Abstract
In order to determine whether phytoplankton growth rates were normal or depressed, total plant carbon (μg l−1) and in situ production rates (μg C l−1 d−1) were measured for phytoplankton assemblages at Weathership Station P (50°N; 145°W) and at 53°N; 145°W in the subarctic Pacific in May and August 1984. Plant carbon, estimated from cell volumes determined using epifluorescence microscopy, was distributed as follow: 28% in the <2 μm fraction, 38% in the 2 to 5 μm size fraction, and the remainder in size classes >5 μm. Carbon-specific growth rates (k), as doublings d−1, were calculated for the phytoplankton assemblages as a whole at each sampling depth down to 100 m for three days in May and for four days in August. The populations in the upper part of the euphotic zone showed average doubling rates of 1 d−1 and thus appeared to be growing at rates normally expected for the prevailing conditions of light and temperature. The low chlorophyll concentrations (0.3 to 0.4 mg chl a m−3) characteristically found in this oceanic region do not seem to be due to very slow growth of algal populations.
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Literature cited
Anderson, G. C., Lam, R. L., Booth, B. C., Glass, J. M. (1977). A description and numerical analysis of the factors affecting the processes of production in the Gulf of Alaska. In: Environmental assessment of the Alaskan continental Shelf, Annual Reports of Principal Investigators for the Year Ending, March 1977, Vol. 7. Receptors — Fish, littoral, benthos. National Oceanic and Atmospheric Administration, U.S. Department of the Interior, Washington, D.C., p. 477–798 (Ref. NOAA-OCSEAP, NOAA 03-5-022-67)
Antia, N. J., McAllister, C. D., Parsons, T. R., Stephens, K. (1963). Measurements of primary production using a large-volume plastic sphere. Limnol. Oceanogr. 8: 166–183
Beers, J. R., Stevenson, M. R., Eppley, R. W., Brooks, E. R. (1971). Plankton populations and upwelling off the coast of Peru, June 1969. Fish. Bull. U.S. 69: 859–876
Bienfang, P. K., Takahashi, M. (1983). Ultraplankton growth rates in a subtropical ecosystem. Mar. Biol. 76: 213–218
Booth, B. C. (1987). The use of autofluorescence for analyzing oceanic phytoplankton communities. Botanica mar. 30: 101–108
Booth, B. C. (1988). Size classes and major taxonomic groups of phytoplankton at two locations in the subarctic Pacific Ocean in May and August, 1984. Mar. Biol. 97: 275–286
Cuhel, R. L., Waterbury, J. B. (1984). Biochemical composition and short term nutrient incorporation patterns in a unicellular marine cyanobacterium, Synechococcus (WH 7803). Limnol. Oceanogr. 29: 370–373
Denman, K. L., Gargett, A. E. (In press). Multiple thermoclines are barriers to vertical exchange in the subarctic Pacific during SUPER, May 1984. J. mar. Res.
Douglas, D. J. (1984). Microautoradiography-based enumeration of photosynthetic picoplankton with estimates of carbon-specific gowth rates. Mar. Ecol. Prog. Ser. 14: 223–228
Durbin, E. G., Krawiec, R. W., Smayda, T. J. (1975). Seasonal studies on the relative importance of different size fractions of phytoplankton in Narragansett Bay (USA). Mar. Biol. 32: 271–287
Emery, W. J., Royer, T. C., Reynold, R. W. (1985). The anomalous tracks of North Pacific drifting buoys 1981–1983. Deep-Sea Res. 32: 315–347
Eppley, R. W. (1972). The temperature and phytoplankton growth in the sea. Fish. Bull. U.S. 70: 1063–1085
Eppley, R. W. (1977). The growth and culture of diatoms. In: Werner, D. (ed.) The biology of diatoms. Blackwell, Oxford, p. 24–64
Eppley, R. W. (1981). Relations between nutrient assimilation and growth in phytoplankton with a brief review of estimates of growth in the ocean. Can. Bull. Fish. aquat. Sciences 210: 251–263
Eppley, R. W., Reid, F. M. H., Strickland, J. D. H. (1970). Estimates of phytoplankton crop size, growth rate and primary production. Bull. Scripps Instn Oceanogr. 17: 33–42
Eppley, R. W., Renger, E. H., Venrick, E. L., Mullin, M. M. (1973). A study of plankton dynamics and nutrient cycling in the central gyre of the North Pacific Ocean. Limnol. Oceanogr. 18: 534–551
Frost, B. W. (1987). Grazing control of phytoplankton stock in the open subarctic Pacific Ocean: a model assessing the role of mesozooplankton, particularly the large calanoid copepods Neocalanus spp. Mar. Ecol. Prog. Ser. 39: 49–68
Furnas, M. J. (1982). Growth rates of summer nanoplankton (<10 μm) populations in Lower Narragansett Bay, Rhode Island, USA. Mar. Biol. 70: 105–115
Furuya, K., Takahashi, M., Nemoto, T. (1986). Summer phytoplankton community structure and growth in a regional upwelling area off Hachijo Island, Japan. J. exp. mar. Biol. Ecol. 96: 43–55
Goldman, J. C., Carpenter, E. J. (1974). A kinetic approach to the effect of temperature on algal growth. Limnol. Oceanogr. 19: 756–766
