Формирование культурных ландшафтов Среднего Поволжья за последние 2 тыс. лет (по результатам почвенно-археологических исследований).

Concealed Evidence of Early Human-Environment Interactions in Sedimentary Archives of Small Rivers in the Forest-Steppe Belt of Eurasia

The results of on-site archaeological investigations alone are not enough to reconstruct landscape histories, because they provide incomplete information on past environments. In contrast, off-site sedimentary archives can provide information on the interaction of natural and human processes.

Клмплексный анализ следов подсечного земледелия в песчаных почвах: Карула (Эстония).

People and environment in the central part of the East European plain in the Late Roman Period and at the beginning of the Early Middle Ages (the example of the Sudzha region, Russia)

Подсечное земледелие как фактор мобильности населения в эпоху Великого переселения в лесостепном регионе Евразии

Мобильность населения в эпоху Великого переселения была обусловлена особой формой хозяйственной организации, получившей распространение в этот период и основанной на сочетании подсеки и пашенного земледелия.

Evidence of coupled wind-fire natural disturbance in Atlantic Maritime forest soils

Forests in the Atlantic Maritime Ecozone of North America are subject to intense, periodic windstorms that entail mass tree uprooting and arboturbation of soil. The time for soil formation is limited by the frequency of extreme windstorms, varying from several decades to centuries during the Holoc

DIAGNOSTIC FEATURES OF THE CHARCOAL ASSEMBLAGES ASSOCIATED WITH THE SWIDDEN CULTIVATION

DYNAMICS OF THE SPATIAL DEMOGRAPHY, LAND-USE, AND LANDSCAPES OF MIDVOLGA DURING THE MIGRATION PERIOD

OFF-SITE ARCHAEOLOGY IN THE FOREST ZONE: APPROACHES TO DELINEATING THE AREAS OF SWIDDEN CULTIVATION

FORMATION OF ANTHROPOGENIC LANDSCAPES ON MID-VOLGA

LONG-TERM POPULATION AND LAND-USE TRENDS IN MIDDLE VOLGA REGION IN EARLY IRON AGE AND MIDDLE AGES

Formation of anthropogenic landscapes in the Middle Volga region in the last two middenia through the use of phytoliths and other proxies in soils

Paleochernozems in the forest zone of central Russia and their evolution during MIS 1

Modern chernozems are developed from loess sediments in the steppe zone and in steppe areas of the forest-steppe zone. Paleochernozems of the Early and Middle Holocene were discovered in the forest zone and within forest biomes of the forest-steppe zone (Alexandrovskiy, Alexandrovskaya, 2005; Chende