Dynamics of Soil Properties and Plant Composition during Postagrogenic Evolution in Different Bioclimatic Zones

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Dynamics of Soil Properties and Plant Composition during Postagrogenic Evolution in Different Bioclimatic Zones. / Telesnina, V. M.; Kurganova, I. N.; Lopes de Gerenyu, V. O.; Ovsepyan, L. A.; Lichko, V. I.; Ermolaev, A. M.; Mirin, D. M.

In: Eurasian Soil Science, Vol. 50, No. 12, 01.12.2017, p. 1515-1534.

Research output: Contribution to journal › Article › peer-review

Author

Telesnina, V. M. ; Kurganova, I. N. ; Lopes de Gerenyu, V. O. ; Ovsepyan, L. A. ; Lichko, V. I. ; Ermolaev, A. M. ; Mirin, D. M. / Dynamics of Soil Properties and Plant Composition during Postagrogenic Evolution in Different Bioclimatic Zones. In: Eurasian Soil Science. 2017 ; Vol. 50, No. 12. pp. 1515-1534.

BibTeX

@article{30962128b09143f59573491ef9a09b1d,

title = "Dynamics of Soil Properties and Plant Composition during Postagrogenic Evolution in Different Bioclimatic Zones",

abstract = "The postagrogenic dynamics of acidity and some parameters of humus status have been studied in relation to the restoration of zonal vegetation in southern taiga (podzolic and soddy-podzolic soils (Retisols)), coniferous-broadleaved (subtaiga) forest (gray forest soil (Luvic Phaeozem)), and forest-steppe (gray forest soil (Haplic Phaeozem)) subzones. The most significant transformation of the studied properties of soils under changing vegetation has been revealed for poor sandy soils of southern taiga. The degree of changes in the content and stocks of organic carbon, the enrichment of humus in nitrogen, and acidity in the 0- to 20-cm soil layer during the postagrogenic evolution decreases from north to south. The adequate reflection of soil physicochemical properties in changes of plant cover is determined by the climatic zone and the land use pattern. A correlation between the changes in the soil acidity and the portion of acidophilic species in the plant cover is revealed for the southern taiga subzone. A positive relationship is found between the content of organic carbon and the share of species preferring humus-rich soils in the forest-steppe zone.",

keywords = "and forest-steppe zones, biodiversity, carbon pool, coniferous-broadleaved, ecologicalcenotic scales, postagrogenic soils, soil acidity, southern-taiga, vegetation demutation",

author = "Telesnina, {V. M.} and Kurganova, {I. N.} and {Lopes de Gerenyu}, {V. O.} and Ovsepyan, {L. A.} and Lichko, {V. I.} and Ermolaev, {A. M.} and Mirin, {D. M.}",

note = "Publisher Copyright: {\textcopyright} 2017, Pleiades Publishing, Ltd.",

year = "2017",

month = dec,

day = "1",

doi = "10.1134/S1064229317120109",

language = "English",

volume = "50",

pages = "1515--1534",

journal = "Eurasian Soil Science",

issn = "1064-2293",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "12",

}

RIS

TY - JOUR

T1 - Dynamics of Soil Properties and Plant Composition during Postagrogenic Evolution in Different Bioclimatic Zones

AU - Telesnina, V. M.

AU - Kurganova, I. N.

AU - Lopes de Gerenyu, V. O.

AU - Ovsepyan, L. A.

AU - Lichko, V. I.

AU - Ermolaev, A. M.

AU - Mirin, D. M.

PY - 2017/12/1

Y1 - 2017/12/1

N2 - The postagrogenic dynamics of acidity and some parameters of humus status have been studied in relation to the restoration of zonal vegetation in southern taiga (podzolic and soddy-podzolic soils (Retisols)), coniferous-broadleaved (subtaiga) forest (gray forest soil (Luvic Phaeozem)), and forest-steppe (gray forest soil (Haplic Phaeozem)) subzones. The most significant transformation of the studied properties of soils under changing vegetation has been revealed for poor sandy soils of southern taiga. The degree of changes in the content and stocks of organic carbon, the enrichment of humus in nitrogen, and acidity in the 0- to 20-cm soil layer during the postagrogenic evolution decreases from north to south. The adequate reflection of soil physicochemical properties in changes of plant cover is determined by the climatic zone and the land use pattern. A correlation between the changes in the soil acidity and the portion of acidophilic species in the plant cover is revealed for the southern taiga subzone. A positive relationship is found between the content of organic carbon and the share of species preferring humus-rich soils in the forest-steppe zone.

AB - The postagrogenic dynamics of acidity and some parameters of humus status have been studied in relation to the restoration of zonal vegetation in southern taiga (podzolic and soddy-podzolic soils (Retisols)), coniferous-broadleaved (subtaiga) forest (gray forest soil (Luvic Phaeozem)), and forest-steppe (gray forest soil (Haplic Phaeozem)) subzones. The most significant transformation of the studied properties of soils under changing vegetation has been revealed for poor sandy soils of southern taiga. The degree of changes in the content and stocks of organic carbon, the enrichment of humus in nitrogen, and acidity in the 0- to 20-cm soil layer during the postagrogenic evolution decreases from north to south. The adequate reflection of soil physicochemical properties in changes of plant cover is determined by the climatic zone and the land use pattern. A correlation between the changes in the soil acidity and the portion of acidophilic species in the plant cover is revealed for the southern taiga subzone. A positive relationship is found between the content of organic carbon and the share of species preferring humus-rich soils in the forest-steppe zone.

KW - and forest-steppe zones

KW - biodiversity

KW - carbon pool

KW - coniferous-broadleaved

KW - ecologicalcenotic scales

KW - postagrogenic soils

KW - soil acidity

KW - southern-taiga

KW - vegetation demutation

UR - http://www.scopus.com/inward/record.url?scp=85042556379&partnerID=8YFLogxK

U2 - 10.1134/S1064229317120109

DO - 10.1134/S1064229317120109

M3 - Article

AN - SCOPUS:85042556379

VL - 50

SP - 1515

EP - 1534

JO - Eurasian Soil Science

JF - Eurasian Soil Science

SN - 1064-2293

IS - 12

ER -

ID: 97810443