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Reexamination of the fractionation of total dissolved phosphorus in seawater using a modified UV-irradiation procedure, and its application to samples from Suruga Bay and Antarctic Ocean

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Abstract

Application of a modified UV-irradiation procedure to the fractionation of total dissolved phosphorus (TDP) in seawater was examined. By using a peristaltic pump, a sample solution was passed through a quartz column which was coiled around the three Hg-lamps and thus consistently exposed to a controlled UV-irradiation flux. The UV-flux was much lower than that historically employed to hydrolyze total dissolved organic phosphorus (DOP). Before and after the UV-irradiation, colorimetric measurements of soluble reactive phosphorus (SRP) were made by the method of Murphy and Riley (1962) to determine the liberation rate of orthophosphate from P-compounds in the sample. Experiments using 19 different P-compounds indicated that organic phosphate-esters containing only monomers of phosphate were readily decomposed by a 20-minute UV-irradiation period. Release of SRP from organic polyphosphates was minimal. The P released by this procedure is operationally referred to as “UV-P”. The procedure described herein was employed for fractionation of TDP in seawater. These studies defined several classes of dissolved P: (1) PO4−P(inorganic phosphate-P), (2) UV-P (Photodecomposable organic-P, most of which consists of organic monophosphate-P), and (3) Org-Poly-P (organic polyphosphate-P). Vertical profiles of DOP and UV-P observed in the oligotrophic regions of Suruga Bay and Antarctic Ocean indicated that UV-P was a major part of total dissolved phosphorus (TDP) in euphotic layers, where inorganic nutrients were probably limiting the active growth of phytoplankton. It is probable that UV-P can be utilized as a source of nutrient-P, in place of PO4−P.

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References

  • Admiraal, W. and D. Werner (1983): Utilization of limiting concentrations of ortho-phosphates and production of extracellular organic phosphates of marine diatoms.J. Plankton Res.,5, 495–513.

    Google Scholar 

  • Armstrong, F. A. J. and S. Tibbitts (1968): Photo-chemical combustion of organic matter in seawater for nitrogen, phosphorus and carbon determination.J. Mar. Biol. Assoc. U. K.,48, 143–152.

    Google Scholar 

  • Armstrong, F. A. J., P. U. Williams and J. D. H. Strickland (1966): Photo-oxidation of organic matter in seawater by ultra-violet radiation, analytical and other applications.Nature,211, 481–483.

    Google Scholar 

  • Berman, T. (1985): Uptake of32P-orthophosphate by algae and bacteria in Lake Kinneret.J. Plankton Res.,7, 71–84.

    Google Scholar 

  • Berman, T. (1988): Differential uptake of orthophosphate and organic phosphorus substrates by bacteria and algae in lake Kinneret.J. Plankton Res.,10, 1239–1249.

    Google Scholar 

  • Bradford, M. E. and H. Peters (1987): The relationship between chemically analyzed phosphorus fractions and bioavailable phosphorus.Limnol. Oceanogr.,32, 1124–1137.

    Google Scholar 

  • Chamberlain, W. and J. Shapiro (1969): On the biological significance of phosphate analysis; Comparison of standard and new methods with a bioassay.Limnol. Oceanogr.,14, 921–927.

    Google Scholar 

  • Currie, D. J. and J. Kalff (1984): The relative importance of bacterioplankton and phytoplankton in phosphorus uptake in freshwater.Limnol. Oceanogr.,29, 311–321.

    Google Scholar 

  • Currie, D. J., E. Benzen and J. Kalff (1986): Does algal-bacterial phosphorus partitioning vary among lakes? A comparative study of orthophosphate uptake and alkaline phosphatase activity in freshwater.Can. J. Fish. Aquat. Sci.,43, 311–318.

    Google Scholar 

  • Dillon, P. J. and F. H. Rigler (1975): A simple method for predicting the capacity of a lake for development based on lake trophic status.J. Fish. Res. Bd. Canada,54, 825–855.

    Google Scholar 

  • Esumi, H., and Y. Saijo (1969): Determination of dissolved organic matter in natural waters by ultraviolet oxidation.Chikyu-kagaku,3, 1–8 (in Japanese).

    Google Scholar 

  • Fukui, F., K. Otomo and S. Okabe (1986): Nutrients depression in the blooming area of Prydz Bay, Antarctica.Mem. Natl. Inst. Polar Res. Spec. Issue,44, 43–54.

    Google Scholar 

  • Fukui, F., N. Kadoya, S. Okabe and Y. Komaki (1987): The surface distribution of nutrients and chlorophylla in the area between 90°W and 20°E of the Antarctic Ocean and adjacent seas.Nankyoku shiryo (Antarctic Rec.),31, 118–130.

    Google Scholar 

  • Goossen, J. T. H. and J. G. Klooslerboer (1978): Determination of phosphate in natural and waste waters after photochemical decomposition and acid hydrolysis of organic phosphorus compounds.Anal. Chem.,50, 707–711.

    Article  Google Scholar 

  • Handa, N. and K. Yanagi (1970): Particulate organic matter of the chlorophylla maximum layer in the ocean.Bull. Plankt. Soc. Japan,17, 42–49 (in Japanese with English abstract).

