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Postpleniglacial repeopling of the Hungarian Plain

Dobosi V. T.

Folia Quaternaria

1999

nr 70

297-315

The postpleniglacial environment of the Hungarian Plain was mosaic-like. The surface is a mixture of the recent alluvium, loess-covered ancient hills, wind-blown sand dunes, and saline oxbow lakes. The flora-spectrum is characterised by the advance of deciduous trees, the Holocene being marked by the appearance of the Acer tataricum. The mammalian fauna becomes depleted, disharmonic and unbalanced (Bajot and Palank climato-faunistic phases). Two cultural phyla are identified in the second part of LUP: - the younger strata of the Epigravettian (younger blade) sites (Dunakanyar, Jaszsag), - sites of Allerod-oscillation with small artefacts made by the Mesolithic technique, but without Mesolithic types.