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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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(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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(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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(Upper Miocene, Lake Pannon, cement marls, lithology, stratigraphy, paleomagnetism, Beočin, Fruška Gora)
Early to Late Miocene (FODOR et al.2005). Late Early Miocene subsidence and sedimentation was an effect of the syn-rift extension phase thatresulted in the formation of various grabens filled byThe Upper Miocene Lake Pannon

Sarmatian consists of hetThe Upper Miocene Lake Pannon marl from the Filijala Open Pit (Beočin, northern Serbia): new geological and ... 97Fig. 2. Geological cross-section A–B through the Miocene sediments on the Filijala Open

work presents major lithological, structural, paleontological and paleomagnetic characteristics of the Upper Miocene Pannonian marl in the Filijala Open Pit of the La Farge Cement Plant near Beočin,northern Serbia. Pannonian


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(Lower Middle Miocene, Badenian limestone, post-Badenian lateritic clays, paleomagnetism, Fruška Gora Mt.)
enabledthe discovery of different Miocene units (undivided the Lower Miocene and Middle Miocene Badenian, predominantly). This is primarily thinking of the so-called Leitha limestone (Middle Miocene, Badenian), whichis an important

постојање различитих миоценских јединица (нерашчлањен доњи миоцен ипрвенствено, баденски кат средњег миоцена). Овде се говори пре свега о тзв. лајтовачким кречњацима(средњи миоцен, баден), важној компоненти у производњи цемента (Лафарж

incross section and boreholes); 2, 3, Lower Miocene lacustrine deposits and volcanites (only in cross section andboreholes); 4, Middle Miocene (Badenian) reef limestone;5, 6, Middle Miocene (Badenian) sandy marl and sandyclay; 7