about microzooplankton

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OLR(! 979)26(125 E. Biological Oceanography 799 oceanic Ceratium species divided similarly to laboratory cultures under analogous conditions of photoperiod and temperature. Includes a cell division micrographic sequence. Institute of Oceanography, University of British Columbia, 2075, Wesbrook Mall, Vancouver, B.C., Canada V6T IW5. (mjj) 79:6148 Wilkinson, M. and I. Tittley, 1979. The marine algae of Elie, Scotland: a re-assessment [of Traill's 1888 survey]. Botanica mar., 22(45: 249-256. Includes species lists. Department of Brewing and Biological Sciences, Heriot-Watt University, Edinburgh, Scotland. 4. Chemistry of marine organisms and biochemistry 79:6149 Salonen, Kalevi and Jouko Sarvala, 1977/78. Estima- tion of the inorganic fraction of total carbon in aquatic invertebrates. Proc. int. Ass. theor, appl. Limnol. (Verb. int. Verein. theor. Angew. Lim- nol.), 20(2): 1221-1225. Methods of differentiating the contributions of organic and inorganic carbon to the biomasses of shelled invertebrates are compared. Lammi Biological Station, University of Helsinki, SF-16900 Lammi, Finland. (rio) 79:6150 Velimirov, B., 1979. Fatty acid composition of kelp on the west coast of South Africa and some eco- logical implications. Botanica mar., 22(4): 237-240. Fatty acid patterns, lipid content (0.4%-0.7% fresh weight) and lipid classes were determined in Laminaria pallida, Ecklonia maxima and Macrocystis angustifolia. Contribution of the laminarians to surface slicks and sea foams was assessed by comparing fatty acid patterns in kelps, slicks and foams. Zoology Department, University of Cape Town, 7700 Rondebosch, South Africa. (izs) 79:6151 Wada, Eitaro and Akihiko Hattori, 1978. Nitrogen isotope effects in the assimilation of inorganic nitrogenous compounds by marine diatoms. Geo- microbiol. J., 1(15: 85-101. The isotopic composition (6~SN) of Phaeodactylum tricornutum and Chaetoceros sp. ranged from 7 to --18°/oo. Fractionation ranged from negligible at growth rates higher than l day - 1, to 1.016 at a growth rate of 0.025 day -~. The N isotope fractionation primarily takes place at the step of N-O bond breaking in nitrate reduction to nitrite. Mitsubishi- Kasei Institute of Life Sciences, il Minamiooya, Machida, Tokyo 194, Japan. (mjj) 5. Plankton (zooplankton, phytoplank- ton, nannoplankton, primary produc- tivity, seston and detritus) 79:6152 Beers, J. R., 1978. About microzooplankton. Monogr. oceanogr. Methodol., U.N., 6: 288-296. Microzooplankton are defined and compositionally characterized. Various aspects of their preservation and storage, taxonomic identification, and field and laboratory study are discussed. Institute of Marine Resources A-018, University of California at San Diego, La Jolla, Calif. 92093, U.S.A. (izs) 79:6153 Boalch, G. T., 1979. The dinoflagellate bloom on the coast of south-west England, August-September 1978. J. mar. biol. Ass. U.K., 59(2): 515-517. The Laboratory, Marine Biological Association, Citadel Hill, Plymouth, England. 79:6154 Conte, M. H., R. G. Otto and P. E. Miller, 1979. Short-term variability in surface catches of ichthyoplankton in the upper Chesapeake Bay. Estuar. coast, mar. Sci., 8(6): 511-522. Knowledge of short-term (i.e., hourly) distribution and abundance of ichthyoplankton as affected by biological and water transport factors is essential to design a sampling scheme capable of accurate estimates of mean numbers and true differences in distribution over larger time periods between different locations. The results of this study are discussed in terms of the confidence which can be assigned to the differences noted. Chesapeake Bay Institute, The Johns Hopkins University, Baltimore, Md. 21218, U.S.A. (sir) 79:6155 Demers, Serge and Louis Legendre, 1979. Effets des mar~es sur la variation circadienne de la capacit~ photosynth~tique.du phytoplancton de l'estuaire du Saint-Laurent. [Tidal effects on the circadian photosynthetic capacity of phytoplank- ton in the St. Lawrence Estuary.] J. expl mar. Biol. Ecol., 39(15: 87-99. GIROQ, Dc~partement de Biologic, Universit6 Laval, Quebec, Canada GIK 7P4. 79:6156 Fornshell, J. A., 1979. Microplnoktou patchiness in the northwest Atlantic Ocean. J. Protozool., 26(2): 270-272.

