Nevin P Kozik

Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction

D. Bond, Daizhao Chen, J. Owens, 2022, Science advances.

Did early land plants produce a stepwise change in atmospheric oxygen during the Late Ordovician (Sandbian ~458 Ma)?

C. Edwards, E. Griffith, M. Saltzman, 2019, Palaeogeography, Palaeoclimatology, Palaeoecology.

Middle–Upper Ordovician (Darriwilian–Sandbian) paired carbon and sulfur isotope stratigraphy from the Appalachian Basin, USA: Implications for dynamic redox conditions spanning the peak of the Great Ordovician Biodiversification Event

T. Them, M. Saltzman, Seth A. Young, 2019, Palaeogeography, Palaeoclimatology, Palaeoecology.

Marine redox variability from Baltica during extinction events in the latest Ordovician–early Silurian

J. Owens, T. Martma, S. Bergström, 2020 .

Integrated sedimentary, biotic, and paleoredox dynamics from multiple localities in southern Laurentia during the late Silurian (Ludfordian) extinction event

J. Owens, Seth A. Young, Nevin P. Kozik, 2020 .

Geochemical Records Reveal Protracted and Differential Marine Redox Change Associated With Late Ordovician Climate and Mass Extinctions

T. Lyons, Benjamin C Gill, J. Owens, 2021, AGU Advances.

Protracted oxygenation across the Cambrian–Ordovician transition: A key initiator of the Great Ordovician Biodiversification Event?

P. Ahlberg, J. Owens, Seth A. Young, 2023, Geobiology.

Progressive marine oxygenation and climatic cooling at the height of the Great Ordovician Biodiversification Event

P. Ahlberg, J. Owens, Seth A. Young, 2023, Global and Planetary Change.