δ13C chemostratigraphy of the Middle and Upper Ordovician succession in the Tartu-453 drillcore, southern Estonia, and the significance of the HICE
The δ13C isotope data from the Tartu-453 core section in southern Estonia enabled creation of a continuous Ordovician carbon isotope record, ranging from the Floian to the end of the Hirnantian. Five positive δ13C excursions and one negative δ13C excursion were recognized. Most of the positive excur...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Estonian Academy Publishers
2014-12-01
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Series: | Estonian Journal of Earth Sciences |
Subjects: | |
Online Access: | http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2014/issue_4/earth-2014-4-195-200.pdf |