The teleconnection between marine silicon supply and desertification in China

Dongfang Yang; Jianping Wu; Shengtao Chen; Qing Lu

doi:10.1007/s00343-007-0116-7

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The teleconnection between marine silicon supply and desertification in China

OriginalPaper | Updated：2023-05-16

- The teleconnection between marine silicon supply and desertification in China
- The teleconnection between marine silicon supply and desertification in China
- 海洋湖沼学报（英文） 2007年25卷第1期页码：116-122
- Affiliations：
  
  1. School of Environmental and Public Health Wenzhou Medical College
  2. North China Sea Environmental Monitoring Center SOA
  3. College of Fishery Science Shanghai Fisheries University
  4. Huanghai Institute of Marine Survey and Engineering
- Author bio：
- Funds：
  
  Funded by the Director’s Foundation of the Beihai Monitoring Center and the State Oceanic Administration and Chinese Academy of Sciences (KZCX 2-207).
- DOI：10.1007/s00343-007-0116-7
  中图分类号：
- 纸质出版：2007
- Accepted：
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The teleconnection between marine silicon supply and desertification in China[J]. 海洋湖沼学报（英文）, 2007,25(1):116-122.

Yang, D., Wu, J., Chen, S. et al. The teleconnection between marine silicon supply and desertification in China., Chin. J. Ocean. Limnol. 25, 116–122 (2007). https://doi.org/10.1007/s00343-007-0116-7
The teleconnection between marine silicon supply and desertification in China[J]. 海洋湖沼学报（英文）, 2007,25(1):116-122. DOI： 10.1007/s00343-007-0116-7.

Yang, D., Wu, J., Chen, S. et al. The teleconnection between marine silicon supply and desertification in China., Chin. J. Ocean. Limnol. 25, 116–122 (2007). https://doi.org/10.1007/s00343-007-0116-7 DOI：

摘要

Abstract

Desertification has been notably expanding in China in the recent decade

especially in North China where dust/sand storm (DSS) frequently assaulted local communities. Analyses in marine ecology found that the earth ecosystem could be able to complement nutrient silicon for keeping sustainable development of marine ecosystem

and decreasing CO2 concentration in the atmosphere; as a result

the area of desertification would be enlarged. Modern human being activities have resulted in constant changes in the amount of silicon transport from land into sea

leading to oversupply of nitrogen and phosphorus but silicon in seawater. The proportion of nitrogen

phosphorus and silicon was seriously imbalanced and the limitation of silicon for phytoplankton growth has become more serious. The silicon deficiency has damaged the marine ecosystem in coastal regions and slowed down the carbon sedimentation in the atmosphere of the world. The authors believe that the continual discharge of CO2 into the atmosphere is the cause for the global warming including marine water temperature rise. Consequently

the earth ecosystem would have to trigger its complementary action to resume to the silicon balance by algae bloom in seawater for reducing air and water temperatures. In order to complement nutrient silicon into the sea

the ecosystem would transport silicon via the atmosphere; therefore

the desertification in the inner land is a natural reaction. As marine phytoplankton booming can reduce the CO2 concentration in the atmosphere and further ease the green-house effect

during this process

a large amount of silicon are demanded by the ecosystem

which human being are unable to stop desertification from happening but slow down the progress and ease the risk. Therefore

as an important role in earth ecosystem

people should reduce the CO2 discharge into the atmosphere first; then

the normal function of river transporting silicon must be restored. In this way

the CO2 in the atmosphere can be kept in balance

the global warming slowed down

marine ecosystem development sustained

the drought in inner land eased

and the desert gradually under-controlled.

关键词

Keywords

references

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

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.

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.

Conley, 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.

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

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

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

Dugdale, R. C., 1985. The effects of varying nutrient concentration on biological production in upwelling regions. CalCOFI Report. 26: 93–96.

