DOCSLIB.ORG

Neuroptera: Osmylidae, Sisyridae)

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

A study on the Hungarian freshwater osmylid and sponge-flies fauna (Neuroptera: Osmylidae, Sisyridae) ABRAHAM LEVENTE ABRAHAM, L.: A study on the Hungarian freshwater osmylid Hungarian freshwater Neuroptera fauna based on the 'and sponge-flies fauna (Neuroptera: Osmyfidae, Sisyridae). collection of their data from the literature and different Abstract: There are four species in the Hungarian freshwater collections of Hungarian museums. Neuroptera fauna according to the redeterminated collections Besides, the seasonal activity of freshwater neu­ found in six Hungarian museums: Osmylus fulvicephalus, Sisyra fuscata, Sisyra terminalis, Sisyra jutlandica. The author ropteroids species in Hungary, the flight activity pat­ gives the collecting data, the distribution maps and both the terns of these species were studied. It gives an impor­ seasonal activity graphs and flight activity patterns of these tant information on their collection possibilities. species. Short evaluations on these species from faunistical, and chorological points of view are also given. Materials and methods Key words: Neuroptera, Osmylidae, Sisyridae, distribution, seasonal activity, day and night activity. The determined collections found in Bakony Natural History Museum (Zirc), Janus Pannonius Museum Introduction Natural History Department (Pecs), Hungarian Natural History Museum (HNHM Budapest), Matra Natural Neuroptera species living presently in. the world are History Museum (Gyongyos), Somogy County Museum known to belong to 17 families (NEW 1989). Most of Natural History Department (Kaposvar) and the Ujhe­ them are considered to be found in terrestrial habitat, Iyi's collection (Budapest) later deposited in HNHM, only five of Neuroptera families (Rapismatidae, were revised. All the other available data from the data­ Osmylidae, Neurothidae, Sisyridae, Polystoechotidae) bases cited in the Hungarian literature were made use .have aquatic larvae or larvae living only near water. of. Besides, several data come from the author's col­ Larvae in family Rapismatidae, Osmylidae and lecting trips. Polystoechotidae are considered to be semiaquatic but Freshwater osmylid and sisyrids were collected by nett­ Neurothidae and Sisyridae species are truly aquatic. ing and beating techniques along the vegetation of Now only Osmylidae, Neurothidae and Sisyridae speci­ watersides and verges. Several specimens were es live in Europe. caught during periods of rest on under bridges, or build­ Osmylidae have about 160 described species distrib­ ings lying close to the water. Light trapping is a very. uted all over the world, expect for North America. Both useful collecting method and, so is collecting them by species occur in Europe, Osmylus fulvicephalus light personally. (Scopoli, 1763) in Hungary, as well, and Osmylus ele­ Summarising the collection data can give a possibility gantissimus Kazanchikov, 1951 in the Crimean penin­ for studying the seasonal activity of imagines. sula and the Caucasian region. Although species Adults are mainly considered to be flying at night, belonging to this genus live near water in damp moss because Malaise