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GeoRef Categories
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Mehikoorma Estonia
Emended Sandbian (Ordovician) conodont biostratigraphy in Baltoscandia and a new species of Amorphognathus Open Access
The middle Darriwilian (Ordovician) δ 13 C excursion (MDICE) discovered in the Yangtze Platform succession in China: implications of its first recorded occurrences outside Baltoscandia Available to Purchase
Stratigraphic chart illustrating the range of Amorphognathus aff. Am. ve... Available to Purchase
First documentation of the Ordovician Guttenberg δ 13 C excursion (GICE) in Asia: chemostratigraphy of the Pagoda and Yanwashan formations in southeastern China Available to Purchase
Comparison of the δ 13 C records from the Tingskullen core (this study), ... Available to Purchase
The δ 13 C curve through the Darriwilian succession in the Mehikoorma (421)... Available to Purchase
Recognizing Tide-Dominated Versus Tide-Influenced Deltas: Middle Devonian Strata of the Baltic Basin Available to Purchase
The Ordovician zone index conodont Amorphognathus ordovicicus Branson & Mehl, 1933 from its type locality and the evolution of the genus Amorphognathus Branson & Mehl, 1933 Available to Purchase
A modern assessment of Ordovician chitinozoans from the Shelve and Caradoc areas, Shropshire, and their significance for correlation Available to Purchase
Integrated conodont biostratigraphy and carbon isotope chemostratigraphy in the Lower–Middle Ordovician of southern Sweden reveals a complete record of the MDICE Available to Purchase
Integrated Upper Ordovician graptolite–chitinozoan biostratigraphy of the Cardigan and Whitland areas, southwest Wales Available to Purchase
Ordovician of the Eastern Baltic palaeobasin and the Tornquist Sea margin of Baltica Open Access
Abstract This paper summarizes recent knowledge on the palaeontology, biostratigraphy, correlation, sea-level and climate history and isotopic geochemistry of the Ordovician rocks in the western and central parts of the East European Craton, in the area extending from the southern margin of the Fennoscandian Shield to the western margin of the Ukrainian Shield. The regional chronostratigraphic standard is briefly summarized and its correlation to the global standard of the Ordovician is addressed. A two-part correlation chart of 10 areas with unique local Ordovician successions is aligned with the most recent international correlation standard of the Ordovician System and presented against the regular timescale. An updated summary of the evolution of the marine assemblages is provided, the principal gaps in the existing extremely rich palaeontological database are identified and the main bioevents are discussed.