A Possible New Species of Dimetrodon (Eupelycosauria: Sphenacodontidae) from the Lower Permian Abo Formation, Socorro County, New Mexico

Kenneth L. Mckeighen, Kendra R. McKeighen, H. W. Mckeighen, S. Lucas
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Abstract

We add to the growing record of Dimetrodon fossils from the Lower Permian Abo Formation in New Mexico with the addition of a potential new species from the Gallina Well locality in Socorro County that previously yielded other material of Dimetrodon in 2010. During a visit to the site in 2014, one of us (KLM Jr.) collected a large vertebra and associated fragments including a 15 cm long neural spine. The neural spine morphology of this specimen is of the more primitive round cross section, most similar to Dimetrodon milleri , the oldest known Dimetrodon from Texas. A significant difference is larger size being at least 50% larger than D. milleri . We also see a temporal difference with the Gallina Well Dimetrodon being late Asselian or early Sakmarian in age and D. milleri being younger in the Sakmarian. The Discovery of this specimen raises several important questions. The first relates to size of early Dimetrodon species. Until the discovery of this specimen all known early Dimetrodon were small. Indeed, all early species, cf. D. milleri from the middle Asselian of New Mexico, D. occidentalis from the upper Asselian of New Mexico, and D. milleri from the Sakmarian of Texas, are all small species. This was thought advantageous to life in an inland and upland habitat, and that larger size arose to take advantage of deltaic habitats. The new species from Gallina Well demonstrates that larger size arose much earlier than previous thought. The diversity of Dimetrodon is also in question with regard to how many species were there in New Mexico deposits. The new Gallina Well Dimetrodon suggest the presence of two contemporaneous species in the Abo Formation. Research since 2009 has revealed Dimetrodon to be a more common, though not the dominant predator, on the Abo floodplains of Permian New Mexico. Much more research is needed to fully understand Dimetrodon from the Lower Permian of New Mexico.
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新墨西哥州索科罗县下二叠世Abo组一可能的双齿龙新种(真齿纲:齿龙科)
我们在新墨西哥州的下二叠世Abo组发现了越来越多的异齿龙化石,并在2010年从索科罗县的加里纳井地区发现了一个潜在的新物种,该物种之前曾发现过其他异齿龙的材料。在2014年的一次现场考察中,我们中的一位(KLM Jr.)收集了一大块椎骨和相关碎片,其中包括一根15厘米长的神经脊柱。这个标本的神经脊柱形态是更原始的圆形截面,最类似于Dimetrodon milleri,这是德克萨斯州已知最古老的Dimetrodon。一个显著的差异是更大的尺寸至少大于50%的d.m iller。我们也看到了时间上的差异,Gallina井Dimetrodon在年龄上是亚塞利亚晚期或早期萨克马里安,而D. milleri在萨克马里安更年轻。这个标本的发现提出了几个重要的问题。第一个与早期双齿龙物种的大小有关。在发现这个标本之前,所有已知的早期异齿龙都很小。事实上,所有早期物种,如新墨西哥州亚塞利亚中部的D. milleri,新墨西哥州亚塞利亚北部的D. occidentalis,以及德克萨斯州萨克马里安的D. milleri,都是小物种。这被认为有利于内陆和高地栖息地的生命,而更大的尺寸出现是为了利用三角洲栖息地。在加里纳韦尔发现的新物种表明,体型较大的物种出现的时间比之前认为的要早得多。关于新墨西哥沉积物中有多少异齿龙物种的多样性也是一个问题。新发现的Gallina井Dimetrodon表明在Abo组存在两个同时期的物种。自2009年以来的研究表明,在新墨西哥州二叠纪的Abo洪泛平原上,异齿龙是一种更常见的掠食者,尽管不是主要的掠食者。要完全了解新墨西哥州下二叠纪的异齿龙,还需要进行更多的研究。
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