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Fenhosuchus is an extinct genus of archosauriform. The holotype, IVPP V 2697, and referred materials have been found in the Hsishihwa locality at , China, from the Upper Ermaying Formation (also Ehrmaying). The locality dates back to the Anisian stage of the Middle Triassic. The genus was named after the Fen River in Shanxi Province from which specimens were found. It may prove to be a chimera being composed of material from several different animals. Some material were believed to represent a rauisuchid. The calcaneum of Fenhosuchus seems to belong to an erythrosuchid or other basal archosauriform. Much of the material of the tarsal bones seem to be similar to those of the genus Shansisuchus. According to Nesbitt (2009) the assessment of Gower (2000) was correct, the holotype is a mix of

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rdf:type
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  • Fenhosuchus (en)
  • 汾河鱷屬 (zh)
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  • 汾河鱷屬（學名：Fenhosuchus）是主龍形類爬行動物的一屬，化石發現於中國山西省的臨汾市，生存年代為三疊紀安尼阶。汾河鱷可能是個嵌合體，由數種不同動物所構成，其中某些化石已被鑑定屬於勞氏鱷科。汾河鱷的似乎屬於引鱷科，或是其他基礎主龍類。跗骨則相當類似山西鱷。 (zh)
  • Fenhosuchus is an extinct genus of archosauriform. The holotype, IVPP V 2697, and referred materials have been found in the Hsishihwa locality at , China, from the Upper Ermaying Formation (also Ehrmaying). The locality dates back to the Anisian stage of the Middle Triassic. The genus was named after the Fen River in Shanxi Province from which specimens were found. It may prove to be a chimera being composed of material from several different animals. Some material were believed to represent a rauisuchid. The calcaneum of Fenhosuchus seems to belong to an erythrosuchid or other basal archosauriform. Much of the material of the tarsal bones seem to be similar to those of the genus Shansisuchus. According to Nesbitt (2009) the assessment of Gower (2000) was correct, the holotype is a mix of (en)
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authority
  • Young, 1964 (en)
fossil range
  • Middle Triassic, (en)
taxon
  • Fenhosuchus (en)
type species
  • Fenhosuchus cristatus (en)
type species authority
  • Young, 1964 (en)
has abstract
  • Fenhosuchus is an extinct genus of archosauriform. The holotype, IVPP V 2697, and referred materials have been found in the Hsishihwa locality at , China, from the Upper Ermaying Formation (also Ehrmaying). The locality dates back to the Anisian stage of the Middle Triassic. The genus was named after the Fen River in Shanxi Province from which specimens were found. It may prove to be a chimera being composed of material from several different animals. Some material were believed to represent a rauisuchid. The calcaneum of Fenhosuchus seems to belong to an erythrosuchid or other basal archosauriform. Much of the material of the tarsal bones seem to be similar to those of the genus Shansisuchus. According to Nesbitt (2009) the assessment of Gower (2000) was correct, the holotype is a mix of Shansisuchus remains and a possible fragment from a paracrocodylomorph or a dinosauriform. Thus, Fenhosuchus cannot be considered a rauisuchian. (en)
  • 汾河鱷屬（學名：Fenhosuchus）是主龍形類爬行動物的一屬，化石發現於中國山西省的臨汾市，生存年代為三疊紀安尼阶。汾河鱷可能是個嵌合體，由數種不同動物所構成，其中某些化石已被鑑定屬於勞氏鱷科。汾河鱷的似乎屬於引鱷科，或是其他基礎主龍類。跗骨則相當類似山西鱷。 (zh)
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