Articles | Volume 7, issue 1
Ocean Sci., 7, 113–127, 2011
Ocean Sci., 7, 113–127, 2011

Research article 08 Feb 2011

Research article | 08 Feb 2011

Phytoplankton distribution and nitrogen dynamics in the southwest indian subtropical gyre and Southern Ocean waters

S. J. Thomalla1,2, H. N. Waldron1, M. I. Lucas3, J. F. Read4, I. J. Ansorge1, and E. Pakhomov5,6 S. J. Thomalla et al.
  • 1Department of Oceanography, University of Cape Town, Private Bag, Rondebosch, Cape Town 7701, South Africa
  • 2Ocean Systems and Climate Group, CSIR, P.O. Box 320 Stellenbosch, 7599, South Africa
  • 3Department of Zoology, University of Cape Town, Private Bag, Rondebosch, Cape Town 7701, South Africa
  • 4National Oceanographic Centre (NOC), Southampton, SO143ZH, UK
  • 5Department of Earth and Ocean Sciences, 6339 Stores Road, Univ. of British Columbia, Vancouver, BC, V6T 1Z4, Canada
  • 6Department of Zoology, University of Fort Hare, Private Bag X1314, Alice 5700, South Africa

Abstract. During the 1999 Marion Island Oceanographic Survey (MIOS 4) in late austral summer, a northbound and reciprocal southbound transect were taken along the Southwest Indian and Madagascar Ridge, between the Prince Edward Islands and 31° S. The sections crossed a number of major fronts and smaller mesoscale features and covered a wide productivity spectrum from subtropical to subantarctic waters. Associated with the physical survey were measurements of size fractionated chlorophyll, nutrients and nitrogen (NO3, NH4 and urea) uptake rates. Subtropical waters were characterised by low chlorophyll concentrations (max = 0.27.3 mg m−3 dominated by pico-phytoplankton cells (> 81%) and very low f-ratios (< 0.1), indicative of productivity based almost entirely on recycled ammonium and urea. Micro-phytoplankton growth was limited by the availability of NO3 (< 0.5 mmol m−3 and Si(OH)4 (< 1.5 mmol m−3 through strong vertical stratification preventing the upward flux of nutrients into the euphotic zone. Biomass accumulation of small cells was likely controlled by micro-zooplankton grazing. In subantarctic waters, total chlorophyll concentrations increased (max = 0.74 mg m−3 relative to the subtropical waters and larger cells became more prevalent, however smaller phytoplankton cells and low f-ratios (< 0.14) still dominated, despite sufficient NO3 availability. The results from this study favour Si(OH)4 limitation, light-limited deep mixing and likely Fe deficiency as the dominant mechanisms controlling significant new production by micro-phytoplankton. The percentage of micro-phytoplankton cells and rates of new production did however increase at oceanic frontal regions (58.6% and 11.22%, respectively), and in the region of the Prince Edward archipelago (61.4% and 14.16%, respectively). Here, water column stabilization and local Fe-enrichment are thought to stimulate phytoplankton growth rates. Open ocean regions such as these provide important areas for local but significant particulate organic carbon export and biological CO2 draw-down in an overall high nutrient low chlorophyll Southern Ocean.