Nitrogen uptake conditions at VERTIGO study sites M Elskens, N Brion, F Dehairs, W Baeyens & N Savoye Pleinlaan 2, B-1050 Brussel , Belgium ([email protected]) Introduction Nitrogen uptake conditions were surveyed in the photic zone at station Aloha 22°45N-158°W during 2004 VERTIGO Hawaii cruise and at station K2 47°N-161°E during 2005 VERTIGO Northwest Pacific cruise using stable isotope techniques. We aimed at determining new production rates, and therefore 15N and 13C isotopically labelled compounds were used in a series of tracer experiments conducted over a 3 week period at the VERTIGO sites. Experimental design 1.At station Aloha, combined 15N (NO3, NO2, NH4, N2) and 13C tracer experiments were conducted over periods of 12 hours under constant illumination and neutral density screens to mimic in situ light attenuation. Sampling depths were 5, 25, 50 & 125m. 2.At station K2, 15N (NO3, NH4) and 13C tracer experiments were conducted over periods of 2, 4 and 6 hours under constant illumination and neutral density screens to mimic in situ light attenuation. Sampling depths were 5, 25, 40 & 50m. Data analysis: A model comparison approach New production assessment 1.Primary production PP (13C) Field measurements Mass balance differential equations 2.f-ratio (15N): Numerical integration Optimization UptkNO3 UptkN2 f ratio UptkDIN UptkDIN Uptk NH4 NO3 NO2 N2 Statistics 3.New production: PNEW = f-ratio x PP Uncertainty assessment 4.Integration of PP and PNEW over the euphotic layer Parameter estimates: C and N flux rates N uptake conditions at the VERTIGO sampling sites K2 Aloha 100 n = 32 90 80 % of DIN uptake rate 100 90 82% 80% Stations 80 Specific NO3 uptake rate d-1 VNO3 f-ratio % 0.0020.006 720 70 70 60 60 50 50 40 40 Ratio to POC flux at 150m (NBST) 30 30 K2 20 20 18% 10 0.020.06 10 9% 6% 4% 0 NH4 Aloha NO3 NO2 N2 PP PNEW mg C m-2 d-1 mg C m-2 d-1 1024 Ratio to POC flux at 150m (NBST) 0 143240 1242 10-12 0.8-1 348585 50171 10-17 2-3 NH4 NO3 Acknowledgments Primary and new production variability over the sampling period 320 13 280 700 C-PP 13 t-test p < 0.001 95% CI 600 Mean PP 500 C-PP 160 95% CI 120 80 60 PNEW t-test p < 0.001 40 400 300 200 PNEW t-test p = 0.005 150 100 50 20 0 170 -2 d -1 200 Production mg C m Production mg C m -2 d -1 240 172 174 176 178 180 Julian days Conclusions 182 184 186 188 0 208 210 212 214 216 218 220 Julian days 222 224 226 228 This research was conducted under grant GOA22/DSCH WER4 as part of the project Geconcerteerde Onderzoekacties supported by the Vrije Universiteit Brussel and under grant G.0021.04 as part of a Research Foundation Flanders project. The authors would like to thank Ken Buesseler for the scientific coordination of the VERTIGO project Two regimes of new production have been identified; K2 shows relatively high nitrate specific uptake rates (VNO3) but rather low new production rates and is characteristic of HNLC regions. Aloha has low VNO3, low new production and behaves typically as an oligotrophic area. At both sites there is an agreement between the estimates of new production and the POC flux samples by neutrally buoyant traps at 150m with an export ratio ranging from 1 (Aloha) to maximally 3 at K2.
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