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Particulate matter stoichiometry driven by microplankton community structure in summer in the Indian sector of the Southern Ocean 5
Rembauville, M.; Blain, S.; Caparros, J.; Salter, I..
Microplankton community structure and particulate matter stoichiometry were investigated in a late summer survey across the Subantarctic and Polar Front in the Indian sector of the Southern Ocean. Microplankton community structure exerted a first order control on PON:POP stoichiometry with diatom-dominated samples exhibiting much lower ratios (4–6) than dinoflagellate and ciliate-dominated samples (10–21). A significant fraction of the total chlorophyll a (30–70%) was located beneath the euphotic zone and mixed layer and sub-surface chlorophyll features were associated to transition layers. Although microplankton community structure and biomass was similar between mixed and transition layers, the latter was characterized by elevated Chl:POC ratios...
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Ano: 2016 URL: https://archimer.ifremer.fr/doc/00324/43484/42942.pdf
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Origin and fate of particulate and dissolved organic matter in a naturally iron-fertilized region of the Southern Ocean 5
Tremblay, L.; Caparros, J.; Leblanc, K.; Obernosterer, I..
Natural iron fertilization of high-nutrient low-chlorophyll (HNLC) waters induces annually occurring spring phytoplankton blooms off the Kerguelen Islands (Southern Ocean). To examine the origin and fate of particulate and dissolved organic matter (POM and DOM), D- and L-amino acids (AA) were quantified at bloom and HNLC stations. Total hydrolyzable AA accounted for 21-25% of surface particulate organic carbon (% POCAA) at the bloom sites, but for 10% at the HNLC site. A marked decrease in % POCAA with depth was observed at the most productive stations leading to values between 3 and 5% below 300 m depth. AA contributed to only 0.9-4.4% of dissolved organic carbon (%DOCAA) at all stations. The only consistent vertical trend was observed at the most...
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Ano: 2015 URL: https://archimer.ifremer.fr/doc/00352/46293/45945.pdf
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