Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence
Authors interpret the data on the soil and sedimentary strata of the Central Russian Up-land (key sites Alexandrovsky and Yamskaya steppe, Belogorie reserve). We used the soil morphology data to reconstruct the evolutionary changes of the environment during the late Pleistocene and Holocene. The sed...
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Theoretical and Applied Ecology
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ftdatacite:10.25750/1995-4301-2017-2-019-023 2023-05-15T18:30:54+02:00 Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence А. S. Kerzhentsev V. Е. Ostroumov 2017 https://dx.doi.org/10.25750/1995-4301-2017-2-019-023 http://envjournal.ru/ari/v2017/v2/17203.pdf ru rus Theoretical and Applied Ecology soil-sedimentary sequence soil formation sedimentation rate chernozem soil cryogenesis soil age soil residuals late Pleistocene Holocene dataset Dataset 2017 ftdatacite https://doi.org/10.25750/1995-4301-2017-2-019-023 2021-11-05T12:55:41Z Authors interpret the data on the soil and sedimentary strata of the Central Russian Up-land (key sites Alexandrovsky and Yamskaya steppe, Belogorie reserve). We used the soil morphology data to reconstruct the evolutionary changes of the environment during the late Pleistocene and Holocene. The sedimentation rate was calculated using a linear approximation of the radiocarbon data. Typical values of the sedimentation rate are of the order of 0.1 mm/year. It was shown that the main source of sediment and sediment layer growth are residual products of soil formation formed in the process of tree waste, forest litter, and humus transforming into clay cutans, ferromanganese nodules and calcareous murrams, original and secondary minerals which turn into sedimentary rocks. During Holocene (10000 years) 420 sm sediment accumulated, their layers changed with the change of natural zones in course of decreasing impact of retreating glacier: tundra, taiga, coniferous broadleaved forest, forest steppe, steppe. Stable climatic optimum with real steppes and typical chernozem established on the territory 5500 years ago. Within this period of time 220 sm layer of loess loam got accumulated there. The residuals appear inside the soil profile during transformation of litter, soil-forming rocks, and mineral eolian sediment. The estimated sedimentation rate can be used to describe the mechanisms of formation of soil-sedimentary sequences Dataset taiga Tundra DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
Russian |
topic |
soil-sedimentary sequence soil formation sedimentation rate chernozem soil cryogenesis soil age soil residuals late Pleistocene Holocene |
spellingShingle |
soil-sedimentary sequence soil formation sedimentation rate chernozem soil cryogenesis soil age soil residuals late Pleistocene Holocene А. S. Kerzhentsev V. Е. Ostroumov Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence |
topic_facet |
soil-sedimentary sequence soil formation sedimentation rate chernozem soil cryogenesis soil age soil residuals late Pleistocene Holocene |
description |
Authors interpret the data on the soil and sedimentary strata of the Central Russian Up-land (key sites Alexandrovsky and Yamskaya steppe, Belogorie reserve). We used the soil morphology data to reconstruct the evolutionary changes of the environment during the late Pleistocene and Holocene. The sedimentation rate was calculated using a linear approximation of the radiocarbon data. Typical values of the sedimentation rate are of the order of 0.1 mm/year. It was shown that the main source of sediment and sediment layer growth are residual products of soil formation formed in the process of tree waste, forest litter, and humus transforming into clay cutans, ferromanganese nodules and calcareous murrams, original and secondary minerals which turn into sedimentary rocks. During Holocene (10000 years) 420 sm sediment accumulated, their layers changed with the change of natural zones in course of decreasing impact of retreating glacier: tundra, taiga, coniferous broadleaved forest, forest steppe, steppe. Stable climatic optimum with real steppes and typical chernozem established on the territory 5500 years ago. Within this period of time 220 sm layer of loess loam got accumulated there. The residuals appear inside the soil profile during transformation of litter, soil-forming rocks, and mineral eolian sediment. The estimated sedimentation rate can be used to describe the mechanisms of formation of soil-sedimentary sequences |
format |
Dataset |
author |
А. S. Kerzhentsev V. Е. Ostroumov |
author_facet |
А. S. Kerzhentsev V. Е. Ostroumov |
author_sort |
А. S. Kerzhentsev |
title |
Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence |
title_short |
Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence |
title_full |
Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence |
title_fullStr |
Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence |
title_full_unstemmed |
Estimation of the continental sedimentation rate in the Belgorod soil-sediment sequence |
title_sort |
estimation of the continental sedimentation rate in the belgorod soil-sediment sequence |
publisher |
Theoretical and Applied Ecology |
publishDate |
2017 |
url |
https://dx.doi.org/10.25750/1995-4301-2017-2-019-023 http://envjournal.ru/ari/v2017/v2/17203.pdf |
genre |
taiga Tundra |
genre_facet |
taiga Tundra |
op_doi |
https://doi.org/10.25750/1995-4301-2017-2-019-023 |
_version_ |
1766214515559497728 |