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Título

An exceptional small vertebrate fauna from the latest middle Miocene of Austria

AutorPrieto, Jérôme; Vasilyan, Davit; Böhme, Madelaine; Gross, Martin; Angelone, Chiara; Casanovas-Vilar, Isaac; Hír, Janós; Hoek Ostende, L. van den; Maul, L.
Palabras clavePalaeoecology
Micromammals
Miocene
Austria
Biogeography
Fecha de publicación2014
CitaciónXII EAVP Meeting (2014)
ResumenThe late Middle Miocene is fascinating for the study of terrestrial palaeoecosystems: following the long period of the Middle Miocene Climatic Optimum, drastic climatic changes induced important faunal re-arrangement and migration within Europe. Rich and diverse fossil faunas are thus of primary importance for the understanding of these processes. The late Middle Miocene is well recorded in various Iberian basins, but complete faunas of this period are rare in Central Europe. Therefore, the recent discovery of an exceptional fossil assemblage of macroand micro-vertebrates in Gratkorn (early Late Sarmatian, Austria, Styria), allows a fresh look on the palaeocommunity following the Mid-Miocene cooling. Based on the degree of corrosion on the dental elements and the presence of pellets, most, but not all, of the small mammal remains (19 species) are tentatively interpreted as a result of accumulation by nocturnal raptors. Probably, part of the fossorial indviduals of the lower vertebrate (including two fish, eight amphibian and 17 reptile taxa) might have been buried in situ, maybe in their own burrows in the sandy soil Lower vertebrates, small mammals and molluscs occur in abundance in the same thin fossil enriched layer, and give a mixed picture of the environment: relatively sparsely vegetated floodplainwith sandysoils, including short-lived ponds, streams or rivulets in the close vicinity, relatively open landscapes, with a dry, semi-arid climate. Indications of „forested area“ are indicated by the gliding mammals. This could indicates the presence of different microhabitats around the excavation place, but mayalso be a taphonomical artefact based on various different agents of accumulation contributingto the thanatocoenosis. Nevertheless, the extreme quick accumulation (decades?) of the fossils.
DescripciónTalk delivered in XII EAVP Meeting – Torino 24-28 June 2014, organized by Dipartimento di Scienze della Terra, Università degli Studi di Torino
URIhttp://hdl.handle.net/10261/124634
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