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Journal articles on the topic 'Pannonian'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Lepirica, Alen, Željka Stjepić-Srkalović, and Dado Srkalović. "GEOMORPHICAL MESO-ENTITY SEMBERIJA LOWLAND PLAIN." Glasnik Rudarsko-geološko-građevinskog fakulteta 10, no. 10 (2022): 9–18. http://dx.doi.org/10.51558/2303-5161.2022.10.10.9.

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In this paper, it was necessary to prove that Semberija is in the geomorphological sense, the southern part of the Pannonian Basin, which is in contact with the Dinaric mountain system. Its done on the basis of the geo- morphological analysis of the terrain, primarily morphotectonic, morphological and morphogenetic similarities with the plain terrain of Pannonia. This was the basis for a complex geomorphological regionalization which included added similarities and connections with the Pannonian Basin in climate, pedogeography and biogeog- raphy sense. Thus, after the complex geomorphological

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2

FERJANČIĆ, SNEŽANA. "THE ALA PANNONIORUM IN THE ARMY OF ILLYRICUM." ИСТРАЖИВАЊА, no. 26 (January 6, 2016): 37–45. http://dx.doi.org/10.19090/i.2015.26.37-45.

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The province of Illyricum, established shortly after Octavian’s Illyrian war and divided into Illyricum Superius (Dalmatia) and Illyricum Inferius (Pannonia) during or after the Pannonian-Dalmatian Rebellion, was garrisoned by several legions and various auxiliary regiments. The list of auxilia includes an ala Pannoniorum. Epigraphic evidence from Dalmatia and Pannonia provides some information on its relocation, as well as on its recruitment. Under Augustus, the regiment was in Dalmatia. It was relocated to Pannonia ca. 15 AD. At the beginning of Vespasian’s reign, the ala Pannoniorum was tra

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3

Kovács, Péter. "Sjeverna granica Panonaca i rijeka Drava / The northern border of the Pannonians and the river Drava." Journal of BATHINVS Association ACTA ILLYRICA / Godišnjak Udruženja BATHINVS ACTA ILLYRICA Online ISSN 2744-1318, no. 2 (December 1, 2018): 217–29. http://dx.doi.org/10.54524/2490-3930.2018.217.

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In his paper the author analyses the change of the Pannon and Pannonian tribes in the province of Pannonia during the early Principate and the northern border of the Pannonian tribes that was, according to the generally accepted view, the Drava river. Based on the written and epigraphic sources (including the new Roman finds from county of Somogy) and the LTD finds, the author concludes that the ethnic border was north of the river in county Somogy as no late Celtic settlements and cemeteries can be pointed out south of Kaposvár.

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4

Domić Kunić, Alka. "Kolapijani / Colapiani." Journal of BATHINVS Association ACTA ILLYRICA / Godišnjak Udruženja BATHINVS ACTA ILLYRICA Online ISSN 2744-1318, no. 4 (December 23, 2020): 107–61. http://dx.doi.org/10.54524/2490-3930.2020.107.

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After conquering the Iapodean center Metulum in 35 BC, Octavian (soon to be Emperor Augustus) set forth towards Segesta with his legions “through the land of the Paeonians not yet conquered by the Romans” (App. Illyr. IV, 22). Appian’s Paeonians were actually the Pannonians, and this paper aims to show that this community was also known as the Colapiani. The land of the Pannonians was located between Octavian’s two main strategic goals (Metulum and Segesta) and it’s reasonable to assume that Octavian wanted to put this land under Roman control as well. According to Appian, Octavian first hoped

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5

Németh, György. "Jewish Elements in the Greek Magic of Pannonia." Journal of Ancient Judaism 1, no. 2 (2010): 181–88. http://dx.doi.org/10.30965/21967954-00102006.

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Numerous names and terms related to Jewish tradition are known from the territory of Roman Pannonia. Pannonian magical inscriptions raise the question, to what extent do names and terms of Hebrew origin bear witness to the presence of Jews in Pannonia in the first three centuries of the imperial age? An almost simultaneous appearance of the silver lamella from Aquincum and the golden lamella from Halbturn proves that the Jewish population of Pannonia not only commemorated itself in official inscriptions but also preserved its identity through amulets.

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6

Vágási, Tünde. "Epigraphic Records of the Friendship of Mithras and Sol in Pannonia." Acta Antiqua Academiae Scientiarum Hungaricae 58, no. 1-4 (2018): 357–76. http://dx.doi.org/10.1556/068.2018.58.1-4.21.

