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    Wyświetlanie 1-6 z 6
    Tytuł:
    Kresťanstvo u Germánov v Karpatskej kotline v 6. storočí
    Christianity among Germanic tribes in the Carpathian Basin in the sixth century
    Autorzy:
    Bystrický, Peter
    Powiązania:
    https://bibliotekanauki.pl/articles/2164346.pdf
    Data publikacji:
    2014-06-30
    Wydawca:
    Wydawnictwo Adam Marszałek
    Tematy:
    German tribes
    early middle ages
    christiany
    Carpathian Basin
    Opis:
    The fourth century saw the beginning of spreading Christianity among Germanic people. The mission of bishop Ulfi las, however, ended in 348 and persecuted Christian Goths fl ed to the territory of the Roman Empire. After the destruction of Gothic kingdoms, the fl eeing Goths were allowed by the Roman emperor Valens to cross the Danube, probably only on condition that they would adopt new faith. Since the emperor himself was an Arian and Arianism preferred theological teaching in the Roman Empire, the Goths, and later other East Germanic tribes, adopted this doctrine instead of Nicene Creed. Germanic people learned only the basic principles of faith and then just continued with their beliefs. Moreover, Jesus was deemed not the only God, but one of many gods. The second part of the study offers a survey of written sources on the Christianity among Germanic tribes in the Carpathian Basin in the sixth century – Rugians, Heruls, Gepids and Lombards. The Rugians led by the king Feletheus (Feva) and his Arian wife Giso dwelt on the left bank of the Danube, opposite the Roman province of Noricum, where at that time St. Severinus preached Christianity, established monasteries, organised defence or evacuation, redeemed captives, procured corn for the starving and healed the sick. Humble and pious Severinus won himself such a reputation that even barbarian kings respected him and listened to his advice and prophecies. The neighbouring Heruls, however, were pagans and sometimes invaded barely defended provinces of Noricum and Pannonia. Though their king received baptism in 528, many of them remained pagans and, according to Procopius, they were the wickedest people in the whole world. The Gepids, like Goths, converted to Arianism. The most signifi cant traces of Gepid Christianity are found in the territory of Pannonia II, especially near the Roman town of Sirmium. Sirmium was one of the most important centres of early Christianity and in the late sixth century, the town having become a seat of Gepid Arian bishop. On the other hand, Lombard Arianism is very problematical. The fi rst mention of their orthodox faith comes from Procopius. Paganism, however, was retained not only by the majority of the tribe, but also by the king and his retinue, even at the time 568 invasion in Italy. Arianism among Lombards probably gained strength only in Italy, where a number of subjugated Gepids accompanied them and where remnants of Arian Goths continued to live. From Alboin to Aripert (altogether 9 rulers) only two kings are mentioned as Arians and only two as Catholics. Though these Germanic tribes adopted Christianity in the Carpathian Basin, they did not stay there long enough to become true Christians. With Slavs and Avars replacing them, the Christianisation of Central Europe had to start from scratch.
    Źródło:
    Historia Slavorum Occidentis; 2014, 1(6); 13-41
    2084-1213
    Pojawia się w:
    Historia Slavorum Occidentis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Middle Bronze Age social networks in the Carpathian Basin
    Społeczne sieci kontaktów w środkowej epoce brązu na terenie Kotliny Karpackiej
    Autorzy:
    Przybyła, Marcin S.
    Powiązania:
    https://bibliotekanauki.pl/articles/1396853.pdf
    Data publikacji:
    2016
    Wydawca:
    Uniwersytet Jagielloński. Instytut Archeologii
    Tematy:
    Middle Bronze Age
    Carpathian Basin
    network analysis
    pottery style
    Opis:
    The paper discusses the development of pottery traditions in the Carpathian Basin around 1600 BC. Set of data describing decoration of vessels originating from 94 archaeological sites is analysed using tools developed by so called network science. Results of this investigation are confronted with the current discussion concerning the cultural change at the transition of Middle and Late Bronze Age. In the last part of the paper I try to draw more general conclusions as regard the nature of social networks in prehistory.