traps and suction traps operating by and debris, other species' larvae, being carnivores, are day can catch only few specimens. Adults in the above definitely terrestrial. mentioned collections, collected personally, were pre­ Neurothidae species (10 sp) are mentioned in sumably caught by sweeping. Palaeartic region and in Australia (NEW 1989). The A very simple experiment was carried out to determine only three species, which have not occurred in Hunga­ the activity patterns of these species. ry yet, live in the Mediterranean region in Europe. Its Living specimens were netted and transported into a .larvae are truly aquatic spreading in running streams lab, then they were placed individually in 300-ml glass and rivers. containers covered with paper wadding. Experiments Sisyridae, a small family, is represented by about 50 started in two hours after keeping these insects in glass species all over the world (MONSERRAT 1977), but containers. At least 10 specimens were used in each only five species can be found in Europe (AS POCK­ experiment. Paper wadding were watered moderately HOLZEL 1994). Their larvae are found to be preying on every three hours and temperature was 25 Co ± 1 Co, sponges and bryozoans in deep water lakes and slow­ as DUELLI (1986) pointed out that 100 % of these ly-moving streams and rivers, but in the prepupal and specimens are active above 20 Co. Natural daylight pupal stage within their cocoon, they lie in terrestrial was used in long-day condition but direct sunshine was habitats. avoided. All experiment conditions were kept standard This study summarises the knowledge on the except natural light changes. Activity of these speci- 264 ABRAHAM LEVENTE mens was checked visually, every quarter of an hour 1968 20" RL, July 1, 1973 10" RL, Bakonynana July during a 24-hour-period. At night activity of specimens 19, 1985 10" It, Aug. 10, 1985 19 AL, were observed by the reflected light of a torch, which Bakonyszentkiraly Hajmaspuszta June 5, 1973 19 US, was operated for 5 seconds for each sample to be checked. BalatonfLired Koloska valley May 27, 1972 30" 19 TS, May 29, 1974 10" 39 TS, Bozsok July 28, 1991 10" 19 The following abbreviations are used: NL, B6dvaszilas Vecsem spring May 22, 1990 10" 49 AP. Ag6csy P. RL. Rezbtmyai L. PA, BLikkzserc Oldal valley June 27, 196510" JJ, Cse­ AL. Abraham L. SH. Steinmann H. GyP. Gyulai P. SzCs. Szinetar Cs. repfalu H6r valley June 3, 1981 10" ?, Cserepfalu HA. Haris A. SzGy. Sziraki Gy. Szarka valley July 3, 1981 10" ?, Csorotnek July 14, JJ. Jablonkay J. TP. Tall6s P. 199319 NS, Di6sjen6 Kiralyhaza Aug. 20, 1954 ? US, KGy. Kovacs Gy. TS. T6th S. Domos May 26, 1957 19 US, Forestsmecske June 1, KL. Kovacs L. uA. Uherkovich A. 1989 19 It, June 15, 1989 1? It, July 16, 1990 19 It, LB. Liptay B. US. Ujhelyi S. Feked Karasica stream June 8 , 1987 10" uA. - NS, MF. Mihalyi F. VA. Varga A. June 8, 1989 10" uA, Fels6szolnok Torok stream June ML. M6czar L. WT. With T. 7, 1994 19 uA, Felsotarkany Fekete len June 12, 1984 NS. N6gnidi S. Mt. Malaise trap 10" uA, Galosfa Sarkozi forest July 30, 1989 20" KL, PA. Podlusany A. It. light trap PS. Pazsiczky S. Gorica Gorica stream May 12, 1988 10" uA, Gyal6ka July 15, 1979 10" TS, Gyongyoshalasz July 11, 1979 