Middle Ordovician paleoenvironmental evolution of the western Laurentian carbonate platform: Evidence for persistent oxygenation of the shallow ocean and implications for biodiversification

Author:

Diamond Charles W.,Saltzman Matthew R.,Lyons Timothy W.,Edwards Cole T.

Funder

NASA Astrobiology Institute

Publisher

Elsevier BV

Reference106 articles.

1. Calcium isotope constraints on a Middle Ordovician carbon isotope excursion;Adiatma;Earth Planet. Sci. Lett.,2024

2. Local and global controls on carbon isotope chemostratigraphy;Ahm,2022

3. Middle and Upper Ordovician stable isotope stratigraphy across the facies belts in the East Baltic;Ainsaar,2004

4. Middle and Upper Ordovician carbon isotope chemostratigraphy in Baltoscandia: a correlation standard and clues to environmental history;Ainsaar;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2010

5. Stratigraphy and facies differences of the Middle Darriwilian Isotopic Carbon Excursion (MDICE) in Baltoscandia;Ainsaar;Estonian J. Earth Sci.,2020

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