Particulate organic matter flux and planktonic new production in the deep ocean View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1979-12

AUTHORS

Richard W. Eppley, Bruce J. Peterson

ABSTRACT

Primary production in the oceans results from allochthonous nutrient inputs to the euphotic zone (new production) and from nutrient recycling in the surface waters (regenerated production). Global new production is of the order of 3.4−4.7 × 109 tons of carbon per year and approximates the sinking flux of paniculate organic matter to the deep ocean. More... »

PAGES

677-680

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/282677a0

DOI

http://dx.doi.org/10.1038/282677a0

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1041861361


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