19 It, Aug. 11, 1979 19 It, Gyongyossolymos Cs6r meadow June 14, 197720" 29 US, June 15, 1977 10" Osmy/us fu/vicepha/us (Scopoli, 1763) US, Gyongyossolymos Nyfrjespuszta June 10, 1971 Abaliget Nyaras valley May 15, 1983 19 uA, Aggtelek 10" Varga Andras, Aug. 14, 1974 10" It, Hajmas stream Bab6tkut June 23, 1993 10" Mt, June 24, 1993 10" Mt, June 5, 1973 10" US, Hidas June 20, 1985 29 uA, Hi­ July 6, 1993 10" Mt, Aggtelek Menes valley May 21, das Mecsekn<3dasdi stream June 2,199410" NS, Hont 1990 10" SzGy, Asz6fo Aug. 10, 1958 10" US, June July 2, 1960 19 LB, Hosszuheteny Hidasi valley July 6, 17, 1965 19 US, Bakonybel Szomorke valley July 5, 1951 10" 19 US, May 16, 1994 20" NS. - uA. J6svafo 1 iii I( / f.r IL FT • I...J. • liii .r. If 1 II XL ~-,-....,l\w'(Q> ~ ~--:: k ,It" " Fig. 1.: Distribution map of Osmylus fulvicephalus in Hungary 1. abra: Az Osmylus fulvicephalus elterjedese Magyarorszagon HUNGARIAN FRESHWATER OSMILYD AND SPONGE-FLIES FAUNA 265 o ++++ +++ + • .. - • ••• • • x xxx x xx x • • • ••• ... _.. • • .- • •• • . .. .. ... ......... ... .. .. I' "I I" 'I"" "I'''''' 'I"" ""I' , ' " " ' 'I " ' '" I " , "i"" 4.20 4.30 5.10 5.20 5.30 6.9 6.19 6.29 7.9 7.19 7.29 8.8 8.18 8.28 time (dd) • Mecsek, Zselic • Alpokalja • Bakony X Borzsony )I( Matra • Biikk + Aggtelek - Zempleni-hegyseg 0 Zalai-dombsag Fig. 2.: Seasonal activity graph of Osmylus fulvicephalus 2. abra: Az Osmylus fulvicephalus szezonalis aktivitasi diagramja July 9, 1970 10" uA, July 1, 1980 ? OS, J6svaf6 J6sva lafOred Garadna valley May 24-28, 1954 19 Os, May spring May 26,198910" 29 uA, May 26,198919 Mt, 24, 1954 10", April 30, 1957 19 WT, April 30, 195920" July 24, 1990 10" uA, J6svaf6 Kees6 May 27, 1989 ?, June 30, 1959 10" ?, Nagyborzsony Kiraly meadow 40" 99 uA, J6svaf6 L6fej spring May 28, 1989 10" 19 June 13, 1957 10" 4 9 MF, June 5, 1966 10" OS, uA, June 19, 199010" 191t, J6svaf6 Tengerszem lake Nagyvisny6 Leany valley June 3, 1957 10" ?, Noszvaj May 29, 1992 19 SzGy, Kaposmer6 June 16, 1991 10" SikfOkOt Aug. 5, 1956 10" ?, Pale July 9, 1979 10" It, HA, Kemenee Kemenee stream June 25, 1950 ?, Parad July ? 1930 10" 29, ? PS, Paszt6 Olomberc KekestetO Pisztrangos lake July 29, 1958 10" OS, Kis­ June 10, 1975 19 VA, Pees SzentkOt June 9, 1992 39 huta K6kapu June 10, 1958 19 Os, May 19, 196630" AL, Porrogszentpal June 27, 1991 10" 39 uA, SH, Kismaros June 1, 1952 ?, KisOjbanya Pasztor Puspokszentlaszl6 June 20, 1989 10" It, Aug. 8, 1989 spring July 1, 1983 10" uA, Koml6 Manfa June 14, 10" It, Aug. 13, 198929 It, Sop ron Tolvaj valley July 15, 1957 10" ML, Koml6 Manfa K61yuk May 26, 1981 10" 1996 19 AL, Szakonyfalu June 23-25, 1957 19 TP, 19 uA, June 11, 1981 19 uA, June 15, 1981 10" 19 July 16,1957 10" OS, Aug. 18, 1957 19 Os, July 12, uA, June 21, 1981 19 uA, July 1, 1981 20" 19 uA, 1959 ? AP, Szarvask6 Margit spring July 17, 197630" Aug. 9, 1981 10" uA, May 1, 1982 19 uA, June 1, ?, July 17, 1976 10" 29 Zald L, Szarvask6 Margit val­ 1982 20" uA, June 3, 1982 30" 19 uA, July 5, 1982 ley June 2, 1961 10", June 2, 1961 10" JJ, Szigliget Hi­ 10" 19 uA, Koml6 Manfa Melegmanyi valley May 24, deg kut July 25, 1990 19 uA.
Recommended publications
  • A Íalvak Foglalkozási Szerkezetének Átalakulása Borsod-Abaúj-Zemplén Megyében

