NEW RECORDS OF THE INVERTEBRATE ICHNOFOSSILS ROBLEDOICHNUS AND TONGANOXICHNUS FROM THE LOWER PERMIAN OF NEW MEXICO

A. J. Lerner, S. Lucas, A. Hunt
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Abstract

Tonganoxichnus robledoensis and Robledoichnus lucasi are ichnotaxa that have previously been reported only from single occurrences in Lower Permian strata of southern New Mexico. Here we record the first occurrence of these ichnotaxa outside of their type localities within the Robledo Mountains Formation, thus augmenting their distribution. Single specimens of each ichnotaxon occur in association on a slab that was collected from New Mexico Museum of Natural History (NMMNH) locality 5383 in the lower part of the Abo Formation in the Red Gap area of the Fra Cristobal Mountains in Sierra County, New Mexico. The specimens are from a 0.7-meter thick unit of thinly bedded, ripplelaminated sandstone. A low diversity tetrapod ichnofauna that is dominated by Batrachichnus occurs at this site. Several specimens of the invertebrate burrow Taenidium have also been found. The paleoenvironment was a fluvial sandflat on a coastal floodplain. symmetrical trace anterior, posterior, and terminal that ichnospecies. Lateral the Robledo Mountains Formation type the mid-line. two types within T. , variations in jumping behavior. three pairs of lateral imprints that anteriorly directed. Fra three pairs of lateral imprints in anterior imprints anteriorly directed, the medial imprints laterally directed, the posterior imprints are posteriorly directed. orientation similarly in T. , resting trace the Upper Carboniferous Two track rows of walking imprints are shown that contain a twoimprint arrangement comparable to the type specimen from the Shalem Colony section of the Robledo Mountains Formation. A separate landing trace is not preserved. The trackway is 7 cm long and 1 cm in external width. It is separated from P-40869 by a distance of 7 cm. The external width of the trackway coincides with the distal width of the leg appendage imprints seen on the associated T. robledoensis . Kozur and Lemone thought that the producer of R. lucasi flying insect. We propose R. lucasi produced by an apterygote monuran, the same Tonganoxichnus
新墨西哥州下二叠纪无脊椎鱼化石robledoichnus和tonganoxichnus的新记录
Tonganoxichnus robledoensis和Robledoichnus lucasi是以前仅在新墨西哥州南部下二叠纪地层中单次发现的鱼类群。在Robledo山组中,我们首次记录了这些鱼类群在其类型位置之外的出现,从而扩大了它们的分布范围。在新墨西哥州塞拉县Fra Cristobal山脉红缺口地区Abo组下部5383号新墨西哥自然历史博物馆(NMMNH)收集的一块石板上,每个鱼分类群的单个标本都出现在一起。这些标本来自0.7米厚的薄层状波纹状砂岩。该遗址发育以Batrachichnus为主的低多样性四足鱼动物群。还发现了几个无脊椎穴居动物的标本。古环境为沿海洪泛平原上的河流沙滩。对称的痕迹前,后,和末端的鱼种。Robledo山组侧向为中线。t的两种类型,跳跃行为的变化。三对侧面的印痕指向前方。有三对外侧印在前印前向,内侧印外向,后印后向。在上石炭世的静止痕迹中,显示了两行行走痕迹,其中包含与Robledo山脉组Shalem群落剖面的模式标本相当的双印记排列。没有保留单独的着陆痕迹。轨道长7厘米,外宽1厘米。它与P-40869相隔7厘米。脚印的外部宽度与在相关的罗博多猿人身上看到的腿部附属物印记的远端宽度一致。Kozur和Lemone认为lucasi飞虫的生产者。我们认为lucasi是由同为Tonganoxichnus的一种单胞体(aptergote monuran)产生的
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