Adamantina Formation
Adamantina Formation | |
---|---|
Stratigraphic range: Late Coniacian-Early Maastrichtian | |
Type | Geological formation |
Unit of | Bauru Group |
Underlies | Uberaba Formation |
Overlies | Santo Anastacio, Caiuá & Araçatuba Formations |
Lithology | |
Primary | Sandstone, calcrete |
Other | Mudstone, siltstone, conglomerate, coal |
Location | |
Coordinates | 21°36′S 50°06′W / 21.6°S 50.1°W |
Approximate paleocoordinates | 25°48′S 33°06′W / 25.8°S 33.1°W |
Region | São Paulo |
Country | Brazil |
Extent | Bauru Basin, Paraná Basin |
Type section | |
Named for | Adamantina |
The Adamantina Formation is a geological formation in the Bauru Basin of western São Paulo state, in southeastern Brazil.
Its strata date back to the Late Cretaceous epoch of the Cretaceous Period, during the Mesozoic Era. The formation is part of the Bauru Group in the northeastern Paraná Basin.
Geology
[edit]Dinosaur remains are among the fossils that have been recovered from the Adamantina Formation.[1] According to some 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, other studies have found a much younger age - Campanian to Maastrichtian (83.5-66 million years ago) of the late Cretaceous.[6][7]
More recent studies lean into the latter category[8] and an unpublished article abstract revealed at the Society of Vertebrate Paleontology in 2017 also argues that the Allen Formation, Loncoche, and Los Alamitos Formation are all contemporaries and are no later than 72.1Ma in age.[9] A zircon was found dating to 87.8 Ma, so this represents a maximum age.[10]
Geological setting
[edit]During the Early Jurassic, the supercontinent Pangea started to drift apart due to the breakup of Gondwana and Laurasia.[11] 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.[12] 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.[12]
The Bauru Basin is a trough that, as Miall (1990) argues,[13] evolved due to “thermo-mechanical subsidence” during the Late Cretaceous, probably due to the breakup of Africa and India.[11] The sediments reach a thickness of up to ~300 m and consist mainly of siliciclastic sediments.[14] The Bauru Group can be subdivided into five different formations [12][15][16][17] 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.[12]
Vertebrate paleofauna
[edit]Crocodylomorphs
[edit]Color key
|
Notes Uncertain or tentative taxa are in small text; |
Crocodylomorphs of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Adamantinasuchus[18] | A. navae | Six specimens and several isolated bone remains. | A zhiphosuchian notosuhian | |||
Aphaurosuchus[19] | A. kaiju | Skull elements and teeth. | A baurusuchine baurusuchid | |||
Armadillosuchus[20] | A. arrudai | A ziphosuchian notosuchian | ||||
Barreirosuchus[21] | B. franciscoi | A peirosaurid notosuchia | ||||
Baurusuchus | B. albertoi[7] | A baurusuchine baurusuchid | ||||
B. pachechoi[22] | A baurusuchine baurusuchid | |||||
B. salgadoensis[22] | A baurusuchine baurusuchid | |||||
Brasileosaurus[22] | B. pachecoi[22] | A notosuchid notosuchian | ||||
Campinasuchus[5] | C. dinizi | A pissarrachampsine baurusuchid | ||||
Caipirasuchus[23] | C. catanduvensis[24] | A sphagesaurid notosuchian | ||||
C. paulistanus | A sphgesaurid notosuchian | |||||
Caryonosuchus[25] | C. pricei | A sphagesaurid notosuchian | ||||
Epoidesuchus[26] | E. tavaresae. | A peirosaurid notosuchian | ||||
Mariliasuchus | M. amarali[22] | Very common. Several specimens - juvenile and adults – with skulls articulated to skeletons, and many isolated materials. Eggs clutches, eggshells, and coprolites were found also. | A notosuchid notosuchian | |||
M. robustus[27] | A notosuchid notosuchian | |||||
Montealtosuchus[28] | M. arrudacamposi | A peirosaurid notosuchian | ||||
Morrinhosuchus[29] | M. luziae | A sphagesaurid notosuchian | ||||
Roxochampsa[30] | R. paulistanus | Several teeth, splenials, and dentaries. | A peirosaurid notosuchian | |||
Sphagesaurus | S. huenei[22] | A sphagesaurid notosuchian | ||||
S. montealtensis[6] | A sphagesaurid notosuchian | |||||
Stratiotosuchus[18] | S. maxhechti | A baurusuchine baurusuchid |
Dinosaurs
[edit]Indeterminate dinosaur remains are known from the formation.[31]
Sauropods
[edit]Sauropods of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
A. mezzalirai |
A lithostrotian titanosaurian | |||||
Arrudatitan[33] | A. maximus | A single partially articulated skeleton. | A aeolosaurin titanosaurian | |||
