Quebrada del Barro Formation: Difference between revisions
Appearance
Content deleted Content added
Tisquesusa (talk | contribs) |
Tisquesusa (talk | contribs) No edit summary |
||
Line 16: | Line 16: | ||
| unitof = [[Marayes Group]] |
| unitof = [[Marayes Group]] |
||
| subunits = |
| subunits = |
||
| underlies = |
| underlies = [[Los Riscos Formation]] |
||
| overlies = |
| overlies = [[Carrizal Formation]] |
||
| thickness = |
| thickness = |
||
| extent = [[Marayes-El Carrizal Basin]] |
| extent = [[Marayes-El Carrizal Basin]] |
||
Line 35: | Line 35: | ||
| map_caption = |
| map_caption = |
||
}} |
}} |
||
The '''Quebrada del Barro Formation''' is a geological [[Formation (geology)|formation]] in [[San Juan Province, Argentina|San Juan Province]], [[Argentina]]. |
The '''Quebrada del Barro Formation''' is a geological [[Formation (geology)|formation]] of the [[Marayes-El Carrizal Basin]] in [[San Juan Province, Argentina|San Juan Province]], [[Argentina]]. The formation underlies the [[Los Riscos Formation]] and overlies the [[Carrizal Formation]].<ref name=Gardini2009_p554>Gardini et al., 2009, p.554</ref> |
||
Its fossils date back to the [[Late Triassic]] epoch of the [[Triassic]] period.<ref name="triassicdistribution">Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Triassic, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 527–528. {{ISBN|0-520-24209-2}}.</ref> Part of the formation may be made into a provincial park following the discovery of the fossils of ''[[Ingentia]]'', a giant dinosaur.<ref>{{Cite news|url=http://naaju.com/argentina/uac-wants-a-provincial-park-in-the-cradle-of-ingenia-prima/|title=Uac wants a provincial park in the cradle of Ingenia Prima |work=Naaju|access-date=2018-07-15|language=en-US}}</ref> |
Its fossils date back to the [[Late Triassic]] epoch of the [[Triassic]] period.<ref name="triassicdistribution">Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Triassic, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 527–528. {{ISBN|0-520-24209-2}}.</ref> Part of the formation may be made into a provincial park following the discovery of the fossils of ''[[Ingentia]]'', a giant dinosaur.<ref>{{Cite news|url=http://naaju.com/argentina/uac-wants-a-provincial-park-in-the-cradle-of-ingenia-prima/|title=Uac wants a provincial park in the cradle of Ingenia Prima |work=Naaju|access-date=2018-07-15|language=en-US}}</ref> |
||
Line 134: | Line 134: | ||
{{portal|Geology|Argentina|Triassic|Prehistory of South America}} |
{{portal|Geology|Argentina|Triassic|Prehistory of South America}} |
||
{{reflist}} |
{{reflist}} |
||
=== Bibliography === |
|||
* {{cite LSA |last=Gardini |first=Carlos |last2=Rivarola |first2=David |last3=Agüera |first3=Maximiliano |last4=Candela |first4=Gerónimo |year=2009 |title=Estructura de la región Sierra de Guayaguas-Marayes, Provincias de San Juan y San Luis |url=http://www.scielo.org.ar/pdf/raga/v65n3/v65n3a12.pdf |journal=[[Revista de la Asociación Geológica Argentina]] |volume=65 |pages=551–565 |accessdate=2018-09-08}} |
|||
[[Category:Geologic formations of Argentina]] |
[[Category:Geologic formations of Argentina]] |
Revision as of 18:18, 23 February 2019
Quebrada del Barro Formation | |
---|---|
Stratigraphic range: Norian | |
Type | Geological formation |
Unit of | Marayes Group |
Underlies | Los Riscos Formation |
Overlies | Carrizal Formation |
Lithology | |
Primary | Sandstone |
