NEHYBA, Slavomír, Pavla PETROVÁ-TOMANOVÁ and Kamil ZAGORŠEK. Sedimentological and palaeocological records of the evolution of the south-western part of the Carpathian Foredeep (Czech Republic) during the Early Badenian. Geological Quarterly. Warszawa, 2008, vol. 52, No 1, p. 45-60. ISSN 1641-7291.
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Basic information
Original name Sedimentological and palaeocological records of the evolution of the south-western part of the Carpathian Foredeep (Czech Republic) during the Early Badenian
Name in Czech Sedimentologický a palaeocologický záznam vývoje jihozápadní části karpatské předhlubně (Česká republika) během spodního badenu
Authors NEHYBA, Slavomír (203 Czech Republic, guarantor), Pavla PETROVÁ-TOMANOVÁ (203 Czech Republic) and Kamil ZAGORŠEK (203 Czech Republic).
Edition Geological Quarterly, Warszawa, 2008, 1641-7291.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Poland
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 0.892
RIV identification code RIV/00216224:14310/08:00025887
Organization unit Faculty of Science
UT WoS 000254925500004
Keywords in English Carpathian Foredeep- Early Badenian- sedimentology- palaeoecology- depositional environment- foraminifers- bryozoans
Tags International impact, Reviewed
Changed by Changed by: prof. RNDr. Slavomír Nehyba, Dr., učo 2710. Changed: 2/7/2009 08:24.
Abstract
The depositional environment of southern part of the Carpathian Foredeep in the Czech Republic was studied in two boreholes using sedimentological and palaeontological methods. Eight lithofacies were recognised within the studied cores of Early Badenian deposits forming two facies associations i.e. deposits of coarse grained Gilbert delta and offshore deposits. Assemblages of foraminifers document age of the Early Badenian (Middle Miocene). Two types of assemblages were recognised: 1. primary taphocoenoses showing original environment of sedimentation, i. e. environment of deeper sublittoral (circalittoral) with low to normal oxygen bottom conditions taking in deep water euryoxibiont foraminifers, numerous planktonic foraminifers, agglutinated ones and mixed assemblages of deep and shallow water foraminifers, 2. secondary taphocoenoses of shallower sublittoral (infralittoral) redeposited into the basin by gravity currents. These assemblages contain shallow water foraminifers coupled with numerous highly diversified bryozoans.
Abstract (in Czech)
The depositional environment of southern part of the Carpathian Foredeep in the Czech Republic was studied in two boreholes using sedimentological and palaeontological methods. Eight lithofacies were recognised within the studied cores of Early Badenian deposits forming two facies associations i.e. deposits of coarse grained Gilbert delta and offshore deposits. Assemblages of foraminifers document age of the Early Badenian (Middle Miocene). Two types of assemblages were recognised: 1. primary taphocoenoses showing original environment of sedimentation, i. e. environment of deeper sublittoral (circalittoral) with low to normal oxygen bottom conditions taking in deep water euryoxibiont foraminifers, numerous planktonic foraminifers, agglutinated ones and mixed assemblages of deep and shallow water foraminifers, 2. secondary taphocoenoses of shallower sublittoral (infralittoral) redeposited into the basin by gravity currents. These assemblages contain shallow water foraminifers coupled with numerous highly diversified bryozoans.
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MSM0021622412, plan (intention)Name: Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální, regionální a lokální úrovni (INCHEMBIOL) (Acronym: INCHEMBIOL)
Investor: Ministry of Education, Youth and Sports of the CR, Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL)
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