Skip to main content
Log in

234Th/238U disequilibrium and particulate organic carbon export in the northern South China Sea

  • Original Articles
  • Published:
Journal of Oceanography Aims and scope Submit manuscript

Abstract

We utilized 234Th, a naturally occurring radionuclide, to quantify the particulate organic carbon (POC) export rates in the northern South China Sea (SCS) based on data collected in July 2000 (summer), May 2001 (spring) and November 2002 (autumn). Th-234 deficit was enhanced with depth in the euphotic zone, reaching a subsurface maximum at the Chl-a maximum in most cases, as commonly observed in many oceanic regimes. Th-234 was in general in equilibrium with 238U at a depth of ∼100 m, the bottom of the euphotic zone. In this study the 234Th deficit appeared to be less significant in November than in July and May. A surface excess of 234Th relative to 238U was found in the summer over the shelf of the northern SCS, most likely due to the accumulation of suspended particles entrapped by a salinity front. Comparison of the 234Th fluxes from the upper 10 m water column between 2-D and traditional 1-D models revealed agreement within the errors of estimation, suggesting the applicability of the 1-D model to this particular shelf region. 1-D model-based 234Th fluxes were converted to POC export rates using the ratios of bottle POC to 234Th. The values ranged from 5.3 to 26.6 mmol C m−2d−1 and were slightly higher than those in the southern SCS and other oligotrophic areas. POC export overall showed larger values in spring and summer than in autumn, the seasonality of which was, however, not significant. The highest POC export rate (26.6 mmol C m−2d−1) appeared at the shelf break in spring (May), when Chl-a increased and the community structure changed from pico-phytoplankton (<2 µm) dominated to nano-phytoplankton (2–20 µm) and micro-phytoplankton (20–200 µm) dominated.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Anderson, R. F. and A. P. Fleer (1982): Determination of natural actinides and plutonium in marine particulate material. Anal. Chem., 54, 1142–1147.

    Article  Google Scholar 

  • Benitez-Nelson, C. R., K. O. Buesseler and G. Crossin (2000): Upper ocean carbon export, horizontal transport, and vertical eddy diffusivity in the southwestern Gulf of Maine. Cont. Shelf Res., 20, 707–736.

    Article  Google Scholar 

  • Borges, A. V., B. Delille and M. Frankignoulle (2005): Budgeting sinks and sources of CO2 in the coastal ocean: Diversity of ecosystems counts. Geophys. Res. Lett., 32, doi:10.1029/2005GL023053.

    Article  Google Scholar 

  • Buesseler, K., L. Ball, J. Andrews, C. Benitez-Nelson, R. Belastock, F. Chai and Y. Chao (1998): Upper ocean export of particulate organic carbon in the Arabian Sea derived from thorium-234. Deep-Sea Res. II, 45, 2461–2487.

    Article  Google Scholar 

  • Buesseler, K. O. (1998): The decoupling of production and particulate export in the surface ocean. Global Biogeochem. Cycles, 12, 297–310.

    Article  Google Scholar 

  • Buesseler, K. O., J. E. Andrews, S. M. Pike and M. A. Charette (2004): The effects of iron fertilization on carbon sequestration in the Southern Ocean. Science, 304, 414–417.

    Article  Google Scholar 

  • Buesseler, K. O., C. R. Benitez-Nelson, S. B. Moran, A. Burd, M. A. Charette, J. K. Cochran, L. Coppola, N. S. Fisher, S. W. Fowler, W. D. Gardner, L. D. Guo, O. Gustafsson, C. Lamborg, P. Masque, J. C. Miquel, U. Passow, P. H. Santschi, N. Savoye, G. Stewart and T. Trull (2006): An assessment of particulate organic carbon to thorium-234 ratios in the ocean and their impact on the application of 234Th as a POC flux proxy. Mar. Chem., 100, 213–233.

