Titlebook: Novel Phytoplankton Blooms; Causes and Impacts o Elizabeth M. Cosper,V. M. Bricelj,E. J. Carpenter Conference proceedings 1989 Springer-Ver

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978-3-642-75282-7Springer-Verlag Berlin Heidelberg 1989

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Novel Phytoplankton Blooms978-3-642-75280-3Series ISSN 0724-5890

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https://doi.org/10.1007/978-3-642-75280-3biomonitoring; ecology; environment; environmental management; growth; nutrition; photosynthesis; phytoplan

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Autotrophic Picoplankton in Narragansett Bay and Their Interaction with Microplanktongen, 1985] are present in northeastern U.S. coastal waters continually at 10.–10./L depending on season, with cyanobacteria (primarily .) and eucaryotic algae at typical concentrations of 10.–10. and 10.–10./L respectively (Carpenter and Campbell, 1988; Glover .., 1985; Johnson and Sieburth, 1979, 1

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Photosynthetic Pigment Composition of the Brown Tide Alga: Unique Chlorophyll and Carotenoid Derivatrvation properties. As an alternative, plant pigments are frequently used a diagnostic markers for distinguishing the various classes of eukaryotic ultraplankton found in natural waters. Chlorophyll . is found in all phototrophic groups, and the presence or absence of the major accessory chlorophyll

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Absorption and Fluorescent Characteristics of the Brown Tide Chrysophyte Its Role on Light Reductionwhere toxic substances produced by the alga detrimently affect the other species growth or aspects of metabolism of other species. The other is where the sheer magnitude of the bloom changes environmental conditions which leads to the demise of other species.

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Lipid Composition and Nutritional Value of the Brown Tide Alga ,densities on the order of 10. l. (Cosper .., 1987; Sieburth .., 1988). This species has not been previously described nor has its biochemical composition been determined. Biochemical analysis, particularly of this cell’s lipid components, is important for understanding its nutritional value for mari

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Dimethylsulfide Production and Marine Phytoplankton: An Additional Impact of Unusual Bloomsdreae, 1986; Bates .., 1987a). This has important implications both in the occurrence of acid precipitation (Charlson and Rodhe, 1982) and cloud formation (Bates .., 1987b; Charlson .., 1987). When combined with terrestrial biogenic sulfur output, this amount equals or exceeds that of anthropogenic