Colonia Orozco: Late/Upper Triassic, Uruguay

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
Varanopidae indet. (Romer and Price 1940)
6 elements
FC-DPV 1182, 1183, 1189, 1199, 1200, 1333 (all are vertebral elements)
    = ? Diapsida indet.
Dias-da-Silva et al. 2006
aff. Sphenacodontidae indet. Marsh 1878
1 individual
FC-DPV 1194 (vertebra)
    = ? Diapsida indet.
Dias-da-Silva et al. 2006
Reptilia
Archosauromorpha indet. (Huene 1946)
Ezcurra et al. 2015 4 specimens
FC-DPV 2641: co-ossified basioccipital and exoccipitals; FC-DPV 2640: anterior cervical vertebra; FC-DPV 2639: middle or posterior cervical vertebra; FC-DPV 2637: middle or posterior cervical vertebra
Pintosaurus magnidentis n. gen., n. sp. Pineiro et al. 2004
Pineiro et al. 2004 1 individual
FC-DPV 1181 (type, partial skull)
Amphibia - Temnospondyli
Dvinosauria indet. Warren 1998
Pineiro et al. 2007 1 individual
FC-DPV 285 (partial skull)
Amphibia - Temnospondyli - Laidleriidae
Uruyiella liminea n. gen., n. sp. Pineiro et al. 2007
Pineiro et al. 2007 1 individual
FC-DPV 1598 (type, partial skull)
Amphibia - Temnospondyli - Mastodonsauridae
Mastodonsauridae indet. Lydekker 1885
Pineiro et al. 2007 3 specimens
FC-DPV 1280, 1305, 1600 (all are partial mandibles)
Amphibia - Temnospondyli
Arachana nigra n. gen., n. sp. Pineiro et al. 2012
Pineiro et al. 2012 1 individual
FC-DPV 1369
see common names

Geography
Country:Uruguay State/province:Cerro Largo
Coordinates: 32.3° South, 54.1° West (view map)
Paleocoordinates:40.2° South, 15.7° West
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period:Triassic Epoch:Late/Upper Triassic
10 m.y. bin:Triassic 3-4
Key time interval:Late/Upper Triassic
Age range of interval:237.00000 - 201.40000 m.y. ago
Stratigraphy
Formation:Buena Vista
Stratigraphic resolution:member
Stratigraphy comments: The fossils of the collection are distributed within an interval of about 20 m. (see measured section in text-fig. in Pineiro et al., 2007).

Although arguments have been made for a Permian age for this locality, an Early Triassic date seems more likely (see discussion in Dias-da-Silva et al. 2006).
Lithology and environment
Primary lithology:red or brown muddy,sandy "siliciclastic"
Secondary lithology:intraclastic conglomerate
Includes fossils?Y
Lithology description: "Buena Vista Formation is characterized by reddish fine sandstone interbedded with lenticular clay layers and intraformational conglomerates [...] The fossils described in this paper were recovered from the conglomerates in the middle part of the Buena Vista Formation." (Pineiro et al., 2003)
Environment:fluvial indet.
Geology comments: "The paleoenvironment is related to the final withdrawal of the sea, and the upper part of this section is characterized by continental and strong fluvial influences." (Pineiro et al., 2003)
"there is a general consensus among authors about the fluvial environmental characterization of the Buena Vista Formation" (Pineiro et al., 2007)
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Preservation of anatomical detail:medium
Articulated whole bodies:none
Associated major elements:some
Disassociated major elements:some
Temporal resolution:snapshot
Collection methods and comments
Reason for describing collection:taxonomic analysis
Collection method comments: FC-DPV = Departamento de Paleontologia, Facultad de Ciencias, Montevideo, Uruguay
Metadata
Also known as:Cerro Largo Localities
Database number:86401
Authorizer:J. Mueller, R. Butler, G. Lloyd Enterer:T. Liebrecht, R. Butler, G. Lloyd
Modifier:R. Butler Research group:vertebrate
Created:2009-02-01 17:03:37 Last modified:2017-12-04 16:58:06
Access level:the public Released:2009-02-01 17:03:37
Creative Commons license:CC BY
Reference information

Primary reference:

29107. G. Pineiro, M. Verde, M. Ubilla and J. Ferigolo. 2003. First Basal Synapsids (“Pelycosaurs”) from the Upper Permian - ?Lower Triassic of Uruguay. Journal of Paleontology 77(2):389-392 [J. Mueller/T. Liebrecht]

Secondary references:

31842 S. Dias-da-Silva, S. Modesto, and C. L. Schultz. 2006. New Material of Procolophon (Parareptilia: Procolophonoidea) from the Lower Triassic of Brazil, with remarks on the ages of the Sanga do Cabral and Buena Vista formations of South America. Canadian Journal of Earth Sciences 43(11):1685-1693 [J. Mueller/T. Liebrecht]
64011 M. D. Ezcurra, P. Velozo, M. Meneghel and G. Pineiro. 2015. Early archosauromorph remains from the Permo-Triassic Buena Vista Formation of north-eastern Uruguay. PeerJ 3:e776 [R. Butler/R. Butler]
29121 G. Pineiro, C. Marsicano, C. Goso and E. Morosi. 2007. Temnospondyl diversity of the Permian-Triassic Colonia Orozco Local Fauna (Buena Vista Formation) of Uruguay. Revista Brasileira de Paleontologia 10(3):169-180 [J. Mueller/T. Liebrecht/M. Carrano]
65041 G. Pineiro, A. Ramos, and C. Marsicano. 2012. A rhinesuchid-like temnospondyl from the Permo-Triassic of Uruguay. Comptes Rendus Palevol 11:65-78 [G. Lloyd/G. Lloyd]
29120 G. Pineiro, A. Rojas, and M. Ubilla. 2004. A new procolophonoid (Reptilia, Parareptilia) from the Upper Permian of Uruguay. Journal of Vertebrate Paleontology 24(4):814-821 [J. Mueller/T. Liebrecht]