108 research outputs found
A Würm glaciális második felének növénytakaró változásai a Kárpát-medence alföldi és hegyvidéki régióiban: refúgiumok és erdőtüzek
KĂ©sĹ‘glaciális Ă©s holocĂ©n oxigĂ©nizotĂłp-alapĂş klĂmarekonstrukciĂł hibahatár-becslĂ©se tavi ĂĽledĂ©kek elemzĂ©se alapján
A stabilizotĂłp-arány tavi ĂĽledĂ©kek paleoklimatolĂłgiai tanulmányozásában törtĂ©nĹ‘ használata a vizek 18O/16O arányának a klĂmával, fĹ‘kĂ©nt a hĹ‘mĂ©rsĂ©klettel valĂł összefĂĽggĂ©sĂ©n alapul (Dansgaard, W. 1964). Adott terĂĽleten a hĹ‘mĂ©rsĂ©klet változásával változik a csapadĂ©k izotĂłp-összetĂ©tele is. Rövidtávon ez az Ă©vszakonkĂ©nti változást, ezerĂ©ves lĂ©ptĂ©kben pedig a klĂmaváltozás mĂ©rtĂ©kĂ©t tĂĽkrözi (Clarke, I. D. – Fritz, P. 1997).
A tavi ĂĽledĂ©kszelvĂ©nyek δ18O vizsgálata klasszikusan az ĂĽledĂ©k biogĂ©n karbonát Ă©s/vagy karbonátvázas biogĂ©n alkotĂłin törtĂ©nik (Morley, D. W. et al. 2004; Barker, P. – Leng, M. J. 2006; Swann, G. E. A. – Leng, M. J. 2009). Karbonátmentes környezetben azonban más megoldást kell találnunk, melyre legalkalmasabbnak az ĂĽledĂ©kben megĹ‘rzött diatĂłmák1 (kovamoszatok, Bacillariophyceae) vázainak szilĂcium-dioxidja bizonyult, melybe az oxigĂ©n a tĂł vizĂ©bĹ‘l Ă©pĂĽl be növekedĂ©sĂĽk során (Magyari, E. K. et al. 2012)
Service marketing examination of Opusztaszer Heritage Park as a rural destination
Today the service industries are developing rapidly therefore the service marketing tasks are getting more
and more into the focus. Those who are engaged in the subject do researches to explore the emotions,
attitudes and purchasing motives in decision-making and the purchasing processes of different services.
Decisions are made not only by companies but costumers, parents, families and circles of friends, too, when
they plan their programs for the weekend considering their income and expenses. That is why we feel
important to examine our subject on the basis of the service marketing of the Opusztaszer National Heritage
Park, which takes a prominent part in the cultural life of the Southern Hungarian Plain, in order to render
help to improve the services of the institution. The examination is complemented with a non-representative
questionnaire survey which, nevertheless, is suitable to give the background to a wider survey. On the basis
of the answers given some chances of improvement have been seen which we are planning to recommend for
the Opusztaszer National Heritage Park
Service marketing examination of Opusztaszer Heritage Park as a rural destination
Today the service industries are developing rapidly therefore the service marketing tasks are getting more and more into the focus. Those who are engaged in the subject do researches to explore the emotions, attitudes and purchasing motives in decision-making and the purchasing processes of different services. Decisions are made not only by companies but costumers, parents, families and circles of friends, too, when they plan their programs for the weekend considering their income and expenses. That is why we feel important to examine our subject on the basis of the service marketing of the Opusztaszer National Heritage Park, which takes a prominent part in the cultural life of the Southern Hungarian Plain, in order to render help to improve the services of the institution. The examination is complemented with a non-representative questionnaire survey which, nevertheless, is suitable to give the background to a wider survey. On the basis of the answers given some chances of improvement have been seen which we are planning to recommend for the Opusztaszer National Heritage Park
Limnological changes and chironomid-inferred summer air temperature from the Late Pleniglacial to the Early Holocene in the East Carpathians
Here we provide the first chironomid record and associated summer air-temperature (T VII ) reconstruction between ca. 16,800-9100 cal yr BP from Lake Saint Anne (SZA), situated in the Eastern Carpathians. SZA was formed by the youngest volcanic eruption of Ciomadul volcano at ca. 29,600 cal yr BP. Our main goals in this study are to test whether warming after Heinrich event 1 (H1; ca. 16,200 cal yr BP) had similar amplitude to the late glacial warming, while Younger Dryas (YD) summers remained relatively warm in this region of Europe. We found the most remarkable chironomid assemblage change with a T VII increase of ~3.5-3.8°C at ca. 16,350 cal yr BP at SZA, followed by another slight T VII increase of ~0.8-1.0°C at ca. 14,450 cal yr BP. Only very minor temperature variations were recorded between 14,450 cal yr BP and 11,700 cal yr BP, with an unexpected T VII decrease in the Early Holocene. Variations in water depth together with increasing analogue problems and paludification from ca. 14,200 cal yr BP onwards may have influenced the reliability of our paleotemperature record obtained from SZA. In addition, Sphagnum -indicated decreasing pH, and hence decreasing nutrient level, likely overrode the effect of summer air-temperature changes during the Early Holocene, and this may explain the bias in the chironomid-inferred summer air-temperature reconstruction in the Early Holocene section
