Nouvelle interprétation biochronologique des grands mammifères d'Ubeidiya, Israël

Eisenmann, Véra; Ballesio, Roland; Beden, Michel; Faure, Martine; Geraads, Denis; Guérin, Claude; Heintz, Émile

doi:10.1016/s0016-6995(83)80040-0

Cited by 6 publications

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“…. ,.., ... Azzaroli, 1983;Bonfay, 1990;Bruijn et al, 1992;Debart et al, 1994;Duvernois, Guerin, 1989;Eisenmann et al, 1983;Eisenmann, 1995;Guerin, 1990;Guerin, Faure, 1982;Steininger et al, 1990;Tchernov, Guerin. 1986;Tore et al, 1993;Zubakov, Borzenkova.…”

Section: Biostratigraphic Analysis Of the Faunaunclassified

“…Column III: Mammalian biozones of Guerin for the Plio-Pleistocene in Europe (with some additions and corrections) Column IV: Subdivision of the Villafranchian Column V: Most known West European localities of Villafranchian mammal fauna. (Correlation of 1-V •taking into account the papers byAzzaroli, 1983; Bonfay, 1990;Bruijn et al, 1992; Debart et al, 1994;Duvernois, Guerin, 1989;Eisenmann et al, 1983;Eisenmann, 1995;Guerin, 1990;Guerin, Faure, 1982;Steininger et al, 1990; Tchernov, Guerin. 1986; Tore et al, 1993; Zubakov, Borzenkova.…”

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Varshets and Slivnitsa – new localities of Villafranchian vertebrate fauna from Bulgaria (taxonomic composition, biostratigraphy and climatochronology)

Spassov¹

1997

GeolBalc

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Two recently discovered rich Bulgarian localities have been studied and described as localities of Villafranchian fauna - Varshets and Slivnitsa. They represent two faunistic complexes immediately succeeding one another in time. Varshets is a Late Pliocene locality. After its fauna it ought to be referred to the biochronological zone MNQ 17, that may be subdivided into two successive subzones. It seems that the fauna of this locality is earlier than that of the marker locality St.-Vallier. The fauna of Varshets numbers more than 100 taxa of vertebrates, including 18 species of Macromammalia. The faunistic complex presupposes a mosaic landscape of open spaces and forests or an open ("park") type of forests. After the climato-stratographic subdivision, the fauna falls at SCT12, or even more probably, at the beginning of SCT11. The locality of Slivnitsa refers to the the very end of the Pliocene and the Late Villafranchian. The fauna consisting of 19 species of Macromammalia too, times it to the beginning of the zone MNQ 18, which probably ought to be also divided into subzones – MNQ18a = Seneze Unit (Final Pliocene) and MNQ18b = Olivola Unit (probably Earliest Pleistocene). The time of this fauna corresponds to the intermediate cooling during the Beregovka warming that falls on the superclimatheme SCT10. The predominance of Bovidae, that are typical of the open spaces, indicates more aridic climate than Varshets. Slivnitsa and Seneze are the earliest localities where the first migration wave of Canis s.str. has appeared from the east. This wave having been spread in most regions of Europe at the beginning of the Pleistocene. It seems that Slivnitsa is also the earliest locality reflecting the appearance of the genus Panthera on the continent.

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Section: Biostratigraphic Analysis Of the Faunaunclassified

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confidence: 99%

Varshets and Slivnitsa – new localities of Villafranchian vertebrate fauna from Bulgaria (taxonomic composition, biostratigraphy and climatochronology)

Spassov¹

1997

GeolBalc

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“…Although with some exceptions, the actualized version of this tripartite division of the Villafranchian has been usually accepted now in the stratigraphy of continental deposits in Europe. Further on, a number of authors divide the Late Villafranchian into Late and Final one (Guerin, 1982;Eisenmann et al, 1983;84 Tchemov, Guerin, 1986). Some modem authors have modified the above-mentioned division of the Villafranchian, having stressed on the existence of two main parts in this stage, and namely, the Late Pliocene and Early Pleistocene ones (Bonifay, 1990;Kostopoulos, 1996).…”

