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Links between the phytoplankton community composition and trace metal distribution in summer surface waters of the Atlantic Southern Ocean

dc.contributor.authorViljoen, Johannes J.en_ZA
dc.contributor.authorWeir, Ianen_ZA
dc.contributor.authorFietz, Susanneen_ZA
dc.contributor.authorCloete, Ryanen_ZA
dc.contributor.authorLoock, Jeanen_ZA
dc.contributor.authorPhilibert, Raissaen_ZA
dc.contributor.authorRoychoudhury, Alakendra N.en_ZA
dc.date.accessioned2019-06-20T07:44:58Z
dc.date.available2019-06-20T07:44:58Z
dc.date.issued2019-06-06
dc.identifier.citationViljoen, J. J., et al. 2019. Links between the phytoplankton community composition and trace metal distribution in summer surface waters of the Atlantic Southern Ocean. Frontiers in Marine Science, 6:295, doi:10.3389/fmars.2019.00295en_ZA
dc.identifier.issn2296-7745 (online)
dc.identifier.otherdoi:10.3389/fmars.2019.00295
dc.identifier.urihttp://hdl.handle.net/10019.1/106281
dc.descriptionCITATION: Viljoen, J. J., et al. 2019. Links between the phytoplankton community composition and trace metal distribution in summer surface waters of the Atlantic Southern Ocean. Frontiers in Marine Science, 6:295, doi:10.3389/fmars.2019.00295.en_ZA
dc.descriptionThe original publication is available at https://www.frontiersin.orgen_ZA
dc.descriptionPublication of this article was funded by the Stellenbosch University Open Access Fund.en_ZA
dc.description.abstractThis study assessed changes in the phytoplankton community related to macronutrient and bioactive trace metal distribution in surface waters of the Atlantic sector of the Southern Ocean, between Cape Town and Antarctica along the GEOTRACES GIPY_05 (mainly along prime meridian) transect in summer 2014–2015. Several general community structure features were reaffirmed, such as the restriction of cyanobacteria to the northern Subtropical Zone, while haptophytes, such as Phaeocystis, along with diatoms, dominate the community north of the Polar Front, and diatoms clearly dominate south of the Polar Front. These community structure changes were often linked with macro- and micro-nutrient composition changes. For example, the concentration of diatoms increased southwards with the availability of silica whereas the cyanobacterial contribution in the northern Subtropical Zone appeared to be linked with labile cobalt depletion. However, these links were not consistent along the entire transect, i.e., no individual nutrient, such as silica or iron, was linked to community composition changes across all water masses. Each station showed a rather unique combination of nutrient and community compositions. Our findings also indicated impacts on the phytoplankton community through trace metal distributions that could be related to a deep mixing event at ∼54∘S and to ice melt at ∼65 and 68∘S. The timing of sampling after such trace metal fluxes proved to be an important consideration, particularly where iron appeared to be preferentially depleted to near-limiting concentrations, possibly driving utilization of other metals. The study highlights the importance of considering a suite of trace metals when assessing controls of phytoplankton variability in the open ocean and emphasizes the need for higher resolution trace metal sampling and multi-element incubation studies to further study the complex relationships between phytoplankton and nutrients.en_ZA
dc.description.urihttps://www.frontiersin.org/articles/10.3389/fmars.2019.00295/full
dc.format.extent17 pages : illustrationsen_ZA
dc.language.isoen_ZAen_ZA
dc.publisherFrontiers Mediaen_ZA
dc.subjectPhytoplankton communityen_ZA
dc.subjectPhaeocystis antarcticaen_ZA
dc.subjectTrace metal samplingen_ZA
dc.subjectPhytoplankton productivity in the Southern Oceanen_ZA
dc.titleLinks between the phytoplankton community composition and trace metal distribution in summer surface waters of the Atlantic Southern Oceanen_ZA
dc.typeArticleen_ZA
dc.description.versionPublisher's versionen_ZA
dc.rights.holderAuthors retain copyrighten_ZA


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