Conodont dating of some Telychian (Silurian) sections in Estonia [PDF]
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.
Männik, Peep
doaj
Triassic conodonts of the Slovenian Basin
Slovenian Basin was formed during the Ladinian following disintegration of the Slovenian Carbonate Platform. It persisted continuously until the Late Cretaceous.
Stanko Buser +2 more
doaj
. The Permian–Triassic boundary sections in north-western Iran belong to the most complete successions, in which the largest mass extinction event in the history of the Earth can be studied.
A. Ghaderi +4 more
semanticscholar +1 more source
Limitotipes of Lower Sakmarian and Artinskian stages boundary in the Urals
The section Usolka and duplicating its section Dal’ny Tulkas (Bashkortostan) are proposed as the stratotypes of the Lower Sakmarian stage boundary and Lower Artinskian stage boundary of the International Stratigraphic scale.
V. V. Chernykh, B. I. Chuvashov
doaj +2 more sources
Triassic deep-water sedimentation in the Bled Basin, eastern Julian Alps, Slovenia
The Bled Basin was a Middle Triassic–Early Cretaceous basin whose remnants are preserved in the eastern Southern Alps in western Slovenia. The early evolution of the basin is recorded in the Upper Ladinian to Lower Jurassic Zatrnik cherty limestone ...
Luka Gale +5 more
doaj +1 more source
Recent developments in the Upper Ordovician and lower Silurian conodont biostratigraphy in Estonia [PDF]
The current state of and the latest developments in the conodont-based biostratigraphical studies of Upper Ordovician and lower Silurian strata in Estonia are discussed.
Männik, Peep
doaj
Polytaxonomic and monotaxonomic zonal biochronological scales in biostratigraphy
The method of increasing the correlation potential of zonal biochronological scales by creating the polytaxonomic complex characteristic of zone subdivisions is proposed. For this operation is necessary the normative zonal scale, by which biozones of the
V. V. Chernykh, N. A. Kucheva
doaj
Lower Silurian biostratigraphy of the Viirelaid core, western Estonia [PDF]
The distribution of five groups of fossils in the upper Llandovery (Telychian) and Wenlock of the Viirelaid core section, Estonia, is presented and discussed in terms of their biozones (conodonts and chitinozoans) and mutual positions (scolecodonts ...
Nestor, Viiu +6 more
doaj
The Middle Carboniferous Boundary in the North of Pay-Khoy – Correlation between the Shallow- and Deep-Water Sequences [PDF]
The paper considers the Lower-Middle Carboniferous boundary interval in the sections of the Pay-Khoy carbonate parautochthone (shallow-water facies) and the Kara slate allochthone (deep-water facies) with respect to the boundary tracing criteria.
A.V. Zhuravlev, Ya.A. Vevel
doaj
Temperature-driven heterochrony as a main evolutionary response to climate changes in conodonts. [PDF]
Souquet L +5 more
europepmc +1 more source

