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Macrobenthic organisms - trace fossil interactions in the Lower Carboniferous Culm Basin (Drahany Upland and Nízký Jeseník Mts. of the Czech Republic)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F25%3A73632107" target="_blank" >RIV/61989592:15310/25:73632107 - isvavai.cz</a>

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Macrobenthic organisms - trace fossil interactions in the Lower Carboniferous Culm Basin (Drahany Upland and Nízký Jeseník Mts. of the Czech Republic)

  • Original language description

    The Lower Carboniferous Culm facies of the Moravo–Silesian Unit (Bohemian Massif) preserves thick siliciclastic turbidite successions of the Rhenohercynian Variscan Culm Basin. In the Drahany Upland the most fossiliferous beds are in outcrops of the Myslejovice Fm. (upper Viséan). The Moravice Fm. (upper Viséan) of the Nízký Jeseník Mts. could be the sedimentary basin equivalent for the Myslejovice Fm. in similar fauna and ichnofauna findings but with some differences in the composition of fossil fauna associations.The aim of this short study is to test whether fossil tracks and macrofossils are often found in close proximity and whether there was direct exploitation and use of the organic matter of dead and buried organisms by the originators of the fossil tracks.Microbial coatings, or biofilms, are often poorly associated with impacts on trace fossils or fossil associations due to the lack of paleontological record. Both in the Drahany Upland and in the Nízký Jeseník Mts. (specifically in the Moravice Fm.) there is only indirect evidence of the dependence of macroorganisms on bacterial coatings. These may be some irregularities occurring in the clay and dusty layered surfaces, which may have been misinterpreted in the past and may belong to microbial coatings based on the similarity of morphology. Bacterial activity often contributes to sediment stabilisation (Gerdes et al., 2000), which could explain the highly diverse communities of trace fossils and fossil remains found at certain sites in the Moravian-Silesian Culm Basin.

  • Czech name

  • Czech description

Classification

  • Type

    D - Article in proceedings

  • CEP classification

  • OECD FORD branch

    10506 - Paleontology

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2025

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    24th Czech – Slovak – Polish Paleontological Conference

  • ISBN

    978-83-941956-8-7

  • ISSN

  • e-ISSN

  • Number of pages

    2

  • Pages from-to

    34-35

  • Publisher name

    The Grzybowski Foundation &amp; Micropress Europe

  • Place of publication

    Kraków

  • Event location

    Kraków

  • Event date

    Oct 23, 2025

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article