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Changing biogeochemistry of the Southern Ocean and its ecosystem implications


Henley, SF and Cavan, EL and Fawcett, SE and Kerr, R and Monteiro, T and Sherrell, RM and Bowie, AR and Boyd, PW and Barnes, DKA and Schloss, IR and Marshall, T and Flynn, R and Smith, S, Changing biogeochemistry of the Southern Ocean and its ecosystem implications, Frontiers in Marine Science, 7 Article 581. ISSN 2296-7745 (2020) [Refereed Article]


Copyright Statement

Copyright 2020 Henley, Cavan, Fawcett, Kerr, Monteiro, Sherrell, Bowie, Boyd, Barnes, Schloss, Marshall, Flynn and Smith. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY)

DOI: doi:10.3389/fmars.2020.00581


The Southern Ocean plays a critical role in regulating global climate as a major sink for atmospheric carbon dioxide (CO2), and in global ocean biogeochemistry by supplying nutrients to the global thermocline, thereby influencing global primary production and carbon export. Biogeochemical processes within the Southern Ocean regulate regional primary production and biological carbon uptake, primarily through iron supply, and support ecosystem functioning over a range of spatial and temporal scales. Here, we assimilate existing knowledge and present new data to examine the biogeochemical cycles of iron, carbon and major nutrients, their key drivers and their responses to, and roles in, contemporary climate and environmental change. Projected increases in iron supply, coupled with increases in light availability to phytoplankton through increased near-surface stratification and longer ice-free periods, are very likely to increase primary production and carbon export around Antarctica. Biological carbon uptake is likely to increase for the Southern Ocean as a whole, whilst there is greater uncertainty around projections of primary production in the Sub-Antarctic and basin-wide changes in phytoplankton species composition, as well as their biogeochemical consequences. Phytoplankton, zooplankton, higher trophic level organisms and microbial communities are strongly influenced by Southern Ocean biogeochemistry, in particular through nutrient supply and ocean acidification. In turn, these organisms exert important controls on biogeochemistry through carbon storage and export, nutrient recycling and redistribution, and benthic-pelagic coupling. The key processes described in this paper are summarised in the Graphical Abstract. Climate-mediated changes in Southern Ocean biogeochemistry over the coming decades are very likely to impact primary production, sea-air CO2 exchange and ecosystem functioning within and beyond this vast and critically important ocean region.

Item Details

Item Type:Refereed Article
Keywords:Southern Ocean, biogeochemistry, primary production, iron, nutrients, carbon, ecosystem, ocean acidification
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Chemical oceanography
Objective Division:Environmental Management
Objective Group:Marine systems and management
Objective Field:Measurement and assessment of marine water quality and condition
UTAS Author:Bowie, AR (Professor Andrew Bowie)
UTAS Author:Boyd, PW (Professor Philip Boyd)
ID Code:150207
Year Published:2020
Web of Science® Times Cited:58
Deposited By:Oceans and Cryosphere
Deposited On:2022-06-02
Last Modified:2022-08-24
Downloads:8 View Download Statistics

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