Balogh Zoltán (szerk.): Neograd 2017. Tanulmányok a 70 éves Praznovszky Mihály tiszteletére - A Dornyay Béla Múzeum Évkönyve 40. (Salgótarján, 2017)

Régészet - Tóth Balázs: Fémleletek a Kárpát-medence szarmata korú szárazföldi gerinces faunájának kutatásában

SZUROMI-KORECZ Andrea, SELMECZI Ildikó

2015 Middle Miocene evaporates from borehole successions in Hungary.

Neogene of the Paratethyan Region. 6th Workshop on the Neogene of Central and South-Eastern Europe, Orfű, Pécs. Hungary. 31 May -3 June. 91-92.

TÓTH Emőke, GÖRÖG Ágnes, LÉCUYER Christophe, MOISETTE Pierre,

BALTER Vincent, MONOSTORI Miklós

2010 palaeoenvironmental reconstruction of the Sarmatian (Middle Miocene)

Central Paratethys based on palaeontological and geochemical analyses of foraminifera, ostracods, gastropods and rodents. Geological Magazine. Cambridge. 147/2. 299-314.

VENCZEL Márton, HÍR János

2013 Amphibians and Squamates from the Miocene of Felsőtárkány Basin, NHungary. Palaeontographica, Abt A. Stuttgart. 300/1-6. 117-158. VENCZEL Márton, $TIUCÄ Emanoil

2008 Late middle Miocene amphibians and squamate reptiles from Taut,

Romania. Geodiversitas. Paris. 30/4. 731-763.

ZELENKA Tibor, PÓKA Teréz, MÁRTONNÉ SZALAY Emőke, PÉCSKAY Zoltán

2005 A Tari Dácittufa Formáció típusszelvényének felülvizsgálata [New data on

stratigraphic posiüon of the Tar Dacite Tuff Formation]. A Magyar állami Földtani Intézet Jelentése a 2004. Évről [Annual Report of the Hungarian Geological Institute on 2004]. Budapest. 73-84.

JÁNOS HÍR

NEW RESULTS IN THE STUDY OF THE SARMATIAN S.STR. VERTEBRATE FAUNAS OF THE CARPATHIAN BASIN

During the last two decades intensive field-work has been managed by the author in Northern Hungary and in Western Romania for collecting microveretebrate faunas from Sarmatian nonmarine and shallow marine sediments. Those are Tá?ad/Tasád, Värciorog/Vércsorog in Romania and Kozárd, Felsőtárkány-Felnémet 2/3, Felsőtárkány- Felnémet 2/7, Felsőtárkány 1, Felsőtárkány 2, Felsőtárkány 3/2, Felsőtárkány 3/8 and Felsőtárkány 3/10 in Northern Hungary.

In this publication we present the complete list of the elaborated fossils (Verterates and Invertebraes) from these localities.

The biochronological correlation of the faunas Tä?ad, Värciorog and Kozárd is possible after the rich invertebrate materials. These localities are possible to classify as Early Sarmatian. Värciorog and Kozárd are referable to the Elphidiwn reginam Zone.

The last crocodiles in the Carpathian Basin are found in Ta$ad, and Värciorog. Those are important markers of a warm subropic climate. In these faunas there are indications

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