English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/93821
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

Title

Carbon Dynamics within Cyclonic Eddies: Insights from a Biomarker Study

AuthorsAlonso-González, Iván J.; Arístegui, Javier; Lee, Cindy; Sánchez-Vidal, Anna; Calafat, Antoni; Fabrés, Joan; Sangrà, Pablo; Mason, Evan
Issue DateDec-2013
PublisherPublic Library of Science
CitationPLoS ONE 8(12): e82447 (2013)
AbstractIt is generally assumed that episodic nutrient pulses by cyclonic eddies into surface waters support a significant fraction of the primary production in subtropical low-nutrient environments in the northern hemisphere. However, contradictory results related to the influence of eddies on particulate organic carbon (POC) export have been reported. As a step toward understanding the complex mechanisms that control export of material within eddies, we present here results from a sediment trap mooring deployed within the path of cyclonic eddies generated near the Canary Islands over a 1.5-year period. We find that, during summer and autumn (when surface stratification is stronger, eddies are more intense, and a relative enrichment in CaCO3 forming organisms occurs), POC export to the deep ocean was 2-4 times higher than observed for the rest of the year. On the contrary, during winter and spring (when mixing is strongest and the seasonal phytoplankton bloom occurs), no significant enhancement of POC export associated with eddies was observed. Our biomarker results suggest that a large fraction of the material exported from surface waters during the late-winter bloom is either recycled in the mesopelagic zone or bypassed by migrant zooplankton to the deep scattering layer, where it would disaggregate to smaller particles or be excreted as dissolved organic carbon. Cyclonic eddies, however, would enhance carbon export below 1000 m depth during the summer stratification period, when eddies are more intense and frequent, highlighting the important role of eddies and their different biological communities on the regional carbon cycle. © 2013 Alonso-González et al.
Description10 pages, 7 figures, 1 table
Publisher version (URL)http://dx.doi.org/10.1371/journal.pone.0082447
URIhttp://hdl.handle.net/10261/93821
DOI10.1371/journal.pone.0082447
Identifiersdoi: 10.1371/journal.pone.0082447
issn: 1932-6203
Appears in Collections:(ICM) Artículos
(IMEDEA) Artículos
Files in This Item:
File Description SizeFormat 
Alonso_et_al_2013.pdf2,62 MBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.