ONTOGENETIC CHANGE IN THE TEMPORAL REGION OF THE EARLY PERMIAN PARAREPTILE DELORHYNCHUS CIFELLII AND THE IMPLICATIONS FOR CLOSURE OF THE TEMPORAL FENESTRA IN AMNIOTES.

A juvenile specimen of Delorhynchus cifellii, collected from the Early Permian fissure-fill deposits of Richards Spur, Oklahoma, permits the first detailed study of cranial ontogeny in this parareptile.The specimen, consisting of a partially articulated skull and mandible, exhibits several features that identify it as juvenile.The dermal tuberositi

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For some stream structures such as barrages, regulators, as well as change of channel cross section, the downstream expansion transitions structures are the common requirement.Eddies, as a result of the flow separation in such structures leads to destruction the bed and sides of the downstream channel.Head loss, on the other hand, produced through

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