Results 161 to 170 of about 665 (187)
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Fusion of sacrals and anatomy inChampsosaurus(Diapsida, Choristodera)

Historical Biology, 2007
Sacral centra are occasionally fused with or without severe deformation in Champsosaurus (Diapsida, Choristodera). The sympatrical occurrence of fusion and non-fusion of sacra in adults through their evolution questions that sacral fusion represents the final form of a simple ontogenetic change or specific variation.
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A “beaded” sphenodontian (Diapsida: Lepidosauria) from the Early Cretaceous of central Mexico

Journal of Vertebrate Paleontology, 1997
ABSTRACT The Albian sphenodontian Pamizinsaurus tlayuaensis, gen. et sp. nov., from the Tlayua Quarry, Central Mexico, is described. The holotype is a posthatchling characterized by the presence of rows of small rounded osteoderms transversally oriented, relatively few hatchling teeth each with well-developed ridges, and a posteriorly displaced ventral
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Limb Ontogeny, Evolution and Aquatic Adaptation in the Neodiapsida (Reptilia: Diapsida)

1995
This study examines the phylogeny and ontogeny of limb evolution in the Neodiapsida (Reptilia). Patterns and sequences of limb ossification are described from the ontogenies of fossil and extant, aquatic and terrestrial, neodiapsids. Taxa described in detail include the extant squamate Varanus timorensis, the fossil neodiapsids Hovasaurus boulei ...
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Geographic and Stratigraphic Distribution of the Triassic Ichthyosauria (Reptilia; Diapsida)

Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 1989
Jack M. Callaway, Judy A. Massare
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Phylogeny of the Sauropterygians (Diapsida; Triassic - Cretaceous)

Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 1987
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The braincase of Youngina capensis (Reptilia: Diapsida; Permian)

Neues Jahrbuch für Geologie und Paläontologie - Monatshefte, 1987
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The first Middle Triassic ichthyopterygian (Reptilia, Diapsida) from Croatia

The Žumberak Mountains are situated in northwestern Croatia, where they represent a part of the Internal Dinarides. A substantial exposure of Triassic sedimentary rock is present in this area, most of which comprises poorly to non-fossiliferous dolostones formed on a carbonate platform.
Vidaković, Fran   +2 more
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