A trematosauroid temnospondyl from the Middle Triassic of Jordan
نویسنده
چکیده
Phylogenetic hypotheses, biogeographic dispersal models, and evolutionary scenarios are difficult to form but easy to reject: a single fossil may be sufficient. Previously neglected or inaccessible regions bear high potential for the discovery of such fossils, because they shed light on new faunas with unorthodox combinations of taxa, and sometimes reveal representatives of clades that were not expected in such a place and time. In the Triassic, many tetrapods reached a worldwide distribution – or at least the fossil record is good enough to document such a distribution. Still, there are regions where the record is poor, with the Middle East ranking among those. Here I report evidence for a Middle Triassic tetrapod from a region that may have been crucial for dispersal of shallow water taxa but hitherto yielded very little material: Jordan. During the Triassic, the Tethys covered vast areas of northern Gondwana, among them northern Africa and the Middle East. In deposits formed under epicontinental, shallow marine conditions, aquatic reptiles (placodonts, nothosaurs, pachypleurosaurs, thalattosaurs) are usually abundant, and a few finds have been reported from the Middle East (Rieppel et al. 1997, 1999). However, the specimen reported here stems from a temnospondyl, representing a clade of early tetrapods (stem-amphibians) believed to have inhabited a vast range of water bodies from rivers and lakes over brackish marshes to epicontinental shallow marine habitats (Schoch & Milner 2000; Laurin & Soler-Gij n 2001). The objective of the present study is to describe the find and elucidate its phylogenetic position among the temnospondyls.
منابع مشابه
Triassic Vertebrate Fossils in Arizona
The Triassic System in Arizona has yielded numerous world-class fossil specimens, including numerous type specimens. The oldest Triassic vertebrates from Arizona are footprints and (largely) temnospondyl bones from the Nonesian (Early Triassic: Spathian) Wupatki Member of the Moenkopi Formation. The Perovkan (early Anisian) faunas of the Holbrook Member of the Moenkopi Formation are exceptional...
متن کاملMessage in a Bottle- a Tale of Two Triassic Temnospondyl (labyrinthodont) Femora from Tasmania
Akerman, K. & Rozefelds, A.C. 2011(9:xii): Message in a bottlea tale of two Triassic temnospondyl (labyrinthodont) femora from 'Talmania. Papers and Proceedings of the Royal Society of7asmania 145: 5-8. ISSN 0080-4703. 4 Dorset Street, Moonah, Tasmania 7009, Australia (KA*); Queensland Museum, GPO Box 3300, South Brisbane, Queensland 4101, Australia (ACR*). *Authors for correspondence: Emails: ...
متن کاملYuanansuchus maopingchangensis sp. nov., the second capitosauroid temnospondyl from the Middle Triassic Badong Formation of Yuanan, Hubei, China
A second species of Yuanansuchus, Y. maopingchangensis, is erected for new temnospondyl material from the Maopingchang site, Yuanan County, Hubei Province, China. These specimens are from the same horizon that produced Y. laticeps, the type species. Y. maopingchangensis shares the following features with Y. laticeps: postorbital portion of skull occupied more than 1/3 of skull length; tabular h...
متن کاملSynchrotron Reveals Early Triassic Odd Couple: Injured Amphibian and Aestivating Therapsid Share Burrow
Fossorialism is a beneficial adaptation for brooding, predator avoidance and protection from extreme climate. The abundance of fossilised burrow casts from the Early Triassic of southern Africa is viewed as a behavioural response by many tetrapods to the harsh conditions following the Permo-Triassic mass-extinction event. However, scarcity of vertebrate remains associated with these burrows lea...
متن کاملTriassic-jurassic Boundary on the Southern Margin of Tethys: Implications of Facies, Tectonics and Volcanism
The facies changes, tectonics and magmatism across the Triassic–Jurassic boundary in the southern Tethyan margin have been studied in Egypt, Sudan, Jordan and Saudi Arabia. In Saudi Arabia and Jordan an unconformable contact is recognized between the Upper Triassic and Lower Jurassic rocks. This unconformity surface is marked by the truncation of the fluvial clastics of the uppermost Triassic b...
متن کامل