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(miocene, Badenian, whale, Paratethys, Bosnia)
and Parathethyc Seaways (Oligocene to Miocene). Annalen des Naturhistorischen Museums in Wien,99A: 279–310.SABOL, M. & HOLEC, P. 2002. Temporal and spatial distribution of Miocene mammals in the western Carpathians(Slovakia)

theworld, their morphology and evolution is not wellknown (FORDYCE & DE MUIZION 2001). In Europe, thePliocene and Miocene species of whales seem to havebeen the most abundant and they were also present inCentral Europe in the region

marine fauna which was once present in theParatethys. Cetacea became extinct during the finalstages of the Miocene, when the Paratethys became afresh water lacustrine environment. The presence offossil whales is thus and indicator







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ensis (HE et al., 2010, LI et al.,2016); Iran, Miocene (GABRIELYAN at al., 2012);Kazahstan Eocene, Oligocene and Miocene (VASILEV,1961; SNIGIREVSKAYA, 1974); Poland, Miocene, onlyreceptacles (KOWALSKI, 2016); Russia, Eocene

нађених у Беранском басену лако се може пратити смена вегетација током миоцена. Године 1995., на локалитету Росуље (Берански басен) у слојевим доњег миоцена, први пут су нађени остацилистова и коренова акватичних – флотантних

fossil plant specimens from the locality Luge (Lower Miocene) and sent them to theNatural History Museum in Belgrade, to the curatorPavle Ivanovič Černjavski. Middle Miocene flora atthe locality Jasikovac was recorded in 1985










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(subsurface geology, blocks subsidence, Upper Cretaceous, Miocene, Quaternary, Belgrade)
Stratigraphically, they correspond to the Middle Miocene Sarmatian and Upper Miocene Pannonian Stage (see LASKAREV et al. 1932; STEVANOVIĆ 1977; KNEŽEVIĆ &ŠUMAR 1993).The Middle Miocene Sarmatian brackish-marinesediments lie un

several different Miocene and Quaternary units. In the deepestborehole DB-6, the flysch deposits were found at a depth of 80 meters. On the left bank of the Sava River inNew Belgrade, only Upper Miocene Pannonian marls and

and the core samples fromthe borehole DB-9. Key: K-Pg, Upper Cretaceous–Paleogene; Sm, Middle Miocene Sarmatian; Pn, Upper Miocene Pannonian; Q1, Pleistocene, Q2, Holocene.Fig. 3. The stratigraphic column and the core samples


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words: bunodont, zygodont, elephantoid, Gomphotherium, Zygolophodon, Miocene, Kruševac Basin,Serbia.Апстракт. Зуби елефантоида из касног-раног и средњег миоцена Европе често показују мешавинебунодонтних и зигодонтних карактеристика

(France, MN7), Wartenberg(Germany, MN8), Bitola (FYR Macedonia, Miocene)(TASSY, 1977; GÖHLICH, 1998; GAREVSKI et al., 2012);G. angustidens: Feldmoching (Germany, Miocene),Achldort (Germany, MN7), Simorre (France, MN7),En Péjouan

fragmented m3 fromKruševac Basin is (most probably) Miocene-aged. It isknown that the Basin sedimentary fill contains EarlyA new elephantoid dental specimen from the Miocene of Kruševac Basin in Central SerbiaGeol. an. Balk



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(Middle Miocene, Badenian, marine transgression, Vrdnik Coal Basin, northern Serbia)
has been reconstructed. The following stratigraphic units were documented: the Lower Miocene,the Middle Miocene Badenian, the Upper Miocene?Pontian, as well as different terrestrial sediments ofPleistocene age, including the

суперпозиционом поретку, присутне суследеће стратиграфске јединице: континенталнојезерски доњи миоцен, морски средњи миоцен баден, горњи миоцен ?понт, те различите плеистоценске наслаге (првенствено тзв. сремска серија илесно-пал

укаже на дискордантан и трансгресиван однос између нерашчлањеног континентално - језерског доњег миоцена и морског средњег миоцена, бадена. Различити копнени и језерски седименти указују на врло мобилну и динамичну палеосредину


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Lake System: integrated results from Middle Miocene Lake Popovac. Nevvsletter on Stratigraphy, 5 1 (1 ]: 117-143.S pajić, 0. 1975. Miocen Braničeva (stratigrafski prikaz) [Miocene of Braničevo (stratigraphic re- view) - in

heteromorphus D e f l a n d r e correspond to this biostrati- graphic level. During the late Early Miocene and Middle Miocene (Badenian), the climate in the Central Paratehys was mainly subtropical. This is supportedAncTpaKT

marine Middle Miocene de- posits of the Serbian Neogene are still considered problematic. The facies distribution, stratigraphy, and tectonic structure of the Belgrade area which com prises early and middle Miocene sediments