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“…The establishment of the boundary Early/ Middle Villafranchian (which could be consid- ,i-- Azzaroli, 1983;Azzaroli et al, 1988;Bonifay, 1990;Bruijn et al, 1992;Debard et al, 1994;Tchemov, Guerin. 1986;Duvemois, Guerin, 1989;Eisenmann et al, 1983;Eisenmann, 1995;Guerin, 1990;Guerin, Faure, 1982;Steininger et al, 1990;Torre et at., 1992;Torre et al, 1993;Zubakov, Borzenkova, 1990;Koufos et al 1995;Kostopoulos, 1996;0. Boeuf-1997 and personal communication r~~mark. The stratigraphic position of the Roccaneyra and Varshets localities is not precised but is within the mentioned limits.…”

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“…Fig.1.Correlation (after Spassov, 1997, with additions) of the climatic and faunistic events of the Late Pliocene and the Early Pleistocene in South Europe (original view-point): Columns I -II: climatostratigraphic scale for Europe -superclimathems (SCD; theirs corelation with the magneto• stratigraphic scale and their calculated absolute age (afterZubakov, Borzenkova, 1990); Column III: The Guerin's mammalian biozones for the Plio-Pleistocene of Europe (with some additions and precisions); Column IV -The Villafranchian subdivision; Column V: The Azzaroli's faunal u. nits and the position of Varshets and Slivnitsa and of some of the most important West European locali~ies of Villafranchian mammalian fauna (The correlation from I to V and the Pliocene-Pleis• tocene boundary-based on publications byAzzaroli, 1983;Azzaroli et al, 1988;Bonifay, 1990;Bruijn et al, 1992;Debard et al, 1994; Tchemov, Guerin. 1986; Duvemois, Guerin, 1989;Eisenmann et al, 1983;Eisenmann, 1995; …”

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The Villafranchian Mammalia fauna and its investigation in Europe, on the Balkans and in Bulgaria

Spassov¹

1997

GeolBalc

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The mammalian fauna of the transition from Pliocene to Pleistocene (usually designated as Villafranchian fauna) is of considerable interest. The first signs of formation of the recent Palearctic fauna should be looked for namely among the Villafranchian one. Because of the fragmentariness of most of the finds and the uneven research degree of different regions, the Villafranchian "Stage" in the mammalian fauna's development remains still insufficiently clarified. The investigations of the Villafranchian fauna are more detailed in W Europe. Corresponding investigations in SE Europe are still more incomplete. Greece and Romania are the only countries of SE Europe with well studied Villafranchian localities. Almost no mammalian megafaunas of that time have been known in Bulgaria so far. Two Bulgarian localities have been recently discovered – Varshets and Slivnitsa. Their investigation has resulted a great richness of vertebrate fossils, so that now they could be placed among the marker localities of Villafranchian fauna within E Europe. Further investigation of the Villafranchian faunistic complexes on the Balkans would considerably contribute to clearing up the migratory routes, the forming and the evolution of this fauna throughout Europe. However, zoogeographical differences are quite probable, thus the biostratigraphic criteria created in W Europe should be applied with a certain attention for the Eastern regions of the continent and especially in the Palearctic areas to the East of Europe.

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Behavioral and Cultural Origins of Neanderthals: A Levantine Perspective

Goren‐Inbar

2011

Vertebrate Paleobiology and Paleoanthropology

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Nouvelle interprétation biochronologique des grands mammifères d'Ubeidiya, Israël

Cited by 6 publications

References 3 publications

Varshets and Slivnitsa – new localities of Villafranchian vertebrate fauna from Bulgaria (taxonomic composition, biostratigraphy and climatochronology)

Varshets and Slivnitsa – new localities of Villafranchian vertebrate fauna from Bulgaria (taxonomic composition, biostratigraphy and climatochronology)

The Villafranchian Mammalia fauna and its investigation in Europe, on the Balkans and in Bulgaria

Behavioral and Cultural Origins of Neanderthals: A Levantine Perspective

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