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The Silica Balance in the World Ocean: A Reestimate

Tréguer, Paul, Nelson, David M., Van Bennekom, Aleido J., DeMaster, David J., Leynaert, Aude, Quéguiner, Bernard·1995·Science

Abstract

The net inputs of silicic acid (dissolved silica) to the world ocean have been revised to 6.1 ± 2.0 teramoles of silicon per year (1 teramole = 10 12 moles). The major contribution (about 80 percent) comes from rivers, whose world average silicic acid concentration is 150 micromolar. These inputs are reasonably balanced by the net ouputs of biogenic silica of 7.1 ± 1.8 teramoles of silicon per year in modern marine sediments. The gross production of biogenic silica (the transformation of dissolved silicate to particulate skeletal material) in surface waters was estimated to be 240 ± 40 teramoles of silicon per year, and the preservation ratio (opal accumulation in sediment/gross production in surface waters) averages 3 percent. In the world ocean the residence time of silicon, relative to total biological uptake in surface waters, is about 400 years.

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Metadata

Authors
Tréguer, P., Nelson, D. M., Van Bennekom, A. J., DeMaster, D. J., Leynaert, A., & Quéguiner, B.
Venue
Science
Published
1995-04-21
Volume
268
Issue
5209
Pages
375-379
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2041885277
Cited by
1,484
References
0
FWCI
15.86
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The Silica Balance in the World Ocean: A Reestimate. https://app.cochat.ai/papers/10.1126/science.268.5209.375
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Tréguer, P., Nelson, D. M., Van Bennekom, A. J., DeMaster, D. J., Leynaert, A., & Quéguiner, B. (1995). The Silica Balance in the World Ocean: A Reestimate. Science. https://doi.org/10.1126/science.268.5209.375

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