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Processes Driving Global Interior Ocean pH Distribution ArchiMer
Lauvset, S. K.; Carter, B. R.; Perez, Ff; Jiang, L-q; Feely, R. A.; Velo, A.; Olsen, A..
Ocean acidification evolves on the background of a natural ocean pH gradient that is the result of the interplay between ocean mixing, biological production and remineralization, calcium carbonate cycling, and temperature and pressure changes across the water column. While previous studies have analyzed these processes and their impacts on ocean carbonate chemistry, none have attempted to quantify their impacts on interior ocean pH globally. Here we evaluate how anthropogenic changes and natural processes collectively act on ocean pH, and how these processes set the vulnerability of regions to future changes in ocean acidification. We use the mapped data product from the Global Ocean Data Analysis Project version 2, a novel method to estimate preformed...
Tipo: Text Palavras-chave: PH; Remineralization; CaCO3; Anthropogenic; Global ocean.
Ano: 2020 URL: https://archimer.ifremer.fr/doc/00676/78793/81066.pdf
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Iron isotopes reveal distinct dissolved iron sources and pathways in the intermediate versus deep Southern Ocean ArchiMer
Abadie, Cyril; Lacan, Francois; Radic, Amandine; Pradoux, Catherine; Poitrasson, Franck.
As an essential micronutrient, iron plays a key role in oceanic biogeochemistry. It is therefore linked to the global carbon cycle and climate. Here, we report a dissolved iron (DFe) isotope section in the South Atlantic and Southern Ocean. Throughout the section, a striking DFe isotope minimum (light iron) is observed at intermediate depths (200–1,300 m), contrasting with heavier isotopic composition in deep waters. This unambiguously demonstrates distinct DFe sources and processes dominating the iron cycle in the intermediate and deep layers, a feature impossible to see with only iron concentration data largely used thus far in chemical oceanography. At intermediate depths, the data suggest that the dominant DFe sources are linked to organic matter...
Tipo: Text Palavras-chave: Iron isotopes; GEOTRACES; South Atlantic; Southern Ocean; Remineralization.
Ano: 2017 URL: https://archimer.ifremer.fr/doc/00367/47864/47859.pdf
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