    A Íalvak Foglalkozási Szerkezetének Átalakulása Borsod-Abaúj-Zemplén Megyében

    A íalvak foglalkozási szerkezetének átalakulása Borsod-Abaúj-Zemplén megyében BODNÁR LÁSZLÓ tanszékvezető docens Borsod-Abaúj-Zemplén megye falusi településhálózata a közelmúlt- ban lényegi változásokon ment keresztül. A végbement koncentráció kapcsán már több helyütt felmerültek azok a sokágú kapcsolatok, amelyek a hálózati nagyságrendi struktúrát és a funkcionális struktúrát fűzik szoros egységbe. A funkcionális fejlődést, egy-egy megye országos fejlődési áramkörbe való gyorsabb bekapcsolódását éppen az ott uralkodó hálózati struktúra lassítja vagy éppen meggátolja. Módosításuk, cLZclZ ct társadalom új térbeli igényeihez való „igazításuk" magas beruházási költségkihatásain jelentkezik. A múltbeli örökség mellett — amely a korábbiakból átöröklött eredmé- nyek összegzője, s egyben a fejlődési folyamatosság biztosítója — a hálózat funkcionális felépítettségc tölti ki tartalommal a településhálózat funkcioná- lis szerkezetét. Ezek, az egymással bonyolult kölcsönkapcsolati rendszerben álló funk- ciók, mint a társadalom alapvető „életjelenségei", mindegyikének sajátos térbeli rendje van, együttesük pedig a funkcionális hálózat térbeli rendszeré- nek meghatározója. A múltbeli rendhez képest új térbeli hálózati struktúra kialakítását, azaz az adott térségnek a maga meglévő igényeihez való formálását tükrözi a településhálózat szerkezete. A településhálózat funkcionális szerkezetének aránytalanságai — azaz a közeli és régmúltból öröklött egyenlőtlen gazdasági fejlettség — miatt, a ter- mészeti erőforrások adta területi pontenciáltól nem kellő
  • Natural Radioactive Element Content of the Old Crystalline Rocks in Southern Transdanubia (Sw Hungary)

    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).
  • Act Cciii of 2011 on the Elections of Members Of

    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.
  • Bükki Nemzeti Park Igazgatóság 2018

    Bükki Nemzeti Park Igazgatóság 2018

    TÁJÉKOZTATÓ A BÜKKI NEMZETI PARK IGAZGATÓSÁG 2018. –BAN BORSOD-ABAÚJ-ZEMPLÉN MEGYE TERÜLETÉN VÉGZETT TEVÉKENYSÉGEIRŐL Összeállította: Rónai Kálmánné Dudás György 2019 június 1. BEVEZETÉS ................................................................................................................................................................ 1 2. A BÜKKI NEMZETI PARK IGAZGATÓSÁG RÖVID BEMUTATÁSA ............................................................. 3 A BÜKKI NEMZETI PARK IGAZGATÓSÁG ALAPFELAFDATAI .............................................................. 3 3. A BÜKKI NEMZETI PARK IGAZGATÓSÁG FŐBB TEVÉKENYSÉGEI 2019 – BEN, KIEMELTEN BORSOD-ABAÚJ-ZEMPLÉN MEGYE TERÜLETÉN .............................................................................................. 4 3.1. VÉDETT TERÜLETEK TERMÉSZETVÉDELMI KEZELÉSE, FENNTARTÁSA, ÉLŐHELY-FEJLESZTÉS, ÉLŐHELY-REKONSTRUKCIÓ ............................................................................................................... 4 3.2.FAJMEGŐRZÉSI PROGRAMOK ..................................................................................................... 14 3.3. ÉLETTELEN TERMÉSZETI ÉRTÉKEK MEGŐRZÉSE, FÖLDTANI, TÁJI ÉS KULTÚRTÖRTÉNETI ÉRTÉKEK MEGŐRZÉSE ..................................................................................................................... 23 3.4. TERMÉSZETVÉDELMI ŐRSZOLGÁLAT ....................................................................................... 28 Hatósági feladatellátás .............................................................................................................
  • Environmental Protection

