Multiproxy reconstruction of the middle Miocene Požega palaeolake in the Southern Pannonian Basin (NE Croatia) prior to the Badenian transgression of the Central Paratethys Sea

Mandić, Oleg; Hajek–Tadesse, Valentina; Bakrač, Koraljka; Reichenbacher, Bettina; Grizelj, Anita; Miknić, Mirjana

doi:10.1016/j.palaeo.2018.12.003

Cited by 20 publications

(10 citation statements)

References 51 publications

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“…Sev eral sam ples, pre vi ously assigned in lab re ports to the Oligocene to early Mio cene in ter val, con tain palynological as sem blages typ i cal of mid dle to up per Mio cene de pos its of the Dacian Ba sin (Ro man and Papaianopol, 1982;£abãrã, 2008, 2014, Casas-Gallego et al, 2020a, mainly gym no sperms (Pinuspollenites, Piceapollis, Abiespollenites, Taxodiaceae) and an gio sperms (e.g., Tricolporopollenites, Caryapollenites, Quercopollenites, Faguspollenites, Sabalpollenites, Tiliapollenites, Alnipollenites, Chenopodiaceae). Among the spores con sid ered as mark ers for the early Mio cene, Mecsekisporites mioceanicus Nagy mainly oc curs in the mid dle Mio cene (Badenian) of the Pannonian Ba sin (Nagy, 2005;Mandic et al, 2019).…”

Section: Palynomorphsmentioning

confidence: 99%

Biostratigraphic re-evaluation of the lower to middle Miocene succession in the Eastern Carpathians: a case study related to the oil fields of the Diapir Fold Zone, Romania

Filipescu

Tămaș²,

Bercea³

et al. 2020

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Section: Palynomorphsmentioning

confidence: 99%

Biostratigraphic re-evaluation of the lower to middle Miocene succession in the Eastern Carpathians: a case study related to the oil fields of the Diapir Fold Zone, Romania

Filipescu

Tămaș²,

Bercea³

et al. 2020

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“…The typical sedimentary successions of the initial basal Lower-Middle Miocene (Ottnangian-Lower Badenian according to Pavelić and Kovačić 2018 and references therein) NCB include continental, alluvial and lacustrine (Southern Pannonian Basin Lake System, SPBLS sensu Mandić et al 2019a) sediments unconformably overlying the strongly tectonized and lithologically heterogeneous pre-Neogene basement (GKRH 2009). The alluvial-lacustrine series of the NCB is generally overlain by Middle Miocene (Badenian) transgressive marine deposits representing a widespread ingression of the Paratethys Sea into the NCB (Ćorić et al 2009;Mandic et al 2012Mandic et al , 2019aMarković 2017;Pavelić and Kovačić 2018). The Ottnangian-Middle Badenian phase of NCB evolution is regarded as syn-rift (Pavelić and Kovačić 2018; see also Balázs et al 2016).…”

Section: North Croatian Basin (Carpathian-pannonian Region)mentioning

confidence: 99%

“…(1) tephrochronology, volcanic provenance and petrogenesis, as well as geodynamic setting of NCB volcaniclastic and volcanic rocks (e.g., Pamić and Balen 2001a;Pécskay et al 2006;Seghedi and Downes 2011;Mandic et al 2012;Lukács et al 2018), and (2) timing of the initial Miocene CP flooding of the NCB (Brlek et al 2018;Pavelić and Kovačić 2018;Mandic et al 2019a). The Lower-Middle Miocene Mts.…”

Section: Introductionmentioning

confidence: 99%

Miocene syn-rift evolution of the North Croatian Basin (Carpathian–Pannonian Region): new constraints from Mts. Kalnik and Požeška gora volcaniclastic record with regional implications

Brlek

Kutterolf

Gaynor

et al. 2020

Int J Earth Sci (Geol Rundsch)

