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Middle Ordovician carbonate facies development, conodont biostratigraphy and faunal diversity patterns at the Lynna River, northwestern Russia

https://doi.org/10.3176/earth.2020.03

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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inferredcites →https://doi.org/10.18261/8200376583-1995-01openalex-snapshot

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inferredcites →https://doi.org/10.3176/earth.2012.1.01openalex-snapshot

Ordovician conodont diversity in the northern Baltic; pp. 1–14

inferredcites →https://doi.org/10.3176/earth.2012.4.03openalex-snapshot

Darriwilian (Middle Ordovician) conodont biostratigraphy in NW Estonia; pp. 210–226

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Diversity and biostratigraphic utility of Ordovician brachiopods in the East Baltic; pp. 176–191

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USE OF GRAPHIC CORRELATION FOR ASSESSING EVENT-STRATIGRAPHIC SIGNIFICANCE AND trans-ATLANTIC RELATIONSHIPS OF ORDOVICIAN K-BENTONITES

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CONFACIES DIFFERENTIATION AND UPPER MIDDLE ORDOVICIAN CORRELATION IN THE BALTOSCANDIAN BASIN

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Dolomitization and sedimentary cyclicity of the Ordovician, Silurian, and Devonian rocks in South Estonia

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Brachiopod macrofaunal distribution through the upper Volkhov – lower Kunda (Lower Ordovician) rocks, Lynna River, St. Petersburg region

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An integrated biostratigraphical analysis of the Volkhov–Kunda (Lower Ordovician) succession at Fågelsång, Scania, Sweden

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Upper Arenig trilobite biostratigraphy and sea-level changes at Lynna River near Volkhov, Russia

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Conodont faunas with Lenodus variabilis in the upper Arenigian to lower Llanvirnian of Sweden

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10. Ordovician Sea Level Changes: A Baltoscandian Perspective

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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The mid-Ordovician meteorite flux to Earth shortly before breakup of the L-chondrite parent body

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Early and early Middle Ordovician chitinozoans from the Baldone drill core, central Latvia

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