Global patterns in oceanic planktonic metabolism

Rates of gross primary production (GPP) and respiration (CR) of plankton communities in the upper ocean were evaluated on the basis of a data set comprising 3149 paired light and dark bottle measurements of volumetric GPP-CR of euphotic zone plankton communities. The data were from 72 published and...

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Bibliographic Details
Published in:Limnology and Oceanography
Main Authors: Regaudie de Gioux, Aurore, Duarte, Carlos M.
Other Authors: European Commission, Ministerio de Ciencia e Innovación (España)
Format: Article in Journal/Newspaper
Language:unknown
Published: American Society of Limnology and Oceanography 2013
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Online Access:http://hdl.handle.net/10261/126502
https://doi.org/10.4319/lo.2013.58.3.0977
https://doi.org/10.13039/501100000780
https://doi.org/10.13039/501100004837
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Summary:Rates of gross primary production (GPP) and respiration (CR) of plankton communities in the upper ocean were evaluated on the basis of a data set comprising 3149 paired light and dark bottle measurements of volumetric GPP-CR of euphotic zone plankton communities. The data were from 72 published and unpublished reports of measurements made between 1981 and 2011 from the open ocean and the Mediterranean Sea. The data set is dominated by measurements in chlorophyll a (Chl a)-rich oceans and North Atlantic waters, with a paucity of measurements in the Indian Ocean and South Pacific Ocean. CR scaled as the 3/4 power of GPP with a power slope of 0.79 ± 0.01, implying that the threshold GPP separating heterotrophic from autotrophic plankton communities is 1.26 mmol O2 m-3 d-1. Plankton communities with Chl a < 0.35 mg m-3 tend to be heterotrophic. Both GPP and CR declined exponentially with depth, but the GPP declined faster, at 42% ± 7% m-1, than CR (29% 6 8% m-1), so that CR increases relative to GPP with depth. © 2013, by the Association for the Sciences of Limnology and Oceanography, Inc. This is a contribution to the ‘‘Malaspina 2010’’ Consolider project funded by the Spanish Ministry of Science and Innovation (CSD2008-00077) and the METAOCEANS Marie Curie Early Stage Research Network (019678-2), funded by the Framework Program 6 of the EU Peer Reviewed