Bryozoan–serpulid–algal–thrombolite bioherms of up to 50 cm size are described from the
Sarmatian (upper Middle Miocene) of the Central Paratethys. They occur on top of lower …

Abstract The Neogene Vienna Basin (VB) is a major hydrocarbon province with a long
history of exploration accumulating extensive stratigraphic and structural information from …

We present previously unknown stacked bowl-shaped bioherms reaching a size of 45 cm in
diameter and 40 cm in height from weakly solidified peloidal sand from the upper Sarmatian …

Recently, attention has been drawn to the recognition of past seagrass for which a number
of proxies have been proposed. Several studies have quoted ostracods as having some …

Abstract the Late Badenian coralline algae-vermetid reefs and the early Sarmatian serpulid-
microbialite reefs distributed widely in the northeastern and eastern borders of the …

Massive evaporites were discovered in the Soltvadkert Trough (Great Plain, Hungary)
correlating to the Badenian Salinity Crisis (13.8 Ma, Middle Miocene) on the basis of …

In this chapter we describe the geology of the structural units of Hungary in the Alp-
Carpathian orogene system and briefly present the most important stages of their evolution …

Palaeoenvironmental changes in the upper Middle Miocene Central Paratethys were
reconstructed by using qualitative and quantitative palaeontological analyses of foraminifera …

A morphometric analysis was performed for the late Middle Miocene bivalve species lineage
of Polititapes tricuspis (Eichwald, 1829)(Veneridae: Tapetini). Specimens from various …

This is the first documentation of Middle Miocene (late Langhian) stromatolites from the
Central Paratethys Sea. These microbialites formed in a lagoonal setting in the Austrian …