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dc.contributor.authorWinton, Victoria
dc.contributor.authorEdwards, R.
dc.contributor.authorDelmonte, B.
dc.contributor.authorEllis, A.
dc.contributor.authorAndersson, P.
dc.contributor.authorBowie, A.
dc.contributor.authorBertler, N.
dc.contributor.authorNeff, P.
dc.contributor.authorTuohy, A.
dc.date.accessioned2017-01-30T12:05:44Z
dc.date.available2017-01-30T12:05:44Z
dc.date.created2016-05-15T19:30:28Z
dc.date.issued2016
dc.identifier.citationWinton, V. and Edwards, R. and Delmonte, B. and Ellis, A. and Andersson, P. and Bowie, A. and Bertler, N. et al. 2016. Multiple sources of soluble atmospheric iron to Antarctic waters. Global Biogeochemical Cycles. 30 (3): pp. 421-437.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/18054
dc.identifier.doi10.1002/2015GB005265
dc.description.abstract

The Ross Sea, Antarctica, is a highly productive region of the Southern Ocean. Significant new sources of iron (Fe) are required to sustain phytoplankton blooms in the austral summer. Atmospheric deposition is one potential source. The fractional solubility of Fe is an important variable determining Fe availability for biological uptake. To constrain aerosol Fe inputs to the Ross Sea region, fractional solubility of Fe was analyzed in a snow pit from Roosevelt Island, eastern Ross Sea. In addition, aluminum, dust, and refractory black carbon (rBC) concentrations were analyzed, to determine the contribution of mineral dust and combustion sources to the supply of aerosol Fe. We estimate exceptionally high dissolved Fe (dFe) flux of 1.2 × 10-6 g m-2 y-1 and total dissolvable Fe flux of 140 × 10-6 g m-2 y-1 for 2011/2012. Deposition of dust, Fe, Al, and rBC occurs primarily during spring-summer. The observed background fractional Fe solubility of ~0.7% is consistent with a mineral dust source. Radiogenic isotopic ratios and particle size distribution of dust indicates that the site is influenced by local and remote sources. In 2011/2012 summer, relatively high dFe concentrations paralleled both mineral dust and rBC deposition. Around half of the annual aerosol Fe deposition occurred in the austral summer phytoplankton growth season; however, the fractional Fe solubility was low. Our results suggest that the seasonality of dFe deposition can vary and should be considered on longer glacial-interglacial timescales.

dc.publisherWiley-Blackwell Publishing
dc.titleMultiple sources of soluble atmospheric iron to Antarctic waters
dc.typeJournal Article
dcterms.source.volume30
dcterms.source.number3
dcterms.source.startPage421
dcterms.source.endPage437
dcterms.source.issn0886-6236
dcterms.source.titleGlobal Biogeochemical Cycles
curtin.departmentDepartment of Physics and Astronomy
curtin.accessStatusFulltext not available


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