Antarctosaurus | A. brasiliensis | Postcranial remains.[34] | A colossosaurian titanosaurian | |||
Brasilotitan | B. nemophagus | Raposo Tavares. | A partial skeleton and dentition. | A lithostrotian titanosaurian | ||
Gondwanatitan | G. faustoi | Partial postcranial skeleton.[35] | A lithostrotian titanosaurian | |||
Maxakalisaurus[36] | M. topai | A fragmentary right maxilla with teeth, twelve cervical vertebrae and some cervical ribs, seven dorsal vertebrae and some dorsal ribs, a neural spine and centrum from the sacrum, six caudal vertebrae, some haemal arches, pieces of the scapulae, both sternal plates, part of the left ischium, both humeri, two metacarpals, part of the fibula, an osteoderm, and some unidentified piece | A lithostrotian titanosaurian |
Theropods
[edit]Theropods of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Abelisauridae Indet.[37] | Indeterminate | Fragment of right premaxilla and a tooth | ||||
Enantiornithes indet.[38] |
Indeterminate |
Near complete jaws and skulls | ||||
Navaornis[39] | N. hesitate | Complete skull and well preserved skeleton | A enantiornithine bird | |||
Unenlagiinae indet.[40] | Indeterminate | A single dorsal vertebra |
Squamates
[edit]Squamates of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Boipeba | B. tayasuensis | A single precloacal vertebra | A large, primitive blind snake |
Amphibians
[edit]Amphibians of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Baurubatrachus | B. santosdoroi | Near Catanduva city, São Paulo.[41] | Remains of two individuals.[41] | A frog. | ||
Mariliabatrachus[42] | M. navai | A frog. |
Turtles
[edit]Turtle of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Yuraramirim[43] | Y. montealtensis | A peiropemydid turtle |
Fish
[edit]Fishes of the Adamantina Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Lepisosteus | L. cominatoi | A gar |
Mammals
[edit]Eutheria incertae sedis, Brasilestes (tribosphenida incertae sedis),[44] gondwanatheres and meridiolestidans.[45]
See also
[edit]- Geologic formations of Brazil
- List of dinosaur-bearing rock formations
- Paleontological sites of Brazil
- Asencio Formation
References
[edit]- ^ 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.
- ^ Turner, A.H.; Calvo, J.O. (2005). "A new sebecosuchian crocodyliform from the Late Cretaceous of Patagonia". Journal of Vertebrate Paleontology. 25 (1): 87–98. doi:10.1671/0272-4634(2005)025[0087:ANSCFT]2.0.CO;2. S2CID 86257810.
- ^ Nava, William R.; Agustín G. Martinelli (2011). "A new squamate lizard from the Upper Cretaceous Adamantina Formation (Bauru Group), São Paulo State, Brazil" (PDF). Anais da Academia Brasileira de Ciências. 83 (1): 291–299. doi:10.1590/S0001-37652011000100017. ISSN 0001-3765. PMID 21437386.
- ^ Turner, A.H.; Sertich, J.W. (2010). "Phylogenetic history of Simosuchus clarki (Crocodyliformes: Notosuchia) from the Late Cretaceous of Madagascar". Journal of Vertebrate Paleontology. 30 (6, Memoir 10): 177–236. Bibcode:2010JVPal..30S.177T. doi:10.1080/02724634.2010.532348. S2CID 86737170.
- ^ a b Ismar De Souza Carvalho; Vicente De Paula Antunes Teixeira; Mara Lúcia Da Fonseca Ferraz; et al. (2011). "Campinasuchus dinizi gen. et sp. nov., a new Late Cretaceous baurusuchid (Crocodyliformes) from the Bauru Basin, Brazil" (PDF). Zootaxa. 2871: 19–42. doi:10.11646/zootaxa.2871.1.2.
- ^ a b Marco Brandalise de Andrade; Reinaldo J. Bertini (2008). "A new Sphagesaurus (Mesoeucrocodylia: Notosuchia) from the Upper Cretaceous of Monte Alto City (Bauru Group, Brazil), and a revision of the Sphagesauridae". Historical Biology. 20 (2): 101–136. Bibcode:2008HBio...20..101B. doi:10.1080/08912960701642949. S2CID 84879725.
- ^ a b Paulo Miranda Nascimento; Hussam Zaher (2010). "A new species of Baurusuchus (Crocodyliformes, Mesoeucrocodylia) from the Upper Cretaceous of Brazil, with the first complete postcranial skeleton described from the family Baurusuchidae" (PDF). Papéis Avulsos de Zoologia. 50 (21): 323‑361. doi:10.1590/s0031-10492010002100001.
- ^ Brusatte, Stephen L.; Candiero, Carolos R.A.; Simbras, Felipe M. (2017). "The Last Dinosaurs of Brazil: The Bauru Group and its implications for the end of the Cretaceous mass extinction". Anias de Academia Brasileira de Ceincias. 89 (3): 1465–1485. doi:10.1590/0001-3765201720160918. PMID 28954171.
- ^ "AGE OF THE ADAMANTINA FORMATION, UPPER BAURU GROUP, LATE CRETACEOUS, BRAZIL". Archived from the original on 2017-11-07. Retrieved 2017-11-03.
