Articles | Volume 10, issue 4
Biogeosciences, 10, 2273–2291, 2013
Biogeosciences, 10, 2273–2291, 2013

Research article 05 Apr 2013

Research article | 05 Apr 2013

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 K. Castro-Morales et al.
  • 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.

Final-revised paper