    Celem artykułu jest przeanalizowanie stopnia podobieństwa tradycji ceramicznych rozwijających się w Kotlinie Karpackiej mniej więcej pomiędzy XVIII i XII stuleciem p.n.e. W tym celu wyselekcjonowane zostały 94 stanowiska, które dostarczyły wystarczająco licznej serii dekorowanej ceramiki. Pochodzący z nich materiał został poddany klasyfikacji, a następnie przeanalizowany z użyciem narzędzi statystycznych, w tym zwłaszcza techniki analizy sieci. W rezultacie możliwe było określenie stopnia pokrewieństwa pomiędzy poszczególnymi stanowiskami, wyróżnienie grup o zbliżonych „recepturach” dekoracji ceramiki oraz zbadanie zależności pomiędzy podobieństwem stylistycznym i bliskością geograficzną. Analiza ta dostarczyła jednocześnie obserwacji wspierających pogląd o chronologicznym zazębianiu się tradycji kultur tellowych oraz licznej grupy zjawisk kulturowych pojawiających się w Kotlinie Karpackiej po XVII–XVI stuleciu p.n.e., które tutaj łącznie określane są jako tradycja mogiłowa. Ostatnia część artykułu poświęcona jest ogólniejszej dyskusji nad charakterem społecznych sieci kontaktów w prehistorii. Miedzy innymi konfrontuję w niej obraz sieci manifestujący się w stylu ceramicznym z kontaktami wyznaczanymi przez reguły deponowania przedmiotów brązowych i wzorce w zakresie architektury.
    Źródło:
    Recherches Archéologiques Nouvelle Serie; 2016, 8; 47-84
    0137-3285
    Pojawia się w:
    Recherches Archéologiques Nouvelle Serie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rhinoceros exploitation at Érd (Hungary). What a place for the megaherbivores in the Neanderthal diet in Hungary?
    Autorzy:
    Daschek, Éva J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2035494.pdf
    Data publikacji:
    2021
    Wydawca:
    Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
    Tematy:
    Middle Palaeolithic
    Rhinocerotidae
    Proboscidea
    rhinoceros exploitation
    mammoth exploitation
    Carpathian Basin
    Opis:
    The Hungarian Transdanubian site of Érd, where a Mousterian industry and abundant osteological material were discovered in the early 1960s is well known to prehistorians. The remains of megaherbivores (Mammuthus primigenius, Coelodonta antiquitatis) are re-examined here under the taphonomic and archaeozoological components in order to complete the Hungarian and European s.l. data and reassess the potential exploitation of these two pachyderms in the Neanderthal diet and economy. The cut marks, the intense activity of carnivores/hyenas and the skeletal profiles indicate a mixed origin of the carcasses. Mortality patterns of rhinoceros are characterized by the presence of young, subadult and adults, and suggest multiple acquisition by active scavenging and/or hunting with quick access. Skeletal profiles suggest a selective transport of rich/nutritive elements by humans to the site. The cut marks and fracturing of some elements (in situ butchery treatment) confirm that Neanderthals consumed these species on site and that they had at least partial primary access. The mode of acquisition seems active with rapid access for a young mammoth. Érd confirms the Neanderthal exploitation of rhinos and mammoths in their steppic environment during the Middle Palaeolithic. Érd is currently the only Hungarian Middle Palaeolithic site with a proven exploitation and consumption of these megaherbivores.
