Lower Cretaceous Anacoracidae? (Lamniformes: Neoselachii); vertebrae and associated dermal scales from Australia

Partially disarticulated shark vertebrae from the Lower Cretaceous Toolebuc Formation in central Queensland and the Bathurst Island Formation in the Northern Territory provide probable evidence of the Anacoracidae in Australia, and are possibly referable to Pseudocorax. Associated with large shark vertebrae from Canary Station, near Boulia, Queensland, are numerous placoid scales of four primary types which indicate a large pelagic shark. The Canary specimen is one of the few Mesozoic sharks known where scales have been found associated with vertebrae. Problems in referring the new shark material to the Anacoracidae and Pseudocorax are discussed. The significance of vertebral structure and scale morphology in Mesozoic shark evolution and ecology is examined. ‘Lamna daviesii’ Etheridge 1888 is considered a nomen dubium as vertebrae of this kind also occur in other genera in the Lamniformes, Orectolobiformes, and Carcharhinidae.     

Selachian scales from the Cenomanian (Late Cretaceous) of Bathurst Island,northern Australia

Seven selachian scale types are described from the middle Cenomanian Moonkinu Formation, outcropping on the southern shores of Bathurst Island in northern Australia. The scales are classified in accordance with previously published scale morphologies of Cretaceous and modern sharks, and are representative of the Orders Squatiniformes (Family Squatinidae), Carcharhiniformes (Family Scyliorhinidae), and Lamniformes (Family Odontaspididae). The presence of typically bottom-dwelling, shallow-water angelsharks (squatinids), catsharks (scyliorhinids), and sand tiger sharks (odontaspidids) within the Moonkinu Formation support an inner neritic depositional environment interpretation for the unit, previously determined from foraminiferal biofacies and lithology. The biostratigraphic potential of these scales can only be assessed after scales from more Cretaceous localities are described and documented.     

Differential diagnosis of cartilaginous dysplasia and probable Osgood–Schlatter's disease in a Mississippian individual from East Tennessee

This paper details the differential diagnosis of an adult female skeleton displaying features consistent with a cartilaginous dysplasia and Osgood–Schlatter's disease. This burial was excavated in 1940 from a Mississippian platform mound at the DeArmond site (40RE12) in Roane County, Tennessee as part of the Works Progress Administration (WPA) and Tennessee Valley Authority (TVA) archaeological investigations. The right humerus and left femur of this individual display traits consistent with achondroplasia, such as shortened length and normal width. However, the rest of the long bones display typical morphology. The affected humerus and femur are 82 mm and 58 mm shorter than their counterparts, respectively. This makes for obvious asymmetry. A review of the various cartilaginous dysplasias was undertaken to identify those conditions concordant with the differential manifestation of the long bone asymmetry. Morphological and radiographic analyses were used to rule out possible diagnoses. The most likely candidate is enchondromatosis out of the presented conditions, as it most commonly affects the long bones, does not affect every bone in the skeleton, and is asymmetrical in its manifestation. In addition to the cartilaginous dysplasia, both anterior proximal tibial metaphyses of this individual display defects that are roughly triangular with pitted, irregular floors. Osgood–Schlatter's disease is caused by repeated trauma to the tibial tuberosity during childhood. This individual would have walked with an obvious limp, and perhaps the added biomechanical stress on both quadriceps muscles as a result caused the injuries and resultant defects to its attachment points. Evidence of these conditions in an adult indicates that the Mississippian people in this community offered some sort of social support to differently‐abled individuals. Copyright © 2009 John Wiley & Sons, Ltd.