2020
DOI: 10.3389/fmars.2020.00581
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Changing Biogeochemistry of the Southern Ocean and Its Ecosystem Implications

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Cited by 145 publications
(170 citation statements)
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References 331 publications
(479 reference statements)
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“…Nevertheless, there is good agreement amongst CMIP5 models that Southern Ocean NPP will increase overall as a result of increased iron supply, changes in mixed layer depth, declining sea ice cover, increasing SST and altered westerly winds (Bopp et al, 2013;Leung et al, 2015;Fu et al, 2016;Moore et al, 2018). Increased iron supply and temperature could also lead to a floristic shift to diatoms and potentially Phaeocystis antarctica, with consequences for benthic and pelagic consumers as well as nutrient uptake, carbon export and large-scale biogeochemical cycling (Henley et al, 2020).…”
Section: Increasing Iron Inputs and Freshwater Flux From Glacial Ice mentioning
confidence: 95%
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“…Nevertheless, there is good agreement amongst CMIP5 models that Southern Ocean NPP will increase overall as a result of increased iron supply, changes in mixed layer depth, declining sea ice cover, increasing SST and altered westerly winds (Bopp et al, 2013;Leung et al, 2015;Fu et al, 2016;Moore et al, 2018). Increased iron supply and temperature could also lead to a floristic shift to diatoms and potentially Phaeocystis antarctica, with consequences for benthic and pelagic consumers as well as nutrient uptake, carbon export and large-scale biogeochemical cycling (Henley et al, 2020).…”
Section: Increasing Iron Inputs and Freshwater Flux From Glacial Ice mentioning
confidence: 95%
“…One of the most important functions of the SO in the Earth System is its uptake of atmospheric CO 2 by physical and biological processes and its release of oceanic CO 2 to the atmosphere (Sarmiento and Le Quere, 1996;Marinov et al, 2006;Gruber et al, 2009Gruber et al, , 2019Lenton et al, 2013;Henley et al, 2020 this volume). However, this uptake is leading to changes in ocean biogeochemistry, which could have devastating consequences for the ecosystem.…”
Section: Biogeochemistry Co 2 Uptake and Ocean Acidificationmentioning
confidence: 99%
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“…While covering only 30% of the global ocean's surface, it is predicted to account up to 75% of the heat uptake (Frölicher et al, 2015), underlining its importance under the reported and predicted impacts of anthropogenic-driven climate change. Thus, a better understanding of Southern Ocean processes on a circumpolar and regional scales and their vulnerability is urgent, especially considering that climate-driven changes over its biogeochemistry likely to impact from primary producers to changes on the ecosystem functioning (Henley et al, 2020).…”
Section: Introductionmentioning
confidence: 99%