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Urszula Myga-Piątek and Oimahmad Rahmonov

describe the evolution of winery landscapes in Europe, while taking into consideration the Mediterranean Basin, Asia Minor, Transcaucasia, and Central Asia. The article is an initial attempt to analyze the expansion of winery landscapes and to identify some of the regularities in their transformations on the basis of the remaining traces and signs that are present in the landscape as well as in the material and non-material culture of local societies in selected areas. Traces refer here to fragments, remnants, scraps of space, but also to the extent of winery

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Thomas Denk, Tuncay H. Güner, Zlatko Kvaček and Johannes M. Bouchal

Rinconada mine, eastern Spain) during the early Miocene. Bot. J. Linn. Soc., 172: 153–174. RÖGL F. 1998. Palaeogeographic considerations for Mediterranean and Paratethys seaways (Oligocene to Miocene). Ann. Naturhist. Mus. Wien, 99 A: 279–310. RÜCKERT-ÜLKÜMEN N. 2003. Fossil ranids from Miocene deposits of Central Anatolia. Istanbul Üniv. Müh. Fak. Yerbilimleri Dergisi, 16(2): 71–74. SACHSE M. 2001. Oleaceous laurophyllous leaf fossils and pollen from the European Tertiary. Rev. Palaeobot. Palynol., 115: 213–234. SAPORTA G. DE. 1865. Etudes sur la

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Kristina Ivančič, Mirka Trajanova, Stjepan Ćorić, Boštjan Rožič and Andrej Šmuc

Kostanjevica (SE Slovenia). Geologija 45, 2, 531–536, Rögl F. 1998: Palaeogeographic Considerations for Mediterranean and Paratethys Seaways (Oligocene to Miocene). Ann. des Naturhist. Mus. Wien. 99A, 279–310. Rögl F., Spezzaferri S. & Ćorić S. 2002: Micropaleontology and biostratigraphy of the Karpatian-Badenian transition (Early– Middle Miocene boundary) in Austria (Central Paratethys). Cour. Forsch.­Inst. Senckenb . 237, 47–67. Rögl F., Ćorić S., Hohenegger J., Pervesler P., Roetzel R., Scholger R., Spezzaferri S. & Stingl K. 2007: Cyclostratigraphy

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Jan Degirmendžić and Krzysztof Kożuchowski

References Bartoszek K., 2006. Niże śródziemnomorskie (Cyclones in the Mediterranean Region). Przegląd Geofizyczny 51(1): 35-43. Conrad V., Pollak L.W., 1950. Methods in climatology. Harvard University Press, Cambridge, Massachusetts. Degirmendžić J., Kożuchowski K., 2014. Sezonowe wahania liczby niżów śródziemnomorskich w Europie Środkowo- wschodniej (Seasonal variation in the number of Mediterranean cyclones in the Central and Eastern Europe). Przegląd Geofizyczny 59(1-2): 5-18. Degirmendžić J

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Salah Saleh, Oya Pamukçu and Ladislav Brimich

Geophys. Res., 3 , 317–354. Woodside J. M., 1976: Regional vertical tectonics in the Eastern Mediterranean Geophys. J. R. Astron. Soc., 47 , 493–514. Youssef M. I., 1968: Structure pattern of Egypt and its interpretation. AAPG Bulletin, 52 (4), 601–614. Zaghloul Z. M., Shaaban F. F., Yousef A. F., 1995: Subsurface Quaternary geothermal reservoir in the Nile Delta area. Journal of Environmental Sciences, 9 , 187–204. Ziegler P. A., 1990: Geological Atlas of Western and Central Europe, Shell International Petroleum Mij. B. V., distributed by

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Geologica Carpathica

The Journal of Geological Institute of Slovak Academy of Sciences

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Kamel Maalaoui and Fouad Zargouni

References Alleman, F., Catalano, R., Fares, F. and Remane, J. 1971. Standard Calpionellid zonation (Upper Tithonian- Valanginian) of the Western Mediterranean province. In: Farinacci, A. (Ed.), Proceedings of the II Planktonic Conference, Roma 1970, 1337-1340. Alleman, F., Grun, W. and Wiedmann, L. 1975. The Berriasian of Caravaca (Prov. of Murcia) in the Subbetic Zone of Spain and its importance for defining this stage and the Jurassic-Cretaceous boundary. Mémoires du Bureau de Recherches Géologiques et Minières, 86, 14

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Janina Bösken, Nicole Klasen, Christian Zeeden, Igor Obreht, Slobodan B Marković, Ulrich Hambach and Frank Lehmkuhl

contrast to extensively studied LPS along the Danube River, deposits further to the south in the Central Balkan region have been poorly investigated so far ( Kostić and Protić, 2000 ; Basarin et al ., 2011 and Obreht et al ., 2014 ). The studied section Stalać is located in this region south of the typical loess distribution area of the Carpathian Basin (Middle Danube Basin) and the Lower Danube Basin, and it is especially important for an integral view on paleoenvironments in the yet poorly investigated interior of the Balkans. This region was under much stronger

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Márton Szabó and László Kocsis

: Palaeogeographic considerations for the Mediterranean and Paratethys seaways (Oligocene to Miocene). Annalen des Naturhistorischen Museums in Wien 99 (A), 279-310. Rögl F. & Steininger F.F. 1983: Vom Zerfall der Tethys zu Mediterran und Paratethys. Die neogene Paläogeographie und Palinspastik des zirkum-mediterranen Raumes. Annalen des Naturhistorischen Museums in Wien 84 (A), 135-163. Rögl F. & Brandstätter F. 1993: The foraminifera genus Amphistegina in the Korytnica Clays (Holy Cross Mts, Central Poland) and its significance in the Miocene of

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Matúš Hyžný, Mathias Harzhauser and Wolfgang Danninger

Crustacés Décapodes Brachyoures. Hebd. Acad. Sci., Sér. D 285, 1049–1052. Harzhauser M. & Piller W.E. 2007: Benchmark data of a changing sea — palaeogeography, palaeobiogeography and events in the Central Paratethys during the Miocene. Palaeogeogr. Palaeoclimatol. Palaeoecol. 253, 8–31. Harzhauser M., Piller W.E. & Steininger F.F. 2002: Circum-Mediterranean Oligo–Miocene biogeographic evolution — the gastropods’ point of view. Palaeogeogr. Palaeoclimatol. Palaeoecol. 183, 103–133. Harzhauser M., Mandic O. & Zuschin M. 2003: Changes in Paratethyan