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Hyperdisease in the late Pleistocene: validation of an early 20th century hypothesis
Authors:Bruce M Rothschild  Richard Laub
Institution:(1) Arthritis Center of Northeast Ohio, 5500 Market Street, Youngstown, OH 44512, USA;(2) Northeastern Ohio Universities College of Medicine, Rootstown, OH 44527, USA;(3) Carnegie Museum of Natural History, Pittsburgh, PA 15213, USA;(4) University of Kansas Museum of Natural History, Lawrence, KS 66045, USA;(5) Buffalo Museum of Science, Buffalo, NY 14211, USA
Abstract:The hypothesis of disease-related large mammal extinction has new support. A unique pathologic zone of resorption was first noticed in a Hiscock Mammut americanum metacarpal. The pathognomonic zone of resorption was present in fifty-nine (52%) of 113 skeletons with feet available for examination. Metacarpals and metatarsals were most commonly affected. Associated rib periosteal reaction is highly suggestive of tuberculosis and the foot lesions were identical to that documented in Bison as pathognomonic for tuberculosis. Recognizing that only a portion of animals infected by infectious tuberculosis develop bone involvement, the high frequency of the pathology in M. americanum suggests that tuberculosis was not simply endemic, but actually pandemic, a hyperdisease. Pandemic tuberculosis was one of several probable factors contributing to mastodon extinction.
Keywords:Tuberculosis  Hyperdisease  Mastodon  Pleistocene  Erosive disease  Bison  Infection
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