Mesoscale surface distribution of biogeochemical characteristics in the Crozet Basin frontal zones (South Indian Ocean)

• Published in: Marine Ecology Progress Series
• Main Authors: Fiala, M., Delille, Bruno, Dubreuil, C., Kopczynska, E., Leblanc, K., Morvan, J., Queguiner, B., Blain, S., Cailliau, C., Conan, P., Corvaisier, R., Denis, M., Frankignoulle, Michel, Oriol, L., Roy, S.
• Other Authors: Unité d'Océanographie Chimique
• Format: Article in Journal/Newspaper
• Language: English
• Published: Inter-Research 2003
• Subjects: frontal zones; nutrients; biogenic silica; chlorophyll a; pCO(2); phytoplankton; bacteria; Life sciences; Aquatic sciences & oceanology; Environmental sciences & ecology; Physical; chemical; mathematical & earth Sciences; Earth sciences & physical geography; Sciences du vivant; Sciences aquatiques & océanologie; Sciences de l’environnement & écologie; Physique; chimie; mathématiques & sciences de la terre; Sciences de la terre & géographie physique; Antarc*; Antarctic
• Online Access: https://orbi.uliege.be/handle/2268/1239; https://doi.org/10.3354/meps249001

peer reviewed A mesoscale study was conducted in January and February 1999 in the Crozet Basin frontal zones (43degrees50' to 45degrees20'S, 61degrees00' to 64degrees30'E) within the southernmost and easternmost convergence area of the Antarctic Circumpolar Current (ACC) and the Agulhas Return Current (ARC). Distribution of biogeochemical parameters was strongly linked to the merged Subtropical (STF) and Subantarctic (SAF) Fronts which mark the border between the cold and less saline subantarctic waters and the warm and more saline subtropical waters. This survey took place during a post-bloom period. Chlorophyll a concentrations were low throughout the study area ranging from 0.2 mug l(-1) in the Polar Frontal Zone (PFZ) to 0.4 mug l(-1) in the Subtropical Zone (STZ). Maximum chlorophyll a values (0.8 mug l(-1)) associated with an increase in biogenic silica concentration (from 0.03 to 0.34 muM) and a diatom peak (1.2 x 10(5) cells l(-1)) were encountered in the northeastern part of the STF edge. Despite northwardly decreasing concentrations of nitrates from 14 muM in the PFZ to 6 PM in the STZ, they were not the main factor limiting phytoplankton growth. Low silicic acid (mean = 0.6 muM) could have limited diatom development in the PFZ and the STZ where diatom numbers were low. In STZ waters, where average diatom numbers were highest, various species of Nitzschia and Thalassiothrix were common, but Pseudonitzschia spp. were dominant. Throughout the survey area, pico- and nano-sized cells dominated the phytoplankton assemblage, and their number was the highest in the STZ. Cyanobacteria, only present in subtropical waters >12.5degreesC, were the major component of the picoplankton size-fraction. While dinoflagellate numbers were low in the Subantarctic Zone (SAZ), their abundance and species numbers increased in the STZ, where Oxytoxum laticeps became dominant and several further large-size species of Prorocentrum, Ceratium and Gymnodinium appeared in addition to those at the STF. The distribution of ...