Abstract
The large diatom Coscinodiscus asteromphalus was separated from seawater in Jiaozhou Bay using a repeated precipitation method, and then, its nutrient compositions of carbon (C), nitrogen (N), phosphorus (P), and silicon (Si ) combined with chlorophyll-a (Chl-a) were examined for the first time for a natural population . Results show that the contents of C, N, P, Si , and Chl-a in C. asteromphalus cells were 35,610.5, 9374.2, 352.4, 1105.5, and 1767.0 pg/cell , respectively, and the corresponding molar ratios of C/N, N/P, Si /P, and Si /N in C. asteromphalus cells were 4.5, 66.0, 2.7, and 0.07, respectively, which are different from the Redfield ratio. Additionally, their C/Chl-a mass ratio was 23.2. High N/P ratio and low Si /P and Si /N ratios in C. asteromphalus cells were consistent with those in particulates of any size and seawater in the bay, reflecting an ecological response of phytoplankton to the nutrient structure of seawater, suggesting Si limitation to phytoplankton growth. The fact that C. asteromphalus spread all over the bay mainly in summer and autumn and the fact that Chl-a content in C. asteromphalus cells could account for a maximum percentage of 78% of those in the water column suggest that the contribution of C. asteromphalus to phytoplankton biomass was significant in Jiaozhou Bay .
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References
Baines, S. B., Twining, B. S., Vogt, S., Balch, W. M., Fisher, N. S., & Nelson, D. M. (2011). Elemental composition of equatorial Pacific diatoms exposed to additions of silicic acid and iron. Deep-Sea Research II, 58, 512–523.
Beardall, J., Young, E., & Roberts, S. (2001). Approaches for determining phytoplankton nutrient limitation. Aquatic Sciences, 63, 44–69.
Bienfang, P. K., & Harrison, P. J. (1984). Co-variation of sinking rate and cellquota among nutrient replete marine phytoplankton. Marine Ecology Progress Series, 14, 297–300.
Brzezinski, M. A. (1985). The Si: C: N ratio of marine diatoms: Interspecific variability and the effect of some environmental variables. Journal of Phycology, 21, 347–357.
Burkhardt, S., & Riebesell, U. (1997). CO2 availability affects elemental composition (C:N:P) of the marine diatom Skeletonema costatum. Marine Ecology Progress Series, 155, 67–76.
Eppley, R. W., Reid, F. M. H., & Strickland, J. D. H. (1970). The ecology of the plankton off La Jolla, California, in the period April through September 1967. Part 1. Estimates of phytoplankton crop size, growth rate and primary production. In J. D. H. Strickland (Ed.), Bulletin, Scripps Institution of Oceanography, Vol. 17, pp 33–42.
Koroleff, F. (1976). Determination of total phosphorus. In K. Grasshoff (Ed.), Methods of seawater analysis (pp. 123–125). Weinheim: Verlag Chemie.
Tada, K., Pithakpol, S., Ichimi, K., & Montani, S. (2000). Carbon, nitrogen, phosphorus, and chlorophyll a content of the large diatom, Coscinodiscus wailesii and its abundance in the Seto Inland Sea, Japan. Fisheries Science, 66, 509–514.
Marchetti, A., & Harrison, P. J. (2007). Coupled changes in the cell morphology and the elemental (C, N, and Si) composition of the pennate diatom Pseudo-nitzschia due to iron deficiency. Limnology and Oceanography: Mathods, 52(5), 2270–2284.
Moal, J., Martin-Jezequel, V., Harris, R. P., Samain, J.-F., & Poulet, S. A. (1987). Interspecific and intraspecific variability of the chemical composition of marine phytoplankton. Oceanologica Acta, 10, 339–346.
Mullin, M. M., Sloan, P. R., & Eppley, R. W. (1966). Relationship between carbon content, cell volume, and area in phytoplankton. Limnology and Oceanography, 11, 307–311.
Parsons, T. R., Takahashi, M., & Hargrave, B. (1984). Biological oceanographic processes (3rd ed.). Oxford: Pergamon Press.
