Bajo de la Carpa Formation explained

Bajo de la Carpa Formation
Type:Geological formation
Period:Santonian
Age:Mid-Late Santonian
~
Prilithology:Sandstone
Otherlithology:Mudstone, siltstone, paleosol
Region:Neuquén & Río Negro Provinces
Country:Argentina
Coordinates:-38.8°N -68.8°W
Paleocoordinates:-43.4°N -49.8°W
Unitof:Neuquén Group
 Río Colorado Subgroup
Underlies:Anacleto Formation
Overlies:Río Neuquén Subgroup
 Plottier Formation
Thickness:Up to 150m (490feet)
Extent:Neuquén Basin

The Bajo de la Carpa Formation is a geologic formation of the Neuquén Basin that crops out in northern Patagonia, in the provinces of Río Negro and Neuquén, Argentina. It is the oldest of two formations belonging to the Río Colorado Subgroup within the Neuquén Group. Formerly, that subgroup was treated as a formation, and the Bajo de la Carpa Formation was known as the Bajo de la Carpa Member.[1]

At its base, this formation conformably overlies the Plottier Formation of the older Río Neuquén Subgroup, and it is in turn overlain by the Anacleto Formation, the youngest and uppermost formation of the Neuquén Group.[2]

The Bajo de la Carpa Formation can reach 150m (490feet) in thickness in some locations, and consists mainly of sandstones of various colors, all of fluvial origin, with thin layers of mudstone and siltstone in between. Geological features such as geodes, chemical nodules, impressions of raindrops, and paleosols (fossil soils) are commonly found in this formation as well.

Fossil content

Reptiles

Vertebrate fossils are abundant within the Bajo de la Carpa Formation:

Small nests with eggs inside, found in this formation, probably belonged to the bird Neuquenornis.[3] Fossil wasp nests have also been found in these rocks.

Crocodylomorphs

Crocodylomorphs reported from the Bajo de la Carpa Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
BarrosasuchusB. neuquenianus[4]
ComahuesuchusC. brachybuccalis
CynodontosuchusC. rothi
LomasuchusL. palpebrosus.
Gasparinisuchus[5] G. peirosauroides
KinesuchusK. overoi[6]
NeuquensuchusN. universitas [7]
Notosuchus N. lepidus
N. terrestris
PeirosaurusP. torminniA fragmentary skull and a partial postcranial skeleton.

Dinosaurs

Ornithischians

Ornithischians reported from the Bajo de la Carpa Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
Ankylosauria[8] Indetermidate.
Mahuidacursor[9] M. lipanglefAn ornithopod.

Sauropods

Sauropods reported from the Bajo de la Carpa Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
BonitasauraB. salgadoiA partial sub-adult skeleton with a lower jaw, a partial vertebrae series, and limb bones.A titanosaur.
InawentuI. oslatusRincón de los Sauces.A partially articulated skeleton, including a nearly complete skull, Several vertebrae from the atlas to the end of the sacrum, and both iliaA titanosaur.
OverosaurusO. paradasorumUpperA fully articulated vertebral series consists of rib bones, dorsals, and ilium.A titanosaur.
RinconsaurusR. caudamirusRincón de los Sauces.Lower.The fossil remains included vertebrae, limb bones, scapula, hip bones (pubis, ilium, and ischium) and several ribs.A titanosaur.
Traukutitan[10] T. eocaudataSitio Trauku.LowerA partial semi-articulated skeleton including both thigh bones and thirteen vertebrae from the anterior and middle tail.A titanosaur.

Theropods

Theropods reported from the Bajo de la Carpa Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
Achillesaurus A. manazzoneiUpperA partial skeleton consists of a sacral vertebra, four tail vertebrae, part of the left thighbone, shin, and foot, and the left ilium.An alvarezsaurid.
AlvarezsaurusA. calvoiAn alvarezsaurid.
Diuqin[11] D. lechiguanae"the isthmus between the southeast coast of Lago Barreales and the northwest coast of Lago Mari Menuco"A fragmentary but associated partial skeletonAn unenlagiine.
Llukalkan [12] L. aliocranianusLa Invernada site.A partial skull.An abelisaur.
NeuquenornisN. volansUpperA skull and a partial postcranial remains.A enantiornithine bird.
PatagopteryxP. eferrariisiUpperThe oldest known flightless bird.
Tratayenia[13] T. rosalesiA well-preserved partial skeletonA megaraptoran theropod.
Velocisaurus[14] V. unicusA noasaur.
Viavenator[15] V. exxoniAn abelisaur.

See also

References

Bibliography

Further reading

Notes and References

  1. Sánchez et al., 2006
  2. Fossa Mancini et al., 1938
  3. Leanza et al., 2004
  4. Coria et al., 2019
  5. Martinelli et al., 2012
  6. Filippi et al., 2018a
  7. Lio et al., 2018
  8. Rozadilla. Sebastián. Agnolín. Federico. Manabe. Makoto. Tsuihiji. Takanobu. Novas. Fernando E.. September 2021. Ornithischian remains from the Chorrillo Formation (Upper Cretaceous), southern Patagonia, Argentina, and their implications on ornithischian paleobiogeography in the Southern Hemisphere. Cretaceous Research. 125. 104881. 10.1016/j.cretres.2021.104881. 2021CrRes.12504881R . 0195-6671.
  9. Cruzado Caballero et al., 2019
  10. Filippi . Leonardo S. . Juárez Valieri . Rubén D. . Gallina . Pablo A. . Méndez . Ariel H. . Gianechini . Federico A. . Garrido . Alberto C. . 2023 . A rebbachisaurid-mimicking titanosaur and evidence of a Late Cretaceous faunal disturbance event in South-West Gondwana . Cretaceous Research . 154 . en . 10.1016/j.cretres.2023.105754 . 0195-6671.
  11. Porfiri . Juan D. . Baiano . Mattia A. . dos Santos . Domenica D. . Gianechini . Federico A. . Pittman . Michael . Lamanna . Matthew C. . 2024-06-14 . Diuqin lechiguanae gen. et sp. nov., a new unenlagiine (Theropoda: Paraves) from the Bajo de la Carpa Formation (Neuquén Group, Upper Cretaceous) of Neuquén Province, Patagonia, Argentina . BMC Ecology and Evolution . 24 . 1 . 77 . 10.1186/s12862-024-02247-w . free . 38872101 . 2730-7182. 11177497 . 2024BMCEE..24...77P .
  12. Filippi et al., 2018b
  13. Porfiri et al., 2018
  14. Filippi et al., 2018b
  15. Filippi et al., 2018b