TY - JOUR
T1 - Unicellular diazotrophy as a source of nitrogen to Leeuwin Current coastal eddies
AU - Holl, C.M.
AU - Waite, Anya
AU - Pesant, S.C.
AU - Thompson, P.A.
AU - Montoya, J.P.
PY - 2007
Y1 - 2007
N2 - N-2-fixation (N-15(2) uptake) and C-fixation (H-2(13) CO3 uptake) rates of the natural phytoplankton assemblage were measured in a pair of counter-rotating mesoscale eddies in the Leeuwin Current, off the coast of Western Australia in October 2003. Day and night incubations of samples from both the surface and the deep chlorophyll maximum (DCM) were performed at nine stations across the warm core (WC) eddy and ten stations across the cold-core (CC) eddy with focal points in the center, the body, and periphery of each eddy. The mean daytime N-2-fixation rate was 33 +/- 16 pmole N L-1 h(-1) (mean +/- SD, N = 18) in the WC eddy and 21 +/- 12 pmoleNL(-1) h(-1) (mean +/- SD, N = 20) in the CC eddy. We found significant time of day and depth effects, with higher N-2-fixation during the day and at the surface in the WC and the CC eddy, respectively. The depth integrated clean a real N-2-fixation rate in the WC eddy was 42.9 +/- 14.1 mu mol N m(-2) d(-1)(mean +/- SD, N = 9), which was significantly greater than that of the CC eddy, 17.1 +/- 8.1 mu mol Nm(-2)d(-1) (mean +/- SD, N= 10). Vertical profiles show measurable but highly variable volumetric rates of N-2-fixation in the upper 100m of the water column ranging from 0.13 to 9.6 pmole N L-1 h(-1), with a mean of 4.3 +/- 1.6 ptnole N L-1 h(-1) (mean +/- SD, N = 10), without any obvious vertical structure. Size-fractionated experiments generally showed no difference in N-2-fixation rates in whole-water samples as compared to < 100-mu m and < 10-mu m size-fractioned samples, suggesting that the diazotropluc assemblage was < 10 mu m. We found no significant differences among size fractions in volumetric C-fixation rates. Simultaneous N-2- and C-fixation rate measurements suggest that N-2-fixation could support only about 2% of total production in the WC eddy and only 0.6% in the CC eddy. Though measurable, N-2-fixation in these eddies does not appear to be the primary source of nitrogenous nutrients to the phytoplankton. (c) 2007 Elsevier Ltd. All rights reserved.
AB - N-2-fixation (N-15(2) uptake) and C-fixation (H-2(13) CO3 uptake) rates of the natural phytoplankton assemblage were measured in a pair of counter-rotating mesoscale eddies in the Leeuwin Current, off the coast of Western Australia in October 2003. Day and night incubations of samples from both the surface and the deep chlorophyll maximum (DCM) were performed at nine stations across the warm core (WC) eddy and ten stations across the cold-core (CC) eddy with focal points in the center, the body, and periphery of each eddy. The mean daytime N-2-fixation rate was 33 +/- 16 pmole N L-1 h(-1) (mean +/- SD, N = 18) in the WC eddy and 21 +/- 12 pmoleNL(-1) h(-1) (mean +/- SD, N = 20) in the CC eddy. We found significant time of day and depth effects, with higher N-2-fixation during the day and at the surface in the WC and the CC eddy, respectively. The depth integrated clean a real N-2-fixation rate in the WC eddy was 42.9 +/- 14.1 mu mol N m(-2) d(-1)(mean +/- SD, N = 9), which was significantly greater than that of the CC eddy, 17.1 +/- 8.1 mu mol Nm(-2)d(-1) (mean +/- SD, N= 10). Vertical profiles show measurable but highly variable volumetric rates of N-2-fixation in the upper 100m of the water column ranging from 0.13 to 9.6 pmole N L-1 h(-1), with a mean of 4.3 +/- 1.6 ptnole N L-1 h(-1) (mean +/- SD, N = 10), without any obvious vertical structure. Size-fractionated experiments generally showed no difference in N-2-fixation rates in whole-water samples as compared to < 100-mu m and < 10-mu m size-fractioned samples, suggesting that the diazotropluc assemblage was < 10 mu m. We found no significant differences among size fractions in volumetric C-fixation rates. Simultaneous N-2- and C-fixation rate measurements suggest that N-2-fixation could support only about 2% of total production in the WC eddy and only 0.6% in the CC eddy. Though measurable, N-2-fixation in these eddies does not appear to be the primary source of nitrogenous nutrients to the phytoplankton. (c) 2007 Elsevier Ltd. All rights reserved.
U2 - 10.1016/j.dsr2.2007.02.002
DO - 10.1016/j.dsr2.2007.02.002
M3 - Article
SN - 0967-0645
VL - 54
SP - 1045
EP - 1054
JO - Deep Sea Research Part II: Topical Studies in Oceanography
JF - Deep Sea Research Part II: Topical Studies in Oceanography
IS - 8-10
ER -