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  • Other Sources  (16)
  • Elsevier  (16)
  • 2020-2022
  • 1995-1999
  • 1985-1989  (16)
  • 1980-1984
  • 1940-1944
  • 1986  (16)
Collection
Source
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  • 2020-2022
  • 1995-1999
  • 1985-1989  (16)
  • 1980-1984
  • 1940-1944
Year
  • 1
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    Fundamentals of Well-log Interpretation - 2. The Interpretation of Logging Data (1986)
    Elsevier
    In:  Amsterdam, Elsevier, vol. Developments in Petroleum Science vol. 15B, no. Publ. No. 12, pp. 9, (ISBN: 0-12-636380-3)
    Details
    Publication Date: 1986
    Keywords: Borehole geophys. ; Textbook of geophysics ; Tectonics ; Geol. aspects ; GFZ ; RUB ; GMG ; 3.45.8 ; UniL ; IfGuG ; in ; Französisch
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Regularities in the pattern of major fault zones of the earth and the origin of arcs (1986)
    Elsevier
    In:  Bull., Open-File Rept., The Origin of Arcs, Amsterdam, Elsevier, vol. 65, no. 1, pp. 63-78, (ISBN 0080419208)
    Details
    Publication Date: 1986
    Keywords: Tectonics ; Geol. aspects ; Fault zone ; Plate tectonics
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Continuum Theories in Solid Earth Physics (1986)
    Elsevier
    In:  Amsterdam, 566+XIII pp., Elsevier, vol. 65, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 95-104, (ISBN: 0-08-044051-7)
    Details
    Publication Date: 1986
    Keywords: Elasticity theory of dislocations ; Textbook of geophysics ; Dislocation
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Variational Methods in Geoscience (1986)
    Elsevier
    In:  Amsterdam, Elsevier, vol. 20, no. Publ. No. 12, pp. 23-40, (ISBN 3935922167)
    Details
    Publication Date: 1986
    Keywords: Textbook of geophysics ; Data analysis / ~ processing ; Elasticity
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    The fractal nature of fracture (1986)
    Elsevier
    In:  Bull., Polar Proj. OP-O3A4, Fractals in Physics, Amsterdam, Elsevier, vol. 24, no. 4, pp. 177-180, (ISBN 0080419208)
    Details
    Publication Date: 1986
    Keywords: Fracture ; FractureT
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    Evidence of a deep-reaching lithospheric root under the Alpine arc (1986)
    Elsevier
    In:  Bull., Polar Proj. OP-O3A4, The Origin of Arcs, Amsterdam, Elsevier, vol. 13, no. Subvol. a, pp. 93-113, (ISBN 0080419208)
    Details
    Publication Date: 1986
    Keywords: CRUST ; earth mantle ; Plate tectonics ; Muller
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    BIBLIOGRAPHY SEISMOLOGY
  • 7
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    Dislocations and their geophysical application (1986)
    Elsevier
    In:  Bull., Open-File Rept., Continuum Theories in Solid Earth Physics, Amsterdam, 566+XIII pp., Elsevier, vol. 186, no. 16, pp. 18-186, (ISBN 0080419208)
    Details
    Publication Date: 1986
    Keywords: Elasticity theory of dislocations ; Dislocation ; Review article
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    BIBLIOGRAPHY SEISMOLOGY
  • 8
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    Stimulated current emission in the Earth: Piezostimulated currents and related geophysical aspects (1986)
    Elsevier
    In:  Professional Paper, Open-File Rept., Thermodynamics of Point Defects and the Relation with Bulk Properties, New York, Elsevier, vol. 1, no. 16, pp. 410-412, 417-420, (ISBN 0080419208)
    Details
    Publication Date: 1986
    Keywords: Geomagnetics ; Earthquake precursor: prediction research ; Earthquake precursor: magnetic ; Geoelectrics ; Physical properties of rocks
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    BIBLIOGRAPHY SEISMOLOGY
  • 9
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    Comparative toxicity of nitrite to freshwater fishes (1986)
    Elsevier
    In:  Aquatic Toxicology, 8 . pp. 129-137.
