Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia

Abstract Contemporary (corresponding to the modern state of ecosystems and land use) and prehistoric (for hypothetic intact natural ecosystems similar to modern virgin ecosystems) stocks of organic carbon were assessed for model regions of southern taiga, forest-steppe and steppe in European Russia....

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Published in:IOP Conference Series: Earth and Environmental Science
Main Authors: Chernova, O V, Ryzhova, I M, Podvezennaya, M A
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2020
Subjects:
Online Access:https://doi.org/10.1088/1755-1315/438/1/012005
https://iopscience.iop.org/article/10.1088/1755-1315/438/1/012005/pdf
https://iopscience.iop.org/article/10.1088/1755-1315/438/1/012005
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author Chernova, O V
Ryzhova, I M
Podvezennaya, M A
author_facet Chernova, O V
Ryzhova, I M
Podvezennaya, M A
author_sort Chernova, O V
collection IOP Publishing
container_issue 1
container_start_page 012005
container_title IOP Conference Series: Earth and Environmental Science
container_volume 438
description Abstract Contemporary (corresponding to the modern state of ecosystems and land use) and prehistoric (for hypothetic intact natural ecosystems similar to modern virgin ecosystems) stocks of organic carbon were assessed for model regions of southern taiga, forest-steppe and steppe in European Russia. The comparison of these stocks enabled an assessment of the integral result of the multidirectional changes in land use that occurred in the studied regions over the historical period. The carbon stocks were determined using a unified cartographic basis, data on taxonomy and texture of soil units, modern land use types and the type and age structure of reconstructed and contemporary vegetation. The results obtained indicate that the modern carbon pool has reduced by 24% compared to the potential prehistoric one in the Kostroma Region and Rostov Region (southern taiga and steppe zones, respectively) and by 37% in the Kursk Region (forest-steppe zone). It was also demonstrated that the contribution of soil to the total organic carbon stock increases southwards, from southern taiga to dry steppe, from 51 to 95% during the prehistoric period and from 62 to 96% currently. The study results show that forestry and agriculture increase the contribution of soil to maintaining the region’s carbon budget.
format Article in Journal/Newspaper
genre taiga
genre_facet taiga
geographic Kostroma
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long_lat ENVELOPE(163.168,163.168,59.040,59.040)
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op_doi https://doi.org/10.1088/1755-1315/438/1/012005
op_rights http://creativecommons.org/licenses/by/3.0/
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op_source IOP Conference Series: Earth and Environmental Science
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spelling crioppubl:10.1088/1755-1315/438/1/012005 2025-03-23T15:45:50+00:00 Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia Chernova, O V Ryzhova, I M Podvezennaya, M A 2020 https://doi.org/10.1088/1755-1315/438/1/012005 https://iopscience.iop.org/article/10.1088/1755-1315/438/1/012005/pdf https://iopscience.iop.org/article/10.1088/1755-1315/438/1/012005 unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 438, issue 1, page 012005 ISSN 1755-1307 1755-1315 journal-article 2020 crioppubl https://doi.org/10.1088/1755-1315/438/1/012005 2025-02-26T08:51:36Z Abstract Contemporary (corresponding to the modern state of ecosystems and land use) and prehistoric (for hypothetic intact natural ecosystems similar to modern virgin ecosystems) stocks of organic carbon were assessed for model regions of southern taiga, forest-steppe and steppe in European Russia. The comparison of these stocks enabled an assessment of the integral result of the multidirectional changes in land use that occurred in the studied regions over the historical period. The carbon stocks were determined using a unified cartographic basis, data on taxonomy and texture of soil units, modern land use types and the type and age structure of reconstructed and contemporary vegetation. The results obtained indicate that the modern carbon pool has reduced by 24% compared to the potential prehistoric one in the Kostroma Region and Rostov Region (southern taiga and steppe zones, respectively) and by 37% in the Kursk Region (forest-steppe zone). It was also demonstrated that the contribution of soil to the total organic carbon stock increases southwards, from southern taiga to dry steppe, from 51 to 95% during the prehistoric period and from 62 to 96% currently. The study results show that forestry and agriculture increase the contribution of soil to maintaining the region’s carbon budget. Article in Journal/Newspaper taiga IOP Publishing Kostroma ENVELOPE(163.168,163.168,59.040,59.040) IOP Conference Series: Earth and Environmental Science 438 1 012005
spellingShingle Chernova, O V
Ryzhova, I M
Podvezennaya, M A
Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia
title Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia
title_full Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia
title_fullStr Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia
title_full_unstemmed Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia
title_short Historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in European Russia
title_sort historical trends in the amount and structure of organic carbon stocks in natural and managed ecosystems in european russia
url https://doi.org/10.1088/1755-1315/438/1/012005
https://iopscience.iop.org/article/10.1088/1755-1315/438/1/012005/pdf
https://iopscience.iop.org/article/10.1088/1755-1315/438/1/012005