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Published in 2018 at "Frontiers in Marine Science"
DOI: 10.3389/fmars.2018.00102
Abstract: Diatom production is mainly supported by the dissolution of biogenic silica (bSiO2) within the first 200 meters of the water column. The upper oceanic layer is enriched in dissolved and/or colloidal organic matter, such as…
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Keywords:
fossil diatoms;
exopolymeric particles;
transparent exopolymeric;
biogenic silica ... See more keywords