The relative roles of modified circumpolar deep water and benthic sources in supplying iron to the recurrent phytoplankton blooms above Pennell and Mawson Banks, Ross Sea, Antarctica

• Published in: Journal of marine systems Vol. 166; pp. 61 - 72
• Main Authors: Hatta, Mariko, Measures, Chris I., Lam, Phoebe J., Ohnemus, Daniel C., Auro, Maureen E., Grand, Maxime M., Selph, Karen E.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-02-2017
• Subjects: Antarctica; Banks; Blooms; Deep water; Iron; Lead (metal); Manganese; Marine; Modified circumpolar deep water; Ross Sea; Stations; Surface water; Water mixing; PS, Antarctica; PS, Ross Sea; Banks; Ross Sea; Iron; Water mixing; Modified circumpolar deep water; Manganese
• ISSN: 0924-7963; 1879-1573
• DOI: 10.1016/j.jmarsys.2016.07.009

The role that dissolved iron (dFe) rich Circumpolar Deep Water (CDW) might play in sustaining the consistently observed discrete patches of high chlorophyll biomass over Pennell Bank (PB) and Mawson Bank (MB) in the Ross Sea, was investigated during January/February 2011. Over a 26-day period, hydrographic and trace metal clean water sampling was carried out adjacent to both of these banks, in some cases repeatedly. Particulate sampling was also accomplished at selected stations by in situ pumping. The results indicate that the dFe content of the CDW is in fact reduced by on-shelf mixing with Antarctic Surface Water as it transitions into modified CDW (MCDW). Our stations above PB, where the maximum bloom is encountered, show no evidence of MCDW presence. In contrast, above MB, where there is a smaller persistent bloom, MCDW was observed. Although both of these stations displayed the imprint of sedimentary Fe input connected to the strong tidal cycles above the banks, the stronger near-bottom density gradient that MCDW produces appears to contribute to reduced vertical mixing of the sedimentary source. Thus, ironically, the presence of MCDW may be hindering the Fe supply to the surface waters, rather than being the source, as originally hypothesized.
•Dissolved Fe within the CDW is diluted by mixing with AASW during the formation of MCDW in the Ross Sea.•MCDW was seen above Mawson Bank but not Pennell Bank.•A sedimentary input of Fe is seen above Pennell Bank.•Strong tidal energy over shallow banks brings Fe-rich deep waters to the euphotic zone.•The presence of MCDW above Mawson Bank hinders mixing of dFe into the euphotic zone.