. Bulletin of the Natural Histort Museum. Geology series. 50 CHARIG AND MILNER. Fig. 39 Baryonyx walked, holotype. BMNH R9951; ventral elements of pelvis. A. left pubis lacking proximal end, posterior view; B, left ischium lacking distal end, lateral, x The distal part of the left pubis is also flattened, with fairly thick, rounded edges; but it seems likely that the plane of flattening was somewhat different from that of the central fragment, parasagittal rather than transverse, from which we infer that there must have been some degree of torsion between the two me
. Bulletin of the Natural Histort Museum. Geology series. 50 CHARIG AND MILNER. Fig. 39 Baryonyx walked, holotype. BMNH R9951; ventral elements of pelvis. A. left pubis lacking proximal end, posterior view; B, left ischium lacking distal end, lateral, x The distal part of the left pubis is also flattened, with fairly thick, rounded edges; but it seems likely that the plane of flattening was somewhat different from that of the central fragment, parasagittal rather than transverse, from which we infer that there must have been some degree of torsion between the two means that the two surfaces would have faced medially and laterally respec-i tively, and the positions of the two edges would have been anterodorsal and posteroventral; meanwhile the blade shows a distinct curvaturen^^ towards the midline as it approaches its distal end. The anterodorsal] a edge thickens towards the distal end, its medial and lateral margins i. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Natural History Museum (London). Andover : Intercept
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