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Summary Regarding the Mithras cult, Pannonia had an exceptional status in the Roman Empire. This unique status was connected with the huge numbers of military forces stationed there. Numerous inscriptions and altars give evidence that Pannonia had an uncommon sensitivity for religions; this is why some local characteristics and relief-versions could be made, for example: dadophores with pelta shields, and unique dedicational forms which are mostly known in Pannonia, and perhaps spread from there to other parts of the Empire. In my paper, I want to show the connections between Mithras and Sol o

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Dobosi, Linda. "Brick and tile kilns in Roman Pannonia – A state of research." Acta Archaeologica Academiae Scientiarum Hungaricae 72, no. 1 (2021): 27–53. http://dx.doi.org/10.1556/072.2021.00003.

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AbstractDozens of Roman tile kilns have come to light in Pannonia during the last one hundred years. This paper summarizes the published tile manufacturing workshops of Pannonia in present-day Hungary, Austria, Slovenia, Croatia, and Serbia. In the first part it gives a short general overview of the structure of a workshop, discusses the problems of defining tile kilns, describes the parts of the kilns themselves and outlines the systems of classifications. The second part gives a description and catalogue of the Pannonian tile kilns.

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8

Milin, Milena. "Pitanje ilirske komponente stanovnistva jugoistocnog dela Donje Panonije u savremenim istrazivanjima." Balcanica, no. 32-33 (2002): 49–60. http://dx.doi.org/10.2298/balc0233049m.

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Following the Symposium on distribution of the Illyrians (4th to 2nd centuries B.C., Sarajevo, 1964), the view that the northern border of the Illyrians ran along the line even much southerner than the Sava (nn.2-8) has been firmly established in our archeology; this attitude has been extended to the Illyrian tribes in Roman times (n.7). At the same time, historians of the pre-Roman and Roman periods in the Balkans still hold the view of predominantly Illyrian origins of the tribes from Lower Pannonia, between the Danube and the lower course of the Sava river (n.9), based on contemporary histo

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Boișteanu, Florian. "FUNERARY REPRESENTATIONS OF THE NORICO-PANNONIAN FEMININE CLOTHING IN ROMAN DACIA." Acta Musei Napocensis 61 (December 10, 2024): 41–68. https://doi.org/10.54145/actamn.i.61.02.

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The present research aims to bring together and to analyse the representations of the Norico-Pannonian clothing from Roman Dacia. They appeared as a way of expressing identity in Noricum and Pannonia and also in regions where former settlers of these two provinces had been colonized. I have identified twenty-seven cases, most of them coming from Dacia Superior. The typological analysis is realized on the representations of peplos-like tunics, bonnets, brooches and torques. In case of the peplos-like tunics, I have only identified five cases, at Apulum, Cristești and Șeica Mică. The bonnet is t

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10

Gaudenyi, Tivadar, and Milan Mihajlović. "The Pannonian Plain: Denomination, Definition and Subdivision." European Journal of Environment and Earth Sciences 3, no. 2 (2022): 13–18. http://dx.doi.org/10.24018/ejgeo.2022.3.2.240.

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The Pannonian Plain is a landscape- and a physico-geographic unit. It encompasses the plain, lowland landscapes of the Pannonian realm. If we follow the Pannonian Plain along the Danube valley, it starts from with Vienna Basin continues downstream till the Iron Gate. The Pannonian Plain (Pannon-alföld / Panonska nizija) can be subdivided in six landscape units. The three main units are: the Vienna Basin (Wiener Becken), the Little Alföld (Kisalföld) and the Alföld. The three smaller units have some kind of connections with the Alföld they are the Inner Somogy (Belső Somogy), the western

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Rundić, Ljupko, Meri Ganić, Slobodan Knežević, and Ali Soliman. "Upper Miocene Pannonian sediments from Belgrade (Serbia): new evidence and paleoenvironmental considerations." Geologica Carpathica 62, no. 3 (2011): 267–78. http://dx.doi.org/10.2478/v10096-011-0021-z.

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Upper Miocene Pannonian sediments from Belgrade (Serbia): new evidence and paleoenvironmental considerationsThe Late Miocene sublittoral marls of the Pannonian Stage (the long-lived Lake Pannon) were studied. From neotectonic point of view, the investigated area represents a natural border between two different morphostructural domains: the Pannonian Basin to the north and the Peri-Pannonian Realm to the south. More than 20 mollusc and 34 ostracod species were identified which indicate the upper part of the Lower Pannonian and the lower part of the Middle Pannonian ("Serbian") predominantly. T

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Olteanu, Radu. "The “Cimpia Moment” (late Miocene, Romania) and the Pannonian-Pontian boundary, defined by ostracods." Journal of Micropalaeontology 8, no. 2 (1989): 239–47. http://dx.doi.org/10.1144/jm.8.2.239.

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Abstract. The boundary between the Pannonian and Pontian (late Miocene) of the Pannonian area is recognised on the basis of ostracod faunas. A comparison is made between the faunas of the Pannonian Basin and the Dacic-Euxine Basin. A transitional fauna with Pannonian elements, but a stronger Pontian component, is described from Cimpia (Romania). This indicates a more gradual transition between the two stages in the Pannonian Basin than in the Dacic-Euxine Basin, where there is a sharp faunal break indicating a period of non-deposition or erosion.

