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A new kinosternoid from the Late Cretaceous Hell Creek Formation of North Dakota and Montana and the origin of the Dermatemys mawii lineage
Authors:Georgia E. Knauss  Walter G. Joyce  Tyler R. Lyson  Dean Pearson
Affiliation:1.SWCA Environmental Consultants, Inc.,Sheridan,USA;2.Department of Geoscience,University of Iowa,Iowa City,USA;3.Institut für Geowissenschaften,University of Tübingen,Tübingen,Germany;4.Division of Vertebrate Paleontology,Yale Peabody Museum of Natural History,New Haven,USA;5.Department of Geology and Geophysics,Yale University,New Haven,USA;6.Marmarth Research Foundation,Marmarth,USA;7.Pioneer Trails Region Museum,Bowman,USA
Abstract:A nearly complete turtle shell from the Late Cretaceous (Maastrichtian) Hell Creek Formation of Slope County, North Dakota, represents the most complete remains to date of a Mesozoic kinosternoid turtle and a new species, Hoplochelys clark nov. sp. The new taxon is diagnosable from other representatives of Hoplochelys by the plesiomorphic placement of the humeral/femoral sulcus behind the hyo/hypoplastral suture and the autapomorphic development of an interrupted median (neural) keel. All six previously named Paleocene (Puercan and Torrejonian) representatives of Hoplochelys lack diagnostic characters and are synonymized as Hoplochelys crassa. A phylogenetic analysis reveals that Hoplochelys spp. and Agomphus pectoralis are most parsimoniously placed within Kinosternoidea along the phylogenetic stem of the extant Mesoamerican River Turtle Dermatemys mawii, extending that taxon’s stem lineage from the early Eocene to the late Maastrichtian. The two primary crown lineages of Kinosternoidea are thus known from the Mesozoic and split prior to the late Campanian. The presence of a thickened cruciform plastron, true costiform processes, only three inframarginals, and the reduction of the medial contact of the abdominals are synapomorphies of Chelydroidea, the clade formed by Chelydridae and Kinosternoidae.
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