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Nitrogen cycling in the Barents Sea–Seasonal dynamics of new and regenerated production in the marginal ice zone
Author(s) -
Kristiansen Svein,
Farbrot Tove,
Wheeler Patricia A,
Publication year - 1994
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.1994.39.7.1630
Subject(s) - bloom , ammonium , nitrogen , nitrate , new production , phytoplankton , nutrient , algal bloom , ammonium nitrate , chemistry , oceanography , zoology , environmental science , botany , biology , geology , organic chemistry
The uptake rates of nitrate, ammonium, and urea were measured with a 15 N technique during seven cruises in the marginal ice zone (MIZ) in the Barents Sea in 1984–1988. The results from all the cruises were pooled to obtain means for the prebloom, bloom, transition, and postbloom periods. New production—nitrate uptake as percent of total uptake—was high (92–96%) during the prebloom and bloom periods and decreased thereafter. Regenerated production—summed ammonium + urea uptake as percent of total uptake—increased through the bloom cycle and was at its maximum (75–93%) during the postbloom period. New production (as percent of the total) was higher in the ice‐filled parts than in the icefree parts, especially during the postbloom period. Nitrate uptake rates, however, were highest (9–25 nM h −1 ) in open and ice‐free parts during the bloom and transition period. Mean growth rate of phytoplankton‐nitrogen was 0.5 doubling d −1 during the bloom and ranged from 0.3 to 0.4 doubling d −1 after the bloom. We hypothesize that primary production in the MIZ is not nutrient limited but is proportional to phytoplankton standing stocks.