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Lazić, Sara. "The Pannonians in ancient historiography from 1st to 4th century." Vojno-istorijski glasnik, no. 2 (2022): 9–21. http://dx.doi.org/10.5937/vig2202009l.

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The Pannonians (as well as other ethnic groups from Illyricum) were depicted as primitive barbarians in ancient historiography. Ancient writers emphasize their bodily strength and military prowess, but also attribute boorishness and cruelty to them. A particularly unfavorable image of Pannonians can be found in testimonies from the 4th century. According to Ammianus Marcellinus, the Pannonian dignitaries in imperial service under Valentinian I were people of "the most despicable kind". They are bloodthirsty and often compared to wild beasts in Ammianus' work. In this paper we will show the gen

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Dévai, Kata. "Juglet Pendants from Pannonia." Acta Archaeologica Academiae Scientiarum Hungaricae 71, no. 2 (2020): 651–60. http://dx.doi.org/10.1556/072.2020.00018.

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Most juglet pendants are of 4th century from Pannonia, the glass is frequently dark, appearing black. Although juglet pendants have a greater concentration in the eastern Mediterranean, they are also widely attested in the empire’s western half. The following paper1 presents nine specimens from Hungary, eight from Pannonia Province. Three exemplars were parts of grave inventories, whose other items are also known (Bogád, Csongrád and Ságvár). All three burials can be securely dated to the fourth century. Despite the attractiveness of M. Stern’s suggestion, there is no good reason to associate

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15

Šačić Beća, Amra. "Reflections and consequences of Tiberius’s Pannonian war on Bosnian Posavina." Godišnjak Centra za balkanološka ispitivanja, no. 48 (January 6, 2022): 237–48. http://dx.doi.org/10.5644/godisnjak.cbi.anubih-48.129.

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In contemporary historiography, the term Bellum Pannonicum implies Tiberius’s conquest of southeastern Pannonia, that is the area between the rivers Drava and Sava, the basin of the rivers Sana, Vrbas and Bosna to the south of the Sava River. This paper accepts the opinion of the contemporary historiography that Tiberius’s war (Bellum Pannonicum) was waged for only 2 years – 12 and 11 BC. It accordingly takes into account the ethno-geographical understanding of Pannonia in the context of the territory of Bosnia and Herzegovina. The paper particularly focuses on the Breuci and Osseriates as two

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Kovács, Péter. "Emperor Avitus in Pannonia?" Acta Archaeologica Academiae Scientiarum Hungaricae 71, no. 2 (2020): 661–68. http://dx.doi.org/10.1556/072.2020.00019.

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In his paper the author examines the sources of the supposed Western Roman military expedition of Emperor Avitus in Pannonia in 455 that was thought to be the last Roman military action in the territory of the former Roman province. Analizing the sources, he comes to the conclusion that during his short reign, Avitus had no time to visit the province and his route (iter) mentioned by Sidonius Apollinaris must be identified with his journey from Arelate to Rome. The Roman military action in Pannonia can probably be identified with a short demonstrative campaign in the SW region of the dioecesis

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Reich, Dieter, Thomas Barta, Karl-Georg Bernhardt, Werner Lazowski, Uwe Raabe, and Luise Schratt-Ehrendorfer. "Cyperus michelianus (Cyperaceae) in the Pannonian region, new for Burgenland." Neilreichia 10 (April 30, 2019): 155–69. https://doi.org/10.5281/zenodo.2630537.

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Distribution, ecology, habitats, phytosociology and threats of Cyperus michelianus are discussed with emphasis on the Pannonian region in Austria. New findings including the first record from Burgenland and known records from literature, herbaria and own observations from the Pannonian region are presented. A map illustrates the distribution of C. michelianus in the Austrian part of the Pannonian region.

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Calic, Jelena, Marko Milosevic, Tivadar Gaudenji, Dragoljub Strbac, and Milovan Milivojevic. "Pannonian plain as a morphostructural unit of Serbia." Glasnik Srpskog geografskog drustva 92, no. 1 (2012): 47–70. http://dx.doi.org/10.2298/gsgd1201047c.

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Differentiation between the terms ?Pannonian Basin? and ?Pannonian Plain? is not clear enough in geographical literature. The paper discusses the usage of the term ?plain? in geomorphology, as well as the usage of a quantitative method for plain delineation, through calculation of relief roughness coefficient (using a digital elevation model). Qualitative analysis, which includes the definition of dominant geomorphological processes and the distribution of Quaternary sediments, is an addition to the quantitative analysis. In the Republic of Serbia, the area of the Pannonian plain defined in th

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Pryhara, O. V. "ГЕОГРАФІЧНА СТРУКТУРА ФЛОРИ ЗАКАРПАТСЬКОЇ РІВНИНИ". Scientific Issue Ternopil Volodymyr Hnatiuk National Pedagogical University. Series: Biology 81, № 3 (2021): 13–17. http://dx.doi.org/10.25128/2078-2357.21.3.2.

