Latest Ordovician–early Silurian palaeoenvironmental changes and palaeotemperature trends indicated by stable carbon and oxygen isotopes from northern Estonia
Brachiopods are the biological constituents most often used for the delineation of stable C and O isotopic compositions in Palaeozoic sediments. We present C and O isotope data for the Late Ordovician and early Silurian to evaluate the palaeotemperatures and palaeoenvironmental variability in Baltic...
Main Authors: | Bilal Gul, Leho Ainsaar, Tõnu Meidla |
---|---|
Format: | Article |
Language: | English |
Published: |
Estonian Academy Publishers
2021-11-01
|
Series: | Estonian Journal of Earth Sciences |
Subjects: | |
Online Access: | https://kirj.ee/wp-content/plugins/kirj/pub/earth-4-2021-196-209_20211115211537.pdf |
Similar Items
-
Ostracods of the Ordovician–Silurian boundary beds: Jūrmala core (Latvia) and its implications for Baltic stratigraphy
by: Tõnu Meidla, et al.
Published: (2020-11-01) -
Searching for the Ordovician–Silurian boundary in Estonia, Latvia and Lithuania
by: Tõnu Meidla, et al.
Published: (2023-06-01) -
Lower Silurian biostratigraphy of the Viirelaid core, western Estonia
by: Nestor, Viiu, et al.
Published: (2007-12-01) -
Hirnantian Isotope Carbon Excursion in Gorny Altai, southwestern Siberia
by: Nikolay V. Sennikov, et al.
Published: (2015-08-01) -
A multiproxy study of the Puhmu core section (Estonia, Upper Ordovician): consequences for stratigraphy and environmental interpretation
by: Dimitri Kaljo, et al.
Published: (2017-05-01)