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Pebas Formation

Coordinates: 7°24′S 75°00′W / 7.4°S 75.0°W / -7.4; -75.0
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Pebas Formation
Stratigraphic range: Early Aquitanian-Tortonian
(Colhuehuapian-Huayquerian)
~21–8 Ma
UnderliesMarañón Formation
OverliesChambira Formation
Area1,000,000 km2 (390,000 sq mi)
Thickness~350–1,074 m (1,148–3,524 ft)
Lithology
PrimarySiltstone, mudstone
OtherCoal/lignite
Location
Coordinates7°24′S 75°00′W / 7.4°S 75.0°W / -7.4; -75.0
Approximate paleocoordinates8°24′S 70°36′W / 8.4°S 70.6°W / -8.4; -70.6
RegionAmazon Basin
Country Brazil
 Colombia
 Ecuador
 Peru
Type section
Named forPebas District

The Pebas Formation is a lithostratigraphic unit of Miocene age, found in western Amazonia. The formation extends over 1,000,000 square kilometres (390,000 sq mi), including parts of Brazil, Peru, Ecuador and Colombia.[1] It is interpreted as representing the deposits of a lake ("Lake Pebas") or series of lakes, formed within the foreland basin of the Andes mountain belt. It is known for its abundant fossil ostracods and molluscs and an unusually diverse group of crocodylians.[2]

Fossil content

Group Fossils Notes
Mammals Dinomyidae indet., ?Octodontoidea indet.
Reptiles Caiman wannlangstoni, Gnatusuchus pebasensis, Gryposuchus pachakamue, Purussaurus neivensis, Kuttanacaiman iquitosensis, Mourasuchus atopus, Paleosuchus sp., Podocnemis sp., Gavialoidea indet.
Fishes cf. Hydrolycus sp., Leporinus sp., Potamotrygon sp., Pristis sp., Anostomidae indet.
Insects Macroteleia yaguarum, Sycorax peruensis

References

  1. ^ Wesselingh et al., 2006
  2. ^ Sala Gismondi et al., 2006
  3. ^ a b c CTA-45 at Fossilworks.org
  4. ^ IQ114 at Fossilworks.org
  5. ^ Amazonian amber at Fossilworks.org

Bibliography

Further reading

  • Template:Cite LSA
  • Marcos C.Bissaro-Júnior, Leonardo Kerber, James L.Crowley, Ana M.Ribeiro, Renato P.Ghilardi, Edson Guilherme, Francisco R.Negri, Jonas P.Souza Filho, Annie S.Hsiou: "Detrital zircon U–Pb geochronology constrains the age of Brazilian Neogene deposits from Western Amazonia." Palaeogeography, Palaeoclimatology, Palaeoecology Volume 516, 15 February 2019, Pages 64–70 doi: 10.1016/j.palaeo.2018.11.032