Late Triassic Metoposaurid Amphibian Skull Allometry: Comparison of the Lamy, New Mexico, Population to Four Other Populations

L. Rinehart, S. Lucas
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Abstract

Metoposaurs (Temnospondyli: Metoposauridae) were large, ubiquitous amphibians of the Late Triassic. They were important members of the Upper Triassic Chinle Group fauna of New Mexico and are found in these strata across the state. One of the most important metoposaur bonebeds in the world occurs in the Adamanian (upper Carnian) Garita Creek Formation near Lamy, NM, where the fossils of hundreds of individuals were hydraulically concentrated on a Late Triassic floodplain. In nearly all metoposaur populations, worldwide, many skull features show shape change throughout ontogenetic growth (allometry). Some workers have believed these allometric growth trajectories to be of taxonomic value. Here, using the largest populations available (for maximum statistical sample size), we investigate the taxonomic utility of these shape changes. Skull allometry in three populations of the metoposaur Koskinonodon perfectum (Lamy, NM; Rotten Hill, TX; Popo Agie Formation of WY) was compared to establish intra-specific variation. Then, three populations representing different genera ( Dutuitosaurus ouazzoui from northern Africa; Koskinonodon perfectum from western North America; Metoposaurus diagnosticus from eastern Europe) were compared to show variation at the generic level. Anteroposterior movement of the orbits and relative skull width at three positions (snout tip at the anterior nares, basal snout at the anterior orbits, greatest width across the quadratojugals) with respect to midline length throughout ontogeny were determined. Relative orbit position moved anteriorly in D. ouazzoui and K. perfectum (Rotten Hill), posteriorly in K. perfectum (Lamy) and K. perfectum (WY), and remained approximately fixed in M. diagnosticus . Skull width allometries were of mixed values, but with rare exceptions, the snout grew wider with respect to length throughout ontogeny, whereas the posterior skull became relatively narrower. Thus, the skulls of juveniles were somewhat triangular, and they grew to be more parallel-sided with a wider, blunter snout in adults. Comparison of the calculated allometric constants from the various populations yielded a surprising result: intra-specific variation in growth patterns was as great as or greater than inter-generic variation. The three K. perfectum populations, including the Lamy metoposaurs, were not significantly more similar to each other than they were to different genera. The salient point of this preliminary work is that allometric skull growth trajectories in metoposaurs probably have little or no taxonomic value, and metoposaur taxa should probably not be erected based solely on variations in growth patterns.
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晚三叠世甲龙类两栖动物颅骨异速测量:新墨西哥州拉米种群与其他四个种群的比较
背龙是生活在晚三叠世的大型、普遍存在的两栖动物。它们是新墨西哥州上三叠统Chinle群动物群的重要成员,在整个州的这些地层中都有发现。世界上最重要的甲龙骨床之一位于内华达州拉米附近的阿达曼尼亚(上卡尼亚)加里塔溪组,在那里的晚三叠世洪泛平原上发现了数百具甲龙化石。在全世界几乎所有的mettoposaur种群中,许多头骨特征在个体发育过程中显示出形状变化(异速生长)。一些工作者认为这些异速生长轨迹具有分类学价值。在这里,我们使用最大的种群(以获得最大的统计样本量)来研究这些形状变化的分类效用。完美龙(Koskinonodon perfectum, Lamy, NM;烂山,得克萨斯州;比较了WY的Popo Agie形成,建立了种内变异。然后是代表不同属的三个种群(来自北非的杜杜托龙;产于北美西部的完美Koskinonodon;对来自东欧的诊断型后鳞龙(Metoposaurus diagnosticus)进行了比较,以显示在属级水平上的差异。在个体发育过程中,眼眶的前后运动和三个位置的相对颅骨宽度(鼻尖在前鼻孔,基底鼻在前眼眶,穿过四方角的最大宽度)与中线长度的关系被确定。相对轨道位置在D. ouazzoui和K. perfectum (Rotten Hill)中向前移动,在K. perfectum (Lamy)和K. perfectum (WY)中向后移动,在M. diagnosticus中大致保持固定。颅骨宽度异速变化的值是混合的,但除了极少数例外,在个体发育过程中,鼻子相对于长度变宽,而后颅骨相对变窄。因此,幼年恐龙的头骨在某种程度上是三角形的,成年恐龙的头骨更平行,鼻子更宽、更钝。对不同居群计算的异速生长常数进行比较,得出了一个惊人的结果:种内生长模式的变异与属间变异一样大,甚至更大。包括拉米上鳞龙在内的三个完美龙居群之间的相似性并不比它们在不同属之间的相似性大得多。这项初步研究的重点在于,异速生长的头盖骨可能很少或根本没有分类学价值,不应该仅仅根据生长模式的变化来建立头盖骨分类群。
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