    Źródło:
    Acta Archaeologica Carpathica; 2021, 56; 13-66
    0001-5229
    2719-4841
    Pojawia się w:
    Acta Archaeologica Carpathica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    A lost carbonate platform deciphered from clasts embedded in flysch: Štramberk-type limestones, Polish Outer Carpathians
    Autorzy:
    Hoffmann, Mariusz
    Kołodziej, Bogusław
    Kowal-Kasprzyk, Justyna
    Powiązania:
    https://bibliotekanauki.pl/articles/1835996.pdf
    Data publikacji:
    2021
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    reefs
    facies
    Štramberk Limestone
    Silesian Ridge
    Jurassic
    Cretaceous
    Carpathian Basin
    Polska
    Opis:
    Limestones designated the Štramberk-type are the most common carbonate exotic clasts (exotics) embedded in the uppermost Jurassic–Miocene flysch deposits of the Polish Outer Carpathians. About 80% of stratigraphically determinable carbonate exotics from the Silesian, Sub-Silesian and Skole units (nappes) are of Tithonian (mostly)–Berriasian (sporadically Valanginian) age. A study of these exotics revealed eight main facies types: coral-microbial boundstones (FT 1), microencruster-microbial-cement boundstones (FT 2), microbial and microbial-sponge boundstones (FT 3), detrital limestones (FT 4), foraminiferal-algal limestones (FT 5), peloidalbioclastic limestones (FT 6), ooid grainstones (FT 7), and mudstones-wackestones with calpionellids (FT 8). Štramberk-type limestones in Poland and the better known Štramberk Limestone in the Czech Republic are remnants of lost carbonate platforms, collectively designated the Štramberk Carbonate Platform. Narrow platforms were developed on intra-basinal, structural highs (some of them are generalized as the Silesian Ridge), with their morphology determined by Late Jurassic synsedimentary tectonics. An attempt was made to reconstruct the facies distribution on the Tithonian–earliest Cretaceous carbonate platform. In the inner platform, coral-microbial patch-reefs (FT 1) grew, while the upper slope of the platform was the depositional setting for the microencruster-microbial-cement boundstones (FT 2). Microbial and microbial-sponge boundstones (FT 3), analogous to the Oxfordian–Kimmeridgian boundstones of the northern Tethyan shelf (also present among exotics), were developed in a deeper setting. In the inner, open part of the platform, foraminiferal-algal limestones (FT 5) and peloidal-bioclastic limestones (FT 6) were deposited. Poorly sorted, detrital limestones (FT 4), including clastsupported breccias, were formed mainly in a peri-reefal environment and on the margin of the platform, in a high-energy setting. Ooid grainstones (FT 7), rarely represented in the exotics, were formed on the platform margin. Mudstones-wackestones with calpionellids (FT 8) were deposited in a deeper part of the platform slope and/or in a basinal setting. In tectonic grabens, between ridges with attached carbonate platforms, sedimentation of the pelagic (analogous to FT 8) and allodapic (“pre-flysch”) Cieszyn Limestone Formation took place. The most common facies are FT 4 and FT 1. Sedimentation on the Štramberk Carbonate Platform terminated in the earliest Cretaceous, when the platform was destroyed and drowned. It is recorded in a few exotics as thin, neptunian dykes (and large dykes in the Štramberk Limestone), filled with dark, deep-water limestones. Reefal facies of the Štramberk Carbonate Platform share similarities in several respects (e.g., the presence of the microencrustermicrobial-cement boundstones) with reefs of other intra-Tethyan carbonate platforms, but clearly differ from palaeogeographically close reefs and coral-bearing facies of the epicontinental Tethyan shelf (e.g., coeval limestones from the subsurface of the Carpathian Foredeep and the Lublin Upland in Poland; the Ernstbrunn Limestone in Austria and Czech Republic). Corals in the Štramberk Limestone and Štramberk-type limestones are the world’s most diverse coral assemblages of the Jurassic–Cretaceous transition. The intra-basinal ridge (ridges), traditionally called the Silesian Cordillera, which evolved through time from an emerged part of the Upper Silesian Massif to an accretionary prism, formed the most important provenance area for carbonate exotic clasts in the flysch of the Silesian Series. They are especially common in the Lower Cretaceous Hradiště Formation and the Upper Cretaceous–Paleocene Istebna Formation. The Baška-Inwałd 204 M. HOFFMANN Et Al. In the Polish Outer Carpathians, shallow-water carbonate sedimentation is recorded only by carbonate clasts, redeposited bioclasts, and very rare, small, unrooted, poorly exposed klippen. Clasts of limestones are exotic to the dominant siliciclastic, uppermost Jurassic–Miocene flysch deposits. They were derived from extrabasinal and intra-basinal source areas of the Carpathian rocks, which periodically emerged and were destroyed. Such rocks were described as “exotic” since the 19th century (“exotischen Graniten”, “exotische Blöcke”; Morlot, 1847; Hohenegger, 1861). In the