Seasonal dynamics in diatom and particulate export fluxes to the deep sea in the Australian sector of the southern Antarctic Zone

• Published in: Journal of Marine Systems
• Main Authors: Rigual-Hernández, Andrés S., Trull, Thomas W., Bray, Stephen G., Closset, Ivia, Armand, Leanne K.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2015
• Subjects: Diatom flux; Particulate flux; Sediment traps; Southern Ocean; Antarctic; Austral; Pacific; The Antarctic; Antarc*; Sea ice
• Online Access: https://researchers.mq.edu.au/en/publications/5cece733-067b-48e5-b3d5-1121d3182f95; https://doi.org/10.1016/j.jmarsys.2014.10.002; http://www.scopus.com/inward/record.url?scp=84908627949&partnerID=8YFLogxK

Particle fluxes were recorded over a one-year period (2001-02) in the southern Antarctic Zone in the Australian Sector of the Southern Ocean. Here, we present the results on the seasonal and vertical variability of biogenic particle and diatom valve fluxes. Total mass and diatom fluxes were highly seasonal, with maxima registered during the austral summer and minima during winter. Biogenic opal dominated sedimentation, followed by carbonate, and very low levels of organic carbon (annual average 1.4%). The strong correlation between opal and organic carbon at both depth levels suggests that a significant fraction of organic matter exported to the deep sea was associated with diatom sedimentation events. Seasonal diatom fluxes appear driven principally by changes in the flux of Fragilariopsis kerguelensis. The occurrence of the sea-ice affiliated diatoms Fragilariopsis cylindrus and Fragilariopsis curta in both sediment traps is considered to correspond to the sedimentation of a diatom bloom advected from an area under the influence of sea ice. Highest fluxes of the subsurface-dwelling species Thalassiothrix antarctica registered at the end of the summer bloom were linked to a drop of the light levels during the summer-autumn transition. This study provides the first annual observation on seasonal succession of diatom species in the Australian sector of the Antarctic Zone, and corresponds, in terms of magnitude and seasonality of diatom fluxes, to those in neighbouring sectors (Pacific and eastern Atlantic).