TY - JOUR
T1 - Middle Miocene vertebrates from the Amazonian Madre de Dios Subandean Zone, Perú
AU - Antoine, Pierre Olivier
AU - Roddaz, Martin
AU - Brichau, Stéphanie
AU - Tejada-Lara, Julia
AU - Salas-Gismondi, Rodolfo
AU - Altamirano, Ali
AU - Louterbach, Mélanie
AU - Lambs, Luc
AU - Otto, Thierry
AU - Brusset, Stéphane
PY - 2013/3/1
Y1 - 2013/3/1
N2 - A new middle Miocene vertebrate fauna from Peruvian Amazonia is described. It yields the marsupials Sipalocyon sp. (Hathliacynidae) and Marmosa (Micoureus) cf. laventica (Didelphidae), as well as an unidentified glyptodontine xenarthran and the rodents Guiomys sp. (Caviidae), " Scleromys" sp., cf. quadrangulatus-schurmanni-colombianus (Dinomyidae), an unidentified acaremyid, and cf. Microsteiromys sp. (Erethizontidae). Apatite Fission Track provides a detrital age (17.1 ± 2.4 Ma) for the locality, slightly older than its inferred biochronological age (Colloncuran-early Laventan South American Land Mammal Ages: ~15.6-13.0 Ma). Put together, both the mammalian assemblage and lithology of the fossil-bearing level point to a mixture of tropical rainforest environment and more open habitats under a monsoonal-like tropical climate. The fully fluvial origin of the concerned sedimentary sequence suggests that the Amazonian Madre de Dios Subandean Zone was not part of the Pebas mega-wetland System by middle Miocene times. This new assemblage seems to reveal a previously undocumented " spatiotemporal transition" between the late early Miocene assemblages from high latitudes (Patagonia and Southern Chile) and the late middle Miocene faunas of low latitudes (Colombia, Perú, Venezuela, and ?Brazil).
AB - A new middle Miocene vertebrate fauna from Peruvian Amazonia is described. It yields the marsupials Sipalocyon sp. (Hathliacynidae) and Marmosa (Micoureus) cf. laventica (Didelphidae), as well as an unidentified glyptodontine xenarthran and the rodents Guiomys sp. (Caviidae), " Scleromys" sp., cf. quadrangulatus-schurmanni-colombianus (Dinomyidae), an unidentified acaremyid, and cf. Microsteiromys sp. (Erethizontidae). Apatite Fission Track provides a detrital age (17.1 ± 2.4 Ma) for the locality, slightly older than its inferred biochronological age (Colloncuran-early Laventan South American Land Mammal Ages: ~15.6-13.0 Ma). Put together, both the mammalian assemblage and lithology of the fossil-bearing level point to a mixture of tropical rainforest environment and more open habitats under a monsoonal-like tropical climate. The fully fluvial origin of the concerned sedimentary sequence suggests that the Amazonian Madre de Dios Subandean Zone was not part of the Pebas mega-wetland System by middle Miocene times. This new assemblage seems to reveal a previously undocumented " spatiotemporal transition" between the late early Miocene assemblages from high latitudes (Patagonia and Southern Chile) and the late middle Miocene faunas of low latitudes (Colombia, Perú, Venezuela, and ?Brazil).
KW - Biochronology
KW - Biogeography
KW - Colloncuran-early Laventan
KW - Fission track age
KW - Marsupialia
KW - Rodentia
KW - Biochronology
KW - Biogeography
KW - Colloncuran-early Laventan
KW - Fission track age
KW - Marsupialia
KW - Rodentia
UR - https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84871158942&origin=inward
UR - https://www.scopus.com/inward/citedby.uri?partnerID=HzOxMe3b&scp=84871158942&origin=inward
U2 - 10.1016/j.jsames.2012.07.008
DO - 10.1016/j.jsames.2012.07.008
M3 - Article
SN - 0895-9811
VL - 42
SP - 91
EP - 102
JO - Journal of South American Earth Sciences
JF - Journal of South American Earth Sciences
ER -