DOCSLIB.ORG

The Karpatian (Late Early Miocene) Flora of the Mecsek Area

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Karpatian (Late Early Miocene) Flora of the Mecsek Area Acta Palaeobotanica 60(1), 51–122, 2020 e-ISSN 2082-0259 https://doi.org/10.35535/acpa-2020-0003 ISSN 0001-6594 The Karpatian (late early Miocene) flora of the Mecsek area LILLA HABLY Botanical Department, Hungarian Natural History Museum, H-1431 Budapest, P.O. box 137, Hungary; e-mail: [email protected] Received 9 September 2019; accepted for publication 28 January 2020 In remembrance of the beautiful summers spent collecting with my family in the Mecsek Mountains ABSTRACT. A rich macroflora has been collected from Karpatian (late early Miocene) layers of the Mecsek Mts during recent decades. The bulk of the fossil assemblage consists of leaves and also fruits of angiosperms. Among the more than a hundred taxa, several endemic species were described: Leguminocarpum mecsekense Andreánszky, Ailanthus mecsekensis Hably, Nyssa gyoergyi sp. nov., Nyssa gergoei sp. nov., Nyssa sp. 1, Clematis csabae sp. nov., Gordonia sp. and Carpolithes gergoei Hably et Erdei sp. nov. Many taxa were last recorded in the Carpathian Basin, e.g. Cedrelospermum, Ziziphus. Other taxa appeared in this flora, e.g. Quercus kubinyii, Podocarpium podocarpum, Liquidambar europaea and Populus populina, and later became dominant in the middle Miocene (Sarmatian) floras or even in the late Miocene (Pannonian) floras. Four main vegetation types were determined. The most significant types are subxerophytic vegetation showing high diversity, swamp veg- etation, riparian vegetation, and a vegetation type growing in habitats with higher rainfall. Thermophilous flora elements are dominant in the assemblage, although “arctotertiary” species also appear. The floristic character of the flora supports the results of an earlier quantitative climate analysis of the Magyaregregy flora, accord- ing to which mean annual temperature was 15.6–16.6°C and coldest-month and warmest-month temperatures were 5–6.2°C and 24.7–27.9°C, respectively. Generally the assemblage presented in this paper extends those climatological findings to the late early Miocene. KEYWORDS: macroflora, late early Miocene, Karpatian, Mecsek Mts, Hungary INTRODUCTION Geological research in the Mecsek Mts dates (2010, 2011), Józsa and Szakmány (2011), back many decades. The extreme variability of Sebe et al. (2015a,b), Miklós (2018) and Kovács its geology, high diversity of rock formations, et al. (2018). and the potential scientific value of strata Palaeontological research on the Mecsek spanning geological ages have attracted many Mts has been very intensive, reflected in work geologists and palaeontologists to this area. published by Strausz (1950). Foraminifers It is beyond the scope of this work to cite and nannoplankton were studied by Korecz- all the relevant literature even in the field of Laky (1968), and Báldi-Beke (1963) respec- Cenozoic research. Only some are mentioned tively. Palynological studies were carried out here. Publications on the Cenozoic geology of by Nagy (1969). The first floristic study of the the Mecsek Mts include Strausz (1926, 1926– Miocene flora of the Mecsek Mts was published 28), Hámor (1964), Nagymarosy (1980, 1985), by Staub (1882), who collected relatively few Chikán (1991), Szakmány and Józsa (1994), specimens from several sites and mentioned Magyar et al. (1999), Sebe (2009), Józsa et. al. the localities Rákpatak-völgy near Ó-Falu, (2009), Barabás (2010, 2011), Konrád and Sebe Nádasd, Hidas, Magyar-Hidas, Német-Hidas, © 2020 W. Szafer Institute of Botany, Polish Academy of Sciences This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited 52 L. Hably / Acta Palaeobotanica 60(1), 51–122, 2020 Váralja, Puszta-Szobák, Komlóvölgy, Aba- be identified. To ground future research, the liget, Tekeres and Rákos, which all, except unidentified specimens are also discussed and for Váralja, represent marl with