Vše

Co hledáte?

Vše
Projekty
Výsledky výzkumu
Subjekty

Rychlé hledání

  • Projekty podpořené TA ČR
  • Významné projekty
  • Projekty s nejvyšší státní podporou
  • Aktuálně běžící projekty

Chytré vyhledávání

  • Takto najdu konkrétní +slovo
  • Takto z výsledků -slovo zcela vynechám
  • “Takto můžu najít celou frázi”

Belemnites and calcareous nannoplankton: Proxy tools for recognising of cryptic Jurassic geological history of Central Europe

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F23%3A00559533" target="_blank" >RIV/67985831:_____/23:00559533 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/00216208:11310/23:10445729

  • Výsledek na webu

    <a href="https://link.springer.com/article/10.1007/s12549-022-00538-y" target="_blank" >https://link.springer.com/article/10.1007/s12549-022-00538-y</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s12549-022-00538-y" target="_blank" >10.1007/s12549-022-00538-y</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Belemnites and calcareous nannoplankton: Proxy tools for recognising of cryptic Jurassic geological history of Central Europe

  • Popis výsledku v původním jazyce

    Belemnites and calcareous nannoplankton (which are both stratigraphically and palaeoecologically important groups of organisms) have been used as crucial evidence for exploring an extended timespan of Jurassic sedimentation in the northern part of the Bohemian Massif. Tectonically and fragmentarily preserved Jurassic strata along the Lausitian Fault have long been considered exclusively as belonging to the Callovian through the Kimmeridgian. Based on a systematic revision of older collections, new sediment sampling and analysing data, the stratigraphic range of Jurassic sedimentation in the northern part of the Bohemian Massif has been extended, at least from the Bajocian until the Tithonian. Belemnite taxa are represented by six species and two taxa identified as Megateuthis cf. M. elliptica and Cylindroteuthis cf. C. puzosiana (five genera belonging to four families) document a stratigraphic range from the Bajocian (Megateuthis suevica and Megateuthis cf. M. elliptica) through the Kimmeridgian. Additionally, calcareous nannofossils do not contradict the Bajocian–Kimmeridgian while also proving the Tithonian age. Moreover, belemnites clearly show the prevailing Tethyan (Belemnopsis fauna) but also Boreal (Cylindroteuthis cf. C. puzosiana) provenance. Recorded fossils reveal a longer time span of sedimentation than previouslyknown (starting at least in the Bajocian and terminating in the Tithonian), suggesting the existence of a significantly larger sedimentary basins that had been eroded prior to the Cenomanian transgression event (Upper Cretaceous).

  • Název v anglickém jazyce

    Belemnites and calcareous nannoplankton: Proxy tools for recognising of cryptic Jurassic geological history of Central Europe

  • Popis výsledku anglicky

    Belemnites and calcareous nannoplankton (which are both stratigraphically and palaeoecologically important groups of organisms) have been used as crucial evidence for exploring an extended timespan of Jurassic sedimentation in the northern part of the Bohemian Massif. Tectonically and fragmentarily preserved Jurassic strata along the Lausitian Fault have long been considered exclusively as belonging to the Callovian through the Kimmeridgian. Based on a systematic revision of older collections, new sediment sampling and analysing data, the stratigraphic range of Jurassic sedimentation in the northern part of the Bohemian Massif has been extended, at least from the Bajocian until the Tithonian. Belemnite taxa are represented by six species and two taxa identified as Megateuthis cf. M. elliptica and Cylindroteuthis cf. C. puzosiana (five genera belonging to four families) document a stratigraphic range from the Bajocian (Megateuthis suevica and Megateuthis cf. M. elliptica) through the Kimmeridgian. Additionally, calcareous nannofossils do not contradict the Bajocian–Kimmeridgian while also proving the Tithonian age. Moreover, belemnites clearly show the prevailing Tethyan (Belemnopsis fauna) but also Boreal (Cylindroteuthis cf. C. puzosiana) provenance. Recorded fossils reveal a longer time span of sedimentation than previouslyknown (starting at least in the Bajocian and terminating in the Tithonian), suggesting the existence of a significantly larger sedimentary basins that had been eroded prior to the Cenomanian transgression event (Upper Cretaceous).

Klasifikace

  • Druh

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

  • CEP obor

  • OECD FORD obor

    10506 - Paleontology

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • 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

    Palaeobiodiversity and Palaeoenvironments

  • ISSN

    1867-1594

  • e-ISSN

    1867-1608

  • Svazek periodika

    103

  • Číslo periodika v rámci svazku

    2

  • Stát vydavatele periodika

    DE - Spolková republika Německo

  • Počet stran výsledku

    23

  • Strana od-do

    303-325

  • Kód UT WoS článku

    000820943700001

  • EID výsledku v databázi Scopus

    2-s2.0-85133546139