scholarly journals Neolithic and Copper Age settlement dynamics in the Western Carpathian Basin and Eastern Alps

2019 ◽  
Vol 46 ◽  
pp. 268-282
Author(s):  
Dimitrij Mlekuž Vrhovnik

The paper tackles the spatio-temporal patterns of Neolithic and Copper Age settlement dynamics in the Western Carpathian Basin and Eastern Alps with spatially explicit use of radiocarbon dates. It focuses on the spatial process of spread, movement, aggregation and segregation in the time frame between 8500 and 5000 cal BP. The distribution of Neolithic and Copper Age sites in the study area is clustered and patchy. The first Neolithic settlements appear as isolated islands or enclaves which then slowly expand to fill neighbouring regions. After 6300 cal BP the study area experienced a significant reduction in the extent of settlement systems, associated with the Late Neolithic to Copper Age transition.  

2019 ◽  
Vol 46 ◽  
pp. 268-282
Author(s):  
Dimitrij Mlekuž Vrhovnik

The paper tackles the spatio-temporal patterns of Neolithic and Copper Age settlement dynamics in the Western Carpathian Basin and Eastern Alps with spatially explicit use of radiocarbon dates. It focuses on the spatial process of spread, movement, aggregation and segregation in the time frame between 8500 and 5000 cal BP. The distribution of Neolithic and Copper Age sites in the study area is clustered and patchy. The first Neolithic settlements appear as isolated islands or enclaves which then slowly expand to fill neighbouring regions. After 6300 cal BP the study area experienced a significant reduction in the extent of settlement systems, associated with the Late Neolithic to Copper Age transition.  


2014 ◽  
Vol 89 (1) ◽  
Author(s):  
Dragoş Diaconescu

Methoden derLes nouvelles méthodes de datation et d’analyse des correspondances et AMS nous permettent de préciser et d’améliorer les schémas de chronologie relative dont nous disposons. Ainsi, pour la culture de Lengyel, (également connue sous le nom de Groupe morave-autrichien oriental), des schémas de chronologie absolue sont disponibles, mais la situation du Bassin des Carpates est actuellement différente: il n’existe pratiquement aucune date publiée pour la culture de Lengyel dans cette région. Un nouveau modèle chronologique pour la culture de Lengyel est proposé ici, sur la base d’une étude de la céramique retrouvée dans les ensembles funéraires qui fait usage de la méthode de l’analyse des correspondances et des approches Bayésiennes. Il en résulte que certains synchronismes (tels Lengyel I and II = Néolithique final = cultures de Tisza-Herpály: Lengyel III = Chalcolithique ancien = culture de Tiszapolgár) ne semblent plus valables.The AMS data and correspondence analysis methodology could correct and improve the relative chronology picture. For Lengyel culture (also named Moravian-Eastern-Austrian group) absolute chronological models have already been proposed. In Carpathian Basin the situation is quite different for the moment. Almost no absolute data are published for Lengyel culture in this area. A new chronological model for Lengyel culture is proposed based on the morphological aspects of the pottery inventory from funerary contexts and using correspondence analysis cross-checked by Bayesian approaches. The most interesting fact is that relative chronology synchronisms such as Lengyel I and II = Late Neolithic = Tisza-Herpály cultures and Lengyel III = Early Copper Age = Tiszapolgár culture do not seem to be valid anymoreModelarea datelor AMS şi utilizarea analizei de corespondenţă, ca şi metode de lucru, pot îmbunătăţi şi corecta tabloul cronologiei relative. Pentru cultura Lengyel (numită şi Grupul Morav – est-austriac) au fost deja propuse modele cronologice absolute. În Bazinul Carpatic situaţia este la acest moment un pic diferită. Extrem de puţine date radiocarbon pentru cultura Lengyel sunt publicate pentru acest areal. Un nou model cronologic al culturii Lengyel este propus aici, bazat pe analiza aspectelor morfologice ale inventarului ceramic provenit din contexte funerare. Analiza de corespondenţă, dublată de abordări Bayesiene ale datelor 14C, au fost folosite ca şi metode de lucru. Cel mai interesant aspect al rezultatelor obţinute este faptul că sincronisme ale cronologiei relative de tip Lengyel I–II = Neolitic Târziu = culturile Tisza-Herpály şi Lengyel III = Epoca Timpurie a Cuprului = cultura Tiszapolgár par a nu mai fi valabile.


