Colonia La Celina - conglomerado osifero: Huayquerian, Argentina
collected by J. Casciotta, A. Cione, J. Noriega and L. Soibelzon and other 1999
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
- Testudines
- Chelidae
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Phrynops sp.
Wagler 1830
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de la Fuente 1992 | |||||||||
Parahydraspis paranaensis n. gen., n. sp.
Wieland 1923
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Wieland 1923 | |||||||||
recombined as Phrynops paranaensis | ||||||||||
YPM VP 001565 | ||||||||||
Reptilia
- Testudines
- Testudinidae
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Testudo paranensis n. sp.
Scalabrini 1887
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Scalabrini 1887 | |||||||||
nomen nudum belonging to Testudinidae | ||||||||||
Mammalia
- Megatheriidae
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Pyramiodontherium sp.
Rovereto 1914
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Brandoni and Carlini 2009 | |||||||||
Mammalia
- Megalonychidae
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Pliomorphus ameghinoi
Kraglievich 1923
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Brandoni 2008 | |||||||||
synonym of Pliomorphus mutilatus | ||||||||||
FCP-V-M-050 | ||||||||||
Mammalia
- Didelphimorphia
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Philander entrerianus
(Ameghino 1899)
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Goin et al. 2013 | |||||||||
FCP-V-M-055 | ||||||||||
Actinopteri
- Characiformes
- Serrasalmidae
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Megapiranha paranensis
Cione et al. 2009
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CICYTTP-PV-P-1-125, isolated tooth crown (paratype). (3 measurements) | ||||||||||
see common names |
Geography
Country: | Argentina | State/province: | Entre Rios |
Coordinates: | 31.6° South, 60.3° West (view map) | ||
Paleocoordinates: | 31.8° South, 58.2° West | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | outcrop |
Time
Period: | Neogene |
10 m.y. bin: | Cenozoic 6 |
Key time interval: | Huayquerian |
Age range of interval: | 7.90000 - 4.90000 m.y. ago |
Stratigraphy
Formation: | Ituzaingo | Member: | Conglomerado Osifero | ||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: The fluvial Ituzaingo Formation overlies the marine unit. This formation is composed of a basal conglomerate (“Conglomerado osifero”) with abundant vertebrate remains which is overlain by almost unfossiliferous whitish to yellow brown sandstones and green mudstones. Terrigenous Pleistocene (Ensenadan to Lujanian in the southern South American continental scale; see Cione and Tonni, 1995, 1996, 2001; Fig. 2), poorly fossiliferous beds assigned to different units overlay the Ituzaingo Formation (Aceñolaza, 1976; Iriondo, 1980; Chebli et al., 1989). The Ituzaingo Formation (as Entre Rios Formation) was correlated with the “Formacio ́n Puelche” of the Buenos Aires province subsoil (Reig, 1957; see below). According to the mammals occurring in the “Conglomerado osifero” and the stratigraphic relationships, the age of the base of Ituzaingo Formation is almost exclusively Tortonian (late Miocene) or Huayquerian in the local chronology (Pascual and Odreman Rivas, 1971; Cione and Tonni, 1995; Fig.2).
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Lithology and environment
Primary lithology: | conglomerate |
Secondary lithology: | white mudstone |
Includes fossils? | Y |
Lithology description: The fluvial Ituzaingo Formation overlies the marine unit (i.e., Parana Fm.). This formation is composed of a basal conglomerate (“Conglomerado osifero”) with abundant vertebrate remains which is overlain by almost unfossiliferous whitish to yellow brown sandstones and green mudstones. See Fig. 2 for further details on lithology and stratigraphy | |
Environment: | fluvial indet. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Collection methods: | field collection | ||
Reason for describing collection: | taxonomic analysis | ||
Collectors: | J. Casciotta, A. Cione, J. Noriega and L. Soibelzon and other | Collection dates: | June 1999 and other |
Metadata
Also known as: | Paraná River | ||
Database number: | 140472 | ||
Authorizer: | C. Jaramillo, E. Vlachos, P. Mannion | Enterer: | G. Ballen, E. Vlachos, M. Kouvari, J. Carrillo |
Modifier: | M. Kouvari | ||
Created: | 2013-03-10 11:53:57 | Last modified: | 2019-09-13 05:10:56 |
Access level: | group members | Released: | 2016-03-10 11:53:57 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
45471. | L. A. Cione, W. M. Dahdul, J. G. Lundberg and A. Machado-Allison. 2009. Megapiranha paranensis, a new genus and species of Serrasalmidae (Characiformes, Teleostei) from the upper Miocene of Argentina. Journal of Vertebrate Paleontology 29(2):350-358 [C. Jaramillo/G. Ballen] |
Secondary references:
71607 | D. Brandoni. 2008. Nuevos materiales de Ortotheriinae (Xenarthra, Tardigrada, Megalonychidae) procedentes del "Mesopotamiense" (Mioceno tardio) de Entre Rios. Instituto Superior de Correlacion Geologica (INSUGEO) Serie Miscelanea 17:11-20 [P. Mannion/M. Kouvari] | |
70178 | D. Brandoni and A. A. Carlini. 2009. On the presence of Pyramiodontherium (Mammalia, Xenarthra, Megatheriidae) in the late Miocene of northeastern Argentina and its biogeographical implications. Rivista Italiana di Paleontologia e Stratigrafia 115(1):111-123 [P. Mannion/M. Kouvari/P. Wagner] | |
63676 | M. S. de la Fuente. 1992. Las tortugas Chelidae del Terciario superior y Cuaternario del territorio argentino. Ameghiniana 29(3):211-229 [E. Vlachos/E. Vlachos] | |
50741 | F. J. Goin, J. I. Noriega, and M. Reyes. 2013. Los Metatheria (Mammalia) del "Mesopotamiense" (Mioceno tardío) de la Provinciade Entre Ríos, Argentina, y una reconsideración de Philander entrerianus (Ameghino, 1899). In D. Brandoni, J.I. Noriega (eds.), El Neógeno de la Mesopotamia argentina 14:109-117 [C. Jaramillo/J. Carrillo] | |
64418 | P. Scalabrini. 1887. Cartas Científicas Museo de la Provincia de Entre Ríos. Tipografía y Encuadernación La Velocidad 1-209 [E. Vlachos/E. Vlachos] | |
62129 | G. R. Wieland. 1923. A new Parana pleurodiran. American Journal of Science 25:1-14 [E. Vlachos/E. Vlachos] |