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

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.

Základní údaje

Originální název

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

Autoři

WEINEROVÁ, Hedvika (203 Česká republika, domácí), Karel HRON (203 Česká republika), Ondřej BÁBEK (203 Česká republika), Daniel ŠIMÍČEK (203 Česká republika) a Jindřich HLADIL (203 Česká republika)

Vydání

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

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

Full Text

Impakt faktor

Impact factor: 2.575

Kód RIV

RIV/00216224:14310/17:00095376

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.sedgeo.2017.04.002

UT WoS

000401597200004

Klíčová slova anglicky

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

Štítky

NZ, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 21. 1. 2020 09:38, Mgr. Marie Šípková, DiS.

Anotace

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.

Návaznosti

GA14-18183S, projekt VaV

Název: Sekvenční stratigrafie devonských bioeventů - výkyvy mořské hladiny na přechodu od klimatického režimu greenhouse k icehouse

Investor: Grantová agentura ČR, Sekvenční stratigrafie devonských bioeventů – výkyvy mořské hladiny na přechodu od klimatického režimu greenhouse k icehouse

Citovat

WEINEROVÁ, Hedvika, Karel HRON, Ondřej BÁBEK, Daniel ŠIMÍČEK a Jindřich HLADIL. Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic). Sedimentary Geology. Amsterdam: Elsevier Science, 2017, roč. 354, June, s. 43-59. ISSN 0037-0738. Dostupné z: https://dx.doi.org/10.1016/j.sedgeo.2017.04.002.

@article{1402930,
   author = {Weinerová, Hedvika and Hron, Karel and Bábek, Ondřej and Šimíček, Daniel and Hladil, Jindřich},
   article_location = {Amsterdam},
   article_number = {June},
   doi = {http://dx.doi.org/10.1016/j.sedgeo.2017.04.002},
   keywords = {compositional analysis; carbonate petrography; multivariate statistics; log-ratio coordinates; Prague Basin; Lower Devonian},
   language = {eng},
   issn = {0037-0738},
   journal = {Sedimentary Geology},
   title = {Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic)},
   url = {http://www.sciencedirect.com/science/article/pii/S0037073817300842?via%3Dihub},
   volume = {354},
   year = {2017}
}

TY  - JOUR
ID  - 1402930
AU  - Weinerová, Hedvika - Hron, Karel - Bábek, Ondřej - Šimíček, Daniel - Hladil, Jindřich
PY  - 2017
TI  - Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic)
JF  - Sedimentary Geology
VL  - 354
IS  - June
SP  - 43-59
EP  - 43-59
PB  - Elsevier Science
SN  - 00370738
KW  - compositional analysis
KW  - carbonate petrography
KW  - multivariate statistics
KW  - log-ratio coordinates
KW  - Prague Basin
KW  - Lower Devonian
UR  - http://www.sciencedirect.com/science/article/pii/S0037073817300842?via%3Dihub
L2  - http://www.sciencedirect.com/science/article/pii/S0037073817300842?via%3Dihub
N2  - 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.
ER  -

WEINEROVÁ, Hedvika, Karel HRON, Ondřej BÁBEK, Daniel ŠIMÍČEK a Jindřich HLADIL. Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic). \textit{Sedimentary Geology}. Amsterdam: Elsevier Science, 2017, roč.~354, June, s.~43-59. ISSN~0037-0738. Dostupné z: https://dx.doi.org/10.1016/j.sedgeo.2017.04.002.

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