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
•
•Sostillo et al 2018: eolian deposits with scarcely developed paleosols. This
•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 | |
| |
| |
cf. Tyrannidae indet.1 Vigors 1825 tyrant flycatcher GHUNLPam 19865/15, proximal epiphysis of right ulna
| |
Mammalia | |
Didelphimorphia indet.4 Gill 1872 marsupial See Prevosti&Pardiñas 2009 for a different interpretation
| |
Toxodontidae indet. Scott 1873 notoungulate | |
Pseudotypotherium subinsigne Rovereto 1914 notoungulate | |
Paedotherium minor Cabrera 1937 notoungulate see also ref 70179 where they talk about Paedotherium sp.
| |
Sigmodontinae indet. Wagner 1843 rodent | |
Tetrastylus sp. Ameghino 1886 caviomorph | |
Pithanotomys macer Ameghino 1888 caviomorph
Phtoramys homogenidens Ameghino 1887 caviomorph | |
Neophanomys biplicatus Rovereto 1914 caviomorph | |
Xenodontomys elongatus n. sp.
| |
Pampamys emmonsae Verzi et al. 1995 spiny rat | |
Orthomyctera sp. Ameghino 1889 caviomorph | |
Lagostomus sp. Brookes 1828 viscacha | |
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
| |
Scelidotheriinae indet. Ameghino 1889 edentate | |
Glyptodontidae indet. Burmeister 1879 glyptodon |