    Article  Google Scholar 

  • Cai, P., Y. Huang, M. Chen, G. Liu and Y. Qiu (2001): Export of particulate organic carbon estimated from 234Th-238U disequilibria and its temporal variation in the South China Sea. Chinese Sci. Bull., 46, 1722–1726 (in Chinese).

    Article  Google Scholar 

  • Cai, P., Y. Huang, M. Chen, L. Guo, G. Liu and Y. Qiu (2002): New production based on 228Ra-derived nutrient budgets and thorium-estimated POC export at the intercalibration station in the South China Sea. Deep-Sea Res. I, 49, 53–66.

    Article  Google Scholar 

  • Cai, P., M. Dai, D. Lv and W. Chen (2006a): An improvement in the small-volume technique for determining thorium-234 in seawater. Mar. Chem., 100, 282–288.

    Article  Google Scholar 

  • Cai, P., M. Dai, W. Chen, T. Tang and K. Zhou (2006b): On the importance of the decay of 234Th in determining size-fractionated C/234Th ratio on marine particles. Geophys. Res. Lett., 33, doi: 10.1029/2006GL027792.

  • Cai, P., W. Chen, M. Dai, Z. Wan, D. Wang, Q. Li, T. Tang and D. Lv (2007): A high-resolution study of particle export in the southern South China Sea based on 234Th:238U disequilibrium. J. Geophys. Res. (in press).

  • Cai, P., M. Dai, D. Lv and W. Chen (2008): Reply to comment by Chin-Chang Hung et al. on “How accurate are 234Th measurements in seawater based on the MnO2-impregnated cartridge technique?”. Geochem. Geophys. Geosyst., 9, doi:10.1029/2007GC001837.

    Article  Google Scholar 

  • Cai, W. and M. Dai (2004): Comment on “Enhanced open ocean storage of CO2 from shelf sea pumping”. Science, 306, 1477C.

    Article  Google Scholar 

  • Cai, W., M. Dai, Y. Wang, W. Zhai, T. Huang, S. Chen, F. Zhang, Z. Chen and Z. Wang (2004): The biogeochemistry of inorganic carbon and nutrients in the Pearl River estuary and the adjacent Northern South China Sea. Cont. Shelf Res., 24, 1301–1319.

    Article  Google Scholar 

  • Cai, W., M. Dai and Y. Wang (2006): Air-sea exchange of carbon dioxide in ocean margins: A province-based synthesis. Geophys. Res. Lett., 33, doi:10.1029/2006GL026219.

    Google Scholar 

  • Chao, S., P. Shaw and S. Wu (1996): Deep water ventilation in the South China Sea. Deep-Sea Res. I, 43, 445–466.

    Article  Google Scholar 

  • Charette, M. A., S. B. Moran, S. M. Pike and J. N. Smith (2001): Investigating the carbon cycle in the Gulf of Maine using the natural tracer thorium-234. J. Geophys. Res.-Oceans, 106, 11553–11579.

    Article  Google Scholar 

  • Chen, J., M. Wiesner, H. Wong, L. Zheng, L. Xu and S. Zheng (1999): Vertical changes of POC flux and indicators of early degradation of organic matter in the South China Sea. Sci. in China (Ser. D), 42, 120–128 (in Chinese).

    Article  Google Scholar 

  • Chen, M., Y. Huang, F. Chen, Y. Qiu, M. Xu and D. Jiang (1997): Particle dynamics in the euphotic zone-VI. The utility of tracer 234Th for studying particle dynamics in the upper water column of the Northeastern South China Sea. J. Tropical Oceanogr., 16, 91–103 (in Chinese).

    Google Scholar 

  • Chen, Y. L. L. (2005): Spatial and seasonal variations of nitrate-based new production and primary production in the South China Sea. Deep-Sea Res. I, 52, 319–340.

    Article  Google Scholar 

  • Coale, K. H. and K. W. Bruland (1987): Oceanic stratified euphotic zone as elucidated by 234Th:238U disequilibria. Limnol. Oceanogr., 32, 189–200.