fish scales. figured. The extremely diverse assemblage is At Váralja, deposits preserving the plant used to reconstruct the flora and vegetation, remains were described as quartz-andesitic and to make a climatic analysis. tuff. The figures, which are drawings of the fossil specimens, help in recognition of some genera and species: Pinus, Daphnogene (given GEOLOGICAL SETTINGS as Cinnamomum by Staub), Ziziphus paradi­ siaca, Zelkova zelkovifolia (given as Planera The area of Mecsek is situated in the SW Ungeri by Staub), Ailanthus confucii, Myrica Pannonian Basin on the Tisza-Dacia megaunit, and Leguminosae gen. et sp. (given as Cas­ a tectonic block south of the Mid-Hungarian sia by Staub). The occurrence of these genera Shear Zone. The Neogene stratigraphy of and species in the small fossil assemblage sug- the eastern Mecsek area was summarized by gests that these taxa were frequent members Hámor (1970), whereas the western part was of the Miocene flora of the Mecsek Mts. Unfor- studied by Chikán (1991) and Barabás (2010). tunately, many of the drawings could not be Widespread Lower Miocene fluvial clastics, identified, and the often-invalid old names do including conglomerates to variegated clays not help in their taxonomic assignment. (Szászvár Formation), are overlain by the Later, Andreánszky (1955) and Pálfalvy Budafa Formation, traditionally regarded as (1953, 1961, 1964, 1967) published data for the of Karpatian (late Burdigalian) age (Gyalog, Miocene Mecsek flora, but they often merely 1996; Gyalog and Budai, 2004; Budai et al., gave lists of flora without providing figures 2015) and consisting of three members: the and descriptions. That work did not constitute Komló Claymarl Member, Pécsvárad Lime- a survey of the Mecsek flora. Over a period of stone Member, and the overlying Budafa more than two decades, I and my colleagues Sandstone Member. The succession is over- have made collections, studied a number of lain by the Badenian (Langhian), with normal taxa, and revised many of them (Hably, 1992b, marine Leitha limestones (Lajta Limestone 2001, 2002; Hably and Thiébaut, 2002). Col- Formation, Pécsszabolcs and Rákos Members) lections made by Krisztina Sebe have yielded in the littoral zone, and offshore sands and data essential to our knowledge of the Mio- silts (Tekeres and Szilágy Formations) in the cene flora of the Mecsek Mts. There are many basins, locally with coal-bearing swamp depos- sampling sites in the Mecsek Mts. Most of the its (Hidas Formation) along the shores. fossil specimens (~90%) were collected in the Most of the fossil plant remains were fos- surroundings of Magyaregregy, mostly from silized in the Komló Claymarl Member (“fish- the so-called fish-scale marl there, but some scale-bearing clay marl”). It is composed of dark also from volcanic deposits. Fossils have been grey, greenish grey, massive or laminated silty preserved in the so-called fish-scale marl in clay marl, calcareous silt and fine sands, with Magyaregregy, Vágyom-völgy; Kisbattyán; numerous fish scales and bones, and sometimes Magyaregregy, Leánykői-árok; Magyaregregy, with tuff interbeds. K/Ar dating measurements Kisréti-árok; Magyaregregy, Farkasordító- from tuff interbeds within the Komló Claymarl árok; Abaliget, Kiskő-hegy; and also Abaliget, showed an age of 16.82 ± 0.65 Ma, i.e. Karpatian Nyáras-völgy. Fossils originated from rhyolitic (late Burdigalian) (Sebe et al., 2019). tuff in Magyaregregy, Almás-patak; Kisbesz- The absence of marine forms in the Péc- terce and Hetvehely, Kán. The late Miocene svárad Limestone and in most of the Komló (Pannonian) flora of Mecsek is not discussed Claymarl indicates a lack of connection to here; details can be found in Hably (2013), normal-salinity seas; thus these rocks are Hably and Sebe (2016) and Hably et al. (2019). lacustrine deposits (Sebe et al., 2019). The The main part of the monograph deals with lake sediments and the fauna suggest that systematics, describing and discussing more instead