Distributions of oxygen and carbon stable isotopes and CFC-12 in the water masses of the Southern Ocean at 30°E from South Africa to Antarctica: results of the CIVA1 cruise

• Published in: Journal of Marine Systems
• Main Authors: Archambeau, Anne-Sophie, Pierre, Catherine, Poisson, Alain, Schauer, Bernard
• Other Authors: Laboratoire de Physique et Chimie Marines (LPCM), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'océanographie dynamique et de climatologie (LODYC), Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), WOCE, CIVA
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 1998
• Subjects: Stable isotopes; 18 O; 13 C; CFC-12; Austral Ocean; [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography; Antarctic; Austral; Prydz Bay; Southern Ocean; The Antarctic; Weddell; Antarc*; Antarctica
• Online Access: https://ird.hal.science/ird-00145342; https://ird.hal.science/ird-00145342/document; https://ird.hal.science/ird-00145342/file/asa_JMS.pdf; https://doi.org/10.1016/S0924-7963(98)00027-X

PAR00002959 International audience This study presents oceanic distributions of stable isotopes (δ 18 O of water and δ 13 C of ΣCO 2 ) and CFC-12 from samples collected during the CIVA1 cruise (February/March 1993), across the Southern Ocean, along a meridian section at 30°E, from South Africa (44°S) to Antarctica (70°S). The isotopic measurements show important variations between the subantarctic surface waters with low δ 18 O–high δ 13 C values and the antarctic surface waters with very low δ 18 O–low δ 13 C values. The surface distributions of δ 13 C values follow the major frontal oceanic structures; the vertical distribution shows the progressive upwelling from the subantarctic zone to the antarctic divergence of 13 C-depleted CO 2 derived from remineralization of organic matter. Along the Antarctic continental shelf, between 2500 and 4000 m, a core of water with δ 18 O values close to −0.1‰ is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. This water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the Weddell gyre or from bottom waters coming from the East and formed near Prydz Bay.