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Graptolite biostratigraphy and biodiversity dynamics in the Silurian System of the Prague Synform (Barrandian area, Czech Republic)

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F23%3A00572149" target="_blank" >RIV/67985831:_____/23:00572149 - isvavai.cz</a>

  • Výsledek na webu

    <a href="http://www.geology.cz/bulletin/contents/art1862" target="_blank" >http://www.geology.cz/bulletin/contents/art1862</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3140/bull.geosci.1862" target="_blank" >10.3140/bull.geosci.1862</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Graptolite biostratigraphy and biodiversity dynamics in the Silurian System of the Prague Synform (Barrandian area, Czech Republic)

  • Popis výsledku v původním jazyce

    Forty six graptolite biozones and seven subzones are recognized in the first compilation of high-resolution Silurian graptolite biostratigraphy in central Bohemia. The durations of these graptolite biozones, deduced from correlation with the Geological Time Scale 2020 age model and the global standard graptolite biozonation, range between ca 0.1 and 1.74 Myr. Each biozone is defined as an interval biozone named after the biozone index species, characterized by a typical biozone assemblage and delineated by bounding horizons with the stratigraphically lowest and/or highest occurrences of the respective index taxa. The Petalolithus folium Biozone is introduced as a replacement of the nearly equivalent Pribylograptus leptotheca Biozone, because the latter is a less common and less easily identified index taxon. Detailed range charts of 385 species of planktic graptolites based on in situ records from 88 localities and section logs in the offshore Silurian succession of the Prague Synform provide a solid data source for the proposed biozonal scheme and subsequent study of regional graptolite faunal dynamics, traced by means of species richness per biozone, mean standing diversity, time-normalized Van Valen's metrics, and FADs/LADs score per biozone. The moderate graptolite diversity of the lower Rhuddanian biozones rose to the mid-Aeronian maximum succeeded by stepwise decline forced by five globally recognized extinction events (mid-Aeronian sedgwickii Event, early Sheinwoodian murchisoni Event, mid-Homerian lundgreni Event, early Ludfordian leintwardinensis Event, and mid- Ludfordian kozlowskii Event). Sixth, early Telychian utilis Event is not observed in the Prague Synform as a results of a graptolite barren interval that separates linnaei and turriculatus biozones. Each mass extinction, although succeeded by recovery and adaptive radiation, resulted in a progressive step-wise reduction of graptolite diversity.

  • Název v anglickém jazyce

    Graptolite biostratigraphy and biodiversity dynamics in the Silurian System of the Prague Synform (Barrandian area, Czech Republic)

  • Popis výsledku anglicky

    Forty six graptolite biozones and seven subzones are recognized in the first compilation of high-resolution Silurian graptolite biostratigraphy in central Bohemia. The durations of these graptolite biozones, deduced from correlation with the Geological Time Scale 2020 age model and the global standard graptolite biozonation, range between ca 0.1 and 1.74 Myr. Each biozone is defined as an interval biozone named after the biozone index species, characterized by a typical biozone assemblage and delineated by bounding horizons with the stratigraphically lowest and/or highest occurrences of the respective index taxa. The Petalolithus folium Biozone is introduced as a replacement of the nearly equivalent Pribylograptus leptotheca Biozone, because the latter is a less common and less easily identified index taxon. Detailed range charts of 385 species of planktic graptolites based on in situ records from 88 localities and section logs in the offshore Silurian succession of the Prague Synform provide a solid data source for the proposed biozonal scheme and subsequent study of regional graptolite faunal dynamics, traced by means of species richness per biozone, mean standing diversity, time-normalized Van Valen's metrics, and FADs/LADs score per biozone. The moderate graptolite diversity of the lower Rhuddanian biozones rose to the mid-Aeronian maximum succeeded by stepwise decline forced by five globally recognized extinction events (mid-Aeronian sedgwickii Event, early Sheinwoodian murchisoni Event, mid-Homerian lundgreni Event, early Ludfordian leintwardinensis Event, and mid- Ludfordian kozlowskii Event). Sixth, early Telychian utilis Event is not observed in the Prague Synform as a results of a graptolite barren interval that separates linnaei and turriculatus biozones. Each mass extinction, although succeeded by recovery and adaptive radiation, resulted in a progressive step-wise reduction of graptolite diversity.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10506 - Paleontology

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/GA20-23363S" target="_blank" >GA20-23363S: Biostratigrafie a dynamika pelagických faun siluru pražské pánve v kontextu velkých environmentálních výkyvů a změn</a><br>

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2023

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    Bulletin of Geosciences

  • ISSN

    1214-1119

  • e-ISSN

    1802-8225

  • Svazek periodika

    98

  • Číslo periodika v rámci svazku

    1

  • Stát vydavatele periodika

    CZ - Česká republika

  • Počet stran výsledku

    78

  • Strana od-do

    1-78

  • Kód UT WoS článku

    000970363200001

  • EID výsledku v databázi Scopus

    2-s2.0-85153875404