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  • Weitere Quellen  (2.258)
  • Wiley  (1.986)
  • Oxford Univ. Press  (229)
  • Am. Geophys. Un.
  • Periodicals Archive Online (PAO)
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  • 1
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    Wiley
    In:  Time Series Analysis, Oslo, Wiley, vol. 111, no. B8, pp. 170, pp. B08303, (ISSN: 1340-4202)
    Publikationsdatum: 1963
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  • 2
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    Wiley
    In:  Chichester, Wiley, vol. 231, no. 3, pp. 2-203, (ISBN 0-470-02298-1)
    Publikationsdatum: 1982
    Schlagwort(e): Data analysis / ~ processing ; Correlation ; Seismic stratigraphy ; Seismics (controlled source seismology)
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
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    Unbekannt
    Wiley
    In:  New York, 2nd Edition, 709 pp., Wiley, vol. 75, no. 2, pp. 2-203, (ISBN: 3-7643-7143-9)
    Publikationsdatum: 1981
    Schlagwort(e): Correlation ; Data analysis / ~ processing ; fit ; Textbook of mathematics
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
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    Unbekannt
    Wiley
    In:  Hoboken, NJ, 633 pp., Wiley, vol. 16B, no. 2, pp. 125-169, (ISBN 0-471-26610-8)
    Publikationsdatum: 2003
    Schlagwort(e): Textbook of mathematics ; Data analysis / ~ processing ; Modelling ; software ; manual ; computer ; algebra ; symbolic ; mathematics
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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    Unbekannt
    Am. Geophys. Un.
    In:  Hannover, Am. Geophys. Un., vol. 20, no. XVI:, pp. 1-14, (ISBN: 1-4020-2968-3)
    Publikationsdatum: 1977
    Schlagwort(e): Velocity depth profile ; CRUST ; Velocity depth profile ; Moho ; Geochemistry ; petrology
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Unbekannt
    Oxford Univ. Press
    In:  Oxford, Oxford Univ. Press, vol. 7, no. XVI:, pp. 227-235, (ISBN 3-342-00685-4)
    Publikationsdatum: 1989
    Schlagwort(e): Inelastic ; Textbook of geophysics ; Physical properties of rocks ; Laboratory measurements ; Textbook of physics
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
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    Unbekannt
    Wiley
    In:  New York, Wiley, vol. 7, no. Publ. No. 12, pp. 127, (ISBN 3-540-44363-0)
    Publikationsdatum: 1965
    Schlagwort(e): Friction ; Physical properties of rocks ; Rock mechanics ; Textbook of geophysics
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
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    Unbekannt
    Am. Geophys. Un.
    In:  Malden, MA, Am. Geophys. Un., vol. 24, no. Publ. No. 12, pp. 95-104, (ISBN: 0-08-043930-6)
    Publikationsdatum: 1993
    Schlagwort(e): Geodesy ; GeodesyY ; Plate tectonics ; Textbook of geophysics ; Textbook of geodesy
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
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    Unbekannt
    Am. Geophys. Un.
    In:  Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 16, pp. 77-86, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Reflectivity ; Deep seismic sounding (espec. cont. crust) ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; Review article ; Project report/description ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 16, pp. 87-90, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Reflectivity ; Tectonics ; Deep seismic sounding (espec. cont. crust) ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 11
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, New York, Am. Geophys. Un., vol. 23, no. 16, pp. 1-35, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1980
    Schlagwort(e): Seismicity ; Fault plane solution, focal mechanism ; Subduction zone ; Plate tectonics
    Standort Signatur Erwartet Verfügbarkeit
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  • 12
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 65, no. 16, pp. 243-271, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1981
    Schlagwort(e): Fault plane solution, focal mechanism ; Tectonics ; Plate tectonics ; Seismology
    Standort Signatur Erwartet Verfügbarkeit
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  • 13
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Earthquake Source Mechanics, Washington, D.C., Am. Geophys. Un., vol. 24, no. 16, pp. 37-47, (ISBN 1-4020-1729-4)
    Publikationsdatum: 1986
    Schlagwort(e): Earthquake precursor: prediction research
    Standort Signatur Erwartet Verfügbarkeit
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  • 14
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 1, pp. 97-100, (ISBN: 3-540-23712-7)
    Publikationsdatum: 1991
    Schlagwort(e): AnisotropyS ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; Stress ; cracks and fractures (.NE. fracturing) ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 15
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. Subvol. a, pp. 377-382, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Deep seismic sounding (espec. cont. crust) ; Earth model, also for more shallow analyses ! ; GeodesyY ; Plate tectonics ; Review article ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 16
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    Unbekannt
    Wiley
    In:  New York, Wiley, vol. 20, pp. 559-932, (ISBN 0-935702-96-2)
    Publikationsdatum: 1975
    Schlagwort(e): TBING ; Statistical investigations
    Standort Signatur Erwartet Verfügbarkeit
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  • 17
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    Unbekannt
    Wiley
    In:  New York - 2nd ed., 372 pp., Wiley, vol. 1, pp. 225, (ISBN 0-471-32192-3)
    Publikationsdatum: 1999
    Schlagwort(e): Textbook of geography ; Textbook of informatics ; GIS
    Standort Signatur Erwartet Verfügbarkeit
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  • 18
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    Unbekannt
    Oxford Univ. Press
    In:  Oxford, Oxford Univ. Press, vol. 3, pp. 158, (ISBN 0-444-50968-2)
    Publikationsdatum: 1964
    Schlagwort(e): Textbook of physics ; Friction ; Physical properties of rocks ; Fluids
    Standort Signatur Erwartet Verfügbarkeit
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  • 19
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    Unbekannt
    Wiley
    In:  New York, 571 pp., Wiley, vol. 5, no. XVI:, pp. 1-14, (ISBN 0-89871-521-0)
    Publikationsdatum: 1976
    Schlagwort(e): Structural geology ; Textbook of geology ; Stress ; Geol. aspects ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
    Standort Signatur Erwartet Verfügbarkeit
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  • 20
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    Unbekannt
    Oxford Univ. Press
    In:  Oxford, 3rd Edition, 459 pp., Oxford Univ. Press, vol. 46, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Publikationsdatum: 1961
    Schlagwort(e): Textbook of mathematics ; Statistical investigations ; Error analysis ; Earthquake hazard
    Standort Signatur Erwartet Verfügbarkeit
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  • 21
    facet.materialart.
    Unbekannt
    Wiley
    In:  Chichester, 2nd ed., xvii + 517 pp., Wiley, vol. 5, no. 22, pp. 662-664, (ISBN 0-470-87000-1 (HB), ISBN 0-470-87001-X (PB))
    Publikationsdatum: 2005
    Schlagwort(e): GIS ; Textbook of informatics ; Textbook of geography ; geography ; management ; policy
    Standort Signatur Erwartet Verfügbarkeit
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  • 22
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    Unbekannt
    Oxford Univ. Press
    In:  New York, 330 pp., Oxford Univ. Press, vol. 1, no. 1, pp. 65-66, (ISBN 0-19-850694-5)
    Publikationsdatum: 2004
    Schlagwort(e): Textbook of physics ; critical ; phenomena, ; elementary ; particles, ; phase ; transitions, ; Ising
    Standort Signatur Erwartet Verfügbarkeit
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  • 23
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    Unbekannt
    Am. Geophys. Un.
