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.
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The deep sea is a major sink for microplastic debris
Lucy C. Woodall, Anna Sànchez‐Vidal, Miquel Canals et al. · Royal Society Open Science · 2014 · 1.9K citations · Full text
Natural Sciences, Environmental Sciences, Marine Sciences +15
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Lamont-Doherty Earth Observatory
Sparkill, United States
45 h-index
139 publications
14.3K citations
Woods Hole Oceanographic Institution
Falmouth, United States
40 h-index
93 publications
15.5K citations

National Oceanography Centre
Southampton, United Kingdom
36 h-index
126 publications
13.8K citations

Centre National de la Recherche Scientifique
Paris, France
36 h-index
247 publications
10.6K citations

Scripps Institution of Oceanography
La Jolla, United States
36 h-index
91 publications
7.5K citations
Columbia University
New York, United States
34 h-index
103 publications
9.3K citations
University of Bremen
Bremen, Germany
34 h-index
99 publications
8.5K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
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81 publications
6.3K citations
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