    Environmental Protection

    HUHR/1101/2.1.4/0005 Sectoral Studies: 4., Environmental Protection Environmental Protection Contents Situation Analysis .................................................................................................................. 2 Historic Preservation ......................................................................................................... 2 Nature Conservation, Protected Areas and Biodiversity ..................................................... 3 National Parks ............................................................................................................... 4 Water Management ........................................................................................................... 4 Surface Waters .............................................................................................................. 4 Inland Inundation ........................................................................................................... 5 Groundwater .................................................................................................................. 5 Precipitation ................................................................................................................... 5 Drinking Water ............................................................................................................... 6 Wastewater Management .................................................................................................. 6 Solid Waste Collection and Handling ................................................................................
  • Adatok a Déli-Bakony Flórájához III. 1113 KITAIBELIA VIII

    Adatok a Déli-Bakony Flórájához III. 1113 KITAIBELIA VIII

    MÉSZÁROS A. – SIMON P.: Adatok a Déli-Bakony flórájához III. 1113 KITAIBELIA VIII. évf. 1. szám pp.: 113-116. Debrecen 2003 Adatok a Déli-Bakony flórájához III. MÉSZÁROS András – SIMON Pál Balaton-felvidéki Nemzeti Park Igazgatóság, H-8200 Veszprém, Vár u. 31. Bevezetés Jelen közleményben folytatjuk a Déli-Bakony florisztikai kutatása (MÉSZÁROS – SIMON, 2001, 2002) során gyûjtött adataink közlését. Az alábbiakban a 2002-ben elõkerült florisztikai újdonságokat adjuk közre. (A Déli-Bakony flórakutatását elõzõ cikkeinkben ismertettük.) Az itt közölt adatok Veszprém, Nemesvámos, Tótvázsony, Nagyvázsony, Öcs, Pula, Taliándörögd, Úrkút, Padragkút és Hegyesd községhatárokból származnak. A fajok elnevezése és sorrendje SIMON (2000) munkája alapján készült. Az adatok egy részérõl fotódokumentáció és herbáriumi dokumentáció is létezik. A fajok lelõhelyeinek elnevezése 1: 10000-es erdészeti üzemi térképek, valamint 1: 10000-es EOTR térképek alapján történt, de néhány esetben, zárójelben téve a helyi vagy a turistatérképeken található elnevezések is szerepelnek. Amennyiben a térképeken nem találtunk földrajzi nevet egy adott területre úgy a helyi elnevezést alkalmaztuk. KOVÁCS J. A. (2002) közleményében számos adatunk (MÉSZÁROS – SIMON 2001) – hivatkozás nélküli – megerõsítését olvashatjuk. Itt szeretnénk megjegyezni, hogy a közelmúltban más szerzõ által már megtalált és leközölt adatokat nem publikálunk. Florisztikai adatok Equisetum telmateia Ehrh.: A padragkúti Köleskepe- Ranunculus lanuginosus L.: A nagyvázsonyi árok útszegélyeiben, árkaiban gyakori. Metszõ-árokban és a padragkúti Köleskepe-árokban Equisetum hyemale L.: A padragkúti Köleskepe-árok szálanként elõfordul. László kút környéki szakaszán több ezer töves Rubus idaeus L.: A nagyvázsonyi Dozmat-rét állománya található. melletti kõbányában kb. 100 m2 –t borít sarjtelepe, Ophioglossum vulgatum L.: Úrkút községhatárban a mely fõként meddõn található. Mangániszap-tároló területén nyír (Betula pendula) Filipendula ulmaria (L.) Maxim.: A nagyvázsonyi uralta foltokban kisebb állományai találhatók.
  • Óvodafenntartó Társulás