    Details
    Publication Date: 2015-06-24
    Description: The primary purpose of this study was to determine the toxicity of nitrite to several species of freshwater fishes and to investigate the underlying physiological mechanisms which account for differential toxicity among species. Green sunfish (Lepornis cyanellus) was the most resistant species studied while the channel catfish (Ictaluruspunctatus) was the least resistant. Ninety-six hour median lethal concentrations correlated significantly with both the percentage of hemoglobin in the methemoglobin form and plasma nitrite concentrations among species. Plasma nitrite levels also correlated significantly with percent methemoglobin. Environmental chloride did not increase the tolerance of largemouth bass (Micropterus salmoides) to nitrite toxicity as it did for channel catfish. These results indicate that plasma nitrite concentrations are the primary determinant of the toxicity of nitrite to fishes. Further, plasma nitrite concentrations in various species depend on the discriminatory ability of the active transport system in fish gills which ordinarily transports chloride ions.
    Type: Article , PeerReviewed
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  • 10
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    Survival strategies of microorganisms in extreme saline environments (1986)
    Elsevier
    In:  Advances in Space Research, 6 (12). pp. 299-306.
    Details
    Publication Date: 2016-01-22
    Description: Halophilic representatives are found in all main lines of evolutionary descendence of microbes: in archaebacteria, Gram-negative and Gram-positive eubacteria, and also in eucaryotes. In principe all halophilic microorganisms have to adapt their surface and membrane structures to their highly ionic environments. Concerning their intracellular compartment two different strategies have been developed: Inorganic ions are largely excluded in some microorganisms while such ions are actively accumulated in others. In particular the second group of organisms has to adapt the whole metabolic machinery to the highly ionic conditions of several molar salts, whereas in the first group only the outer surface of the cytoplasmic membrane and the extracytoplasmic structures are in contact with high concentrations of inorganic ions. In this latter group, a variety of organic solutes is accumulated in response to increases of the salinity of the environment.
    Type: Article , PeerReviewed
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  • 11
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    Oxygen isotope constraints on surface ocean temperatures (1986)
    Elsevier
    In:  Quaternary Research, 26 (1). pp. 121-134.
    Details
    Publication Date: 2016-06-16
    Description: Published oxygen isotope results from benthic and planktonic foraminifera are used to constrain the extent to which surface ocean temperatures in the tropics changed between glacial and interglacial time. The possible impacts of bioturbation and of the redistribution of 18O16O ratios within the sea, putting aside the oxygen isotope results, are consistent with the CLIMAP project conclusion that tropical ocean temperatures remained within ±2°C of their present value.
    Type: Article , PeerReviewed
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  • 12
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    The holstein interglaciation: Time-stratigraphic position and correlation to stable-isotope stratigraphy of deep-sea sediments (1986)
    Elsevier
    In:  Quaternary Research, 26 (3). pp. 283-298.
    Details
    Publication Date: 2016-09-02
    Description: Marine molluscan shells from para-type and other loclities of the Holsteinian interglaciation were dated by ThU and the electron spin resonance (ESR) method to more than 350,000 and 370,000 yr B.P., beyond the limit of ThU dating. The high age estimate is corroborated by a KAr age of 420,000 yr B.P. determined from volcanic ash near the base of the Ariendorf paleosol in the Middle Rhine valley believed to be a pedostratigraphic equivalent of the Holsteinian. Shells from the Herzeele marine unit III, an equivalent of the Wacken (Dömnitz) warm stage in northern France and subsequent to the Holsteinian, revealed ages between 300,000 and 350,000 yr B.P. A correlation of these two warm stages with marine oxygen-isotope stages 11 and 9 on the SPECMAP and CARTUNE time scales is suggested. From the benthic oxygen-isotope record one may infer that no exceptionally high global sea-level rise corresponds to the large transgressions of the Holstein Sea in northern Germany. Therefore, a significant proportion of the transgression was probably the result of an unusually large local glacial-isostatic depression caused by the extreme buildup of ice during the preceding Elster glaciation (stage 12). According to the deep-sea record, it lasted approximately 50% longer than the subsequent cold stage 10. The outstanding soil formation with Braunlehm and the well-developed thermal optimum of the Holsteinian are tentatively related to a phase of minimum sea-ice cover in the Norwegian-Greenland Sea, as deduced from long benthic carbon-isotope records from the central Atlantic.
    Type: Article , PeerReviewed
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  • 13
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    Dissolution of biogenic carbonates: Effects of skeletal structure (1986)
    Elsevier
    In:  Marine Geology, 71 (3-4). pp. 341-362.
