Biostratigraphy of the Lower/Middle Tournaisian (Mississippian)
limestones in the Moravian Karst: preliminary results

a 2013

Biostratigraphy of the Lower/Middle Tournaisian (Mississippian) limestones in the Moravian Karst: preliminary results

KUMPAN, Tomáš, Jiří KALVODA a Štěpán RAK

Základní údaje

Originální název

Biostratigraphy of the Lower/Middle Tournaisian (Mississippian) limestones in the Moravian Karst: preliminary results

Autoři

KUMPAN, Tomáš (203 Česká republika, garant, domácí), Jiří KALVODA (203 Česká republika, domácí) a Štěpán RAK (203 Česká republika)

Vydání

Grzybowski Foundation Special Publication No. 19. Abstarct volume of 14th Czech - Slovak - Polish Palaeontological Conference and 9th Polish Micropalaeontological Workshop, 2013 Kraków (eds. Bak, M.; Kowal-Kasprzyk, J.; Waskowska, A.; Kaminski, M.), 2013

Další údaje

Jazyk

angličtina

Typ výsledku

Konferenční abstrakt

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Polsko

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/13:00066984

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-83-88927-34-8

Klíčová slova anglicky

Carboniferous;micropaleontology;conodonts;foraminifers;trilobites;brachiopods;ichthyoliths

Změněno: 10. 3. 2014 15:46, Mgr. Tomáš Kumpan, Ph.D.

Anotace

V originále

In the southern part of the Moravian Karst (NE of Brno, Czech Republic) are well exposed Upper Devonian to Mississippian sequences with excellent sedimentary record through the stage boundaries. The Frasnian/Famennian (Hladil et al. 1991), Famennian/Tournaisian (Kumpan et al. 2013) and Tournaisian/Viseán boundaries (Kalvoda et al. 2010) were determined both biostratigraphically and eventostratigraphically. Preliminary results of the recent biostratigraphic research on the Lower/Middle Tournaisan Substage boundary in the sections Lesní lom, Anaklety and Říčka Valley are presented herein. Joint presence of conodonts and foraminifers gives a good opportunity for precise correlation between the deep to shallow water successions in the Western and Eastern Europe. Ichthyoliths, trilobites, brachiopods and other fauna is also present. Complete succession of the Early Turnaisian conodont zones (from the sulcata up to the hassi Zone) was previously documented above the the well preserved Famennian beds in the Lesní lom Quarry, Brno-Líšeň (Kumpan et al. 2013). Abundant conodonts of the upper part of the hassi and sandbergi Zone and foraminiferal association of the foram. zone Prochernyshinella disputabilis (Kulagina 2013) were studied recently. Abundant conodonts of the quadruplicata Zone were documented 400 m SE to the Bělka Mill in the Říčka Valley together with foraminifers of the top of P. disputabilis or the lower part of P. tchernyshinensis Zone. In the Anaklety sections are Lower to Middle Tournaisian limestones preserved with hiatus above the Upper Famennian (Rutová 2009). Foraminiferal association typical for the Palaeospiroplectammina tchernyshinensis Zone (Poty et al. 2006, Kulagina 2013) were found with conodonts of the M. Tournaisian base (crenulata conodont Zone). Trilobite association described from this level consits of very specific forms [Liobole (Sulcubole) aff. Castroi, Linguaphillipsia cracoviensis, Liobole (Panibole) sp., Piltonia krasensis] which are known from the Moravian Karst for the first time (except Piltonia). Also free small-sized brachiopod valves of the suborder Chonetidina (Rugosochonetes?), Productidina and Spiriferida, lingulids and chondrichthyan ichthyolits (e.g. families Phoebodontidae and Protacrodontidae) are present. Acknowledgements: Supported by the Czech Science Foundation (grant P210/11/1891).

Návaznosti

GAP210/11/1891, projekt VaV

Název: Hranice devonu a karbonu v Evropě - multidisciplinární přístup

Investor: Grantová agentura ČR, Hranice devonu a karbonu v Evropě - multidisciplinární přístup

Citovat

KUMPAN, Tomáš, Jiří KALVODA a Štěpán RAK. Biostratigraphy of the Lower/Middle Tournaisian (Mississippian) limestones in the Moravian Karst: preliminary results. In Grzybowski Foundation Special Publication No. 19. Abstarct volume of 14th Czech - Slovak - Polish Palaeontological Conference and 9th Polish Micropalaeontological Workshop, 2013 Kraków (eds. Bak, M.; Kowal-Kasprzyk, J.; Waskowska, A.; Kaminski, M.). 2013. ISBN 978-83-88927-34-8.