Dugdale, R. C., B. H. Jones, J. J. Macclsaac et al., 1981. Adaptation of nutrient assimilation. In: Platt, T., ed., Physiological bases of phytoplankton ecology. Canadian Bulletin of Fisheries and Agriculture Sciences 210: 234–250.

Huang, S. G., J. D. Yang, W. D. Ji, X. L. Yang and G. X. Chen, 1983. Proceedings of International Symposium on Sedimentation on the Continental Shelf with Special Reference to the Fast China Sea. Vol. 1, China Ocean Press, Beijing, 241–249.

Humborg, C., V. Lttekkot, A. Cociasu, and B. von Bodungen, 1997. Effect of Danube River dam on Black Sea biogeochemistry and ecosystem structure. Nature 386: 385–388.

Liu, Z. Y., 2002. Why does dust/sand storm increase? China National Conditions and Strength 6: 34–35. (in Chinese)

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

Paytan, A., 2000. Global change: Iron uncertainty. Nature 406: 468–469.

Sakshaug, E., D. Slagstad and O. Holm-Hansen, 1991. Factors controlling the development of phytoplankton blooms in the Antarctic Ocean—a mathematical model. Marine Chemistry 35: 259–271.

Stefánsoon, U. and F. A. Richards, 1963. Processes contributing to the nutrient distributions off the Columbia River and strait of Juan de Fuca. Limmol. Oceanogr. 8: 394–410.

Toggweller, J. R., 1999. An ultimate limiting nutrient. Nature 400: 511–512

Turner, R. E. and N. N. Rabalais, 1991. Changes in Mississippi River water quality this century—implications for coastal food webs. Science 41: 140–147.

Wang, T., W. Wu, X. Xue, Q. W. Sun, W. M. Zhang, Z. W. Han, 2004. Spatial-temporal changes of sandy desertified land during last 5 decades in northern China. Acta Geographica Sinica 2, 203–212. (In Chinese)

Yang, X. L. and M. Y. Zhu, 1990. The new development of phytoplankton metabolism study. J. of Oceanography of Huanghai & Bohai Seas 3: 65–72.

Yang, D. F., H. Li, Y. M. Zhang et al., 2000. The factor and way of limiting nutrient for the growth of phytoplankton. Marine Sciences 24(12): 47–50.

Yang, D. F., Z. H. Gao, Y. Chen et al., 2002a. The Biogechemical Process of Silicon. Marine Sciences 26(3): 35–36.

Yang, D. F., J. Zhang, J. B. Lu et al., 2002b. 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): 208–225.

Yang, D. F., J. Zhang, Z. H. 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. F., Z. H. Gao, Y. Chen, J. Zhang and P. G. Wang, 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 Si. Chin. J. Oceanol. Limnol. 21(2): 114–133.

Yang, D. F., Z. H. Gao, J. Zhang, W. L. Cui, Q. Shi, 2004a. Examination of daytime length’s influence on phytoplankton growth in Jiaozhou Bay, China. Chin. J. Oceanol. Limnol. 22(1): 70–82

Yang, D. F., Z. H. Gao, Y. Chen, P. G. Wang, P. Y. Sun, 2004b. Examination of seawater temperature’s influence on phytoplankton growth in Jiaozhou Bay, North China. Chin. J. Oceanol. Limnol. 22(2): 166–175.

Yang, D. F., Y. Chen, Z. H. Gao, J. Zhang, and F. Wang, 2005a. Silicon limitation on primary production and its destiny in Jiaozhou Bay, China IV. Transect offshore the coast with estuaries. Chin. J. Oceanol. Limnol. 23(1): 72–90.

Yang, D. F., Z. H. Gao, Y. Chen, P. G. Wang, P. Y. Sun and S. Liu, 2005b. Silicon limitation on primary production and its destiny in Jiaozhou Bay, China V. Silicon deficit process. Chin. J. Oceanol. Limnol. 23(2): 169–175.

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