Deep-sea Sedimentation

Deep-Sea Sedimentation is the process of deposition and accumulation of particulate matter on the ocean floor at depths typically exceeding 2,000 meters, distinguished from other sedimentary processes by its isolation from terrestrial sediment sources, slow rates of deposition, and dominance of biogenic, pelagic, and authigenic components in the absence of significant bottom-current reworking.

1.7K

Publications

124.4K

Citations

4.4K

Authors

1.1K

Institutions

Publications per year

2017–2026

272

Authors

4.4K

  1. WB
    Wolfgang Berger

    Scripps Institution of Oceanography, United States

    11 publications · 1.1K citations

    11

    h-index

  2. CR
    Craig R. Smith

    University of Hawaiʻi at Mānoa, United States

    11 publications · 1.2K citations

    11

    h-index

  3. IN
    I Nick McCave

    University of Cambridge, United Kingdom

    12 publications · 1.7K citations

    11

    h-index

  4. BC
    Bruce C. Heezen

    Lamont-Doherty Earth Observatory, United States

    10 publications · 1.3K citations

    10

    h-index

  5. AB
    Antje Boëtius

    Max Planck Institute for Marine Microbiology, Germany

    10 publications · 676 citations

    10

    h-index

1–5 of 4.4K

Venues

  1. Marine Geology

    137 publications · 7.8K citations

    49

    h-index

  2. Geochimica et Cosmochimica Acta

    75 publications · 10.3K citations

    49

    h-index

  3. Nature

    66 publications · 9.2K citations

    41

    h-index

  4. Science

    51 publications · 5.1K citations

    34

    h-index

  5. 34

    h-index

1–5