The Ituzaingó Formation (Spanish : Formación Ituzaingó ), in older literature also described as Entre Ríos or Entrerriana Formation , is an extensive geological formation of Late Miocene (Tortonian , or Huayquerian in the SALMA classification ) age in the Paraná Basin of the Corrientes , Santa Fe and Entre Ríos Provinces in Mesopotamia , northeastern Argentina .[ 1] The formation comprises mudstones , cross-bedded sandstones and conglomerates deposited in a fluvio -deltaic environment and is renowned for the preservation of a rich fossil assemblage, including many mammals , birds , reptiles , fish , bivalves , foraminifera , ichnofossils and flora .
Map of the Paraná River drainage basin with the river indicated. Most outcrops of the Ituzaingó Formation flank the middle course of the Paraná River.
The Ituzaingó Formation was first described by De Alba in 1953 and later by Herbst in 1971.[ 2] The up to 150 metres (490 ft), but in most areas between 10 and 20 metres (33 and 66 ft) thick formation is found in an area of 120,000 square kilometres (46,000 sq mi),[ 3] stretching from the Paraná River to 40 kilometres (25 mi) east of Tostado .[ 4] The Ituzaingó Formation crops out in the northeasternmost part of Argentina (Mesopotamia ), in the provinces of Corrientes , Santa Fe and Entre Ríos , among other locations along the banks of the Paraná River .[ 5]
The formation overlies the marine Paraná Formation and is unconformably overlain by the Puerto Alvear ,[ 6] Hernandarías and Yupoí Formations of Early Pleistocene (Uquian and Ensenadan respectively) age.[ 5] [ 7] [ 8] At the shores of the Paraná River, the formation underlies the Timbúes Formation .[ 9] In certain places along the same river, the formation cuts into the underlying Rosario Formation .[ 10]
The formation contains a basal conglomeratic member "Conglomerado osífero" (bony conglomerate ) with abundant vertebrate remains.[ 11] This conglomerate is overlain by almost unfossiliferous whitish to yellow brown sandstones and green mudstones. The Ituzaingó Formation (as Entre Ríos Formation) was correlated with the Puelches Formation of the subsurface of Buenos Aires Province . According to the mammals occurring in the conglomerate and the stratigraphic relationships, the age of the base of Ituzaingo Formation is almost exclusively Tortonian (Late Miocene ) or Huayquerian in the SALMA classification.[ 12]
Depositional environment
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The formation, as the Paraná and Puelches Formations, has been deposited in a vast Miocene tidal flat environment.[ 13] Both the terrestrial and freshwater fauna of the Ituzaingó Formation indicates a climate warmer than present. The freshwater vertebrate record suggests important basin connections with Amazonian basins.[ 11]
Alternatively, the Conglomerado Osífero Member has been interpreted as tide -dominated fluvial channels, pertaining to the marine Paraná Formation.[ 14]
Huayquerian correlations
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^ Ituzaingó Formation at Fossilworks .org
^ Vezzosi, 2015, p.27
^ Vezzosi, 2015, p.28
^ Vezzosi, 2015, p.29
^ a b Franco, 2014, p.16
^ Brunetto, 2013, p.22
^ Cione et al., 2000, p.195
^ Cione et al., 2009, p.3
^ Vezzosi, 2015, p.41
^ Vezzosi, 2015, p.75
^ a b Cione et al., 2005, p.49
^ a b c d e f g h i Colonia La Celina at Fossilworks .org
^ Torra, 2005, p.46
^ Martín Pérez, 2013, p.291
^ Martín Pérez, 2013, p.27
^ Cione et al., 2005, p.58
^ Brandoni, 2013, p.135
^ a b c d e f g h i Paraná, Pueblo Brugo to Diamante, Ituzaingó Fm. Archived 2022-11-10 at the Wayback Machine at Fossilworks .org
^ Noriega & Agnolin, 2008, pp.272-285
^ Agnolin & Noriega, 2012
^ a b c d e Ciudad de Paraná at Fossilworks .org
^ a b Candela, 2005, pp.43–46
^ a b Scillato et al., 2013, pp.119–120
^ a b Góis et al., 2013, p.177
^ Brandoni & Scillato, 2007, p.430
^ Brandoni & Scillato, 2007, p.431
^ Brandoni, 2008, p.14
^ Brandoni, 2008, p.16
^ Brandoni, 2011, p.36
^ Brandoni, 2014, p.34
^ Scheyer & Delfino, 2016, p.56
^ a b Bona, P.; Barrios, F.; Ezcurra, M.D.; Victoria, M.; Blanco, F.; Cidade, G.M. (2024). "New taxa of giant caimans from the southernmost hyperdiverse wetlands of the South American late Miocene". Journal of Systematic Palaeontology . 22 (1). doi :10.1080/14772019.2024.2375027 .
^ Cione et al., 2009, p.4
^ Cione et al., 2013, p.70
^ a b Cione et al., 2005, p.52
^ Azpelicueta & Cione, 2016, p.221
^ a b Torra, 2005, p.45
^ Franco, 2018, p.646
^ Franco, 2014, p.25
^ Brea et al., 2013a, pp.45-47
^ Brea et al., 2013b, p.4
^ Franco & Brea, 2015, p.3
^ Moya & Brea, 2020
El Neógeno de la Mesopotamia argentina
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: CS1 maint: multiple names: authors list (link )
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