    In:  Washington, D.C., Am. Geophys. Un., vol. 22, no. 1, pp. 65-66, (ISBN 0-596-00610-1)
    Publikationsdatum: 1991
    Schlagwort(e): Deep seismic sounding (espec. cont. crust) ; Earth model, also for more shallow analyses ! ; Review article ; Reflection seismics ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 24
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    Unbekannt
    Wiley
    In:  New York, Wiley, vol. 6, no. Publ. No. 12, pp. 81-89, (ISBN 0-444-50971-2)
    Publikationsdatum: 1967
    Schlagwort(e): Textbook of geophysics
    Standort Signatur Erwartet Verfügbarkeit
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  • 25
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    Unbekannt
    Wiley
    In:  New York, Wiley, vol. 98, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 95-104, (ISBN: 1-4020-1592-5)
    Publikationsdatum: 1989
    Schlagwort(e): Rock mechanics ; Laboratory measurements
    Standort Signatur Erwartet Verfügbarkeit
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  • 26
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    Unbekannt
    Oxford Univ. Press
    In:  New York, 2nd ed. (1st in 1988), 559 pp., Oxford Univ. Press, vol. 52, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 95-104, (ISBN: 0-08-044051-7)
    Publikationsdatum: 2000
    Schlagwort(e): Rheology ; Inelastic ; Textbook of engineering ; Textbook of geophysics
    Standort Signatur Erwartet Verfügbarkeit
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  • 27
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    Unbekannt
    Wiley
    In:  Mathematical Methods for Digital Computers, Volume 1, Sapporo, Japan, Wiley, vol. 17, no. 16, pp. 211-236, (ISBN 0080419208)
    Publikationsdatum: 1967
    Schlagwort(e): Inversion
    Standort Signatur Erwartet Verfügbarkeit
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  • 28
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 37, no. 16, pp. 149-168, (ISBN 0080419208)
    Publikationsdatum: 1981
    Schlagwort(e): GeodesyY ; Project report/description ; Geol. aspects ; Tectonics ; Plate tectonics
    Standort Signatur Erwartet Verfügbarkeit
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  • 29
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    Unbekannt
    Wiley
    In:  Professional Paper, The Application of Modern Physics to the Earth and Planetary Interiors, New York, Wiley, vol. 9, no. 16, pp. 223-246, (ISBN 1-4020-1729-4)
    Publikationsdatum: 1967
    Schlagwort(e): Stress ; Tectonics ; Inelastic
    Standort Signatur Erwartet Verfügbarkeit
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  • 30
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 24, no. 231, pp. 111-121, (ISBN: 3-540-23712-7)
    Publikationsdatum: 1981
    Schlagwort(e): Tectonics ; Plate tectonics ; GeodesyY ; Geol. aspects
    Standort Signatur Erwartet Verfügbarkeit
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  • 31
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Geocomplexity and the Physics of Earthquakes, Washington, Am. Geophys. Un., vol. 120, no. 1, pp. 147-163, (ISBN: 3-540-23712-7)
    Publikationsdatum: 2000
    Schlagwort(e): Stress ; Geothermics ; Non-linear effects ; Fracture ; Seismicity ; Fluids ; AGU ; Modelling ; Rock mechanics ; Friction
    Standort Signatur Erwartet Verfügbarkeit
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  • 32
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 4, pp. 121-134, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Body waves ; P-waves ; Shear waves ; Borehole geophys. ; Anisotropy ; Review article ; Luschen ; Soellner ; Sollner ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 33
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Reflection Seismology: A Global Perspective, Braunschweig, Am. Geophys. Un., vol. 13, no. 4, pp. 31-42, (ISBN 0080419208)
    Publikationsdatum: 1986
    Schlagwort(e): Reflection seismics ; Geol. aspects ; Tectonics
    Standort Signatur Erwartet Verfügbarkeit
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  • 34
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    Unbekannt
    Wiley
    In:  Bull., Polar Proj. OP-O3A4, Earth Rheology, Isostasy and Eustasy, London, Wiley, vol. 13, no. 4, pp. 125-134, (ISBN 0080419208)
    Publikationsdatum: 1979
    Schlagwort(e): Rheology ; Creep observations and analysis ; Lithosphere
    Standort Signatur Erwartet Verfügbarkeit
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  • 35
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, The Earth's Crust, Hannover, Am. Geophys. Un., vol. 20, no. Subvol. a, pp. 289-317, (ISBN 0080419208)
    Publikationsdatum: 1977
    Schlagwort(e): Review article ; Velocity depth profile ; CRUST ; Modelling ; Velocity depth profile ; Moho ; Geochemistry ; petrology
    Standort Signatur Erwartet Verfügbarkeit
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  • 36
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Earthquake Source Mechanics, Washington, D.C., Am. Geophys. Un., vol. 1, no. 1, pp. 25-35, (ISBN 0080419208)
    Publikationsdatum: 1986
    Schlagwort(e): Earthquake precursor: prediction research ; Fault zone
    Standort Signatur Erwartet Verfügbarkeit
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  • 37
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 16, pp. 363-370, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Deep seismic sounding (espec. cont. crust) ; Reflectivity ; Review article ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 38
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 5, no. 16, pp. 215-242, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1981
    Schlagwort(e): Seismicity ; Subduction zone ; Plate tectonics
    Standort Signatur Erwartet Verfügbarkeit
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  • 39
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Open-File Rept., Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 13, no. 16, pp. 87-110, (ISBN 0080419208)
    Publikationsdatum: 1981
    Schlagwort(e): Tectonics ; Plate tectonics ; Geol. aspects
    Standort Signatur Erwartet Verfügbarkeit
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  • 40
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Open-File Rept., Earthquake Prediction: an International Review, Washington D. C., Am. Geophys. Un., vol. 4, no. 2, pp. 497-509, (ISBN 0080419208)
    Publikationsdatum: 1981
    Schlagwort(e): Earthquake precursor: prediction research ; China
    Standort Signatur Erwartet Verfügbarkeit
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  • 41
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    Unbekannt
    Am. Geophys. Un.
    In:  AGU Spring Meeting, S21A-09, Baltimore, Am. Geophys. Un., vol. 11, no. TR 80-12, pp. 1-9
    Publikationsdatum: 1989
    Schlagwort(e): Seismic networks ; NOISE ; Seismology
    Standort Signatur Erwartet Verfügbarkeit
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  • 42
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    Unbekannt
    Wiley
    In:  Time Series Analysis, Philadelphia, Wiley, vol. 161, no. 2, pp. 155, pp. L06304, (ISSN: 1340-4202)
    Publikationsdatum: 1963
    Standort Signatur Erwartet Verfügbarkeit
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  • 43
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    Unbekannt
    Oxford Univ. Press
    In:  Cary, NC 27513; 304 pp., Oxford Univ. Press, vol. 1, no. 3, pp. 632 pp., (ISBN 0-19-513895-3)
    Publikationsdatum: 2000
    Schlagwort(e): Statistical investigations ; Textbook of geophysics ; Textbook of geology ; Textbook of informatics ; GIS ; Bayesian ; Maximum ; Entropy ; (Boundary Element Method)
    Standort Signatur Erwartet Verfügbarkeit
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  • 44
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    Unbekannt
    Am. Geophys. Un.
