Psephosauriscus
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''Psephosauriscus'' is an extinct genus of placodont reptile from the Middle Triassic of Israel and Egypt. It is known from bony armor plates that have been found from
Makhtesh Ramon Makhtesh Ramon ( he, מכתש רמון; ''lit.'' Ramon Crater/Makhtesh ; ar, وادي الرمان, links=no) is a geological feature of Israel's Negev desert. Located some 85 km south of the city of Beersheba, the landform is the world' ...
in Israel's Negev desert and Araif en Naqua on Egypt's Sinai Peninsula. The genus was erected in 2002 as a replacement name for several species of the genus ''Psephosaurus'', which was named in 1957. It includes the species ''P. mosis'', ''P. ramonensis'', ''P. sinaiticus'', and a possible fourth species, ''P. rhombifer''. All species, with the exception of ''P. ramonensis'', were once assigned to the genus ''Psephosaurus''. Remains of ''P. mosis'' and ''P. ramonensis'' were found in Makhtesh Ramon, while ''P. sinaiticus'' and ''P. rhombifer'' were found in Araif en Naqua.


History

Armor of ''Psephosauriscus'' is abundant in Middle Triassic limestone in the Sinai and Negev regions, which is comparable to the Muschelkalk of European rock sequences. While the German Muschelkalk contains many nearly complete skeletons of placodonts, the only non-armor skeletal bones from the Middle East are two partial skulls and a fragmentary lower jaw, which cannot be assigned to ''Psephosauriscus'' or any other placodont because of their lack of diagnostic features. Remains of ''Psephosauriscus'' come from two deposits called the ''
Beneckeia ''Beneckeia'' is a genus of Lower to Middle Triassic ammonites included in the ceratitid Ceratitida is an order that contains almost all ammonoid cephalopod genera from the Triassic as well as ancestral forms from the Upper Permian, the excep ...
'' beds and the '' Ceratites'' beds, named after their most common
ammonite Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttlefish) ...
fossils. The ''Beneckeia'' beds date back to the Anisian stage of the Middle Triassic, and the ''Ceratites'' beds date back to the end of the Anisian and beginning of the Ladinian stage. Swedish paleontologist F. Brotzen described placodont armor from Makhtesh Ramon in 1957, naming the species ''Psephosaurus mosis'' and ''Psephosaurus picardi'' from the ''Beneckeia'' and ''Ceratites'' beds, respectively. ''P. picardi'' is now considered a ''
nomen dubium In binomial nomenclature, a ''nomen dubium'' (Latin for "doubtful name", plural ''nomina dubia'') is a scientific name that is of unknown or doubtful application. Zoology In case of a ''nomen dubium'' it may be impossible to determine whether a s ...
'' because it was based on an impression of the inner surface of the carapace that did not possess any distinct features. In 1959, Austrian paleontologist Georg Haas named ''P. sinaiticus'' and ''P. rhombifer'' from Araif en Naqua. In 2002, paleontologist Olivier Rieppel erected the genus ''Psephosauriscus'' to include most of the species named by Brotzen and Haas, which he considered distinct from the type species of ''Psephosaurus'', ''P. suevicus'', named by Eberhard Fraas from the Middle Triassic of Germany. Rieppel noted differences between the armor plates of ''P. suevicus'' and the Middle Eastern species that warranted a new genus. However, ''P. rhombifer'' could not be assigned with certainty to ''Psephosauriscus'' because the holotype specimen described by Haas had since been lost. Rieppel reported additional material from Araif en Naqua that showed similarities to ''P. rhombifer'' and the species of ''Psephosauriscus'', which he tentatively described as a species within ''Psephosauriscus'', ''Psephosauriscus cf. rhombifer''. Rieppel also named ''Psephosauriscus ramonensis'' as an entirely new species.


Species

The type species of ''Psephosauriscus'', ''P. mosis'', is known from a single specimen including portions of the
carapace A carapace is a Dorsum (biology), dorsal (upper) section of the exoskeleton or shell in a number of animal groups, including arthropods, such as crustaceans and arachnids, as well as vertebrates, such as turtles and tortoises. In turtles and tor ...
and plastron. The scutes that cover the armor plates do not have as well-defined a shape as the hexagonal osteoderms that lay underneath them. The osteoderms that form the plastron are relatively large. Some osteoderms have a raised keel. Two distinct ridges along either side of the shell separate the carapace, a lateral wall of smaller osteoderms, and the plastron. ''P. ramonensis'' is known from a partial carapace and connected plastron. The osteoderms of the carapace have smoother edges than most other species of ''Psephosauriscus'', and lack the keel of species like ''P. mosis''. The carapace curves into the lateral wall of the body without a separating ridge as in ''P. mosis'', but a lower ridge does separate the lateral wall from the plastron. ''P. sinaiticus'' is known from several armor fragments and larger pieces of the carapace and plastron. The osteoderms of the carapace and plastron are smaller than those of other species. As in ''P. mosis'', two ridges separate run along the side of the shell. ''P. cf. rhombifer'' can be distinguished from the three other species of ''Psephosauriscus'' by the rectangular shape of its scutes. Unlike the smooth shells of other species, the carapace of ''P. cf. rhombifer'' has a bumpy surface; each osteoderm is covered in radiating grooves and has a small depression at its center.


References

{{Taxonbar, from=Q20722690 Middle Triassic reptiles of Africa Placodonts Anisian life Anisian genus first appearances Ladinian genus extinctions Sauropterygian genera