of jaw shape and function through time. We find that morphological and biomechanical mandibular disparity are decoupled: mandibular shape disparity follows taxonomic diversity, with a steady increase through the Mesozoic. By contrast, biomechanical disparity builds to a peak in the Late Jurassic that corresponds to increased functional variation among sauropods. The reduction in biomechanical disparity following this peak coincides with the J/K extinction, the associated loss of sauropod and stegosaur diversity, and the decline of cycadophytes. We find no specific correspondence between biomechanical disparity and the proliferation of angiosperms. Continual ecological and functional replacement of pre-existing taxa accounts for disparity patterns through much of the Cretaceous, with the exception of several unique groups, such as psittacosaurids that are never replaced in their biomechanical or morphological profiles.
非哺乳动物食草动物对外部生态驱动因素的形态学响应尚未在较长时间尺度上进行量化。食草性非鸟类恐龙是测试此类响应的理想群体,因为它们在陆地生态系统中占据主导地位超过1.55亿年,并且包括有史以来最大的食草动物。恐龙的辐射被几个具有重要生态意义的事件打断,包括三叠纪/侏罗纪(Tr/J)和侏罗纪/白垩纪(J/K)边界的灭绝、苏铁类植物的衰退以及被子植物的起源,所有这些都可能对食草动物群落产生深远影响。在这里,我们首次对蜥脚形亚目和鸟臀目恐龙的形态学和生物力学差异进行分析,以研究颌骨形状和功能随时间的变化模式。我们发现形态学和生物力学下颌差异是脱钩的:下颌形状差异遵循分类学多样性,在中生代稳步增加。相比之下,生物力学差异在晚侏罗世达到峰值,这与蜥脚类恐龙功能变异的增加相对应。这个峰值之后生物力学差异的减少与J/K灭绝、相关的蜥脚类恐龙和剑龙多样性的丧失以及苏铁类植物的衰退相吻合。我们没有发现生物力学差异与被子植物增殖之间的特定对应关系。在白垩纪的大部分时间里,现存类群的持续生态和功能替代解释了差异模式,但有几个独特的类群除外,比如鹦鹉嘴龙科,它们在生物力学或形态学特征上从未被替代。