Cancañiri Formation

The Cancañiri Formation, also named as Cancañiri Tillite, is a Katian to Hirnantian geologic formation of central Bolivia. The pebbly, argillaceous sandstones, shales and siltstones of the up to 1,500 metres (4,900 ft) thick formation,[1] were deposited in a glacial foreshore to deep water turbiditic environment.[2][3][4][5] The formation is named after Cancañiri, a mining town close to Llallagua, where a local legend of a possessed woman is believed.[6] The formation overlies the San Benito Formation in Cochabamba and the Amutara Formation in other parts. The Cancañiri Formation is overlain by the Uncía Formation.[7]

Cancañiri Formation
Stratigraphic range: Katian-Hirnantian
~460–439 Ma
TypeGeological formation
UnderliesUncía Formation
OverliesAmutara & San Benito Formations
ThicknessUp to 1,500 m (4,900 ft)
Lithology
PrimarySandstone, shale
OtherSiltstone
Location
Coordinates17.7°S 66.3°W / -17.7; -66.3
Approximate paleocoordinates44.2°S 127.4°W / -44.2; -127.4
RegionCochabamba & Potosí Departments
Country Bolivia
ExtentCordillera Oriental
Type section
Named forCancañiri
Cancañiri Formation (Bolivia)

Fossil content

The formation has provided the following fossils:

  • Destombesium pacochicoensis
  • Dinorthis flabellulum
  • Drabovinella curiosa
  • Tunariorthis cardocanalis
  • Oanduporella sp.
  • Rostricellula sp.

See also

References

Bibliography

Further reading

  • V. Havlicek and L. Branisa. 1980. Ordovician brachiopods of Bolivia: Succession of assemblages, climate control, affinity to Anglo-French and Bohemian provinces. Rozpravy Ceskoslovenske Akademie Ved. Rada Matematickych a Prirodnich Ved. Academia Praha, Prague, Czechoslovakia 90(1):1-54
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