Studia bot. hung. 42, pp. 153–183, 2011 PALAEOGENE AND NEOGENE LOCALITIES IN THE NORTH HUNGARIAN MOUNTAIN RANGE B. ERDEI1, L. HABLY1, I. SELMECZI2 and L. KORDOS2 1Department of Botany, Hungarian Natural History Museum, H–1476 Budapest, Pf. 222, Hungary;
[email protected] 2Geological Institute of Hungary, H–1143 Budapest, Stefánia út 14, Hungary Selected Palaeogene and Neogene fossil plant localities in the North Hungarian Mountain Range, introduced to participants of the 8th European Palaeobotany-Palynology Confe- rence in Budapest, 2010, are presented here with site descriptions and data on the fossil plant record. Key words: EPPC, fossil plant, Hungary, Neogene, Palaeogene, post-congress field trip guide INTRODUCTION A post-congress field trip of the 8th European Palaeobotany-Palynology Conference (EPPC 2010, 6–10 July, 2010, Budapest, Hungary) introduced several Palaeogene and Neogene fossil plant localities in the North Hunga- rian Mountain Range, i.e. the Visonta opencast lignite mine, and sites at Ipolytarnóc, the Eger-Kiseged roadcut, Rudabánya, and Erdõbénye. The field trip guide presented here intends to aggregate both published and un- published data on the fossil plant record at the localities. SITE DESCRIPTIONS Geology The Pannonian stage (standard chronostratigraphy: Tortonian/Messinian) compri- ses one of the thickest non-marine late Neogene sedimentary sequences in Europe (RASSER and HARZHAUSER 2008). This sequence was deposited in the Pannonian Basin during the Late Miocene and Pliocene, following the cessation of intermittent marine connections of Studia Botanica Hungarica, 42, 2011 Hungarian Natural History Museum, Budapest 154 ERDEI, B., HABLY, L., SELMECZI, I. and KORDOS, L. the basin towards the Mediterranean in the Middle Miocene (POPOV et al.