Guillard, R. R. L. (1973). Division rates. In: Stein, J. R. (ed.) Handbook of phycological methods, Vol. I. Cambridge University Press, New york, p. 289–312
Hobson, L. A. (1971). Relationships between particulate organic carbon and microorganisms in upwelling areas off SW Africa. Investigaćon pesq. 35: 195–208
Iturriaga, R., Mitchell, B. G. (1986). Chroococcoid cyanobacteria: a significant component in the food web dynamics of the open ocean. Mar. Ecol. Prog. Ser. 28: 291–297
Joint, I. R., Owens, N. J. P., Pomroy, A. J. (1986). Seasonal production of photosynthetic picoplankton and nanoplankton in the Celtic Sea. Mar. Ecol. Prog. Ser. 28: 251–258
Joint, I. R., Pomroy, A. J. (1983). Production of picoplankton and small nanoplankton in the Celtic Sea. Mar. Biol. 77: 19–27
Joint, I. R., Pomroy, A. J. (1986). Photosynthetic characteristics of nanoplankton and picoplankton from the surface mized layer. Mar. Biol. 92: 465–474
Laws, E. A., Redalje, D. G., Haas, L. W., et al. (1984). High phytoplankton growth and production rates in oligotrophic Hawaiian coastal waters. Limnol. Oceanogr. 29: 1161–1169
Li, W. K., Subba Rao, D. V., Harrison, W. G., Smith, J. C., Cullen, J. J., Irwin, B., Platt, T. (1983). Autotrophic picoplankton in the tropical ocean. Science, N.Y. 219: 292–295
Lorenzen, C. J., Welschmeyer, N. A., Copping, A. E. (1983). Particulate organic carbon flux in the subarctic Pacific. Deep-Sea Res. 30: 639–643
McAllister, C. D., Parsons, T. R., Strickland, J. D. H. (1960). Primary productivity at Station “P” in the north-east Pacific Ocean. J. Cons. perm.int. Explor. Mer 25: 240–259
Miller, C. B., Denman, K. L., Gargett, A. E., Mackas, D. L., Wheeler, P., Booth, B. C., Frost, B. W., Landry, M. R., Lewin, J., Lorenzen, C. J., Perry, M. J., Dagg, M., Welschmeyer, N. (In press). Lower trophic level production dynamics in the oceanic subarctic Pacific Ocean. Bull. Ocean Res. Inst. Univ. Tokyo
Morris, I., Glover, H. (1981). Physiology of photosynthesis by marine coccoid cyanobacteria — some ecological implications. Limnol. Oceanogr. 26: 957–961
Platt, T., Subba Rao, D. V., Irwin, B. (1983). Photosynthesis of picoplankton in the oligotrophic ocean. Nature, Lond. 301: 702–704
Redalje, D. G. (1983). Phytoplankton carbon biomass and specific growth rates determined with the labeled chlorophyll a technique. Mar. Ecol. Prog. Ser 11: 217–225
Redalje, D. G., Laws, E. A. (1981). A new method for estimating phytoplankton growth rates and carbon biomass. Mar. Biol. 62: 73–79
Ryther, J. H., Menzel, D. W. (1965). On the production, composition and distribution of organic matter in the Western Arabian Sea. Deep-Sea Res. 12: 199–209
Saino, T., Hattori, A. (1977). Estimate of the growth rate of phytoplankton in the surface waters of the Bering Sea and the northern north Pacific. Mar. Sci. Communs 3: 1–19
Sheldon, R. W., Sutcliffe, W. H. (1978). Generation times of 3 hours for Sargasso Sea microplankton determined by ATP analysis. Limnol. Oceanogr. 23: 1051–1055
Smayda, T. J. (1973). The growth of Skeletonema costatum during the winter-spring bloom in Narragansett Bay, R. I. Norw. J. Bot. 20: 219–247
Smayda, T. J. (1975). Phased cell division in natural populations of the marine diatom Ditylum briightwelli and the potential significance of diel phytoplankton behavior in the sea. Deep-Sea Res. 22: 151–165
Strathmann, R. R. (1967). Estimating the organic carbon content of phytoplankton from cell volume of plasma volume. Limnol. Oceanogr. 12: 411–418
Strickland, J. D. H., Holm-Hansen, O., Eppley, R. W., Linn, R. J. (1969). The use of a deep tank in plankton ecology. I. Studies of the growth and composition of phytoplankton crops at low nutrient levels. Limnol. Oceanogr. 14: 23–24
Swift, E., Durbin, E. G. (1972). The phased division and cytological characteristics of Pyrocystis spp. can be used to estimate doubling times of their populations in the sea. Deep-Sea Res. 19: 189–198
Tabata, S., Paert, J. L. (1985). Statistics of oceanographic data based on hydrographic/STD casts made at Ocean Station P during August 1956 through June 1981. Can. Data Rep. Hydrogr. Ocean Sciences 31: 1–133
Utermöhl, H. (1931). Neue Wege in der quantitativen Erfassung des Planktons (mit besonderer Berücksichtigung des Ultraplanktons). Verh. int. Verein. theor. angew. Limnol. 5: 567–596
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Communicated by P. C. Schroeder, Pullman
Contribution No. 1695 of the School of Oceanography, University of Washington, Seattle, Washington 98195, USA
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Booth, B.C., Lewin, J. & Lorenzen, C.J. Spring and summer growth rates of subarctic Pacific phytoplankton assemblages determined from carbon uptake and cell volumes estimated using epifluorescence microscopy. Mar. Biol. 98, 287–298 (1988). https://doi.org/10.1007/BF00391207
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DOI: https://doi.org/10.1007/BF00391207