The integrated biostratigraphy and palaeoenvironments across the Jurassic-Cretaceous boundary in the Dedina section (eastern Serbian Carpathians)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F24%3A00582421" target="_blank" >RIV/67985831:_____/24:00582421 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61989100:27350/24:10254911

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S0195667123003452?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0195667123003452?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.cretres.2023.105817" target="_blank" >10.1016/j.cretres.2023.105817</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The integrated biostratigraphy and palaeoenvironments across the Jurassic-Cretaceous boundary in the Dedina section (eastern Serbian Carpathians)

Popis výsledku v původním jazyce

Upper Tithonian to lower Berriasian carbonate sequence of the Getic Nappe System was studied near Golubac using an integrated biostratigraphy approach based on calpionellid, calcareous dinoflagellate, nannofossil, foraminifer, and palynomorph record. Calpionellids allowed subdivision of the section to standard calpionellid zones including the Colomi and Alpina subzones on the TithonianeBerriasian transition. Nannofossil Nannoconus wintereri proves the presence of the NC0 Zone. Foraminifer fauna on the TithonianeBerriasian transition contain zonal marker Globospirillina neocomiana and some other potential stratigraphic markers, whose range and taxonomy have to be fixed yet. Poor palynomorph spectra consist of long-ranging Lower-Cretaceous spores and pollen, and a few dinoflagellate cysts known from the Berriasian. Integrated biostratigraphy of the TithonianeBerriasian oligotrophic openmarine carbonate facies of the Dedina section contributes to the stratigraphic framework necessary for the definition of the Berriasian Global Boundary Stratotype Section and Point.

Název v anglickém jazyce

The integrated biostratigraphy and palaeoenvironments across the Jurassic-Cretaceous boundary in the Dedina section (eastern Serbian Carpathians)

Popis výsledku anglicky

Upper Tithonian to lower Berriasian carbonate sequence of the Getic Nappe System was studied near Golubac using an integrated biostratigraphy approach based on calpionellid, calcareous dinoflagellate, nannofossil, foraminifer, and palynomorph record. Calpionellids allowed subdivision of the section to standard calpionellid zones including the Colomi and Alpina subzones on the TithonianeBerriasian transition. Nannofossil Nannoconus wintereri proves the presence of the NC0 Zone. Foraminifer fauna on the TithonianeBerriasian transition contain zonal marker Globospirillina neocomiana and some other potential stratigraphic markers, whose range and taxonomy have to be fixed yet. Poor palynomorph spectra consist of long-ranging Lower-Cretaceous spores and pollen, and a few dinoflagellate cysts known from the Berriasian. Integrated biostratigraphy of the TithonianeBerriasian oligotrophic openmarine carbonate facies of the Dedina section contributes to the stratigraphic framework necessary for the definition of the Berriasian Global Boundary Stratotype Section and Point.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

<a href="/cs/project/GA20-10035S" target="_blank" >GA20-10035S: Průlomové instrumentální metody v globálních korelacích s vysokou rozlišovací schopností na hranici jura-křída</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Cretaceous Research

ISSN

0195-6671

e-ISSN

1095-998X

Svazek periodika

158

Číslo periodika v rámci svazku

June

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

26

Strana od-do

105817

Kód UT WoS článku

001179233800001

EID výsledku v databázi Scopus

2-s2.0-85183997900