A new elephantoid dental specimen from the Miocene of Krusevac basin in Central Serbia

Radović, Predrag; Bradić-Milinović, Katarina

doi:10.2298/gabp1802001r

Cited by 3 publications

(2 citation statements)

References 13 publications

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“…The fossil shark teeth from Serbia have been poorly studied in comparison with other fossils (e.g. ĐURIĆ et al, 2017: RADOVIĆ & BRADIĆ-MILINKOVIĆ, 2018 ). The Middle Miocene (Badenian) sediments from Serbia are exposed in various regions of the country.…”

Section: Introductionmentioning

confidence: 99%

Middle Miocene shark teeth from the southern margin of the Pannonian basin system (Serbia, Central Paratethys)

Jovanović¹,

Trif

Codrea

et al. 2019

Geol An Balk Poluos

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This paper describes Middle Miocene (Badenian) shark teeth from Serbia and discusses their geographical distribution at other localities of the Central Paratethys. The shark teeth originate from Višnjica (near Belgrade), from Višnjica Clay, or the 'Pleurotoma Clay'. The variety of sharks is very low, but according to these fossils Višnjica is the richest among Serbian localities. The sharks teeth reported in the paper belong to the following taxa: Otodus (Megaselachus) megalodon (AGASSIZ, 1835), Hemipristis serra AGASSIZ, 1835 and Odontaspididae indet. The high diversity of invertebrates (molluscs, echinoids, corals etc.) and other coeval fossil assemblages indicate a warm period (the Middle Miocene Climatic Optimum), which preceded the Middle Miocene Climatic Transition.

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Section: Introductionmentioning

confidence: 99%

Middle Miocene shark teeth from the southern margin of the Pannonian basin system (Serbia, Central Paratethys)

Jovanović¹,

Trif

Codrea

et al. 2019

Geol An Balk Poluos

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“…The Paleogene and Neogene deposits in last few years were investigated from different aspects (e.g. đOrđevIć-MILuTINOvIć, 2018;radOvIć, 2018;jOvaNOvIć et al, 2019a, b) and this paper is one more contribution to knowledge of these deposits.…”

Section: Introduction -Geological Settingmentioning

confidence: 99%

Palaeoflora of Kamenica (Pranjani basin, western Serbia)

Lazarević

Milovanović²,

Milivojević

et al. 2019

Geol An Balk Poluos

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Palaeofloras of the Paleogene in Serbia are relatively rare, especially in comparison with floras from Neogene sediments. Most Paleogene phytoassociations from the territory of Serbia existed in a dry and warm climate. The youngest Paleogene phytoassociation originates from the Pranjani Basin (Western Serbia), locality Kamenica. The age of this palaeoflora is determined as Late Oligocene. This fossil plant assemblage is different from other Paleogene phytoassociations. The palaeoflora from Kamenica is characterized with leaf imprints larger than in other Paleogene fossil floras. Furthermore, it differs in taxonomical composition. The prevailing forms are conifers and representatives of broad-leaved evergreen forests. In other Paleogene phytoassociations, elements of broad-leaved evergreen forests are extremely rare. The dominating elements in the palaeoflora of Kamenica are the conifers, especially Glyptostrobus, Pinus, Sequoia and Tetraclinis. The representatives of the broad-leaved evergreen forests are Laurus, Magnolia, ?Quercus?, etc. [Project of the Serbian Ministry of Education, Science and Technological Development, Grant no. 176015, Grant no. 33003 and Grant no. 176016]

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The proboscidean fauna (Mammalia) from the middle Miocene lignites of Gračanica near Bugojno (Bosnia–Herzegovina)

Göhlich

2020

Palaeobio Palaeoenv

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A new elephantoid dental specimen from the Miocene of Krusevac basin in Central Serbia

Cited by 3 publications

References 13 publications

Middle Miocene shark teeth from the southern margin of the Pannonian basin system (Serbia, Central Paratethys)

Middle Miocene shark teeth from the southern margin of the Pannonian basin system (Serbia, Central Paratethys)

Palaeoflora of Kamenica (Pranjani basin, western Serbia)

The proboscidean fauna (Mammalia) from the middle Miocene lignites of Gračanica near Bugojno (Bosnia–Herzegovina)

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