Jump to content

Coquimbo Formation

Coordinates: 30°20′21″S 71°32′03″W / 30.33917°S 71.53417°W / -30.33917; -71.53417
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Tisquesusa (talk | contribs) at 13:55, 9 September 2018 (expand). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Coquimbo Formation
Stratigraphic range: MioceneMid Pleistocene
~23–1.2 Ma
TypeGeological formation
UnderliesAlluvium
OverliesLiman Formation
Thickness63 m (207 ft)
Lithology
PrimaryConglomerate, sandstone, siltstone, shale and coquina
OtherClay lenses, terra rossa
Location
Coordinates30°20′21″S 71°32′03″W / 30.33917°S 71.53417°W / -30.33917; -71.53417
Approximate paleocoordinates30°06′S 70°18′W / 30.1°S 70.3°W / -30.1; -70.3
RegionCoquimbo Region
Country Chile
ExtentTongoy Bay
Type section
Named forCoquimbo

Coquimbo Formation (Spanish: Formación Coquimbo) is a Miocene to Middle Pleistocene sedimentary formation located in Coquimbo Region in Norte Chico, Chile. The lowermost unit belongs to the lower Miocene, with the third-deepest unit dated at 11.9 ± 1.0 Ma. The uppermost unit of the formation is estimated at 1.2 Ma. In the area of Tongoy, the Coquimbo Formation was deposited in an ancient bay that was formed in a graben or half-graben, with a normal fault dipping east. Sea level changes during the Holocene have caused erosion to cut several marine terraces into the formation.[1]

Fossil content

The following fossils have been found in the formation:

SALMA Group Fossils Notes
Montehermosan Mammals Delphinus domeykoi, Megaptera hubachi, Pliopontos sp., ?Squalodon sp., Balaenidae indet.
Birds cf. Palaeospheniscus sp., Spheniscus sp., Diomedeidae indet., Spheniscidae indet.
Fish Carcharodon carcharias
Mayoan Cosmopolitodus hastalis

See also

References

  1. ^ Le Roux, J.P.; Olivares, Danisa M.; Nielsen, Sven N.; Smith, Norman D.; Middleton, Heather; Fenner, Juliane; Ishman, Scott E. (2006). "Bay sedimentation as controlled by regional crustal behaviour, local tectonics and eustatic sea-level changes: Coquimbo Formation (Miocene–Pliocene), Bay of Tongoy, central Chile" (PDF). Sedimentary Geology. 184 (1–2): 133–153. Retrieved 11 April 2016.
  2. ^ Coquimbo at Fossilworks.org
  3. ^ Bahia de Guayacan at Fossilworks.org
  4. ^ Bahia Herradura at Fossilworks.org
  5. ^ La Cantera at Fossilworks.org
  6. ^ Chanaral de Aceituno at Fossilworks.org
  7. ^ Tongoy area Unit 11 at Fossilworks.org
  8. ^ Tongoy area Unit 4 at Fossilworks.org

Further reading

  • C. Acosta Hospitaleche, J. Canto, and C. P. Tambussi. 2006. Pingüinos (Aves, Spheniscidae) en Coquimbo (Mioceno Medio-Plioceno Tardio), Chile y su vinculación con las corrientes oceánicas. Revista Española de Paleontología 21(1):115-122