    Google Scholar 

  • Handa, N., K. Yanagi and K. Matsunaga (1972): Vertical distribution of detrital materials in the Pacific Ocean and their biochemical nature.Mem. Ist., Ital. Idorobiol.,29, Suppl. 53–71.

    Google Scholar 

  • Henriksen, A. (1970): Determination of total nitrogen, phosphorus and iron in freshwater by photo-oxidation with ultra-violet radiation.Analyst,95, 601–608.

    Article  Google Scholar 

  • Ichinoe, N., A. Honma and H. Fujie (1987): Photolysis of some organic phosphate compounds.Anal. Sci.,3, 273–274.

    Google Scholar 

  • Jackson, G. A. and P. U. Williams (1985): Importance of dissolved organic nitrogen and phosphorus to biological nutrient cycling.Deep-Sea Res.,32, 223–235.

    Article  Google Scholar 

  • Karl, D. M. and P. Bossard (1985): Measurement and significance of ATP and adenine nucleotide pool turnover in microbial cells and environmental samples.J. Microbiol. Methods,3, 125–139.

    Article  Google Scholar 

  • Karl, D. M. and M. D. Bailiff (1989): The measurement and distribution of dissolved nucleic acids in aquatic environments.Limnol. Oceanogr.,34, 543–558.

    Google Scholar 

  • Menzel, D. and N. Corwin (1965): The measurement of total phosphorus in sea water based on the liberation of organically bound fractions by persulfate oxidation.Limnol. Oceanogr.,10, 280–283.

    Google Scholar 

  • Miyata, K. and A. Hattori (1986a): A simple fractionation method for determination of phosphorus components in phytoplankton: Application to natural populations of phytoplankton in summer surface waters of Tokyo Bay.J. Oceanogr. Soc. Japan,42, 255–265.

    Article  Google Scholar 

  • Miyata, K. and A. Hattori (1986b): Distribution and seasonal variation of phosphorus in Tokyo Bay.J. Oceanogr. Soc. Japan,42, 209–222.

    Google Scholar 

  • Murphy, J. and L. P. Riley (1962): A modified single solution method for the determination of phosphate in natural waters.Anal. Chim. Acta,27, 31–36.

    Article  Google Scholar 

  • Orrett, K. and D. M. Karl (1987): Dissolved organic phosphorus production in surface seawaters.Limnol. Oceanogr.,32, 383–395.

    Google Scholar 

  • Perry, M. J. and R. W. Eppley (1981): Phosphate uptake by phytoplankton in the central North Pacific Ocean.Deep-Sea Res.,28, 39–49.

    Article  Google Scholar 

  • Ridal, J. J. and R. M. Moore (1990): A re-examination of the measurement of dissolved organic phosphorus in seawater.Mar. Chem.,29, 19–31.

    Article  Google Scholar 

  • Schindler, D. W. (1975): Eutrophication and recovery in experimental lakes: Implications for lake management.Science,184, 897–899.

    Google Scholar 

  • Smith, S. V. and M. J. Atkinson (1984): Phosphorus limitation of net production in a confined ecosystem.Nature,307, 626–627.

    Article  Google Scholar 

  • Smith, S. V., M. J. Kimmerer and T.W. Walsh (1986): Vertical flux and biogeochemical turnover regulate nutrient limitation of net organic production in the North Pacific Gyre.Limnol. Oceanogr.,31, 161–167.

    Google Scholar 

  • Solorzano, L. and J. H. Sharp (1980): Determination of total dissolved phosphorus and particulate phosphorus in natural waters.Limnol. Oceanogr.,25, 87–97.

    Google Scholar 

  • Strickland, J. D. H. and T. R. Parsons (1972): Practical handbook of seawater analysis. 2nd. ed.Fish. Res. Bd. Canada Bull.,167, 311 pp.

  • UNESCO (1969): On the preparation of CSK standards for marine nutrient analysis. Chemistry Working Group, Subcommittee for CSK, National Committee on Oceanic Research, Science council of Japan, 56p.

  • Yanagi, K. (1982a): Studies on the distribution and biochemical composition of particulate organic matter in the Pacific Ocean. Doctoral Thesis, Tokai University, p. 109 (in Japanese).

  • Yanagi, K. (1982b): Variation of organic composition of a diatom,Phaeodactylum tricornutum, cultured under different conditions of light intensity and nutrient concentration.Bull. Soc. Seawater Sci. Japan,35, 289–298 (in Japanese with English abstract).

    Google Scholar 

  • Yanagi, K. and M. Yasuda (1981): A fractional determination of dissolved organic phosphorus (DOP) by an UV-irradiation procedure and variations of DOP composition in a culture medium of a diatom.Annual Meeting Oceanogr. Soc. Japan (Abstract), p. 138 (in Japanese).

  • Yanagi, K., H. Kuge and Y. Noguchi (1990): Characteristics in distribution of nutrients and particulate organic matter in Hakata Bay.Bull. Coll. Liberal Arts, Kyushu Sangyo Univ. Japan,27, 375–412 (in Japanese).

    Google Scholar 

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Yanagi, K., Yasuda, M. & Fukui, F. Reexamination of the fractionation of total dissolved phosphorus in seawater using a modified UV-irradiation procedure, and its application to samples from Suruga Bay and Antarctic Ocean. J Oceanogr 48, 267–281 (1992). https://doi.org/10.1007/BF02233987

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  • DOI: https://doi.org/10.1007/BF02233987

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