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
Phrynops sp. Wagler 1830
de la Fuente 1992
Parahydraspis paranaensis n. gen., n. sp. Wieland 1923
Wieland 1923
recombined as Phrynops paranaensis
YPM VP 001565
Reptilia - Testudines - Testudinidae
Testudo paranensis n. sp. Scalabrini 1887
Scalabrini 1887
nomen nudum belonging to Testudinidae
Mammalia - Megatheriidae
Pyramiodontherium sp. Rovereto 1914
Brandoni and Carlini 2009
Mammalia - Megalonychidae
Pliomorphus ameghinoi Kraglievich 1923
Brandoni 2008
synonym of Pliomorphus mutilatus
FCP-V-M-050
Mammalia - Didelphimorphia
Philander entrerianus (Ameghino 1899)
Goin et al. 2013
FCP-V-M-055
Actinopteri - Characiformes - Serrasalmidae
Megapiranha paranensis Cione et al. 2009
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).
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]