Adamantina Formation
Adamantina Formation Stratigraphic range: Upper Cretaceous |
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Type | Geological formation |
Location | |
Country | Brazil |
The Adamantina Formation is a geological formation in Brazil whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[1] According to most studies,[2][3][4][5] the Adamantina Formation dates from the Turonian to the Santonian stage (90-83.5 million years ago) of the late Cretaceous, although some studies found much younger age - Campanian to Maastrichtian (83.5-66 million years ago) of the late Cretaceous.[6][7]
Contents
Geological setting
During the Early Jurassic, the supercontinent Pangea started to drift apart due to the breakup of Gondwana and Laurasia.[8] The breakup of Gondwana caused the formation of the large Parana Basin. This basin has a size of ~1,100,000km2 and can be found not only in Brazil but also in Paraguay, Uruguay, and Argentina.[9] The separation of the supercontinent and the breakup of Brazil and Africa was accompanied by volcanism that caused large eruptions of flood basalts. These volcanic rocks formed the Serra Geral Formation which underlies the deposits of the Bauru Group.[9] The Bauru Basin is a trough that, as Miall (1990) argues,[10] evolved due to “thermo-mechanical subsidence” during the Late Cretaceous, probably due to the breakup of Africa and India.[8] The sediments reach a thickness of up to ~300 m and consist mainly of siliciclastic sediments.[11] The Bauru Group can be subdivided into five different formations [9][12][13][14] from bottom to top: Caiua, Santo Anastacio, Adamantina, and Uberaba. Not all formations are equally well represented in the different states and differences occur according their sedimentary composition and therefore also in their naming.[9]
Vertebrate paleofauna
Crurotarsans
Color key
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Notes Uncertain or tentative taxa are in small text; |
Crocodylomorphs of the Adamantina Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
A. navae |
Six specimens and several isolated bone remains. |
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A. arrudai |
A notosuchian |
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B. franciscoi |
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B. albertoi[7] |
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B. pachechoi[18] |
A baurusuchid |
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B. salgadoensis[18] |
A baurusuchid |
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B. pachecoi[18] |
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C. paulistanus |
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C. dinizi |
A baurusuchid |
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C. pricei |
A sphagesaurid |
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G. paulistanus |
Known only from two isolated teeth.[17] |
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M. amarali[18] |
Very common. Several specimens - juvenile and adults – with skull articulated to skeleton, and many isolated materials. Eggs clutches, eggshells and coprolites was found also. |
A notosuchian |
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M. robustus[21] |
A notosuchian |
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M. arrudacamposi |
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M. luziae |
A notosuchian |
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S. huenei[18] |
A sphagesaurid |
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S. montealtensis[6] |
A sphagesaurid |
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S. maxhechti |
A baurusuchid |
Ornithodirans
Indeterminate dinosaur remains are known from the formation.[1]
Dinosaurs of the Adamantina Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Abelisauridae[24] |
Indeterminate |
"fragment of rt. premaxilla and a tooth" |
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A. mezzalirai |
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A. maximus |
"Single partially articulated skeleton." |
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"A." brasiliensis |
"Postcranial remains."[27] |
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G. faustoi |
"Partial postcranial skeleton."[28] |
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M. topai |
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P. nevesi |
5 incomplete teeth, 7 caudal vertebrae, part of right pubis, right tibia, and an articulation of the right fibula |
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Unenlagiinae indet.[30] |
A single dorsal vertebra. |
See also
References
- ↑ 1.0 1.1 Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 600-604. ISBN 0-520-24209-2.
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- ↑ 7.0 7.1 Lua error in package.lua at line 80: module 'strict' not found.
- ↑ 8.0 8.1 Rabassa, J. (2014). Some concepts on Gondwana landscapes: long-term landscape evolution, genesis, distribution and age. In Gondwana Landscapes in southern South America (pp. 9-46). Springer Netherlands.
- ↑ 9.0 9.1 9.2 9.3 Goldberg, K., & Garcia, A. J. (2000). Palaeobiogeography of the Bauru Group, a dinosaur-bearing Cretaceous unit, northeastern Paraná Basin, Brazil. Cretaceous Research, 21(2), 241-254
- ↑ Miall, A. D. (1990). Principles of sedimentary basin analysis (Vol. 633, p. 499). New York: Springer-Verlag.
- ↑ Candeiro, C. R. A., Abranches, C. T., Abrantes, E. A., Avilla, L. D. S., Martins, V. C., Moreira, A. L., ... & Bergqvist, L. P. (2004). Dinosaurs remains from western São Paulo state, Brazil (Bauru Basin, Adamantina Formation, Upper Cretaceous). Journal of South American Earth Sciences, 18(1), 1-10.
- ↑ Soares, P. C., Landim, P. M. B., Fulfaro, V. J., & Neto, A. S. (1980). Ensaio de caracterização estratigráfica do Cretáceo no estado de São Paulo: Grupo Bauru. Revista Brasileira de Geociências, 10(3), 177-185.
- ↑ Souza Jr, J. J. (1984). O Grupo Bauru na porcao mais setentrional da Bacia Sedimentar do Paraná. In 33 Congresso Brasileiro de Geologia, Rio de Janeiro (Vol. 2, pp. 944-957).
- ↑ Dias-Brito, D., Musacchio, E. A., de Castro, J. C., Maranhão, M. S. A. S., Suárez, J. M., & Rodrigues, R. (2001). Grupo Bauru: uma unidade continental do Cretáceo no Brasil-concepções baseadas em dados micropaleontológicos, isotópicos e estratigráficos. Revue de Paléobiologie, 20(1), 245-304.
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- ↑ 18.0 18.1 18.2 18.3 18.4 18.5 18.6 Lua error in package.lua at line 80: module 'strict' not found.
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- ↑ Ariel H. Méndez, Fernando E. Novas & Fabiano V. Iori (2014) New record of abelisauroid theropods from the Bauru Group (Upper Cretaceous), São Paulo State, Brazil. Revista Brasileira de Paleontologia 17(1): 23-32 doi:10.4072/rbp.2014.1.03
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
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- ↑ "Table 13.1," in Weishampel, et al. (2004). Page 270.
- ↑ "Table 13.1," in Weishampel, et al. (2004). Page 269.
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