| DC Field | Value | Language |
|---|
| dc.contributor.author | Chendev, Yu. G. | - |
| dc.contributor.author | Fedyunin, I. V. | - |
| dc.contributor.author | Inshakov, A. A. | - |
| dc.contributor.author | Dudin, D. I. | - |
| dc.contributor.author | Belevantsev, V. G. | - |
| dc.date.accessioned | 2021-11-23T12:05:00Z | - |
| dc.date.available | 2021-11-23T12:05:00Z | - |
| dc.date.issued | 2021 | - |
| dc.identifier.citation | Contrasting variants of soil development at archaeological sites on floodplains in the forest-steppe of the Central Russian Upland / Chendev Yu.G. [et al.] // Eurasian Soil Science. - 2021. - Vol.54, №4.-P. 461-477. - Doi: 10.1134/S1064229321040050. | ru |
| dc.identifier.uri | http://dspace.bsu.edu.ru/handle/123456789/44315 | - |
| dc.description.abstract | The soils of archaeological sites on river floodplains with contrasting history of the Holocene soil evolution in the south and north of the forest-steppe zone on the Central Russian Upland have been studied. The conditions for the meadow-chernozemic soil development on the high floodplain in the lower course of the Savala River (Voronezh oblast) were most favorable in the Early Holocene (10.3-9 ka BP); 9 ka BP, the soil humus profile was two times deeper than it is today | ru |
| dc.language.iso | en | ru |
| dc.subject | agriculture | ru |
| dc.subject | pedology | ru |
| dc.subject | Central Russian Upland | ru |
| dc.subject | river floodplains | ru |
| dc.subject | archaeological sites | ru |
| dc.subject | synlithogenic soils | ru |
| dc.subject | paleosols | ru |
| dc.subject | evolution of soils | ru |
| dc.subject | chernozems | ru |
| dc.subject | phaeozems | ru |
| dc.title | Contrasting variants of soil development at archaeological sites on floodplains in the forest-steppe of the Central Russian Upland | ru |
| dc.type | Article | ru |
| Appears in Collections: | Статьи из периодических изданий и сборников (на иностранных языках) = Articles from periodicals and collections (in foreign languages)
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