Hoffman Devin K, Edwards Hunter R, Barrett Paul M, Nesbitt Sterling J
Department of Geosciences, Virginia Polytechnic Institute and State University (Virginia Tech), Blacksburg, VA, USA.
Department of Geological Sciences, University of Cape Town, Rondebosch, South Africa.
PeerJ. 2019 Nov 5;7:e7970. doi: 10.7717/peerj.7970. eCollection 2019.
Following the Permo-Triassic mass extinction, Archosauriformes-the clade that includes crocodylians, birds, and their extinct relatives outside crown Archosauria-rapidly diversified into many distinct lineages, became distributed globally, and, by the Late Triassic, filled a wide array of resource zones. Current scenarios of archosauriform evolution are ambiguous with respect to whether their taxonomic diversification in the Early-Middle Triassic coincided with the initial evolution of dietary specializations that were present by the Late Triassic or if their ecological disparity arose sometime after lineage diversification. Late Triassic archosauriform dietary specialization is recorded by morphological divergence from the plesiomorphic archosauriform tooth condition (laterally-compressed crowns with serrated carinae and a generally triangular lateral profile). Unfortunately, the roots of this diversification are poorly documented, with few known Early--Middle Triassic tooth assemblages, limiting characterizations of morphological diversity during this critical, early period in archosaur evolution. Recent fieldwork (2007-2017) in the Middle Triassic Manda Beds of the Ruhuhu Basin, Tanzania, recovered a tooth assemblage that provides a window into this poorly sampled interval. To investigate the taxonomic composition of that collection, we built a dataset of continuous quantitative and discrete morphological characters based on in situ teeth of known taxonomic status (e.g., , : = 65) and a sample of isolated teeth ( = 31). Using crown heights from known taxa to predict tooth base ratio (= base length/width), we created a quantitative morphospace for the tooth assemblage. The majority of isolated, unassigned teeth fall within a region of morphospace shared by several taxa from the Manda Beds (e.g., , ); two isolated teeth fall exclusively within a "" morphospace. A non-metric multidimensional scaling ordination ( = 67) of 11 binary characters reduced overlap between species. The majority of the isolated teeth from the Manda assemblage fall within the morphospace. This indicates these teeth are plesiomorphic for archosauriforms as exhibits the predicted plesiomorphic condition of archosauriform teeth. Our model shows that the conservative tooth morphologies of archosauriforms can be differentiated and assigned to species and/or genus, rendering the model useful for identifying isolated teeth. The large overlap in tooth shape among the species present and their overall similarity indicates that dietary specialization lagged behind species diversification in archosauriforms from the Manda Beds, a pattern predicted by Simpson's "adaptive zones" model. Although applied to a single geographic region, our methods offer a promising means to reconstruct ecological radiations and are readily transferable across a broad range of vertebrate taxa throughout Earth history.
二叠纪-三叠纪大灭绝之后,主龙形类(包括鳄形类、鸟类以及冠主龙类之外已灭绝的近亲的进化枝)迅速分化为许多不同的谱系,分布到全球各地,到三叠纪晚期,占据了各种各样的资源区。目前关于主龙形类进化的设想在以下方面并不明确:它们在三叠纪早中期的分类多样化是否与三叠纪晚期出现的食性特化的初始进化同时发生,或者它们的生态差异是否在谱系多样化之后的某个时间出现。三叠纪晚期主龙形类的食性特化通过与近祖主龙形类牙齿状况(侧面压缩的牙冠、有锯齿状的嵴以及大致呈三角形的侧面轮廓)的形态差异得以记录。不幸的是,这种多样化的根源记录很少,已知的三叠纪早中期牙齿组合很少,限制了对主龙类进化这一关键早期阶段形态多样性的描述。最近在坦桑尼亚鲁胡胡盆地中三叠统曼达组的野外工作(2007 - 2017年)发现了一个牙齿组合,为这个采样不足的时期提供了一个窗口。为了研究该组合的分类组成,我们基于已知分类地位的原位牙齿(例如, , := 65)和一组孤立牙齿样本( = 31)构建了一个连续定量和离散形态特征的数据集。利用已知分类单元的牙冠高度来预测牙根比率(=牙根长度/宽度),我们为牙齿组合创建了一个定量形态空间。大多数孤立的、未分配的牙齿落在曼达组几个分类单元共有的形态空间区域内(例如, , );两颗孤立牙齿完全落在一个“ ”形态空间内。对11个二元特征进行的非度量多维尺度排序( = 67)减少了物种之间的重叠。曼达组合中的大多数孤立牙齿落在 形态空间内。这表明这些牙齿是主龙形类的近祖形态,因为 呈现出主龙形类牙齿预测的近祖状态。我们的模型表明,主龙形类保守的牙齿形态可以被区分并归为物种和/或属,使得该模型可用于识别孤立牙齿。现存物种之间牙齿形状的大量重叠以及它们的总体相似性表明,来自曼达组的主龙形类的食性特化落后于物种多样化,这是辛普森“适应区”模型预测的一种模式。尽管应用于单个地理区域,但我们的方法提供了一种重建生态辐射的有前景的手段,并且很容易在地球历史上广泛的脊椎动物分类群中转移应用。