Skip to main content
Log in

Significance of nanoplankton in the Chesapeake Bay estuary and problems associated with the measurement of nanoplankton productivity

  • Published:
Marine Biology Aims and scope Submit manuscript

Abstract

Over a 2-year program of monthly cruises covering the entire Chesapeake Bay (USA), the phytoplankters which passed 35 μm mesh were responsible for 89.6% of the phytoplankton productivity. On a single summer cruise, the <35 μm phytoplankton fraction was responsible for 93.4% of the chlorophyll a and 100% of the primary productivity. The <10 μm fraction was responsible for 81.3% of the chlorophyll a and 94% of the productivity. The difference in biomass in the <35 μm and the <10 μm fractions was significant (P=0.025), but no significant difference in the productivity could be demonstrated. Laboratory experiments demonstrated that recently assimilated carbon can be lost with gravity screening. Considering both this and the effect of herbivorous zooplankters enclosed in productivity incubations, a prescreening rather than postscreening technique is recommended for studying nanoplankton productivity.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

Literature Cited

  • Anderson, G. C.: Fractionation of phytoplankton communities off the Washington and Oregon coasts. Limnol. Oceanogr. 10, 477–480 (1965).

    Google Scholar 

  • Carpenter, J. H.: The Chesapeake Bay Institute technique for the Winkler dissolved oxygen method. Limnol. Oceanogr. 10, 141–143 (1965).

    Google Scholar 

  • —, D. W. Pritchard and R. C. Whaley: Observations of eutrophication and nutrient cycles in some coastal plain estuaries. In: Eutrophication: causes, consequences, correctives, pp 210–221. Washington: National Academy of Sciences 1969.

    Google Scholar 

  • Cowles, R. P.: A biological study of the offshore waters of Chesapeake Bay. Bull. Bur. Fish., Wash. 46, 277–381 (1930).

    Google Scholar 

  • Eppley, R. W.: Temperature and phytoplankton growth in the sea. Fish. Bull. U.S. 70, 1068–1085 (1972).

    Google Scholar 

  • Findenegg, I.: Relationship between standing crop and primary productivity. In: Primary productivity in aquatic environments, pp 271–289. Ed. by C. R. Goldman. Berkeley: University of California Press 1965.

    Google Scholar 

  • Flemer, D. A.: Primary production in the Chesapeake Bay. Chesapeake Sci. 11, 117–129 (1970).

    Google Scholar 

  • — and J. Olmon: Daylight incubator estimates of primary production in the mouth of the Patuxent River, Maryland. Chesapeake Sci. 12, 105–110 (1971).

    Google Scholar 

  • Gelin, C.: Primary production and chlorophyll a content of nanoplankton in a eutrophic lake. Oikos 22, 230–234 (1971).

    Google Scholar 

  • Gilmartin, M.: The primary production of a British Columbia fjord. J. Fish. Res. Bd Can. 21, 505–538 (1964).

    Google Scholar 

  • Holmes, R. W.: Surface chlorophyll-a, surface primary production, and zooplankton volumes in the Eastern Pacific Ocean. Rapp. P.-v. Réun. Cons. perm. int. Explor. Mer 144, 109–116 (1958).

    Google Scholar 

  • — and G. C. Anderson: Size fractionation of C14 labeled natural phytoplankton communities. In: Symposium on marine microbiology, pp 241–250. Ed. by C. C. Oppenheimer. Springfield: C. C. Thomas 1963.

    Google Scholar 

  • Holm-Hansen, O.: Determination of particulate organic nitrogen. Limnol. Oceanogr. 13, 175–178 (1968).

    Google Scholar 

  • Kalff, J.: Phytoplankton abundance and primary production rates in two arctic ponds. Ecology 48, 558–565 (1967a).

    Google Scholar 

  • —: Phytoplankton dynamics in an aretic lake. J. Fish. Res. Bd Can. 24, 1861–1871 (1967b).

    Google Scholar 

  • —: Netplankton and nanoplankton production and biomass in a north temperate zone lake. Limnol. Oceanogr. 17, 712–720 (1972).

    Google Scholar 

  • Loftus, M. E. and J. H. Carpenter: A fluorometric method for determining chlorophyll a, b, and c. J. mar. Res. 29, 319–338 (1971).

    Google Scholar 

  • —, D. V. Subba Rao and H. H. Seliger: Growth and dissipation of phytoplankton in Chesapeake Bay. I. Response to a large pulse of rainfall. Chesapeake Sci. 13, 282–299 (1972).

    Google Scholar 

  • Lohmann, H.: Neue Untersuchungen über den Reichtum des. Meeres an Plankton und über die Brauchbarkeit der verschiedenen Fangmethoden. Helgoländer wiss. Meeresunters. 7, 1–86 (1903).

    Google Scholar 

  • Malone, T. C.: The relative importance of nanoplankton and netplankton as primary producers in the California Current System. Fish. Bull. U.S. 69, 799–820 (1971a).

