Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia

Conodonts from the type region of the Oandu Regional Stage (Katian, Upper Ordovician) in NE Estonia were studied. Here, the lower boundary of the stage corresponds to a discontinuity surface at the base of the Hirmuse Formation and, in conodont succession, is marked by the disappearance of Semiacont...

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Main Author: Peep Männik
Format: Article
Language:English
Published: Estonian Academy Publishers 2017-02-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_1/earth-2017-1-1-12.pdf
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spelling doaj-ba91cb2c4bc3489da6ae84abb3b8da112020-11-25T02:04:22ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47281736-75572017-02-0166111210.3176/earth.2017.0210.3176/earth.2017.02Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE EstoniaPeep Männik0Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; peep.mannik@ttu.eeConodonts from the type region of the Oandu Regional Stage (Katian, Upper Ordovician) in NE Estonia were studied. Here, the lower boundary of the stage corresponds to a discontinuity surface at the base of the Hirmuse Formation and, in conodont succession, is marked by the disappearance of Semiacontiodus sp. and Besselodus? sp. The most characteristic taxa of the Oandu Stage are Phragmodus undatus, Icriodella cf. superba and Plectodina sp., which are rare or missing below and above this stratigraphic interval in Estonia. The comparison of conodont faunas from North and South Estonia suggests that the strata in North Estonia correspond to the upper part of the Oandu Stage only as identified in sections in South Estonia. However, the position of the lower boundary of the stage in South Estonia is highly problematic. The boundary between the Amorphognathus tvaerensis and A. superbus conodont zones in Estonia lies within the (upper) Oandu Stage.http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_1/earth-2017-1-1-12.pdfconodontsbiostratigraphyOandu StageKatianUpper OrdovicianEstonia.
collection DOAJ
language English
format Article
sources DOAJ
author Peep Männik
spellingShingle Peep Männik
Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia
Estonian Journal of Earth Sciences
conodonts
biostratigraphy
Oandu Stage
Katian
Upper Ordovician
Estonia.
author_facet Peep Männik
author_sort Peep Männik
title Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia
title_short Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia
title_full Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia
title_fullStr Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia
title_full_unstemmed Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia
title_sort conodont biostratigraphy of the oandu stage (katian, upper ordovician) in ne estonia
publisher Estonian Academy Publishers
series Estonian Journal of Earth Sciences
issn 1736-4728
1736-7557
publishDate 2017-02-01
description Conodonts from the type region of the Oandu Regional Stage (Katian, Upper Ordovician) in NE Estonia were studied. Here, the lower boundary of the stage corresponds to a discontinuity surface at the base of the Hirmuse Formation and, in conodont succession, is marked by the disappearance of Semiacontiodus sp. and Besselodus? sp. The most characteristic taxa of the Oandu Stage are Phragmodus undatus, Icriodella cf. superba and Plectodina sp., which are rare or missing below and above this stratigraphic interval in Estonia. The comparison of conodont faunas from North and South Estonia suggests that the strata in North Estonia correspond to the upper part of the Oandu Stage only as identified in sections in South Estonia. However, the position of the lower boundary of the stage in South Estonia is highly problematic. The boundary between the Amorphognathus tvaerensis and A. superbus conodont zones in Estonia lies within the (upper) Oandu Stage.
topic conodonts
biostratigraphy
Oandu Stage
Katian
Upper Ordovician
Estonia.
url http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_1/earth-2017-1-1-12.pdf
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