To explore shape variability among crocodylian skull tables, an analysis using geometric morphometric methods is conducted with the inclusion of extant and fossil taxa. Skull tables are variable and the differences likely play a role in hydrodynamics, species recognition, and biomechanical adaptations. Comparisons of allometric change within taxa are explored revealing that adults significantly diverge from juvenile skull table morphologies in most species and these changes happen in a stereotyped way. In all analyses, adults of the smallest extant taxa plot alongside the juveniles of related taxa and heterochrony may explain the maintenance of these morphologies into adulthood.When landmarks representing the supratemporal fenestrae are included, longirostrine taxa are broadly separated from one another due to variation in the size of the supratemporal fenestrae. The hypotheses of previous studies suggesting that the size of the supratemporal fenestrae is influenced by snout length-with longer snouts corresponding to larger fenestrae-must be reevaluated. Although species of the crocodyloids Tomistoma and Euthecodon approach or exceed the length of the snout in gavialoids, their supratemporal fenestrae are proportionally smaller-this suggests a phylogenetic constraint in crocodyloids regardless of snout length.

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Natural Trap Cave is a sinkhole cave located in Big Horn County in northern Wyoming. The cave preserves many Quaternary taxa, including pollen and large carnivorous and herbivorous mammals such as various felids and ungulates. Many of these taxa went extinct in North America following the late Pleistocene megafaunal extinction. The cave was first excavated in the 1970s and 80s by teams from the University of Kansas and the University of Missouri, and more recently by teams from Des Moines University, The University of Adelaide, and The University of Rochester, along with a wide variety of volunteers. Specimens from this cave have been used to elucidate floral change in the area, disentangle ancient food webs, and extend the hypothesized range for Beringian wolves. Horses are the most common megafaunal group from this site, encompassing two genera: Equus and Haringtonhippus, the “New World stilt‐legged” horse, based on post‐cranial elements and mitochondrial DNA. Some recent studies have shown that horse taxa can be identified by tooth occlusal surface morphology. This study aims to test if isolated equid cheek teeth from Natural Trap Cave can be identified to the genus level, between Equus and Haringtonhippus using geometric morphometrics. 2D landmarks and sliding semi‐landmarks were taken around the periphery of a set of upper cheek teeth, including the areas of greatest curvature at the metastyle, mesostyle, parastyle, and around the protocone and post protoconal valley. Principal component analyses on known specimens do in fact separate Equus and Haringtonhippus, and this difference is statistically sigificant, with the primary difference being the width of the protocone. Additionally, molars and premolars also occupied significantly different areas of morphospace, opening up the possibility of identifying tooth position on unknown specimens as well. With the abundance of isolated horse teeth (either Equus or Haringtonhippus) from Natural Trap Cave, having a reliable means to distinguish between genera will allow us to better study the ecological differences between them and better understand the environment and faunal interactions in late Pleistocene Wyoming. Support or Funding Information NSF EAR/SGP 1425059 (Natural Trap Cave Revisited: Ancient DNA, Climate and the Megafaunal Extinction) Julie Meachen, PI

One of the interesting features of modern sloths is the vasculature patterns of their upper and lower limbs. Even though sloths are endothermic like other mammals, their mean body temperature tends to be lower, more variable, and more linked to the ambient temperature than other placental mammals. Like some other mammals from environments with temperature extremes, they possess rete arteriovenous bundles, which work as an effective heat exchange mechanism, where heat from distally flowing arterial blood is transferred to proximally flowing venous blood. This minimizes the heat loss from the extremities while still maintaining blood flow. The temperature gradient increases in the rete system when the animal’s core temperature decreases, which cools the limbs and preserves core body heat. When the body temperature rises the flow through the superficial venous system increases, which promotes heat loss and body cooling. This begs the question of how this complex vasculature system may or may not extend to the distal phalanges and claws of the sloth, perhaps their most distinctive feature. One possibility could be that to work with the limb cooling function of the rete system, the distal phalanx and claw may be poorly vascularized so as not to increase chances for heat loss. However, considering the extensive and important use of their claws, they may require extensive vascularization to withstand the large amount of stress they are often under. This study uses Micro CT scans of sloth ungual phalanges to visualize their vascular channels. In both modern and extinct giant ground sloths, vascular networks through the bone of the ungual phalanx are quite extensive, and are very clearly linked to externally visible channels and impressions left by the proper digital arteries. In ground sloths these internal vascular channels quickly branch on either side and continue distally, letting off smaller branches as they go. These channels are rather large, even appearing to be artificial drill holes on one specimen that has the distal end broken off. Modern sloths show a similar pattern, but their vascular channels take up proportionally less space in the bone than in the giant ground sloths. This difference may be due extinct giant ground sloths’ more varied use of their claws. These complex patterns show that sloth claws require a significant blood supply, and may indicate that the rete system is effective enough that by the time the arterial blood gets to the distal phalanx it has been sufficiently cooled to not be a significant source of heat loss.