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Impacts of long-term increase in silicon concentration on diatom blooms in Lake Kasumigaura, Japan

Published online by Cambridge University Press:  19 November 2014

Hiroyuki Arai  and
Takehiko Fukushima
Hiroyuki Arai*
Affiliation:
Graduate School of Life and Environmental Sciences, University of Tsukuba, Tsukuba, Ibaraki 305-8572, Japan
Takehiko Fukushima
Affiliation:
Graduate School of Life and Environmental Sciences, University of Tsukuba, Tsukuba, Ibaraki 305-8572, Japan
*
*Corresponding author: [email protected]
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Abstract

In the eutrophic Lake Kasumigaura in Japan, a trend of dissolved Si (DSi) concentration was detected over the last three decades, probably caused by the DSi release enhanced by an increase in sediment resuspension for the same period (Arai et al., Limnol., 13, 81–95, 2012). The present study described the long-term trends of the magnitude and seasonality of diatom blooms in the lake during 1981–2010 using the database and assessed the influencing factors for the trends by the numerical simulation of DSi and diatoms. The box model was developed based on the lake budgets (inflow, outflow, release and sedimentation) and the simple diatom growth model depending on DSi, temperature and light condition. As results, database analysis detected a long-term trend of increasing diatom abundance and a shift of blooming season from spring and autumn to the winter–spring period. Si could be regarded as a main nutrient factor limiting diatom growth by analyzing N:P:Si ratios. Our model simulation relatively well-reproduced the increasing trend and the shift of seasonality of DSi and diatoms, even though peaks of diatom blooms were underestimated in some years. Among input variables, the concentration of resuspended sediments radically increased. The model simulation with the input variables or parameters changed suggested as follows: (1) the recent DSi release from resuspended sediments enhanced diatom abundance and (2) the degradation of light condition caused by resuspension affected the shift of blooming season. These findings implicate the significance of the interactions between sediments and water to phytoplankton blooms.

Keywords

Silicondiatomsreleasemodel simulationLake Kasumigaura
Type
Research Article
Information
Annales de Limnologie - International Journal of Limnology , Volume 50 , Issue 4 , 2014 , pp. 335 - 346
Copyright
© EDP Sciences, 2014

