X. Chen et al., Distribution and controlling mechanisms of primary production on the Louisiana-Texas continental shelf, J MAR SYST, 25(2), 2000, pp. 179-207
The northwest (NW) Gulf of Mexico is marked by strong seasonal patterns in
regional and mesoscale circulation and variable effects of riverine/estuari
ne discharge, which influence distributions of nutrients, phytoplankton bio
mass and primary production. During a series of five cruises in the NW Gulf
of Mexico in 1993 and 1994, an extensive data set was collected including
nutrients, phytoplankton biomass (chlorophyll a), and photosynthesis-irradi
ance (P-E) parameters. Primary production was estimated using P-E parameter
s in conjunction with profiles of biomass and irradiance. Relatively high b
iomass and primary production were observed in inner shelf waters during sp
ring conditions of high river discharge. This was attributed to the retenti
on of biomass and nutrients on the shelf by the combination of high river o
utflow and a westward flow along the inner shelf with consequent onshore Ek
man component. During summer, when surface currents shifted towards the nor
th and east, values of nutrients, biomass and primary production were relat
ively high east of Galveston Bay and decreased outward from the coast. This
pattern was apparently a consequence of nutrient inputs from riverine, upw
elling and benthic sources. Nutrients, biomass and productivity in the west
ern portion of the study area in summer were generally lower as a result of
the upcoast Row of oligotrophic offshore water. Inter-annual variability w
as observed between November 1993 and 1994 with higher biomass and producti
vity occurring in November 1993. This was partially attributed to higher ri
ver discharge prior to November 1993, retention of biomass and nutrients by
the downcoast flow along the inner shelf, and possibly, injection of nutri
ents onto the shelf at the shelf break. Our findings demonstrate that the i
nteraction of circulation and availability of Light and nutrients are large
ly responsible for variations in primary production. Nitrogen appeared to b
e the primary limiting nutrient, however, a potential for phosphate limitat
ion was also observed particularly during periods of higher river discharge
. Light availability was a critical variable during the fall and winter mon
ths, when higher primary production was restricted to shallow waters where
vertical mixing was constrained by bottom topography. In deep waters, count
eractive changes in nutrient and light availability apparently resulted in
minor temporal variation between seasons. The annual carbon production in t
he Louisiana-Texas (LATEX) continental shelf region was estimated to be 159
g C m(-2) year(-1), which is within the range of prior estimates for this
region. Given that the area of the study region was approximately 140,000 k
m(2), this would be equivalent to an areal carbon production of about 22.2
million metric tons. (C) 2000 Elsevier Science B.V. All rights reserved.