Microblade Production in the Sukhotino-4 Industry, Eastern Transbaikalia

We have analyzed microblade production at Sukhotino-4, a stratified site in the southern part of Chita, Eastern Transbaikalia, excavated in the 1970s and 1980s. Its lithic industry specialized in bifacial tools and, to a large extent, in microblades and tools made on them. The sample includes over 300 cores and their preforms intended for manufacturing microblades and found in eleven layers. On the basis of morphological and typological analyses, we reveal an absolute predominance of narrow-faced microcores, including wedge-shaped ones. Most microcores from all layers of Sukhotino-4 were made according to a standard scheme, which concerned all stages, from the choice of blanks to the use of the core. The analysis of metric parameters suggests that most microcores have a frontal height of 25–30 mm and a width of 9–11 mm. The predominance of a single standard in the preparation of blanks and in the utilization of cores allowed us to describe the Sukhotino type of narrow-faced microcores. Other types are represented by just a few specimens. Morphological and typological homogeneity of most microcores and bifacial tools from all layers, correlating with the Sartan glacial cooling, suggests that the Upper Paleolithic industry of Sukhotino-4 existed for a long time.

Authors

Institutions

Publication Details

Journal
Archaeology Ethnology and Anthropology of Eurasia
Published
2025-04-03
DOI
https://doi.org/10.17746/1563-0110.2025.53.1.025-033
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Microblade Production in the Sukhotino-4 Industry, Eastern Transbaikalia

V. I. Tashak, E. V. Kovychev
Archaeology Ethnology and Anthropology of Eurasia
Geology and Paleoclimatology Research
article

Microblade Production in the Sukhotino-4 Industry, Eastern Transbaikalia

V. I. Tashak, E. V. Kovychev
article en

Abstract

We have analyzed microblade production at Sukhotino-4, a stratified site in the southern part of Chita, Eastern Transbaikalia, excavated in the 1970s and 1980s. Its lithic industry specialized in bifacial tools and, to a large extent, in microblades and tools made on them. The sample includes over 300 cores and their preforms intended for manufacturing microblades and found in eleven layers. On the basis of morphological and typological analyses, we reveal an absolute predominance of narrow-faced microcores, including wedge-shaped ones. Most microcores from all layers of Sukhotino-4 were made according to a standard scheme, which concerned all stages, from the choice of blanks to the use of the core. The analysis of metric parameters suggests that most microcores have a frontal height of 25–30 mm and a width of 9–11 mm. The predominance of a single standard in the preparation of blanks and in the utilization of cores allowed us to describe the Sukhotino type of narrow-faced microcores. Other types are represented by just a few specimens. Morphological and typological homogeneity of most microcores and bifacial tools from all layers, correlating with the Sartan glacial cooling, suggests that the Upper Paleolithic industry of Sukhotino-4 existed for a long time.

Archaeology Ethnology and Anthropology of EurasiaVol. 53(1)
Transbaikal State University (RU), Institute of Mongolian Buddhist and Tibetan Studies (RU), Institute of History, Archaeology and Ethnography of the Peoples of Far-East (RU)
Openalex Percentile: Top 88%
Geology and Paleoclimatology Research
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.