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First evidence of Pinaceae and Fagaceae in the fossil wood record of the Ceske stredohori Mts. (Czech Republic): A comprehensive study of fossiliferous sites in pyroclastic rocks surrounding the late Oligocene Mila stratovolcano

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F24%3A10169057" target="_blank" >RIV/00025798:_____/24:10169057 - isvavai.cz</a>

  • Alternative codes found

    RIV/44555601:13520/24:43898433 RIV/00216208:11310/24:10493040

  • Result on the web

    <a href="https://doi.org/10.1016/j.revpalbo.2024.105097" target="_blank" >https://doi.org/10.1016/j.revpalbo.2024.105097</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.revpalbo.2024.105097" target="_blank" >10.1016/j.revpalbo.2024.105097</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    First evidence of Pinaceae and Fagaceae in the fossil wood record of the Ceske stredohori Mts. (Czech Republic): A comprehensive study of fossiliferous sites in pyroclastic rocks surrounding the late Oligocene Mila stratovolcano

  • Original language description

    A comprehensive anatomical and mineralogical study of fossil wood fragments from fields in the vicinity of Becov and Brvany villages (NW Bohemia, Czech Republic) indicates that Taxodioxylon gypsaceum (Cupressaceae s.l.) predominates, but also identifies another coniferous wood: Pinuxylon parryoides (Pinaceae) and three angiosperms Quercoxylon bockhianum, Castanoxylon bavaricum and Lithocarpoxylon sp. (all Fagaceae). This paper therefore presents the first occurrence of Pinaceae and Fagaceae fossil wood in the volcanic rocks of the Ceske Stredohori Mts. as well as its youngest palaeobotanical record in general, late Oligocene in age (26.56 +/- 0.38 Ma). The samples were buried by alkaline pyroclastic deposits and were mineralized by carbonates. Two distinct depositional processes burying the fossil woods were identified. Closer to the vent, the woods occur in a near-vent pyroclastic fall deposits of the former pyroclastic cone, whereas more distant sites consist of pyroclastic flow deposits. Carbonate mineralization mostly consists of dolomite, but subordinate amounts of magnesite (likely the first time this is documented in fossil wood) as well as calcite and siderite are present. Only one sample collected in the same area, bearing clear signs of riverbed transport (Lithocarpoxylon sp.), was perfectly silicified, but its origin remains unclear.

  • 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

    10507 - Volcanology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Review of Palaeobotany and Palynology

  • ISSN

    0034-6667

  • e-ISSN

    1879-0615

  • Volume of the periodical

    325

  • Issue of the periodical within the volume

    3-4

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    21

  • Pages from-to

  • UT code for WoS article

    001228001400001

  • EID of the result in the Scopus database

    2-s2.0-85189771065