Articles | Volume 14, issue 5
https://doi.org/10.5194/bg-14-1123-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/bg-14-1123-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Manganese in the west Atlantic Ocean in the context of the first global ocean circulation model of manganese
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL,
CEA–Orme des Merisiers, 91191 Gif-sur-Yvette, France
Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA De Bilt, the Netherlands
Rob Middag
Department of Chemistry, NIWA/University of Otago Research Centre for
Oceanography, Dunedin 9054, New Zealand
Department of Ocean Sciences & Institute of Marine Sciences,
University of California Santa Cruz, CA 95064, USA
NIOZ Royal Netherlands Institute for Sea Research, Department of Ocean
Systems, and Utrecht University, P.O. Box 59, 1790 AB Den Burg, Texel, the Netherlands
Jean-Claude Dutay
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL,
CEA–Orme des Merisiers, 91191 Gif-sur-Yvette, France
Hein de Baar
NIOZ Royal Netherlands Institute for Sea Research, Department of Ocean
Systems, and Utrecht University, P.O. Box 59, 1790 AB Den Burg, Texel, the Netherlands
University of Groningen (RUG), Postbus 72, 9700 AB Groningen, the Netherlands
Matthieu Roy-Barman
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL,
CEA–Orme des Merisiers, 91191 Gif-sur-Yvette, France
Marion Gehlen
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL,
CEA–Orme des Merisiers, 91191 Gif-sur-Yvette, France
Alessandro Tagliabue
University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, UK
Andreas Sterl
Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA De Bilt, the Netherlands
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- Resource Availability and Entrainment Are Driven by Offsets Between Nutriclines and Winter Mixed‐Layer Depth S. Rigby et al. 10.1029/2019GB006497
- Low cerium among the dissolved rare earth elements in the central North Pacific Ocean H. de Baar et al. 10.1016/j.gca.2018.03.003
- Replacement Times of a Spectrum of Elements in the North Atlantic Based on Thorium Supply C. Hayes et al. 10.1029/2017GB005839
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- Elemental composition of suspended particles across the southeastern continental shelf off the coast of North Florida and South Georgia: Provenance, transport, fate and implications to mid-outer shelf water column processes. H. Windom 10.1016/j.csr.2019.03.005
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- Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6 R. Séférian et al. 10.1007/s40641-020-00160-0
- Response of Dissolved Trace Metals to Dust Storms, Sediment Resuspension, and Flash Floods in Oligotrophic Oceans T. Benaltabet et al. 10.1029/2023GB007858
- A hydrothermal plume on the Southwest Indian Ridge revealed by a multi-proxy approach: Impact on iron and manganese distributions (GEOTRACES GS02) C. Baudet et al. 10.1016/j.marchem.2024.104401
- A global biogeography analysis reveals vulnerability of surface marine zooplankton to anthropogenic stressors C. Richon et al. 10.1016/j.oneear.2023.12.002
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Short summary
We ran a global ocean model to understand manganese (Mn), a biologically essential element. Our model shows that (i) in the deep ocean, dissolved [Mn] is mostly homogeneous ~0.10—0.15 nM. The model reproduces this with a threshold on MnO2 of 25 pM, suggesting a minimal particle concentration is needed before aggregation and removal become efficient.
(ii) The observed distinct hydrothermal signals are produced by assuming both a strong source and a strong removal of Mn near hydrothermal vents.
We ran a global ocean model to understand manganese (Mn), a biologically essential element. Our...
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