    Article  Google Scholar 

  • Cochran, J. K., C. Barnes, D. Achman and D. T. Hirschberg (1995): Thorium-234/Uranium-238 disequilibrium as an indicator of scavenging rates and particulate organic carbon fluxes in the Northeast Water Polynya, Greenland. J. Geophys. Res., 100, 4399–4410.

    Article  Google Scholar 

  • Dagg, M., R. Benner, S. Lohrenz and D. Lawrence (2004): Transformation of dissolved and particulate materials on continental shelves influenced by large rivers: plume processes. Cont. Shelf Res., 24, 833–858.

    Article  Google Scholar 

  • Dai, M., W. Zhai, W. Cai, J. Callahan, B. Huang, S. Shang, T. Huang, X. Li, Z. Lu, W. Chen and Z. Chen (2007): Effects of an estuarine plume-associated bloom on the carbonate system in the lower reaches of the Pearl River estuary and the coastal zone of the northern South China Sea. Cont. Shelf Res. (in press).

  • Eppley, R. W. and B. J. Peterson (1979): Particulate organic matter flux and planktonic new production in the deep ocean. Nature, 282, 677–680.

    Article  Google Scholar 

  • Fang, W., P. Shi, Q. Mao and Z. Gan (2000): Variation of upper ocean in the northern South China Sea from mooring station observations. Acta Oceanol. Sinica, 22, 23–30 (in Chinese).

    Google Scholar 

  • Frankignoulle, M. and A. V. Borges (2001): European continental shelf as a significant sink for atmospheric carbon dioxide. Global Biogeochem. Cycles, 15, 569–576.

    Article  Google Scholar 

  • Gustafsson, O., K. O. Buesseler, W. R. Geyer, S. B. Moran and P. M. Gschwend (1998): An assessment of the relative importance of horizontal and vertical transport of particle-reactive chemicals in the coastal ocean. Cont. Shelf Res., 18, 805–829.

    Article  Google Scholar 

  • Hu, J., H. Kawamura, H. Hong and Y. Qi (2000): A review on the currents in the South China Sea: Seasonal circulation, South China Sea warm current and Kuroshio intrusion. J. Oceanogr., 56, 607–624.

    Article  Google Scholar 

  • Knap, A., A. Michaels, A. Close, H. Ducklow and A. Dickson (1996): Protocols for the Joint Global Ocean Flux Study (JGOFS) Core Measurements. JGOFS Report Nr. 19, vi+170 pp. Reprint of the IOC Manuals and Guides No. 29, UNESCO 1994.

  • Ku, T. L., K. G. Knauss and G. G. Mathieu (1977): Uranium in open ocean: Concentration and isotopic composition. Deep-Sea Res., 24, 1005–1017.

    Article  Google Scholar 

  • Liang, Y., D. Yuan, Q. Li and Q. Lin (2006): Flow injection analysis of nanomolar level orthophosphate in seawater with solid phase enrichment and colorimetric detection. Mar. Chem., 103, 122–130.

    Article  Google Scholar 

  • Liu, K. K., L. Atkinson, C. T. A. Chen, S. Gao, J. Hall, R. W. Macdonald, L. Talaue McManus and R. Quiñones (2000): Exploring continental margin carbon fluxes on a global scale. EOS, Trans., AGU, 81, 641–644.

    Article  Google Scholar 

  • Liu, K. K., S. Y. Chao, P. T. Shaw, G. C. Gong, C. C. Chen and T. Y. Tang (2002): Monsoon-forced chlorophyll distribution and primary production in the South China Sea: observations and a numerical study. Deep-Sea Res. I, 49, 1387–1412.

    Article  Google Scholar 

  • Ning, X., F. Chai, H. Xue, Y. Cai, C. Liu and J. Shi (2004): Physical-biological oceanographic coupling influencing phytoplankton and primary production in the South China Sea. J. Geophys. Res., 109, doi: 10.1029/2004JC002365.

