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Concentration of fulvic acid in the growth bands of hermatypic corals in relation to local precipitation

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Abstract

Coral growth rate and the concentrations of fulvic acid in the growth bands of the hermatypic coral Porites lutea Edwards & Haime and Favia maxima Veron were investigated in samples taken from 1986 to 1988 in the waters of southern Taiwan (22°05′≈36′N, 120°24′≈50′E). These were analyzed against the local annual precipitation, the locality of the sampling sites, the construction activity on nearby land and coral species. The results showed that the annual growth rate of P. lutea was 1.08±0.12 cm while F. maxima was 0.83±0.09 cm. The amount of fulvic acid incorporated in the growth band was positively correlated with the local annual precipitation. However, the correlation coefficient varied from as high as 0.9519 to as low as 0.0921 due to different topographies of the sampling sites, dilution factors from the ocean and construction activities along the coast. F. maxima was found to be more sensitive than P. lutea in terms of fulvic acid uptake from the surrounding waters. The study of fluorescence in the skeleton of hermatypic corals is a reasonable approach to biomonitor the environment after consideration of local factors.

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References

  • Bak RPM, Laane WPM (1987) Annual black bands in skeletons of reef corals. Mar Ecol Prog Ser 38:169–175

    Google Scholar 

  • Barnard LA, Macintyre IG, Pierce JW (1974) Possible environmental index in tropical reef corals. Nature 252:210–220

    Google Scholar 

  • Boto K, Isdale P (1985) Fluorescent bands in massive corals result from terrestrial fulvic acid inputs to nearshore zone. Nature 315:96–397

    Google Scholar 

  • Chen CTA, Chang KH, Fang LS (1992) Recent changes of zinc and Sr-90 in banded corals in southern Taiwan. In: Marsh J (ed) “Asia-Pacific Marine Resources and Development”. Taylor and Francis, New York (in press)

    Google Scholar 

  • Cortes J, Risk MJ (1985) A reef under siltation stress: Cahuita, Costa Rica. Bull Mar Sci 36:339–356

    Google Scholar 

  • Dodge RE, Vaisnys JR (1975) Hermatypic coral growth banding as environmental recorder. Nature 258:706–708

    Google Scholar 

  • Dodge RE, Jickells TD, Knap AH, Boyd S, Bak RPM (1984) Reef-building coral skeletons as chemical pollution (Phosphorus) indicators. Mar Pollut Bull 15:178–187

    Google Scholar 

  • Druffel EM (1982) Banded corals: changes in oceanic carbon-14 during the little ice age. Science 218:13–19

    Google Scholar 

  • Flor TH, More WS (1977) Radium/calcium and uranium/calcium determinations for western atlantic reef corals. Proc 3rd Int Coral Reef Symp 2:555–562

    Google Scholar 

  • Goreau TJ (1977) Coral skeletal chemistry: physiological and environmental regulation of stable isotopes and trace metals in Montastrea annularis. Proc R Soc London Ser B 196:291–315

    Google Scholar 

  • Hudson JH, Shinn EA, Halley RB, Lidz B (1976) Sclerochronology-a tool for interpreting past environments. Geology 4:361–364

    Google Scholar 

  • Isdale PJ (1984) Fluorescent bands in massive corals record centuries of coastal rainfall. Nature 310:578–579

    Google Scholar 

  • Isdale PJ (1988) Construction of historical analogues of terrestrial runoff inputs to reef areas using fluorescing bands in nearshore massive coral (abstract). 6th Int Coral Reef Symp, Townsville, Australia, p 200

  • Ma TYH (1937) On the growth rate of reef corals and its relation to sea water temperature. Palaeont Sin Ser B 16:1–426

    Google Scholar 

  • Meyers-Schulte KJ, Hedges JI (1986) Molecular evidence for a terrestrial component of organic matter dissolved in ocean water. Nature 321:61–63

    Google Scholar 

  • Patzold J (1984) Growth rhythms recorded in stable isotopes and density bands in the reef coral Porites lobata (Cebu, Philippines). Coral Reefs 3:87–90

    Google Scholar 

  • Scoffin TP, Tudhope AW, Brown BE (1989) Fluorescent and skeletal density banding in Porites lutea from Papua New Guinea and Indonesia. Coral Reefs 7:169–178

    Google Scholar 

  • Stuermer DH, Harvey GR (1974) Humic substances from sea water. Nature 250:480–481

    Google Scholar 

  • Wang CH, Huang CY (1987) Oxygen and carbon isotope records in the coral Favia speciosa of Nanwan bay, Southern Taiwan. Acta Oceanogr Taiwanica 18:150–157

    Google Scholar 

  • Wang CH, Huang CY (1989) The eleven-year isotopic records in the coral Favia speciosa of Nanwan bay, southern Taiwan. Acta Oceanogr Taiwanica 24:96–107

    Google Scholar 

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Fang, LS., Chou, YC. Concentration of fulvic acid in the growth bands of hermatypic corals in relation to local precipitation. Coral Reefs 11, 187–191 (1992). https://doi.org/10.1007/BF00301991

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