Abstract

Arthritic lesions have been frequently diagnosed in the fossil record, with spondyloarthropathy (a type of erosive and pan-mammalian arthritis) being one of the most common types described to date for mammals, though not restricted to this group. Here, we identify spondyloarthropathy in fossil bones from the late Pleistocene in Brazil assignable to a large glyptodont individual. Bone erosions in the peripheral joints (viz., the ulna, radius, left femur and tibiae-fibulae) associated with osteosclerosis allow the diagnosis of spondyloarthropathy. The presence of osteophytes in seven bones of the forelimbs (viz., the ulna and radius) and hind limbs (viz., the tibiae-fibulae, left femur and patellae) and a subchondral cyst in one element (viz., the left femur) indicate secondary osteoarthritis. A calcified deposition on the articular surface of the left patella indicates the presence of calcium pyrophosphate deposition disease, which, like the observed osteoarthritic alterations, likely represents a complication of spondyloarthropathy. This is the first report of spondyloarthropathy for xenarthrans.

Highlights

  • Arthritis includes a wide variety of joint diseases, including those in which the proliferation of new bone is the main feature and those in which the key characteristic is bone erosion [1,2]

  • We report a case of spondyloarthropathy in a glyptodont, one of the most abundant and diversified members of the Pleistocene megafauna of South America

  • The fossil accumulations in these sediments are composed mostly of mammalian remains belonging to species typical of the Quaternary of the Brazilian Intertropical Region [12]

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Summary

Introduction

Arthritis includes a wide variety of joint diseases, including those in which the proliferation of new bone is the main feature (osteoarthritis) and those in which the key characteristic is bone erosion [1,2]. It is characterized by the propensity to form new bone, to ossify insertion sites of tendons or ligaments, to erode or asymmetrically fuse peripheral joints and to present articular lesions in the vertebral column and the sacroiliac joint [1,2,3]. Such alterations are associated with a specific histocompatibility antigen, HLA-B27 [1,2,3]. Its earliest appearances in the fossil records are in archosaurs from the Triassic and Jurassic periods [6,7]

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