A highly diverse ichnofauna in Late Triassic deep-sea fan deposits of Oman

Ichnos (Impact Factor: 1.08). 09/2007; 16(5):179-185. DOI: 10.2110/palo.2006.p06-098r


We encountered a highly diverse ichnofauna within the deep-sea fan
deposits of the Upper Triassic Al Ayn Formation in Oman. It comprises
32 ichnogenera: 18 ichnogenera represent predepositional graphoglyptids
and other trace fossils that are preserved as casts onturbidite soles, and 14 ichnogenera represent postdepositional tracefossils that penetrate turbidite beds. The relatively large size of the area studied certainly favors encountering a high number of ichnogenera. The diversity we found approximately doubles the value that has often been stated in the literature and contradicts the paradigm that the Triassic represents a time of low ichnodiversity in the deep
sea. Although the data are limited, in general the recovery of deepsea tracemakers has been very slow owing to environmental disturbances that resulted from cold-bottom-water circulation after the Carboniferous–Permian glaciation. The high ichnodiversity in the Al
Ayn Formation is explained by its paleogeographic position and locally formed warm bottom waters. The Al Ayn deposits accumulated adjacent to wide evaporitic and carbonate shelves, indicating continuous warm conditions. The Al Ayn clastic system was likely influenced
by dense, salt-rich, warm water flowing back to the ocean from the carbonate and evaporitic shelf area. The downwelling water may have reduced the effects of cold water that formed during the Late Paleozoic glaciation and the Permian–Triassic anoxia, and, thus, it
may have provided a refuge habitat. Despite the global trend of lowdiversity deep-sea ichnocoenoses, refuge habitats may have been established in areas less affected by the otherwise harsh conditions.

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Available from: Alfred Uchman, Nov 29, 2014
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    • "Thalassinoides is a facies-crossing trace fossil, most typical of shallow-marine environments (Palmer 1978; Archer and Maples 1984; Frey et al. 1984; Mangano and Buatois 1991) and is produced mainly by crustaceans (Frey et al. 1984). T. suevicus has been noted even at greater depths (Uchman 1995, 1998; Uchman and Tchoumatchenco 2003; Wetzel et al. 2007). According to Uchman (1995), the crustaceans producing Thalassinoides may survive transport in turbiditic currents and produce burrows under anoxic conditions for a limited number of days. "
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