Paleolandscape reconstruction based on the study of a buried soil of the bronze age in the broadleaf forest area of the russian plain

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Paleolandscape reconstruction based on the study of a buried soil of the bronze age in the broadleaf forest area of the russian plain. / Aseyeva, Elena; Makeev, Alexander; Kurbanova, Fatima; Kust, Pavel; Rusakov, Alexey; Khokhlova, Olga; Mihailov, Evgeniy; Puzanova, Tatiana; Golyeva, Alexandra.

In: Geosciences (Switzerland), Vol. 9, No. 3, 111, 03.2019.

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

Author

Aseyeva, Elena ; Makeev, Alexander ; Kurbanova, Fatima ; Kust, Pavel ; Rusakov, Alexey ; Khokhlova, Olga ; Mihailov, Evgeniy ; Puzanova, Tatiana ; Golyeva, Alexandra. / Paleolandscape reconstruction based on the study of a buried soil of the bronze age in the broadleaf forest area of the russian plain. In: Geosciences (Switzerland). 2019 ; Vol. 9, No. 3.

BibTeX

@article{e00c0711f2984776bc44312522d32231,

title = "Paleolandscape reconstruction based on the study of a buried soil of the bronze age in the broadleaf forest area of the russian plain",

abstract = "Late Holocene landscape evolution at the southern frontier of the forest belt of European Russia is studied based on detailed morphological, analytical and microbiomorphic research of a soil chronosequence that included a surface soil and a soil buried under the Bronze Age kurgan. Both soils (Folic Eutric Cambisols) are formed on similar geomorphic surfaces in the same parent material and in close proximity to each other. The soil morphology and the key analytical features are controlled by low-reactive parent material and imply close similarity of the present landscapes and those of the Bronze age. At the same time the morphological features show that the buried soil was influenced by the phase of weak aridization, which led to the formation of a dark mull humus horizon. Microbiomorphic assemblages (phytoliths, pollen) support the earlier conclusion that the soils of the study area had being developed mostly under forest vegetation.",

keywords = "Abashevo archaeological culture, Atlantic, Broadleaf forest, Cambisol, Kurgans, Non-reactive parent material, Paleosol, Subboreal, CHERNOZEMS, STEPPE, paleosol, HOLOCENE, PALEOSOLS, non-reactive parent material, RECORDS, kurgans, broadleaf forest",

author = "Elena Aseyeva and Alexander Makeev and Fatima Kurbanova and Pavel Kust and Alexey Rusakov and Olga Khokhlova and Evgeniy Mihailov and Tatiana Puzanova and Alexandra Golyeva",

year = "2019",

month = mar,

doi = "10.3390/geosciences9030111",

language = "English",

volume = "9",

journal = "Geosciences (Switzerland)",

issn = "2076-3263",

publisher = "MDPI AG",

number = "3",

}

RIS

TY - JOUR

T1 - Paleolandscape reconstruction based on the study of a buried soil of the bronze age in the broadleaf forest area of the russian plain

AU - Aseyeva, Elena

AU - Makeev, Alexander

AU - Kurbanova, Fatima

AU - Kust, Pavel

AU - Rusakov, Alexey

AU - Khokhlova, Olga

AU - Mihailov, Evgeniy

AU - Puzanova, Tatiana

AU - Golyeva, Alexandra

PY - 2019/3

Y1 - 2019/3

N2 - Late Holocene landscape evolution at the southern frontier of the forest belt of European Russia is studied based on detailed morphological, analytical and microbiomorphic research of a soil chronosequence that included a surface soil and a soil buried under the Bronze Age kurgan. Both soils (Folic Eutric Cambisols) are formed on similar geomorphic surfaces in the same parent material and in close proximity to each other. The soil morphology and the key analytical features are controlled by low-reactive parent material and imply close similarity of the present landscapes and those of the Bronze age. At the same time the morphological features show that the buried soil was influenced by the phase of weak aridization, which led to the formation of a dark mull humus horizon. Microbiomorphic assemblages (phytoliths, pollen) support the earlier conclusion that the soils of the study area had being developed mostly under forest vegetation.

AB - Late Holocene landscape evolution at the southern frontier of the forest belt of European Russia is studied based on detailed morphological, analytical and microbiomorphic research of a soil chronosequence that included a surface soil and a soil buried under the Bronze Age kurgan. Both soils (Folic Eutric Cambisols) are formed on similar geomorphic surfaces in the same parent material and in close proximity to each other. The soil morphology and the key analytical features are controlled by low-reactive parent material and imply close similarity of the present landscapes and those of the Bronze age. At the same time the morphological features show that the buried soil was influenced by the phase of weak aridization, which led to the formation of a dark mull humus horizon. Microbiomorphic assemblages (phytoliths, pollen) support the earlier conclusion that the soils of the study area had being developed mostly under forest vegetation.

KW - Abashevo archaeological culture

KW - Atlantic

KW - Broadleaf forest

KW - Cambisol

KW - Kurgans

KW - Non-reactive parent material

KW - Paleosol

KW - Subboreal

KW - CHERNOZEMS

KW - STEPPE

KW - paleosol

KW - HOLOCENE

KW - PALEOSOLS

KW - non-reactive parent material

KW - RECORDS

KW - kurgans

KW - broadleaf forest

UR - http://www.scopus.com/inward/record.url?scp=85069537212&partnerID=8YFLogxK

UR - http://www.mendeley.com/research/paleolandscape-reconstruction-based-study-buried-soil-bronze-age-broadleaf-forest-area-russian-plain

U2 - 10.3390/geosciences9030111

DO - 10.3390/geosciences9030111

M3 - Article

AN - SCOPUS:85069537212

VL - 9

JO - Geosciences (Switzerland)

JF - Geosciences (Switzerland)

SN - 2076-3263

IS - 3

M1 - 111

ER -

ID: 50033618