Ocean Anoxia

Ocean Anoxia is a biogeochemical state of the marine environment characterized by the severe depletion or absence of dissolved oxygen in seawater, distinguishing it from other oceanic redox conditions by its capacity to disrupt aerobic marine ecosystems and mediate large-scale perturbations in the global carbon cycle.

486

Publications

52.1K

Citations

1.8K

Authors

661

Institutions

Publications per year

2017–2026

168

Authors

1.8K

  1. TJ
    Thomas J. Algeo

    University of Cincinnati, United States

    14 publications · 2.2K citations

    14

    h-index

  2. SW
    Simon W. Poulton

    University of Leeds, United Kingdom

    14 publications · 1.9K citations

    14

    h-index

  3. AD
    Ariel D. Anbar

    Arizona State University, United States

    13 publications · 2.6K citations

    13

    h-index

  4. JS
    Jaap S. Sinninghe Damsté

    Royal Netherlands Institute for Sea Research, Netherlands

    11 publications · 929 citations

    11

    h-index

  5. PB
    Paul B. Wignall

    University of Leeds, United Kingdom

    10 publications · 2.5K citations

    10

    h-index

1–5 of 1.8K

Venues

  1. Earth and Planetary Science Letters

    27 publications · 2.3K citations

    25

    h-index

  2. Palaeogeography Palaeoclimatology Palaeoecology

    21 publications · 1.1K citations

    19

    h-index

  3. Geology

    18 publications · 2.8K citations

    18

    h-index

  4. Proceedings of the National Academy of Sciences

    PNAS · 15 publications · 1.8K citations

    15

    h-index

  5. Paleoceanography

    14 publications · 2.8K citations

    13

    h-index

1–5