In search for the Basal Emsian GSSP in the Prague Synform: Mramorka – a possible candidate section

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F24%3A00585468" target="_blank" >RIV/67985831:_____/24:00585468 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.schweizerbart.de/papers/nos/detail/57/103997/In_search_for_the_Basal_Emsian_GSSP_in_the_Prague_Synform_Mramorka_a_possible_candidate_section" target="_blank" >https://www.schweizerbart.de/papers/nos/detail/57/103997/In_search_for_the_Basal_Emsian_GSSP_in_the_Prague_Synform_Mramorka_a_possible_candidate_section</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1127/nos/2024/0795" target="_blank" >10.1127/nos/2024/0795</a>

Jazyk výsledku

angličtina

Název v původním jazyce

In search for the Basal Emsian GSSP in the Prague Synform: Mramorka – a possible candidate section

Popis výsledku v původním jazyce

The present GSSP for the basal Emsian boundary remains among the most problematic issues in the global Paleozoic stratigraphy as it is accented by the International Commission on Stratigraphy (ICS/IUGS). The former traditional Pragian Stage of the Lower Devonian that has been originally based on the Praha Formation in the Prague Synform was thus drastically reduced. Herein is presented a possible candidate section for the prospective basal GSSP redefinition – the Mramorka section near Chýnice, Prague Synform, Czech Republic. It has the typical varied development of the upper part of the Praha Formation including the Bohemian Graptolite Event (BGE), i.e. a prominent lithological marker in the NW flank of the Prague Synform. In order to provide a robust dataset for the rigorous evaluation of the GSSP potential of this candidate section, data from complex multiproxy studies including biostratigraphy, sedimentology, gamma-ray spectrometry, magnetic susceptibility, multi-element geochemistry (INAA, EDXRF), and stable isotopes (δ18O, δ13C) are presented. The boundary criterion is the gracilis Event that is close to the traditional boundary between the Pragian and Emsian stages. The event is characterized by a conodont Latericriodus bilatericrescens gracilis Bultynck, 1985, which widely occurs in NW part of Gondwana. The lowermost entry of the taxon within the Prague Synform has been recorded in the Mramorka section, 145 cm below the BGE interval. The sedimentology of the Mramorka section is characterized by grey nodular calcisiltites largely influenced by ichnofabric, but the BGE interval consists mostly of darker grey, ichnofossil-poor, platy limestones interbedded with black calcareous shales. The data obtained from multiproxy studies in the Mramorka section show a marked change in geochemical proxies within and above the BGE. The values of CGR and elements typical for terrigenous input show relatively higher values below the BGE interval and a gradual decrease above the BGE. The BGE interval is characterized by elevated paleoredox and paleoproductivity proxies. REEN values show mostly the MREE bulge pattern and are linked mainly to terrigenous (especially aeolian) supply. The MS is largely tied to the terrigenous input, but is also influenced by authigenic Fe minerals. δ13C values change markedly above the BGE. The sediments below the BGE interval are considered to record the culminating transgression and strata above the BGE interval the highstand. The BGE interval itself records the maximum flooding. If present, the BGE interval close above the gracilis Event may serve an independent marker for approximation of the prospective GSSP boundary.

Název v anglickém jazyce

In search for the Basal Emsian GSSP in the Prague Synform: Mramorka – a possible candidate section

Popis výsledku anglicky

The present GSSP for the basal Emsian boundary remains among the most problematic issues in the global Paleozoic stratigraphy as it is accented by the International Commission on Stratigraphy (ICS/IUGS). The former traditional Pragian Stage of the Lower Devonian that has been originally based on the Praha Formation in the Prague Synform was thus drastically reduced. Herein is presented a possible candidate section for the prospective basal GSSP redefinition – the Mramorka section near Chýnice, Prague Synform, Czech Republic. It has the typical varied development of the upper part of the Praha Formation including the Bohemian Graptolite Event (BGE), i.e. a prominent lithological marker in the NW flank of the Prague Synform. In order to provide a robust dataset for the rigorous evaluation of the GSSP potential of this candidate section, data from complex multiproxy studies including biostratigraphy, sedimentology, gamma-ray spectrometry, magnetic susceptibility, multi-element geochemistry (INAA, EDXRF), and stable isotopes (δ18O, δ13C) are presented. The boundary criterion is the gracilis Event that is close to the traditional boundary between the Pragian and Emsian stages. The event is characterized by a conodont Latericriodus bilatericrescens gracilis Bultynck, 1985, which widely occurs in NW part of Gondwana. The lowermost entry of the taxon within the Prague Synform has been recorded in the Mramorka section, 145 cm below the BGE interval. The sedimentology of the Mramorka section is characterized by grey nodular calcisiltites largely influenced by ichnofabric, but the BGE interval consists mostly of darker grey, ichnofossil-poor, platy limestones interbedded with black calcareous shales. The data obtained from multiproxy studies in the Mramorka section show a marked change in geochemical proxies within and above the BGE. The values of CGR and elements typical for terrigenous input show relatively higher values below the BGE interval and a gradual decrease above the BGE. The BGE interval is characterized by elevated paleoredox and paleoproductivity proxies. REEN values show mostly the MREE bulge pattern and are linked mainly to terrigenous (especially aeolian) supply. The MS is largely tied to the terrigenous input, but is also influenced by authigenic Fe minerals. δ13C values change markedly above the BGE. The sediments below the BGE interval are considered to record the culminating transgression and strata above the BGE interval the highstand. The BGE interval itself records the maximum flooding. If present, the BGE interval close above the gracilis Event may serve an independent marker for approximation of the prospective GSSP boundary.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/GA21-21829S" target="_blank" >GA21-21829S: Návrh na ustanovení mezinárodního stratotypu GSSP spodní hranice stupně ems v pražské synformě</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

Newsletters on Stratigraphy

ISSN

0078-0421

e-ISSN

—

Svazek periodika

57

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

31

Strana od-do

171-201

Kód UT WoS článku

001157706300001

EID výsledku v databázi Scopus

2-s2.0-85193744117