general geological literature, the term “exotic clasts” is usually used (Flügel, 2010, p. 172), whereas in the Polish geological literature, the term “exotics” (Polish “egzotyki” including also carbonate exotics), is also commonly applied. On the basis of fossils, facies and microfacies, these clasts (pebbles, rarely blocks) are mostly described as Devonian–Carboniferous (Malik, 1978, 1979; Burtan et al., 1983; Tomaś et al., 2004) and Upper Jurassic–lowermost Cretaceous (the present paper and references therein), more rarely Middle Jurassic (Książkiewicz, 1935, 1956a; Barczyk, 1998; Olszewska and Wieczorek, 2001), Early Cretaceous (Oszczypko et al., 1992, 2006, 2020; Krobicki et al., 2005), Late Cretaceous (Książkiewicz, 1956a; Gasiński, 1998) and Palaeogene in age (Leszczyński, 1978; Rajchel and Myszkowska, 1998; Leszczyński et al., 2012; Minor-Wróblewska, 2017). At the beginning of these studies, the focus was on small, unrooted klippen, namely the Andrychów Klippen (called also Klippes) near Wadowice (Zeuschner, 1849; Hohenegger, 1861; Uhlig, 1904; Książkiewicz, 1935, 1971b; Nowak, 1976; Gasiński, 1998; Olszewska and Wieczorek, 2001), and in Kruhel Wielki, near Przemyśl (Niedźwiedzki, 1876; Wójcik, 1907, 1913, 1914; Bukowy and Geroch, 1956; Morycowa, 1988; Olszewska et al., 2009), now poorly exposed. Subsequently, exotic pebbles, much more common and providing data on more facies, were studied more frequently. The first attempt to describe exotics, including crystalline rocks, was presented by Nowak (1927). Jurassic–Cretaceous carbonate exotics at Bachowice, containing facies unknown at other localities in the Polish Outer Carpathians, were described by Książkiewicz (1956a). The preliminary results of studies, which encompassed the entire spectrum of carbonate exotics from the western part of the Polish Outer Carpathians, were presented by Burtan et al. (1984). Malik (1978, 1979) described both Palaeozoic and Mesozoic carbonate clasts in the Hradiště Sandstone of the Silesian Unit, but other studies were mostly concerned with the Štramberk-type limestones from selected outcrops. The studies of these limestones, if concerned with exotics at many localities, were focused on their fossil content (e.g., Kołodziej, 2003a; Bucur et al., 2005; Ivanova and Kołodziej, 2010; Kowal-Kasprzyk, 2014, 2018) or presented only the preliminary results of facies studies (e.g., Hoffmann and Kołodziej, 2008; Hoffmann et al., 2008). Carbonate platforms, the existence of which was deciphered from detrital carbonate components, are called lost carbonate platforms (e.g., Belka et al., 1996; Flügel, 2010; Kukoč et al., 2012). Clasts and other shallowwater components are, metaphorically, witnesses to lost carbonate factories (the term is taken from Coletti et al., 2015). Analyses of the age and lithology of exotic clasts have been applied in the reconstruction of the provenance areas of the clasts and their palaeogeography and the development of the sedimentary sequences of the Polish Outer Carpathians (e.g., Książkiewicz, 1956b, 1962, 1965; Unrug, 1968; Oszczypko, 1975; Oszczypko et al., 1992, 2006; Hoffmann, 2001; Krobicki, 2004; Słomka et al., 2004; Malata et al., 2006; Poprawa and Malata, 2006; Poprawa et al., 2006a, b; Strzeboński et al., 2017; Kowal-Kasprzyk et al., 2020). Štramberk-type limestones are most common among the exotics. It is a field term that refers to limestones, mostly beige in colour, that are supposed to be the age and facies equivalents of the Tithonian–lower Berriasian Štramberk Limestone in Moravia (Czech Republic; Eliáš and Eliášová, 1984; Picha et al., 2006). The Štramberk Limestone and the Štramberk-type limestones of both countries were deposited on platforms, attached to the intrabasinal ridges and margins of the basin of the Outer Carpathians. These platforms are collectively termed the Štramberk Carbonate Platform. The terms “Štramberk Limestone” and “Štramberk-type limestones” have been widely used in the area of the former Austro-Hungarian Empire for the field description of shallow-water limestones of assumed Late Jurassic age, usually occurring within flysch deposits of the Outer Carpathians. Upper Jurassic–lowermost Cretaceous shallow-water limestones in Romania (commonly forming mountains or ridges, e.g., Pleş et al., 2013, 2016), in Bulgaria and Serbia (Tchoumatchenco et al., 2006), and Ukraine (Krajewski and Schlagintweit, 2018), and in Turkey (Masse et al., 2015) sometimes are referred to as the Štramberk-type limestones as well. In the Austrian-German literature similar limestones in the Alps are known as the Plassen Limestone (e.g., Steiger and Wurm, 1980; Schlagintweit et al., 2005). Biostratigraphic studies revealed that some carbonate clasts, accounting for several percent of the exotics and commonly Ridge and the Sub-Silesian Ridge were the source areas for clasts from the Silesian and Sub-Silesian units (e.g., in the Hradiště Formation), while the Northern (Marginal) Ridge was the source for clasts from the Skole Unit (e.g., in the Maastrichtian–Paleocene Ropianka Formation).