    In:  Washington, D. C., Am. Geophys. Un., vol. 16, no. XVI:, pp. 1-14, (ISBN: 1-4020-2968-3)
    Publikationsdatum: 1972
    Schlagwort(e): Fracture ; Rock mechanics ; Inelastic ; Fluids
    Standort Signatur Erwartet Verfügbarkeit
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  • 45
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    Unbekannt
    Oxford Univ. Press
    In:  New York, 230 pp., Oxford Univ. Press, vol. 15, no. Publ. No. 12, pp. 585, (ISBN 0080424309)
    Publikationsdatum: 2000
    Schlagwort(e): ethics ; moral ; misconduct ; objectivity ; ideology ; repeatability ; method
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  • 46
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    Wiley
    In:  New York, Wiley, vol. 7, no. Publ. No. 12, pp. 127, (ISBN 1-58488-323-5)
    Publikationsdatum: 1978
    Schlagwort(e): Seismic stratigraphy
    Standort Signatur Erwartet Verfügbarkeit
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  • 47
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    Unbekannt
    Am. Geophys. Un.
    In:  Washington, Am. Geophys. Un., vol. 120, no. Publ. No. 12, pp. 81-89, (ISBN 0-444-50971-2)
    Publikationsdatum: 2000
    Schlagwort(e): Chaotic behaviour ; FractureT ; Fracture ; Seismicity ; SOC ; Pattern recognition ; AGU ; Modelling ; Stress ; Stress drop ; Rock mechanics ; Friction
    Standort Signatur Erwartet Verfügbarkeit
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  • 48
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    Unbekannt
    Wiley
    In:  New York, Wiley, vol. 25, no. Publ. No. 12, pp. 95-104, (ISBN: 0-08-043930-6)
    Publikationsdatum: 1977
    Schlagwort(e): Textbook of geophysics ; Seismology ; Gravimetry, Gravitation ; TIDES ; Geomagnetics ; Geothermics
    Standort Signatur Erwartet Verfügbarkeit
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  • 49
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    Unbekannt
    Wiley
    In:  New York, 3rd Edition, 538 pp., Wiley, vol. 14, no. 1, pp. 1-40, (ISBN 3-7643-6675-3)
    Publikationsdatum: 1987
    Schlagwort(e): Reflection seismics ; Textbook of geophysics ; Applied geophysics
    Standort Signatur Erwartet Verfügbarkeit
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  • 50
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    Unbekannt
    Am. Geophys. Un.
    In:  Washington, D.C., Am. Geophys. Un., vol. 1, no. 1, pp. 1-40, (ISBN 0-06-057199-3)
    Publikationsdatum: 1978
    Schlagwort(e): Earthquake precursor: prediction research ; Review article ; China
    Standort Signatur Erwartet Verfügbarkeit
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  • 51
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 1, no. 2, pp. 169-188, (ISBN 0-87590-532-3, AGU Code: GD0305323)
    Publikationsdatum: 1981
    Schlagwort(e): Geol. aspects ; Project report/description ; GeodesyY ; Tectonics ; Plate tectonics
    Standort Signatur Erwartet Verfügbarkeit
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  • 52
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 4, pp. 39-46, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Borehole geophys. ; Reflection seismics ; Deep seismic sounding (espec. cont. crust) ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 53
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    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Flow and Fracture of Rocks, Washington, D. C., Am. Geophys. Un., vol. 16, no. 1, pp. 275-284, (ISBN 0080419208)
    Publikationsdatum: 1972
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  • 54
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    Unbekannt
    Wiley
    In:  Chichester, 292 pp., Wiley, vol. 45, pp. ii + 37 pp. + 35 figs. + 4 tabs., (ISBN 0-471-95596-5)
    Publikationsdatum: 1998
    Schlagwort(e): Textbook of informatics ; FTN90 ; Gegenueberstellung ; der ; beiden ; Programmiersprachen ; PIK ; Potsdam
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  • 55
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    Wiley
    In:  New York, Wiley, vol. 2, no. XVI:, pp. 1-14, (ISBN 0-08-043751-6)
    Publikationsdatum: 1986
    Schlagwort(e): Data analysis / ~ processing
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  • 56
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    Oxford Univ. Press
    In:  Oxford, Oxford Univ. Press, vol. 34, no. 1, pp. 65-66, (ISBN: 3-528-02574-3)
    Publikationsdatum: 1990
    Schlagwort(e): Textbook of informatics ; FTN90 ; software ; compiler
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  • 57
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    Unbekannt
    Oxford Univ. Press
    In:  Dordrecht, Oxford Univ. Press, vol. 20, no. Publ. No. 12, pp. 81-89, (ISBN 8189304143)
    Publikationsdatum: 1998
    Schlagwort(e): Textbook of geophysics ; Fluids ; PAG
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  • 58
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    Am. Geophys. Un.
    In:  Malden, MA, Am. Geophys. Un., vol. 23, no. Publ. No. 12, pp. 95-104, (ISBN: 0-08-043930-6)
    Publikationsdatum: 1993
    Schlagwort(e): Geodesy ; GeodesyY ; Plate tectonics ; Textbook of geophysics ; Textbook of geodesy
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  • 59
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    Unbekannt
    Am. Geophys. Un.
    In:  Malden, MA, Am. Geophys. Un., vol. 25, no. Publ. No. 12, pp. 95-104, (ISBN: 0-08-043930-6)
    Publikationsdatum: 1993
    Schlagwort(e): Geodesy ; Handbook of geophysics ; Handbook of geodesy ; Instruments
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  • 60
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    Am. Geophys. Un.
    In:  Washington, D.C., Am. Geophys. Un., vol. 2, no. 1, pp. 1-40, (ISBN 0-06-057199-3)
    Publikationsdatum: 1978
    Schlagwort(e): Earthquake precursor: prediction research ; Review article ; China
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  • 61
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    Wiley
    In:  Mathematische Methoden für Digitalrechner, Sapporo, Japan, Wiley, vol. 1, no. 16, pp. 106-126, (ISBN 0080419208)
    Publikationsdatum: 1967
    Schlagwort(e): Inversion
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  • 62
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    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 37, no. 16, pp. 272--293, (ISBN: 3-540-23712-7)
    Publikationsdatum: 1981
    Schlagwort(e): Seismicity ; Tectonics ; Deep seismic sounding (espec. cont. crust)
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  • 63
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    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, The Earth's Crust, Rotterdam, Am. Geophys. Un., vol. 20, no. 2, pp. 626-675, (ISBN 0080419208)
    Publikationsdatum: 1977
    Schlagwort(e): Geothermics ; Review article ; USA
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  • 64
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 4, pp. 121-133, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Borehole geophys. ; Seismics (controlled source seismology) ; Vertical seismic profiling ; KTB ; Luschen ; Soellner ; Sollner ; Meissner ; Duerbaum ; Durbaum
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  • 65
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    Am. Geophys. Un.
    In:  Bull., Polar Proj. OP-O3A4, Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 4, pp. 69-76, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): PPREP ; Deep seismic sounding (espec. cont. crust) ; Reflectivity ; Tectonics ; Geol. aspects ; Review article ; Reflection seismics ; Meissner ; Duerbaum ; Durbaum
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  • 66
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    Am. Geophys. Un.
