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Contribution of combined carbohydrates to dissolved and particulate organic carbon after the spring bloom in the Bay of Biscay

par Engel, Anja;Händel, N.;De Bodt, Caroline ;Harlay, Jérôme ;Piontek, J.;Chou, Lei
Référence Continental shelf research, 45, page (42-53)
Publication Publié, 2012

Article révisé par les pairs

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Résumé :

Two cruises were conducted after the diatom spring bloom in the northern Bay of Biscay (2006, 2007), to assess the contribution of combined carbohydrates to organic carbon partitioning. Partitioning of total organic carbon (TOC) into particulate organic carbon (POC) and dissolved organic carbon (DOC) differed between the two years, particularly for depths above 60m, and was related to the vernal development of the system: a post spring-bloom system in 2007, and a more stratified summer system with higher coccolithophore abundance in 2006. In general, contribution of POC to TOC ranged between 4% and 28% and decreased with depth. Concentration of high-molecular-weight (HMW;>1kDa) dissolved combined carbohydrates (dCCHO) ranged from 0.6 to 1.4μmolL -1 and contributed between 4% and 11% to DOC. Concentration of particulate combined carbohydrates (pCCHO) varied between 0.03 and 1.3μmolL -1. A high contribution of pCCHO to POC was observed in 2007, i.e. 22-60% C compared to 3-10% C in 2006, and coincided with a higher abundance of transparent exopolymer particles (TEP). TEP accounted for 0.4-2.0μmolCL -1 in 2007 and 0.5-1.5μmolCL -1 in 2006. Above 60m, differences in contribution of TEP-C to POC were most pronounced yielding 15.4±3.0% in 2007 compared to relatively low 4.8±1.4%, in 2006. TEP-C could explain about 60% in 2007 and about 40% of pCCHO-C in 2006. Hence, TEP were identified as a substantial component of pCCHO and POC, particularly in the wake of the spring bloom. Molecular composition of CCHO, i.e. HMW-dCCHO+pCCHO, revealed little difference between the years but strong variation over depth. Uronic acids (URA) were identified as a major component of CCHO (20-40%). Our study indicates that the distribution and composition of CCHO in surface seawater are determined by biogeochemical processes on a seasonal scale. A better knowledge of CCHO cycling and molecular signature has therefore a high potential for a better tracing of carbon dynamics in shelf sea ecosystems. © 2012 Elsevier Ltd.