Particulate organic carbon export from the North and South Atlantic gyres: The Th-234/U-238 disequilibrium approach

Subtropical ocean gyres are believed to be characterized by low carbon export from the surface into the deep ocean. However, due to their large areas, even relatively small average export could be of significance for the global carbon cycle. To better constrain carbon export from the surface ocean in such regions, radioactive disequilibria between the particlereactive; short-lived radionuclide Th-234 (half-life 24.1 d) and its parent U-238 were used to estimate fluxes of Th-234 and particulate organic carbon (POC) from surface waters of the North and South Atlantic subtropical gyres and their fringes. Samples were collected between similar to 50 degrees S and similar to 50 degrees N as part of the Atlantic Meridional Transect (AMT) programme during April/May 2004 (AMT14). Application of a steady-state model to the Th-234 data revealed particle export from the surface (Th-234 deficit) and, in one instance, some evidence for shallow particle remineralisation at depth (Th-234 excess). Export fluxes of POC were calculated from water column Th-234/U-238 disequilibria and the POC to Th-234 ratios on large rapidly sinking particles (> 50 mu m). Based on latitudinal distributions of selected hydrographic and biological parameters within the topmost 300m of the water column, the transect was divided into six regions: `temperate' (35 degrees-50 degrees N and 35 degrees-50 degrees S), `oligotrophic' (20 degrees-35 degrees N and 5 degrees-35 degrees S), 'equatorial' (5 degrees S-5 degrees N), and 'upwelling' (5 degrees-20 degrees N). The lowest Th-234-derived POC export fluxes were found in the oligotrophic gyres and ranged from 0 in the northern to 6 mmol C m(-2) d(-1) in the southern oligotrophic, indicating a tightly coupled food web. Enhanced POC export was associated with the equatorial region (25 mmol C m(-2) d(-1)) and the upwelling region north of the equator (15 mmol C m(-2) d(-1)). POC export in the temperate regions ranged from 7 mmol C m(-2) d(-1) to a maximum of 41 mmol C m(-2) d(-1). High fluxes at the poleward edges of the oligotrophic gyres probably result from episodic nutrient-loading processes associated with submesoscale features. Estimates of instantaneous primary production (PP) were compared with Th-234-derived POC export, the latter bearing information from the past few weeks. Most export efficiencies that were calculated based on this comparison were high (10s%), suggesting uncoupling of PP and export estimates due to the different time scales of the approaches. Moreover, this uncoupling points to the occurrence of pulsed high-export events that could be easily missed by instantaneous sampling but traced by temporally quasi-integrating tracers such as Th-234. Results from this study suggest that although carbon export in the oligotrophic centres of the gyres may be low, carbon sequestration in the temperate fringes of the gyres as well as in the equatorial and upwelling regions can be substantial, and that spatio-temporal variability in these areas of the world's oceans needs to be considered more fully in the context of global oceanic carbon sequestration. (c) 2006 Elsevier Ltd. All rights reserved.