of a system of smaller lakes, a con- than 100 taxa. The Mecsek flora is extremely tiguous waterbody called Lake Mecsek existed diverse. Beside the well-known common spe- in the area. Karpatian to early Badenian cies, many rare taxa occur in the assemblage, age of the lake is indicated by K/Ar age and and a high number of specimens could not biostratigraphic dating of the overlying marine L. Hably / Acta Palaeobotanica 60(1), 51–122, 2020 53 deposits described above (Sebe et al., 2019). D e s c r i p t i o n. Stem fragment with nodes, The Pécsvárad and Komló Members are both 6.0 cm long, 0.5 cm wide. The stem jointed at interpreted as lake deposits and differ very the nodes. Four strong ridges on stem surface. much from the Budafa Sandstone Member; D i s c u s s i o n. Heer (1855) described numer- therefore, Sebe et al. (2019) united the two ous specimens from the Tertiary flora of Swit- members as a separate formation, the Feked zerland. Andreánszky (1959) published the Formation. Consequently, the fish-scale-bear- species from the Sarmatian and Badenian flo- ing clay marl sediments preserving the plant ras of Hungary. There are several specimens fossils belong to the Feked Formation, Komló in the Miocene flora of Verőce (Hungary; Hably Claymarl Member, dated as Karpatian (late in progress). It occurs in several European Burdigalian) (Sebe et al., 2019). Tertiary floras as Equisetum sp. (Bohemian Massif; Akhmetiev et al., 2009). MATERIAL AND METHODS Pteridopsida The fossil specimens are predominantly leaf impressions, but fruits and seeds, mainly winged Polypodiales ones, also frequently occur. Impressions are generally well preserved in the fish-scale marl owing to the fine- Blechnaceae grained sediment; however, cuticles are not preserved or are too poorly preserved for cuticular analysis. In Woodwardia muensteriana some cases, twigs with some leaves or rarely with leaf (C. Presl in Sternberg) Kräusel and fruit remains are observed. A fossil flower is an exceptional remain, with the stamens, both the theca Pl. 1, fig. 2 and filaments, having been fossilized, but no pollen is Pecopteris münsteriana preserved.
Load more

Recommended publications
  • APPROVED PLANT LIST Midtown Alliance Tree Well Adoption Program
    APPROVED PLANT LIST Midtown Alliance Tree Well Adoption Program Midtown Alliance launched the Tree Well Adoption program with the primary goal of enriching the experience of Midtown’s workers and residents while encouraging sustainability through the use of low-water, urban tolerant plant species. This list of plants was created to aid individuals and organizations in selecting plant material to plant in their adopted tree wells. This plant list is intended to encourage individual character in the tree wells, rather than restrict creativity in the selection of plants. The plants on the approved list were selected based on the following criteria: • Perennial. All plants listed are perennial, meaning they last for two or more growing seasons. Once established, these plants will require less water to maintain than annuals. • Heat tolerant. Plants in tree wells are exposed to high temperatures caused by vehicles and heat reflected from surrounding buildings, asphalt, and other urban surfaces. They must also be tolerant to high daytime temperatures, typical of Atlanta’s summer months, and cold hardy in the winter months. Atlanta is located in USDA Plant Hardiness Zone 7b/8a. • Water wise. Urban tree wells are surrounded by impervious surfaces and thus, are highly susceptible to periods of drought. Suitable plants must be able to survive periods of low rainfall. • Pollution tolerant. Vehicle exhaust may leave deposits and pollutants on plant foliage, which can kill sensitive plants. • Encourage wildlife. Flowering plants attract insects such as butterflies while others provide food sources for birds and other wildlife. • Grown locally. Many of the plants listed are native to the Atlanta area, and all can be found at local nurseries.
