ON SUSPENDED BARITE AND TIlE OXYGEN MINIMUM IN THE SOUTHERN OCEAN

• Published in: Global Biogeochemical Cycles
• Main Authors: Dehairs, Frank, Goeyens, L., Stroobants, N., Bernard, P., Goyet, Catherine, Poisson, Alain, Chesselet, R.
• Other Authors: Vrije Universiteit Brussel (VUB), UNIVERSITY OF ANTWERP WILRIJK BEL, Partenaires IRSTEA, Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Laboratoire de Physique et Chimie Marines (LPCM), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Centre des Faibles Radioactivités, Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 1990
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces; environment; Antarctic; Indian; Southern Ocean; The Antarctic; Antarc*
• Online Access: https://hal.science/hal-03561342; https://hal.science/hal-03561342/document; https://hal.science/hal-03561342/file/Global%20Biogeochemical%20Cycles%20-%20March%201990%20-%20Dehairs%20-%20On%20suspended%20barite%20and%20the%20oxygen%20minimum%20in%20the%20Southern%20Ocean.pdf; https://doi.org/10.1029/GB004i001p00085

International audience Particulate Ba profiles were measured in the Indian sector of the southern ocean. The largest fraction (>80%) of this barium is present as barite microcrystals. The profiles of total barium are characterized by a subsurface maximum between 200 and 500 m depth in the vicinity of the oxygen minimum. Highest barira values are found just south of the Polar Front, while lowest values occur close to the Antarctic Divergence. Between the divergence and the Polar Front a fight inverse relationship is observed between oxygen in the oxygen minimum and barium in the barium maximum. This relationship disappears north of the Polar Front. Since suspended barite is known to be of biological origin, the correlation of barite with oxygen suggests that the observed decrease of oxygen in the oxygen minimum, between the divergence and the Polar Front is due to local consumption of oxygen. It is proposed that deep low oxygen water is advected towards the Divergence where upwelling occurs and where this water subsequently partly spreads out to the north, northeast , as entrained by the Antarctic Circumpolar Current.