Department of Microbiology and Marine Biogeochemistry, Royal Netherlands Institute for Sea Research (NIOZ), Landsdiep 4, 1797 SZ `t Horntje, the Netherlands
Gert-Jan Reichart
Department of Ocean Systems, Royal Netherlands Institute for Sea Research (NIOZ), Landsdiep 4, 1797 SZ `t Horntje, the Netherlands
Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
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Total article views: 9,054 (including HTML, PDF, and XML)
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Element cycles in oxygen-depleted areas such as upwelling areas inform future deoxygenation scenarios. The Benguela upwelling system shows strong decoupling of nitrogen and phosphorus cycling due to seasonal shelf anoxia. Anaerobic processes result in pelagic nitrogen loss as N2. At the same time, sediments are rich in fish-derived and bacterial phosphorus, with high fluxes of excess phosphate, altering deep-water nitrogen:phosphorus ratios. Such alterations can affect ocean functioning.
Element cycles in oxygen-depleted areas such as upwelling areas inform future deoxygenation...