    Google Scholar 

  • —: The relative importance of netplankton and nannoplankton as primary producers in neritic and oceanic tropical waters. Limnol. Oceanogr. 16, 633–639 (1971b).

    Google Scholar 

  • —: Diurnal rhythms in netplankton and nannoplankton assimilation ratios. Mar. Biol. 10, 285–289 (1971c).

    Google Scholar 

  • Marshall, H. G.: Diurnal distribution of phytoplankton from a single station at the mouth of the James River. Ohio J. Sci. 66, 253–255 (1966a).

    Google Scholar 

  • —: The distribution of phytoplankton along a 140 mile transect in the Chesapeake Bay. Va J. Sci. 17, 105–119 (1966b).

    Google Scholar 

  • Patten, B. C., R. A. Mulford and J. E. Warinner: An annual phytoplankton cycle in the lower Chesapeake Bay. Chesapeake Sci. 4, 1–20 (1963).

    Google Scholar 

  • Rodhe, W.: The primary production in lakes: some results and restrictions of the C14 method. Rapp. P.-v. Réun Cons. perm. int. Explor. Mer 144, 122–128 (1958).

    Google Scholar 

  • —, R. A. Vollenweider and A. Nauwerck: The primary production and standing crop of phytoplankton. In: Perspectives in marine biology, pp 299–328. Ed. by A. A. Buzzati-Traverso. Berkeley: University of California Press 1958.

    Google Scholar 

  • Saijo, Y. and K. Takesue: Further studies on the size distribution of photosynthesizing phytoplankton in the Indian Ocean. J. oceanogr. Soc. Japan 20, 264–271 (1965).

    Google Scholar 

  • Schiemer, E. W. and D. W. Pritchard: An induction conductivity temperature indicator. Tech. Rep. Chesapeake Bay Inst. 25 (Ref. 61-4), 1–75 (1961).

    Google Scholar 

  • Steemann-Nielsen, E.: The use of radioactive carbon (C14) for measuring organic production in the sea. J. Cons. perm. int. Explor. Mer 18, 117–140 (1952).

    Google Scholar 

  • — and E. A. Jensen: Primary oceanic production. The autotrophic production of organic matter in the ocean. Galathea Rep. 1, 49–136 (1957).

    Google Scholar 

  • Strickland, J. D. H.: Production of organic matter in the primary stages of the marine food chain. In: Chemical oceanography, Vol. 1. pp 477–610. Ed. by J. P. Riley and G. Skirrow. New York: Academic Press 1965.

    Google Scholar 

  • Tate, M. W. and R. C. Clelland: Nonparametric and shortcut statistics in the social, biological, and medical sciences, 171 pp. Danville, Illinois: Interstate 1957.

    Google Scholar 

  • Taylor, W. R.: Inorganic nutrient requirements for marine phytoplankton organisms. Occ. Publs Narragansett mar. Lab., Univ. Rhode Isl. 2, 17–24 (1964).

    Google Scholar 

  • Teixeira, C.: Relative rates of photosynthesis and standing stock of net phytoplankton and nanoplankton. Bolm Inst. Oceanogr., S Paulo 13, 53–60 (1963).

    Google Scholar 

  • Thomas, J. P.: Release of dissolved organic matter from natural populations of marine phytoplankton. Mar. Biol. 11, 311–323 (1971).

    Google Scholar 

  • Watt, W. D.: Measuring the primary production rates of individual phytoplankton species in natural mixed populations. Deep Sea Res. 18, 329–339 (1971).

    Google Scholar 

  • Whaley, R. C., J. H. Carpenter and R. L. Baker: Nutrient data summary 1964, 1965, 1966: Upper Chesapeake Bay (Smith Point to Turkey Point), Potomac, South, Severn, Magothy, Back, Chester, and Miles Rivers, and Eastern Bay. Spec. Rep. Chesapeake Bay Inst. 12 (Ref. 66-4), 1–77 (1966).

    Google Scholar 

  • Williams, P. J. LeB., T. Berman and O. Holm-Hansen: Potential sources of error in the measurement of low rates of planktonic photosynthesis and excretion. Nature New Biol. 236, 91–92 (1972).

    PubMed  Google Scholar 

  • Wolfe, J. J., B. Cunningham, N. F. Wilkerson and J. T. Barnes: An investigation of the microplankton of Chesapeake Bay. J. Elisha Mitchell scient. Soc. 42, 25–54 (1926).

    Google Scholar 

  • Yentsch, C. A. and J. H. Ryther: Relative significance of the net plankton and nannoplankton in the waters of Vineyard Sound. J. Cons. perm. int. Explor. Mer 24, 231–238 (1959).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Additional information

Communicated by J. Bunt, Miami

Rights and permissions

Reprints and permissions

About this article

Cite this article

McCarthy, J.J., Rowland Taylor, W. & Loftus, M.E. Significance of nanoplankton in the Chesapeake Bay estuary and problems associated with the measurement of nanoplankton productivity. Marine Biology 24, 7–16 (1974). https://doi.org/10.1007/BF00402842

Download citation

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00402842

Keywords

Navigation