Features of the development of steppe chernozems were established based on the study of soils of different age groups at archaeological sites. Differences in the formation of phytomass and morphological maturity of the soil profile in the recovery of different age successions were shown. A regional model of the humus horizon steppe soil over time allowed us to estimate the time interval at which the processes of humus accumulation and morphological maturity of the soil profile are relatively at equilibriumyesBelgorod State Universit
During the second half of the Holocene, the Russian Plain experienced several climatic oscillations ...
The peculiarities of historical phases of steppe ecosystems transformation influenced by grazing pre...
Temporal changes in soils of forest landscapes of the forest-steppe zone - Haplic Luvisols and Greyz...
yesFeatures of the development of steppe chernozems were established based on the study of soils of ...
The results of long-term studies of chernozem development in anthropogenically disturbed landscapes ...
The uptake and transformation of organic matter were studied in phytocenoses characterizing the basi...
Geoarchaeological methods were used to study chronosequences of surface soils in the steppe zone an...
Based on investigating dated anthropogenic structures, we present the results derived from studying ...
The study of soils of different ages in different physiographic regions of the Crimean Peninsula mad...
Fallow lands in ancient agricultural areas of Northwestern Crimea which had experienced repeated pha...
Soil catenas crossing various archeological objects with an age of 360-1800 years have been studied ...
The aim of the study was to comparatively analyse the soils of fallow lands of different times near ...
An inventory of published data on the natural evolution of forest-steppe, steppe, and semidesert soi...
The questions of phytobiota evolution and formation of steppes in the vast region of the south of Ea...
The article is dedicated to soil and archaeological investigations of hill forts located in the sout...
During the second half of the Holocene, the Russian Plain experienced several climatic oscillations ...
The peculiarities of historical phases of steppe ecosystems transformation influenced by grazing pre...
Temporal changes in soils of forest landscapes of the forest-steppe zone - Haplic Luvisols and Greyz...
yesFeatures of the development of steppe chernozems were established based on the study of soils of ...
The results of long-term studies of chernozem development in anthropogenically disturbed landscapes ...
The uptake and transformation of organic matter were studied in phytocenoses characterizing the basi...
Geoarchaeological methods were used to study chronosequences of surface soils in the steppe zone an...
Based on investigating dated anthropogenic structures, we present the results derived from studying ...
The study of soils of different ages in different physiographic regions of the Crimean Peninsula mad...
Fallow lands in ancient agricultural areas of Northwestern Crimea which had experienced repeated pha...
Soil catenas crossing various archeological objects with an age of 360-1800 years have been studied ...
The aim of the study was to comparatively analyse the soils of fallow lands of different times near ...
An inventory of published data on the natural evolution of forest-steppe, steppe, and semidesert soi...
The questions of phytobiota evolution and formation of steppes in the vast region of the south of Ea...
The article is dedicated to soil and archaeological investigations of hill forts located in the sout...
During the second half of the Holocene, the Russian Plain experienced several climatic oscillations ...
The peculiarities of historical phases of steppe ecosystems transformation influenced by grazing pre...
Temporal changes in soils of forest landscapes of the forest-steppe zone - Haplic Luvisols and Greyz...