    In:  Bull., Open-File Rept., The Earth beneath the Continents: A Volume in Honor of Merle A. Tuve, Leiden, Am. Geophys. Un., vol. 10, no. 87-17, pp. 611-, (ISBN 0080419208)
    Publikationsdatum: 1966
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  • 67
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    Unbekannt
    Am. Geophys. Un.
    In:  AGU Fall Meeting, S22A-06, San Francisco, Am. Geophys. Un., vol. 10, no. DS 1980:17, pp. 5763-5768, (ISBN 3-933346-037)
    Publikationsdatum: 1987
    Schlagwort(e): Seismology ; Artificial intelligence (AI) ; kbs ; Detectors ; Discrimination ; Expert systems
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  • 68
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Open-File Rept., Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 16, pp. 371-376, (ISBN 0080419208)
    Publikationsdatum: 1991
    Schlagwort(e): Deep seismic sounding (espec. cont. crust) ; Plate tectonics ; Meissner ; Duerbaum ; Durbaum
    Standort Signatur Erwartet Verfügbarkeit
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  • 69
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Continental Lithosphere: Deep Seismic Reflections, Washington, D.C., Am. Geophys. Un., vol. 22, no. 16, pp. 291-298, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1991
    Schlagwort(e): Reflectivity ; Anisotropy ; Mineralogy ; Deep seismic sounding (espec. cont. crust) ; Meissner ; Duerbaum ; Durbaum
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  • 70
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 4, no. 16, pp. 307-312, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1981
    Schlagwort(e): Stress ; Plate tectonics ; GeodesyY
    Standort Signatur Erwartet Verfügbarkeit
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  • 71
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Open-File Rept., Continental and Oceanic Rifts, Washington D.C., Am. Geophys. Un., vol. 8, no. 16, pp. 17-29, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1982
    Schlagwort(e): Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Stress ; GeodesyY ; Plate tectonics ; Iceland
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  • 72
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    Unbekannt
    Am. Geophys. Un.
    In:  Bull., Open-File Rept., Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, Washington, D. C., Am. Geophys. Un., vol. 4, no. 16, pp. 122-148, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 1981
    Schlagwort(e): Review article ; Geol. aspects ; Tectonics ; Plate tectonics
    Standort Signatur Erwartet Verfügbarkeit
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  • 73
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    Unbekannt
    Am. Geophys. Un.
    In:  Professional Paper, Open-File Rept., Earthquake Prediction: an International Review, Washington D. C., Am. Geophys. Un., vol. 4, no. 2, pp. 153-172, (ISBN 0080419208)
    Publikationsdatum: 1981
    Schlagwort(e): Earthquake precursor: prediction research ; Seismicity ; Gutenberg-Richter magnitude frequency b-value ; Earthquake hazard ; seismic ; gap
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  • 74
    Publikationsdatum: 2016-12-13
    Beschreibung: Experimental studies linking community composition to functioning are typically confined to small and closed micro- or mesocosms. Such restricted conditions may affect both species’ biology and their environment. Yet, targeting simple features in the behaviour of species may circumvent these constraints. Focusing on ecological functions provided by dung beetles, we test whether large, open-top cages – MESOCLOSURES – will intercept the flight trajectories of beetles, thereby allowing manipulation of local community composition. MESOCLOSURES were built in both tropical forest (Brazil) and temperate grasslands (Finland), thus testing their general efficiency. Within the respective environments, we varied different aspects of MESOCLOSURE design: in the tropical forest, we examined the impact of MESOCLOSURE dimensions on exclusion efficiency, whereas in the temperate grassland, we assessed the potential for selectively excluding and including community members by different mesh sizes. In the temperate environment, we also went from method to application, using MESOCLOSURES to relate community composition to functioning under two simulated grazing regimes. MESOCLOSURES allowed efficient manipulation of dung beetle communities, maintaining dung beetle densities at intended levels in both temperate and tropical systems. In the tropics, the smallest cages (1 × 1 m) offered the highest contrast in beetle densities inside vs. outside of the fence, whereas the largest cages (9 × 9 m) offered the lowest. Nonetheless, densities inside cages never exceed one-fifth of those outside. At the temperate site, manipulations of community structure through mesh size yielded significant differences in functioning and suggested an interaction between small dung-dwelling species and large tunnelling species. Within cages, higher grazing was reflected in augmented dung removal. We conclude that MESOCLOSURES can be effectively used to study dung beetle functions across habitats and latitudes. As applied insights, the present study adds resolution to the significance of different functional groups of dung beetles and shows that grazing pressure may have an important impact on the ecosystem functions that they provide. Overall, this study suggests that targeted manipulation of dispersal may offer new solutions for linking fauna to ecosystem functions with minimal impact on the processes measured.
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  • 75
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    Wiley
    In:  Journal of Raman Spectroscopy, 45 (5). pp. 349-358.
    Publikationsdatum: 2016-12-13
    Beschreibung: Micro-Raman spectroscopy has been used on adult bivalve shells to investigate organic and inorganic shell components but has not yet been applied to bivalve larvae. It is known that the organic matrix of larval shells contains pigments, but less is known about the presence or source of these molecules in larvae. We investigated Raman spectra of seven species of bivalve larvae to assess the types of pigments present in shells of each species and how the ratio of inorganic : organic material changes in a dorso-ventral direction. In laboratory experiments, we reared larvae of three clam species in waters containing different organic signatures to determine if larvae incorporated compounds from source waters into their shells. We found differences in spectra and pigments between most species but found less intraspecific differences. A neural network classifier for Raman spectra classified five out of seven species with greater than 85% accuracy. There were slight differences between the amount and type of pigment present along the shell, with the prodissoconch I and shell margin areas being the most variable. Raman spectra of 1-day-old larvae were found to be differentiable when larvae were reared in waters with different organic signatures. With micro-Raman spectroscopy, it may be possible to identify some unknown species in the wild and trace their natal origins, which could enhance identification accuracy of bivalve larvae and ultimately aid management and restoration efforts.
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  • 76
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    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Oceans, 121 (10). pp. 7650-7672.
    Publikationsdatum: 2019-09-23
    Beschreibung: The Denmark Strait Overflow (DSO) contributes roughly half to the total volume transport of the Nordic overflows. The overflow increases its volume by entraining ambient water as it descends into the subpolar North Atlantic, feeding into the deep branch of the Atlantic Meridional Overturning Circulation. In June 2012, a multiplatform experiment was carried out in the DSO plume on the continental slope off Greenland (180 km downstream of the sill in Denmark Strait), to observe the variability associated with the entrainment of ambient waters into the DSO plume. In this study, we report on two high-dissipation events captured by an autonomous underwater vehicle (AUV) by horizontal profiling in the interfacial layer between the DSO plume and the ambient water. Strong dissipation of turbulent kinetic energy of O( math formula) W kg−1 was associated with enhanced small-scale temperature variance at wavelengths between 0.05 and 500 m as deduced from a fast-response thermistor. Isotherm displacement slope spectra reveal a wave number-dependence characteristic of turbulence in the inertial-convective subrange ( math formula) at wavelengths between 0.14 and 100 m. The first event captured by the AUV was transient, and occurred near the edge of a bottom-intensified energetic eddy. Our observations imply that both horizontal advection of warm water and vertical mixing of it into the plume are eddy-driven and go hand in hand in entraining ambient water into the DSO plume. The second event was found to be a stationary feature on the upstream side of a topographic elevation located in the plume pathway. Flow-topography interaction is suggested to drive the intense mixing at this site.
