Caleufú (Miocene of Argentina)

Where: La Pampa, Argentina (35.7° S, 64.7° W: paleocoordinates 35.8° S, 63.0° W)

• coordinate stated in text

• outcrop-level geographic resolution

When: Cerro Azul Formation, Messinian (7.2 - 5.3 Ma)

• Verzi and Montalvo 2008: based on the “stage of evolution" of octodontids they concluded that this is of Huayquerian age.

•Prevosti and Pardinas 2009: critique the above study. The lack of isotopic or paleomagnetic data coupled with the isolation of this locality and the absence of a local stratigraphic succession inhibit its correlation with other palaeontological comparable sites and a robust inference about its chronology. The “stage of evolution” of a taxon is not a biostratigraphic tool, thus we cannot rule out the possibility that the Caleufú assemblage has an Early Pliocene (Montehermosan) age.

•Sostillo et al 2018: The Cerro Azul Formation deposits (Linares et al., 1980) are discontinuous along the whole occupied area in the provinces of La Pampa and Buenos Aires (Fig. 2). They are composed of silts, sandy silts and very thin silty sands, reddish and brown colored, with a homogeneous and com- pact general aspect, and frequent carbonate nodules and evidences of pedogenic processes (Folguera and Zárate, 2009). Visconti et al. (2010) interpreted them as eolian deposits characterized by loessic materials, with a high per- centage of lithic fragments and volcaniclastic sediments. Detailed geological and stratigraphic descriptions of the Cerro Azul Formation are provided by Linares et al. (1980), Goin et al. (2000), Visconti et al. (2010), and Folguera and Zárate (2009).

•Prevosti et al. (2023): By combining our new radioisotopic dates with biochronology (Supplementary Table S6), a further refinement of the sigmodontine temporal record is now possible. Our results indicate a median age of 5.773 Ma (range 6.214 –5.115 Ma) for the Caleufú assemblage.

• formation-level stratigraphic resolution

Environment/lithology: loess; paleosol/pedogenic, concretionary, brown, gray, sandy siltstone

• Schmidt et al. 2018: Deposits at Telen, Bajo Giuliani, El Guanaco and Caleufú were interpreted as loess-like deposits with immature palaeosols and little diagenetic alteration (Montalvo et al., 2008, 2016; Verzi et al., 2008).

•Sostillo et al 2018: eolian deposits with scarcely developed paleosols. This

• sandy siltstones diffusely stratified 0.8 to 1.0 m thick, cemented by carbonates, and with abundant

•scattered calcareous concretions and rounded manganese nodules

•Verzi et al. 2003: El afloramiento de la Formación Cerro Azul en Caleufú (figura 1.A) está constituido por limolitas loessoides cementadas por carbonatos, en las cuales se pueden diferenciar tres niveles (figura 1.B). El nivel inferior (portador de los fósiles) y el superior, tienen una potencia de 80 y 50 cm, respectivamente; son de color pardo anaranjado grisáceo, presentan abundantes concreciones calcáreas dispersas y generalmente amorfas. El nivel medio, de 50 cm de espesor, es más arcilloso y de color pardo anaranjado pálido; presenta cutanes de hábito cúbico y concreciones calcáreas cilíndricas, alargadas verticalmente. Estas últimas son interpretadas como rizolitos.

Size classes: macrofossils, mesofossils

Primary reference: D. H. Verzi and C. I. Montalvo. 2008. The oldest South American Cricetidae (Rodentia) and Mustelidae (Carnivora): Late Miocene faunal turnover in Central Argentina and the Great American Biotic Interchange. Palaeogeography, Palaeoclimatology, Palaeoecology 267(3-4):284-291 [C. Jaramillo/J. Carrillo]more details

Purpose of describing collection: paleoecologic analysis

PaleoDB collection 141939: authorized by Carlos Jaramillo, entered by Juan Carrillo on 03.04.2013, edited by Grace Varnham, Miranta Kouvari, Philip Mannion and Kateryn Pino

Creative Commons license: CC BY (attribution)

Taxonomic list

unclassified
  -
Aves
 Falconiformes - Falconidae
Milvago sp.1 Spix 1824 caracara
GHUNLPam 19867/16, distal end of left humerus
 Tinamiformes - Tinamidae
cf. Eudromia sp.1 Geoffroy 1832 tinamou
GHUNLPam 21566/22, proximal end of left carpometacarpus
 Passeriformes - Tyrannidae
cf. Tyrannidae indet.1 Vigors 1825 tyrant flycatcher
GHUNLPam 19865/15, proximal epiphysis of right ulna
Mammalia
 Marsupialia -
Didelphimorphia indet.4 Gill 1872 marsupial
See Prevosti&Pardiñas 2009 for a different interpretation
 Notoungulata - Toxodontidae
Toxodontidae indet. Scott 1873 notoungulate
 Notoungulata - Mesotheriidae
Pseudotypotherium subinsigne Rovereto 1914 notoungulate
 Notoungulata - Hegetotheriidae
Tremacyllus sp.2 Ameghino 1891 notoungulate
Tremacyllus impressus8 Ameghino 1888 notoungulate
GHUNLPam multiple specimens
Paedotherium minor Cabrera 1937 notoungulate
see also ref 70179 where they talk about Paedotherium sp.
 Rodentia - Cricetidae
Sigmodontinae indet. Wagner 1843 rodent
"Necromys" bonapartei5 Reig 1978 rodent
 Rodentia - Dinomyidae
Tetrastylus sp. Ameghino 1886 caviomorph
Tetrastylus intermedius7 Rovereto 1914 caviomorph
GHUNLPam 19830
 Rodentia - Octodontidae
Pithanotomys macer Ameghino 1888 caviomorph
Phtoramys homogenidens Ameghino 1887 caviomorph
 Rodentia -
Neophanomys recens n. sp.9 Verzi et al. 2011 caviomorph
Holotype: GHUNLPam 19602
Neophanomys biplicatus Rovereto 1914 caviomorph
 Rodentia - Ctenomyidae
Xenodontomys elongatus n. sp. Verzi et al. 2003 caviomorph
GHUNLPam 19714
 Rodentia - Echimyidae
Pampamys emmonsae Verzi et al. 1995 spiny rat
 Rodentia - Caviidae
Orthomyctera sp. Ameghino 1889 caviomorph
 Rodentia - Chinchillidae
Lagostomus sp. Brookes 1828 viscacha
 Panameriungulata - Proterotheriidae
Proterotheriidae indet. Ameghino 1887 placental
Diplasiotherium pampa6 Soria 2001 placental
GHUNLPam 21589, associated left maxillary fragment with P4-M2 and left mandibular fragment with incomplete p4-m1
  - Mylodontidae
Scelidotheriinae indet. Ameghino 1889 edentate
Proscelidodon gracillimus3 Rovereto 1914 edentate
GHUNLPam 21108
 Cingulata - Glyptodontidae
Glyptodontidae indet. Burmeister 1879 glyptodon