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MEPS 288:35-43 (2005)
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Abstract
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Ammonium cycling under a strong oxygen gradient associated with the Oxygen Minimum Zone off northern Chile (~23°S)
Verónica Molina1,2,3,*, Laura Farías2,3,4, Yoanna Eissler3, Luis Antonio Cuevas1,3,Carmen E. Morales3,4, Rubén Escribano3,4
1Programa de Postgrado, Departamento Oceanografía, 2Programa Regional de Oceanografía Física y Clima (PROFC), 3Centro de Investigación Oceanográfica en el Pacífico Sur-Oriental
(FONDAP-COPAS), 4Departamento de Oceanografía, Universidad de Concepción, PO Box 160-C, Correo 3, Concepción, Chile
*Email: vemolina@udec.cl

ABSTRACT: Ammonium (NH4+) cycling rates under different dissolved oxygen (DO) conditions in the water column, at a coastal upwelling area off northern Chile (~23°S), were estimated. Net NH4+ regeneration
(eukaryotes and prokaryotes) and NH4+ oxidation (nitrifying bacteria) rates were examined by means of selective inhibitor assays (cycloheximide and allylthiourea) under dark conditions. Whole water samples for incubations were taken
in the oxycline, low-DO zone (30 m; 69 µM DO), and in the upper boundary of the Oxygen Minimum Zone (OMZ), suboxic zone (50 m; <5 µM DO). Net NH4+ regeneration and consumption were also determined in size-fractionated
(<200 µm) experiments with water samples obtained from the suboxic zone (50 m) and the base of the mixed layer, oxic zone (15 m; 104 µM DO). Results indicate that, in the oxycline, prokaryotes were responsible for most of the
NH4+ cycling, with regeneration and oxidation rates of ~1.3 and 0.56 µM d1, respectively. This, in turn, favoured NH4+ and NO3 accumulation in this layer,
characterised by strong physicalchemical gradients (temperature, salinity and DO), and accompanied by lower abundances of cyanobacteria (0.09 × 105 cells ml1) and heterotrophic nanoflagellates (HNF; 15.6 cells
ml1). In the oxic and suboxic layers, eukaryotes appear to be the main contributors to net NH4+ regeneration (4.6 to 17.7 µM d1), supporting a high net NH4+ dark
prokaryote consumption, including high potential NH4+ oxidation (0.95 to 1.34 µM d1) in the suboxic zone. The abundances of bacteria, cyanobacteria and HNF were higher in these layers (>1.2 ×
106, >0.9 × 105 and >37 cells ml1, respectively), indicating a potential large impact on NH4+ cycling.
KEY WORDS: Ammonium regeneration · Nitrification potential · Bacterioplankton · Heterotrophic nanoflagellates · Oxygen Minimum Zone · Upwelling area · Northern Chile
Full text in pdf format

Published in MEPS Vol.
288
(2005) on March 10
Print ISSN: 0171-8630; Online ISSN: 1616-1599.
Copyright © Inter-Research, Oldendorf/Luhe, 2005
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