Társas megkĂĽzdĂ©si minták Ă©s identitáskonstrukciĂłs folyamatok azonosĂtása törtĂ©nelmi tárgyĂş elbeszĂ©lĂ©sekben = Exploring coping strategies and processes of identity construction in fictional and non-fictional historical narratives
KĂsĂ©rleti kutatásokkal igazoltuk, hogy a csoportközi Ă©szlelĂ©sben a saját csoport iránti pozitĂv elfogultság, illetve a kĂĽlsĹ‘ csoportok negatĂv megkĂĽlönböztetĂ©se akkor jelentkezik, ha a helyzetben a csoportok közötti törtĂ©nelmi konfliktus aktualizálĂłdik. Az Ă©szlelĂ©sben megnyilvánulĂł elfogultság fĂĽgg a szemĂ©lyek nemzeti azonosulásának tĂpusátĂłl Ă©s mĂ©rtĂ©kĂ©tĹ‘l. Ugyanebben a kĂsĂ©rletsorozatban kidolgoztuk Ă©s igazoltuk a törtĂ©nelmi pályához kapcsolĂłdĂł kollektĂv Ă©rzelmek kategĂłriáját. A kutatás cĂ©ljára kifejlesztett tartalomelemzĹ‘ eszközökkel három törtĂ©nelmi esemĂ©ny (honfoglalás, kiegyezĂ©s, Trianoni bĂ©keszerzĹ‘dĂ©s) szöveges bemutatását elemeztĂĽk 1900-tĂłl napjainkig megjelent közĂ©piskolás törtĂ©nelem könyvekben, illetve 16 törtĂ©nelmi esemĂ©nyt elemeztĂĽnk kortárs általános-Ă©s közĂ©piskolai tankönyvekben valamint egy 500 fĹ‘s mintátĂłl nyert laikus törtĂ©nelmi elbeszĂ©lĂ©sekben. Az eredmĂ©nyek azt mutatták, hogy mind a törtĂ©nelemkönyvek, mind a laikus elbeszĂ©lĂ©sek a magyar csoportot illetĹ‘en alacsony ágenciájĂş identitást közvetĂtenek. A huszadik századi traumatikus esemĂ©nyek kognitĂv elaboráciĂłja csak az utĂłbbi Ă©vtizedben indult meg. A törtĂ©nelmi regĂ©nyek identitás közvetĂtĹ‘ funkciĂłjának tartalomelemzĂ©ses vizsgálatiban megállapĂtottuk, hogy a csoportközi konfliktust elbeszĂ©lĹ‘ szövegek kategoriális empátiát hĂvnak elĹ‘. A regĂ©nyek magyar szereplĹ‘inek Ă©rzelmi kĂ©szletĂ©t a depresszĂv dinamika jellemzi. Nagy számban jelennek meg a törtĂ©nelmi pályához kapcsolĂłdĂł Ă©rzelmek. | Experimental research provided evidence that ingroup favoritism in intergroup perception is enhanced by actualization of historical intergroup conflict. Ingroup favoritism depends on type and strength of national identification. In a series of experiments we have elaborated and verified the category of historical trajectory related emotions as a type of collective emotions. Content analytic tools which have been developed for the purpose of studying historical texts were used to analyzing three historical events in high school history books published from 1900 on. Similar study was carried out with 16 historical events in contemporary secondary school and high school history books, and with lay history stories gathered from a stratified sample of 500 subjects. Results show that both history books and lay stories transmit a kind of national identity which is characterized by low agency. Cognitive elaboration of the traumatic events of the twentieth century has begin only int he past decade. Studies of historical novels' functions in mediating national identity provided evidence that narratives on intergroup conflicts evoke categorial empathy. Emotional repository of Hungarian characters is dominated by depressive dynamics. There is a high frequency of historical trajectory related emotions
Linguistic Parameters of Spontaneous Speech for identifying Mild Cognitive Impairment and Alzheimer’s Disease
Holocene treeline and timberline changes in the South Carpathians (Romania): Climatic and anthropogenic drivers on the southern slopes of the Retezat Mountains
Two high-altitude lake-sediment sequences (Lake Lia, 1910 m a.s.l. and Lake Bucura, 2040 m a.s.l.) from the Retezat Mountains (South Carpathians, Romania) were analysed using multi-proxy methods to study responses of treeline, timberline and alpine/subalpine vegetation to climate change and human impact during the past 16,000 years. Woody species (Pinus mugo, Pinus cembra, Picea abies and Juniperus communis) reached Lake Lia between 12,000 and 11,800 cal. yr BP, whereas P. mugo colonised the shores of Lake Bucura at 9600 cal. yr BP. Lake Lia was in the timberline ecotone between 8000 and 3200 cal. yr BP, in semi-open P. cembra and Picea abies woodland, probably mixed with P. mugo on the steeper slopes. Lake Bucura was surrounded by the upper part of the krummholz zone during the mid-Holocene. The increase in P. cembra after c. 6000 cal. yr BP around Lake Lia suggests that the composition of the timberline forest changed. The disappearance of P. cembra and Picea abies around Lake Lia at ~3000 cal. yr BP reflects descent of the timberline. A large mean July temperature decline between 3300 and 2800 cal. yr BP may have driven or at least contributed to the descent of the Picea abies?P. cembra forests. An increase in human indicator pollen types in Lake Bucura around 4200 cal. yr BP may reflect human impact in the naturally open alpine zone in the Late Bronze Age. In contrast, human impact likely appeared considerably later, around 2650 cal. yr BP (Early Iron Age) around Lake Lia in the upper subalpine zone. Human impact likely intensified after 2200 cal. yr BP at both sites that resulted in the lowering of the krummholz zone. We conclude that climate change and human impact both played an important role in the lowering of the treeline and timberline in the late-Holocene
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