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Miaolingian (Cambrian) trilobite biostratigraphy and carbon isotope chemostratigraphy in the Tingskullen drill core, Oland, Sweden

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F21%3AN0000131" target="_blank" >RIV/60460709:41330/21:N0000131 - isvavai.cz</a>

  • Result on the web

    <a href="https://kirj.ee/earth-publications/?filter%5Byear%5D=2021&filter%5Bissue%5D=412&" target="_blank" >https://kirj.ee/earth-publications/?filter%5Byear%5D=2021&filter%5Bissue%5D=412&</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3176/earth.2021.03" target="_blank" >10.3176/earth.2021.03</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Miaolingian (Cambrian) trilobite biostratigraphy and carbon isotope chemostratigraphy in the Tingskullen drill core, Oland, Sweden

  • Original language description

    The Cambrian succession of the Tingskullen drill core from northern Oland comprises Cambrian Series 2 and Miaolingian (Wulivan Stage) siliciclastic strata. The major portion of the succession is represented by the Miaolingian Borgholm Formation, which, in ascending order, is subdivided into the Mossberga, Barstad and Aleklinta members. The Aleklinta Member is barren of body fossils, whereas the Mossberga and BArstad members are moderately to highly fossiliferous and biostratigraphically reasonably well constrained. Trilobites and agnostoids from the BArstad Member are indicative of the Acadoparadoxides pin us Zone. The Mossberga Member has not yielded any zonal guide fossils but is tentatively assigned to the Eccaparadoxides insularis Zone. A delta C-13(org) curve throughout the Borgholm Formation shows a general positive trend up section without any distinctive excursion, suggesting that the Wulivan Acadoparadoxides (Baltoparadoxides) oelandicus Superzone (the Oelandicus beds) of Oland is younger than the negative Redlichiid-Olenellid Extinction Carbon isotope Excursion (ROECE), which is known from near the top of Stage 4 and close to the traditional Lower-Middle Cambrian boundary in several parts of the world.

  • 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

  • Continuities

    S - Specificky vyzkum na vysokych skolach

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

    ESTONIAN JOURNAL OF EARTH SCIENCES

  • ISSN

    1736-4728

  • e-ISSN

    1736-7557

  • Volume of the periodical

    70

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    EE - ESTONIA

  • Number of pages

    18

  • Pages from-to

    18-35

  • UT code for WoS article

    000609229300002

  • EID of the result in the Scopus database

    2-s2.0-85099604457