Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia

The distribution of conodonts in the Lower–Middle Ordovician beds was studied in five drill core sections of south­eastern Estonia. Ten conodont zones and six subzones, from the Paroistodus proteus Zone to the Eoplacognathus lindstroemi Subzone, were established. The peculiarity of the studied seque...

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Main Author: Viive Viira
Format: Article
Language:English
Published: Estonian Academy Publishers 2011-03-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_1/earth-2011-1-1-21.pdf
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author Viive Viira
author_facet Viive Viira
author_sort Viive Viira
collection DOAJ
description The distribution of conodonts in the Lower–Middle Ordovician beds was studied in five drill core sections of south­eastern Estonia. Ten conodont zones and six subzones, from the Paroistodus proteus Zone to the Eoplacognathus lindstroemi Subzone, were established. The peculiarity of the studied sequence is that the Volkhov Stage is notably poor in conodonts, in particular Baltoniodus species. Large specimens of Drepanodus arcuatus and Protopanderodus rectus, however, are found in great numbers in the uppermost Volkhov and lower Kunda stages. The deeper shelf conodont faunas recognized in SE Estonia (Central Baltoscandian confacies belt) are compared with shallow shelf faunas of northern Estonia (North Estonian confacies belt).
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spelling doaj.art-ade42e3b7d4140c2829d06a07a2ff63f2022-12-21T19:05:53ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47282011-03-0160112110.3176/earth.2011.1.01Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent RussiaViive ViiraThe distribution of conodonts in the Lower–Middle Ordovician beds was studied in five drill core sections of south­eastern Estonia. Ten conodont zones and six subzones, from the Paroistodus proteus Zone to the Eoplacognathus lindstroemi Subzone, were established. The peculiarity of the studied sequence is that the Volkhov Stage is notably poor in conodonts, in particular Baltoniodus species. Large specimens of Drepanodus arcuatus and Protopanderodus rectus, however, are found in great numbers in the uppermost Volkhov and lower Kunda stages. The deeper shelf conodont faunas recognized in SE Estonia (Central Baltoscandian confacies belt) are compared with shallow shelf faunas of northern Estonia (North Estonian confacies belt).http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_1/earth-2011-1-1-21.pdfconodontsbiostratigraphyLower OrdovicianMiddle OrdovicianEstonia.
spellingShingle Viive Viira
Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia
Estonian Journal of Earth Sciences
conodonts
biostratigraphy
Lower Ordovician
Middle Ordovician
Estonia.
title Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia
title_full Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia
title_fullStr Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia
title_full_unstemmed Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia
title_short Lower and Middle Ordovician conodonts from the subsurface of SE Estonia and adjacent Russia
title_sort lower and middle ordovician conodonts from the subsurface of se estonia and adjacent russia
topic conodonts
biostratigraphy
Lower Ordovician
Middle Ordovician
Estonia.
url http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_1/earth-2011-1-1-21.pdf
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