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Does Presence of a Mid-Ocean Ridge Enhance Biomass and Biodiversity? ArchiMer
Priede, Imants G.; Bergstad, Odd Aksel; Miller, Peter I.; Vecchione, Michael; Gebruk, Andrey; Falkenhaug, Tone; Billett, David S. M.; Craig, Jessica; Dale, Andrew C.; Shields, Mark A.; Tilstone, Gavin H.; Sutton, Tracey T.; Gooday, Andrew J.; Inall, Mark E.; Jones, Daniel O. B.; Martinez-vicente, Victor; Menezes, Gui M.; Niedzielski, Tomasz; Sigurosson, Porsteinn; Rothe, Nina; Rogacheva, Antonina; Alt, Claudia H. S.; Brand, Timothy; Abell, Richard; Brierley, Andrew S.; Cousins, Nicola J.; Crockard, Deborah; Hoelzel, A. Rus; Hoines, Age; Letessier, Tom B.; Read, Jane F.; Shimmield, Tracy; Cox, Martin J.; Galbraith, John K.; Gordon, John D. M.; Horton, Tammy; Neat, Francis; Lorance, Pascal.
In contrast to generally sparse biological communities in open-ocean settings, seamounts and ridges are perceived as areas of elevated productivity and biodiversity capable of supporting commercial fisheries. We investigated the origin of this apparent biological enhancement over a segment of the North Mid-Atlantic Ridge (MAR) using sonar, corers, trawls, traps, and a remotely operated vehicle to survey habitat, biomass, and biodiversity. Satellite remote sensing provided information on flow patterns, thermal fronts, and primary production, while sediment traps measured export flux during 2007–2010. The MAR, 3,704,404 km2 in area, accounts for 44.7% lower bathyal habitat (800–3500 m depth) in the North Atlantic and is dominated by fine soft sediment...
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Ano: 2013 URL: http://archimer.ifremer.fr/doc/00135/24650/22683.pdf
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Southern Ocean deep-water carbon export enhanced by natural iron fertilization ArchiMer
Pollard, Raymond T.; Salter, Ian; Sanders, Richard J.; Lucas, Mike I.; Moore, C. Mark; Mills, Rachel A.; Statham, Peter J.; Allen, John T.; Baker, Alex R.; Bakker, Dorothee C. E.; Charette, Matthew A.; Fielding, Sophie; Fones, Gary R.; French, Megan; Hickman, Anna E.; Holland, Ross J.; Hughes, J. Alan; Jickells, Timothy D.; Lampitt, Richard S.; Morris, Paul J.; Nedelec, Florence; Nielsdottir, Maria; Planquette, Helene; Popova, Ekaterina E.; Poulton, Alex J.; Read, Jane F.; Seeyave, Sophie; Smith, Tania; Stinchcombe, Mark; Taylor, Sarah; Thomalla, Sandy; Venables, Hugh J.; Williamson, Robert; Zubkov, Mike V..
The addition of iron to high- nutrient, low- chlorophyll regions induces phytoplankton blooms that take up carbon(1-3). Carbon export from the surface layer and, in particular, the ability of the ocean and sediments to sequester carbon for many years remains, however, poorly quantified(3). Here we report data from the CROZEX experiment(4) in the Southern Ocean, which was conducted to test the hypothesis that the observed north - south gradient in phytoplankton concentrations in the vicinity of the Crozet Islands is induced by natural iron fertilization that results in enhanced organic carbon flux to the deep ocean. We report annual particulate carbon fluxes out of the surface layer, at three kilometres below the ocean surface and to the ocean floor. We...
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Ano: 2009
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