References

geomorf

Геоморфология и палеогеография

Geomorfologiya i Paleogeografiya

2949-17892949-1797

10.31857/S0435428122050042

geomorf-3124

Research Article

Проблемы палеопочвоведения и геоархеологии

Problems of palaeopedology and geoarchaeology

Палеочерноземы времени развития срубной культуры и тренды позднеголоценовой эволюции почв лесостепи Восточно-Европейской равнины

Paleochernozems of the Srubnaya culture period and trends of Late Holocene evolution of soils in the East European Plain forest-steppe

Чендев

Ю. Г.

Chendev

Yu. G.

sciences@mail.ru

Пузанова

Т. А.

Puzanova

T. A.

Курбанова

Ф. Г.

Kurbanova

F. G.

Белгородский государственный национальный исследовательский университет (BelSU), БелгородРоссияBelgorod State National Research University (BelSU), BelgorodRussian Federation

Московский государственный университет имени М.В. Ломоносова, географический факультет, МоскваРоссияLomonosov Moscow State University, Faculty of Geography, MoscowRussian Federation

Институт географии РАН, МоскваРоссияInstitute of Geography RAS, MoscowRussian Federation

2022

13022023

535103115

2023

Чендев Ю.Г., Пузанова Т.А., Курбанова Ф.Г.

Chendev Y.G., Puzanova T.A., Kurbanova F.G.

Данная работа распространяется под лицензией Creative Commons Attribution 4.0.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://geomorphology.igras.ru/jour/article/view/3124

Выполнен сравнительный анализ признаков черноземов, погребенных под курганами периода срубной культурно-исторической общности (3600–3400 л. н.), их аналогов более ранних (4200– 3700 л. н.) и более поздних (2500–2200 л. н.) периодов, а также современных компонентов почвенного покрова на территории центра Восточно-Европейской равнины. Черноземы периода срубной культуры формировались в обстановке заметных биоклиматических изменений, последовавших вслед за периодом среднесуббореальной аридизации климата. Установлено, что биохимическая перестройка профиля по содержанию почвенного органического вещества опережала морфологическую перестройку с формированием более мощной темноцветной части профиля черноземов. Автоморфные палеочерноземы срубного времени характеризовались большей однородностью морфологических свойств (на всех изученных участках – черноземы типичные) по сравнению с современными аналогами (возникли два ареала черноземов – выщелоченных и типичных). Черноземы выщелоченные возникли на участках с меньшими запасами карбонатов в почвообразующих породах по сравнению с чернозмами типичными. Общий тренд позднеголоценовой эволюции черноземов выщелоченных и типичных состоял в увеличении мощности гумусовых горизонтов (в среднем на 20 см) и почвенных профилей (в среднем на 20 см) при неизменности мощности переходной части профиля (А1В+ВА1) и горизонтов В (Вк). Отличия состояли в разных глубинах выщелачивания почвенных профилей от карбонатов.

A comparative analysis of the features of the chernozems buried under the mounds of the Srubnaya culture (3600–3400 years ago), earlier (4200–3700 years ago) and later analogues (2500–2200 years ago) have been carried out. Also, modern chernozems of the East European Plain central part were studied. The chernozems of the Srubnaya culture period were formed in an environment of noticeable bioclimatic transformations after the period of the Middle Subboreal climate aridization. It was found that the biochemical rearrangement of the profile in terms of the content of soil organic matter outplaced the morphological transformation with the formation of a thicker dark-colored part of the chernozem profile. The automorphic paleochernozems of the Srubny period were characterised by a greater homogeneity of morphological properties (in all studied areas, they were identified as typical chernozems with high carbonate table) compared to their modern analogues (two areas of chernozems were formed – leached and typical). Leached chernozems were formed in areas with lower carbonate content in the parent materials compared to the areas of typical chernozems. The general trend of the Late Holocene evolution of leached and typical automorphic chernozems consisted of an increase in the thickness of humus horizons (by an average of 20 cm) and soil profiles (by an average of 20 cm). In contrast, the thickness of the transitional part of the profile (A1B + BA1) and horizons B (Bk) remained the same. Differences were connected with different depth of leaching from carbonates in the studied soils.

лесостепьВосточная Европачерноземыэволюция почвпоздний голоценсрубная культура

forest-steppeEastern Europechernozemssoil evolutionLate HoloceneSrubnaya culture

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The authors declare that there are no conflicts of interest present.