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The geographical analysis of flora vascular plants of the Transcarpathian plain has been carried out. It has been found that in the geographical distribution the species of flora belong to 16 types of areas. In the geographical range of flora the leading position is occupied by Golarctic (131), Eurasian (426), Eurasian-Mediterranean (138), and European (144) types of habitats. The presence of the autochthonous Transcarpathian and Pannonian flora core, including endemic and sub-endemic species was idfentified, its wide geographical connection with the flora of the Pannonia, the Mediterranean ha

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Katona, Gergely, Balázs Tóth, and Zsolt Bálint. "Notes on the nomenclature of Eublemma pannonica (Freyer, 1840): a rectification and a new subspecies name (Lepidoptera: Erebidae, Eublemminae)." Annales Musei historico-naturalis hungarici 112 (2020): 125–37. http://dx.doi.org/10.53019/annlsmushistnathung.2020.112.125.

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The erebid moth Eublemma pannonica (Freyer, 1840) is a distinctive species of the Pannonian region. The species-group name panonica Freyer, 1840 is an incorrect original spelling what needs a rectification. This spelling has been forgotten until its appearance in the catalogue compiled by Robert W. Poole in 1989 for noctuid names and it is again in use. The other original spelling pannonica Freyer, 1840 is the correct one, what was in general usage until 1989. On the basis of voluminous literature references these spellings are discussed. The name Eublemma panonica ronkayorum Fibiger, Zilli &a

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Katona, Gergely, Tóth Balázs, and Zsolt Bálint. "Notes on the nomenclature of Eublemma pannonica (Freyer, 1840): a rectification and a new subspecies name (Lepidoptera: Erebidae, Eublemminae)." Annales Musei historico-naturalis hungarici 112 (July 22, 2021): 125–37. https://doi.org/10.53019/AnnlsMusHistNatHung.2020.112.125.

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Abstract – The erebid moth Eublemma pannonica (Freyer, 1840) is a distinctive species of the Pannonian region. The species-group name panonica Freyer, 1840 is an incorrect original spelling what needs a rectification. This spelling has been forgotten until its appearance in the catalogue compiled by Robert W. Poole in 1989 for noctuid names and it is again in use. The other original spelling pannonica Freyer, 1840 is the correct one, what was in general usage until 1989. On the basis of voluminous literature references these spellings are discussed. The name Eublemma&

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Ganic, Meri, Ljupko Rundic, Slobodan Knezevic, and Vesna Cvetkov. "The Upper Miocene Lake Pannon marl from the Filijala Open Pit (Beocin, northern Serbia): New geological and paleomagnetic data." Annales g?ologiques de la Peninsule balkanique, no. 71 (2010): 95–108. http://dx.doi.org/10.2298/gabp1071095g.

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This work presents major lithological, structural, paleontological and paleomagnetic characteristics of the Upper Miocene Pannonian marl in the Filijala Open Pit of the La Farge Cement Plant near Beocin, northern Serbia. Pannonian marl lies between the underlying heterogeneous Sarmatian deposits and the overlying set of Pontian sand beds and Quaternary sediments. The open pit is located on the NE range of Fruska Gora, a horst structure with a core of Paleozoic, Mesozoic and Paleogene rocks in a complex structural pattern. Pannonian sediments, which are part of a younger structural stage, depos

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Guskov, E. A. "DISBANDMENT OF THE PRAETORIAN GUARD IN 193 A.D." Izvestiya of Samara Scientific Center of the Russian Academy of Sciences. History Sciences 6, no. 1 (2024): 120–29. http://dx.doi.org/10.37313/2658-4816-2024-6-1-120-129.

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In 193, the governor of Upper Pannonia, Septimius Severus, who had been proclaimed emperor by the Pannonian legions, captured Rome, overthrowing and killing Didius Julianus, who had been proclaimed emperor in the capital. Before the next act of war for the throne with the Syrian and British governors, who also had been proclaimed emperors, Severus reformed the Praetorian Guard which supported Julianus. Ancient authors report that the Praetorians were disbanded, and in their place Severus recruited soldiers from his legions. The author analyzes the reasons for the disbandment of the Praetorian

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LUBENESCU, Victoria. "Biostratigraphic correlations between the Dacian and Pannonian Basins from Romania." Geo-Eco-Marina No 22/2016, no. 10 (2016): 161–79. https://doi.org/10.5281/zenodo.889931.

