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Biogeosciences, 10, 2273-2291, 2013
www.biogeosciences.net/10/2273/2013/
doi:10.5194/bg-10-2273-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Biological production in the Bellingshausen Sea from oxygen-to-argon ratios and oxygen triple isotopes
K. Castro-Morales1,*, N. Cassar2,**, D. R. Shoosmith3, and J. Kaiser1
1School of Environmental Sciences, University of East Anglia, Norwich, UK
2Geosciences Department, Princeton University, Princeton, USA
3British Antarctic Survey, Cambridge, UK
*now at: Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
**now at: Division of Earth and Ocean Sciences, Nicholas School of the Environment, Duke University, Durham, NC, USA

Abstract. We present estimates of mixed-layer net community oxygen production (N) and gross oxygen production (G) of the Bellingshausen Sea in March and April 2007. N was derived from oxygen-to-argon (O2/Ar) ratios; G was derived using the dual-delta method from triple oxygen isotope measurements. In addition, O2 profiles were collected at 253 CTD stations. N is often approximated by the biological oxygen air–sea exchange flux (Fbio based on the O2/Ar supersaturation, assuming that significant horizontal or vertical fluxes are absent. Here we show that the effect of vertical fluxes alone can account for Fbio values < 0 in large parts of the Bellingshausen Sea towards the end of the productive season, which could otherwise be mistaken to represent net heterotrophy. Thus, improved estimates of mixed-layer N can be derived from the sum of Fbio, Fe (entrainment from the upper thermocline during mixed-layer deepening) and Fv (diapycnal eddy diffusion across the base of the mixed layer). In the winter sea ice zone (WSIZ), the corresponding correction results in a small change of Fbio = (30 ± 17) mmol m−2 d−1 to N = (34 ± 17) mmol m−2 d−1. However, in the permanent open ocean zone (POOZ), the original Fbio value of (−17 ± 10) mmol m−2 d−1 gives a corrected value for N of (−2 ± 18) mmol m−2 d−1. We hypothesize that in the WSIZ, enhanced water column stability due to the release of freshwater and nutrients from sea ice melt may account for the higher N value. These results stress the importance of accounting for physical biases when estimating mixed-layer marine productivity from in situ O2/Ar ratios.

Citation: Castro-Morales, K., Cassar, N., Shoosmith, D. R., and Kaiser, J.: Biological production in the Bellingshausen Sea from oxygen-to-argon ratios and oxygen triple isotopes, Biogeosciences, 10, 2273-2291, doi:10.5194/bg-10-2273-2013, 2013.
 
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