Higher Level - east of Scarritt Pocket: Deseadan, Argentina
Country: | Argentina |
State/province: | Chubut |
Coordinates: |
44.7° South, 68.4° West (view map) |
Paleocoordinates: | 44.3° South, 63.8° West (Wright 2013) |
Basis of coordinate: | based on nearby landmark |
Geographic resolution: | small collection |
|
10 m.y. bin: | Cenozoic 4-5 |
Key time interval: | Deseadan |
Age range of interval: | 28.9 - 20.9 m.y. ago |
Formation: | Sarmiento |
Stratigraphic resolution: | group of beds |
Stratigraphy comments: Higher than Crater Lake beds
Eocene–Oligocene ‘Tobas del Sarmiento’, Sarmiento Group or Sarmiento Formation (Feruglio 1949; Andreis et al. 1975; Spalletti & Mazzoni 1977, 1979; Reguero & Escribano 1996). Regarding the age of Sarmiento formation, absolute dates are lacking for Cabeza Blanca, but Deseadan levels have been dated in other localities such as Salla, Bolivia (29.4–25.65 Ma), Moquegua, Peru (26.25 Ma), and Chubut, Argentina, Gran Barranca (29.4–24.2 Ma) and Scarritt Pocket (27.17 Ma) (Dunn et al. 2013 and references therein; Vucetich et al. 2014). |
Primary lithology: | not reported |
Environment: | terrestrial indet. |
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods: | field collection |
Reason for describing collection: | taxonomic analysis |
Database number: | 49852 |
Authorizer: | J. Alroy, J. Zijlstra |
Enterer: | J. Wertheim, J. Zijlstra |
Modifier: | M. Kouvari |
Research group: | vertebrate |
Created: | 2005-04-28 10:49:41 |
Last modified: | 2025-02-22 15:12:02 |
Access level: | the public |
Released: | 2005-04-28 10:49:41 |
Creative Commons license: | CC0 |
13361. | | R.G. Chaffee. 1952. The Deseadan vertebrate fauna of the Scarritt Pocket, Patagonia. Bulletin of the American Museum of Natural History 98:505-562 [J. Alroy/J. Wertheim/J. Wertheim] |
13081 | | L. G. Marshall, R. L. Cifelli, R. E. Drake and G. H. Curtis. 1986. Vertebrate paleontology, geology, and geochronology of the Tapera de López and Scarritt Pocket, Chubut Province, Argentina. Journal of Paleontology 60(4):920-951 [D. Croft/D. Croft/D. Croft] |