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The author presents the Sarmatian to Dacian (Paludina beds), evolution of the mollusc faunas (markers), shared alike by the Dacian and Pannonian (eastern part) basins. The mollusc associations from the Congeria beds (Pannonian s. str.) correlate with the Maeotian mollusc assemblages from the Dacian Basin. The Upper Congeria beds, probably starting from the ‘E Zone’ (Papp, 1951), correlate with the Pontian associations in the Dacian Basin. The author suggests that the Pannonian s.str./Pontian boundary should be set out in a lower position compared to the similar Dacian Basin boundary; consideri

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Gúthy, Tibor, Ernő Takács, Attila Csaba Kovács, et al. "Recent developments in imaging the earth’s crust by deep seismic data beneath the eastern parts of the Pannonian Basin." Interpretation 6, no. 1 (2018): SB23—SB35. http://dx.doi.org/10.1190/int-2016-0206.1.

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The first multicoverage, low-frequency deep reflection surveys in the Pannonian Basin were initiated in the late 1980s and were focused to southeast Hungary, where hydrocarbon and geothermal reserves were known. Deep seismic profiles (Pannonian Geotraverse transects) were shot according to the standards of hydrocarbon exploration data acquisition parameters to get information from the deep crust and the upper mantle. At the turn of the millennium, the international CELEBRATION 2000 deep seismic survey provided a large-scale velocity model of the Pannonian Basin and its surroundings. The substa

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Rundic, Ljupko. "Late miocene ostracodes of Serbia: Morphologic and palaeoenvironmental considerations." Annales g?ologiques de la Peninsule balkanique, no. 67 (2006): 89–100. http://dx.doi.org/10.2298/gabp0667089r.

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About 11.5 million years ago, a tectonic uplift of the Eastern and Western Carpathians separated the Pannonian Basin from the rest of the Paratethys. This orogenesis event caused an unconformity between the Sarmatian brackish sediments and the Pannonian lake-sea deposits. More than 6 Ma later, in these parts of the Paratethys, changes in the geographic framework, hydrological conditions and brackish - caspibrackish water chemistry led to the disappearance of restricted marine forms of life. A few euryhaline and marginal marine species survived this environmental change. Among the ostracodes, s

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Thomson, Ian. "The Scholar as Hero in Ianus Pannonius' Panegyric on Guarinus Veronensis." Renaissance Quarterly 44, no. 2 (1991): 197–212. http://dx.doi.org/10.2307/2862708.

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Specialists in the Italian Renaissance know the importance of the great humanist Guarinus Veronensis (1374-1460) and are familiar with the salient points of his life. Still lacking is a series of up-to-date monographs on his more important students and the part they played in the spread of humanism in Europe. Recently, however, there have appeared in English several studies of Ianus Pannonius (1434-72), once described by Guarinus as "a studentboarder of mine, Pannonian by race but Italian in manners, an admirable, indeed a stupendous scholar.

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Ga´ti, Guyla. "Pannonian international catalysis symposium." Applied Catalysis 65, no. 2 (1990): N23. http://dx.doi.org/10.1016/s0166-9834(00)83163-2.

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Migotti, Branka. ""Pannonian altars" - a reinterpretation." Hortus Artium Medievalium 12 (January 2006): 239–42. http://dx.doi.org/10.1484/j.ham.2.305380.

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ALEKSA, KNEŽEVIĆ, DŽIGURSKI DEJANA, LJEVNAIĆ MAŠIĆ BRANKA, ĆUPINA BRANKO, and MILOŠEV DRAGIŠA. "PLANT COVER OF NATURAL PASTURES LOCATED IN THE VICINITY OF THE TOWN OF NOVI KNEŽEVAC." Contemporary Agriculture (2011) 60, no. 1-2 (2011): 22–30. https://doi.org/10.5281/zenodo.7275996.

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Specific features of the plant cover of the natural pastures located in the vicinity of the town of Novi Kneževac (the Vojvodina Province, Serbia) result from their floristic, ecological, plant geographic, florogenetic and phytocoenological characteristics. Floristic characteristics result from 205 taxa. Of the 205 taxa, 191 taxa (177 species, six subspecies, three varieties and five forms) were listed on account of their distinctive floristic characteristics. Ecological characteristics result from 55 halophyte taxa with the ecological index S<sub>+</sub>. Plant geographic characteristics resu

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Ćorić, Stjepan. "Calcareous nannofossils from the middle/upper Miocene succession of Pécs-Danitzpuszta, southern Hungary: cosmopolitan Paratethys and endemic Lake Pannon assemblages." Földtani Közlöny 151, no. 3 (2021): 253–65. http://dx.doi.org/10.23928/foldt.kozl.2021.151.3.253.