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  • 77
    Publikationsdatum: 2020-10-26
    Beschreibung: Male secondary sexual traits are targets of inter- and/or intrasexual selection, but can vary due to a correlation with life-history traits or as by-product of adaptation to distinct environments. Trade-offs contributing to this variation may comprise conspicuousness towards conspecifics versus inconspicuousness towards predators, or between allocating resources into coloration versus the immune system. Here, we examine variation in expression of a carotenoid-based visual signal, anal-fin egg-spots, along a replicate environmental gradient in the haplochromine cichlid fish Astatotilapia burtoni. We quantified egg-spot number, area, and coloration; applied visual models to estimate the trait's conspicuousness when perceived against the surrounding tissue under natural conditions; and used the lymphocyte ratio as a measure for immune activity. We find that (i) males possess larger and more conspicuous egg-spots than females, which is likely explained by their function in sexual selection; (ii) riverine fish generally feature fewer but larger and/or more intensively colored egg-spots, which is probably to maintain signal efficiency in intraspecific interactions in long-wavelength shifted riverine light conditions; and (iii) egg-spot number and relative area correlate with immune defense, suggesting a trade-off in the allocation of carotenoids. Taken together, haplochromine egg-spots feature the potential to adapt to the respective underwater light environment, and are traded-off with investment into the immune system
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  • 78
    Publikationsdatum: 2020-02-06
    Beschreibung: The ocean's potential to export carbon to depth partly depends on the fraction of primary production (PP) sinking out of the euphotic zone (i.e., the e-ratio). Measurements of PP and export flux are often performed simultaneously in the field, although there is a temporal delay between those parameters. Thus, resulting e-ratio estimates often incorrectly assume an instantaneous downward export of PP to export flux. Evaluating results from four mesocosm studies, we find that peaks in organic matter sedimentation lag chlorophyll a peaks by 2 to 15 days. We discuss the implications of these time lags (TLs) for current e-ratio estimates and evaluate potential controls of TL. Our analysis reveals a strong correlation between TL and the duration of chlorophyll a buildup, indicating a dependency of TL on plankton food web dynamics. This study is one step further toward time-corrected e-ratio estimates
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  • 79
    Publikationsdatum: 2020-07-20
    Beschreibung: Tephra provides regional chronostratigraphical marker horizons that can link different climate archives with highly needed accuracy and precision. The results presented in this work exemplify, however, that the intermittent storage of tephra in ice sheets and during its subsequent iceberg transport, especially during glacial stages, constitutes a potential source of serious error for the application of tephrochronology to Nordic Seas and North Atlantic sediment archives. The peak shard concentration of the rhyolitic component of the North Atlantic Ash Zone II (NAAZ-II) tephra complex, often used to correlate marine and ice core records in Marine Isotope Stage (MIS) 3, is shown to lag the eruption event by ca. 100–400 years in some North Atlantic and Norwegian Sea cores. While still allowing for a correlation of archives on millennial timescales, this time delay in deposition is a major obstacle when addressing the lead–lag relationship on short timescales (years to centuries). A precise and accurate determination of lead–lag relationships between archives recording different parts of the climate system is crucial in order to test hypotheses about the processes leading to abrupt climate change and to evaluate results from climate models. Copyright # 2011 John Wiley & Sons, Ltd.
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  • 80
    Publikationsdatum: 2020-02-06
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  • 81
    Publikationsdatum: 2020-06-23
    Beschreibung: A multiproxy study of palaeoceanographic and climatic changes in northernmost Baffin Bay shows that major environmental changes have occurred since the deglaciation of the area at about 12 500 cal. yr BP. The interpretation is based on sedimentology, benthic and planktonic foraminifera and their isotopic composition, as well as diatom assemblages in the sedimentary records at two core sites, one located in the deeper central part of northernmost Baffin Bay and one in a separate trough closer to the Greenland coast. A revised chronology for the two records is established on the basis of 15 previously published AMS 14C age determinations. A basal diamicton is overlain by laminated, fossil-free sediments. Our data from the early part of the fossiliferous record (12 300–11 300 cal. yr BP), which is also initially laminated, indicate extensive seasonal sea-ice cover and brine release. There is indication of a cooling event between 11 300 and 10 900 cal. yr BP, and maximum Atlantic Water influence occurred between 10 900 and 8200 cal. yr BP (no sediment recovery between 8200 and 7300 cal. yr BP). A gradual, but fluctuating, increase in sea-ice cover is seen after 7300 cal. yr BP. Sea-ice diatoms were particularly abundant in the central part of northernmost Baffin Bay, presumably due to the inflow of Polar waters from the Arctic Ocean, and less sea ice occurred at the near-coastal site, which was under continuous influence of the West Greenland Current. Our data from the deep, central part show a fluctuating degree of upwelling after c. 7300 cal. yr BP, culminating between 4000 and 3050 cal. yr BP. There was a gradual increase in the influence of cold bottom waters from the Arctic Ocean after about 3050 cal. yr BP, when agglutinated foraminifera became abundant. A superimposed short-term change in the sea-surface proxies is correlated with the Little Ice Age cooling.
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  • 82
    Publikationsdatum: 2021-04-23
    Beschreibung: Stable isotope compositions can potentially be used to trace atmospheric Cd inputs to the surface ocean and anthropogenic Cd emissions to the atmosphere. Both of these applications may provide valuable insights into the effects of anthropogenic activities on the cycling of Cd in the environment. However, a lack of constraints for the Cd isotope compositions of atmospheric aerosols is currently hindering such studies. Here, we present stable Cd isotope data for aerosols collected over the Tropical Atlantic Ocean. The samples feature variable proportions of mineral dust-derived and anthropogenic Cd, yet exhibit similar isotope compositions, thus negating the distinction of these Cd sources using isotopic signatures in this region. Isotopic variability between these two atmospheric Cd sources may be identified in other areas, and thus warrants further investigation. Regardless, these data provide important initial constraints on the isotope composition of atmospheric Cd inputs to the ocean.
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  • 83
    Publikationsdatum: 2020-02-06
    Beschreibung: Aim: The lives of juvenile leatherback turtles are amongst the most enigmatic of all marine mega-vertebrates. For these cryptic organisms, ocean models provide important insights into their dispersion from natal sites. Here, corroborated by fisheries bycatch data, we simulate spatio-temporal variation in hatchling dispersion patterns over five decades from the World's largest leatherback turtle nesting region. Location: Equatorial Central West Africa (3.5°N to −6°S) spanning the Gulf of Guinea in the North, Gabon and the Republic/Democratic Republic of the Congo in the South. Results: Due to dynamic oceanic conditions at these equatorial latitudes, dispersion scenarios differed significantly: (1) along the north to south gradient of the study region, (2) seasonally and (3) between years. From rookeries to the north of the equator, simulated hatchling retention rates within the Gulf of Guinea were very high (〉99%) after 6 months of drift, whilst south of the equator, retention rates were as low as c. 6% with the majority of simulated hatchlings dispersing west into the South Atlantic Ocean with the South Equatorial Current. Seasonal dispersion variability was driven by wind changes arising from the yearly north/southward migration of the intertropical convergence zone resulting in the increasing westerly dispersion of hatchlings throughout the hatching season. Annual variability in wind stress drove a long-term trend for decreased retention within the Gulf of Guinea and increased westerly dispersion into habitats in the South Atlantic Ocean. Main conclusions: Shifts in dispersion habitats arising from spatio-temporal oceanic variability expose hatchlings to different environments and threats that will influence important life history attributes such as juvenile growth/survival rates; anticipated to impact the population dynamics and size/age structure of populations into adulthood. The impacts of local and dynamic oceanic conditions thus require careful considerations, such as subregional management, when managing marine populations of conservation concern.
