Where: England, United Kingdom (50.7° N, 3.3° W: paleocoordinates 13.4° N, 10.8° E)
• coordinate stated in text
• small collection-level geographic resolution
When: Otter Sandstone Formation (Sherwood Sandstone Group), Anisian (247.2 - 242.0 Ma)
• "Stratigraphically, the skull was found about 3 m below the top of Andy Newell’s Unit C, the Pennington Point Member of Gallois, and layer 21 of Hounslow and McIntosh (2003). According to the magnetostratigraphy of these authors, the age of this horizon is within the late Illyrian (latest Anisian), equivalent to the lower part of the Tethyian P. trammeri (conodont) Zone."
•
•"The [Otter Sandstone Formation] is dated as Anisian on the basis of faunal comparisons and matching with palynologically dated units in the English Midlands... This has since been confirmed by magnetostratigraphy (Hounslow and McIntosh 2003), who found that the lower parts of the Otter Sandstone Formation correspond to the early and mid Anisian, and the upper parts, which contain the majority of the macrofossils correlate with late Anisian and latest Anisian magnetozones on the marine standard."
• formation-level stratigraphic resolution
Environment/lithology: fluvial; sandstone
Size class: macrofossils
Collected by Mark Hounslow in 1999
Collection methods: quarrying
Primary reference: D. W. E. Hone and M. J. Benton. 2008. A New Genus of Rhynchosaur from the Middle Triassic of South-West England. Palaeontology 51(1):95-115 [J. Mueller/T. Liebrecht/T. Liebrecht]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 88974: authorized by Richard Butler, entered by Richard Butler on 27.04.2009
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
Bentonyx sidensis n. gen. n. sp.
Bentonyx sidensis n. gen. n. sp. Langer et al. 2010 rhynchosaur BRSUG 27200, nearly complete articulated skull
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