Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic

The succession of chitinozoans in the East Baltic Přídolí Series was studied in the Ohesaare, Ventspils D-3, Pavilosta and Dubovskoye (Northern-Gusevskaya 2) drill cores. Some differences in biozonal characteristics were observed between the shallower and deeper facies sections. The lower P...

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Main Author: Viiu Nestor
Format: Article
Language:English
Published: Estonian Academy Publishers 2011-11-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_4/earth-2011-4-191-206.pdf
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author Viiu Nestor
author_facet Viiu Nestor
author_sort Viiu Nestor
collection DOAJ
description The succession of chitinozoans in the East Baltic Přídolí Series was studied in the Ohesaare, Ventspils D-3, Pavilosta and Dubovskoye (Northern-Gusevskaya 2) drill cores. Some differences in biozonal characteristics were observed between the shallower and deeper facies sections. The lower Přídoli Eisenackitina kerria–Ancyrochitina tomentosa regional Biozone is described from the Ohesaare (Estonia) and Ventspils and Pavilosta (Latvia) cores and the Fungochitina kosovensis global Biozone from the Dubovskoye (Kaliningrad district) core. The middle Přídolí Salopochitina filifera regional Biozone is represented in all studied sections. The upper Přídolí Anthochitina superba global Biozone is described from the Ventspils core, correlating with the range interval of Margachitina sp. in the Dubovskoye core. In the uppermost Přídolí the Ancyrochitina lemniscata regional Biozone is distinguished for the first time in the Ventspils and Dubovskoye cores. All biozones were correlated with regional strati­graphical units, as well as with conodont and vertebrate biozones in the Ventspils core.
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spelling doaj.art-0a0c25e69f264d92a54ec94683eb56532022-12-22T03:51:43ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47282011-11-0160419120610.3176/earth.2011.4.01Chitinozoan biostratigraphy of the Přídolí Series of the East BalticViiu NestorThe succession of chitinozoans in the East Baltic Přídolí Series was studied in the Ohesaare, Ventspils D-3, Pavilosta and Dubovskoye (Northern-Gusevskaya 2) drill cores. Some differences in biozonal characteristics were observed between the shallower and deeper facies sections. The lower Přídoli Eisenackitina kerria–Ancyrochitina tomentosa regional Biozone is described from the Ohesaare (Estonia) and Ventspils and Pavilosta (Latvia) cores and the Fungochitina kosovensis global Biozone from the Dubovskoye (Kaliningrad district) core. The middle Přídolí Salopochitina filifera regional Biozone is represented in all studied sections. The upper Přídolí Anthochitina superba global Biozone is described from the Ventspils core, correlating with the range interval of Margachitina sp. in the Dubovskoye core. In the uppermost Přídolí the Ancyrochitina lemniscata regional Biozone is distinguished for the first time in the Ventspils and Dubovskoye cores. All biozones were correlated with regional strati­graphical units, as well as with conodont and vertebrate biozones in the Ventspils core.http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_4/earth-2011-4-191-206.pdfSilurianPřídolíEast Balticchitinozoans.
spellingShingle Viiu Nestor
Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic
Estonian Journal of Earth Sciences
Silurian
Přídolí
East Baltic
chitinozoans.
title Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic
title_full Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic
title_fullStr Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic
title_full_unstemmed Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic
title_short Chitinozoan biostratigraphy of the Přídolí Series of the East Baltic
title_sort chitinozoan biostratigraphy of the pridoli series of the east baltic
topic Silurian
Přídolí
East Baltic
chitinozoans.
url http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_4/earth-2011-4-191-206.pdf
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