    Óvodafenntartó Társulás

    Csurgó Kistérségi Többcélú Társulás Társulási Megállapodásának Módosító Okirata Csurgó Kistérségi Többcélú Társulás Társulási Megállapodását (a továbbiakban: Megállapodás) a társulás alapító tagjai, azaz Berzence Nagyközség Önkormányzat Képviselő-testülete, Csurgó Város Önkormányzat Képviselő-testülete, Csurgónagymarton Község Önkormányzat Képviselő-testülete, Gyékényes Község Önkormányzat Képviselő-testülete, Iharos Község Önkormányzat Képviselő-testülete, Iharosberény Község Önkormányzat Képviselő-testülete, Inke Község Önkormányzat Képviselő-testülete, Őrtilos Község Önkormányzat Képviselő-testülete, Pogányszentpéter Község Önkormányzat Képviselő-testülete, Porrog Község Önkormányzat Képviselő-testülete, Porrogszentkirály Község Önkormányzat Képviselő-testülete, Porrogszentpál Község Önkormányzat Képviselő-testülete, Somogybükkösd Község Önkormányzat Képviselő-testülete, Somogycsicsó Község Önkormányzat Képviselő-testülete, Somogyudvarhely Község Önkormányzat Képviselő-testülete, Szenta Község Önkormányzat Képviselő-testülete, Zákány Község Önkormányzat Képviselő-testülete valamint Zákányfalu Község Önkormányzata Képviselő-testülete, a közöttük 2004. június 21-én létrejött és többször módosított Megállapodást az alábbiak szerint módosítják: 1. A Csurgó Kistérségi Többcélú Társulás társulási megállapodás I. Általános rendelkezések fejezet 3. pontja helyébe a következő rendelkezés lép: „3. A Társulás székhelye: 8840 Csurgó, Széchenyi tér 2. Lakosságszáma: 17158 Fő. A továbbiakban a társulás lakosságszáma a költségvetési törvényben meghatározott
  • IDŐJÁRÁS Quarterly Journal of the Hungarian Meteorological Service Vol

    IDŐJÁRÁS Quarterly Journal of the Hungarian Meteorological Service Vol

    IDŐJÁRÁS Quarterly Journal of the Hungarian Meteorological Service Vol. 117, No. 2, April – June, 2013, pp. 219–237 Projected changes in the drought hazard in Hungary due to climate change Viktória Blanka1*, Gábor Mezősi1*, and Burghard Meyer2 1University of Szeged, Egyetem u. 2-6. H-6722 Szeged, Hungary 2Universität Leipzig, Ritterstraße 26. DE-04109 Leipzig, Germany *Corresponding authors E-mails: [email protected], [email protected] (Manuscript received in final form December 18, 2012) Abstract–In the Carpathian Basin, drought is a severe natural hazard that causes extensive damage. Over the next century, drought is likely to remain one of the most serious natural hazards in the region. Motivated by this hazard, the analysis presented in this paper outlines the spatial and temporal changes of the drought hazard through the end of this century using the REMO and ALADIN regional climate model simulations. The aim of this study was to indicate the magnitude of the drought hazard and the potentially vulnerable areas for the periods 2021–2050 and 2071–2100, assuming the A1B emission scenario. The magnitude of drought hazard was calculated by aridity (De Martonne) and drought indices (Pálfai drought index, standardised anomaly index). By highlighting critical drought hazard areas, the analysis can be applied in spatial planning to create more optimal land and water management to eliminate the increasing drought hazard and the related wind erosion hazard. During the 21st century, the drought hazard is expected to increase in a spatially heterogeneous manner due to climate change. On the basis of temperature and precipitation data, the largest increase in the drought hazard by the end of the 21st century is simulated to occur in the Great Hungarian Plain.
  • Analysis of the Transdanubian Region of Hungary According to Plant Species Diversity and Floristic Geoelement Categories