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Mts. Kalnik and Požeška gora volcaniclastic sequences hold valuable information concerning the Miocene syn-rift evolution of the North Croatian Basin, and the evolution of the Carpathian-Pannonian Region and the Central Paratethys. We present volcanological, high-precision geochronological, and compositional data of volcanic glass to constrain their tephrochronology, magmatic provenance, and timing of the initial Central Paratethys flooding of the North Croatian Basin. Based on CA-ID-TIMS U-Pb zircon ages (18.060 ± 0.023 Ma for Mt. Kalnik and 15.345 ± 0.020 Ma for Mt. Požeška gora) and coeval 40 Ar/ 39 Ar sanidine ages (18.14 ± 0.38 Ma and 18.25 ± 0.38 Ma for Mt. Kalnik and 15.34 ± 0.32 Ma and 15.43 ± 0.32 Ma for Mt. Požeška gora), Mt. Kalnik rhyolitic massive ignimbrites and Mt. Požeška gora rhyolitic primary volcaniclastic turbidites are coeval with Carpathian-Pannonian Region Miocene post-collisional silicic volcanism, which was caused by lithospheric thinning of the Pannonian Basin. Their affiliation to Carpathian-Pannonian Region magmatic activity is supported by their subduction-related geochemical signatures. Although Mts. Kalnik and Požeška gora volcaniclastics are coeval with the Bükkalja Volcanic Field Csv-2 rhyolitic ignimbrites, North Alpine Foreland Basin, Styrian Basin, Vienna Basin, and Dinaride Lake System bentonites and volcaniclastic deposits, reliable tephrochronological interpretations based on comparison of volcanic glass geochemical composition are not possible due to a lack of data and/or methodological discrepancies. Our new high-precision geochronology data prove that the initial Middle Miocene (Badenian) marine flooding of parts of the North Croatian Basin occurred at least ~ 0.35 Ma (during the NN4 Zone) before the generally accepted ~ 15 Ma maximum flooding age at the basin scale, calibrating the timing of the onset of the widespread "mid-Langhian" Central Paratethys flooding.

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“…Congeriinae shells are usually strongly leached, available only as external or internal moulds (Mandic et al . 2019a). The material is dominated by young and juvenile individuals and shell fragments, yet contains a number of fully preserved adult valves.…”

Section: Systematic Palaeontologymentioning

confidence: 99%

The Serbian Lake System: a stepping stone for freshwater molluscs in the middle Miocene

Neubauer

Mandić

Jovanović

et al. 2020

Papers in Palaeontology

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The first in-depth revision of a lacustrine freshwater mollusc fauna of the Serbian Lake System (SLS) is carried out. We describe and discuss well-preserved faunas from two localities in central and southern Serbia (Ma dere and Medo sevac), along with the reinvestigation of type material of several species described in the late nineteenth and early twentieth centuries. Our revision yields 14 species of gastropods, with the families Hydrobiidae (six species) and Planorbidae (four species) being most abundant, along with one species each of Neritidae, Melanopsidae, Bithyniidae and Bulinidae, as well as two dreissenid bivalve species. Three of the hydrobiid gastropods are new to science, Prososthenia milosevici sp. nov., Prososthenia? naissensis sp. nov., and Prososthenia rundici sp. nov., and so is the bivalve Trigonipraxis madjerensis sp. nov.

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Multiproxy reconstruction of the middle Miocene Požega palaeolake in the Southern Pannonian Basin (NE Croatia) prior to the Badenian transgression of the Central Paratethys Sea

Cited by 20 publications

References 51 publications

Biostratigraphic re-evaluation of the lower to middle Miocene succession in the Eastern Carpathians: a case study related to the oil fields of the Diapir Fold Zone, Romania

Biostratigraphic re-evaluation of the lower to middle Miocene succession in the Eastern Carpathians: a case study related to the oil fields of the Diapir Fold Zone, Romania

Miocene syn-rift evolution of the North Croatian Basin (Carpathian–Pannonian Region): new constraints from Mts. Kalnik and Požeška gora volcaniclastic record with regional implications

The Serbian Lake System: a stepping stone for freshwater molluscs in the middle Miocene

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