Wg. Harrison et al., THE KINETICS OF NITROGEN-UTILIZATION IN THE OCEANIC MIXED-LAYER - NITRATE AND AMMONIUM INTERACTIONS AT NANOMOLAR CONCENTRATIONS, Limnology and oceanography, 41(1), 1996, pp. 16-32
The concentration-dependent uptake of nitrate (NO3) and its inhibition
by ammonium (NH4) were surveyed in surface waters of the North Atlant
ic Ocean. Low-level NO3 determinations combined with conventional trac
er methods provided the first comprehensive data set on NO3 utilizatio
n kinetics at nanomolar concentrations. Uptake followed saturation kin
etics described by the Michaelis-Menten equation. The half-saturation
parameter for uptake (K-N) ranged 2-3 orders of magnitude, covarying w
ith ambient NO3 concentrations. K-N concentrations in oceanic waters a
veraged similar to 20-30 nM. NH4 half-saturation parameters could only
be approximated (i.e. K-A + A), but observations suggested that K-A a
nd K-N were of similar magnitude in oceanic waters. Maximum uptake rat
es of nitrate, rho(m(N)), and ammonium, rho(m(A)), covaried, but rho(m
(A)) almost always exceeded rho(m(N)); in oceanic waters, the disparit
y was an order of magnitude or greater. Most of the variability in rho
(m(N)) and rho(m(A)) could be explained by variations in phytoplankton
biomass and temperature. The slope of the uptake vs. concentration re
lationship, alpha, was also investigated but was highly variable and c
ould not be related to any of the oceanographic properties observed; a
lpha(A) was generally greater than alpha(N). Kinetics analysis showed
that NH4 is preferentially utilized over NO3 over the full spectrum of
nitrogen concentrations, nanomolar to micromolar. The inhibition of N
O3 uptake by NH4 was also parameterized using the Michaelis-Menten exp
ression. The inhibition half-saturation parameter (K-i) covaried with
K-N, but K-i concentrations in oceanic waters (similar to 40-50 nM) al
ways exceeded K-N. Maximum inhibition (I-m) was rarely complete (i.e.
I-m < 1), even at 2,000 nM ammonium. Overall, results suggest that nit
rogen utilization parameters currently used in ecosystem models of the
open ocean should be re-examined.