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