Paleopedological studies of the Voytsehovka cemetery barrows

The article deals with analysis of paleosoils of the Voytsehovka a cemetery, investigated by the Fastov archaeological expedition in 2011—2012. The most significant materials were obtained from the clearing made in barrows No. 1 and 2. The mounds were erected in the Late Bronze Age and belong to the...
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Autor*in:	Matviishyna, Zh.N. [verfasserIn] Lysenko, S.D. [verfasserIn] Kushnir, A.S. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch ; Russisch

Erschienen:	2021

Schlagwörter:	volyn late trupolye culture bronze age trzhinets cultural circle komarov culture burial mounds paleosoil

Übergeordnetes Werk:	In: Материалы по археологии и истории античного и средневекового Причерноморья - Cimmeria Publishing, 2020, (2021), 12, Seite 13-76
Übergeordnetes Werk:	year:2021 ; number:12 ; pages:13-76

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.24411/2713-2021-2020-00001

Katalog-ID:	DOAJ055849024

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language	English Russian
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author	Matviishyna, Zh.N.
spellingShingle	Matviishyna, Zh.N. misc CC1-960 misc DJK1-77 misc volyn misc late trupolye culture misc bronze age misc trzhinets cultural circle misc komarov culture misc burial mounds misc paleosoil misc Archaeology misc History of Eastern Europe Paleopedological studies of the Voytsehovka cemetery barrows
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topic_title	CC1-960 DJK1-77 Paleopedological studies of the Voytsehovka cemetery barrows volyn late trupolye culture bronze age trzhinets cultural circle komarov culture burial mounds paleosoil
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title	Paleopedological studies of the Voytsehovka cemetery barrows
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title_sort	paleopedological studies of the voytsehovka cemetery barrows
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title_auth	Paleopedological studies of the Voytsehovka cemetery barrows
abstract	The article deals with analysis of paleosoils of the Voytsehovka a cemetery, investigated by the Fastov archaeological expedition in 2011—2012. The most significant materials were obtained from the clearing made in barrows No. 1 and 2. The mounds were erected in the Late Bronze Age and belong to the Komarov culture of the Trzhinets cultural circle (the middle — the 3rd quarter of the 2nd millennium BCE). Trypolye settlement of stage CII (the end of the 4th millennium BCE) preceded time of the building of these kurgans. A gray forest soil was traced in barrow 1 (2011), similar to those that now is forming under broadleaf forests. Climate conditions were much better than modern ones. Zoning (zone of the mixed forest) was placed to the north. Large areas were occupied by hornbeam and beech forests; there were areas of open spaces with lush grass vegetation. The modern soil in the barrow 2 (2012) can be defined as sod-strongly podzolic, but the illuvial horizon with cultural remains may characterize the conditions of forest soil formation, close to the regime of formation of soils of a more warm-temperate regime — brown podzolic forest soils, which developed in conditions of less continental but a more uniformly humid climate. The natural zones represented a westerly version of a warm-temperate climate (similar to the Carpathian one) and, probably, the territory was covered with broad-leaved forests with areas of open spaces. The profile of an older soil is also recorded under the mound, close to podzolic chernozems or dark gray forest soils.
abstractGer	The article deals with analysis of paleosoils of the Voytsehovka a cemetery, investigated by the Fastov archaeological expedition in 2011—2012. The most significant materials were obtained from the clearing made in barrows No. 1 and 2. The mounds were erected in the Late Bronze Age and belong to the Komarov culture of the Trzhinets cultural circle (the middle — the 3rd quarter of the 2nd millennium BCE). Trypolye settlement of stage CII (the end of the 4th millennium BCE) preceded time of the building of these kurgans. A gray forest soil was traced in barrow 1 (2011), similar to those that now is forming under broadleaf forests. Climate conditions were much better than modern ones. Zoning (zone of the mixed forest) was placed to the north. Large areas were occupied by hornbeam and beech forests; there were areas of open spaces with lush grass vegetation. The modern soil in the barrow 2 (2012) can be defined as sod-strongly podzolic, but the illuvial horizon with cultural remains may characterize the conditions of forest soil formation, close to the regime of formation of soils of a more warm-temperate regime — brown podzolic forest soils, which developed in conditions of less continental but a more uniformly humid climate. The natural zones represented a westerly version of a warm-temperate climate (similar to the Carpathian one) and, probably, the territory was covered with broad-leaved forests with areas of open spaces. The profile of an older soil is also recorded under the mound, close to podzolic chernozems or dark gray forest soils.
abstract_unstemmed	The article deals with analysis of paleosoils of the Voytsehovka a cemetery, investigated by the Fastov archaeological expedition in 2011—2012. The most significant materials were obtained from the clearing made in barrows No. 1 and 2. The mounds were erected in the Late Bronze Age and belong to the Komarov culture of the Trzhinets cultural circle (the middle — the 3rd quarter of the 2nd millennium BCE). Trypolye settlement of stage CII (the end of the 4th millennium BCE) preceded time of the building of these kurgans. A gray forest soil was traced in barrow 1 (2011), similar to those that now is forming under broadleaf forests. Climate conditions were much better than modern ones. Zoning (zone of the mixed forest) was placed to the north. Large areas were occupied by hornbeam and beech forests; there were areas of open spaces with lush grass vegetation. The modern soil in the barrow 2 (2012) can be defined as sod-strongly podzolic, but the illuvial horizon with cultural remains may characterize the conditions of forest soil formation, close to the regime of formation of soils of a more warm-temperate regime — brown podzolic forest soils, which developed in conditions of less continental but a more uniformly humid climate. The natural zones represented a westerly version of a warm-temperate climate (similar to the Carpathian one) and, probably, the territory was covered with broad-leaved forests with areas of open spaces. The profile of an older soil is also recorded under the mound, close to podzolic chernozems or dark gray forest soils.
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title_short	Paleopedological studies of the Voytsehovka cemetery barrows
url	https://doi.org/10.24411/2713-2021-2020-00001 https://doaj.org/article/f5d6156653ce480c92f368420f9884cd https://cyberleninka.ru/article/n/paleopedologicheskie-issledovaniya-kurganov-voytsehovskogo-mogilnika https://doaj.org/toc/2713-2021
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author2	Lysenko, S.D. Kushnir, A.S.
author2Str	Lysenko, S.D. Kushnir, A.S.
ppnlink	172778930X
callnumber-subject	CC - Archaeology
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doi_str	10.24411/2713-2021-2020-00001
callnumber-a	CC1-960
up_date	2024-07-03T17:23:28.726Z
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The most significant materials were obtained from the clearing made in barrows No. 1 and 2. The mounds were erected in the Late Bronze Age and belong to the Komarov culture of the Trzhinets cultural circle (the middle — the 3rd quarter of the 2nd millennium BCE). Trypolye settlement of stage CII (the end of the 4th millennium BCE) preceded time of the building of these kurgans. A gray forest soil was traced in barrow 1 (2011), similar to those that now is forming under broadleaf forests. Climate conditions were much better than modern ones. Zoning (zone of the mixed forest) was placed to the north. Large areas were occupied by hornbeam and beech forests; there were areas of open spaces with lush grass vegetation. 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