An unusually large metaposaurid from the Salitral Formation of the Chinle Group (Upper Triassic: Carnian?) on lands belonging to the Pueblo of Jemez

K. Madalena, K. Zeigler, S. Sumida
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Abstract

Lands belonging to the Pueblo of Jemez in north-central New Mexico include sedimentary strata that range in age from Mississippian to Pleistocene, and include excellent exposures of Upper Triassic strata. The Salitral Formation of the lower Chinle Group (Upper Triassic: Carnian) are present in the southeastern corner of the Jemez Reservation in an area that is complexly faulted. Samples for paleomagnetic analyses have been taken from the area in order to clarify the stratigraphic relationships and are currently in progress. Material pertaining to a metoposaurid amphibian was recovered from a grayish-purple calcrete nodule horizon in the lower Salitral Formation, approximately 7-8 m above the underlying Shinarump (=Agua Zarca) Formation. The fossil-bearing horizon is comprised primarily of a poorly consolidated conglomeratic lens dominated by calcareous nodules from 1-10 cm diameter. This unit also contains moderately abundant fragments of metoposaur and phytosaur material. Metoposaurid material includes cranial and shoulder girdle elements as well as teeth. Phytosaur material includes teeth and osteoderms with a characteristically high dorsal ridge. The metoposaurid specimens are fragmentary, but are significant for their extraordinary size. A partial interclavicle is conservatively reconstructed as well over 450 cm in width. The largest specimen reported from Texas is 430 cm, and a specimen previously reported as the largest from New Mexico is 400 cm in width. Published sizes of metoposaurid interclavicles from the Chinle Formation of New Mexico and the Dockum Formation of West Texas average 307 m and 313 cm respectively. Thus, the Jemez metoposaur is one of the largest ever reported, approximately 47-48% larger than those published averages, and approximately 5% larger than the largest one yet reported. Although measurements of the thickness of dermal elements of the pectoral girdle are not commonly available, the Jemez metoposaur also appears remarkable in this regard, measuring over 2.5 cm from deep to superficial surfaces.
来自Chinle群(上三叠统:卡尼亚?)的Salitral组的一种异常大的变质龙,位于属于耶梅斯普韦布洛的土地上
位于新墨西哥州中北部的耶梅斯普韦布洛的土地上有从密西西比世到更新世的沉积层,其中包括上三叠统地层的优秀暴露。下秦乐群(上三叠统:卡尼期)沙里特尔组发育于热梅兹保留地东南角,是一个复杂的断陷区。为了澄清地层关系,已经从该地区提取了古地磁分析样本,目前正在进行中。在下部Salitral组的灰紫色钙质结核层位中发现了一种甲状纲两栖动物的材料,该层位位于下伏Shinarump组(=Agua Zarca)组上方约7-8米处。含化石层位主要由胶结不良的砾岩透镜体组成,以直径1 ~ 10 cm的钙质结核为主。这个单元还包含了相当多的mettoposaur和phytosaur材料碎片。后头龙材料包括颅骨和肩带元素以及牙齿。植龙的物质包括牙齿和具有典型的高背脊的骨皮。这些后鳞龙标本是碎片状的,但因其巨大的体型而具有重要意义。保守地重建了部分锁骨,宽度超过450厘米。据报道,来自德克萨斯州的最大的标本有430厘米长,而以前报道的来自新墨西哥州的最大标本有400厘米宽。新墨西哥州Chinle组和西德克萨斯州Dockum组已公布的中跖龙锁骨的平均尺寸分别为307 m和313 cm。因此,杰梅兹metosaurus是迄今为止报道过的最大的龙之一,比已发表的平均大小大约大47-48%,比迄今报道过的最大的龙大约大5%。虽然胸带皮肤成分厚度的测量并不常见,但在这方面,杰梅兹表龙也很引人注目,从深层到表层的测量超过2.5厘米。
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