Silicon limitation on primary production and its destiny in Jiaozhou Bay, China

Yang Dongfang; Gao Zhenhui; Wang Peigang; Sun Peiyan; Liu Shuang

doi:10.1007/BF02894234

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Silicon limitation on primary production and its destiny in Jiaozhou Bay, China

OriginalPaper | Updated：2023-05-16

- Silicon limitation on primary production and its destiny in Jiaozhou Bay, China
- Silicon limitation on primary production and its destiny in Jiaozhou Bay, China
- 海洋湖沼学报（英文） 2005年23卷第2期页码：169-175
- Affiliations：
  
  1. College of Fishery Science Shanghai Fisheries University
  2. Beihai Monitoring Center State Oceanic Administration
  3. Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  This study was funded by the key subject development of Shanghai Education Council (04SC12), the Director’s Foundation of the Beihai Monitoring Center and the State Oceanic Administration and Chinese Academy of Science (KZCX 2-207).
- DOI：10.1007/BF02894234
  中图分类号：
- 纸质出版：2005
- Accepted：
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Silicon limitation on primary production and its destiny in Jiaozhou Bay, China[J]. 海洋湖沼学报（英文）, 2005,23(2):169-175.

Dongfang, Y., Zhenhui, G., Peigang, W. et al. Silicon limitation on primary production and its destiny in Jiaozhou Bay, China., Chin. J. Ocean. Limnol. 23, 169–175 (2005). https://doi.org/10.1007/BF02894234
Silicon limitation on primary production and its destiny in Jiaozhou Bay, China[J]. 海洋湖沼学报（英文）, 2005,23(2):169-175. DOI： 10.1007/BF02894234.

Dongfang, Y., Zhenhui, G., Peigang, W. et al. Silicon limitation on primary production and its destiny in Jiaozhou Bay, China., Chin. J. Ocean. Limnol. 23, 169–175 (2005). https://doi.org/10.1007/BF02894234 DOI：

摘要

Abstract

Silicon is a necessary nutrient for diatoms

silicon uptake in diatom reproduction decreased seawater silicon content. This paper clarified the characteristics of silicon transferring in the sea

which plays an important role in phytoplankton growth

zooplankton graze and marine ecosystem. Analysis revealed that silicate is supplied by terrestrial sources

through plankton uptake

death

and eventually deposits to the sea bottom

and cannot diffuse upward. This is a general silicon deficit process. Many global marine waters showed the same silicon transfer route: land→silicon biogeochemical process→sea bottom. River flow brings abundant silicate into marine waters

silicate concentration in the waters decreased in the distance away from the river estuaries. In discussion of silicon characteristics and its transfer route

it was considred that the main factor controlling the mechanism of diatom and non-diatom red tides occurrence is silicon

and the changes in silicon source. Human activities

such as sea-route cutting by building embankment and dam

and silicon supplement by the sea

such as sandstorm

rainstorm and storm tide

have largely impaired the earth ecosystem and hugely threatened the human existence. It is suggested in this paper that man should resume the original face of the Si input into the sea to keep natural ecosystem in sustainable pattern.

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references

Armstrong, F. A. J., 1965. Silicon.In: Riley J. P. and G. Skirrow, eds, Chemical Oceanography, Vol. 1, Chap. 10. Academic Press, London.

Bienfang, P. K., P. J. Harrison and L. M. Quarmby, 1982. Sinking rate response to depletion of nitrate, phosphate and silicate in fourine diatoms.Mar. Biol. 67: 295–302.

Broecker, W. S. and T. H. Peng, 1982. Tracers in the Sea. Eldigio Press, Lamout-Doherty Geological Obsergvatory of Columbia University, Palisades, New York. pp. 690.

Brzezinski, M. A. and D. M. Nelson, 1989. Seasonal changes in the silicon cycle with a Gulf Stream warm-core ring.Deep-sea Research 36: 1 009–1 030.

Brzezinski, M. A., 1992. Cell-cycle effects on the kinetics of silicic acid uptake and resource competition among diatoms.Journal of Plankton Research 14: 1 511–1 536.

Brzezinski, M. A., R. J. Olson and S. W. Chisholm, 1990. Silicon availability and cell-cycle progression in marine diatoms.Marine Ecology Progress Series 67: 83–96.

Comley, D. J. and T. C. Malone, 1992. Annual cycle of dissolved silicate in Chesapeake Bay: implications for the production and fate of phytoplankton biomass.Marine Ecology Progress Series 81: 121–128.

De Master, D. J., 1981. The supply and accumulation of silica in the marine environment.Geochimica et Cosmochimica Acta 45: 1 715–1 732.

Dugdale, R. C., 1972. Chemical oceanography and primary productivity in upwelling regions.Geoforum 11: 47–61.

Dugdale, R. C., 1983. Effects of source nutrient concentrations and nutrient regeneration on production of organic matter in coastal upwelling centers.In: Pt. Suess A. E. and J. Thiede, eds. Coastal Upwelling. Plenum Press, New York. p. 175–182.

Dugdale, R. C. and J. J. Goering, 1967. Uptake of new and regenerated forms of nitrogen in primary productivity.Limn. and Oceanog. 12: 196–206.

Dugdale, R. C., B. H. Jones, J. J. Macclsaac and J. J. Goering, 1981. Adaptation of nutrient assimilation.In: Platt, T. ed., Physiological bases of phytoplankton ecology, Canadian Bulletin of Fisheries and Agriculture Sciences. p. 234–250.

Dugdale, R. C., F. P. Wilkerson and H. J. Minas, 1995. The role of a silicate pump in driving new production.Deep-sea Res(I) 42(5): 697–719.