    Źródło:
    Annales Societatis Geologorum Poloniae; 2021, 91, 3; 203-251
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    New data about chronology of the impact of the Hunyadihalom-Lažňany horizon on Younger Danubian cultures north of the Carpathian Mountains
    Nowe dane na temat chronologii oddziaływania horyzontu Hunyadihalom-Lažňany na młodsze społeczności naddunajskie na północ od Karpat
    Autorzy:
    Wilk, Stanisław
    Powiązania:
    https://bibliotekanauki.pl/articles/442480.pdf
    Data publikacji:
    2016
    Wydawca:
    Uniwersytet Jagielloński. Instytut Archeologii
    Tematy:
    Eneolithic
    chronology
    graves
    Lublin-Volhynian culture
    Hunyadihalom-Lažňany horizon
    Carpathian Basin
    Lesser Poland
    Opis:
    The subject of this article is connections from Carpathian Basin in the Lublin-Volhynian (LV-C) culture – the first Eneolithic culture in Lesser Poland. Comparative analysis of the pottery from the LV-C child grave no 7 in Książnice (Lesser Poland) points towards the Hunyadihalom-Lažňany horizon as the mainstream source of analogies; and, according to the scheme proposed by Sławomir Kadrow and Anna Zakościelna, the LV-C drew on these analogies at the end of phase III or approx. 3700 –3600 BC (Kadrow, Zakościelna 2000). While, the radiocarbon dating (5180±35BP) dates the grave to approx. 4050 –3940 BC, which according to the scheme proposed by Kadrow and Zakościelna would mean that we are dealing with a feature from phase II. Of extreme importance which influenced the interpretation of the grave were the new data related to absolute chronology of the of the Copper Age in the Carpathian Basin. In the light of new radiocarbon chronology of the Hunyadihalom-Lažňany horizon (ca. 4200 –3800 BC, according Raczky, Siklósi 2013; ca. 4000 –3800 BC according Brummack, Diaconescu 2014), the date of grave 7 from Książnice corresponds well to the ceramic inventory with the characteristics of the Hunyadihalom-Lažňany horizon. The presence of the Hunyadihalom-Lažňany influences in Lesser Poland in the late 5th and 4th millennia BC forces us to pose the questions about their role in the spread of “Chalcolithic” attributes north of the Carpathian Mountains. There is clearer support for the thesis that the new cultural trends, which were expressed by the sepulchral ideology borrowed from the area of the Carpathian Basin emphasizing the elitism of burials, drawing clearer distinctions between the sacred and the profane in the spatial sense, and strongly emphasizing sexual dimorphism, could be to a greater extent the result of the influences of the Hunyadihalom-Lažňany horizon, and not just – as has traditionally been accepted – of the Tiszapolgár and Bodrogkeresztúr cultures.
