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The limestone layers are skeletal (vertebrate and invertebrate) packstones to wackestones and are interpreted as episodic thin-bedded turbidite and debris flow deposits that resulted from redeposition of slope sediments. Forty-seven vertebrate fossils were collected that consist of complete and fragmented cranial and postcranial elements belonging to Eosauropterygia, Thalattosauria, and Ichthyosauria, including the genus Shonisaurus. Bones are frequently disassociated and show predepositional abrasion and breakage. Another less common taphonomic mode is observed, characterized by several large associated elements, representing a single individual, found parallel to bedding and draped by shale. Rare Osteichthyes and Chondrichthyes teeth are also present. Bivalve and conodont fossils indicate a middle Norian age for the assemblage.<\/jats:p>","DOI":"10.2110\/palo.2009.p09-010r","type":"journal-article","created":{"date-parts":[[2009,8,20]],"date-time":"2009-08-20T11:16:33Z","timestamp":1250766993000},"page":"603-615","source":"Crossref","is-referenced-by-count":10,"title":["Deposition and taphonomy of the Hound Island Late Triassic vertebrate fauna: Fossil preservation within subaqueous gravity flows"],"prefix":"10.2110","volume":"24","author":[{"given":"Thomas L","family":"Adams","sequence":"first","affiliation":[{"name":"1Southern Methodist University, Roy M. 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