Fott, B., 1971. Algenkunde. VEB Gustav Fischer Verlag. Translated by D. Luo, Shanghai Scientific & Technical Publisher, Shanghai, China. Alga. 1980. p. 370–448. (in Chinese)

Farnas, M. J., 1990. In situ growth rates of marine phytoplankton: approaches to measurement, community and species growth rate.Journal of Plankton Research 12: 1 117–1 151.

Groupe, M., 1976. Resultats des campagnes a la mer No. 10, CINECA 5 Cruise Rep. CNEO, Brest.

Horne, R. A., 1969. The structure of water and the chemistry of the Hydrosphere.Marine Chemistry 13: 146–149.

Kemp, A. E. S., J. Pike, R. B. Pearce and C. B. Lange, 2000. The “fall dump”—a new perspective on the role of a “shade flora” in the annual cycle of diatom production and export flux.Deep-sea Res. II47: 2 129–2 154.

Lewin J. C., 1962. Silicification.In: Lewin, R.E. ed., Physiology and Biochemistry of the Algae, Academic Press, New York. p. 445–455.

Lutjeharms, J. R. E., N. M. Walters and B. R. Allarson, 1985. Oceanic frontal system and biological enhancement.In: Siegfried, W. R., P. R. Condy and R. M. Laws, eds Antarctic Nutrient Cycles and Food Weds. Springer-Verlag, Berlin. p. 11–21.

Minas, H. J., L. A. Codispoti, and R. C. Dugdale, 1982. Nutrients and primary production in the upwelling region off northwest Africa. Rapp. P.-v. Reun. Const. Int. Explor. Mer180: 141–176.

Nelson, D. M., P. Tréguer, M. A. Brzezinski, A. Leynaert, and B. Quéguiner, 1995. Production and dissolution of biogenic silica in the ocean: revised global estimates, comparison with regional data and relationship with biogenic sedimentation.Global Biogeochemical Cycles 9: 359–372.

Steemann-Nielsen, E., 1975. Marine Photosynthesis. Amsterdam. Elsevier Scientific Pub. Co. Translated into Chinese by Zhou B. and Z. Wen, 1979. Science Press, Beijing, China. p. 28–35.

Nybakken, J. W., 1982. Marine Biology: An Ecological Approach. Harper & Row Publishers Inc., New York. Translated into Chinese by Lin, G. and H. Li, 1991. Marine Press, Beijing, China. p. 39–42. (in Chinese)

Qian, S., Y. Wang and G. Chen, 1983. Jiaozhou Bay diatoms.Journal of Shandong Marine College 13(1): 39–56. (in Chinese)

Smetacek, V., 1999. Bacteria and silica cycling.Nature 397: 475–476.

Smetacek, V., 2000. The giant diatom dump.Nature 406: 574–575.

Kiyozi, K., 1960. Phytoplankton. Star Publishing House (Kosai Sha). Translated by R. Hua, Shanghai Scientific & Technical Publisher, Shanghai, China. p. 18–51. (in Chinese)

Spencer, C. P., 1975. The Micronutrient Elements.In: Riley, J. P. and G. Skirrow, eds., Chemical Oceanography, Vol. 2, 2nd ed., Academic Press, New York, p. 245–300.

Sverdrup, H. U., M. W. Johnson and R. H. Fleming, 1942. The Oceans. Prentice Hall, New York. Translated into Chinese by H. Mao, 1959. Science Press, Beijing, China. p. 665–676, 685–691.

Tréguer, P., D. M. Nelson, A. J. van Bennekom, D. J. De-Master, A. Leynaert and B. Quéguiner, 1995. The silica balance in the world ocean: a reestimate.Science 268: 375–379.

Tréguer, P. and A. J. van Bennekom, 1991. The annual production of biogenic silica in the Antarctic Ocean.Marine Chemistry 35: 477–487.

van Bennekom, A. J., G. W. Berger, S. J. van der Gaast and R. T. P. de Vries, 1988. Primary productivity and the silica cycle in the Southern Ocean (Atlantic Sector).Palaeogeogr., Palaeoclimatol., Palaeoecol. 67: 19–30.

Xiao, Y., S. Gao and H. Zhang, 1992. Biological environment in Jiaozhou Bay: zooplankton.In: Ruiyu Liu, ed., Ecology and Living Resources of Jiaozhou Bay, Science Press, Beijing, China. p. 170–202. (in Chinese)

Yang, D., J. Jing, L. Zhang et al., 2002. Examination of silicate limitation of primary production in the Jiaozhou Bay, North China I. Silicate being a limiting factor of phytoplankton primary production.Chin. J. Oceanol. Limnol. 20(3): 208–25.

Yang, D., J. Zhang, Z. Gao et al., 2003a. Examination of silicate limitation of primary production in the Jiaozhou Bay, North China II. Critical value and time of silicate limitation and satisfaction of the phytoplankton growth.Chin. J. Oceanol. Limnol. 21(1): 46–63.

Yang, D., Z. Gao, Y. Chen et al., 2003b. Examination of silicate limitation of primary production in the Jiaozhou Bay, North China III. Judgment method, rules and uniqueness of nutrient limitation among N, P, and SiChin. J. Oceanol. Limnol. 21(2): 114–133.

Yang, D., Y. Chen, Z. Gao et al., 2005. Silicate limitation on primary production and its destiny in Jiaozhou Bay, China IV. Study on cross-bay transect from estuary to oceanChin. J. Oceanol. Limnol. 23(1): 72–90.

Yang, X., M. Zhu, 1990. The new development of phytoplankton metabolism study.Journal of Oceanography of Huanghai & Bohai Seas 3: 65–72. (in Chinese)

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