Spynie main quarry (quarry 3), near Elgin: Carnian - Norian, United Kingdom
collected by Newton, Westoll

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
Ornithosuchus woodwardi n. gen., n. sp. Newton 1894
3 individuals
BMNH R2409/2410 (holotype), skull and postcranial skeleton; BMNH R8170, dorsal vertebrae and pectoral/forelimb elements; GSM 91072-78, 91080-81, 91085-65, series of vertebrae, scutes, forelimb, femora
Hyperodapedon gordoni Huxley 1859
Benton and Spencer 1995 2 individuals
NMS specimens - two skulls. These specimens were formerly listed as held in the Newcastle University collections
see common names

Geography
Country:United Kingdom State/province:Scotland County:Moray
Coordinates: 57.7° North, 3.3° West (view map)
Paleocoordinates:34.0° North, 0.8° West
Basis of coordinate:stated in text
Geographic resolution:outcrop
Time
Period:Triassic Epoch:Late/Upper Triassic
Key time interval:Carnian - Norian
Age range of interval:237.00000 - 208.50000 m.y. ago
Stratigraphy
Formation:Lossiemouth Sandstone
Stratigraphic resolution:group of beds
Stratigraphy comments: Age of the Lossiemouth Sandstone Formation is based upon vertebrate biostratigraphy, with comparisons made to the faunal assemblages from the lower part of the Maleri Formation (India), the upper part of the Santa Maria Formation (Brazil) and the Ischigualasto Formation (Argentina). This is suggestive of a late Carnian to early Norian age (Benton & Walker 2011).
Lithology and environment
Primary lithology:gray lithified calcareous sandstone
Includes fossils?Y
Lithology description: "In the main quarry, 20 m faces may be seen displaying grey jointed sandstone, highly silaceous at the top and more calcareous lower down, weathering orange." General description of Lossiemouth Sandstones: "The Lossiemouth Sandstones are white, buff, yellow, or pinkish. Grain size is usually uniform with grains well-rounded. The rock is composed of quartz, feldspar, and rare brownish chert and quartzite. Cements are usually overgrowths of secondary quartz and feldspar, but calcite and fluorspar may also occur. The sandstones may be finely laminated, but more usually they show large-scale cross-beds on well-weathered surfaces. These features, as well as the absence of pebbles, the rarity of micas and heavy minerals, strongly suggest aeolian deposition".
Environment:dune
Geology comments: "Foreset analysis indicates a prevailing south-westerly wind forming barchan dunes. Dunes up to 20 m high migrated across the flood plain during arid intervals"
Taphonomy
Modes of preservation:body,mold/impression
Size of fossils:macrofossils
Preservation of anatomical detail:good
Articulated whole bodies:some
Associated major elements:some
Fragmentation:occasional
Spatial resolution:parautochthonous
Collection methods and comments
Reason for describing collection:taxonomic analysis
Collectors:Newton, Westoll
Metadata
Also known as:Ornithosuchus holotype site
Database number:89008
Authorizer:R. Butler Enterer:R. Butler
Modifier:M. Carrano Research group:vertebrate
Created:2009-04-28 06:55:51 Last modified:2015-06-29 11:35:15
Access level:the public Released:2009-04-28 06:55:51
Creative Commons license:CC BY
Reference information

Primary reference:

9482. E. T. Newton. 1894. Reptiles from the Elgin Sandstone. — Description of two new genera. Philosophical Transactions of the Royal Society of London B 185:573-607 [M. Carrano/M. Carrano/M. Carrano]

Secondary references:

29844 M. J. Benton. 1983. The Triassic reptile Hyperodapedon from Elgin: functional morphology and relationships. Philosophical Transactions of the Royal Society of London, Series B 302:605-720 [R. Butler/R. Butler]
15587ETE M. J. Benton and P. S. Spencer. 1995. Fossil Reptiles of Great Britain. Chapman & Hall, London 1-386 [M. Carrano/K. Maguire/J. Tennant]
29840 M. J. Benton and A. D. Walker. 1985. Palaeoecology, taphonomy, and dating of Permo-Triassic reptiles from Elgin, north-east Scotland. Palaeontology 28:207-234 [R. Butler/R. Butler]
51970 E. T. Newton. 1905. Notes on the Triassic fossils (excluding Rhaetic) in the Museum of the Geological Survey at Jermyn Street, London. Report of the British Association for the Advancement of Science 1904:282-285 [M. Carrano/M. Carrano]
55639 R. L. Paton. 1975. A Catalogue of Fossil Vertebrates in the Royal Scottish Museum, Edinburgh. Part Four / Amphibia & Reptilia. Royal Scottish Museum Information Series. Geology 5 1-38 [M. Carrano/M. Carrano]
13771ETE A. D. Walker. 1964. Triassic reptiles from the Elgin area: Ornithosuchus and the origin of carnosaurs. Philosophical Transactions of the Royal Society of London, Series B, Biological Sciences 248:53-134 [M. Carrano/M. Carrano/M. Carrano]