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In search for the Basal Emsian GSSP in the Prague Synform: Mramorka – a possible candidate section

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F24%3A00585468" target="_blank" >RIV/67985831:_____/24:00585468 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.schweizerbart.de/papers/nos/detail/57/103997/In_search_for_the_Basal_Emsian_GSSP_in_the_Prague_Synform_Mramorka_a_possible_candidate_section" target="_blank" >https://www.schweizerbart.de/papers/nos/detail/57/103997/In_search_for_the_Basal_Emsian_GSSP_in_the_Prague_Synform_Mramorka_a_possible_candidate_section</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1127/nos/2024/0795" target="_blank" >10.1127/nos/2024/0795</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    In search for the Basal Emsian GSSP in the Prague Synform: Mramorka – a possible candidate section

  • Original language description

    The present GSSP for the basal Emsian boundary remains among the most problematic issues in the global Paleozoic stratigraphy as it is accented by the International Commission on Stratigraphy (ICS/IUGS). The former traditional Pragian Stage of the Lower Devonian that has been originally based on the Praha Formation in the Prague Synform was thus drastically reduced. Herein is presented a possible candidate section for the prospective basal GSSP redefinition – the Mramorka section near Chýnice, Prague Synform, Czech Republic. It has the typical varied development of the upper part of the Praha Formation including the Bohemian Graptolite Event (BGE), i.e. a prominent lithological marker in the NW flank of the Prague Synform. In order to provide a robust dataset for the rigorous evaluation of the GSSP potential of this candidate section, data from complex multiproxy studies including biostratigraphy, sedimentology, gamma-ray spectrometry, magnetic susceptibility, multi-element geochemistry (INAA, EDXRF), and stable isotopes (δ18O, δ13C) are presented. The boundary criterion is the gracilis Event that is close to the traditional boundary between the Pragian and Emsian stages. The event is characterized by a conodont Latericriodus bilatericrescens gracilis Bultynck, 1985, which widely occurs in NW part of Gondwana. The lowermost entry of the taxon within the Prague Synform has been recorded in the Mramorka section, 145 cm below the BGE interval. The sedimentology of the Mramorka section is characterized by grey nodular calcisiltites largely influenced by ichnofabric, but the BGE interval consists mostly of darker grey, ichnofossil-poor, platy limestones interbedded with black calcareous shales. The data obtained from multiproxy studies in the Mramorka section show a marked change in geochemical proxies within and above the BGE. The values of CGR and elements typical for terrigenous input show relatively higher values below the BGE interval and a gradual decrease above the BGE. The BGE interval is characterized by elevated paleoredox and paleoproductivity proxies. REEN values show mostly the MREE bulge pattern and are linked mainly to terrigenous (especially aeolian) supply. The MS is largely tied to the terrigenous input, but is also influenced by authigenic Fe minerals. δ13C values change markedly above the BGE. The sediments below the BGE interval are considered to record the culminating transgression and strata above the BGE interval the highstand. The BGE interval itself records the maximum flooding. If present, the BGE interval close above the gracilis Event may serve an independent marker for approximation of the prospective GSSP boundary.

  • 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

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/GA21-21829S" target="_blank" >GA21-21829S: Proposal for the GSSP of the Basal Emsian Boundary in the Prague Synform</a><br>

  • 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

    Newsletters on Stratigraphy

  • ISSN

    0078-0421

  • e-ISSN

  • Volume of the periodical

    57

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    31

  • Pages from-to

    171-201

  • UT code for WoS article

    001157706300001

  • EID of the result in the Scopus database

    2-s2.0-85193744117