1982
DOI: 10.1016/s0016-6995(82)80054-5
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Phytosaur remains (Reptilia, Thecodontia)from the Upper Triassic of North-Eastern Thailand

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Cited by 26 publications
(18 citation statements)
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“…Restricted to the Upper Triassic of central Europe; south-west Germany (Trossingen-Aixheim region, Pfaffenhofen): Keuper succession, Middle Keuper, Stubensandstein, middle Stubensandstein, sandstone subunits sc2 and sc3 (Stoll 1929;Brenner 1973); Austria: Dachsteinkalk (Buffetaut 1993); northern Italy: Dolomia Principale, Calcare di Zorzino Formation (Renesto and Paganoni 1998;Renesto and Lombardo 1999). Reports of Mystriosuchus elsewhere are either misidenti®cations (North Germany: von Huene 1922) or represent undiagnostic phytosaur remains (Madagascar: Guth 1963).…”
Section: Synonym Belodon Von Meyer In Von Meyer and Plieninger 1844mentioning
confidence: 99%
“…Restricted to the Upper Triassic of central Europe; south-west Germany (Trossingen-Aixheim region, Pfaffenhofen): Keuper succession, Middle Keuper, Stubensandstein, middle Stubensandstein, sandstone subunits sc2 and sc3 (Stoll 1929;Brenner 1973); Austria: Dachsteinkalk (Buffetaut 1993); northern Italy: Dolomia Principale, Calcare di Zorzino Formation (Renesto and Paganoni 1998;Renesto and Lombardo 1999). Reports of Mystriosuchus elsewhere are either misidenti®cations (North Germany: von Huene 1922) or represent undiagnostic phytosaur remains (Madagascar: Guth 1963).…”
Section: Synonym Belodon Von Meyer In Von Meyer and Plieninger 1844mentioning
confidence: 99%
“…Phytosaurs are basal pseudosuchian archosaurs that had a semi‐aquatic lifestyle, much like extant crocodylians (Hungerbühler 2002), and lived during the Late Triassic. Remains of the group occur nearly worldwide and have been found in the south‐western and eastern United States, Germany, India, Thailand, Morocco, Madagascar and Brazil (Jaeger 1828; Mehl 1913; Camp 1930; Dutuit 1977; Chatterjee 1978; Buffetaut and Ingavat 1982; Hungerbühler 2002; Kischlat and Lucas 2003): this pattern of distribution may be related to palaeogeographic features of Pangaea. Phytosaurs are a major component of the fauna of the Chinle Formation and Dockum Group of the south‐western United States, and ‘leptosuchine’ phytosaurs are often used in conjunction with other components of the fauna as biostratigraphic markers within the Late Triassic (Camp 1930; Hunt and Lucas 1991; Lucas and Hunt 1993; Lucas 1998).…”
mentioning
confidence: 98%
“…Huene, ; Doyle & Sues, ), and the Germanic Basin of central Europe and nearby areas (e.g. Meyer, , ; Huene, , ; Kuhn, , ; Hungerbühler, , ; Hungerbühler & Hunt, ; Dzik, ; Brusatte et al ., ), with rarer material known from elsewhere, including Morocco (Dutuit, 1977a, b; Fara & Hungerbühler, ), Turkey (Buffetaut, Martin & Monod, ), India (Huene, ; Chatterjee, ), Thailand (Buffetaut & Ingavat, ) and Brazil (Kischlat & Lucas, ).…”
Section: Introductionmentioning
confidence: 99%