4.7 Article

Changing Biogeochemistry of the Southern Ocean and Its Ecosystem Implications

期刊

FRONTIERS IN MARINE SCIENCE
卷 7, 期 -, 页码 -

出版社

FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2020.00581

关键词

Southern Ocean; biogeochemistry; primary production; iron; nutrients; carbon; ecosystem; ocean acidification

资金

  1. United Kingdom Natural Environment Research Council [NE/S000348/1, NE/K010034/1]
  2. South African National Research Foundation's Antarctic Programme (SANAP) [105539, 110735]
  3. UCT Vice-Chancellor's Future Leaders 2030 award
  4. DSI's Biogeochemistry Research Infrastructure Platform (BIOGRIP)
  5. CNPq [304937/20185]
  6. CAPES [88887.360799/201900]
  7. PROVOCCAR project grant from CNPq/PROANTAR [442628/2018-8]
  8. Australian Research Council [FT130100037, DP150100345, DP190103504]
  9. Antarctic Climate and Ecosystems Cooperative Research Centre
  10. Laureate Fellowship from the Australian Research Council [FL160100131]
  11. UCT Vice Chancellor Doctoral Research Scholarships
  12. UCT Postgraduate Funding Merit Awards
  13. South African National Research Foundation [114590]
  14. UCT Science Faculty Fellowship
  15. NERC [bas0100036, NE/S000348/1, NE/K010034/1] Funding Source: UKRI

向作者/读者索取更多资源

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.

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