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  • 84
    Publikationsdatum: 2020-07-20
    Beschreibung: An investigation was carried out on larvae of the oceanic tropical squid Sthenoteuthis pteropus in the equatorial Atlantic (2°30′N–7°S;12°W –8°30′E) The age of the larvae was calculated from the statolith microstructure of 20 larvae; mortality was estimated from the size structure of 1128 larvae. The larval stage lasts 32–38 days. At ages ranging from 14 to 38 days. the daily relative growth rates of mantle length decrease from 7.5 to 2.8% day −1 and from 14–16 to 5.8% of body weight day −1 At age 12–24 days, mortality rates were estimated using both raw catch data and corrected data accounting for net avoidance. The mean value of raw mortality rates was 0.189, the corrected value was 0.158. During the proboscis division (transformation of the larva into juvenile) at age 25–35 days, a sharp decrease in larval growth rates and a simultaneous increase in mortality rates (raw 0.443, corrected 0.379) were observed.
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  • 85
    Publikationsdatum: 2020-02-06
    Beschreibung: The waning stage(s) of the Tethyan ocean(s) in the Balkans are not well understood. Controversy centres on the origin and life-span of the Cretaceous Sava Zone, which is allegedly a remnant of the last oceanic domain in the Balkan Peninsula, defining the youngest suture between Eurasia- and Adria-derived plates. In order to investigate to what extent late-Cretaceous volcanism within the Sava zone is consistent with this model, we present new age data together with trace-element and Sr–Nd–Pb isotope data for the Klepa basaltic lavas from the central Balkan Peninsula. Our new geochemical data show marked differences between the Cretaceous Klepa basalts (Sava Zone) and the rocks of other volcanic sequences from the Jurassic ophiolites of the Balkans. The Klepa basalts mostly have Sr–Nd–Pb isotopic and trace-element signatures that resemble enriched within-plate basalts, substantially different from Jurassic ophiolite basalts with MORB, BAB and IAV affinities. Trace-element modelling of the Klepa rocks indicates 2–20% polybaric melting of a relatively homogeneously metasomatised mantle source that ranges in composition from garnet lherzolite to ilmenite+apatite bearing spinel–amphibole lherzolite. Thus, the residual mineralogy is characteristic of a continental rather than oceanic lithospheric mantle source, suggesting an intracontinental within-plate origin for the Klepa basalts. Two alternative geodynamic models are internally consistent with our new findings: i) if the Sava Zone represents remnants of the youngest Neotethyan Ocean, magmatism along this zone would be situated within the forearc region and triggered by ridge subduction; ii) if the Sava Zone delimits a diffuse tectonic boundary between Adria and Europe, which had already collided in the Late Jurassic, the Klepa basalts together with a number of other magmatic centres represent volcanism related to transtensional tectonics.
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  • 86
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    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Oceans, 122 (4). 2830-2846 .
    Publikationsdatum: 2020-02-06
    Beschreibung: The upstream sources and pathways of the Denmark Strait Overflow Water and their variability have been investigated using a high-resolution model hindcast. This global simulation covers the period from 1948 to 2009 and uses a fine model mesh (1/20°) to resolve mesoscale features and the complex current structure north of Iceland explicitly. The three sources of the Denmark Strait Overflow, the shelfbreak East Greenland Current (EGC), the separated EGC, and the North Icelandic Jet, have been analyzed using Eulerian and Lagrangian diagnostics. The shelfbreak EGC contributes the largest fraction in terms of volume and freshwater transport to the Denmark Strait Overflow and is the main driver of the overflow variability. The North Icelandic Jet contributes the densest water to the Denmark Strait Overflow and shows only small temporal transport variations. During summer, the net volume and freshwater transports to the south are reduced. On interannual time scales, these transports are highly correlated with the large-scale wind stress curl around Iceland and, to some extent, influenced by the North Atlantic Oscillation, with enhanced southward transports during positive phases. The Lagrangian trajectories support the existence of a hypothesized overturning loop along the shelfbreak north of Iceland, where water carried by the North Icelandic Irminger Current is transformed and feeds the North Icelandic Jet. Monitoring these two currents and the region north of the Iceland shelfbreak could provide the potential to track long-term changes in the Denmark Strait Overflow and thus also the AMOC.
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  • 87
    Publikationsdatum: 2017-05-02
    Beschreibung: The diet composition of Emperor Penguin Aptenodytes forsteri chicks was examined at Auster and Taylor Glacier colonies, near Australia's Mawson station, Antarctica, between hatching in mid-winter and fledging in mid-summer by “water-offloading” adults. Chicks at both colonies were fed a similar suite of prey species. Crustaceans occurred in 82% of stomach samples at Auster and 87% of stomachs at Taylor Glacier and were heavily digested: their contribution to food mass could not be quantified. Fish, primarily bentho-pelagic species, accounted for 52% by number and 55% by mass of chick diet at Auster, and squid formed the remainder. At Taylor Glacier the corresponding values were 27% by number and 31% by mass of fish and 73% by number and 69% by mass of squid. Of the 33 species or taxa identified, the fish Trematomus eulepidotus and the squid Psychroteuthis glacialis and Allu-roteuthis antarcticus accounted for 64% and 74% of the diets by mass at Auster and Taylor Glacier, respectively. The sizes of fish varied temporally but not in a linear manner from winter to summer. Adult penguins captured fish ranging in length from 60 mm (Pfeura-gramma antarcticum) to 250 mm (T. eulepidotus) and squid (P. glacialis) from 19 to 280 mm in mantle length. The length-frequency distribution of P. glacialis showed seasonal variation, with the size of squid increasing from winter to summer. The energy density of chick diet mix increased significantly prior to “fledging”.
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  • 88
    facet.materialart.
    Unbekannt
    Wiley
    In:  Biologie in unserer Zeit, 24 (4). pp. 192-199.
    Publikationsdatum: 2020-06-05
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  • 89
    Publikationsdatum: 2020-02-06
    Beschreibung: The North Atlantic Current (NAC) is subject to variability on multiannual to decadal time scales, influencing the transport of volume, heat, and freshwater from the subtropical to the eastern subpolar North Atlantic (NA). Current observational time series are either too short or too episodic to study the processes involved. Here we compare the observed continuous NAC transport time series at the western flank of the Mid-Atlantic Ridge (MAR) and repeat hydrographic measurements at the OVIDE line in the eastern Atlantic with the NAC transport and circulation in the high-resolution (1/20°) ocean model configuration VIKING20 (1960–2008). The modeled baroclinic NAC transport relative to 3400 m (24.5 ± 7.1 Sv) at the MAR is only slightly lower than the observed baroclinic mean of 27.4 ± 4.7 Sv from 1993 to 2008, and extends further north by about 0.5°. In the eastern Atlantic, the western NAC (WNAC) carries the bulk of the transport in the model, while transport estimates based on hydrographic measurements from five repeated sections point to a preference for the eastern NAC (ENAC). The model is able to simulate the main features of the subpolar NA, providing confidence to use the model output to analyze the influence of the North Atlantic Oscillation (NAO). Model based velocity composites reveal an enhanced NAC transport across the MAR of up to 6.7 Sv during positive NAO phases. Most of that signal (5.4 Sv) is added to the ENAC transport, while the transport of the WNAC was independent of the NAO.
