Middle Miocene (Serravallian; upper Badenian-lower Sarmatian) dinoflagellate cysts from Bad Deutsch-Altenburg, Vienna Basin, Austria

Middle Miocene (Serravallian; upper Badenian-lower Sarmatian) deposits recovered in ten cored boreholes (83 samples) in Bad Deutsch-Altenburg, Vienna Basin, were analysed palynologically for the first time. The strata belong to the Rabensburg Formation of the Baden Group. The lateral distribution of the boreholes in reference to a Mesozoic ridge makes this area interesting for studying various aspects such as deposits distribution, stratigraphy and paleoenvironmental reconstruction. A diverse and well-preserved in-situ dinoflagellate cyst association has been identified. Middle Miocene age-diagnostic species including <i>Unipontidinium aquaeductum, Labyrinthodinium truncatum</i>, <i>Cerebrocysta poulsenii, Habibacysta tectata, Cannosphaeropsis passio</i> and <i>Operculodinium</i>? <i>borgerholtense</i> are recorded. Their occurrences allow correlation with dinoflagellate cyst biozonations on a regional scale. Based on the identified dinoflagellate cysts and by correlation with calcareous nannoplankton and ostracods, from the same set of samples, a Serravallian age – corresponding to a late Badenian and early Sarmatian age (Regional Paratethys Stages) – is confirmed. Reworked (Cretaceous and Paleogene) dinoflagellate cyst assemblages, also well preserved, were recorded abundantly from boreholes HA 521 and HA 573 (SW of the Mesozoic ridge). In accordance with ostracods, the Badenian/Sarmatian boundary can be traced in the upper part of borehole HA 66 based on an abrupt change in the dinoflagellate cyst assemblages. The upper Badenian strata were deposited in a costal to inner shelf environment with terrigenous (siliceous sand and pelite) and carbonate sediments but also palynomorphs. The recorded dinoflagellate cysts reflect marine, tropical to warm-temperate climatic conditions. The composition of the recorded dinoflagellate assemblages is very close to that of the Middle Miocene assemblages of the Mediterranean, indicating water exchanges between the Central Paratethys and the Mediterranean during the late Badenian (early Serravallian).