  • Okubo, A. (1971): Oceanic diffusion diagrams. Deep-Sea Res., 18, 789–802.

    Google Scholar 

  • Parsons, T., Y. Maita and C. Lalli (1984). A Manual of Chemical and Biological Methods for Seawater Analysis. Pergamon Press, New York, 107–109, 115–122.

    Book  Google Scholar 

  • Pike, S. M., K. O. Buesseler, J. A. Andrews and N. Savoye (2005): Quantification of 234Th recovery in small volume sea water samples by inductively coupled plasma mass spectrometry. J. Radioanal. Nuclear Chem., 263, 355–360.

    Article  Google Scholar 

  • Platt, T., D. V. S. Rao and B. Irvin (1983): Photosynthesis of picoplankton in the oligotrophic ocean. Nature, 301, 702–704.

    Article  Google Scholar 

  • Rodriguez y Baena, A. M., J. C. Miquel, P. Masqué, P. P. Povinec and J. La Rosa (2006): A single vs. double spike approach to improve the accuracy of 234Th measurements in small-volume seawater samples. Mar. Chem., 100, 269–281.

    Article  Google Scholar 

  • Rutgers van der Loeff, M. M., K. Buesseler, U. Bathmann, I. Hense and J. Andrews (2002): Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic. Deep-Sea Res. II, 49, 3849–3869.

    Article  Google Scholar 

  • Savoye, N., K. O. Buesseler, D. Cardinal and F. Dehairs (2004): 234Th deficit and excess in the Southern Ocean during spring 2001: particle export and mineralization. Geophys. Res. Lett., 31, doi: 10.1029/2004GL019744.

    Article  Google Scholar 

  • Shaw, P. and S. Chao (1994): Surface circulation in the South China Sea. Deep-Sea Res. I, 41, 1663–1683.

    Article  Google Scholar 

  • Tsunogai, S., S. Watanabe and T. Sato (1999): Is there a “continental shelf pump” for the absorption of atmospheric CO2? Tellus B-Chemical and Physical Meteorology, 51, 701–712.

    Article  Google Scholar 

  • Wang, H. L., B. Q. Huang and H. Hong (1997): Size-fractionated productivity and nutrient dynamics of phytoplankton in subtropical coastal environments. Hydrobiologia, 352, 97–106.

    Article  Google Scholar 

  • Waples, J. T., C. Benitez-Nelson, N. Savoye, M. M. Rutgers van der Loeff, M. Baskaran and Ö. Gustafsson (2006): An introduction to the application and future use of 234Th in aquatic systems. Mar. Chem., 100, 166–189.

    Article  Google Scholar 

  • Wei, C. L. and J. W. Murray (1992): Temporal variations of 234Th activity in the water column of Dabob Bay: Particle scavenging. Limnol. Oceanogr., 37, 296–314.

    Article  Google Scholar 

  • Zhai, W. D., M. H. Dai, W. J. Cai, Y. C. Wang and H. S. Hong (2005): The partial pressure of carbon dioxide and air-sea fluxes in the northern South China Sea in spring, summer and autumn. Mar. Chem., 96, 87–97.

    Article  Google Scholar 

  • Zhuang, W., J. Hu, Z. He, G. Zeng and Z. Chen (2003): An analysis on surface temperature and salinity from Southern Taiwan strait to Zhujiang River Estuary during July–August, 2000. J. Tropical Oceanogr., 22, 69–76 (in Chinese).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Minhan Dai.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Chen, W., Cai, P., Dai, M. et al. 234Th/238U disequilibrium and particulate organic carbon export in the northern South China Sea. J Oceanogr 64, 417–428 (2008). https://doi.org/10.1007/s10872-008-0035-z

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10872-008-0035-z

Keywords

Navigation