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Quantitative analyses on calcareous nannofossils were carried out on 109 middle/late Miocene (Sarmatian/ Pannonian) samples from the section at Pécs-Danitzpuszta sand pit (Hungary). The lower part of the section, which can be assigned to the Sarmatian, contains normal marine low-diversity assemblages dominated by Calcidiscus leptoporus, Reticulofenestra pseudoumbilicus, Sphenolithus moriformis and Syracosphaera spp. accompanied by didemnid ascidian spicules (Perforocalcinela fusiformis). The middle/late Miocene (Sarmatian/Pannonian) boundary is characterized by the last occurrences of normal m

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Codrea, Vlad. "THE PANNONIAN FLORA OF THE CHIUZBAIA FOSSILIFEROUS SITE / FLORA PANNONIANĂ A SITULUI FOSILIFER CHIUZBAIA." Acta Palaeontologica Romaniae, no. 21 (1) (December 7, 2024): 3–4. https://doi.org/10.35463/j.apr.2025.01.01.

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Klimo, Atila. "Mineral waters of the Pannonian basin spas in the Republic of Serbia." Srpski arhiv za celokupno lekarstvo 139, no. 3-4 (2011): 203–8. http://dx.doi.org/10.2298/sarh1104203k.

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Introduction. The fact itself that thermo-mineral waters and mud have healing effects has always attracted attention throughout the history to exploit, explore and study their benefit on the human body. Modern lifestyle and the speed of life endanger man?s psycho-physical health. This is why people more often return to old time proven values, the nature and natural health resorts. Objective. To establish hydro-geological conditions for the formation of mineral water and to summarize their balneological characteristics in spas, i.e., in rehabilitation centres of the Pannonian basin of the Repub

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Zakar, Erika, Edit Zajácz, Tímea Rácz, János Oláh, András Jávor, and Szilvia Kusza. "Morpometric study of Hungarian honey bee (Apis mellifera L.) colonies." Acta Agraria Debreceniensis, no. 51 (February 10, 2013): 59–63. http://dx.doi.org/10.34101/actaagrar/51/2063.

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The honey bees are essential for the pollination of agricultural plants. The Pannonian honey bee, Apis mellifera pannonica, is native to Hungary, only these subspecies are being bread in our country. The parameters have been separated the pannon and italian honey bee subspecies, the colour of tergit, the cubital index and proboscis length. The morphometric analisys is of special importance because this, on the one hand, shows correlation with honey bee production and on the other hand, the pure morphometric charactersitics is the basis of any potential honey bee export. Mitochondrial DNA and m

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Slezák, Michal, Štefánia Farkašovská, and Richard Hrivnák. "Non-native plant species in alder-dominated forests in Slovakia: what does the regional- and the local-scale approach bring?" Folia Oecologica 47, no. 2 (2020): 100–108. http://dx.doi.org/10.2478/foecol-2020-0012.

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AbstractEuropean riparian forests are in general susceptible to plant invasions compared to other natural forest habitats. Their descriptive vegetation overviews with phytosociological affiliation contain detail insight into species composition patterns at various geographical scales, but quantitative assessment of the relationship between non-native plant richness and measured environmental variables is still scarce. We used two vegetation datasets of alder-dominated forests to analyse plant invasion patterns in the Pannonian and the Carpathian region of Slovakia. A large dataset of 918 veget

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Sáró, Csilla. "Pannonian women's headwear-related accessories." Acta Archaeologica Academiae Scientiarum Hungaricae 75, no. 1 (2024): 19–41. http://dx.doi.org/10.1556/072.2024.00008.

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AbstractThe main goal of this paper is to study a specific element of women's depicted costumes. Pictures on stone monuments present local, so-called native women wearing complex attire of cloth, headwear, brooches, jewels, and other dress accessories. Thirteen stone monuments from Hungary depict local women with headwear-related accessories. The main questions are: what kind of accessories are they, and how can we evaluate their presence on depicted attires? I collected analogous depictions from other Provinces and studied archaeological material. Finally, I concluded that these headwear-rela

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Ceglar, Andrej, Adina-Eliza Croitoru, Joan Cuxart, et al. "PannEx: The Pannonian Basin Experiment." Climate Services 11 (August 2018): 78–85. http://dx.doi.org/10.1016/j.cliser.2018.05.002.

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Ryczkowski, J. "Third Pannonian Symposium on Catalysis." Applied Catalysis A: General 129, no. 2 (1995): N17—N18. http://dx.doi.org/10.1016/0926-860x(95)80225-8.

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Harzhauser, Mathias, Oleg Mandic, Matthias Kranner, et al. "The Sarmatian/Pannonian boundary at the western margin of the Vienna Basin (City of Vienna, Austria)." Austrian Journal of Earth Sciences 111, no. 1 (2018): 26—A4. http://dx.doi.org/10.17738/ajes.2018.0003.