    [Show full text]
  • O Babarc Község Önkormányzata 40 80 0 0 2 0 0 Liptód Község
    SZOCIÁLIS ÉS GYERMEKVÉDELMI Brado- Lily Brado- Kesz- Brado- Lily FŐIGAZGATÓSÁG Maszk man gél life tyű lin 1L 1L BARANYA MEGYEI KIRENDELTSÉG 1L 500ml 300ml O Babarc Község Önkormányzata 40 80 0 0 2 0 0 Liptód Község Önkormányzata 40 80 0 0 2 0 0 Versend Község Önkormányzata Kerekítve 100 200 0 0 4 0 0 Összesen 80 160 0 0 4 0 0 SZOCIÁLIS ÉS GYERMEKVÉDELMI Brado- Lily Brado- Kesz- Brado- Lily FŐIGAZGATÓSÁG Maszk man gél life tyű lin 1L 1L BARANYA MEGYEI KIRENDELTSÉG 1L 500ml 300ml O Baksa Község Önkormányzata 400 400 0 0 20 0 0 Adorjás Község Önkormányzata 40 80 0 0 2 0 0 Baranyahídvég Községi Önkormányzat 40 80 0 0 2 0 0 Bogádmindszent Község Önkormányzata 152 232 0 0 7 0 9 Hegyszentmárton Község Önkormányzata 152 232 0 0 7 0 9 Kisszentmárton Község Önkormányzata 40 80 0 0 2 0 0 Ózdfalu Község Önkormányzata 76 116 0 0 3 0 0 Sámod Község Önkormányzata 40 80 0 0 2 0 0 Tengeri Község Önkormányzata Téseny Község Önkormányzata 40 80 0 0 2 0 0 Kerekítve 1000 1400 0 0 47 0 18 Összesen 980 1380 0 0 47 0 18 SZOCIÁLIS ÉS GYERMEKVÉDELMI Brado- Lily Brado- Kesz- Brado- Lily FŐIGAZGATÓSÁG Maszk man gél life tyű lin 1L 1L BARANYA MEGYEI KIRENDELTSÉG 1L 500ml 300ml O Beremendi Gyermekjóléti és Szociális Társulás 1778 1941 14 38 77 10 36 Kistapolca Község Önkormányzata 40 80 0 0 2 0 0 Kerekítve 1800 2000 14 38 79 10 36 Összesen 1818 2021 14 38 79 10 36 SZOCIÁLIS ÉS GYERMEKVÉDELMI Brado- Lily Brado- Kesz- Brado- Lily FŐIGAZGATÓSÁG Maszk man gél life tyű lin 1L 1L BARANYA MEGYEI KIRENDELTSÉG 1L 500ml 300ml O Bicsérd Községi Önkormányzata 40 80 0 0 2 0 0
    [Show full text]
  • Natural Radioactive Element Content of the Old Crystalline Rocks in Southern Transdanubia (Sw Hungary)
    Acta Mineralogica-Petrographica, Szeged, XL, 121-138, 1999 NATURAL RADIOACTIVE ELEMENT CONTENT OF THE OLD CRYSTALLINE ROCKS IN SOUTHERN TRANSDANUBIA (SW HUNGARY) E. PÁL MOLNÁR*, I. VADOS**, I. GERZSON**, B. KÓBOR* •Department of Mineralogy, Geochemistry and Pétrology, Attila József University "Mecsekérc Environment Protection Co. ABSTRACT On the basis of systématisation of several thousand radioactive element content analyses made in laboratories since the 50's, U and Th content of old granitoid rocks of Southern Transdanubia proved to be much higher than the average U and Th content of granitoids in the world. This value of rocks from areas west of Mecsek Mountains as well as near Szalatnak village and Pecs city is twice higher than the world average. Areas west of the Mecsek Mountains show higher U and lower Th contents than areas east of these mountains. Uranium accumulation is higher in aplites and hydrothermal formations than in granites. The western and eastern granites are less and highly sensitive to leaching, respectively. The intensive U migration resulted in significant U accumulation in young sediments in some places. INTRODUCTION Study of natural radioactive element (U /Ra1, Th, K) content of the rocks in Hungary was performed by the Mecseki Ércbányászati Vállalat (Mecsek Ore Mining Company) until 1990, when uranium exploration was stopped in Hungary. Aim of the analyses was to research U sources, therefore, rocks supposed to contain perspective U accumulation were mainly studied. The aim of this paper is to elaborate many thousands radiological data of granitoid rocks, gneisses and amphibolite-like metamorphic rocks coming from Southern Transdanubia (south of the Szekszárd-Kaposvár-Kutas line to the state boundary, and east of the Kutas-Csokonyavisonta-Barcs line to the Danube).
