Age of the Kalana Lagerstätte, early Silurian, Estonia

The Kalana quarry in central Estonia is known for its exceptionally well-preserved non-calcified algal and other fossils. The interval with the fossil Konservat Lagerstätte in the Kalana section has previously been tentatively dated as early Aeronian. Recent findings of graptolites now enable more p...

Full description

Bibliographic Details
Main Authors: Peep Männik, Oive Tinn, David K. Loydell, Leho Ainsaar
Format: Article
Language:English
Published: Estonian Academy Publishers 2016-05-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2016/Issue_2/earth-2016-2-105-114.pdf
id doaj-291a2bde1729439e826cfa6f272960cb
record_format Article
spelling doaj-291a2bde1729439e826cfa6f272960cb2020-11-24T21:39:27ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47281736-75572016-05-0165210511410.3176/earth.2016.1010.3176/earth.2016.10Age of the Kalana Lagerstätte, early Silurian, EstoniaPeep Männik0Oive Tinn1David K. Loydell2Leho Ainsaar3Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; peep.mannik@ttu.eeDepartment of Geology, University of Tartu, Ravila 14a, 50411 Tartu, Estonia; oive.tinn@ut.eeSchool of Earth and Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK; david.loydell@port.ac.ukDepartment of Geology, University of Tartu, Ravila 14a, 50411 Tartu, Estonia; leho.ainsaar@ut.eeThe Kalana quarry in central Estonia is known for its exceptionally well-preserved non-calcified algal and other fossils. The interval with the fossil Konservat Lagerstätte in the Kalana section has previously been tentatively dated as early Aeronian. Recent findings of graptolites now enable more precise dating of these beds. The strata yielding the Lagerstätte are not older than the mid-Aeronian and correspond to the Pribylograptus leptotheca graptolite Biozone. In terms of conodont biostratigraphy they correlate with the middle of the Pranognathus tenuis conodont Biozone. It has also become evident that the uppermost Jõgeva Beds of the Nurmekund Formation, and probably also the uppermost Ikla Member of the Saarde Formation, are younger than previously thought and correlate with the Pribylograptus leptotheca graptolite Biozone. Our data additionally indicate that the conodont genus Aulacognathus had appeared by the mid-Aeronian.http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2016/Issue_2/earth-2016-2-105-114.pdfKalana Lagerstätteconodontsgraptolitesbiostratigraphyearly SilurianEstonia.
collection DOAJ
language English
format Article
sources DOAJ
author Peep Männik
Oive Tinn
David K. Loydell
Leho Ainsaar
spellingShingle Peep Männik
Oive Tinn
David K. Loydell
Leho Ainsaar
Age of the Kalana Lagerstätte, early Silurian, Estonia
Estonian Journal of Earth Sciences
Kalana Lagerstätte
conodonts
graptolites
biostratigraphy
early Silurian
Estonia.
author_facet Peep Männik
Oive Tinn
David K. Loydell
Leho Ainsaar
author_sort Peep Männik
title Age of the Kalana Lagerstätte, early Silurian, Estonia
title_short Age of the Kalana Lagerstätte, early Silurian, Estonia
title_full Age of the Kalana Lagerstätte, early Silurian, Estonia
title_fullStr Age of the Kalana Lagerstätte, early Silurian, Estonia
title_full_unstemmed Age of the Kalana Lagerstätte, early Silurian, Estonia
title_sort age of the kalana lagerstätte, early silurian, estonia
publisher Estonian Academy Publishers
series Estonian Journal of Earth Sciences
issn 1736-4728
1736-7557
publishDate 2016-05-01
description The Kalana quarry in central Estonia is known for its exceptionally well-preserved non-calcified algal and other fossils. The interval with the fossil Konservat Lagerstätte in the Kalana section has previously been tentatively dated as early Aeronian. Recent findings of graptolites now enable more precise dating of these beds. The strata yielding the Lagerstätte are not older than the mid-Aeronian and correspond to the Pribylograptus leptotheca graptolite Biozone. In terms of conodont biostratigraphy they correlate with the middle of the Pranognathus tenuis conodont Biozone. It has also become evident that the uppermost Jõgeva Beds of the Nurmekund Formation, and probably also the uppermost Ikla Member of the Saarde Formation, are younger than previously thought and correlate with the Pribylograptus leptotheca graptolite Biozone. Our data additionally indicate that the conodont genus Aulacognathus had appeared by the mid-Aeronian.
topic Kalana Lagerstätte
conodonts
graptolites
biostratigraphy
early Silurian
Estonia.
url http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2016/Issue_2/earth-2016-2-105-114.pdf
work_keys_str_mv AT peepmannik ageofthekalanalagerstatteearlysilurianestonia
AT oivetinn ageofthekalanalagerstatteearlysilurianestonia
AT davidkloydell ageofthekalanalagerstatteearlysilurianestonia
AT lehoainsaar ageofthekalanalagerstatteearlysilurianestonia
_version_ 1725931373771882496