Other | Siltstone |
Location | |
Coordinates | 31°54′S 67°12′W / 31.9°S 67.2°W |
Approximate paleocoordinates | 40°48′S 30°00′W / 40.8°S 30.0°W |
Region | San Juan Province |
Country | Argentina |
Extent | Marayes-El Carrizal Basin |
The Quebrada del Barro Formation is a geological formation of the Marayes-El Carrizal Basin in San Juan Province, Argentina. The formation underlies the Los Riscos Formation and overlies the Carrizal Formation.[1]
Its fossils date back to the Late Triassic epoch of the Triassic period.[2] Part of the formation may be made into a provincial park following the discovery of the fossils of Ingentia, a giant dinosaur.[3]
Fossil content
Dinosaurs
Theropods of the Quebrada del Barro Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Material | Notes | Images | ||
Lucianovenator[4] | L. bonoi | "Cervical vertebrae, a sacrum and a partial pelvis" | A coelophysid theropod | |||
Leyesaurus | L. marayensis |
Sauropodomorphs of the Quebrada del Barro Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Material | Notes | Images | ||
I. prima |
"cervical and dorsal vertebrae, scapula" |
|||||
Riojasaurus[6] | R. incertus | "a skull, leg bones, vertebrae" | A riojasaurid sauropodomorph |
Dinosauromorphs
Dinosauromorphs of the Quebrada del Barro Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Material | Notes | Images | ||
Dromomeron[7] | D. gigas | a lagerpetid dinosauromorph |
Rhynchocephalians
Rhynchocephalians of the Quebrada del Barro Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Material | Notes | Images | ||
Sphenotitan[8] | S. leyesi | "skull, maxilla, dorsal vertebrae, sacral vertebrae, caudal vertebra" | a opisthodont sphenodontian |
References
- ^ Gardini et al., 2009, p.554
- ^ Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Triassic, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 527–528. ISBN 0-520-24209-2.
- ^ "Uac wants a provincial park in the cradle of Ingenia Prima". Naaju. Retrieved 2018-07-15.
- ^ Ricardo N. Martínez; Cecilia Apaldetti (2017). "A late Norian-Rhaetian coelophysid neotheropod (Dinosauria, Saurischia) from the Quebrada del Barro Formation, northwestern Argentina". Ameghiniana. in press. doi:10.5710/AMGH.09.04.2017.3065.
- ^ Apaldetti; Martínez, Ricardo N.; Cerda, Ignatio A.; Pol, Diego; Alcober, Oscar (2018). "An early trend towards gigantism in Triassic sauropodomorph dinosaurs". Nature Ecology & Evolution. 2 (8): 1227–1232. doi:10.1038/s41559-018-0599-y. PMID 29988169.
- ^ "Riojasaurus." In: Dodson, Peter & Britt, Brooks & Carpenter, Kenneth & Forster, Catherine A. & Gillette, David D. & Norell, Mark A. & Olshevsky, George & Parrish, J. Michael & Weishampel, David B. The Age of Dinosaurs. Publications International, LTD. p. 41. ISBN 0-7853-0443-6.
- ^ Ricardo N. Martínez; Cecilia Apaldetti; Gustavo A. Correa; Diego Abelín (2016). "A Norian lagerpetid dinosauromorph from the Quebrada del Barro Formation, northwestern Argentina". Ameghiniana. 53 (1): 1–13. doi:10.5710/AMGH.21.06.2015.2894.
- ^ Martinez, R. N.; Apaldetti, C.; Colombi, C. E.; Praderio, A.; Fernandez, E.; Malnis, P. S.; Correa, G. A.; Abelin, D.; Alcober, O. (2013). "A new sphenodontian (Lepidosauria: Rhynchocephalia) from the Late Triassic of Argentina and the early origin of the herbivore opisthodontians". Proceedings of the Royal Society B: Biological Sciences. 280 (1772): 20132057. doi:10.1098/rspb.2013.2057. PMC 3813332. PMID 24132307.