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...
Main Author: | |
---|---|
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 |
id |
doaj-053046141171445981be9c0f1245484a |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT mannikpeep conodontdatingofsometelychiansiluriansectionsinestonia |
_version_ |
1725799302155993088 |