Also known as Cantera Bidegain
Where: Tacuarembó, Uruguay (31.7° S, 56.0° W: paleocoordinates 29.0° S, 20.0° W)
• coordinate stated in text
• outcrop-level geographic resolution
When: Batoví Member (Tacuarembó Formation), Kimmeridgian to Kimmeridgian (157.3 - 145.0 Ma)
• bed-level stratigraphic resolution
Environment/lithology: fluvial; fine-grained, quartzose, silty sandstone and massive, medium-grained, brown, green sandstone
•extensive stratum of silty sandstones"; "massive, medium-grained, greenish brown sandstones" / "fine graided, quartzose, silty sandstones"
Size classes: macrofossils, mesofossils
Collected by M. Soto, D. Perea
Collection methods: quarrying, surface (in situ),
Primary reference: M. Soto, M. S. S. de Carvalho, J. G. Maisey, D. Perea, and J. Da Silva. 2012. Coelacanth remains from the Late Jurassic–?earliest Cretaceous of Uruguay: the southernmost occurrence of the Mawsoniidae. Journal of Vertebrate Paleontology 32(3):530-537 [M. Carrano/M. Carrano]more details
Purpose of describing collection: general faunal/floral analysis
PaleoDB collection 213192: authorized by Oliver Rauhut, entered by Oliver Rauhut on 27.08.2020, edited by Matthew Carrano and Grace Varnham
Creative Commons license: CC BY (attribution)
Taxonomic list
Osteichthyes | |
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Coelacanthimorpha | |
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Reptilia | |
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Torvosaurus sp.2 Galton and Jensen 1979 tetanuran theropod six teeth; FC-DPV 2343, FC-DPV 2971, FC-DPV 2972, MGT-1139, MGT-1184, MGT-1204
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