    [Show full text]
  • Act Cciii of 2011 on the Elections of Members Of
    Strasbourg, 15 March 2012 CDL-REF(2012)003 Opinion No. 662 / 2012 Engl. only EUROPEAN COMMISSION FOR DEMOCRACY THROUGH LAW (VENICE COMMISSION) ACT CCIII OF 2011 ON THE ELECTIONS OF MEMBERS OF PARLIAMENT OF HUNGARY This document will not be distributed at the meeting. Please bring this copy. www.venice.coe.int CDL-REF(2012)003 - 2 - The Parliament - relying on Hungary’s legislative traditions based on popular representation; - guaranteeing that in Hungary the source of public power shall be the people, which shall pri- marily exercise its power through its elected representatives in elections which shall ensure the free expression of the will of voters; - ensuring the right of voters to universal and equal suffrage as well as to direct and secret bal- lot; - considering that political parties shall contribute to creating and expressing the will of the peo- ple; - recognising that the nationalities living in Hungary shall be constituent parts of the State and shall have the right ensured by the Fundamental Law to take part in the work of Parliament; - guaranteeing furthermore that Hungarian citizens living beyond the borders of Hungary shall be a part of the political community; in order to enforce the Fundamental Law, pursuant to Article XXIII, Subsections (1), (4) and (6), and to Article 2, Subsections (1) and (2) of the Fundamental Law, hereby passes the following Act on the substantive rules for the elections of Hungary’s Members of Parliament: 1. Interpretive provisions Section 1 For the purposes of this Act: Residence: the residence defined by the Act on the Registration of the Personal Data and Resi- dence of Citizens; in the case of citizens without residence, their current addresses.
    [Show full text]
  • 26/2015 (10.16)
    MAGYAR LABDARÚGÓ SZÖVETSÉG Baranya Megyei Igazgatóság Tel.: +36-72-532-705 Fax.: +36-72-212-715 E-mail: [email protected] Web: baranya.mlsz.hu Bankszámla szám: 11707024-20480734 Cím: H-7621 Pécs, Tímár u. 21. Levelezési cím: H-7601 Pécs, Postafiók 174. Számlázási cím: 1112 Budapest, Kánai út 2. D. 26/2015. (10.16) számú Megyei Hivatalos Értesítő A Versenybizottság határozatai 337/2015 (10.09) számú határozat A Nagyárpádi SK sportszervezet képviselője írásban bejelentette a sportszervezet U15 csapata visszalépését a 2015-2016. évi Megyei U15 bajnokságtól. A Versenybizottság a Nagyárpádi SK csapatát kizárja a bajnokságból V.Sz. 66. § (3) a) pontja alapján. A VB. a Nagyárpádi SK U15 csapata eddig lejátszott mérkőzéseinek eredményét (pontok és gólkülönbség) a bajnokságban résztvevő valamennyi sportszervezetnél eltörli a V.Sz-66. § (4) bekezdése szerint. 338/2015 (10.15) számú határozat A 2015. október 11-ére kiírt PFC Versend – Ivándárda SE Megyei IV. o. „A” cs. ffi felnőtt bajnoki mérkőzés elmaradt, mert a PFC Versend csapata – a mérkőzésre – létszámhiány miatt – nem tudott kiállni (a bajnokság során első alkalommal). A Versenybizottság megállapította, hogy a mérkőzés elmaradásáért a PFC Versend a felelős, ezért a mérkőzés végeredményét – 3-0 gólkülönbséggel – a vétlen Ivándárda SE csapata javára igazolja. A PFC Versend felnőtt csapatának évi összeredményéből a VB. – egyszeri alkalommal – 3 (három) büntetőpontot levon a V.Sz. 55. § (1), (7), (8) a) alapján. 339/2015 (10.15) számú határozat A 2015. október 11-én lejátszott Szentdénes FC – Abaliget SE Megyei IV. o. B cs. ffi felnőtt bajnoki mérkőzésen a Szentdénes FC sportszervezet részéről a létszámhiányos kiállás tényét (a bajnokság során első alkalommal) a VB.
