Abstract

In the article the materials of the Novhorod-Siverskyi site research both in the 1930's, and relatively recently, are analyzed. First of all, attention is paid to the faunal collection. The faunal associations from old excavations are coherent, typical of a cold steppe environment from the glacial period, near a riparian forest. However, it seems to result to a mix between natural taphonomic complexes and animal remains associated with human activity. Judging by the flint collection from the old excavations, the site was inhabited by representatives of the Pushkari type. New research yielded two archaeological layers that are very poor in flint artefacts. Concerning fauna, the faunal spectrum is restricted in both layers, with the woolly mammoth, the woolly rhinoceros, the horse and the reindeer in the lower and upper layers. In the upper layer there are also the bison, the fox and the hare. According to taphonomic observations, the bones had remained for a long time at an open air before being buried, in subsurface in a wet environment but few submitted to precipitations in link with permafrost activities. Particularly in the lower layer (2) some remains appear to be in place, while others seem to have been imported by hydraulic phenomena, either from the top of the promontory or from the Desna River. In the upper layer (1), some bones show possible anthropogenic impacts of breakage, linked to marrow recovery. In both layers we have some cranial and postcranial elements, mainly from adults sensu lato which could correspond to human predation. They could correspond to temporary camps of quite small human groups, potentially occupied at the end of the cold season/beginning of the warm season.

Highlights

  • The climatically unstable final part of the Pleistocene has caused paleoenvironmental and geog­ raphical changes and forced Palaeolithic hunters-gatherers to adapt (Clark et al 2009, p. 710-714; Lambeck et al 2014, p. 15296-15303)

  • It seems to result to a mix between natural taphonomic complexes and animal remains associated with human activity

  • Judging by the flint collection from the old excavations, the site was inhabited by representatives of the Pushkari type

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Summary

Introduction

The climatically unstable final part of the Pleistocene has caused paleoenvironmental and geog­ raphical changes and forced Palaeolithic hunters-gatherers to adapt (Clark et al 2009, p. 710-714; Lambeck et al 2014, p. 15296-15303). The Upper Pleniglacial started around 26 000 BP, corresponding to the OIS 2. The active development of the territory of the Middle Desna basin in the Upper Palaeolithic is associated with the ancient population, which left behind the sites of the so-called Pushkari type. This specific variant of the Gravettian technocomplex is represented foremost by the sites of Pushkari I, Pohon and Kliusy, which are dated by 23—20 000 BP In addition to them, the earliest evidence of the development of the territory by ancient people includes the complex of Obolonnia site with Epiaurignacian features In addition to them, the earliest evidence of the development of the territory by ancient people includes the complex of Obolonnia site with Epiaurignacian features (Ступак та ін. 2014, c. 9-30; Demay et al 2020, p. 83; 2021, p. 258-289) and probably the complex of the site of Pushkari III, which has specific features

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