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Abstract Sarmatian and Pannonian cores, drilled at the western margin of the Vienna Basin in the City of Vienna, reveal a complex succession of marine and lacustrine depositional environments during the middle to late Miocene transition. Two Sarmatian and two Pannonian transgressive-regressive sequences were studied in detail. Identical successions of benthic faunal assemblages and similar patterns in magnetic susceptibility logs characterise these sequences. This allows a correlation of the boreholes over a distance of ~3.5 km across one of the major marginal faults of the Vienna Basin. Biost

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Jaksic, Predrag. "Aspects of butterfly zoogeography of some Pannonian island mountains." Zbornik Matice srpske za prirodne nauke, no. 128 (2015): 7–19. http://dx.doi.org/10.2298/zmspn1528007j.

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Specific geology and tectonic history of the Pannonian plain is pointed out. Lower mountains and hills, specific to the area, are highlighted. They most likely were islands in the period of Paratethys and Pannonian Sea: Mal? Karpaty, Vertes, Bakony, Mec?sek, Medvednica, Papuk, Fruska Gora and Avala. A head-to-head comparison has been done as well as a comparison with the site Moh?cs, a typical plain habitat in the Pannonian plain. The existence of specific elements of butterfly fauna of island mountains is dis?cussed. According to the existing data from literature, the list of 163 butterfly sp

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Radivojevic, Dejan. "Evolution of the southeastern part of the Pannonian Basin and its implications." Annales g?ologiques de la Peninsule balkanique, no. 00 (2023): 8. http://dx.doi.org/10.2298/gabp230624008r.

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The southeastern part of the Pannonian Basin System probably represents the most important area for determining its origin and evolution. The geodynamics also influenced the way that sediments fill the basin and therefore the economic resources that can be found in these sediments. All this led to the fact that the Pannonian Basin is the most developed part of our country. The great scientific value of this area is found in the fact that it represents an excellent training ground for the demonstration of the opening of the Pannonian basin system as well as the progradation of sediments from th

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Kovács, Zoltán. "Scleractinia fauna from the Middle Miocene deposits of Letkés (Börzsöny Mts, Hungary)." Földtani Közlöny 154, no. 4 (2024): 423–48. https://doi.org/10.23928/foldt.kozl.2024.154.4.423.

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A rich Middle Miocene Scleractinia fauna is described and illustrated from the Badenian (Middle Miocene) deposits of Letkés (Bagoly Hill, Börzsöny Mts, N Pannonian Basin, Hungary). The material consists of both zooxanthellate (e.g., Echinopora, Porites, Solenastrea, Tarbellastraea, Turbinaria), and azooxanthellate (e.g., Balanophyllia, Caryophyllia, Flabellum, Stephanophyllia) taxa. The 25 species represent the most highly diverse coral assemblage of the Pannonian Basin. Eleven species are recorded for the first time in Hungary.

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Rundic, Ljupko. "Some species of the Genus Hemicytheria Pokorny (Ostracoda, Crustacea) from the Upper Miocene of Serbia." Annales g?ologiques de la Peninsule balkanique, no. 64 (2002): 137–51. http://dx.doi.org/10.2298/gabp0264137r.

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The ostracod genus Hemicytheria is very important for biostratigraphy of the caspibrackish deposits of the Pannonian basin. More than twenty species are known from regions of central Serbia and adjacent provinces. Most of them being found in the Pannonian and Pontian sediments (Sokac, 1972; Krstic, 1985; Rundic, 1992, 1993, 1997). Herein, three new species are reported for the first time: Hemicytheria setosa n. sp., Hemicytheria carinata n. sp., Hemicytheria portaferrica n. sp.

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Sebe, Krisztina, Gyula Konrád, and Orsolya Sztanó. "An exceptional surface occurrence: the middle to upper Miocene succession of Pécs-Danitzpuszta (SW Hungary)." Földtani Közlöny 151, no. 3 (2021): 235–52. http://dx.doi.org/10.23928/foldt.kozl.2021.151.3.235.

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The Pécs-Danitzpuszta sand pit is the most important outcrop of the oldest Pannonian (upper Miocene, Tortonian) deposits in southern Hungary. A trench excavated in 2018 exposed Lake Pannon deposits and underlying Paratethys strata down to the upper Badenian (Serravallian), and together with the sand pit they make up a continuous sedimentary succession with a true thickness of ~220 metres. Due to tectonic deformation, middle Miocene deposits and carbonates in the lowermost Pannonian are overturned. Layers become vertical close to the marl-sand boundary, then the dip changes to normal, with cont

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Filipescu, Sorin, Franz Wanek, Angela Miclea, Arjan De Leeuw, and Iuliana Vasiliev. "Micropaleontological response to the changing paleoenvironment across the Sarmatian-Pannonian boundary in the Transylvanian Basin (Miocene, Oarba de Mureş section, Romania)." Geologica Carpathica 62, no. 1 (2011): 91–102. http://dx.doi.org/10.2478/v10096-011-0008-9.

