Chemical data on ashy soils as an information basis for dating archaeological sites

As a special type of parent rock associated with human activities both in antiquity and nowadays, ash widely occurs in the settlements’ functional zones and their cultural layers. Soils developed on ash deposits of various genesis can be presented as soil chronosequences, which forms an information...

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Main Authors: Fedor N. Lisetskii, Arseniy O. Poletaev, Vladimir F. Stolba
Format: Article
Language:English
Published: Elsevier 2021-02-01
Series:Data in Brief
Subjects:
Ash
Online Access:http://www.sciencedirect.com/science/article/pii/S2352340920315705
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spelling doaj-c8ad90a6fc7e43afb5372840f1085c572020-12-31T04:42:54ZengElsevierData in Brief2352-34092021-02-0134106691Chemical data on ashy soils as an information basis for dating archaeological sitesFedor N. Lisetskii0Arseniy O. Poletaev1Vladimir F. Stolba2Federal and Regional Centre for Aerospace and Surface Monitoring of the Objects and Natural Resources, Belgorod National Research University, Belgorod 308015, Russian Federation; Corresponding author:Institute of Earth Sciences, Belgorod National Research University, Belgorod 308015, Russian FederationBerlin-Brandenburgische Akademie der Wissenschaften, Jägerstrasse 22/23, D-10117 Berlin, GermanyAs a special type of parent rock associated with human activities both in antiquity and nowadays, ash widely occurs in the settlements’ functional zones and their cultural layers. Soils developed on ash deposits of various genesis can be presented as soil chronosequences, which forms an information basis for determining the time at which settlements and their economic zones went out of use (“Archaeological ash deposits and soils formed on ash in the south of the East European Plain. Quaternary International” [1]). Studies of ash deposits and soils formed on ash were conducted in three regions of the East European Plain which differ in extent of forest cover. Geochemical associations of accumulated and dispersed elements in the upper horizon of soils of different age in relation to the original ash were determined. This makes it possible to calculate the time of biogeochemical transformation of ash in the course of pedogenesis, thus offering a new dating technique for archaeologists.http://www.sciencedirect.com/science/article/pii/S2352340920315705Archaeological soilsAshAsh DepositsFuelPedoarchaeologyGeoarchaeology
collection DOAJ
language English
format Article
sources DOAJ
author Fedor N. Lisetskii
Arseniy O. Poletaev
Vladimir F. Stolba
spellingShingle Fedor N. Lisetskii
Arseniy O. Poletaev
Vladimir F. Stolba
Chemical data on ashy soils as an information basis for dating archaeological sites
Data in Brief
Archaeological soils
Ash
Ash Deposits
Fuel
Pedoarchaeology
Geoarchaeology
author_facet Fedor N. Lisetskii
Arseniy O. Poletaev
Vladimir F. Stolba
author_sort Fedor N. Lisetskii
title Chemical data on ashy soils as an information basis for dating archaeological sites
title_short Chemical data on ashy soils as an information basis for dating archaeological sites
title_full Chemical data on ashy soils as an information basis for dating archaeological sites
title_fullStr Chemical data on ashy soils as an information basis for dating archaeological sites
title_full_unstemmed Chemical data on ashy soils as an information basis for dating archaeological sites
title_sort chemical data on ashy soils as an information basis for dating archaeological sites
publisher Elsevier
series Data in Brief
issn 2352-3409
publishDate 2021-02-01
description As a special type of parent rock associated with human activities both in antiquity and nowadays, ash widely occurs in the settlements’ functional zones and their cultural layers. Soils developed on ash deposits of various genesis can be presented as soil chronosequences, which forms an information basis for determining the time at which settlements and their economic zones went out of use (“Archaeological ash deposits and soils formed on ash in the south of the East European Plain. Quaternary International” [1]). Studies of ash deposits and soils formed on ash were conducted in three regions of the East European Plain which differ in extent of forest cover. Geochemical associations of accumulated and dispersed elements in the upper horizon of soils of different age in relation to the original ash were determined. This makes it possible to calculate the time of biogeochemical transformation of ash in the course of pedogenesis, thus offering a new dating technique for archaeologists.
topic Archaeological soils
Ash
Ash Deposits
Fuel
Pedoarchaeology
Geoarchaeology
url http://www.sciencedirect.com/science/article/pii/S2352340920315705
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AT arseniyopoletaev chemicaldataonashysoilsasaninformationbasisfordatingarchaeologicalsites
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