    [Show full text]
  • Vascular Plant and Vertebrate Inventory of Montezuma Castle National Monument Vascular Plant and Vertebrate Inventory of Montezuma Castle National Monument
    Schmidt, Drost, Halvorson In Cooperation with the University of Arizona, School of Natural Resources Vascular Plant and Vertebrate Inventory of Montezuma Castle National Monument Vascular Plant and Vertebrate Inventory of Montezuma Castle National Monument Plant and Vertebrate Vascular U.S. Geological Survey Southwest Biological Science Center 2255 N. Gemini Drive Flagstaff, AZ 86001 Open-File Report 2006-1163 Southwest Biological Science Center Open-File Report 2006-1163 November 2006 U.S. Department of the Interior U.S. Geological Survey National Park Service In cooperation with the University of Arizona, School of Natural Resources Vascular Plant and Vertebrate Inventory of Montezuma Castle National Monument By Cecilia A. Schmidt, Charles A. Drost, and William L. Halvorson Open-File Report 2006-1163 November, 2006 USGS Southwest Biological Science Center Sonoran Desert Research Station University of Arizona U.S. Department of the Interior School of Natural Resources U.S. Geological Survey 125 Biological Sciences East National Park Service Tucson, Arizona 85721 U.S. Department of the Interior Dirk Kempthorne, Secretary U.S. Geological Survey Mark Myers, Director U.S. Geological Survey, Reston, Virginia: 2006 Note: This document contains information of a preliminary nature and was prepared primarily for internal use in the U.S. Geological Survey. This information is NOT intended for use in open literature prior to publication by the investigators named unless permission is obtained in writing from the investigators named and from the Station Leader. Suggested Citation Schmidt, C. A., C. A. Drost, and W. L. Halvorson 2006. Vascular Plant and Vertebrate Inventory of Montezuma Castle National Monument. USGS Open-File Report 2006-1163.
    [Show full text]
  • Közbeszerzési Hatóság Hivatalos Lapja Tájékoztató Az Eljárás Eredményéről a Közbeszerzési Eljárás Eredménye I
    Komló és Térsége szociális alapszolgáltatásainak komplex fejlesztése megnevezésű pályázat keretében informatikai és egyéb eszközök beszerzése Közbeszerzési Értesítő száma: 2018/103 Beszerzés tárgya: Árubeszerzés Hirdetmény típusa: Tájékoztató az eljárás eredményéről/2015 KÉ Eljárást megindító felhívás Közbeszerzési Értesítőben történt közzététele nélkül odaítélt Eljárás fajtája: szerződés az alább felsorolt esetekben A Kbt. 113. § szerinti nyílt eljárás Közzététel dátuma: 2018.05.31. Iktatószám: 8698/2018 CPV Kód: 30000000-9 Komlói Kistérség Többcélú Önkormányzati Ajánlatkérő: Társulás 1 7346 Bikal, Zrínyi u. 2. 7394 Bodolyabér, Petőfi u. 21. 7347 Egyházaskozár, Fő tér 10-11.; 7347 Egyházaskozár, Fő tér 9. 7348 Hegyhátmaróc, Hunyadi u. 71. 7694 Hosszúhetény, Fő u. 168. 7333 Kárász, Petőfi u. 36. 7300 Komló, Kossuth L. u 103.; 7300 Komló, Városház tér 1; 7300. Komló, Kazinczy u, 2-4. 7370 Oroszló, Petőfi u. 29. 7334 Szalatnak, Béke u. 2. 7349 Szászvár, Bányász tér 1. 7333 Vékény, Fő u. 51. 7396 Magyarszék, Kossuth L. u. 51. 7304 Mánfa, Fábián Béla u. 56. 7305 Mecsekpölöske, Szabadság u. 21. 7334 Köblény, Kossuth L. tér 1. 7331 Liget, József Attila u. 9. 7332 Magyaregregy, Kossuth L. u. 73. 7394 Magyarhertelend, Kossuth L. u. 46. 7351 Máza, Kossuth L. u. 24.;7346 Bikal, Zrínyi u. 2. 7347 Egyházaskozár, Fő tér 10-11., 7347 Egyházaskozár, Fő tér 9. 7348 Hegyhátmaróc, Hunyadi u. 71. 7694 Hosszúhetény, Fő u. 168. 7333 Kárász, Petőfi u. 36. Teljesítés helye: 7300 Komló, Kossuth L. u 103.; 7300 Komló, Városház tér 1; 7300. Komló, Kazinczy u, 2-4. 7370 Oroszló, Petőfi u. 29. 7334 Szalatnak, Béke u. 2. 7349 Szászvár, Bányász tér 1. 7333 Vékény, Fő u.
