新石器时代、铜器时代和青铜器时代的林地组成和在大匈牙利平原、东欧和中欧的开发

Gabriella Darabos , Máté Róbert Merkl , Pál Raczky , András Füzesi , Attila Gyucha , Danielle J. Riebe , William A. Parkinson , Magdalena Moskal-del-Hoyo , Szilvia Fábián , Karola Molnár , Gabriella Hajdrik , Tamás Hajdu , Anett Gémes , Gábor Csüllög , Edit Mester , János Dani , Vajk Szeverényi , Viktória Kiss , Přemysl Bobek , Dénes Saláta , Enikő Katalin Magyari
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摘要

在大匈牙利平原(GHP)的史前群落中,森林草原和洪泛平原林地的开发始于公元前约6000 cal 。迄今为止,在全新世考古遗址上只进行了零散和不规则的木炭分析,因此GHP林地的物种组成主要来自花粉记录。本研究旨在通过对新石器时代早期、中期和晚期以及铜器和青铜时代中期考古遗址的系统采样和分析来填补这一空白。一些考古遗址附近的花粉记录伴随着木炭组合以及潜在的植被和土壤图。结果表明,河漫滩和森林草原主要以橡树为主,主要用作建筑木材和薪柴。高、低漫滩森林木本成分(杨木、柳、黄曲柳)均有代表。榆树种(榆木种)分布广泛,经常共同支配木炭组合。在新石器时代晚期东南GHP的长期木炭组合中,榆木比东北GHP更常见。土壤和潜在植被图显示草甸土为主,黑钙土草甸土偶有。在潜在的植被中,洪泛平原林地占主导地位,今天可能存在欧莱维斯和欧莱维斯,这证实了新石器时代匈牙利东南部的冲积森林占主导地位,可能具有高幅度的地下水位波动。在早期铜石器时代(4500-4000 cal BC),我们发现东南GHP中的榆树在花粉和木炭组合中都有明显的下降,这表明气候变化和/或病原体导致了榆树的下降。与巴尔干地区相比,我们证明了GHP的东南边界是一个主要的环境屏障,其北部是广阔的河岸和冲积林与草原橡树林交替存在。新石器时代早期的社区必须适应这种环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Neolithic, Copper, and Bronze Age woodland composition and exploitation in the Great Hungarian Plain, East‐Central Europe
In the prehistoric communities of the Great Hungarian Plain (GHP), the exploitation of forest steppe and floodplain woodlands started at ∼6000 cal BC. So far, only scattered and irregular wood charcoal analyses have been performed on Holocene archaeological sites, therefore the species composition of the GHP woodlands is known mainly from pollen records. This study aims to fill this gap by systematic sampling and analysis of key Early, Middle and Late Neolithic, and Copper and Middle Bronze Age archaeological sites. Pollen records from the vicinity of some archaeological sites accompany the charcoal assemblages along with potential vegetation and soil maps. Our results show that oak (Quercus sp.) was dominant in the floodplain and forest steppe, used as construction timber and firewood. Both high and low floodplain forest woody elements (Populus, Salix, Fraxinus) were represented. Elm species (Ulmus spp.) were widespread and often co-dominated the charcoal assemblages. In the long-term charcoal assemblages of the Late Neolithic SE GHP, Ulmus was more frequent than in the NE GHP. Soil and potential vegetation maps of these sites show meadow soil predominance with occasional chernozem meadow soils. Floodplain woodlands predominate in the potential vegetation with the likely presence of U. laevis and U. minor today corroborating the predominance of alluvial forests in SE Hungary during the Neolithic likely with high amplitude water table fluctuation. During the Early Chalcolithic (4500–4000 cal BC), we found a significant decline in Ulmus in the SE GHP both in the pollen and charcoal assemblages suggesting a climate change and/or pathogen induced elm-decline. In comparison with the Balkan region, we demonstrated that the SE border of the GHP was a major environmental barrier, north of which vast riparian and alluvial forests were alternating with steppe oak woods. The Early Neolithic communities had to adapt to this environment.
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