J 2017

Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic)

WEINEROVÁ, Hedvika, Karel HRON, Ondřej BÁBEK, Daniel ŠIMÍČEK, Jindřich HLADIL et. al.

Basic information

Original name

Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic)

Authors

WEINEROVÁ, Hedvika (203 Czech Republic, belonging to the institution), Karel HRON (203 Czech Republic), Ondřej BÁBEK (203 Czech Republic), Daniel ŠIMÍČEK (203 Czech Republic) and Jindřich HLADIL (203 Czech Republic)

Edition

Sedimentary Geology, Amsterdam, Elsevier Science, 2017, 0037-0738

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

Netherlands

Confidentiality degree

není předmětem státního či obchodního tajemství

References:

Impact factor

Impact factor: 2.575

RIV identification code

RIV/00216224:14310/17:00095376

Organization unit

Faculty of Science

UT WoS

000401597200004

Keywords in English

compositional analysis; carbonate petrography; multivariate statistics; log-ratio coordinates; Prague Basin; Lower Devonian

Tags

Tags

International impact, Reviewed
Změněno: 21/1/2020 09:38, Mgr. Marie Šípková, DiS.

Abstract

V originále

Quantitative allochem compositional trends across the Lochkovian-Pragian boundary Event were examined at three sections recording the proximal to more distal carbonate ramp environment of the Prague Basin. Multivariate statistical methods (principal component analysis, correspondence analysis, cluster analysis) of point-counted thin section data were used to reconstruct facies stacking patterns and sea-level history. Both the closed-nature allochem percentages and their centred log-ratio (clr) coordinates were used. Both these approaches allow for distinguishing of lowstand, transgressive and highstand system tracts within the Praha Formation, which show gradual transition from crinoid-dominated fades deposited above the storm wave base to dacryoconarid-dominated facies of deep-water environment below the storm wave base. Quantitative compositional data also indicate progradative-retrogradative trends in the macrolithologically monotonous shallow-water succession and enable its stratigraphic correlation with successions from deeper-water environments. Generally, the stratigraphic trends of the clr data are more sensitive to subtle changes in allochem composition in comparison to the results based on raw data. A heterozoan-dominated allochem association in shallow-water environments of the Praha Formation supports the carbonate ramp environment assumed by previous authors.

Links

GA14-18183S, research and development project
Name: Sekvenční stratigrafie devonských bioeventů - výkyvy mořské hladiny na přechodu od klimatického režimu greenhouse k icehouse
Investor: Czech Science Foundation