F. Djindjian (ed.), Les Sociétés Humaines Face Aux Changements Climatiques, Volume 2: La Protohistoire, Des Débuts De L’holocène Au Début Des Temps Historiques: 89-124. Oxford: Archaeopress., 2022
Neolithization processes have frequently been investigated from the environmental perspective. Ho... more Neolithization processes have frequently been investigated from the environmental perspective. However, there are many ambiguities inherent in palaeoenvironmental data, especially when confronted with archaeological ones. There are also very different visions as to the role of environmental factors in development of human societies. In the contribution the most urgent problems induced by the application of an environmental approach to explain prehistoric processes, including those of neolithization, were characterised. Then, the potential role of environmental (particularly climatic) proxies in the modelling the appearance and spread of the First Neolithic in SouthEast Europe was demonstrated. In particular, the issue of the extent to which the Neolithic diffusions and possible adaptations were triggered or slowed down by Holocene global climate events was analysed. It was hypothesised, as one of possible scenarios, that the speed of neolithization of SouthEast Europe was not uniform and regular. In a measure, in some areas, this was due to the necessity to adapt to 'new' environmental conditions. However, first and foremost, these processes were evoked by the occurrence of favourable conditions ('occasions') created by global and local environmental transformations ('opportunistic colonisation').
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Papers by Marek Nowak
c. 3750/3700 BC and existed until c. 2800 BC. “Funnel Beaker” acculturation of the late Lengyel-Polgár populations could play a large part in the origins of the local branch of this culture. For many years, the TRB seemed to be scarcely represented. This notion has changed since early 1970s onwards, due to more and more intensive investigations. Currently, western Lesser Poland is perceived as an equally important region of the TRB development as other the most important ones both in Lowland and Upland zones. The local TRB communities were characterised by varied patterns of settlement and economic behaviours. These patterns were correlated withecological differences.
c. 3750/3700 BC and existed until c. 2800 BC. “Funnel Beaker” acculturation of the late Lengyel-Polgár populations could play a large part in the origins of the local branch of this culture. For many years, the TRB seemed to be scarcely represented. This notion has changed since early 1970s onwards, due to more and more intensive investigations. Currently, western Lesser Poland is perceived as an equally important region of the TRB development as other the most important ones both in Lowland and Upland zones. The local TRB communities were characterised by varied patterns of settlement and economic behaviours. These patterns were correlated withecological differences.