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  • 1
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    Continuum Mechanics: 3. Foundations of Elasticity Theory (1987)
    Gordon and Breach Sc. Publ.
    In:  New York, Gordon and Breach Sc. Publ., vol. 10, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 329, (ISBN 3-7643-6653-2)
    Details
    Publication Date: 1987
    Keywords: Textbook of physics ; Elasticity
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Continuum Mechanics: 4. Problems of Non-Linear Elasticity (1987)
    Gordon and Breach Sc. Publ.
    In:  New York, Gordon and Breach Sc. Publ., vol. 10, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 329, (ISBN 3-7643-6653-2)
    Details
    Publication Date: 1987
    Keywords: Textbook of physics ; Elasticity ; Non-linear effects
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Continuum Mechanics: 2. The Rational Mechanics of Materials (1987)
    Gordon and Breach Sc. Publ.
    In:  New York, Gordon and Breach Sc. Publ., vol. 10, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 329, (ISBN 3-7643-6653-2)
    Details
    Publication Date: 1987
    Keywords: Textbook of physics ; Elasticity
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Cyclonic cold-core eddy in the eastern North Atlantic. II. Nutients, phytoplankton and bacteriaplankton (1987)
    Inter Research
    In:  Marine Ecology Progress Series, 39 . pp. 153-167.
    Details
    Publication Date: 2018-05-04
    Description: A cyclonic cold-core eddy in the Northeast Atlantic of about 100 km in diameter at the sea surface was investigated in May 1985, approximately 3 wk after it had separated from the Polar Front. A strong thermocline, which was shallower but more pronounced than in the ambient water, separated a warm surface layer within the eddy from deeper cold water, while horizontal salinity gradients marked the boundary to the ambient water. The cold-core eddy could be distinguished from amblent Northeast Atlantic water in terms of its nutrient chemistry, phytoplankton species distribution and abundance, bacterial numbers and cell size. The surface layer of the eddy was distinct from deeper eddy water, and was characterized by high concentrations of chlorophyll a, total phytoplankton biomass, dinoflagellates and bacteria. At the eddy's margin diatoms were predominant. It is argued that the physical isolation of the eddy surface layer due to the formation of a shallow thermocline led to rapid utilisation of nutrients. This probably enabled the development of a dinoflagellate-dominated phytoplankton population and of organisms capable of heterotrophic regenerative processes.
    Type: Article , PeerReviewed
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    PAPER (OCEANREP)
  • 5
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    Compartmental models of nitrogen cycling in tropical and temperate marine environments (1987)
    Inter Research
    In:  Marine Ecology Progress Series, 38 . pp. 137-149.
    Details
    Publication Date: 2018-05-04
    Description: Time-course measurements of 15N tracer kinetics in particulate organic and in N+4 pools from tropical and temperate regions were used to test several compartmental models describing the exchange of I5N tracer in microplankton communities. Several lines of evidence suggested the involvement of a third, dissolved pool, arbitrarily labelled dissolved organic nitrogen (DON). Although the kinetic patterns of tracer movement were different between the tropical statlons and the temperate one, the same 3-compartmental model in which PON and DON can exchange material only through the intermediate of NH: gave the best fit. Only the transfer coefficients were modified. Results show that compartmental analysis is useful for the estimation of compartmental transfer rates and for testing the assumptions implicit in any given model.
    Type: Article , PeerReviewed
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  • 6
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    Giant protistan parasites on the gills of cephalopods (Mollusca) (1987)
    Inter Research
    In:  Diseases of Aquatic Organisms, 3 . pp. 119-125.
    Details
    Publication Date: 2021-06-21
    Description: Large Protista of unknown taxonomic affinities are described from 3 species of coleoid squids, and are reported from many other species of cephalopods. The white to yellow-orange, ovoid cyst-like parasites are partially embedded within small pockets on the surface of the gills, often in large numbers. Except for a holdfast region on one side of the large end, the surface of the parasite is elaborated into low triangular plates separated by grooves. The parasites are uninucleate; their cytoplasm bears lipid droplets and presumed paraglycogen granules. Trichocysts, present in a layer beneath the cytoplasmic surface, were found by transmission electron microscopy to be of the dinoflagellate type. Further studies are needed to clarify the taxonomic position of these protists.
    Type: Article , PeerReviewed
    Format: text
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