2019 ◽  
Vol 8 (2) ◽  
pp. 186-199
Author(s):  
Viktor Vladimirovich Morozov

The paper deals with the analysis of the Novoilyinskaya culture sites existed in the Lower Kama region between the Kama Neolithic culture collapse and the Copper Age cultures with porous (shell tempered) ceramics appearance. The analysis of the ceramic complex of the Novoilyinskaya culture shows its similarity with the comb ornamented pottery of the Kama Neolithic culture according to a number of indicators. A lack of clear data on stratigraphy and spatial distribution of finds as well as a small series of absolute dates do not give a clear idea of the formation time and the development of the Novoilyinskaya culture. Currently available data show that the Samara collar (Ivanovskaya) traditions disappeared until the last quarter of the 5th Millennium cal BC. Specific ceramics of the Neolithic-type shape is formed in the Lower Kama region. At the same time the Novoilyinskaya culture ceramics of the Ik and Belaya Rivers interfluve has some features which are the reminiscences of the Levshinskaya stage which are not characteristic for the Middle and Upper Kama region. These features are: thickening on the inner side of the rim; rows of pits and bulges (formed by pits imprinted from the inner side) under the rim; closed forms of the pots and an ornamentation - stepping comb impressions. The proximity of the ceramic complexes of the Novoilyinskaya culture sites to the Late Neolithic ceramics of the Kama culture as well as the radiocarbon dates and the absence of the metalworking evidences prove the functioning of the Novoilyinskaya culture sites of the Lower Kama region during the border of the Stone Age and the period of Early Metals. Another important question is - which southern components took part in the formation of the Novoilyinskaya type or influenced it. Researchers of the forest-steppe Copper Age cultures supposed that in the process of forest Copper Age cultures formation - the Garin and Bor cultures as well as the Middle Volga variant of the Volosovo culture - the Tok and even Altata elements took part. In our opinion, the influence of the Tok traditions is already clearly visible on the Novoilyinskaya culture ceramics. This conclusion is supported by the ⁴C dates which established the synchronicity of the Tok and Novoilyinskaya sites.


2021 ◽  
Vol 10 (3) ◽  
pp. 12-21
Author(s):  
Zsuzsa Hegedűs

In the Late Neolithic and Copper Age of the Carpathian Basin, we can find several examples of burials without bodies – symbolic burials. One of the main goals of their creation may have been to give a focal point to funerary rites in cases when a member of the community could not have been laid to rest properly. Thus, we can assume they played a key role in coping with bereavement and trauma. In some cases, the analysis of the finds of symbolic burials provides an opportunity to reconstruct the identities associated with them to a certain degree.


2016 ◽  
Vol 33 (1) ◽  
pp. 11-26
Author(s):  
Katarina Botić

Abstract Southern outskirts of Carpathian basin, namely the region between Sava, Drava and Danube rivers, have specific climate conditions today partially influenced by geological structure and geographical position. In this region Neolithic Starčevo and Sopot cultures are observed. Radiocarbon dates for Neolithic cultures are used to build a time frame which is compared with climate proxies, especially with Holocene rapid climate events (8.2, 5.9 and 4.2 ka), to draw a conclusion on when and how these cultures developed in southern regions of Carpathian basin. Lacking firm geoarchaeological data the results are not conclusive but can provide some insight on how the climate may have directly and indirectly influenced development of Neolithic and beginning of Eneolithic period in the region.