    [Show full text]
  • Cross-Border Bike Project, and Entitled for Funding in the IPA Hungary-Croatia Cross-Border Cooperation Program
    Hungary-Croatia IPA Cross-border Co-operation Programme 2007-2013 PROJECT PARTNER: HUNGARY-CROATIA IPA CROSS-BORDER PÉCS URBAN CO-OPERATION PROGRAM 2007-2013 DEVELOPMENT COMPANY Cross -border Bike Project BICYCLE TOURISM HUHR/1101/1.2.2/1004 Development of Pécs- Osijek-Antunovac- Ivanovac biking route 1 Contents 1.Introduction .......................................................................................................................................... 3 2. The description of the project ............................................................................................................. 4 2.1. Aims .............................................................................................................................................. 5 2.2. Expected results, the position of the project in the International Bicycle Network ................... 8 3. Bicycle tourism .................................................................................................................................. 11 3.1. Bicycle and tourism worldwide .................................................................................................. 11 3.2. Bicycle tourism along the borders .............................................................................................. 15 3.3. Cycling and tourism within the framework of the IPA projects ................................................. 17 3.4. Bicycle and tourism in Baranya and Pécs .................................................................................. 19 3.5.
    [Show full text]
  • Berberine: Botanical Occurrence, Traditional Uses, Extraction Methods, and Relevance in Cardiovascular, Metabolic, Hepatic, and Renal Disorders
    REVIEW published: 21 August 2018 doi: 10.3389/fphar.2018.00557 Berberine: Botanical Occurrence, Traditional Uses, Extraction Methods, and Relevance in Cardiovascular, Metabolic, Hepatic, and Renal Disorders Maria A. Neag 1, Andrei Mocan 2*, Javier Echeverría 3, Raluca M. Pop 1, Corina I. Bocsan 1, Gianina Cri¸san 2 and Anca D. Buzoianu 1 1 Department of Pharmacology, Toxicology and Clinical Pharmacology, “Iuliu Hatieganu” University of Medicine and Pharmacy, Cluj-Napoca, Romania, 2 Department of Pharmaceutical Botany, “Iuliu Hatieganu” University of Medicine and Pharmacy, Cluj-Napoca, Romania, 3 Department of Environmental Sciences, Universidad de Santiago de Chile, Santiago de Chile, Chile Edited by: Berberine-containing plants have been traditionally used in different parts of the world for Anna Karolina Kiss, the treatment of inflammatory disorders, skin diseases, wound healing, reducing fevers, Medical University of Warsaw, Poland affections of eyes, treatment of tumors, digestive and respiratory diseases, and microbial Reviewed by: Pinarosa Avato, pathologies. The physico-chemical properties of berberine contribute to the high diversity Università degli Studi di Bari Aldo of extraction and detection methods. Considering its particularities this review describes Moro, Italy various methods mentioned in the literature so far with reference to the most important Sylwia Zielinska, Wroclaw Medical University, Poland factors influencing berberine extraction. Further, the common separation and detection *Correspondence: methods like thin layer chromatography, high performance liquid chromatography, and Andrei Mocan mass spectrometry are discussed in order to give a complex overview of the existing [email protected] methods. Additionally, many clinical and experimental studies suggest that berberine Specialty section: has several pharmacological properties, such as immunomodulatory, antioxidative, This article was submitted to cardioprotective, hepatoprotective, and renoprotective effects.
    [Show full text]
  • 17/2015 (08.14)
    MAGYAR LABDARÚGÓ SZÖVETSÉG Baranya Megyei Igazgatóság Tel.: +36-72-532-705 Fax.: +36-72-212-715 E-mail: [email protected] Web: baranya.mlsz.hu Bankszámla szám: 11707024-20480734 Cím: H-7621 Pécs, Tímár u. 21. Levelezési cím: H-7601 Pécs, Postafiók 174. Számlázási cím: 1112 Budapest, Kánai út 2. D. 17/2015. (08.14) számú Megyei Hivatalos Értesítő A Versenybizottság határozatai 163/2015 (07.13.) számú határozat A Versenybizottság a Beremendi ÉSK 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 164/2015 (07.13.) számú határozat A Versenybizottság a Boda ÖSE 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 165/2015 (07.13.) számú határozat A Versenybizottság a Bogád SE 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 166/2015 (07.13.) számú határozat A Versenybizottság a Bólyi SE 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 167/2015 (07.13.) számú határozat A Versenybizottság a Dózsa MgTSZ SE Geresdlak 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 168/2015 (07.13.) számú határozat A Versenybizottság a Mohácsi TE 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 169/2015 (07.13.) számú határozat A Versenybizottság a Pécsi EAC 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta. 170/2015 (07.13.) számú határozat A Versenybizottság a Pécsváradi Spartacus SE 2015-2016. évi Baranya Megyei I. o. férfi felnőtt nagypályás bajnokságra beadott nevezését elfogadta.
