Ammonium Recycling Limits Nitrate Use in the Oceanic Subarctic Pacific
Seasonal and diel changes in nutrient concentrations and nitrogen assimilation rates were used to assess the effects of $NH_4^+$ on $NO_3^-$ assimilation. Surface-water $NO_3^-$ concentrations ranged from 6 to $17 \mu M while NH_4^+$ concentrations ranged from 0 to $0.4 \mu M$. Total N assimilation...
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Published in: | Limnology and oceanography Vol. 35; no. 6; pp. 1267 - 1278 |
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Main Authors: | , |
Format: | Journal Article |
Language: | English |
Published: |
Waco, TX
American Society of Limnology and Oceanography
01-09-1990
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Subjects: | |
Online Access: | Get full text |
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Summary: | Seasonal and diel changes in nutrient concentrations and nitrogen assimilation rates were used to assess the effects of $NH_4^+$ on $NO_3^-$ assimilation. Surface-water $NO_3^-$ concentrations ranged from 6 to $17 \mu M while NH_4^+$ concentrations ranged from 0 to $0.4 \mu M$. Total N assimilation ranged from 84 to $732 nM d^-1$ but showed no seasonal trend. $NH_4^+$ and urea concentrations were <1% of total dissolved inorganic N, but use of this "regenerated" N still accounted for 44-89% of total N assimilation. Rates of $NO_3^-$ assimilation were negatively correlated with ambient $NH_4^+$ concentrations, and concentrations of $NH_4^+$ between 0.1 and $0.3 \mu M$ caused complete inhibition of $NO_3^-$ assimilation $NO_3^-$ was more important as a source of N in spring than in summer. We attribute this pattern to a summer increase in turnover rates for $NH_4^+$. Turnover times for the dissolved $NH_4^+$ pool were half as long in August as in May. Grazing and recycling in the euphotic zone apparently both play significant roles in preventing depletion of $NO_3^-$ in the oceanic subarctic Pacific. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0024-3590 1939-5590 |
DOI: | 10.4319/lo.1990.35.6.1267 |