Radiocarbon ◽  
2009 ◽  
Vol 51 (3) ◽  
pp. 1071-1109 ◽  
Author(s):  
Richard W Yerkes ◽  
Attila Gyucha ◽  
William Parkinson

This article presents the results of a multiscalar analysis of 168 radiocarbon dates from Neolithic and Copper Age sites on the Great Hungarian Plain. We examined chronological patterns at different geographic scales to explore socioeconomic changes that occurred during the transition from the Neolithic to the Copper Age. The beginning and end of the Late Neolithic (5000–4500 cal BC) and Early Copper Age (4500–4000 cal BC) were modeled with 14C dates calibrated with the CALIB 5.01 program and IntCal04 calibration curve. Our attempts to identify chronological subphases within these 500-yr-long periods were confounded by multiple intercepts in the calibration curve. The analysis indicated that terminal Late Neolithic (4700–4300 cal BC) and “transitional” Proto-Tiszapolgár occupations (4600–4250 cal BC) at tell sites were contemporary with initial Early Copper Age habitations (4450–4250 cal BC). Calibrated dates from small Early Copper Age settlements at Vészto-Bikeri and Körösladány-Bikeri document changes in community and household organization that took place over several decades during the transition to the Copper Age. Bayesian analysis indicated that the small fortified sites were occupied contiguously in phases of 30–50 yr. The younger Körösladány-Bikeri site was established before the older Vészto-Bikeri site was abandoned. When large nucleated Late Neolithic communities dispersed and established small Early Copper Age settlements, the pattern of vertical accretion that had created the Late Neolithic tells gave way to a pattern of horizontal settlement accretion at the smaller settlements.


Radiocarbon ◽  
1992 ◽  
Vol 34 (3) ◽  
pp. 859-866 ◽  
Author(s):  
Ede Hertelendi ◽  
Ferenc Horváth

We investigated chronological questions of five Late Neolithic settlements in the Hungarian Tisza-Maros region. Fifty new radiocarbon dates provide an internal chronology for the developmental phases of the tell settlements, and place them into the wider framework of the southeastern European Neolithic. An example is presented of how a unique type of stratigraphic excavation helps the interpretation of radiocarbon data, which are in contradiction with the stratigraphic position of the samples.


Author(s):  
Ana Catarina Sousa ◽  
Victor S. Gonçalves ◽  
André Texugo ◽  
Ana Ramos-Pereira

This article is the result of archaeological and paleoenvironmental investigations carried out within the scope of the ANSOR project in the Sorraia valley (Coruche), on the left bank of the Lower Tagus. In the analysis of settlement dynamics between 5500 and 1800 a.n.e. we considered four moments: 1) The first peasant societies of the ancient Neolithic; 2) The Middle and Late Neolithic; 3) Chalcolithic; 4) The Early Bronze Age. The Sorraia valley was also framed in the framework of the Center and South of Portugal during the period under analysis. Interpretative models are presented for changes in the implantation patterns in the four stages under study, oscillating between paleoenvironmental factors and the socio-economic changes registered in the old peasant societies. 


1972 ◽  
Vol 38 ◽  
pp. 389-407 ◽  
Author(s):  
R. Burleigh ◽  
I. H. Longworth ◽  
G. J. Wainwright

SummaryIf the fine structure of the carbon-14 deviation curve published by Professor H. E. Suess (in Proceedings of the 12th Nobel Symposium, I. U. Olsson (ed.), 1970) is correct, then the period from c. 2200 bc to c. 1700 bc in radiocarbon years falls within one of the insensitive regions in which carbon-14 determinations could have a number of alternative chronological values and hence could not be used to order archaeological evidence. Without disputing the now well established general trend of radiocarbon variation, it is the purpose of this paper to suggest, from recurrent evidence drawn from four recently studied Late Neolithic enclosures, that the detailed structure of Suess' curve is not necessarily valid. Uncalibrated radiocarbon dates based on the conventional 5570 year half-life of carbon-14 are used throughout this paper.


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