Candelária Formation, Paraná Basin

Coordinates: 29°36′S 53°30′W / 29.6°S 53.5°W / -29.6; -53.5
Source: Wikipedia, the free encyclopedia.
Candelária Formation
Ma
Approximate paleocoordinates
42°24′S 14°42′W / 42.4°S 14.7°W / -42.4; -14.7
RegionRio Grande do Sul
CountryBrazil
ExtentParaná Basin
Type section
Named forCandelária

The Candelária Formation, in other literature also referred to as Candelária Sequence,

Tuvalian
, from 231.4 to approximately 222 Ma.

The Candelária Formation is composed of

therapsids as well as early dinosaurs were found in the formation in the vicinity of Agudo
.

Description

Candelária Sequence in the Paraná Basin

The Candelária Formation or Sequence corresponds to a third-order sequence placed in the Santa Maria Supersequence. The basal portion of the formation consists of a coarsening-upward succession that begins with red

humid climate. The formation contains the Hyperodapedon and Riograndia Assemblage Zones.[6][7]

The red beds are divided into a non-fossiliferous portion at the base, and an upper fossiliferous unit. Coprolites and putative rhizoliths are present. A light-colored cross-bedded sandstone also occurs at the top of the formation and represents a river channel. It is delimited by an erosive contact with the underlying red beds.[5]

The Candelária Formation is considered a local equivalent of the Caturrita Formation,[8] which it partly underlies. It overlies the Santa Maria Formation.[9] The formation is correlated with the Ischigualasto Formation of the Ischigualasto-Villa Unión Basin in northwestern Argentina.[2]

Basin history

Stratigraphic chart of the Paraná Basin, with the Candelária Formation belonging to the Gondwana II Supersequence

The megaregional Paraná Basin, covering an approximate area of 1,500,000 square kilometres (580,000 sq mi) in southeastern South America, was in the late

Karoo Basin in South Africa and the Fremouw Formation of present-day Antarctica.[10]

Fossil content

Limb bone osteohistology of Brasilitherium riograndensis
Ulna osteohistology of Brasilodon quadrangularis

The formation has provided fossils of

therapsids characteristic of the Late Triassic, as well as early dinosaurs.[4]

Group Fossils Assemblage zone Image Notes
Dinosaurs Erythrovenator jacuiensis [11]
Macrocollum itaquii
[12]
Dinosauria indet.
[13]
Archosauromorpha indet. [14]
Therapsids
Brasilitherium riograndensis
Riograndia
Brasilitherium riograndensis
[2]
Brasilodon quadrangularis Riograndia [2]
Botucaraitherium belarminoi Riograndia [15]
Irajatherium hernandezi Riograndia
[2]
Prozostrodon brasiliensis Hyperodapedon
[2][16]
Siriusgnathus niemeyerorum [14]
Probainognathia indet. [14]
Rhynchosaurs Hyperodapedon sp. Hyperodapedon
[7][16]
Rhynchocephalians Lanceirosphenodon ferigoloi Riograndia [17]

See also

References

  1. ^ Müller et al., 2017, p.543
  2. ^ a b c d e f Botha-Brink, 2018, p.7
  3. ^ Martinelli et al., 2017, p.528
  4. ^ a b Candelária Formation at Fossilworks.org
  5. ^ a b Pretto et al., 2015, p.2
  6. ^ Soares et al., 2014, p.1675
  7. ^ a b Pacheco et al., 2017, p.2
  8. ^ Da Rosa & Faccini, 2005, p.21
  9. ^ Da Rosa & Faccini, 2005, p.18
  10. ^ Milani et al., 2007
  11. ^ Rodrigo T. Müller (2020). "A new theropod dinosaur from a peculiar Late Triassic assemblage of southern Brazil". Journal of South American Earth Sciences. in press: Article 103026. doi:10.1016/j.jsames.2020.103026.
  12. PMID 30463923
    .
  13. ^ Müller et al., 2018, p.545
  14. ^ a b c Niemeyer, Agudo at Fossilworks.org
  15. ^ Soares et al., 2014, p.1677
  16. ^ a b Marchezan at Fossilworks.org
  17. ^ Romo de Vivar et al., 2020

Bibliography

Further reading