Počet záznamů: 1  

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

  1. 1.
    SYSNO ASEP0432316
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevInvestigation of vegetation history of buried chernozem soils using near-infrared spectroscopy (NIRS)
    Tvůrce(i) 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)
    Celkový počet autorů9
    Zdroj.dok.Quaternary International. - : Elsevier - ISSN 1040-6182
    Roč. 365, 16 April (2015), s. 203-211
    Poč.str.9 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovaHolocene ; paleopedology ; paleoecology ; near-infrared spectroscopy ; chernozem ; buried paleosol
    Vědní obor RIVDF - Pedologie
    Institucionální podporaARU-G - RVO:67985912
    UT WOS000353334700015
    EID SCOPUS84928215975
    DOI10.1016/j.quaint.2014.07.035
    AnotaceThe 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.
    PracovištěArcheologický ústav Praha
    KontaktLada Šlesingerová, slesingerova@arup.cas.cz, Tel.: 257 014 412
    Rok sběru2016
Počet záznamů: 1  

  Tyto stránky využívají soubory cookies, které usnadňují jejich prohlížení. Další informace o tom jak používáme cookies.