Thursday, November 15, 2012

Experiments in Giantism During the Triassic

Unique bone histology in partial large bone shafts from Aust Cliff (England, Upper Triassic): an early independent experiment in gigantism


1. Ragna Redelstorff (a)
2. P. Martin Sander (b)
3. Peter M. Galton (c)


a. Zoology Department, University of Cape Town, Private Bag X3, Rondebosch, 7701, Cape Town, South Africa

b. Steinmann Institute for Geology, Mineralogy and Palaeontology, University of Bonn,
Nussallee 8, 53115 Bonn, Germany

c. College of Naturopathic Medicine, University of Bridgeport, Bridgeport, Connecticut, USA


Two giant partial bone shafts, possible femora, from the Rhaetian Bone Bed (Upper Triassic) of Aust Cliff in SW England continue to conceal their origin. The most striking characteristic of these bones is their size, showing that dinosaur-like gigantism had already evolved by the Late Triassic. Based on their characteristic, columnar shaft morphology, Galton (2005) suggested they came from a prosauropod or stegosaur. The bone histology of both specimens is very similar: the cortex is always rather thin, not exceeding 10 mm, and is of fibrolamellar type with longitudinal primary osteons. The primary osteons show a rather unusual feature, the development of a secondary osteon inside the primary one. The bone surface in both specimens shows open vascular canals, suggesting that the animals were still growing at the time of death, but an external fundamental system (EFS) is visible in the outermost cortex of specimen BRSMG Cb3870. The external cortex shows dense growth marks, but their annual nature is difficult to ascertain. The bones are probably dinosaurian, as indicated by the fibrolamellar bone, and possibly belong to an unknown basal sauropodomorph lineage. Alternatively, some very large pseudosuchians may have evolved fibrolamellar bone independently as an adaptation for reaching giant size.

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