    Details
    Publication Date: 2016-06-23
    Description: Dissolution of biogenic shallow-water carbonates exposed on deep-sea moorings indicates that skeletal structure is important for the rate of disintegration of biogenic carbonates, besides mineralogy and grain size of particles. The aragonites and high Mg-calcites used represent a wide spectrum of mineralogies and types of skeletal framework. The particles were deployed at different water depths on a mooring in the Drake Passage for 52 days. Weight loss curves for the various types of particles show the relative importance of the different structural factors for the disintegration of these biogenic carbonates. Organic coatings, intraskeletal pore spaces, and sizes and shapes of individual crystallites in the skeletons may be more important than carbonate mineralogy and particle size in cases. The presence of internal sediments, cement aggregates and natural contaminations and of diatoms incorporated during growth into carbonate skeletons, strongly influence the disintegration of the skeletal materials. The first step of particle disintegration is the selective removal of impurities. This step is analogous to a “cleaning” of specimens. It is succeeded by initial dissolution, by strong dissolution and finally by disintegration.
    Type: Article , PeerReviewed
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  • 14
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    On the influence of frictional parameterization in wind-driven ocean circulation models (1986)
    Elsevier
    In:  Dynamics of Atmospheres and Oceans, 10 (1). pp. 63-92.
    Details
    Publication Date: 2018-01-24
    Description: In a series of numerical experiments the wind-driven ocean circulation is studied in an idealized, rectangular model ocean, which is forced by steady zonal winds and damped by lateral and/or bottom friction. The problem as described by the barotropic vorticity equation is characterized by a Rossby number (R) and horizontal and/or vertical Ekman numbers (EL, EB) only. With free-slip conditions at the boundaries steady solutions for all chosen values of R are obtained, provided the diffusivity is sufficiently large. For both the forms of frictional parameterization a northern boundary current emerges with an eastward penetration scale depending on R. The recirculation pattern in the oceanically relevant ‘intermediate’ range of R is strongly affected by the type of friction. If lateral diffusion dominates bottom friction, a strong recirculating sub-gyre emerges in the northwestern corner of the basin. Its shape resembles the vertically integrated transport fields in recent eddy resolving model (EGCM) studies. The maximum transport is increased to values several times larger than the Sverdrup transport. The increase in transport is coupled with a development of closed contours of potential vorticity, enabling a nearly free inertial flow. This behaviour provides a sharp contrast to the bottom friction case (Veronis) where inertial recirculation only takes place with values of R so large that the eastward jet reaches the eastern boundary. It is shown that the linear friction law puts a strong constraint on the flow by preventing an intense recirculation in a small part of the basin. A reduction of the diffusivity (EL) in the lateral friction case leads to quasi-steady solutions. The interaction with eddies becomes an integral part of the time mean energetics but does not influence the recirculation character of the flow. The main conclusion of the study is that the horizontal structure of the EGCM-transport fields can be explained in terms of a steady barotropic model where lateral friction represents the dominant dissipation mechanism
    Type: Article , PeerReviewed
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  • 15
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    Responses to water-borne chemicals by the octopus Eledone cirrhosa (Lamarck, 1798) (1986)
    Elsevier
    In:  Journal of Experimental Marine Biology and Ecology, 104 . pp. 23-30.
    Details
    Publication Date: 2021-01-19
    Description: The octopus Eledone cirrhosa (Lamarck 1798), enclosed in a small chamber of flowing sea water, was tested for responses to water-borne chemicals. Incidence of body movements and change in ventilation rate were recorded by a non-invasive technique- At concentrations no more than 1x10 -4M at the animal, the octopuses responded to betaine, proline, alanine, lactic acid, and serine (order of decreasing sensitivity)- Glutamic acid and trimethylamine oxide were considerably less stimulatory, arginine and taurine were hardly more effective than sea-water controls.
    Type: Article , PeerReviewed
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  • 16
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    Methane oxidation in sediment and water column environments - Isotope evidence (1986)
    Elsevier
    In:  Organic Geochemistry, 10 (4-6). pp. 759-768.
    Details
    Publication Date: 2018-09-04
    Description: Microbial anaerobic oxidation of methane in sediments is a kinetic process associated with a carbon isotope effect which enriches the remaining methane in 13C. Three, models: % residual methane, higher hydrocarbon enrichment, and CO2-CH4 coexisting pairs are used to independently calculate fractionation factors (αc) in the range of 1.002–1.014, which overlap the range determined by culture studies, αc is smaller than that associated with methanogenesis by CO2 reduction or by acetate-type fermentation, and comparison of the coexisting CO2-CH4 pairs can distinguish between the formation and consumption processes. Methane oxidation in sediments continues to a threshold concentration of ca. 0.2 mM; the residual methane is either unavailable or unattractive to consumption. Minor amounts of methane may also be produced simultaneously in the methane consumption zone, influencing the apparent fractionation factor in this zone.
    Type: Article , PeerReviewed
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