The Brazilian Quaternary terrestrial Carnivora are represented by the following families: Canidae, Felidae, Ursidae, Procyonidae Mephitidae and Mustelidae. Their recent evolutionary history in South America is associated with the uplift of the Panamanian Isthmus, and which enabled the Great American Biotic Interchange (GABI). Here we present new fossil records of Carnivora found in a cave in Aurora do Tocantins, Tocantins, northern Brazil. A stratigraphical controlled collection in the sedimentary deposit of the studied cave revealed a fossiliferous level where the following Carnivora taxa were present: Panthera onca, Leopardus sp., Galictis cuja, Procyon cancrivorus, Nasua nasua and Arctotherium wingei. Dating by Electron Spinning Resonance indicates that this assemblage was deposited during the Last Glacial Maximum (LGM), at least, 22.000 YBP. The weasel, G. cuja, is currently reported much further south than the record presented here. This may suggest that the environment around the cave was relatively drier during the LGM, with more open vegetation, and more moderate temperatures than the current Brazilian Cerrado.
Os autores estudam 6 espécies de nematódeos encontrados em 21 peixes coletados no Oceano Atlântico na Costa Continental Portuguesa e Costa no Norte da África. Dos 21 peixes necropsiados 7 (33,3%) estavam parasitados por nematódeos. Os hospedeiros bem como os nematódeos encontrados e as freqüências de positividade são as seguintes: 6 exemplares de Beryx decadactylus um dos quais parasitado por Ascarophis morrhuae (16,6%); 3 Lethrinus atlanticus um dos quais parasitado por Luzonema cruzi gen. n. sp. n. (33,3%); 3 Scyliorhynus canicula sendo 2 parasitados por Proleptus obutusus (66,6%); 8 de Raja clavata sendo um parasitado por Proleptus robustus (12,5%) e outro por Pseudanisakis rajae (12,5%); 1 Conger conger parasitado por Cucullanus longispiculum sp. n. (100 %). Pseudanisakis rajae é referido pela primeira vez no Oceano Atlântico e como parasita de Raja clavata. Beryx decadactylus é referido pela primeira vez como hospedeiro de Ascarophis morrhuae.
The evolutionary history of the genus Galictis in South America probably begins after the Great American Biotic Interchange. Two species are recognised: Galictis vittata and Galictis cuja. The latter are more frequently found in open areas in southern South America and the first occurs in humid forests from northern South America to Central America. Apparently, they do not occur in sympatry. Both are differentiate by the presence of a metaconid in the first inferior molar of G. vittata and for its bigger size when compared to G. cuja. The fossil record of Galictis is scarce, G. cuja is known by few specimens from Argentina, Chile and Brazil; G. vittata have only one record from Southern Brazil. The specimens related to this record were collected by Peter Lund and are housed at the Statens Naturhistoriske Museum. However, the specimens published by Lund are not fossils. Thus, it is presented here other unpublished specimens collected by Lund and housed at the same museum that we recognise as the first G. vittata fossils. Additionally, it is described here the first fossil record for G. cuja from the late Pleistocene of Brazil -an almost complete mandible recovered from sedimentary deposits from Central Brazil.
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