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OLR(! 979)26(125 E. Biological Oceanography 799

oceanic Ceratium species divided similarly to laboratory cultures under analogous conditions of photoperiod and temperature. Includes a cell division micrographic sequence. Institute of Oceanography, University of British Columbia, 2075, Wesbrook Mall, Vancouver, B.C., Canada V6T IW5. (mjj)

79:6148 Wilkinson, M. and I. Tittley, 1979. The marine algae

of Elie, Scotland: a re-assessment [of Traill's 1888 survey]. Botanica mar., 22(45: 249-256. Includes species lists. Department of Brewing and Biological Sciences, Heriot-Watt University, Edinburgh, Scotland.

4. Chemistry of marine organisms and biochemistry

79:6149 Salonen, Kalevi and Jouko Sarvala, 1977/78. Estima-

tion of the inorganic fraction of total carbon in aquatic invertebrates. Proc. int. Ass. theor, appl. Limnol. (Verb. int. Verein. theor. Angew. Lim- nol.), 20(2): 1221-1225.

Methods of differentiating the contributions of organic and inorganic carbon to the biomasses of shelled invertebrates are compared. Lammi Biological Station, University of Helsinki, SF-16900 Lammi, Finland. (rio)

79:6150 Velimirov, B., 1979. Fatty acid composition of kelp

on the west coast of South Africa and some eco- logical implications. Botanica mar., 22(4): 237-240.

Fatty acid patterns, lipid content (0.4%-0.7% fresh weight) and lipid classes were determined in Laminaria pallida, Ecklonia maxima and Macrocystis angustifolia. Contribution of the laminarians to surface slicks and sea foams was assessed by comparing fatty acid patterns in kelps, slicks and foams. Zoology Department, University of Cape Town, 7700 Rondebosch, South Africa. (izs)

79:6151 Wada, Eitaro and Akihiko Hattori, 1978. Nitrogen

isotope effects in the assimilation of inorganic nitrogenous compounds by marine diatoms. Geo- microbiol. J., 1(15: 85-101.

The isotopic composition (6~SN) of Phaeodactylum tricornutum and Chaetoceros sp. ranged from 7 to --18°/oo. Fractionation ranged from negligible at growth rates higher than l day - 1, to 1.016 at a growth rate of 0.025 day -~. The N isotope fractionation primarily takes place at the step of N-O bond breaking in nitrate reduction to nitrite. Mitsubishi-

Kasei Institute of Life Sciences, il Minamiooya, Machida, Tokyo 194, Japan. (mjj)

5. Plankton (zooplankton, phytoplank- ton, nannoplankton, primary produc- tivity, seston and detritus)

79:6152 Beers, J. R., 1978. About microzooplankton. Monogr.

oceanogr. Methodol., U.N., 6: 288-296.

Microzooplankton are defined and compositionally characterized. Various aspects of their preservation and storage, taxonomic identification, and field and laboratory study are discussed. Institute of Marine Resources A-018, University of California at San Diego, La Jolla, Calif. 92093, U.S.A. (izs)

79:6153 Boalch, G. T., 1979. The dinoflagellate bloom on the

coast of south-west England, August-September 1978. J. mar. biol. Ass. U.K., 59(2): 515-517. The Laboratory, Marine Biological Association, Citadel Hill, Plymouth, England.

79:6154 Conte, M. H., R. G. Otto and P. E. Miller, 1979.

Short-term variability in surface catches of ichthyoplankton in the upper Chesapeake Bay. Estuar. coast, mar. Sci., 8(6): 511-522.

Knowledge of short-term (i.e., hourly) distribution and abundance of ichthyoplankton as affected by biological and water transport factors is essential to design a sampling scheme capable of accurate estimates of mean numbers and true differences in distribution over larger time periods between different locations. The results of this study are discussed in terms of the confidence which can be assigned to the differences noted. Chesapeake Bay Institute, The Johns Hopkins University, Baltimore, Md. 21218, U.S.A. (sir)

79:6155 Demers, Serge and Louis Legendre, 1979. Effets des

mar~es sur la variation circadienne de la capacit~ photosynth~tique.du phytoplancton de l'estuaire du Saint-Laurent. [Tidal effects on the circadian photosynthetic capacity of phytoplank- ton in the St. Lawrence Estuary.] J. expl mar. Biol. Ecol., 39(15: 87-99. GIROQ, Dc~partement de Biologic, Universit6 Laval, Quebec, Canada GIK 7P4.

79:6156 Fornshell, J. A., 1979. Microplnoktou patchiness in

the northwest Atlantic Ocean. J. Protozool., 26(2): 270-272.