Number of the records: 1  

Investigation of vegetation history of buried chernozem soils using near-infrared spectroscopy (NIRS)

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    SYSNO ASEP0432316
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleInvestigation of vegetation history of buried chernozem soils using near-infrared spectroscopy (NIRS)
    Author(s) Vysloužilová, B. (CZ)
    Ertlen, D. (FR)
    Šefrna, L. (CZ)
    Novák, T. (HU)
    Virágh, K. (HU)
    Rué, M. (FR)
    Campaner, A. (FR)
    Dreslerová, Dagmar (ARU-G) RID, SAI, ORCID
    Schwartz, D. (FR)
    Number of authors9
    Source TitleQuaternary International. - : Elsevier - ISSN 1040-6182
    Roč. 365, 16 April (2015), s. 203-211
    Number of pages9 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsHolocene ; paleopedology ; paleoecology ; near-infrared spectroscopy ; chernozem ; buried paleosol
    Subject RIVDF - Soil Science
    Institutional supportARU-G - RVO:67985912
    UT WOS000353334700015
    EID SCOPUS84928215975
    DOI10.1016/j.quaint.2014.07.035
    AnnotationThe environmental conditions of the evolution of chernozems in Central Europe have not been satisfactory explained. In this paper, seven buried chernozems were investigated using near-infrared spectroscopy (NIRS) in order to get information about the former vegetation cover. Near-infrared (NIR) data were collected from organic matter of recent natural grasslands and forests. The spectra from these two groups of soils were perfectly discriminated by a multivariate statistical analysis. The statistical model was applied on the buried soils. There are four types of vegetation development within the chernozems before the burial. Comparison to other paleoenvironmental proxies shows no major contradiction and confirms the potential of the NIRS as a paleopedological proxy. The identified changes of vegetation are from grassland vegetation to forest vegetation and vice versa. These changes bring new data to the discussion about the pedogenesis of chernozems. According to the radiocarbon dating, buried soils developed and were preserved not only in the Preboreal and the Boreal, but also in later phases of the Holocene.
    WorkplaceInstitute of Archaeology (Prague)
    ContactLada Šlesingerová, slesingerova@arup.cas.cz, Tel.: 257 014 412
    Year of Publishing2016
Number of the records: 1  

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