The oldest rocks of the Holy Cross Mountains, Poland – biostratigraphy of the Cambrian Czarna Shale Formation in the vicinity of Kotuszów

Szczepanik, Z.; Żylińska, A.

doi:10.1515/agp-2016-0013

Artykuł - szczegóły

Tytuł artykułu

The oldest rocks of the Holy Cross Mountains, Poland – biostratigraphy of the Cambrian Czarna Shale Formation in the vicinity of Kotuszów

Autorzy

Szczepanik Z. , Żylińska A.

Treść / Zawartość

Pełne teksty:

AGP_3_2016_Szczepanik_Zylinska_The_oldest.pdf

Pobierz

Identyfikatory

DOI

10.1515/agp-2016-0013

Warianty tytułu

Języki publikacji

Abstrakty

Three lower Cambrian acritarch assemblages recognized in four outcrops in the vicinity of Kotuszów in the southernmost part of the Palaeozoic inlier of the Holy Cross Mountains span a stratigraphic interval from the uppermost part of the Asteridium tornatum–Comasphaeridium velvetum Assemblage Zone to the Skiagia ornata–Fimbriaglomerella membranacea Assemblage Zone (most probably its lower part). According to current views (Moczydłowska and Yin 2012), this interval corresponds to the upper part of the Fortunian and to Stage 2 of the Terreneuvian Series. The strata yielding the oldest assemblage are thus the oldest precisely documented rocks in the Palaeozoic succession of the Holy Cross Mountains, and the oldest Cambrian rocks exposed on the surface in Poland. The current biostratigraphic scheme for the pre-trilobitic part of the Cambrian System in the Holy Cross Mountains should be modified so that it is based on local acritarch interval subzones.

Słowa kluczowe

Cambrian Fortunian Terreneuvian Holy Cross Mountains Kotuszów acritarcha biostratigraphy

kambr fortun terenew Góry Świętokrzyskie Kotuszów Acritarcha biostratygrafia

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2016

Tom

Vol. 66, no. 3

Strony

267--280

Opis fizyczny

Bibliogr. 127 poz., rys., tab., 4 k. tabl.

Twórcy

autor

Szczepanik Z.

zbigniew.szczepanik@pgi.gov.pl

Holy Cross Branch of the Polish Geological Institute-National Research Institute, Zgoda 21, PL-25-953 Kielce, Poland

autor

Żylińska A.

anna.zylinska@uw.edu.pl

Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland

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Uwagi

The research was financed by the statutory funds of the Polish Geological Institute – National Research Institute (subject no. 61.2401.1302.00.0 – Cambrian and Ordovician acritarchs from the Holy Cross Mountains and their significance for current geological research; ZS) and by the Institute of Geology, Faculty of Geology, University of Warsaw (individual grant to AŻ). The final version of the paper greatly benefited from the constructive reviews by Gerd Geyer (Wūrzburg) and Thomas Servais (Lille), for which we are extremely grateful.

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