Oxygen and carbon stable isotope records of the
Lochkovian-Pragian boundary interval from the Prague Basin
(Lower Devonian, Czech Republic)

J 2020

Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic)

WEINEROVÁ, Hedvika; Ondřej BÁBEK; Ladislav SLAVÍK; Hubert VONHOF; Michael M. JOACHIMSKI et. al.

Základní údaje

Originální název

Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic)

Autoři

WEINEROVÁ, Hedvika; Ondřej BÁBEK; Ladislav SLAVÍK; Hubert VONHOF; Michael M. JOACHIMSKI a Jindřich HLADIL

Vydání

Palaeogeography, Palaeoclimatology, Palaeoecology, Amsterdam, Elsevier, 2020, 0031-0182

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10506 Paleontology

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 3.318

Kód RIV

RIV/00216224:14310/20:00114584

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.1016/j.palaeo.2020.110036

UT WoS

000591245000045

EID Scopus

2-s2.0-85091775844

Klíčová slova anglicky

Palaeozoic; Barrandian area; Climate changes; Conodont apatite; Carbonate; Diagenesis

Štítky

14315010, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 1. 2021 14:38, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Climate changes close to the Lochkovian-Pragian Event are still widely discussed. Carbonate delta 18O and delta 13C and conodont apatite delta 18O from medial to distal carbonate ramp sediments were analysed to provide further stable isotope data from the stratotype area in the Prague Basin. The uppermost Silurian to lower Emsian delta 18O trends are put into an updated conodont biostratigraphy framework. Carbonate delta 18O and delta 13C are discussed in the context of facies-dependent diagenesis. The delta 13C pattern measured from different sections enables the correlation of intervals with development of different facies inside the Prague Basin. Positive delta 13C shifts are often coupled with trends of decreasing computed gamma-ray (CGR) values interpreted as regressions, whereas negative delta 13C shifts commonly coincide with opposite trends in CGR. The Lochkovian-Pragian boundary interval coincided with an increase in carbonate delta 13C and an increase in the delta 18O of conodont apatite and carbonate, which we interpret as consequence of climate cooling. Generally, the Lochkovian was warmer than the Pragian and earliest Emsian.

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

GA19-17435S, projekt VaV

Název: Paleoklimatologický význam paleozoických červených pelagických karbonátů: časově specifické facie nebo produkty mikrobiální aktivity?

Investor: Grantová agentura ČR, Paleoklimatologický význam paleozoických červených pelagických karbonátů: časově specifické facie nebo produkty mikrobiální aktivity?

Citovat

WEINEROVÁ, Hedvika; Ondřej BÁBEK; Ladislav SLAVÍK; Hubert VONHOF; Michael M. JOACHIMSKI a Jindřich HLADIL. Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic). Palaeogeography, Palaeoclimatology, Palaeoecology. Amsterdam: Elsevier, 2020, roč. 560, December 2020, s. 1-17. ISSN 0031-0182. Dostupné z: https://doi.org/10.1016/j.palaeo.2020.110036.

@article{1711136,
   author = {Weinerová, Hedvika and Bábek, Ondřej and Slavík, Ladislav and Vonhof, Hubert and Joachimski, Michael M. and Hladil, Jindřich},
   article_location = {Amsterdam},
   article_number = {December 2020},
   doi = {https://doi.org/10.1016/j.palaeo.2020.110036},
   keywords = {Palaeozoic; Barrandian area; Climate changes; Conodont apatite; Carbonate; Diagenesis},
   language = {eng},
   issn = {0031-0182},
   journal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
   title = {Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic)},
   url = {https://doi.org/10.1016/j.palaeo.2020.110036},
   volume = {560},
   year = {2020}
}

TY  - JOUR
ID  - 1711136
AU  - Weinerová, Hedvika - Bábek, Ondřej - Slavík, Ladislav - Vonhof, Hubert - Joachimski, Michael M. - Hladil, Jindřich
PY  - 2020
TI  - Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic)
JF  - Palaeogeography, Palaeoclimatology, Palaeoecology
VL  - 560
IS  - December 2020
SP  - 1-17
EP  - 1-17
PB  - Elsevier
SN  - 00310182
KW  - Palaeozoic
KW  - Barrandian area
KW  - Climate changes
KW  - Conodont apatite
KW  - Carbonate
KW  - Diagenesis
UR  - https://doi.org/10.1016/j.palaeo.2020.110036
L2  - https://doi.org/10.1016/j.palaeo.2020.110036
N2  - Climate changes close to the Lochkovian-Pragian Event are still widely discussed. Carbonate delta 18O and delta 13C and conodont apatite delta 18O from medial to distal carbonate ramp sediments were analysed to provide further stable isotope data from the stratotype area in the Prague Basin. The uppermost Silurian to lower Emsian delta 18O trends are put into an updated conodont biostratigraphy framework. Carbonate delta 18O and delta 13C are discussed in the context of facies-dependent diagenesis. The delta 13C pattern measured from different sections enables the correlation of intervals with development of different facies inside the Prague Basin. Positive delta 13C shifts are often coupled with trends of decreasing computed gamma-ray (CGR) values interpreted as regressions, whereas negative delta 13C shifts commonly coincide with opposite trends in CGR. The Lochkovian-Pragian boundary interval coincided with an increase in carbonate delta 13C and an increase in the delta 18O of conodont apatite and carbonate, which we interpret as consequence of climate cooling. Generally, the Lochkovian was warmer than the Pragian and earliest Emsian.
ER  -

WEINEROVÁ, Hedvika; Ondřej BÁBEK; Ladislav SLAVÍK; Hubert VONHOF; Michael M. JOACHIMSKI a Jindřich HLADIL. Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic). \textit{Palaeogeography, Palaeoclimatology, Palaeoecology}. Amsterdam: Elsevier, 2020, roč.~560, December 2020, s.~1-17. ISSN~0031-0182. Dostupné z: https://doi.org/10.1016/j.palaeo.2020.110036.

Přehled o publikaci