    Analysis of the Transdanubian Region of Hungary According to Plant Species Diversity and Floristic Geoelement Categories

    FOLIA OECOLOGICA – vol. 44, no. 1 (2017), doi: 10.1515/foecol-2017-0001 Review article Analysis of the Transdanubian region of Hungary according to plant species diversity and floristic geoelement categories Dénes Bartha1*†, Viktor Tiborcz1* *Authors with equal contribution 1Department of Botany and Nature Conservation, Faculty of Forestry, University of West Hungary, H-9400 Sopron, Bajcsy-Zsilinszky 4, Hungary Abstract Bartha, D., Tiborcz, V., 2017. Analysis of the Transdanubian region of Hungary according to plant species diversity and floristic geoelement categories.Folia Oecologica, 44: 1–10. The aim of this study was to describe the proportion of floristic geoelements and plant biodiversity in the macroregions of Transdanubia. The core data source used for the analysis was the database of the Hungar- ian Flora Mapping Programme. The analysed data were summarized in tables and distribution maps. The percentage of continental elements was higher in dry areas, whereas the proportion of circumboreal elements was higher in humid and rainy parts of Transdanubia. According to the climatic zones, the highest value of continental geoelement group occurred in the forest-steppe zone. The plant species diversity and geoele- ments were analysed also on a lower scale, with Transdanubia specified into five macroregions. The highest diversity values were found in the Transdanubian Mountain and West-Transdanubian regions because of the climatic, topographic, and habitat diversity. Keywords Borhidi’s climatic zones, climatic variables, floristic geoelement categories, macroregion, species diversity, Transdanubia Introduction Hungary is influenced by many different environmental In some European countries, floristic assessments conditions which are also reflected in the floristic diver- have already been made based on published flora at- sity.
  • February 2009 with the Support of the Conference on Jewish Material Claims Against Germany & the Conference of European Rabbis

    February 2009 with the Support of the Conference on Jewish Material Claims Against Germany & the Conference of European Rabbis

    Lo Tishkach Foundation European Jewish Cemeteries Initiative Avenue Louise 112, 2nd Floor | B-1050 Brussels | Belgium Telephone: +32 (0) 2 649 11 08 | Fax: +32 (0) 2 640 80 84 E-mail: [email protected] | Web: www.lo-tishkach.org The Lo Tishkach European Jewish Cemeteries Initiative was established in 2006 as a joint project of the Conference of European Rabbis and the Conference on Jewish Material Claims Against Germany. It aims to guarantee the effective and lasting preservation and protection of Jewish cemeteries and mass graves throughout the European continent. Identified by the Hebrew phrase Lo Tishkach (‘do not forget’), the Foundation is establishing a comprehensive publicly-accessible database of all Jewish burial grounds in Europe, currently featuring details on over 9,000 Jewish cemeteries and mass graves. Lo Tishkach is also producing a compendium of the different national and international laws and practices affecting these sites, to be used as a starting point to advocate for the better protection and preservation of Europe’s Jewish heritage. A key aim of the project is to engage young Europeans, bringing Europe’s history alive, encouraging reflection on the values that are important for responsible citizenship and mutual respect, giving a valuable insight into Jewish culture and mobilising young people to care for our common heritage. Preliminary Report on Legislation & Practice Relating to the Protection and Preservation of Jewish Burial Grounds Hungary Prepared by Andreas Becker for the Lo Tishkach Foundation in February 2009 with the support of the Conference on Jewish Material Claims Against Germany & the Conference of European Rabbis.
  • Research Article

