Nutrient distributions in an anticyclonic eddy in the northeast Atlantic Ocean, with reference to nanomolar ammonium concentrations

Citation
Ems. Woodward et Ap. Rees, Nutrient distributions in an anticyclonic eddy in the northeast Atlantic Ocean, with reference to nanomolar ammonium concentrations, DEEP-SEA II, 48(4-5), 2001, pp. 775-793
Citations number
33
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
ISSN journal
09670645 → ACNP
Volume
48
Issue
4-5
Year of publication
2001
Pages
775 - 793
Database
ISI
SICI code
0967-0645(2001)48:4-5<775:NDIAAE>2.0.ZU;2-L
Abstract
The micromolar concentrations of nitrate, nitrite, silicate, phosphate and ammonium; and the nanomolar concentrations of nitrate, nitrite and ammonium were studied during a Lagrangian study of an anti-cyclonic eddy situated i n the Iceland Basin of the North Atlantic Ocean. Underway surface transects , carried out across the eddy at the beginning and end of the survey period of 2 weeks, showed a decrease in the surface-water concentrations of nitra te and phosphate, with a concomitant increase in the phytoplankton biomass and surface-water temperature. The trajectory of the eddy was tracked by a release of SF6 tracer, and regular water column sampling was carried out at the centre of the tracer patch over a period of 11 days. A storm after the first 5 days of the cruise brought about a transport into the surface mixe d layer of colder sub-thermocline waters, which resulted in significant nut rient enrichment of nitrate, phosphate and silicate in the euphotic zone. T his transport of nutrients, in particular nitrate, into the surface-mixed l ayer demonstrates the importance of eddies in the open ocean for sustaining 'new' production within the euphotic zone. We also report observations of a mmonium at concentrations from 45 to 935 nmol l(-1) for the northeast Atlan tic using an automated analytical system. The presence of an ammonium maxim um in the water column related to the thermocline, chlorophyll maximum, and the primary nitrite maximum. (C) 2001 Elsevier Science Ltd. All rights res erved.