Dissolved inorganic carbon, alkalinity, nutrient and oxygen seasonal and interannual variations at the Antarctic Ocean JGOFS-KERFIX site

• Published in: Deep Sea Research Part I: Oceanographic Research Papers
• Main Authors: Louanchi, Ferial, Ruiz-Pino, Diana, Jeandel, Catherine, Brunet, Christian, Schauer, Bernard, Masson, Annick, Fiala, Michel, Poisson, Alain
• Other Authors: Laboratoire de Physique et Chimie Marines (LPCM), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Université de Brest (UBO)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2001
• Subjects: Nutrient cycles; Carbon cycle; Oceanic mixed layer; Biogeochemical cycles; Antarctic zone; Biological production; Temporal distribution; Oxygen; Carbon dioxide; [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]; Antarctic; The Antarctic; Kerguelen; Indian; Antarctic Ocean; Antarc*
• Online Access: https://hal.archives-ouvertes.fr/hal-01245602; https://doi.org/10.1016/S0967-0637(00)00086-8

International audience JGOFS-KERFIX (KERguelen point FIXe) time-series station, located south of the polar front in the Indian sector of the Antarctic Ocean, was occupied monthly between January 1990 and March 1995. Annual cycles of dissolved inorganic carbon (DIC), total alkalinity (TALK), oxygen (O2) and nutrients (nitrate, silicate, phosphate and ammonia) in the upper ocean are presented for this site. From seasonal drawdown of nutrients and DIC, we estimate a spring–summer net community production of 3.2±0.5 mol m −2 and C/N/P ratios of 100/16/1. The Si/N ratio varies between 1.8 and 3, suggesting low iron concentrations. The spring–summer biogenic silicon export derived from silicate drawdown is 1.18 mol m −2 , consistent with model estimates of silicate export at this site. Seasonal and interannual variations of oxygen, nitrate and DIC due to physical and biological processes are quantified using a simple month-to-month budget formulation. From these budgets, an annual net community production of 5.7±3.3 mol m −2 yr −1 is estimated, about twice the averaged spring–summer production, indicating that, at KERFIX, there is a positive net community production throughout the year. Air–sea CO2 fluxes show that KERFIX is a strong CO2 sink for the atmosphere of 2.4–5.1 mol m −2 yr −1 in 1993, depending on the gas exchange formulation used. A 2.1–3.3 mol m −2 yr −1 outgassing of O2 is observed at KERFIX except in 1993 and 1994 where a decreasing trend of temperature induces an increase of O2 solubility.