Abstract
Total labile organic carbon was estimated in the euphotic zone of the Baltic Sea by a method based on the determination of the biological oxygen demand (BOD); the method is extremely simple, requires little sample water, and is quite precise (±4.5 μmol O2/l or ±40.4 μgClab/l). The amount found was 1,150 μgClab/l, or about 29% of the total organic carbon. At 1 m, a relationship between biological activity, as measured by chlorophyll content, and the amount of labile carbon was found: ln Clab (μg/l)=ln 6.87 (μg/l) +0.272 ln chlorophyll (μg/l), with a correlation coefficient of 0.86, which is significantly greater than zero at the 0.001 level.
Similar content being viewed by others
Literature Cited
Anderson, G.C. and R.P. Zeutschel: Release of dissolved organic matter by marine phytoplankton in coastal and offshore areas of the Northeast Pacific Ocean. Limnol. Oceanogr. 15, 402–407 (1970)
Barber, R.T.: Dissolved organic carbon from deep water resists microbial oxidation. Nature, Lond. 220, 274–275 (1968)
Chung, C.J.: Primary production and release of dissolved organic carbon from phytoplankton in the western North Atlantic Ocean. Deep-Sea Res. 19, 731–735 (1972)
Duursma, E.K.: The production of dissolved organic matter in the sea, as related to the primary gross production of organic matter. Neth. J. Sea Res. 2, 85–94 (1963)
Ehrhardt, M.: The particulate organic carbon and nitrogen and the dissolved organic carbon in the Gotland Deep in May 1968. Kieler Meeresforsch. 25, 71–80 (1969)
Fonselius, S.: On biogenic elements and organic matter in the Baltic. Ambio spec. Rep. 1, 29–36 (1972)
Hobson, L.A., D.W. Menzel and R.T. Barber: Primary productivity and sizes of pools of organic carbon in the mixed layer of the ocean. Mar. Biol. 19, 298–306 (1973)
Holm-Hansen, O., J.D.H. Strickland and P.M. Williams: A detailed analysis of biologically important substances in a profile off southern California. Limnol. Oceanogr. 11, 548–561 (1966)
Lorenzen, C.J.: Surface chlorophyll as an index of the depth, chlorophyll content, and primary productivity of the euphotic layer. Limnol. Oceanogr. 15, 479–480 (1970)
Menzel, D.W. and J.H. Ryther: Organic carbon and the oxygen minimum in the South Atlantic Ocean. Deep-Sea Res. 15, 327–337 (1968)
Morris, A.W. and P. Foster: The seasonal variation of dissolved organic carbon in the inshore waters of the Menai Strait in relation to primary production. Limnol. Oceanogr. 16, 987–989 (1971)
Ogura, N.: Dissolved organic carbon in the equitorial region of the Central Pacific. Nature, Lond. 227, 1335–1336 (1970)
—: Rate and extent of decomposition of dissolved organic matter in surface seawater, Mar. Biol. 13, 89–93 (1972)
Rakestraw, N.W.: Oxygen consumption in seawater over long periods. J. mar. Res. 6, 259–263 (1947)
Redfield, A.C., B.H. Ketchum and F.A. Richards: The influence of organisms on the composition sea water. In: The sea, Vol. 2. pp 26–77. Ed. by M.N. Hill, New York: Interscience 1963
Richards, F.A., J.D. Cline, W.W. Broenkow and L.P. Atkinson: Some consequences of the decomposition of organic matter in Lake Nitinat, an anoxic fjord. Limnol. Oceanogr. 10, R185-R201 (1965)
Thomas, J.P.: Release of dissolved organic matter from natural populations of marine phytoplankton. Mar. Biol. 11, 311–323 (1971)
Wallen, D.G. and G.H. Green: The nature of the photosynthate in natural phytoplankton populations in relation to light quality. Mar. Biol. 10, 157–168 (1971)
ZoBell, C.E.: The effect of oxygen tension on the rate of oxidation of organic matter in sea water by bacteria. J. mar. Res. 3, 211–233 (1940)
Zsolnay, A.: Distribution of labile and residual particulate carbon in the Baltic Sea. Mar. Biol. 21, 13–18 (1973)
Author information
Authors and Affiliations
Additional information
Communicated by O. Kinne, Hamburg
Rights and permissions
About this article
Cite this article
Zsolnay, A. Total labile carbon in the euphotic zone of the Baltic Sea as measured by BOD. Mar. Biol. 29, 125–128 (1975). https://doi.org/10.1007/BF00388984
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00388984