English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/25423
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:


DOM fluorescence, a tracer for biogeochemical processes in a coastal upwelling system (NW Iberian Peninsula)

AuthorsNieto-Cid, Mar ; Álvarez-Salgado, Xosé Antón ; Gago, Jesús ; Pérez, Fiz F.
KeywordsDissolved organic matter
Humic substances
Amino acids
Seasonal cycle
Coastal upwelling
NW Iberian Peninsula
Issue Date1-Aug-2005
PublisherInter Research
CitationMarine Ecology Progress Series 297: 33-50 (2005)
AbstractFluorescence of dissolved organic matter (FDOM) was determined for the first time during a complete seasonal cycle in a coastal upwelling system (Ría de Vigo, NW Spain). Specific excitation/emission wavelengths for the refractory humic substances and the labile aromatic amino acids were detected and quantified. The distribution of the fluorescence of marine humic substances (FDOMM) correlated significantly with nutrient salts (r = 0.62, p < 0.001) and dissolved oxygen (r < –0.71, p < 0.001), after removal of the effect of water masses mixing. It suggests that humic substances are a by-product of organic matter mineralisation processes in shelf bottom waters. It was estimated that about 10% of the organic carbon degraded in the water column was transformed into humic substances, which were produced in the ría at a rate of about 0.1 ppb eq (parts per billion equivalents) quinine sulphate d–1. The distribution of the fluorescence of dissolved aromatic amino acids (FDOMT) correlated significantly with the distribution of particulate proteins (r > 0.57, p < 0.001). FDOMT can be used to trace sites of net accumulation of labile DOM in (1) the photic layer (at a rate of about 0.5 ppb eq tryptophan d–1), where labile DOM is produced from phytoplankton exudation and/or lysis and (2) the bottom nepheloid layer (at a rate of about 0.2 ppb eq tryptophan d–1), due to an in situ enhancement of the microbial activity and/or a release from sediment pore waters.
Description18 pages, 9 figures, 2 tables.
Publisher version (URL)http://dx.doi.org/10.3354/meps297033
Appears in Collections:(IIM) Artículos
Files in This Item:
File Description SizeFormat 
m297p033.pdf1,87 MBAdobe PDFThumbnail
Show full item record
Review this work

Related articles:

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