Micromorphological Features and Formation Processes of the Cultural Layer in the Early Medieval Town of Dzhankent (Eastern Aral Sea Region, Kazakhstan)

This paper presents the results of a study on the stratigraphy, morphology, micromorphology, chemical, and physicochemical characteristics of the cultural layer in the residential area of the early medieval town of Dzhankent (Eastern Aral Sea region, Kazakhstan). The town is located in an arid paleo-deltaic landscape with a dynamic water supply. Sets of diagnostically significant micromorphological features are described, including: 1) features resulting from anthropogenic input and redistribution of matter (plant detritus, phytoliths, bone fragments, etc.); 2) pedofeatures resulting from the transformation of human-introduced material by anthropogenic processes (pyrogenic forms of carbonates, organic and phosphate-organic pedofeatures); 3) pedofeatures consisting of carbonates, gypsum, and iron oxides, mainly associated with natural processes. Stratigraphic units of the cultural layer, along with the processes and conditions of their formation, were defined, and the archaeological context was interpreted for each lithostratigraphic unit based on their morphological and analytical characteristics. The upper stratigraphic unit consists of the destruction products of adobe materials, with ash interlayers, some of which are stratigraphically traceable and likely correspond to fire events. The middle unit comprises residential and domestic sediments, including a series of living surfaces, and contains an ash layer possibly resulting from a fire event. The lower unit is composed of alluvial-delta deposits slightly impacted by residential activities and periodically affected by fluctuating groundwater. The distribution of organic carbon and phosphorus in the cultural layer corresponds well with the observed organic substrates at the macro-stratigraphic level, being significantly higher in loose layers rich in plant detritus, charcoal, ash, and bone material. However, the analytical characteristics of the cultural layer (pH, electroconductivity, contents of organic carbon, phosphorus, carbonates, gypsum), determined from homogenized samples of the stratigraphic units, do not always align with the composition observed at the micromorphological level (abundance of micro-artifacts, anthropogenic, and soil microfeatures). These discrepancies are primarily due to the extremely high lateral and microstratigraphic heterogeneity of the cultural layer.