    Przedmiotem niniejszego artykułu są wpływy ugrupowań środkowej epoki miedzi z Kotliny Karpackiej na kulturę lubelsko-wołyńską – pierwszą eneolityczną kulturę w Małopolsce. Analiza porównawcza ceramiki z grobu 7 kultury lubelsko-wołyńskiej z Książnic (Małopolska) wskazuje jako główny nurt analogii horyzont Hunyadihalom-Lažňany, do którego nawiązania wg schematu Sławomira Kadrowa i Anny Zakościelnej, występują w KLW pod koniec fazy III, czyli ok. 3700–3600 BC (Kadrow, Zakościelna 2000). Jednocześnie data radiowęglowa (5180±35BP) dość precyzyjnie umieszcza omawiany zespół na przełomie V i IV tysiąclecia BC, a dokładniej ok. 4050–3940 BC, co wg schematu S. Kadrowa i A. Zakościelnej oznacza, iż mielibyśmy do czynienia z obiektem z fazy II. Niezwykle ważnym czynnikiem, który wpłynął na interpretację omawianego grobu okazały się nowe dane dotyczące chronologii absolutnej epoki miedzi w Kotlinie Karpackiej. W świetle nowej chronologii radiowęglowej horyzontu Hunyadihalom-Lažňany w Kotlinie Karpackiej (ok. 4200 – 3800 BC wg Raczky, Siklósi 2013; ok. 4000 – 3800 BC wg Brummack, Diaconescu 2014), data z grobu 7 z Książnic dobrze współgra z inwentarzem ceramicznym o cechach horyzontu Hunyadihalom-Lažňany. Obecność wpływów Hunyadihalom-Lažňany w Małopolsce na przełomie V i IV tysiąclecia BC zmusza do postawienia pytań o ich znaczenie w rozprzestrzenianiu się atrybutów „epoki miedzi” na północ od Karpat. Coraz wyraźniej rysuje się teza, że nowe trendy kulturowe, których wyrazem była zapożyczona z terenu Kotliny Karpackiej ideologia sepulkralna podkreślająca elitaryzm pochówków, wyodrębniająca sacrum i profanum w sensie przestrzennym, oraz silnie akcentująca dymorfizm płciowy, mogły być w większym stopniu wynikiem oddziaływań horyzontu Hunyadihalom- -Lažňany, a nie tylko, jak tradycyjnie zakładano, kultur Tiszapolgár i Bodrogkeresztúr.
    Źródło:
    Recherches Archéologiques Nouvelle Serie; 2016, 8; 7-27
    0137-3285
    Pojawia się w:
    Recherches Archéologiques Nouvelle Serie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    When did the Little Ice Age end and the Recent Global Warming Startin Hungary? Late Reflections About a Scientific Faith Debate
    Autorzy:
    RÁCZ, Lajos
    Powiązania:
    https://bibliotekanauki.pl/articles/2081254.pdf
    Data publikacji:
    2016
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    historia klimatu
    zmiany klimatyczne
    mała epoka lodowcowa
    basen karpacki
    globalne ocieplenie
    climate history
    climate change
    Little Ice Age
    Recent Global Warming
    Carpathian Basin
    Opis:
    We try to fi nd answer to the question: when did the Little Ice Age end and the Recent Global Warming start in Hungary? Based on the temperature time series of Budapest and data about the freezing of the Danube from the 1810s the cooling of the climate is perceiveable. The cool-cold and rainy climate system showed two centres of gravity during the 19th century, the fi rst in the 1830s and 1840s, the second in the last two decades of the 19th century. Furthermore, despite the rising of the temperature the climate remained mostly cool and wet until the 1940s. According to the global tendencies there is no obvious climate change trend, though the temperature became colder in decades’ average, but the fl uctuations were very hectic, as usual in transition periods. The diminution in the quantity of precipitation already started in the 1940s though, and proved to be stable. The breakthrough of the Recent Global Warming’s climate system became apparent from the 1980s based on the data of Budapest’s time series. That’s when the ’mediterranean climate-scissors’ opened, and the Danube’s basin became warmer and drier. Even if we examine the tendency of the temperature and precipitation changing in the 20th century separately, we can’t get a clear picture. The warming obviously shows from the last decade of the 19th century, but according to the researchers who are sceptic about Recent Global Warming we can’t use one of the biggest cooling downs in history that occured in the last third of the 19th century as a reference point. The climate regime that was signifi cantly more pluvial than the reference period lasted till the 1940s, and there are no signs of the climate becoming signifi cantly drier prior to the 1980s. If we consider the rise of temperature as the only indicator of the Global Warming, then the warming started in the last decades of the 19th century in Hungary as well. If we consider the decrease in the amount of precipitation to be decisive, then this process started in the 1940s, although there was no signifi cant drying tendency before the 1970s.
    Źródło:
    Historyka studia metodologiczne; 2016, 46; 197-208
    0073-277X
    Pojawia się w:
    Historyka studia metodologiczne
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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