Transformation of soils and environmental conditions in the semidesert low Volga region within the past 4000 yearsстатья
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 26 января 2022 г.
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Авторы:
Demkin V.A.,
Demkina T.S.,
Borisov A.V.,
Yakimov A.S.,
Sergatskov I.V.
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Журнал:
Eurasian Soil Science
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Том:
37
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Номер:
3
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Год издания:
2004
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Издательство:
Maik Nauka/Interperiodica Publishing
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Местоположение издательства:
Russian Federation
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Первая страница:
230
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Последняя страница:
241
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Аннотация:
Paleosols buried under kurgans of the Bronze (ca. 2000 BC and 1600-1500 BC), Early Iron (200-300 AD), and Medieval (1200-1300 AD) ages and surface light chestnut soils and solonetzes have been studied within the territory of the Northern Caspian Plain composed of Khvalyn deposits. Regularities of long-term changes in morphological features and chemical properties of semidesert soils within the past 4000 years are discussed. Data on the state of soil microbial communities during this period are presented. The reconstruction of climatic fluctuations in the region is made on the basis of paleosol and microbiological data. © 2004 by MAIK "Nauka/Interperiodica" (Russia).
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Добавил в систему:
Борисов Александр Владимирович