Miramar (level 1): Lujanian, Argentina

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Mammalia - Cingulata
Lomaphorus sp. Ameghino 1889
MAMM-PV 016
Mammalia - Cingulata - Glyptodontidae
Panochthus sp. Burmeister 1866
MAMM-PV 024
Glyptodon sp. Owen 1839
MAMM-PV 025
Mammalia - Cingulata - Panochthidae
Neosclerocalyptus sp. Paula Couto 1957
MAMM-PV 021, 022
Mammalia - Mylodontidae
Scelidotherium sp. Owen 1839
MAMM-PV 017
Mammalia - Perissodactyla - Equidae
Equus (Amerhippus) sp. (Hoffstetter 1950)
invalid subgroup of Equus
MAMM-PV 001 - 008
see common names

Geography
Country:Argentina State/province:Cordoba
Coordinates: 30.9° South, 62.7° West (view map)
Paleocoordinates:30.9° South, 62.7° West
Basis of coordinate:stated in text
Geographic resolution:small collection
Time
Period:Quaternary Epoch:Pleistocene
10 m.y. bin:Cenozoic 6
Key time interval:Lujanian
Age range of interval:0.30000 - 0.01170 m.y. ago
Stratigraphy
Formation:Tezanos Pinto
Stratigraphic resolution:group of beds
Stratigraphy comments: The Tezanos Pinto Formation was dated by Kröhling (1999a,b) and Kröhling and Iriondo (1999) by a series of TL age estimates in Santa Fe and Córdoba provinces, and more recently by Kemp et al. (2004) by OSL at the type locality of Tortugas (Santa Fe Province). TL dates at the base of the Tezanos Pinto Formation gave ages of 35.89 ? 1.03 ky BP, 31.69 ? 1.62 ky BP, and 32.00 ky BP. OSL dates obtained by Kemp et al. (2004) suggest that the base of this unit may be considerably older, ca. 149.4 ? 9.5 ky BP. At the top of this formation, TL dates gave ages of 8.15 ? 0.40 ky BP below the paleosol and 9.39 ? 0.63 ky BP (Kröhling, 1999a,b; Kröhling and Iriondo, 1999).

Biostratigraphic mammal assemblage 1: Neosclerocalyptus paskoensise Equus (Amerhippus) assemblage zone with type area and profile based on the San Francisco locality, referred to the Lujanian (late Pleistoceneeearly Holocene), and comparable to the Equus (Amerhippus) neogeus Biozone of Buenos Aires Province;
Lithology and environment
Primary lithology:paleosol/pedogenic poorly lithified muddy siltstone
Includes fossils?Y
Lithology description: The Tezanos Pinto Formation is typical loess, composed of silt, with clay in variable and subordinate amounts, and with rare fine to very fine sand (Kröhling and Iriondo, 1999). The top of this formation is marked by a Hypsithermal palaeosoil, partially eroded, and typi- cally represented by a Bt horizon (Kröhling, 1999a,b; Kröhling and Iriondo, 1999).
Environment:loess
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Reason for describing collection:biostratigraphic analysis
Collection method comments: Cruz 2013 re-examined the specimens & stratigraphy of fossil localities of Cordoba including this one.
Taxonomic list comments:The fossil material of Miramar is housed in the regional museum of Miramar MAMM
Metadata
Database number:197919
Authorizer:P. Mannion Enterer:M. Kouvari
Research group:vertebrate
Created:2018-11-29 08:04:42 Last modified:2018-11-29 08:04:42
Access level:the public Released:2018-11-29 08:04:42
Creative Commons license:CC BY
Reference information

Primary reference:

67447. L. E. Cruz. 2013. Biostratigraphy and geochronology of the late Cenozoic of Córdoba Province (central Argentina). Journal of South American Earth Sciences 42:250-259 [P. Mannion/M. Kouvari]