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Long-term history of woodland under human impact, archaeoanthracological synthesis for lowlands in Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985912%3A_____%2F21%3A00546727" target="_blank" >RIV/67985912:_____/21:00546727 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/21:10438826

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S1040618220306807?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1040618220306807?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.quaint.2020.10.054" target="_blank" >10.1016/j.quaint.2020.10.054</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Long-term history of woodland under human impact, archaeoanthracological synthesis for lowlands in Czech Republic

  • Original language description

    The vegetation history of lowland woodlands in Central Europe is closely related with human activities. Our study is focused on the evaluation of a large archaeo-anthracological dataset from a large-scale territory in Central Europe. Our dataset contains about 240 891 charcoal records from 474 localities. Our research focuses on the reconstruction of the woodland history in the surroundings of archaeological sites from the Neolithic (7600 BP) to the Migration Period (1450 BP) and reveals differences in the anthracological records among regions of the Czech Republic. A comparison of long-term charcoal records from regions with a different presence of human activities has allowed for a special evaluation of vegetation trends. Environmental conditions in the regions are not uniform and our study detects the variability of charcoal assemblages and different vegetation histories among the localities. The smallest differences of species composition among regions were recorded in the Neolithic. Land-use changes during the Bronze Age accelerated the compositional change of the woodland vegetation. We distinguish 3 different types of woodland history, which are based on trends in the charcoal taxa composition: a) slight vegetation changes and predominance of Quercus, b) important changes of woodland composition during the Bronze Age, c) slight vegetation changes and high abundance of Pinus. Vegetation trends, which began in the Bronze Age, continued into the Iron Age. The Late Holocene woodland transformation was related to the migration trends of Carpinus, Fagus and Abies. Overall, it is clear that the transformation of woodland vegetation had an east-west direction and our study area shows a significant difference among regions. The results of our study show that abundant archaeo-anthracological records from many sites and periods can also rectify the gaps sometimes observed in charcoal sequences of individual sites.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    60102 - Archaeology

Result continuities

  • Project

    <a href="/en/project/GA19-14292S" target="_blank" >GA19-14292S: Long-term history of woodland under human impact, archaeoathracological synthesis for lowlands in Czech Republic</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Quaternary International

  • ISSN

    1040-6182

  • e-ISSN

    1873-4553

  • Volume of the periodical

    593-594

  • Issue of the periodical within the volume

    20 August

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    9

  • Pages from-to

    195-203

  • UT code for WoS article

    000661935400002

  • EID of the result in the Scopus database

    2-s2.0-85095844807