Santa Lucía Formation

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Santa Lucía Formation
Stratigraphic range: Maastrichtian-Paleocene (typically Tiupampan)
~67–62 Ma
TypeGeological formation
Unit of
Underlies
OverliesEl Molino Formation
Thickness381.35 m (1,251.1 ft)
Lithology
PrimaryShale, marl
OtherSiltstone
Location
Coordinates18°00′46.0″S 65°24′23.4″W / 18.012778°S 65.406500°W / -18.012778; -65.406500Coordinates: 18°00′46.0″S 65°24′23.4″W / 18.012778°S 65.406500°W / -18.012778; -65.406500
RegionCochabamba
Country Bolivia
Type section
Location, Mizque
Coordinates18°00′46.0″S 65°24′23.4″W / 18.012778°S 65.406500°W / -18.012778; -65.406500
Approximate paleocoordinates20°42′S 52°30′W / 20.7°S 52.5°W / -20.7; -52.5
Santa Lucía Formation is located in Bolivia
Santa Lucía Formation
Santa Lucía Formation (Bolivia)

The Santa Lucía Formation is a Maastrichtian to Paleocene (Danian) geologic formation in Bolivia. Fossil ornithopod tracks have been reported from the Cretaceous lower part of the formation.[1] It is the type formation of the Tiupampan South American land mammal age.

Description[]

Paleogeography of Northern South America
65 Ma, by Ron Blakey

The Santa Lucía Formation is a formation of the in Bolivia dated to the Paleocene, 60 to 58.2 Ma.[2] It overlies the Cretaceous El Molino Formation and is overlain by the . The formation is laterally equivalent with the of northern Argentina,[3] and time-equivalent with the of Argentina, the Maria Farinha Formation of the in northern Brazil and the Guaduas Formation of the Altiplano Cundiboyacense and fossiliferous Cerrejón Formation of the Cesar-Ranchería Basin, Colombia.

The 381.35 metres (1,251.1 ft) thick formation consists of reddish sandy shales, marls and siltstones deposited in a fluvial to lacustrine environment.[4][5]

Paleontological significance[]

The oldest known "condylarth" fauna of the Tertiary of South America comes from basal Paleocene strata of the Santa Lucía Formation at Tiupampa. It includes five genera and seven species: , , , , , , and .[6] Because of its unique fauna, the Santa Lucía Formation at Tiupampa has been chosen as the earliest South American land mammal age giving rise to the Tiupampan.

At the Parotani tracksite, poorly preserved ichnofossils were found in the Maastrichtian part of the formation, left possibly by a carnosaur.[7]

Fossil content[]

The fossiliferous formation has provided the following fossils:

Group Fossils Notes
Mammals Alcidedorbignya inopinata, , , , , , Khasia cordillerensis, , Mayulestes ferox, , , Peradectes austrinum, Pucadelphys andinus, , , , , , , Cimolestes sp., , Henricosborniidae or Oldfieldthomasiidae,
Reptiles & amphibians Coniophis sp., Cynodontosuchus cf. rothi, , , Lapparentemys vilavilensis, Podocnemis ?brasiliensis, , Zulmasuchus querejazus, Aniliidae, Boidae, ?Madtsoiidae, Tropidophiidae, Gymnophiona, Carnosauria indet., Ornithopoda indet.
Fishes , , Enchodus oliveirai, Gasteroclupea branisai, , , Lepidosiren cf. paradoxa, , , Hoplias sp., Lepisosteus sp., , Percichthys sp., Phareodus sp., , , Ictaluridae indet.

See also[]

References[]

  1. ^ Weishampel, et al., 2004, pp.517-607
  2. ^ Sempere et al., 1997, p.709
  3. ^ Sempere et al., 1997, p.712
  4. ^ Jiménez, 2012, p.11
  5. ^ Renner & Velasco, 2000, p.25
  6. ^ De Muizon & Cifelli, 2000, p.47
  7. ^ Leonardi, 1994, p.40
  8. ^ a b c Gayet et al., 1991, p.403
  9. ^ a b c Tiupampa 1 at Fossilworks.org
  10. ^ Buffetaut & Marshall, 1991
  11. ^ Rage, 1991a, pp.499-501
  12. ^ Rage, 1991b, pp.503-508
  13. ^ Vila Vila at Fossilworks.org

Bibliography[]

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