NDLI: Depositional environment changes during the early–late Serravallian boundary dated by the Central Paratethys bioevents

Content Provider	Springer Nature Link
Author	Ruman, Andrej Rybár, Samuel Hudáčková, Natália Šujan, Michal Halásová, Eva
Copyright Year	2017
Abstract	The early–late Serravallian boundary (Badenian–Sarmatian) is a key interval for understanding Central Paratethys evolution. Environmental changes resulted in a great regional faunal turnover known as the Badenian-Sarmatian extinction event (BSEE). Here, we present a high-resolution sedimentological and biostratigraphical study from a rare site located on the Vienna and Danube basin junction (Slovakia). Four Middle Miocene depositional cycles/episodes ranked between 13.1 and 12.6 Ma are described in detail: (1) early Serravallian (13.1 Ma or older) shallow-marine episode; (2) early Serravallian (Badenian; Bulimina–Bolivina biozone; ~13.1 Ma or younger) outer shelf cycle; (3) late Serravallian (Sarmatian; large Elphidia biozone; ~12.6 Ma or younger) inner shelf cycle; (4) late Serravallian? A sedimentary episode represented by a scour filled with a reworked Serravallian (Upper Badenian and Sarmatian) material. The middle Miocene strata are overlaying and discordantly separated by Quaternary fluvial (floodplain) sediments (2.58 Ma or younger). These episodes reflect the early–late Serravallian turnover documented in the bioevents and in the sedimentological record.
Starting Page	1
Ending Page	13
Page Count	13
File Format	PDF
ISSN	01729179
Journal	Facies
Volume Number	63
Issue Number	2
e-ISSN	16124820
Language	English
Publisher	Springer Berlin Heidelberg
Publisher Date	2017-01-16
Publisher Place	Berlin, Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Vienna Basin Middle Miocene Quaternary Sedimentology Bioevents Biogeosciences Geochemistry Paleontology Ecology
Content Type	Text
Resource Type	Article
Subject	Geology Stratigraphy Paleontology

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