Conodont dating of some Telychian (Silurian) sections in Estonia

Several Telychian–Sheinwoodian strata exposed in Estonia are precisely dated using conodont biostratigraphy. The beds in the Valgu-1 section correspond to the uppermost Distomodus staurognathoides and Pterospathodus eopennatus ssp. n. 1 zones. In the Valgu-2 and Valgu-3 sections only the P. eopennat...

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Main Author: Männik, Peep
Format: Article
Language:English
Published: Estonian Academy Publishers 2008-09-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://eap.ee/public/Estonian_Journal_of_Earth_Sciences/2008/issue_3/earth-2008-3-156-169.pdf
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spelling doaj-053046141171445981be9c0f1245484a2020-11-24T22:13:55ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47282008-09-01573156169Conodont dating of some Telychian (Silurian) sections in EstoniaMännik, PeepSeveral Telychian–Sheinwoodian strata exposed in Estonia are precisely dated using conodont biostratigraphy. The beds in the Valgu-1 section correspond to the uppermost Distomodus staurognathoides and Pterospathodus eopennatus ssp. n. 1 zones. In the Valgu-2 and Valgu-3 sections only the P. eopennatus ssp. n. 1 Zone is exposed. The strata in the Velise-Kõrgekalda section correspond to the Lower subzone of the P. amorphognathoides angulatus Zone. Marlstones in the Jädivere section are assigned to the P. a. lennarti Zone. In the Avaste section part of the P. a. lithuanicus Zone is exposed. On the Saastna Peninsula two stratigraphical intervals, the lower corresponding to the Upper subzone of the P. a. amorphognathoides Zone and the upper to the Upper Kockelella ranuliformis Zone, crop out along the shoreline. In Saastna the exposed strata are separated by a covered interval corresponding to five conodont zones, from the Lower Pseudooneotodus bicornis Zone to the Lower K. ranuliformis Zone.http://eap.ee/public/Estonian_Journal_of_Earth_Sciences/2008/issue_3/earth-2008-3-156-169.pdfconodontsstratigraphyTelychianSheinwoodianSilurianEstonia
collection DOAJ
language English
format Article
sources DOAJ
author Männik, Peep
spellingShingle Männik, Peep
Conodont dating of some Telychian (Silurian) sections in Estonia
Estonian Journal of Earth Sciences
conodonts
stratigraphy
Telychian
Sheinwoodian
Silurian
Estonia
author_facet Männik, Peep
author_sort Männik, Peep
title Conodont dating of some Telychian (Silurian) sections in Estonia
title_short Conodont dating of some Telychian (Silurian) sections in Estonia
title_full Conodont dating of some Telychian (Silurian) sections in Estonia
title_fullStr Conodont dating of some Telychian (Silurian) sections in Estonia
title_full_unstemmed Conodont dating of some Telychian (Silurian) sections in Estonia
title_sort conodont dating of some telychian (silurian) sections in estonia
publisher Estonian Academy Publishers
series Estonian Journal of Earth Sciences
issn 1736-4728
publishDate 2008-09-01
description Several Telychian–Sheinwoodian strata exposed in Estonia are precisely dated using conodont biostratigraphy. The beds in the Valgu-1 section correspond to the uppermost Distomodus staurognathoides and Pterospathodus eopennatus ssp. n. 1 zones. In the Valgu-2 and Valgu-3 sections only the P. eopennatus ssp. n. 1 Zone is exposed. The strata in the Velise-Kõrgekalda section correspond to the Lower subzone of the P. amorphognathoides angulatus Zone. Marlstones in the Jädivere section are assigned to the P. a. lennarti Zone. In the Avaste section part of the P. a. lithuanicus Zone is exposed. On the Saastna Peninsula two stratigraphical intervals, the lower corresponding to the Upper subzone of the P. a. amorphognathoides Zone and the upper to the Upper Kockelella ranuliformis Zone, crop out along the shoreline. In Saastna the exposed strata are separated by a covered interval corresponding to five conodont zones, from the Lower Pseudooneotodus bicornis Zone to the Lower K. ranuliformis Zone.
topic conodonts
stratigraphy
Telychian
Sheinwoodian
Silurian
Estonia
url http://eap.ee/public/Estonian_Journal_of_Earth_Sciences/2008/issue_3/earth-2008-3-156-169.pdf
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