Earth:Candeleros Formation

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Candeleros Formation
Stratigraphic range: early Cenomanian
~99–97 Ma
Fm Candeleros cerro Vagon.jpg
Candeleros Formation near Cerro El Vagon, Neuquen, Argentina
TypeGeological formation
Unit ofNeuquén Group
 Río Limay Subgroup
UnderliesHuincul Formation
OverliesLohan Cura Formation
Thickness300 m (980 ft)
Lithology
PrimaryEolian sandstone
OtherConglomerate, siltstone, paleosol
Location
Coordinates [ ⚑ ] : 39°24′S 69°12′W / 39.4°S 69.2°W / -39.4; -69.2
Paleocoordinates [ ⚑ ] 46°30′S 45°30′W / 46.5°S 45.5°W / -46.5; -45.5
RegionMendoza, Neuquén & Río Negro Provinces
CountryArgentina
ExtentNeuquén Basin
Type section
Named forCandeleros Hill
Named byWichmann
Year defined1929
Candeleros Formation is located in Argentina
Candeleros Formation
Candeleros Formation (Argentina)

The Candeleros Formation (formerly known as the Candeleros Member of the "Río Limay Formation") is a geologic formation that crops out in the Río Negro, Neuquén, and Mendoza provinces of northern Patagonia, Argentina . It is the oldest formation in the Neuquén Group and belongs to the Rio Limay Subgroup. Formerly that subgroup was treated as a formation, and the Candeleros Formation was known as the Candeleros Member.[1]

Description

The type locality of the Candeleros Formation is Candeleros Hill in Neuquén Province, after which the formation was named by Wichmann in 1929.[2] This formation unconformably overlies the Lohan Cura Formation, and it is in turn overlain by the Huincul Formation, also a unit of the Neuquén Group. The sediments of the latter are of lighter greenish and yellow colors and the boundary between the Candeleros and Huincul formations is easily recognizable.[3]

The Candeleros Formation is almost 300 metres (980 ft) thick in some sections. Overall, the formation represents a part of the ancient Kokorkom desert with braided river system, made up mostly of sandstones and conglomerates. There are also isolated sections that represent eolian (wind-blown) deposition, as well as siltstones deposited under swamp conditions. Paleosols (soil deposits) are common in some sections as well.[1][3]

Fossil content

The Candeleros Formation has a very diverse fossil fauna, including:

In 2021, fossil material of a giant titanosaur sauropod, distinct from Andesaurus and probably exceeding Patagotitan in size, was described from the formation by Otero et al. (2021).[9]

Amphibians

Frogs
Taxa Species Locality Stratigraphic position Material Notes Images
Avitabatrachus A. uliana A Pipimorpha frog.
Rhynchocephalians
Taxa Species Locality Stratigraphic position Material Notes Images
Priosphenodon P. avelasi A Rhynchocephalian.
Priosphenodon NT small.jpg
Tika T. giacchinoi A Rhynchocephalian.

Fish

Taxa Species Locality Stratigraphic position Material Notes Images
Ceratodus C. argentinus A lungfish.

Dinosaur

Ornithischian

Taxa Species Locality Stratigraphic position Material Notes Images
Bonaparteichnium B. tali Footprints. An Iguanodont.
Jakapil J. Kaniukura MPCA-PV-630, a partial skeleton including several osteoderms and a complete lower jaw. A Thyreophora ornithopod.
Jakapil skeletal.webp

Saurischian

Sauropod
Taxa Species Locality Stratigraphic position Material Notes Images
Andesaurus A. delgadoi A titanosaur.
Andesaurus LM.png
Limaysaurus L. tessonei' A rebbachisaurid sauropod.
Nopcsaspondylus N. alarconensis A rebbachisaurid sauropod.
Rayososaurus R. agrioensis A rebbachisaurid sauropod.
Titanosauria indeterminate.
Theropod
Taxa Species Locality Stratigraphic position Material Notes Images
Abelichnus A. astigerrae
Alnashetri A. cerropoliciensis An alvarezsauroid theropod.
Alnashetri LM.png
Bicentenaria B. argentina A coelurosaur.
Bicentenaria.jpg
Buitreraptor B. gonzalezorum A dromaeosaurid theropod.
BuitreraptorROM.JPG
Ekrixinatosaurus E. novasi An Abelisaurid theropod.
Ekrixinatosaurus novasi by Henrique Paes.png
Giganotosaurus G. carolinii A skeletal specimen. A carcharodontosaurid theropod.
Giganotos Db.jpg

Mammals

Taxa Species Locality Stratigraphic position Material Notes Images
Cronopio C. dentiacutus La Buitrera. Neuquén Group. MPCA PV 454, a partial skull without skull roof, basicranium, and squamosals, and from the referred specimens MPCA PV 450, a partial left lower jaw with damaged teeth, and MPCA PV 453, an incomplete skull with a relatively complete right lower jaw missing some teeth. A small insectivorous mammal that belongs to the Meridiolestida family.
Cronopio NT.jpg

Reptiles

Taxa Species Locality Stratigraphic position Material Notes Images
Araripesuchus A. buitreraensis
Najash N. rionegrina

See also

References

  1. 1.0 1.1 Sánchez et al., 2006
  2. Wichmann, 1929
  3. 3.0 3.1 Leanza et al., 2004
  4. Agnolin, Federico; Rozadilla, Sebastián; Juárez-Valieri, Rubén; Meso, Jorge (2023-10-25). "Oldest azhdarchid (Pterosauria) record from South America" (in es). Revista del Museo Argentino de Ciencias Naturales. Nueva serie 25 (2): 309–314. ISSN 1853-0400. http://revista.macn.gob.ar/ojs/index.php/RevMus/article/view/825. 
  5. Canale et al., 2016
  6. Calvo, Jorge O. (1991). "Huellas de dinosaurios en la Formación Río Limay (Albiano-Cenomaniano?), Picún Leufú, Provincia del Neuquén, República Argentina (Ornithischia-Saurischia: Sauropoda-Theropoda)". Ameghiniana 28 (3): 241–258. https://www.researchgate.net/publication/283994360. 
  7. "A new Cretaceous thyreophoran from Patagonia supports a South American lineage of armoured dinosaurs". Scientific Reports 12 (1): Article number 11621. 2022. doi:10.1038/s41598-022-15535-6. PMID 35953515. 
  8. Leonardi, 1994, p. 79
  9. Otero et al., 2021

Bibliography