Search results for "Miocene"

showing 6 items of 116 documents

New species of Deinogalerix (Mammalia, Eulipotyphla) from the late Miocene of Scontrone (Abruzzo, central Italy)

2017

Deinogalerix is a typical component of the late Miocene insular fauna of Gargano (south-eastern Italy). Remains of this taxon had also been found over the last 20 years at the early Tortonian site of Scontrone (Abruzzo, central Italy), but they had never been described in detail. Two new species are introduced. One of them, D. samniticus sp. nov., is larger sized and better documented, and received a formal description. The other entity is clearly distinct from D. samniticus sp. nov., but it is merely represented by a single mandible. It is therefore presented here as a different, but undetermined species, Deinogalerix sp. Comparative analyses show that the new species have exclusive dental…

new speciesAbruzzo (central Italy)endemisminsular colonizationlate MioceneSettore GEO/01 - Paleontologia E PaleoecologiaDeinogalerix
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Vasseuromys rambliensis sp. nov. (Gliridae, Mammalia) from the Ramblian (Lower Miocene) of the Tudela Formation (Ebro basin, Spain)

2012

In this paper, a new species of Vasseuromys, V. rambliensis sp. nov., from the locality Pico del Fraile 1 (PF1, Ebro basin, North-eastern Spain) is described. The association of Ligerimys, Peridyromys murinus and Simplomys simplicidens, and the absence of Eucricetodon and Democricetodon, allows dating of the PF1 locality as Late Ramblian (Early Miocene, MN3, local zone A). Main diagnostic features of V. rambliensis sp. nov. are the presence of four extra ridges in the lower molars, a very reduced anterotropid and a metaloph connected to the posteroloph and not to the protocone. The size and morphology of V. rambliensis sp. nov. are very close to V. bacchius from the upper part of unit MN2, …

new speciesEspañaMioceneBiostratigraphyStructural basinOceanographyCuenca EbroProtoconePaleontologyRamblianGenusGliridaeGeology
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Paleoclimatic changes in the Serravallian record of the Mediterranean area

2004

planktonic foraminiferaPaleoclimatology; planktonic foraminifera; stable isotope; Miocene; Mediterraneanstable isotopeMioceneMediterraneanSettore GEO/01 - Paleontologia E PaleoecologiaPaleoclimatologyPaleoclimatology planktonic foraminifera stable isotope late Middle Miocene MediterraneanSettore GEO/08 - Geochimica E Vulcanologia
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Nuevas faunas de micromamíferos del Terciario continental de la Depresión Intermedia (provincia de Cuenca, España centro-oriental)

1986

In this paper the fossil content of nine new micromammal bearing localities and that of 15 levels in a borehole from the Loranca Basin (eastern Tague Basin, Prov. of Cuenca) is described. The age ranges from early Arvernian (Late Oligocene) to Turolian (Late Miocene). 47 rodent and lagomorph taxons have been found which are arranged in 8 biostratigraphic units. The Loranca-2 borehole contains 15 fossiliferous levels covering the Upper Oligocene/Lower Miocene. These additional data complete the faunal sequence published by Díaz & López(1919). The stratigraphic framework of the basin needs a revision because of the new faunal data.<br><br>Se presenta una serie de 9 nuevos yaci…

secuencia estratigráfica.Depresión IntermediaBiozoneStructural basinLate Miocenesondeo MicromamíferosSequence (geology)PaleontologyLoranca basinmicromamalsdepresión intermediamicromamíferosQE1-996.5sondeocontinentalborcholelcsh:QE1-996.5biostratigraphic sequence.Terciario continentalGeologyterciario continentallcsh:GeologyMicromamíferosTertiaryGeologyEstudios Geológicos
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Integrated analyses of syn-tectonic basin fill to costrain the deformation evolution in a fold thrust belt: field examples from the sicilian chain

2011

sedimentary basins synsedimentary tectonics Sicily late Miocene early Pliocene
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Mystemys giganteus n. gen. et sp.: an enigmatic and rare cricetid from the Terre Rosse M013 fissure filling (Gargano, Southeastern Italy).

2016

Mystemys giganteus is a new strongly endemic cricetid that occurs only in the recently discovered M013 Terre Rosse fissure filling of the Gargano area. This species was presented alongside the other taxa of the M013 fissure in a previous paper and it is here described in detail. Although the material includes only five molars, Mystemys is exceptional for its very large size (length of M1: 6.23 mm) and peculiar morphology. The molars are heavy built with bulged and robust cusps, tubercular crests, narrow valleys, very thick and crenulated enamel. The morphological features of Mystemys are very carefully described, with special focus on the evolutionary modifications induced by isolation. The…

taxonomyinsular domainevolutionMioceneSettore GEO/01 - Paleontologia E PaleoecologiaCricetidae
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