Where: Cusco, Peru (12.9° S, 71.4° W: paleocoordinates 13.6° S, 67.5° W)
• coordinate stated in text
• small collection-level geographic resolution
When: Santacrucian (17.5 - 16.3 Ma)
• The MD-61 section is 30 m thick. It consists of individual or stacked brownish sandstone bodies (deposited in fluvial channels, point bars, stream floods, and/or waning flows) separated by reddish mudstones with carbonate nodules, further testifying to the presence of a floodplain with frequent subaerial exposure under oxidizing conditions (Fig. 1E). Fossil verte- brate remains are scattered within the lower 5-m thick sand body. This early Miocene sequence is unconformably overlain by unconsolidated Pleistocene terrace conglomerates.
Environment/lithology: "channel"; lithified, medium-grained, coarse, ferruginous, sandy sandstone
Size class: macrofossils
Preservation: original phosphate
Collected in 2011
• MUSM: Museo de Historia Natural de la Universidad Nacional Mayor San Marcos, Lima, Perú
Primary reference: L. Marivaux, R. Salas-Gismondi, J. Tejada, G. Billet, M. Louterbach, JVink, J. Bailleul, M. Roddaz, and P.O. Antoine. 2012. A platyrrhine talus from the early Miocene of Peru (Amazonian Madre de Dios Sub-Andean Zone). Journal of Human Evolution 63:696-703 [C. Jaramillo/J. Ceballos/M. Uhen]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 145126: authorized by Carlos Jaramillo, entered by Juliana Ceballos on 27.05.2013, edited by Andrés Cárdenas
Creative Commons license: CC BY (attribution)
Taxonomic list
Mammalia | |
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cf. Saimiri sp. Voigt 1831 squirrel monkey MUSM-2024: Its size approximates that of the talus of some living large marmosets or small tamarins (Cebidae, Callitrichinae). MUSM-2024 would thus document a tiny Saimiri-like cebine, with the body size of a large marmoset
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Notoungulata sp. Roth 1903 notoungulate |