Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-05T16:15:27.360Z Has data issue: false hasContentIssue false

Plant production on the Fladen ground

Published online by Cambridge University Press:  11 May 2009

John H. Steele
Affiliation:
The Marine Laboratory, Aberdeen

Extract

The quantitative study of phytoplankton production may be pursued in many ways, but these ways can be divided into two general methods of approach. There is, first, the direct estimation of a production rate for a particular sample of the population; for example, the light-dark bottle technique for measuring oxygen production (Gaarder & Gran, 1927; Riley, 1939) and the new 14C technique (Steeman Nielsen, 1952). These estimates are made under conditions which must be, to some extent, artificial. Secondly, there is the direct estimation of relevant variables in the sea (phosphate, oxygen, chlorophyll concentration, etc.) from which production is calculated on the basis of hypotheses about the behaviour of phytoplankton. These hypotheses are, of necessity, simplifications of a mass of laboratory experiments and of previous field work. Riley, Stommel & Bumpus (1949) give a full account of this approach and of the difficulties involved in it.

Type
Research Article
Copyright
Copyright © Marine Biological Association of the United Kingdom 1956

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Barker, H. A., 1935. Culture and physiology of the marine dinoflagellates. Arch. Mikrobiol., Bd. 6, pp. 157–81.Google Scholar
Braarud, T. & Rossavik, E., 1951. Observations on the marine dinoflagellate Prorocentrum micans Ehrenb. in culture. Avh. norske VidenskAkad. (1, Mat. Kl), No. 1, 18 pp.Google Scholar
Chu, S. P., 1946. Utilization of organic phosphorus by phytoplankton. J. Mar. biol. Ass. U.K., Vol. 26, pp. 285–95.CrossRefGoogle ScholarPubMed
Conseil, Perm. Internat. Pour L'Explor. De La Mer, 1933. Atlas de température et salinité de Veau de surface de la Mer du Nord et de la Manche. 32 pp. Copenhagen: Bureau du Conseil.Google Scholar
Fleming, R. H., 1939. The control of diatom populations by grazing. J. Cons. int. Explor. Mer, Vol. 14, pp. 210–27.Google Scholar
Fraser, J. H., 1954. Zooplankton collections made by Scottish research vessels during 1953. Ann. biol., Copenhague, Vol. 10 (1953), pp. 99101.Google Scholar
Gaarder, T. C. & Gran, H. H., 1927. Investigations of the production of plankton in the Oslo Fjord. Rapp. Cons. Explor. Mer, Vol. 42, 48 pp.Google Scholar
Gauld, D. T. & Raymont, J. E. G., 1953. The respiration of some planktonic cope-pods, II. J. Mar. biol. Ass. U.K., Vol. 31, pp. 447–60.Google Scholar
Gross, F. & Zeuthen, E., 1948. The buoyancy of plankton diatoms: a problem of cell physiology. Proc. roy. Soc. B, Vol. 135, pp. 382–9.Google Scholar
Harvey, H. W., 1950. On the production of living matter in the sea off Plymouth. J. Mar. biol. Ass. U.K., Vol. 29, pp. 97137.Google Scholar
Harvey, H. W., 1953. Note on the absorption of organic phosphorus compounds by Nitzschia closterium in the dark. J. Mar. biol. Ass. U.K., Vol. 31, pp. 475–6.Google Scholar
Johnston, R., 1953. Hydrography. North Sea. Chemical observations. Ann. biol, Copenhague, Vol. 9 (1952), pp. 99103.Google Scholar
Johnston, R., 1954. Hydrography. North Sea. Chemical observations. Ann. biol, Copen-hague, Vol. 10 (1953), pp. 84–6.Google Scholar
Ketchum, B. H., 1939. The development and restoration of deficiencies in the phosphorus and nitrogen composition of unicellular plants. J. cell. comp. Physiol., Vol. 13, pp. 373–81.Google Scholar
Lwoff, A., ed., 1951. Biochemistry and Physiology of Protozoa, Vol. 1, 434 pp. New York: Academic Press.Google Scholar
Nicholls, A. V., 1933. On the biology of Calanus finmarchicus. III. Vertical distribution and diurnal migration in the Clyde sea area. J. Mar. biol. Ass. U.K., Vol. 19, pp. 139–64.Google Scholar
Parr, A. E., 1936. On the probable relationship between vertical stability and lateral mixing processes. J. Cons. int. Explor. Mer, Vol. 11, pp. 308–13.Google Scholar
Rabinowitch, E. I., 1945. Photosynthesis and Related Processes, Vol. 1, 599 pp. New York: Interscience Publishers.Google Scholar
Raymont, J. E. G. & Gauld, D. T., 1951. The respiration of some planktonic cope-pods. J. Mar. biol. Ass. U.K., Vol. 29, pp. 681–93.Google Scholar
Riley, G. A., 1939. Plankton studies. II. The western North Atlantic, May-June 1939. J. Mar. Res., Vol. 2, pp. 145–62.CrossRefGoogle Scholar
Riley, G. A., 1941. Plankton studies. III. Long Island Sound. Bull. Bingham oceanogr. Coll., Vol. 7, Art. 3, 93 pp.Google Scholar
Riley, G. A., 1946. Factors controlling phytoplankton population on Georges Bank. J. Mar. Res., Vol. 6, pp. 5473.Google Scholar
Riley, G. A., 1952. Phytoplankton of Block Island Sound. Bull. Bingham oceanogr. Coll., Vol. 13, Art. 3, pp. 4064.Google Scholar
Riley, G. A., 1953. Theory of growth and competition in natural populations. J. Fish. Res. Bd Can., Vol. 10, pp. 211–23.Google Scholar
Riley, G. A., Stommel, H. & Bumpus, D. F., 1949. Quantitative ecology of the plankton of the western North Atlantic. Bull. Bingham oceanogr. Coll., Vol. 12, Art. 3, 169 pp.Google Scholar
Steeman, E. Nielsen, 1952. The use of radioactive carbon (C14) for measuring organic production in the sea. J. Cons. int. Explor. Mer, Vol. 18, pp. 117–40.Google Scholar
Sverdrup, H. U., Johnston, M. W. & Fleming, R. H., 1942. The Oceans; their Physics, Chemistry and general Biology. 1087 pp. New York: Prentice-Hall.Google Scholar
Tait, J. B., 1937. Surface water drift in the North Sea and Faroe-Shetland Channel. Sci. Invest. Fish. Scot., 1937, No. 1, 60 pp.Google Scholar
Tait, J. B., 1954. Hydrography, North Sea, northern North Sea and approaches. Ann. biol., Copenhague, Vol. 10 (1953), pp. 82–4.Google Scholar