@proceedings{1169144,
   author = {Kumpan, Tomáš and Kalvoda, Jiří and Rak, Štěpán},
   booktitle = {Grzybowski Foundation Special Publication No. 19. Abstarct volume of 14th Czech - Slovak - Polish Palaeontological Conference and 9th Polish Micropalaeontological Workshop, 2013 Kraków (eds. Bak, M.; Kowal-Kasprzyk, J.; Waskowska, A.; Kaminski, M.)},
   keywords = {Carboniferous;micropaleontology;conodonts;foraminifers;trilobites;brachiopods;ichthyoliths},
   language = {eng},
   isbn = {978-83-88927-34-8},
   title = {Biostratigraphy of the Lower/Middle Tournaisian (Mississippian) limestones in the Moravian Karst: preliminary results},
   year = {2013}
}

TY  - CONF
ID  - 1169144
AU  - Kumpan, Tomáš - Kalvoda, Jiří - Rak, Štěpán
PY  - 2013
TI  - Biostratigraphy of the Lower/Middle Tournaisian (Mississippian) limestones in the Moravian Karst: preliminary results
SN  - 9788388927348
KW  - Carboniferous;micropaleontology;conodonts;foraminifers;trilobites;brachiopods;ichthyoliths
N2  - In the southern part of the Moravian Karst (NE of Brno, Czech Republic) are well exposed Upper Devonian to Mississippian sequences with excellent sedimentary record through the stage boundaries. The Frasnian/Famennian (Hladil et al. 1991), Famennian/Tournaisian (Kumpan et al. 2013) and Tournaisian/Viseán boundaries (Kalvoda et al. 2010) were determined both biostratigraphically and eventostratigraphically. Preliminary results of the recent biostratigraphic research on the Lower/Middle Tournaisan Substage boundary in the sections Lesní lom, Anaklety and Říčka Valley are presented herein. Joint presence of conodonts and foraminifers gives a good opportunity for precise correlation between the deep to shallow water successions in the Western and Eastern Europe. Ichthyoliths, trilobites, brachiopods and other fauna is also present. Complete succession of the Early Turnaisian conodont zones (from the sulcata up to the hassi Zone) was previously documented above the the well preserved Famennian beds in the Lesní lom Quarry, Brno-Líšeň (Kumpan et al. 2013). Abundant conodonts of the upper part of the hassi and sandbergi Zone and foraminiferal association of the foram. zone Prochernyshinella disputabilis (Kulagina 2013) were studied recently. Abundant conodonts of the quadruplicata Zone were documented 400 m SE to the Bělka Mill in the Říčka Valley together with foraminifers of the top of P. disputabilis or the lower part of P. tchernyshinensis Zone. In the Anaklety sections are Lower to Middle Tournaisian limestones preserved with hiatus above the Upper Famennian (Rutová 2009). Foraminiferal association typical for the Palaeospiroplectammina tchernyshinensis Zone (Poty et al. 2006, Kulagina 2013) were found with conodonts of the M. Tournaisian base (crenulata conodont Zone). Trilobite association described from this level consits of very specific forms [Liobole (Sulcubole) aff. Castroi, Linguaphillipsia cracoviensis, Liobole (Panibole) sp., Piltonia krasensis] which are known from the Moravian Karst for the first time (except Piltonia). Also free small-sized brachiopod valves of the suborder Chonetidina (Rugosochonetes?), Productidina and Spiriferida, lingulids and chondrichthyan ichthyolits (e.g. families Phoebodontidae and Protacrodontidae) are present. Acknowledgements: Supported by the Czech Science Foundation (grant P210/11/1891).
ER  -

KUMPAN, Tomáš, Jiří KALVODA a Štěpán RAK. Biostratigraphy of the Lower/Middle Tournaisian (Mississippian) limestones in the Moravian Karst: preliminary results. In \textit{Grzybowski Foundation Special Publication No. 19. Abstarct volume of 14th Czech - Slovak - Polish Palaeontological Conference and 9th Polish Micropalaeontological Workshop, 2013 Kraków (eds. Bak, M.; Kowal-Kasprzyk, J.; Waskowska, A.; Kaminski, M.)}. 2013. ISBN~978-83-88927-34-8.

Podrobný výpis o publikaci