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dc.contributor.authorDurkin, Colleen A.  Concept link
dc.contributor.authorEstapa, Margaret L.  Concept link
dc.contributor.authorBuesseler, Ken O.  Concept link
dc.date.accessioned2015-08-26T14:39:06Z
dc.date.available2015-08-26T14:39:06Z
dc.date.issued2015-02-27
dc.identifier.citationMarine Chemistry 175 (2015): 72-81en_US
dc.identifier.urihttps://hdl.handle.net/1912/7505
dc.description© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Marine Chemistry 175 (2015): 72-81, doi:10.1016/j.marchem.2015.02.011.en_US
dc.description.abstractCarbon and nutrients are transported out of the surface ocean and sequestered at depth by sinking particles. Sinking particle sizes span many orders of magnitude and the relative influence of small particles on carbon export compared to large particles has not been resolved. To determine the influence of particle size on carbon export, the flux of both small (11–64 μm) and large (> 64 μm) particles in the upper mesopelagic was examined during 5 cruises of the Bermuda Atlantic Time Series (BATS) in the Sargasso Sea using neutrally buoyant sediment traps mounted with tubes containing polyacrylamide gel layers and tubes containing a poisoned brine layer. Particles were also collected in surface-tethered, free-floating traps at higher carbon flux locations in the tropical and subtropical South Atlantic Ocean. Particle sizes spanning three orders of magnitude were resolved in gel samples, included sinking particles as small as 11 μm. At BATS, the number flux of small particles tended to increase with depth, whereas the number flux of large particles tended to decrease with depth. The carbon content of different sized particles could not be modeled by a single set of parameters because the particle composition varied across locations and over time. The modeled carbon flux by small particles at BATS, including all samples and depths, was 39 ± 20% of the modeled total carbon flux, and the percentage increased with depth in 4 out of the 5 months sampled. These results indicate that small particles (< 64 μm) are actively settling in the water column and are an important contributor to carbon flux throughout the mesopelagic. Observations and models that overlook these particles will underestimate the vertical flux of organic matter in the ocean.en_US
dc.description.sponsorshipFunding for this study was provided by the National Science Foundation Chemical Oceanography Program (OCE-1260001 and 1406552 to M. L. Estapa) and the Woods Hole Oceanographic Institution Devonshire Postdoctoral Scholarship awarded to C. A. Durkin. Funding for the DeepDOM cruise was provided by the National Science Foundation Chemical Oceanography Program (OCE-1154320 to E. B. Kujawinski and K. Longnecker, WHOI).en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherElsevieren_US
dc.relation.urihttps://doi.org/10.1016/j.marchem.2015.02.011
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectParticle sizeen_US
dc.subjectParticle settlingen_US
dc.subjectCarbon cycleen_US
dc.subjectSediment trapsen_US
dc.subjectMesopelagic zoneen_US
dc.titleObservations of carbon export by small sinking particles in the upper mesopelagicen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.marchem.2015.02.011


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Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 International