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  • 90
    facet.materialart.
    Unbekannt
    Oxford Univ. Press
    In:  ICES Journal of Marine Science, 52 (1). pp. 127-137.
    Publikationsdatum: 2020-07-29
    Beschreibung: A number of reproductive indices were compared with a subjective maturity scale for assessment of Loligo forbesi maturity. The ratio between nidamental gland length and mantle length corresponded well with female maturation, as did the ovary mass-soma mass and nidamental gland mass-soma mass ratios. For males, the ratio between spermatophoric complex mass and somatic mass was found to be the most suitable for maturity assessment. The timing of recruitment and maturation of L. forbesi in Irish waters was described from the size and maturity of squid in commercial landings in the south of Ireland during the years 1991–1993. Immature squid first appeared in commercial catches in July and August, and this represented the main period of recruitment. A second period of recruitment was apparent in December 1991, but was not identified in the 1992–1993 season. Mature females were present in the commercially exploited population between November and April, with a small number also found in the summer. The abundance of egg masses was used to indicate timing of spawning. Egg masses recovered from the Cork coast indicated that peak spawning occurred during the winter months, but continued on a small scale for much of the year.
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  • 91
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    Unbekannt
    AGU (American Geophysical Union) | Wiley
    In:  Geophysical Research Letters, 44 (9). pp. 4246-4255.
    Publikationsdatum: 2020-02-06
    Beschreibung: While the Earth's surface has considerably warmed over the past two decades, the tropical Pacific has featured a cooling of sea surface temperatures in its eastern and central parts, which went along with an unprecedented strengthening of the equatorial trade winds, the surface component of the Pacific Walker Circulation (PWC). Previous studies show that this decadal trend in the trade winds is generally beyond the range of decadal trends simulated by climate models when forced by historical radiative forcing. There is still a debate on the origin of and the potential role that internal variability may have played in the recent decadal surface wind trend. Using a number of long control (unforced) integrations of global climate models and several observational data sets, we address the question as to whether the recent decadal to multidecadal trends are robustly classified as an unusual event or the persistent response to external forcing. The observed trends in the tropical Pacific surface climate are still within the range of the long-term internal variability spanned by the models but represent an extreme realization of this variability. Thus, the recent observed decadal trends in the tropical Pacific, though highly unusual, could be of natural origin. We note that the long-term trends in the selected PWC indices exhibit a large observational uncertainty, even hindering definitive statements about the sign of the trends.
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  • 92
    Publikationsdatum: 2017-06-07
    Beschreibung: The Denmark Strait Overflow (DSO) today compensates for the northward flowing Norwegian and Irminger branches of the North Atlantic Current that drive the Nordic heat pump. During the Last Glacial Maximum (LGM), ice sheets constricted the Denmark Strait aperture in addition to ice eustatic/isostatic effects which reduced its depth (today ∼630 m) by ∼130 m. These factors, combined with a reduced north-south density gradient of the water-masses, are expected to have restricted or even reversed the LGM DSO intensity. To better constrain these boundary conditions, we present a first reconstruction of the glacial DSO, using four new and four published epibenthic and planktic stable-isotope records from sites to the north and south of the Denmark Strait. The spatial and temporal distribution of epibenthic δ18O and δ13C maxima reveals a north-south density gradient at intermediate water depths from σ0∼28.7 to 28.4/28.1 and suggests that dense and highly ventilated water was convected in the Nordic Seas during the LGM. However, extremely high epibenthic δ13C values on top of the Mid-Atlantic Ridge document a further convection cell of Glacial North Atlantic Intermediate Water to the south of Iceland, which, however, was marked by much lower density (σ0∼28.1) The north-south gradient of water density possibly implied that the glacial DSO was directed to the south like today and fed Glacial North Atlantic Deep Water that has underthrusted the Glacial North Atlantic Intermediate Water in the Irminger Basin.
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  • 93
    Publikationsdatum: 2017-07-18
    Beschreibung: We investigated genetic differentiation among populations of the clonal grass Elymus athericus, a common salt-marsh species occurring along the Wadden Sea coast of Europe. While E. athericus traditionally occurs in the high salt marsh, it recently also invaded lower parts of the marsh. In one of the first analyses of the genetic population structure in salt-marsh species, we were interested in population differentiation through isolation-by-distance, and among strongly divergent habitats (low and high marsh) in this wind- and water-dispersed species. High and low marsh habitats were sampled at six sites throughout the Wadden Sea. Based on reciprocal transplantation experiments conducted earlier revealing lower survival of foreign genotypes we predicted reduced gene flow among habitats. Accordingly, an analysis with polymorphic cross-species microsatellite primers revealed significant genetic differentiation between high and low marsh habitats already on a very small scale (〈 100 m), while isolation-by-distance was present only on larger scales (60–443 km). In an analysis of molecular variance we found that 14% of the genetic variance could be explained by the differentiation between habitats, as compared to only 8.9% to geographical (isolation-by-distance) effects among six sites 2.5–443 km distant from each other. This suggests that markedly different selection regimes between these habitats, in particular intraspecific competition and herbivory, result in habitat adaptation and restricted gene flow over distances as small as 80 m. Hence, the genetic population structure of plant species can only be understood when considering geographical and selection-mediated restrictions to gene flow simultaneously.
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  • 94
    facet.materialart.
    Unbekannt
    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Oceans, 122 (4). pp. 3481-3499.
    Publikationsdatum: 2020-02-06
    Beschreibung: We examine the mean pathways, transit timescales, and transformation of waters flowing from the Pacific and the marginal seas through the Indian Ocean (IO) on their way toward the South Atlantic within a high-resolution ocean/sea-ice model. The model fields are analyzed from a Lagrangian perspective where water volumes are tracked as they enter the IO. The IO contributes 12.6 Sv to Agulhas leakage, which within the model is 14.1 ± 2.2 Sv, the rest originates from the South Atlantic. The Indonesian Through-flow constitutes about half of the IO contribution, is surface bound, cools and salinificates as it leaves the basin within 10–30 years. Waters entering the IO south of Australia are at intermediate depths and maintain their temperature-salinity properties as they exit the basin within 15–35 years. Of these waters, the contribution from Tasman leakage is 1.4 Sv. The rest stem from recirculation from the frontal regions of the Southern Ocean. The marginal seas export 1.0 Sv into the Atlantic within 15–40 years, and the waters cool and freshen on-route. However, the model's simulation of waters from the Gulfs of Aden and Oman are too light and hence overly influenced by upper ocean circulations. In the Cape Basin, Agulhas leakage is well mixed. On-route, temperature-salinity transformations occur predominantly in the Arabian Sea and within the greater Agulhas Current region. Overall, the IO exports at least 7.9 Sv from the Pacific to the Atlantic, thereby quantifying the strength of the upper cell of the global conveyor belt.
