Sarmatian (Late Middle Miocene) gastropod assemblages of the central Paratethys

M Harzhauser, T Kowalke - Facies, 2002 - Springer
M Harzhauser, T Kowalke
Facies, 2002Springer
A rather diverse gastropod fauna from Sarmatian deposits of the Austrian/Hungarian
Eisenstadt-Sopron Basin was studied. The fauna derives from two layers of clay and silt
within a siliciclastic section at St. Margarethen in Burgenland (Austria). These layers are
interpreted as littoral mudflats which formed during the Sarmatian (Late Middle Miocene)
along the western coast of the Central Paratethys. Strong shifts in the composition of the
gastropod fauna, dominated by Potamididae (Cenogastropoda: Cerithioidea), within each …
Summary
A rather diverse gastropod fauna from Sarmatian deposits of the Austrian/Hungarian Eisenstadt-Sopron Basin was studied. The fauna derives from two layers of clay and silt within a siliciclastic section at St. Margarethen in Burgenland (Austria). These layers are interpreted as littoral mudflats which formed during the Sarmatian (Late Middle Miocene) along the western coast of the Central Paratethys. Strong shifts in the composition of the gastropod fauna, dominated by Potamididae (Cenogastropoda: Cerithioidea), within each layer indicate successions of limnic-fluvial to oligohaline, brackish-littoral, and marine-littoral environments. These shifts in facies are reflected by an alternational of thePotamides hartbergensis assemblage,Granulolabium bicinctum assemblage, and thePotamides disjunctus assemblage.
The speciesJujubinus turriculus (Eichwald, 1850),Gibbula buchi (Dubois, 1831), andCylichnina elongata (Eichwald, 1830) are reported for the first time from the Sarmatian of the Paratethys.Mitrella agenta nov. sp. (Neogastropoda: Columbellidae) is introduced as a new species. These species might represent relics of the diverse Badenian fauna but could also prove a minor ingression of marine species from an adjacent bioprovince in the Late SarmatianMactra “Zone”.
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