Abstract We describe the Late Pliocene paleoenvironment and paleoclimate of the Pula
fossil site of the western Pannonian Basin, Hungary, which occurs within a lacustrine …

Abstract The last systematic research (1996–2000) of the Early Villányian Hajnáčka I site
(MN 16a) yielded many new fossils and geological data. Six stages could be identified in the …

Two Pliocene localities in Transdanubia (Hungary), Pula and Gérce, have been explored by
L. Hably since 1991. The plant fossils were reported by Fischer & Hably (1991), Kvaček et …

Life and depositional environments in the sublittoral zone of Lake Pannon, a large, brackish
Paratethyan lake from the Late Miocene, were reconstructed from fossils and facies of the …

The fossil-bearing deposits of Żabia Cave (Częstochowa Upland, Poland) yielded a diverse
vertebrate fauna (75 taxa in total) of middle Early Pleistocene age. The assemblage …

The Somssich Hill 2 site, situated near the municipality of Villány (South Hungary) was
originally excavated by Dénes Jánossy between 1975 and 1984. It is one of the richest …

This study from the Sremski Karlovci clay pit in northern Serbia sheds new light on the
physicochemical conditions, ecology and evolution of the Paludina Lake–the Pliocene …

The Danube Basin situated at the Alpine–Carpathian–Pannonian junction represents a
region of the Central Paratethys strongly influenced by orogen building processes and …

Two new palaeobotanical sites, Gérce and Pula from western Hungary, found in volcanic
craters are characterized in terms of floristic composition, vegetation, and palaeoclimate …

Pula maar is a partially eroded Pliocene maar-diatreme volcano, part of the Mio-Pliocene
Bakony-Balaton Highland Volcanic Field. The surficial remnant of the maar-diatreme …