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Micropaleontological response to the changing paleoenvironment across the Sarmatian-Pannonian boundary in the Transylvanian Basin (Miocene, Oarba de Mureş section, Romania) The Sarmatian-Pannonian transition has been investigated in Section A of Oarba de Mureş in the central Transylvanian Basin. Micropaleontological assemblages are diagnostic for different environmental settings and demonstrate a clear zonation, which was used to reconstruct the genetic units. Five stratigraphic sequences were described and subdivided based on the microfossil assemblages. Transgressive intervals were documente

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Pandolfi, Luca, Mihály Gasparik, and Imre Magyar. "Rhinocerotidae from the Upper Miocene deposits of the Western Pannonian Basin (Hungary): implications for migration routes and biogeography." Geologica Carpathica 67, no. 1 (2016): 69–82. http://dx.doi.org/10.1515/geoca-2016-0004.

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Abstract Although the rhinoceros remains have high biochronological significance, they are poorly known or scarcely documented in the uppermost Miocene deposits of Europe. Several specimens collected from the Upper Miocene (around 7.0 Ma, Turolian) deposits of Kávás (Pannonian Basin, Western Hungary), previously determined as Rhinoceros sp., are revised and described in this paper. The postcranial remains of these specimens belong to “Dihoplus” megarhinus (de Christol) on the basis of the morphological and morphometric characters of humerus, radii, metacarpal and metatarsal elements. An overvi

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OLTEANU, Radu. "Atlas of the Pannonian and Pontian ostracods from the eastern area of the Pannonian Basin." Geo-Eco-Marina No 17/2011 (December 31, 2011): 135–79. https://doi.org/10.5281/zenodo.56927.

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Abstract. The present paper is neither dogmatic, nor authoritative. In my view, palaeontology is a humanistic discipline which – apart from describing the hard skeleton (the palaeontologic species) and beyond it – attempts to suggest the time when the fossil species existed, their way of life, the morphologic change (called adaptation) they went through and, sometimes, show the evolution of life. Show how life grows. This work seeks to inquire, question,generate as many questions as possible, targeting new research. It is an Atlas and not a Monography, a monographic work. Hence, th

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Saftić, Bruno, Josipa Velić, Orsolya Sztano, Györgyi Juhasz, and Željko Ivković. "Tertiary Subsurface Facies, Source Rocks and Hydrocarbon Reservoirs in the SW Part of the Pannonian Basin (Northern Croatia and South-Western Hungary)." Geologia Croatica 56, no. 1 (2003): 101–22. http://dx.doi.org/10.4154/232.

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The Neogene sedimentary successions of the Drava, Sava and Slavonija–Srijem depressions in the SW part of the Pannonian Basin Systemare built up of three 2nd order megacycles separated by four majorerosional unconformities. The first megacycle contains terrestrial tomarine syn-rift and early post-rift sediments of Early to Mid-Mioceneage. The second is built up of Late Miocene Lake Pannon deposits,while the third contains those sediments which were deposited inthe remnants of Lake Pannon and in the subsequent fluvial systems,in areas of continuous subsidence associated with basin inversionfrom

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Vasiliev, Iuliana, Koraljka Bakrač, Marijan Kovačić, Hayfaa Abdoul Aziz, and Wout Krijgsman. "Palaeomagnetic Results from the Sarmatian/Pannonian Boundary in North-Eastern Croatia (Vranovi? Section, Našice Quarry)." Geologia Croatica 60, no. 2 (2007): 151–63. http://dx.doi.org/10.4154/gc.2007.04.

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The Sarmatian/Pannonian boundary in the Central Paratethys basin is marked by a major regressive event, which isolated the basin from the open sea and resulted in a palaeoenvironmental change from restricted marine to brackish water ecosystems. The exact age of this environmental change is still ambiguous since direct age control on the boundary interval is lacking, mainly due to the scarcity of suitable sections. The Vranovi? section in the Našice Quarry in Croatia, however, is relatively long and continuously exposed. A detailed sedimentological and biostratigraphic study indicates that it c

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Szemerédi, Máté, Réka Lukács, Andrea Varga, et al. "Permian felsic volcanic rocks in the Pannonian Basin (Hungary): new petrographic, geochemical, and geochronological results." International Journal of Earth Sciences 109, no. 1 (2019): 101–25. http://dx.doi.org/10.1007/s00531-019-01791-x.

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AbstractTwo distinct Permian volcanic epochs were revealed in the Pannonian Basin (eastern Central Europe) by U–Pb zircon geochronology: an older one (~ 281 Ma, Cisuralian) in the ALCAPA Mega-unit (Central Transdanubia, Hungary) and a younger volcanic episode (~ 267–260 Ma, Guadalupian) in the Tisza Mega-unit (Southern Transdanubia and the eastern Pannonian Basin, Hungary). The former is represented by dacitic subvolcanic rocks (dykes) and lavas, while the latter is dominantly by crystal-rich rhyolitic–rhyodacitic/dacitic ignimbrites and subordinate rhyodacitic/dacitic lavas. Whole-rock (major

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