    Research Article

    kj8 z Available online at http://www.journalcra.com INTERNATIONAL JOURNAL OF CURRENT RESEARCH International Journal of Current Research Vol. 11, Issue, 05, pp.3546-3552, May, 2019 DOI: https://doi.org/10.24941/ijcr.34579.05.2019 ISSN: 0975-833X RESEARCH ARTICLE THE CAVE OPENING TYPES OF THE BAKONY REGION (TRANSDANUBIAN MOUNTAINS, HUNGARY) *Márton Veress and Szilárd Vetési-Foith Department of Physical and Geography, University of Pécs, Pécs, Hungary ARTICLE INFO ABSTRACT Article History: The genetic classification of the cave openings in the Bakony Region is described. The applied Received 09th February, 2019 methods are the following: studying the relation between the distribution of phreatic caves and the Received in revised form quality of the host rock and in case of antecedent valley sections, making theoretical geological 12th March, 2019 longitudinal profiles. The phreatic caves developed at the margins of the buried karst terrains of the th Accepted 15 April, 2019 mountains. The streams of these terrains created epigenetic valleys, while their seeping waters created th Published online 30 May, 2019 karst water storeys over the local impermeable beds. Cavity formation took place in the karst water storeys. Phreatic cavities also developed in the main karst water of the mountains. The caves are Key Words: primarily of valley side position, but they may occur on the roof or in the side of blocks. The cavities Gorge, Phreatic Cave, of valley side position were opened up by the streams downcutting the carboniferous rocks (these are Development of Cave openings. the present caves of the gorges). While cavities of block roof position developed at the karst water storey at the mound of the block.
  • Settlement Slovak County District (JÁRÁS) FHL Film Nr

    Settlement Slovak County District (JÁRÁS) FHL Film Nr

    Page 1 of 31 Slovak Settlement Ordered Settlement (Magyar) (Cont') Settlement Slovak County District (JÁRÁS) FHL Film Nr. Sellye Aala Nytra HORNÁ NITRA 2150642 Item 3 Abrahámfalu Abrahamovce Szepes 2162280 Item 2 Abrány Abranovce Saros 2162305 Item 1 Agyidócz Adidovce Zemplin 722668 Elecske Aleksince Nytra HORNÁ NITRA 2159445 Item 5 Elecske (folyt.) Aleksince Nytra HORNÁ NITRA 2159446 Item 1 Andacs Andac Nytra HORNÁ NITRA 2159448 Item 4 Andód Andovce Nytra DOLNÁ NITRA 2150804 Item 2 Andód (folyt.) Andovce Nytra DOLNÁ NITRA 2150805 Item 1 Andrásvágás Andrasovce Saros 2189248 Item 3 Orló Andrejovka Saros 2162317 Item 2 Ardanóc Ardanovce Nytra DOLNÉ OBDOKOVCE 2154311 Item 10 Dvorecz puszta Ardanovce Nytra DOLNÉ OBDOKOVCE 2159436 Item 4 Arnótfalu Arnutovce Szepes 2162280 Item 3 Bábafalu Babie Saros 2189407 Item 1 Balpataka Babín Potok Saros 2150640 Item 4 Babindol Babindol Nytra HORNÁ NITRA 2159440 Item 6 Bacska Backa Zemplin 722671 Bacskó Backov Zemplin 722671 Bajcs puszta Bajc Komárom UDVARD 2202017 Item 1 Bajor Bajerov Saros 2189246 Item 1 Bajorvágás Bajerovce Saros 2162317 Item 3 Baldócz Baldovce Szepes 2162280 Item 4 Banka Banka Nytra NOVÉ MESTO NAD VÁHOM 2150817 Item 3 Banka (folyt.) Banka Nytra NOVÉ MESTO NAD VÁHOM 2150818 Item 1 Bánkeszi Bánov Nytra DOLNÁ NITRA 2150655 Item 6 Bánkeszi (folyt.) Bánov Nytra DOLNÁ NITRA 2150656 Item 1 Bánócz Bánovce nad Ondavou Zemplin 722672 Bánszka Banské Zemplin 722673 Barancs Baranc Zemplin 722672 Bartos Lehotka Bartosova Lehôtka Bars 2201274 Item 2 Bartosfalu Bartosovce Saros 2150640 Item 5 Baskócz