Early winter barium excess in the southern Indian Ocean as an annual remineralisation proxy (GEOTRACES GIPr07 cruise).

• Published in: Biogeosciences
• Main Authors: van Horsten, Natasha René, Planquette, Hélène, Sarthou, Géraldine, Ryan-Keogh, Thomas James, Lemaitre, Nolwenn, Mtshali, Thato Nicholas, Roychoudhury, Alakendra, Bucciarelli, Eva
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2022
• Subjects: Barium; GEOTRACES; Austral; Indian; Southern Ocean
• Online Access: http://hdl.handle.net/1834/42803; https://doi.org/10.5194/bg-19-3209-2022

he Southern Ocean (SO) is of global importance to the carbon cycle, and processes such as mesopelagic remineralisation that impact the efficiency of the biological carbon pump in this region need to be better constrained. During this study early austral winter barium excess (Baxs) concentrations were measured for the first time, along 30∘ E in the southern Indian Ocean. Winter Baxs concentrations of 59 to 684 pmol L−1 were comparable to those observed throughout other seasons. The expected decline of the mesopelagic Baxs signal to background values during winter was not observed, supporting the hypothesis that this remineralisation proxy likely has a longer timescale than previously reported. A compilation of available SO mesopelagic Baxs data, including data from this study, shows an accumulation rate of ∼0.9 µmol m−2 d−1 from September to July that correlates with temporally integrated remotely sensed primary productivity (PP) throughout the SO from data spanning ∼20 years, advocating for a possible annual timescale of this proxy. The percentage of mesopelagic particulate organic carbon (POC) remineralisation as calculated from estimated POC remineralisation fluxes over integrated remotely sensed PP was ∼2-fold higher south of the polar front (19 ± 15 %, n=39) than north of the polar front (10 ± 10 %, n=29), revealing the higher surface carbon export efficiency further south. By linking integrated remotely sensed PP to mesopelagic Baxs stock, we could obtain better estimates of carbon export and remineralisation signals within the SO on annual and basin scales. Chllenges 4, 9 Published Refereed