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- ^ a b Nobre, Pedro Henrique; Carvalho, Ismar de Souza (2006). "Adamantinasuchus navae: A new Gondwanan Crocodylomorpha (Mesoeucrocodylia) from the Late Cretaceous of Brazil" (PDF). Gondwana Research. 10 (3–4): 370–378. Bibcode:2006GondR..10..370N. doi:10.1016/j.gr.2006.05.008. Archived from the original (PDF) on 2011-07-06.
- ^ Martins, Kawan Carvalho; Queiroz, Marcos Vinicius; Ruiz, Juan Vítor; Langer, Max Cardoso; Montefeltro, Felipe Chinaglia (2023-08-25). "A new Baurusuchidae (Notosuchia, Crocodyliformes) from the Adamantina Formation (Bauru Group, Upper Cretaceous), with a revised phylogenetic analysis of Baurusuchia". Cretaceous Research. 153: 105680. doi:10.1016/j.cretres.2023.105680. ISSN 0195-6671.
- ^ Marinho, Thiago S.; Carvalho, Ismar S. (2009). "An armadillo-like sphagesaurid crocodyliform from the Late Cretaceous of Brazil". Journal of South American Earth Sciences. 27 (1): 36–41. Bibcode:2009JSAES..27...36M. doi:10.1016/j.jsames.2008.11.005.
- ^ Fabiano Vidoi Iori; Karina Lucia Garcia (2012). "Barreirosuchus franciscoi, um novo Crocodylomorpha Trematochampsidae da Bacia Bauru, Brasil". Revista Brasileira de Geociências. 42 (2): 397–410. doi:10.5327/z0375-75362012000200013 (inactive 1 November 2024).
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: CS1 maint: DOI inactive as of November 2024 (link)[permanent dead link ] - ^ a b c d e f Carvalho, Ismar de Souza; Campos, Antonio de Celso Arruda; Nobre, Pedro Henrique (2005). "Baurusuchus salgadoensis, a new Crocodylomorpha from the Bauru Basin (Cretaceous), Brazil" (PDF). Gondwana Research. 8 (1): 11–30. Bibcode:2005GondR...8...11C. doi:10.1016/S1342-937X(05)70259-8. Archived from the original (PDF) on 2010-09-21.
- ^ Fabiano V. Iori; Ismar S. Carvalho (2011). "Caipirasuchus paulistanus, a new sphagesaurid (Crocodylomorpha, Mesoeucrocodylia) from the Adamantina Formation (Upper Cretaceous, Turonian–Santonian), Bauru Basin, Brazil". Journal of Vertebrate Paleontology. 31 (6): 1255–1264. Bibcode:2011JVPal..31.1255I. doi:10.1080/02724634.2011.602777. S2CID 128482509.
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- ^ Alexander W. A. Kellner; Diogenes A. Campos; Douglas Riff; Marco Brandalise de Andrade (2011). "A new crocodylomorph (Sphagesauridae, Notosuchia) with horn-like tubercles from Brazil". Zoological Journal of the Linnean Society. 163 (s1): S57–S65. doi:10.1111/j.1096-3642.2011.00712.x.
- ^ Ruiz, Juan V.; Queiroz, Marcos V. L.; Martins, Kawan C.; Godoy, Pedro L.; Iori, Fabiano V.; Langer, Max C.; Montefeltro, Felipe C.; Bronzati, Mario (2024-08-29). "A new Peirosauridae (Crocodyliformes, Notosuchia) from the Adamantina Formation (Bauru Group, Late Cretaceous), with a revised phylogenetic analysis of Sebecia". The Anatomical Record. doi:10.1002/ar.25559. PMID 39210546.
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- ^ Iori, F.V.; Carvalho, I.S. (2009). "Morrinhosuchus luziae, um novo Crocodylomorpha Notosuchia da Bacia Bauru, Brasil". Revista Brasileira de Geociências. 39 (4): 717–725. doi:10.25249/0375-7536.2009394717725 (inactive 1 November 2024).
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- ^ Gabriel S. Ferreira; Fabiano V. Iori; Guilherme Hermanson; Max C. Langer (2018). "New turtle remains from the Late Cretaceous of Monte Alto-SP, Brazil, including cranial osteology, neuroanatomy and phylogenetic position of a new taxon". PalZ. 92 (3): 481–498. Bibcode:2018PalZ...92..481F. doi:10.1007/s12542-017-0397-x. S2CID 134701879.
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- Adamantina Formation
- Geologic formations of Brazil
- Cretaceous Brazil
- Sandstone formations
- Mudstone formations
- Siltstone formations
- Conglomerate formations
- Coal formations
- Coal in Brazil
- Alluvial deposits
- Fluvial deposits
- Lacustrine deposits
- Aeolian deposits
- Cretaceous paleontological sites of South America
- Paleontology in Brazil
- Environment of São Paulo (state)
- Landforms of São Paulo (state)