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References

Arai, H. and Fukushima, T., 2012. Silicon budget of eutrophic Lake Kasumigaura, Japan. J. Soils Sediments, 12, 1501–1507.CrossRefGoogle Scholar
Arai, H., Fukushima, T. and Komatsu, K., 2012. Increase in silicon concentrations and release from suspended solids and bottom sediments in Lake Kasumigaura, Japan. Limnology, 13, 81–95.CrossRefGoogle Scholar
Bailey-Watts, A.E., 1976a. Planktonic diatoms and some diatom-silica relations in a shallow eutrophic Scottish loch. Freshw. Biol., 6, 69–80.CrossRefGoogle Scholar
Bailey-Watts, A.E., 1976b. Planktonic diatoms and silica in Loch Leven, Kinross, Scotland: a one month silica budget. Freshw. Biol., 6, 203–213.CrossRefGoogle Scholar
Barbiero, R.P., Tuchman, M.L., Warren, G.J., and Rockwell, D.C., 2002. Evidence of recovery from phosphorus enrichment in Lake Michigan. Can. J. Fish. Aquat. Sci., 59, 1639–1647.CrossRefGoogle Scholar
Bormans, M. and Webster, I.T., 1999. Modelling the spatial and temporal variability of diatoms in the River Murray. J. Plankton Res., 21, 581–598.CrossRefGoogle Scholar
Brzezinski, M.A., 1985. The Si:C:N ratio of marine diatoms: interspecific variability and the effect of some environmental variables. J. Phycol., 21, 347–357.CrossRefGoogle Scholar
Callies, U., Scharfe, M. and Ratto, M., 2008. Calibration and uncertainty analysis of a simple model of silica-limited diatom growth in the Elbe River. Ecol. Modell., 213, 229–244.CrossRefGoogle Scholar
Conley, D.J., Kilham, S.S. and Theriot, E., 1989. Differences in silica content between marine and freshwater diatoms. Limnol. Oceanogr., 34, 205–213.CrossRefGoogle Scholar
Conley, D.J., Sommer, M., Meunier, J.D., Kaczorek, D. and Saccone, L., 2006. Silicon in the terrestrial biogeosphere. In: Ittekkot, V., Unger, D., Humborg, C. and Tac An, N. (eds.), The Silicon Cycle: Human Perturbations and Impacts on Aquatic Systems, Island, Washington, DC, 13–28.Google Scholar
Ferris, J.A. and Lehman, J.T., 2007. Interannual variation in diatom bloom dynamics: roles of hydrology, nutrient limitation, sinking, and whole lake manipulation. Water Res., 41, 2551–2562.CrossRefGoogle ScholarPubMed
Foundation of River and Watershed Environment Management, 2007. Research of the runoff mechanism for silicate and other dissolved inorganic matters in river (in Japanese).
Fukushima, T., 1984. Studies on the change characteristics and management of water quality in a shallow lake (in Japanese).
Fukushima, T., Kawamura, S., Seki, T., Onda, Y., Imai, A. and Matsushige, K., 2005. Why has Lake Kasumigaura become turbid? Verh. Int. Verein. Limnol., 29, 732–737.Google Scholar
Fukushima, T., Kamiya, K., Onda, Y., Imai, A. and Matsushige, K., 2010. Long-term changes in lake sediments and their influences on lake water quality in Japanese shallow lakes. Fund. App. Limnol., 177, 177–188.CrossRefGoogle Scholar
Gibson, C.E., 1984. Sinking rates of planktonic diatoms in an unstratified lake: a comparison of field and laboratory observations. Freshw. Biol., 14, 631–638.CrossRefGoogle Scholar
Harashima, A., Kimoto, T., Wakabayashi, T. and Toshiyasu, T., 2006. Verification of the silica deficiency hypothesis based on biogeochemical trends in the aquatic continuum of Lake Biwa – Yodo River – Seto Inland Sea, Japan. AMBIO, 35, 36–42.CrossRefGoogle ScholarPubMed
Havens, K.E., Fukushima, T., Xie, P., Iwakuma, T., James, R.T., Takamura, N., Hanazato, T. and Yamamoto, T., 2001. Nutrient dynamics and the eutrophication of shallow lakes Kasumigaura (Japan), Donghu (PR China), and Okeechobee (USA). Environ. Pollut., 111, 263–272.CrossRefGoogle Scholar
Humborg, C., Ittekkot, V., Cociasu, A. and Bodungen, B., 1997. Effect of Danube river dam on Black sea biogeochemistry and ecosystem structure. Nature, 386, 385–388.CrossRefGoogle Scholar
Imai, A., Fukushima, T., and Matsushige, K., 1999. Effects of iron limitation and aquatic humic substances on the growth of Microcystis aeruginosa. Can. J. Fish. Aquat. Sci., 56, 1929–1937.CrossRefGoogle Scholar
Ittekkot, V., Humborg, C. and Schafer, P., 2000. Hydrological alterations and marine biogeochemistry: a silicate issue? Bioscience, 50, 776–782.CrossRefGoogle Scholar
Köhler, J., Hilt, S., Adrian, R., Nicklisch, A., Kozerski, H.P. and Walz, N., 2005. Long-term response of a shallow, moderately flushed lake to reduced external phosphorus and nitrogen loading. Freshw. Biol., 50, 1639–1650.CrossRefGoogle Scholar
Koszelnik, P. and Tomaszek, J.A., 2008. Dissolved silica retention and its impact on eutrophication in a complex of mountain reservoirs. Water Air Soil Pollut., 189, 189–198.CrossRefGoogle Scholar
