Talampaya Formation

The Talampaya Formation is an Early Triassic (Olenekian) geologic formation in the Ischigualasto-Villa Unión Basin of La Rioja Province in northwestern Argentina. The pink to red sandstones of the formation represent the oldest sedimentary unit in the basin, overlying basement rock and were deposited in a high-energy braided river environment. Ichnofossils, probably left by an archosaur chirotherian, were found in the formation. The formation crops out in the Talampaya National Park, which was designated a UNESCO World Heritage Site in 2000.

Talampaya Formation
Stratigraphic range: Olenekian
~251.3–247.2 Ma
↓
Sandstones in Talampaya National Park
TypeGeological formation
Unit ofPaganzo Group
UnderliesTarjados Formation
OverliesBasement
ThicknessUp to 400 m (1,300 ft)
Lithology
PrimarySandstone
OtherConglomerate, tuff
Location
Coordinates29.6°S 68.1°W / -29.6; -68.1
Approximate paleocoordinates46.0°S 40.2°W / -46.0; -40.2
RegionLa Rioja Province
Country Argentina
ExtentIschigualasto-Villa Unión Basin
Type section
Named forTalampaya River
Named byRomer & Jensen
Year defined1966
Talampaya Formation (Argentina)

Description

The formation was first defined by Romer and Jensen in 1966,[1] based on a type section exposed in the Talampaya River canyon.[2] The Talampaya Formation belongs to the Paganzo Group.[3]

The formation represents the oldest sedimentary unit in the Ischigualasto-Villa Unión Basin in the Talampaya National Park of La Rioja Province, overlying Paleozoic basement, formed by the Tuminico Formation.[4] The Talampaya Formation is overlain by the arid fluvial sandstones and conglomerates of the Tarjados Formation, eroding the Talampaya Formation.[5]

The formation, reaching a maximum thickness of 400 metres (1,300 ft) with a general thickness of approximately 260 metres (850 ft),[6][7] comprises pink to reddish sandstones,[8] deposited in a fluvial environment, dominated by high-energy braided rivers producing sheet floods.[9][10] The sediments were deposited under uniform climatic conditions with temperate to warm temperatures and high humidity.[11] Other facies recognized in the formation are alluvial fan deposits with thin tuffaceous beds and conglomerates, covered by a section of basaltis and other volcanic agglomerates and eolian sandstones.[12]

Tetrapod ichnofossils, probably belonging to a chirotherian (and possibly an archosaur),[11] were discovered in the formation southeast of Pagancillo by Argentina paleontologist José Bonaparte in 1964.[3]

See also

References
  1. Caselli, 1998, p.22
  2. Caselli, 1998, p.23
  3. Leonardi, 1994, p.19
  4. Aceituno Cieri et al., 2015, p.59
  5. Balabusic et al., 2001, p.26
  6. Aceituno Cieri et al., 2015, p.60
  7. Monetta et al., 2000, p.648
  8. Talampaya Formation
  9. Caselli, 1998, p.147
  10. Balabusic et al., 2001, p.25
  11. Balabusic et al., 2001, p.28
  12. Caselli, 1998, p.24

Bibliography

Further reading
  • Bonaparte, J.F. 1978. El Mesozóico de América de Sur y sus Tetrapodos - The Mesozoic of South America and its tetrapods. Opera Lilloana 26. 1–596.
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