Anfiteatro de Ticó formation

The Anfiteatro de Ticó is a geological formation from the Deseado Massif Basin in the province of Santa Cruz, Argentina.

Anfiteatro de Ticó Formation
Stratigraphic range: Aptian
~119–116 Ma
TypeGeological formation
Unit ofBaqueró Group
UnderliesBajo Tigre Formation
Lithology
Primarysandstone, Siltstone
OtherConglomerate
Location
Coordinates48.5°S 69.2°W / -48.5; -69.2
Approximate paleocoordinates49.4°S 35.4°W / -49.4; -35.4
RegionSanta Cruz
CountryArgentina
ExtentDeseado Massif Basin
Type section
Named forAnfiteatro de Ticó, Santa Cruz, Argentina
Named bySergio Archangelsky
Anfiteatro de Ticó formation (Argentina)

Paleobiology

The Anfiteatro de Ticó preserves a rich and diverse flora including macrofossils, mesofossils, and microfossils. These have been object of detailed investigations since the 1960'.[1][2]

Depositional environments

The formation is of continental origin, and includes riparian and lacustrine deposits.

Paleobiota

Bryophytes
  • Ricciopsis grandensis
Horsetails
Ferns
Conifers
  • Alkastrobus peltatus
  • Apterocladus lanceolatus
  • Morenostrobus fertilis
  • Podocarpus dubius
  • Squamastrobus tigrensis
  • Tarphyderma glabra
  • Tomaxellia degiustoi
  • Tomaxellia biforme
  • Trisacocladus tigrensis
Ginkgoales
Cycadales
  • Restrepophyllum chiguoides
  • Eobowenia incrassata
  • Sueria rectivervis
  • Mesosigneria coriacea
  • Mesosigneria oblonga
  • Ticoa harrisii
  • Ticoa lanceolata
  • Ticoa magnipinnulata
  • Pseudoctenis crassa
  • Pseudoctenis dentata


References

  1. Llorens, M.; Loinaze, V.S. Perez; Passalia, M.G.; Vera, E.I. (February 2020). "Palynological, megafloral and mesofossil record from the Bajo Grande area (Anfiteatro de Ticó Formation, Baqueró Group, Upper Aptian), Patagonia, Argentina". Review of Palaeobotany and Palynology. 273: 104137. doi:10.1016/j.revpalbo.2019.104137. hdl:11336/106118. ISSN 0034-6667.
  2. Perez Loinaze, Valeria S.; Vera, Ezequiel I.; Passalia, Mauro G.; Llorens, Magdalena; Friedman, Richard; Limarino, Carlos O.; Césari, Silvia N. (December 2013). "High-precision U–Pb zircon age from the Anfiteatro de Ticó Formation: Implications for the timing of the early angiosperm diversification in Patagonia". Journal of South American Earth Sciences. 48: 97–105. doi:10.1016/j.jsames.2013.08.005. ISSN 0895-9811.


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