Redfield, A. C., Ketchum, B. H., & Richards, F. (1963). The influence of organisms on the composition of seawater. In M. N. Hill (Ed.), The sea (Vol. 2, pp. 26–77). New York: Wiley.
Ríos, A. F., Fraga, F., Pérez, F. F., & Figueiras, F. G. (1998). Chemical composition of phytoplankton and particulate organic matter in the Ría de Vigo (NW Spain). Scientia Marina, 62(3), 257–271.
Sakshaug, E., Andresen, K., Myklestad, S., & Olsen, Y. (1983). Nutrient status of phytoplankton communities in Norwegian waters marine, brackish, and fresh as revealed by their chemical composition. Journal of Plankton Research, 5, 175–196.
Segura-Noguera, M., Dolors, B., & Jose-Manuel, F. (2012). An improved energy-dispersive X-ray microanalysis method for analyzing simultaneously carbon, nitrogen, oxygen, phosphorus, sulfur, and other cation and anion concentrations in single natural marine microplankton cells. Limnology and Oceanography-Methods, 10, 666–680.
Segura-Noguera, M., Dolors, B., & Jose-Manuel, F. (2016). Taxonomic and environmental variability in the elemental composition and stoichiometry of individual dinoflagellate and diatom cells from the NW Mediterranean Sea. PLoSONE, 11(4), e0154050. https://doi.org/10.1371/journal.pone.0154050.
Shen, Z. L. (2001). Historical changes in nutrient structure and its influences on phytoplankton composition in Jiaozhou Bay. Estuarine, Coastal and Shelf Science, 52, 211–224.
Shen, Z. L., Liu, Q., Wu, Y. L, & Yao, Y. (2006). Nutrient structure of seawater and ecological responses in Jiaozhou Bay, China. Estuarine, Coastal and Shelf Science, 69(1–2), 299–307.
Shen, Z. L., Wu, Y. L., Liu, Q., & Yao, Y. (2008). Nutrient compositions of cultured Thalassiosira rotula and Skeletonema costatum from the Jiaozhou Bay in China. Acta Oceanologica Sinica, 27(4), 147–155.
Strathmann, R. R. (1967). Estimating organic carbon content of phytoplankton from cell volume or plasma volume. Limnology and Oceanography, 12, 411–418.
Strickland, J. D. H. (1960). Measuring the production of marine phytoplankton. Bulletin of the Fisheries Research Board of Canada, 122, 172 p.
Sun, J., Liu, D. Y., Qian, S. B. (2000). Estimating biomass of phytoplankton in the Jiaozhou Bay I. Phytoplankton biomass estimated from cell volume or plasma volume. Acta Oceanologica Sinica, 19 (2), 97–110.
Taguchi, S. (1976). Relationships between photosynthesis and cell size of marine diatoms. Journal of Phycology, 12, 185–189.
Treguer, P., & Gueneley, S. (1988). Biogenic silica and particulate organic matter from the Indian Sectoer of the Southern Ocean. Marine Chemistry, 23, 167–180.
Werner, D. (1971). The life cycle with sexual phase in the marine diatom Coscinodiscus asteromphalus. II. Surface-dependant differentiation during the vegetative celldiminutio. Archiv Fur Mikrobiologie, 80, 115–133.
Yang, H. M., & Liu, Q. (1995). A modified method for determination of particulate organic carbon (POC) and particulate nitrogen (PN) in seawater. In J. H. Dong & N. Z. Jiao (Eds.), Ecology studies in Jiaozhou Bay (pp. 53–56). Beijing: Science Press. (in Chinese with English abstract).
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Shen, Z., Shi, Q., Zheng, S., Pan, S. (2020). Nutrient Composition and Biomass of Coscinodiscus asteromphalus in Jiaozhou Bay, China. In: Shen, Z. (eds) Studies of the Biogeochemistry of Typical Estuaries and Bays in China. Springer Earth System Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-58169-8_17
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