Particle-reactive radionuclides (²³⁴Th, ²¹⁰Pb, ²¹⁰) as tracers for the estimation of export production in the South China Sea

Abstract. The time-series station, SEATS (18° N, 116° E) in the South China Sea was visited six times during October 2006–December 2008 to carry out seawater sampling and floating trap deployments for the determination of distributions and fluxes of POC, PIC, PN, ²³⁴Th, ²¹⁰Pb, and ²¹⁰Po in the upper 200 m of the water column. Radionuclide deficiencies resulted in removal fluxes from the euphotic layer of 1.1×10³–1.8×10³ dpm m⁻²d⁻¹ and 7.1–40.2 dpm m⁻²d⁻¹ for ²³⁴Th and ²¹⁰Po, respectively. Due to atmospheric input, an excess of ²¹⁰Pb relative to ²²⁶Ra is commonly observed in the upper water column. Sinking fluxes of total mass, POC, PIC, PN, ²³⁴Th, ²¹⁰Pb, and ²¹⁰Po measured at the euphotic depth were low in summer-fall and high in winter-spring, reflecting the seasonal variability of biological pumping. Excluding the suspiciously low primary productivity data point in July 2007, a relatively high e-ratio of 0.28–0.69 was estimated by the ratio of the POC flux at the euphotic depth and the integrated primary productivity. The ratios of ²³⁴Th, ²¹⁰Pb, and ²¹⁰Po to organic carbon, inorganic carbon, and nitrogen in the sinking particles were combined with the disequilibria of ²³⁴Th–²³⁸U, ²¹⁰Pb–²²⁶Ra, and ²¹⁰Po–²¹⁰Pb to estimate export fluxes of POC, PIC, and PN from the euphotic layer. Compared with measured fluxes by the sediment trap and estimated fluxes by other approaches, it is concluded that the export production in the South China Sea, ranging from 1.8 to 21.3 mmol-C m⁻²d⁻¹, can be reasonably estimated using ²³⁴Th, ²¹⁰Pb, and ²¹⁰Po as carbon proxies.