Temperature effects on carbon-specific respiration rate and sinking velocity of diatom aggregates – potential implications for deep ocean export processes

Most deep ocean carbon flux profiles show low and almost constant fluxes of particulate organic carbon (POC) in the deep ocean. However, the reason for the non-changing POC fluxes at depths is unknown. This study presents direct measurements of formation, degradation, and sinking velocity of diatom...

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Bibliographic Details
Published inBiogeosciences Vol. 10; no. 6; pp. 4073 - 4085
Main Authors Iversen, M. H, Ploug, H
Format Journal Article
LanguageEnglish
Published Katlenburg-Lindau Copernicus GmbH 20.06.2013
Copernicus Publications
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