Palaeoecology and sedimentology of the Miocene marine and terrestrial deposits in the “Medieval Quarry” on Devínska Kobyla Hill (Vienna Basin)

Pivko, D.; Hudáčková, N.; Hrabovský, J.; Sládek, I.; Ruman, A.

doi:10.7306/gq.1357

Artykuł - szczegóły

Tytuł artykułu

Palaeoecology and sedimentology of the Miocene marine and terrestrial deposits in the “Medieval Quarry” on Devínska Kobyla Hill (Vienna Basin)

Autorzy

Pivko D. , Hudáčková N. , Hrabovský J. , Sládek I. , Ruman A.

Treść / Zawartość

Pełne teksty:

Pivko_D_Palaoecology__Geol. Quart._Vol. 61_No 3_2017.pdf

Pobierz

Identyfikatory

DOI

10.7306/gq.1357

Warianty tytułu

Języki publikacji

Abstrakty

Dramatic tectonic and sea level changes of the Central Paratethys realm during the Middle Miocene resulted in changes of the coastal and seabed morphology affecting the composition of the marine association and the distribution of the facies along the coast. Three different episodes (marine-terrestrial-marine) in the environmental evolution are interpreted. A lower marine unit (Badenian; Lower Serravallian) reflects organodetrital sedimentation on and around an algal bioherm. Low terrigenous input maërl facies of typical rhodalgal carbonate factory type characterise the top of the algal mound. On the slopes, a rim of rhodechfor facies separated the bioherm from the rest of the bottom which had a seagrass cover. This high-energy rhodechfor carbonate factory is described from the Central Paratethys realm for the first time. It is composed mostly of coralline algae (Mesophyllum, Lithothamnion, Spongites and Lithophyllum), benthic foraminifers (Elphidium crispum, Neoconorbina terquemi, Miniacina sp., Borelis melo), echinoids (cidaroid, spatangoid and diadematoid groups) and bryozoans. Uplift of the Malé Karpaty Mts. resulted in tectonic activity in the vicinity, documented by the presence of clastic dikes and normal faults in the profile studied. Subsequent fluvial and terrestrial sedimentation is represented by regolith, palaeosoil and channel body deposits set discordantly on the top of lagoonal deposits. Finally, the third episode is represented by the Sarmatian transgressive marine sequence, which is characterized by coarse pebbly deposit eroded from an uplifted pre-Neogene basement. The strata studied originated in a warm temperate climate around the Badenian–Sarmatian transition.

Słowa kluczowe

rhodechfor rhodalgal palaeoecology sedimentology Middle Miocene Central Paratethys

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2017

Tom

Vol. 61, No. 3

Strony

549--568

Opis fizyczny

Bibliogr. 116 poz., rys., tab., wykr.

Twórcy

autor

Pivko D.

pivko@fns.uniba.sk

Comenius University, Faculty of Natural Sciences, Department of Geology and Paleontology, Mlynská dolina, Ilkovičova 6, 842 15 Bratislava, Slovakia

autor

Hudáčková N.

Comenius University, Faculty of Natural Sciences, Department of Geology and Paleontology, Mlynská dolina, Ilkovičova 6, 842 15 Bratislava, Slovakia

autor

Hrabovský J.

Slovak Academy of Sciences, Earth Science Institute, Dúbravská cesta 9, 840 05 Bratislava, Slovakia

autor

Sládek I.

Comenius University, Faculty of Natural Sciences, Department of Geology and Paleontology, Mlynská dolina, Ilkovičova 6, 842 15 Bratislava, Slovakia

autor

Ruman A.

Comenius University, Faculty of Natural Sciences, Department of Geology and Paleontology, Mlynská dolina, Ilkovičova 6, 842 15 Bratislava, Slovakia

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Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).

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Bibliografia

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