INVESTIGADORES
CARLINI Alfredo Armando
artículos
Título:
New Palaeogene cingulates (Mammalia, Xenarthra) from Santa Rosa, Perú and their importance in the context of South American faunas.
Autor/es:
CIANCIO MR.; CARLINI AA.; CAMPBELL KE; SCILLATO-YANÉ GJ
Revista:
JOURNAL OF SYSTEMATIC PALAEONTOLOGY
Editorial:
CAMBRIDGE UNIV PRESS
Referencias:
Lugar: Cambridge; Año: 2013 p. 727 - 741
ISSN:
1477-2019
Resumen:
Abstract. The record of Palaeogene cingulate xenarthrans in low latitudes 33 is very poor. 34 In this sense, the cingulate fauna from the Yurúa River near Santa Rosa in eastern Perú is 35 important because it is one of the oldest known from the Palaeogene from Perú and 36 because of its tropical latitudinal position. Although remains are scarce, we recognize 37 three new taxa: two species of Astegotheriinae (Dasypodidae); Parastegosimpsonia 38 peruana nov. gen. et sp., of small size, related to Eocene species from Patagonia, and 39 another new species, ?Parastegosimpsonia, which consists of an incomplete osteoderm 40 representing the largest species of this tribe. A third species, Yuruatherium tropicalis nov. 41 gen. et sp., of indeterminate suprageneric rank, shares features with Machlydotherium 42 Ameghino (Casamayoran-Tinguirirican SALMA ?middle Eocene-early Oligocene of 43 Patagonia) and is similar to Eocoleophorus Oliveira et al. (Deseadan SALMA ?late 44 Oligocene of Brazil). Also we assign to Yuruatherium nov. gen. the species 45 ?Machlydotherium intortum (from the late Eocene of Patagonia). Sediments bearing 46 these cingulates also yielded rodents, marsupials, and notoungulates, among the most 47 frequent mammals. The absolute age of the sediments is unknown, but an estimated age 48 is inferred from the studies of mammalian assemblages. Even so the age of the Santa 49 Rosa local fauna is still controversial and, given the groups taken into account, could be 50 from early Eocene to late Oligocene. According to sequences of southern cingulate 51 faunas (especially those of Dasypodidae), the cingulates from Santa Rosa also suggest an 52 age between the late Eocene to early Oligocene for the fauna. Nevertheless, the very low 53 latitude of Santa Rosa local fauna should be taken into account because in lower latitudes 54 it is not uncommon to find taxa with a more generalized set of characters than those 55 displayed by taxa of contemporary levels in higher latitudes.