El Molino Formation
The El Molino Formation is a Maastrichtian geologic formation pertaining to the Puca Group of central Bolivia. The formation comprises fine-grained sandstones and sandy limestones with stromatolites deposited in a shallow marine to lacustrine environment. The formation has provided fossils of Dolichochampsa minima,[1] and ichnofossils of Ankylosauria indet., Ornithopoda indet., Theropoda indet. and Titanosauridae indet.[2][3][4] The tracksite of Cal Orcko is the best known example of the ichnofossil locations of the formation. The ichnofossil of Ligabueichnum bolivianum may be attributed to an ankylosaur.[5] The fossil fish species Dasyatis molinoensis is named after the formation.
| El Molino Formation Stratigraphic range: Maastrichtian ~70–66 Ma | |
|---|---|
| Type | Geological formation |
| Unit of | Puca Group |
| Underlies | Santa Lucía Formation |
| Overlies | Chaunaca Formation |
| Lithology | |
| Primary | Sandstone |
| Other | Limestone |
| Location | |
| Coordinates | 19.5°S 65.8°W |
| Approximate paleocoordinates | 22.0°S 51.8°W |
| Region | Cochabamba, Chuquisaca & Potosí Departments |
| Country |  |
| Extent | Altiplano & Potosí Basins |
  El Molino Formation (Bolivia) | |
Fossil content
Other fossils retrieved from the formation are:[6]
- Coelodus toncoensis
- Dagetella sudamericana
- Dasyatis branisai, D. molinoensis, D. schaefferi
- Gasteroclupea branisai
- Ischyrhiza hartenbergeri
- Latinopollia suarezi
- Lepidotyle enigmatica
- Ligabueichnum bolivianum[5]
- Noterpeton bolivianum
- Phaerodusichthys taverni
- Pucabatis hoffstetteri
- Pucapristis branisi
- Stephanodus minimus
- Lepidosiren cf. paradoxa
- Andinichthys sp.
- Ceratodus sp.
- Enchodus sp.
- Lepisosteus sp.
- Pucalithus sp.[7]
- Rhineastes sp.
- Santosius sp.
- Anura indet.
- Bolividentrosaurus Viciousia.
- Crocodylia indet.
- Dryolestidae indet.
- Eutheria indet.
- cf. Cyprinodontiformes indet.
- Gymnophiona indet.
- Heterotidinae indet.
- ?Madtsoiidae indet.
- Podocnemidae indet.
- Pycnodontidae indet.
- Boliviaposeidon indet.
- Siluriformes indet.
- Tetragonopterinae indet.
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gollark: The range isn't anywhere near as good as you would get with some sort of high-powered HF transceiver, but you can skip the legal wotsits, and LoRaWAN stuff is available as cheap modules IIRC.
gollark: Er, LoRaWAN.
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gollark: In the US you can't transmit encrypted signals over amateur bands IIRC.
See also
References
- Buffetaut, 1987
- Lockley et al., 2002, p.389
- La Palca village at Fossilworks.org
- Cal Orcko tracksite at Fossilworks.org
- Leonardi, 1994, p.39
- Pajcha Pata at Fossilworks.org
- Leonardi, 1994, p.40
Bibliography
- Buffetaut, É. 1987. Occurrence of the crocodilian Dolichochampsa minima (Eusuchia, Dolichochampsidae) in the El Molino Formation of Bolivia. Bulletin de la Société Belge de Géologie 96. 195–199.
- Leonardi, Giuseppe. 1994. Annotated Atlas of South America Tetrapod Footprints (Devonian to Holocene) with an appendix on Mexico and Central America, 1–248. Ministerio de Minas e Energia - Companhia de Pesquisa de Recursos Minerais, Geological Service of Brazil. Accessed 2019-03-25.
- Lockley, M.G.; A.S. Schulp; C.A. Meyer; G. Leonardi, and D.K. Mamani. 2002. Titanosaurid trackways from the Upper Cretaceous of Bolivia: evidence for large manus, wide-gauge locomotion and gregarious behaviour. Cretaceous Research 23. 383–400. Accessed 2019-03-03.
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