    [Show full text]
  • Adatok a Baranyai-Dombság Flórájához -..:::: Kitaibelia
    17 KITAIBELIA XIII. évf. 1. szám pp.: 17-28. Debrecen 2008 Adatok a Baranyai-dombság flórájához PURGER Dragica Pécsi Tudományegyetem, TTK, Biológiai Intézet, Állatökológia Tanszék, H-7624 Pécs, Ifjúság útja 6. [email protected] Bevezetés A Mecseken és környékén végzett botanikai kutatások több mint kétszáz éves történetét HORVÁT Adolf Olivér munkái foglalják össze (HORVÁT 1942, 1958, 1975, 1976, 1977). Az elmúlt évtizedekben végzett florisztikai felmérések eredményei számos adattal gazdagították ismereteinket a Baranyai-dombság növényvilágáról (KEVEY 1986, 1988, 1995, 2001, KEVEY & HORVÁT 2000, DÉNES 1997, TÓTH 1998, 1999, 2000). Az utóbbi öt évben országszerte intenzív terepbotanikai kutatások folytak, és a legújabb eredmények (K EVEY 2004, PÁL 2002 a, b, 2003, PURGER 2002 a, 2002 b, CSIKY et al. 2005) arról tanúskodnak, hogy a vizsgált terület még sok feltáratlan botanikai értéket rejt. A vizsgált terület és módszerek A Baranyai-dombság a Mecsekt ől délre-délkeletre terül el. Négy részre tagolódik. Délen a Pécsi-síkság, attól északkeletre, pedig a Geresdi-dombság helyezkedik el. Legnagyobb részét a Dél-Baranyai dombság kistáj teszi ki. A Baranyai-dombság negyedik részét, mint egy sziget a Villányi hegység képezi (MAROSI & SOMOGYI 1990). Ez utóbbi tájegységet azonban e munkában mell őzzük, tekintettel arra, hogy a növényföldrajzi dolgozatokban a Villányi-hegységet általában külön (pl. MOLNÁR 1999), vagy a Mecsekkel együtt tárgyalják (pl. BORHIDI 2006). A félreértések elkerülése végett itt jegyzem meg, hogy az el őző cikkemben (PURGER 2002 a) a „Baranyai-dombság” név alatt a Dél-Baranyai dombságot értettem. Mindazonáltal, az egész térséget, és ezt a területet is, a geográfusok és a botanikusok több néven tárgyalyák: pl.: Mecsekalja (HORVÁT 1942), Tolna-Baranyai dombvidék (BORHIDI 2006, PÁL 2003).
    [Show full text]
  • 8 Book Review.Indd
    88 Chronicle – Hungarian Geographical Bulletin 66 (2017) (1) 88–89. CHRONICLE György Lovász (1931–2016) A prominent representative of Hungarian physical channel erosional geography, one of the last of his generation, passed processes, trig- away on 3 October 2016. Professor György Lovász gered by river was born on 23 May 1931 in Budapest. He studied regulation works. geography and history at the Budapest University, He also pointed where he gathered rich experience in fieldwork out the impact of under the guidance of Professor Sándor Láng. recent tectonics While he worked as a teacher in a vocational school on riverbed inci- of Nagykanizsa and in a primary school of Gyál, sion and subsid- Professor Béla Bulla encouraged him to start with ence of the afore- scientific research. mentioned three In 1956 his first academic paper appeared in print rivers (published on the origin of the ’meridional valleys’ of the Zala in the Journal of Hills, an issue which is still a subject of heated de- Hydrology and bates among Hungarian geomorphologists. He him- Hydromechanics self also returned to this topic and summarised his in 2007). opinion in a paper published in 1970. The thesis written for obtaining the university Working in the Transdanubian Institute of the doctorate in 1959 was concerned with the evolution Hungarian Academy of Sciences in Pécs, his favourite of the Lenti Basin. He also studied the evolution of topics encompassed the geomorphological issues of the Drava floodplain and concluded that the basin, the Mecsek Mountains, such as the planated surfaces, originally thought to be uniform was dissected into the evolution of the Pécs Basin and the karst and loess subbasins during the Holocene.
    [Show full text]