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
Main Authors: M. H. Iversen, H. Ploug
Format: Article
Language:English
Published: Copernicus Publications 2013-06-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/10/4073/2013/bg-10-4073-2013.pdf