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Late Turonian ostracod assemblages record a shift from mesotrophic to oligtrophic hemipelagic deposits in the Bohemian Cretaceous Basin (Czech Republic)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F19%3A00000125" target="_blank" >RIV/00025798:_____/19:00000125 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/19:10398617

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0195667118304270" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0195667118304270</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.cretres.2019.06.006" target="_blank" >10.1016/j.cretres.2019.06.006</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Late Turonian ostracod assemblages record a shift from mesotrophic to oligtrophic hemipelagic deposits in the Bohemian Cretaceous Basin (Czech Republic)

  • Original language description

    The late Turonian marine benthic ostracods have been identified in the hemipelagic marlstones and limestones of the Bohemian Cretaceous Basin situated between the Boreal and Tethyan Realms. Cytherella cf. concava, C. cf. ovata, Cytherelloidea hindei and C. stricta (all Platycopida and survivors of the upper Cenomanian OAE2 low-oxygen level) were dominant in the monotonous poorly fossiliferous marlstone of the Jizera Formation. The cooling associated with cool water shift to the south and marked by the Hyphantoceras Event enabled the spread of the diverse Boreal faunae and the ostracod fauna of the Teplice Formation, which highly resembles the British Islands ostracod associations. Their biodiversity increased in mesotrophic conditions and the maximum was attained in an oligotrophic system depleted in nutrition. The ratio of Platycopida/Podocopida changed from 9:1 in hypoxic dark marlstone to 1:2 in times of supposed oligotrophic, well aerated conditions in the grayish and dark marlstones deposited in the period of maximum flooding surface. Although the dinoflagellates and coccolithophorids of appropriate size were very common to abundant for filter feeder platycopids, they were replaced upwards by deposit feeder podocopids.

  • 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

    10506 - Paleontology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2019

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Cretaceous Research

  • ISSN

    0195-6671

  • e-ISSN

  • Volume of the periodical

    104

  • Issue of the periodical within the volume

    104160

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    19

  • Pages from-to

    nestránkováno

  • UT code for WoS article

    000488316300004

  • EID of the result in the Scopus database

    2-s2.0-85071104166