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Ponomarenko, E.

Publications and source records attributed to Ponomarenko, E..

2 recordsLinked to original sources

Swidden pollen spectra are unique, having no modern analogues

O_LISlash-and-burn cultivation (SABC), a widespread premodern agricultural practice, shaped vegetation across the temperate zone of Eurasia for millennia, yet the SABC-associated plant communities and their modern analogues remain poorly understood. C_LIO_LIWe compared 74 fossil pollen spectra from radiocarbon-dated swidden horizons with 223 modern surface soil spectra using non-metric multidimensional scaling and cluster analysis. C_LIO_LIThe results show that slash-and-burn cultivation creates a unique palynological assemblage in soil, distinguishable from forests, meadows, fallows, and ruderal habitats. This signature was most pronounced in sites from broad-leaved coniferous forest, where cryptogam diversity was highest. C_LIO_LIHere, we report that pollen spectra from buried swidden soils across the Eastern European forest zone consistently form a distinct and cohesive cluster, lacking modern analogues. These spectra are characterized by high proportions of Betula, Tilia, Epilobium angustifolium, cereal pollen, and a diverse assemblage of spores (Marchantia, Lycopodium, Pteridium), reflecting a mosaic of post-cultivation successional stages. C_LIO_LIInsect activity, particularly pollen-storing burrows of ground-nesting bees, may enhance the swidden signal through selective accumulation of fireweed entomophilous pollen. C_LIO_LIOur results provide SABC reference pollen spectra for temperate mixed and deciduous forest zones and can be used as a tool for reconstructing the extinct suite of plant communities associated with swidden cultivation. C_LI

ecology↗

Pollen indicators of slash-and-burn agriculture in forest soils and peatlands: a case study of Zvenigorod biological station (Moscow region, Russia)

This study aimed to analyze pollen indicators of slash-and-burn agriculture in soils and aquatic deposits of the southern forest zone of Eastern Europe. Pollen spectra from buried swidden soils (500 - 1800 cal BP) were compared with coeval peat layers and modern surface soils. Swidden horizons exhibited highly distinctive pollen spectra, characterized by Betula dominance, low conifer pollen, and the presence of cultivation indicators (Cerealia) and post-fire succession taxa (Chamaenerion, Pteridium, Marchantia). The abundance of insect-pollinated Chamaenerion angustifolium - the most prominent indicator - suggests both its wide distribution in swidden landscapes and a possible link to ground-nesting bee activity, which may aid in identifying buried swiddens. In peat records, the onset of slash-and-burn agriculture was marked by microcharcoal, a decline in late-successional trees, a rise in pioneer taxa, and the appearance of agricultural indicators. Betula dominance in both archives reflects secondary stands typical of long-term swidden use. However, indicators of cultivation and succession were much less pronounced in peat. Our results show that paleosol pollen spectra provide reliable, site-specific evidence of swidden agriculture through local indicator taxa and traces of bee activity, though they tend to overrepresent local vegetation. In contrast, peat and lake records offer broader regional perspectives but detect swidden activity only indirectly. These insights provide a methodological basis for localizing ancient agricultural practices in future archeology and palaeoecology-related studies.

ecology↗