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  • Other Sources  (28)
  • Institut für Meereskunde  (15)
  • Springer  (13)
  • 1985-1989  (17)
  • 1980-1984  (11)
  • 1920-1924
  • 1
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    Isopycnic potential vorticity atlas of the North Atlantic Ocean - monthly mean maps - (1987)
    Institut für Meereskunde
    In:  Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 165 . Institut für Meereskunde, Kiel, Germany, 108 pp.
    Details
    Publication Date: 2013-10-16
    Type: Report , NonPeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 2
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    Sediment acoustics (1989)
    Springer
    In:  Bull., Open-File Rept., Lecture Notes in Earth Sciences, Berlin, Springer, vol. 89, no. 1, pp. Paper A 25 - A 34, (ISBN 1-86239-165-3, vi + 330 pp.)
    Details
    Publication Date: 1989
    Keywords: Seismics (controlled source seismology) ; Textbook of geophysics ; Acoustics
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Finite Differenzen und Elemente. Numerische Lösungen von Variationsproblemen und partiellen Differentialgleichungen (1989)
    Springer
    In:  Berlin, Springer, vol. 20, no. 1, pp. 662-664, (ISBN 1-58488-320-0)
    Details
    Publication Date: 1989
    Keywords: Handbook of mathematics ; Finite Element Method ; Finite difference method ; DGL
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Pattern recognition for earthquake detection by mental pictures (1987)
    Springer
    In:  Bull., Polar Proj. OP-O3A4, ASST'87, Berlin, Springer, vol. 81A, no. 16, pp. 347-350, (ISBN: 3-540-23712-7)
    Details
    Publication Date: 1987
    Keywords: Detectors ; Seismology ; Pattern recognition
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Molecular association of Cu, Zn, Cd and 210Po in the digestive gland of the squid Nototodarus gouldi (1987)
    Springer
    In:  Marine Biology, 95 (1). pp. 87-91.
    Details
    Publication Date: 2017-03-29
    Description: The squid Nototodarus gouldi (McCoy, 1888) was caught by bottom trawl in Port Phillip Bay, Australia in February 1985. The squid accumulates in its digestive gland high levels of trace metals, with up to 100 μg Cd g-1 dry tissue, 1 200 μg g-1 copper and 1 500 μg g-1 zinc and up to 24 Bq g-1 of the naturally occurring radionuclide polonium-210. The molecular binding of these elements in six squid was investigated using column chromatography. Two poorly resolved copper peaks were associated with proteins of average molecular weights of 11 500 and 18 000. The two squid containing the highest levels of cadmium in their digestive glands (44 and 88 μg g-1) had cadmium associated with a peak of molecular weight intermediate between the copper-binding peaks, but this peak was absent from squid containing lower levels of cadmium. Zinc was associated with ligands of less than 1 500 molecular weight. The 210Po eluted with proteins of greater than 70 000 molecular weight, and there was no evidence of binding to low molecular weight proteins. Different mechanisms appear to be involved in the binding and control of the four elements.
    Type: Article , PeerReviewed
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  • 6
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    Geophysical prospecting on the Santorini Islands (1984)
    Springer
    In:  Bulletin of Volcanology, 47 (3). pp. 447-466.
    Details
    Publication Date: 2017-05-05
    Description: A program of geophysical research was carried out as a preliminary stage of study of the Santorini volcanic group. This area is of remarkable geothermal and volcanological interest, and the definition of a volcanological structural model is the starting point for an understanding of the local geodynamic processes. Gravity, magnetic and geoelectrical data proved that: (i) the core of the volcanic edifice consists of a sedimentary-metamorphic basement; (ii) the basement is tectonically disturbed and a linear tectonic system produces a graben-type structure in the middle part of the area.
    Type: Article , PeerReviewed
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  • 7
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    Surface-film microbial populations: diel amino acid metabolism, carbon utilization, and growth rates (1986)
    Springer
    In:  Marine Biology, 92 (2). pp. 289-297.
    Details
    Publication Date: 2020-07-14
    Description: Microheterotrophic dissolved free amino acid (DFAA) utilization, and microbial community and bacterial community carbon production and growth were studied using 3H-labeled organics as tracers in marine surface-film and subsurface (10 cm) waters off Baja California in November 1983. DFAA utilization was generally more rapid during the day (0.14 to 0.38 nM h-1) than at night (0.04 to 0.14 nM h-1) in surface-film and subsurface waters, but the percent of utilized amino acid which was respired was always greater during the night (22 to 57%) compared to the day (14 to 18%). Utilization of DFAA-carbon was estimated to range from 0.3 to 5.3 μg C l-1 d-1 for all stations studied. In six of the 8 samples examined, the percentage of microbial carbon accounted for by the bacterial component of the population (1.4 to 5.9%) was strikingly similar to the percentage of microbial carbon production accounted for by bacterial carbon production (1.9 to 5.1%). In all of these six samples, total microbial specific-growth rates and bacterial specific-growth rates were approximately equivalent (0.9 to 2.2 d-1 for the microbial community; 0.7 to 1.9 d-1 for bacteria). The two exceptions were samples apparently influenced by transient flagellate populations migrating into the surface or subsurface waters at night. These observations support the conclusion that surface films contain unique and highly active microbial populations.
    Type: Article , PeerReviewed
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  • 8
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    Eruption ages and magma supply rates during the Miocene evolution of Gran Canaria: Single-crystle 40Ar/39Ar laser ages (1988)
    Springer
    In:  Naturwissenschaften, 75 . pp. 616-617.
    Details
    Publication Date: 2020-03-18
    Type: Article , PeerReviewed
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  • 9
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    Foraminifera as sea-level indicators (1986)
    Springer
    In:  In: Sea-Level Research : a manual for the collection and evaluation of data. , ed. by Plassche, O. Springer, Dordrecht, pp. 435-456.
    Details
    Publication Date: 2016-01-11
    Description: There are over 1000 foraminiferal species presently living in marine environments, but relatively few of these can be used as direct indicators of sea level. We detail here certain assemblages occupying marsh environments that can be used for that purpose. Marsh foraminiferal assemblages have been shown to occur worldwide within narrowly defined vertical zones some of which extend less than 10 cm in total vertical range. These assemblage zones, once known, can be relocated in paleo-marsh deposits and accurately related to paleo-sea level. The key to success of these organisms as sea-level indicators is that their primary controlling factor appears to be elevation above mean sea level. Other foraminiferal assemblages are controlled by a series of parameters (eg. salinity, temperature, dissolved O2, etc.) which often have no direct relationship with actual water depth. Under appropriate circumstances, some information concerning sea level can be derived from other foraminiferal assemblages using indirect means. For instance areas which have undergone substantial emergence often contain small basins which, prior to emergence, were marine. The marine sediments at the bottom can be identified using foraminifera and the sill elevation of the basin can then be related to some prior sea-level stand. Both these methods have imperfections, but in areas where both emergence and submergence have taken place they can be combined to obtain a relatively complete sea-level history.
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 10
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    POSEIDON Reise 72 [POS72] Fahrtbericht (1981)
    Institut für Meereskunde
    In:  Institut für Meereskunde , Kiel, 20 pp.
    Details
    Publication Date: 2015-07-20
    Description: Die 72. Reise der FS Poseidon fand zwischen dem 9. und 13. März 1981 im Skagerrak statt.
    Type: Report , NonPeerReviewed
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