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dc.contributor.authorSaito, Mak A.  Concept link
dc.contributor.authorNoble, Abigail E.  Concept link
dc.contributor.authorHawco, Nicholas J.  Concept link
dc.contributor.authorTwining, Benjamin S.  Concept link
dc.contributor.authorOhnemus, Daniel C.  Concept link
dc.contributor.authorJohn, Seth G.  Concept link
dc.contributor.authorLam, Phoebe J.  Concept link
dc.contributor.authorConway, Tim M.  Concept link
dc.contributor.authorJohnson, Rod  Concept link
dc.contributor.authorMoran, Dawn M.  Concept link
dc.contributor.authorMcIlvin, Matthew R.  Concept link
dc.date.accessioned2017-11-16T16:50:15Z
dc.date.available2017-11-16T16:50:15Z
dc.date.issued2017-10-20
dc.identifier.citationBiogeosciences 14 (2017): 4637-4662en_US
dc.identifier.urihttps://hdl.handle.net/1912/9376
dc.description© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 14 (2017): 4637-4662, doi:10.5194/bg-14-4637-2017.en_US
dc.description.abstractThe stoichiometry of biological components and their influence on dissolved distributions have long been of interest in the study of the oceans. Cobalt has the smallest oceanic inventory of inorganic micronutrients and hence is particularly vulnerable to influence by internal oceanic processes including euphotic zone uptake, remineralization, and scavenging. Here we observe not only large variations in dCo : P stoichiometry but also the acceleration of those dCo : P ratios in the upper water column in response to several environmental processes. The ecological stoichiometry of total dissolved cobalt (dCo) was examined using data from a US North Atlantic GEOTRACES transect and from a zonal South Atlantic GEOTRACES-compliant transect (GA03/3_e and GAc01) by Redfieldian analysis of its statistical relationships with the macronutrient phosphate. Trends in the dissolved cobalt to phosphate (dCo : P) stoichiometric relationships were evident in the basin-scale vertical structure of cobalt, with positive dCo : P slopes in the euphotic zone and negative slopes found in the ocean interior and in coastal environments. The euphotic positive slopes were often found to accelerate towards the surface and this was interpreted as being due to the combined influence of depleted phosphate, phosphorus-sparing (conserving) mechanisms, increased alkaline phosphatase metalloenzyme production (a zinc or perhaps cobalt enzyme), and biochemical substitution of Co for depleted Zn. Consistent with this, dissolved Zn (dZn) was found to be drawn down to only 2-fold more than dCo, despite being more than 18-fold more abundant in the ocean interior. Particulate cobalt concentrations increased in abundance from the base of the euphotic zone to become  ∼  10 % of the overall cobalt inventory in the upper euphotic zone with high stoichiometric values of  ∼  400 µmol Co mol−1 P. Metaproteomic results from the Bermuda Atlantic Time-series Study (BATS) station found cyanobacterial isoforms of the alkaline phosphatase enzyme to be prevalent in the upper water column, as well as a sulfolipid biosynthesis protein indicative of P sparing. The negative dCo : P relationships in the ocean interior became increasingly vertical with depth, and were consistent with the sum of scavenging and remineralization processes (as shown by their dCo : P vector sums). Attenuation of the remineralization with depth resulted in the increasingly vertical dCo : P relationships. Analysis of particulate Co with particulate Mn and particulate phosphate also showed positive linear relationships below the euphotic zone, consistent with the presence and increased relative influence of Mn oxide particles involved in scavenging. Visualization of dCo : P slopes across an ocean section revealed hotspots of scavenging and remineralization, such as at the hydrothermal vents and below the oxygen minimum zone (OMZ) region, respectively, while that of an estimate of Co* illustrated stoichiometrically depleted values in the mesopelagic and deep ocean due to scavenging. This study provides insights into the coupling between the dissolved and particulate phase that ultimately creates Redfield stoichiometric ratios, demonstrating that the coupling is not an instantaneous process and is influenced by the element inventory and rate of exchange between phases. Cobalt's small water column inventory and the influence of external factors on its biotic stoichiometry can erode its limited inertia and result in an acceleration of the dissolved stoichiometry towards that of the particulate phase in the upper euphotic zone. As human use of cobalt grows exponentially with widespread adoption of lithium ion batteries, there is a potential to affect the limited biogeochemical inertia of cobalt and its resultant ecology in the oceanic euphotic zone.en_US
dc.description.sponsorshipThis work was funded by the National Science Foundation as part of the US GEOTRACES North Atlantic Zonal Transect program under grants OCE-0928414 and OCE-1435056 (to Mak A. Saito), OCE-0928289 (to Benjamin S. Twining), OCE-0963026 (to Phoebe Lam) and support from the Gordon and Betty Moore Foundation (3782 to Mak A. Saito).en_US
dc.language.isoen_USen_US
dc.publisherCopernicus Publications on behalf of the European Geosciences Unionen_US
dc.relation.urihttps://doi.org/10.5194/bg-14-4637-2017
dc.rightsAttribution 3.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/
dc.titleThe acceleration of dissolved cobalt's ecological stoichiometry due to biological uptake, remineralization, and scavenging in the Atlantic Oceanen_US
dc.typeArticleen_US
dc.identifier.doi10.5194/bg-14-4637-2017


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Attribution 3.0 Unported
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