Kristiansen, S. and Hoell, E.E., 2002. The importance of silicon for marine production. Hydrobiologia, 484, 21–31.CrossRefGoogle Scholar
Li, M., Xu, K., Watanabe, M. and Chen, Z., 2007. Long-term variations in dissolved silicate, nitrogen, and phosphorus flux from the Yangtze River into the East China Sea and impacts on estuarine ecosystem. Estuar. Coast. Shelf. Sci., 71, 3–12.CrossRefGoogle Scholar
Matsuoka, Y., 1984. An eutrophication model of Lake Kasumigaura. Res. Rep. Natl. Inst. Environ. Stud. Jpn., 54, 53–242 (in Japanese with English abstract).Google Scholar
Muraoka, K. and Fukushima, T., 1986. On the box model for prediction of water-quality in eutrophic lakes. Ecol. Modell., 31, 221–236.CrossRefGoogle Scholar
Nagai, M., Sugiyama, M. and Hori, T., 2001. Environmental chemistry of rivers and lakes, Part VII. Fractionation by calculation of suspended particulate matter in Lake Biwa into three types of particles of different origins. Limnology, 2, 147–155.CrossRefGoogle Scholar
NIES, 2013. Lake Kasumigaura Database. Available online at: http://db.cger.nies.go.jp/gem/moni-e/inter/GEMS/database/kasumi/contents/database/datalist.html, Cited on 16 August 2013.
Officer, C.B. and Ryther, J.H., 1980. The possible importance of silicon in marine eutrophication. Mar. Ecol. Prog. Ser., 3, 83–91.CrossRefGoogle Scholar
Ptacnik, R., Andersen, T., and Tamminen, T., 2010. Performance of the Redfield Ratio and a family of nutrient limitation indicators as thresholds for phytoplankton N vs. P limitation. Ecosystems, 13, 1201–1214.CrossRefGoogle Scholar
Redfield, A.C., Ketchum, B.H. and Richards, F.A., 1963. The influence of organismson the composition of sea-water. In: Hill, M.N. (ed.), The Sea, Volume 2: The Composition of Sea-Water Comparative and Descriptive Oceanography, Harvard University Press, Cambridge, 26–77.Google Scholar
Reynolds, C.S., 1973. The seasonal periodicity of planktonic diatoms in a shallow eutrophic lake. Freshw. Biol., 3, 89–110.CrossRefGoogle Scholar
Scavia, D. and Fahnenstiel, G.L., 1987. Dynamics of Lake Michigan phytoplankton: mechanisms controlling epilmnetic communities. J. Great Lakes Res., 13, 103–120.CrossRefGoogle Scholar
Schelske, C.L., 1985. Biogeochemical silica mass balances in Lake Michigan. Biogeochemistry, 1, 197–218.CrossRefGoogle Scholar
Schelske, C.L., 1999. Diatoms as mediators of biogeochemical silica depletion in the Laurentian Great Lakes. In: Stoermer, E.F. and Smol, J.P. (eds.), The Diatoms: Applications for the Environmental and Earth Science. Cambridge University, Cambridge, 73–84.CrossRefGoogle Scholar
Seki, T., Fukushima, T., Imai, A. and Matsushige, K., 2006. Turbidity increase and sediment resuspension in Lake Kasumigaura. Doboku Gakkai Ronbunshu G, 62, 122–134 (in Japanese with English abstract).CrossRefGoogle Scholar
Shatwell, T., Köhler, J. and Nicklisch, A., 2013. Temperature and photoperiod interactions with silicon-limited growth and competition of two diatoms. J. Plankton Res., 35, 957–971.CrossRefGoogle Scholar
Sicko-Goad, L., Schelske, C.L. and Stoermer, E.F., 1984. Estimation of intracellular carbon and silica content of diatoms from natural assemblages using morphometric techniques. Limnol. Oceanogr., 29, 1170–1178.CrossRefGoogle Scholar
Sommer, U. and Stabel, H.H., 1983. Silicon consumption and population density changes of dominant planktonic diatoms in Lake Constance. J. Ecol., 71, 119–130.CrossRefGoogle Scholar
Takamura, N., Otsuki, A., Aizaki, M. and Nojiri, Y., 1992. Phytoplankton species shift accompanied by transition from nitrogen dependence to phosphorus dependence of primary production in Lake Kasumigaura, Japan. Arch. Hydrobiol., 124, 129–148.Google Scholar
Takano, K. and Hino, S., 1996. The effect of silicon concentration on replacement of dominant diatom species in a silicon-rich Lake. Jpn. J. Limnol., 57, 153–162.CrossRefGoogle Scholar
Teodoru, C., Dimopoulos, A. and Wehrli, B., 2006. Biogenic silica accumulation in the sediments of Iron Gate I Reservoir on the Danube River. Aquat. Sci., 68, 469–481.CrossRefGoogle Scholar
Titman, D. and Kilham, P., 1976. Sinking in freshwater phytoplankton: some ecological implications of cell nutrient status and physical mixing processes. Limnol. Oceanogr., 21, 409–417.CrossRefGoogle Scholar
Tomioka, N., Imai, A., and Komatsu, K., 2011. Effect of light availability on Microcystis aeruginosa blooms in shallow hypereutrophic Lake Kasumigaura. J. Plankton Res., 33, 1263–1273.CrossRefGoogle Scholar
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