The Devonian-Carboniferous boundary in the Moravian Karst
(Czech Republic)

J 2021

The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic)

KUMPAN, Tomáš, Jiří KALVODA, Ondřej BÁBEK, Tomáš Matys GRYGAR, Jiří FRÝDA et. al.

Základní údaje

Originální název

The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic)

Autoři

KUMPAN, Tomáš (203 Česká republika, garant, domácí), Jiří KALVODA (203 Česká republika, domácí), Ondřej BÁBEK (203 Česká republika), Tomáš Matys GRYGAR a Jiří FRÝDA

Vydání

Palaeobiodiversity And Palaeoenvironments, Heidelberg, Springer-Verlag, 2021, 1867-1594

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10506 Paleontology

Stát vydavatele

Německo

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.736

Kód RIV

RIV/00216224:14310/21:00118753

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1007/s12549-019-00409-z

UT WoS

000516244400001

Klíčová slova anglicky

Bohemian Massif; Famennian-Tournaisian boundary; Hangenberg Crisis; Conodonts; Foraminifers; Geochemistry

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 19. 7. 2021 09:46, Mgr. Marie Šípková, DiS.

Anotace

V originále

The continuous and well-accessible Devonian-Carboniferous boundary successions of the Czech Republic are part of the Brunovistulian Unit, which belongs to the Variscan Rhenohercynian Zone of the Bohemian Massif. The well-studied sections, with almost continuous carbonate sedimentation, crop out in the Moravian Karst area and are characterised by carbonate turbidites (Lesní lom) and hemipelagic successions (Křtiny). In the Lesní lom quarry, a complete succession of conodont zones of the Devonian-Carboniferous boundary interval (Upper expansa, praesulcata, costatus-kockeli, kockeli, sulcata/kuehni, bransoni, duplicata zones) was documented in calciturbidites and can be correlated with coeval foraminiferal zones (Quasiendothyra kobeitusana, Quasiendothyra konensis and Tournayellina pseudobeata zones). The Hangenberg Crisis and its three phases can be well recognised both with lithological, biostratigraphical and geochemical approaches in the Lesní lom section. At Křtiny, the nodular limestones yielded conodonts of the Devonian-Carboniferous boundary interval, but missing protognathodid fauna hampered identification of the kockeli Zone. A stratigraphic gap covering the basal part of the sulcata/kuehni Zone or strong condensation can be inferred from the occurrence of the transitional morphotype Si. sulcata-bransoni at the base of this zone. The tested “Montpellier criterion” for the Devonian-Carboniferous boundary redefinition can be used only in the Lesní lom section, where the first Protognathodus kockeli occurs above the regressive Hangenberg Sandstone Event deposits.

Návaznosti

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

KUMPAN, Tomáš, Jiří KALVODA, Ondřej BÁBEK, Tomáš Matys GRYGAR a Jiří FRÝDA. The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic). Palaeobiodiversity And Palaeoenvironments. Heidelberg: Springer-Verlag, 2021, roč. 101, č. 2, s. 473-485. ISSN 1867-1594. Dostupné z: https://dx.doi.org/10.1007/s12549-019-00409-z.

@article{1674559,
   author = {Kumpan, Tomáš and Kalvoda, Jiří and Bábek, Ondřej and Grygar, Tomáš Matys and Frýda, Jiří},
   article_location = {Heidelberg},
   article_number = {2},
   doi = {http://dx.doi.org/10.1007/s12549-019-00409-z},
   keywords = {Bohemian Massif; Famennian-Tournaisian boundary; Hangenberg Crisis; Conodonts; Foraminifers; Geochemistry},
   language = {eng},
   issn = {1867-1594},
   journal = {Palaeobiodiversity And Palaeoenvironments},
   title = {The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic)},
   url = {https://doi.org/10.1007/s12549-019-00409-z},
   volume = {101},
   year = {2021}
}

TY  - JOUR
ID  - 1674559
AU  - Kumpan, Tomáš - Kalvoda, Jiří - Bábek, Ondřej - Grygar, Tomáš Matys - Frýda, Jiří
PY  - 2021
TI  - The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic)
JF  - Palaeobiodiversity And Palaeoenvironments
VL  - 101
IS  - 2
SP  - 473-485
EP  - 473-485
PB  - Springer-Verlag
SN  - 18671594
KW  - Bohemian Massif
KW  - Famennian-Tournaisian boundary
KW  - Hangenberg Crisis
KW  - Conodonts
KW  - Foraminifers
KW  - Geochemistry
UR  - https://doi.org/10.1007/s12549-019-00409-z
L2  - https://doi.org/10.1007/s12549-019-00409-z
N2  - The continuous and well-accessible Devonian-Carboniferous boundary successions of the Czech Republic are part of the Brunovistulian Unit, which belongs to the Variscan Rhenohercynian Zone of the Bohemian Massif. The well-studied sections, with almost continuous carbonate sedimentation, crop out in the Moravian Karst area and are characterised by carbonate turbidites (Lesní lom) and hemipelagic successions (Křtiny). In the Lesní lom quarry, a complete succession of conodont zones of the Devonian-Carboniferous boundary interval (Upper expansa, praesulcata, costatus-kockeli, kockeli, sulcata/kuehni, bransoni, duplicata zones) was documented in calciturbidites and can be correlated with coeval foraminiferal zones (Quasiendothyra kobeitusana, Quasiendothyra konensis and Tournayellina pseudobeata zones). The Hangenberg Crisis and its three phases can be well recognised both with lithological, biostratigraphical and geochemical approaches in the Lesní lom section. At Křtiny, the nodular limestones yielded conodonts of the Devonian-Carboniferous boundary interval, but missing protognathodid fauna hampered identification of the kockeli Zone. A stratigraphic gap covering the basal part of the sulcata/kuehni Zone or strong condensation can be inferred from the occurrence of the transitional morphotype Si. sulcata-bransoni at the base of this zone. The tested “Montpellier criterion” for the Devonian-Carboniferous boundary redefinition can be used only in the Lesní lom section, where the first Protognathodus kockeli occurs above the regressive Hangenberg Sandstone Event deposits.
ER  -

KUMPAN, Tomáš, Jiří KALVODA, Ondřej BÁBEK, Tomáš Matys GRYGAR a Jiří FRÝDA. The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic). \textit{Palaeobiodiversity And Palaeoenvironments}. Heidelberg: Springer-Verlag, 2021, roč.~101, č.~2, s.~473-485. ISSN~1867-1594. Dostupné z: https://dx.doi.org/10.1007/s12549-019-00409-z.

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