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  • 95
    Publikationsdatum: 2020-02-06
    Beschreibung: The transition from benthos to plankton requires multiple adaptations, yet so far it remains unclear how these are acquired in the course of the transition. To investigate this process, we analyzed the genetic diversity and distribution patterns of a group of foraminifera of the genus Bolivina with a tychopelagic mode of life (same species occurring both in benthos and plankton). We assembled a global sequence data set for this group from single-cell DNA extractions and occurrences in metabarcodes from pelagic environmental samples. The pelagic sequences all cluster within a single monophyletic clade within Bolivina. This clade harbors three distinct genetic lineages, which are associated with incipient morphological differentiation. All lineages occur in the plankton and benthos, but only one lineage exhibits no limit to offshore dispersal and has been shown to grow in the plankton. These observations indicate that the emergence of buoyancy regulation within the clade preceded the evolution of pelagic feeding and that the evolution of both traits was not channeled into a full transition into the plankton. We infer that in foraminifera, colonization of the planktonic niche may occur by sequential cooptation of independently acquired traits, with holoplanktonic species being recruited from tychopelagic ancestors
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  • 96
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    Unbekannt
    Wiley
    In:  Journal of Microscopy, 131 (2). pp. 173-186.
    Publikationsdatum: 2017-07-13
    Beschreibung: Many of the difficulties of staining plastic embedded tissues for light and electron microscopy derive from physical exclusion of hydrophilic staining reagents by hydrophobic embedding media. Structures which stain most intensely with hydrophilic reagents usually contain less hydrophobic plastic than do non-staining structures. Such incomplete infiltration is apparently caused by exclusion of viscous, hydrophobic monomers by physically dense and/or well hydrated tissue elements. In keeping with this, generalized staining of tissues embedded in hydrophobic media does occur when hydrophobic reagents are used. Staining of plastic-free structures with single hydrophilic reagents or with sequences of such reagents, is, however, largely rate-controlled. The surprising similarity of hydrophilic and hydrophobic plastic embedding media is discussed. Limits of this simple model are explored, with a consideration of the roles of fixative and of monomer-tissue reactions
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  • 97
    Publikationsdatum: 2017-06-15
    Beschreibung: At the largest time and space scales, the pace of erosion and chemical weathering is determined by tectonic uplift rates. Deviations from equilibrium arise from the transient response of landscape denudation to climatic and tectonic perturbations. We posit that the constraint of mass balance, however, makes it unlikely that such disequilibrium persists at the global scale over millions of years, as has been proposed for late Cenozoic erosion. We synthesize weathering fluxes, global sedimentation rates, sediment yields and tectonic motions to show a remarkable constancy in the pace of Earth-surface evolution over the last 10 Ma and support the null hypothesis – that global rates of landscape change have remained constant over this time period, despite global climate change and mountain building events. This work undermines the hypothesis that increased weathering due to mountain building or climate change was the primary agent for a decrease in global temperatures.
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  • 98
    Publikationsdatum: 2018-03-15
    Beschreibung: INTRODUCTION: Lichens are self-sustaining partnerships comprising fungi as shape-forming partners for their enclosed symbiotic algae. They produce a tremendous diversity of metabolites (1050 metabolites described so far). OBJECTIVES: A comparison of metabolic profiles in nine lichen species belonging to three genera (Lichina, Collema and Roccella) by using an optimised extraction protocol, determination of the fragmentation pathway and the in situ localisation for major compounds in Roccella species. METHODS: Chemical analysis was performed using a complementary study combining a Taguchi experimental design with qualitative analysis by high-performance liquid chromatography coupled with mass spectrometry techniques. RESULTS: Optimal conditions to obtain the best total extraction yield were determined as follows: mortar grinding to a fine powder, two successive extractions, solid:liquid ratio (2:60) and 700 rpm stirring. Qualitative analysis of the metabolite profiling of these nine species extracted with the optimised method was corroborated using MS and MS/MS approaches. Nine main compounds were identified: 1 β-orcinol, 2 orsellinic acid, 3 putative choline sulphate, 4 roccellic acid, 5 montagnetol, 6 lecanoric acid, 7 erythrin, 8 lepraric acid and 9 acetylportentol, and several other compounds were reported. Identification was performed using the m/z ratio, fragmentation pathway and/or after isolation by NMR analysis. The variation of the metabolite profile in differently organised parts of two Roccella species suggests a specific role of major compounds in developmental stages of this symbiotic association. CONCLUSION: Metabolic profiles represent specific chemical species and depend on the extraction conditions, the kind of the photobiont partner and the in situ localisation of major compounds.
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  • 99
    facet.materialart.
    Unbekannt
    AGU (American Geophysical Union) | Wiley
    In:  Geochemistry, Geophysics, Geosystems, 18 (6). 2305-2320 .
    Publikationsdatum: 2020-02-06
    Beschreibung: The potential of mining seafloor massive sulfide deposits for metals such as Cu, Zn, and Au is currently debated. One key challenge is to predict where the largest deposits worth mining might form, which in turn requires understanding the pattern of subseafloor hydrothermal mass and energy transport. Numerical models of heat and fluid flow are applied to illustrate the important role of fault zone properties (permeability and width) in controlling mass accumulation at hydrothermal vents at slow spreading ridges. We combine modeled mass-flow rates, vent temperatures, and vent field dimensions with the known fluid chemistry at the fault-controlled Logatchev 1 hydrothermal field of the Mid-Atlantic Ridge. We predict that the 135 kilotons of SMS at this site (estimated by other studies) can have accumulated with a minimum depositional efficiency of 5% in the known duration of hydrothermal venting (58,200 year age of the deposit). In general, the most productive faults must provide an efficient fluid pathway while at the same time limit cooling due to mixing with entrained cold seawater. This balance is best met by faults that are just wide and permeable enough to control a hydrothermal plume rising through the oceanic crust. Model runs with increased basal heat input, mimicking a heat flow contribution from along-axis, lead to higher mass fluxes and vent temperatures, capable of significantly higher SMS accumulation rates. Nonsteady state conditions, such as the influence of a cooling magmatic intrusion beneath the fault zone, also can temporarily increase the mass flux while sustaining high vent temperatures.
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  • 100
    Publikationsdatum: 2020-02-06
    Beschreibung: Diazotrophic dinitrogen (N2) fixation contributes ~76% to "new" nitrogen inputs to the sunlit open ocean, but environmental factors determining N2 fixation rates are not well constrained. Excess phosphate (phosphate-nitrate/16 〉 0) and iron availability control N2 fixation rates in the eastern tropical North Atlantic (ETNA), but it remains an open question how excess phosphate is generated within or supplied to the phosphate-depleted sunlit layer. Our observations in the ETNA region (8°N-15°N, 19°W-23°W) suggest that Prochlorococcus and Synechococcus, the two ubiquitous non-diazotrophic cyanobacteria with cellular N:P ratios higher than the Redfield ratio, create an environment of excess phosphate, which cannot be explained by diapycnal mixing, atmospheric, and riverine inputs. Thus, our results unveil a new biogeochemical niche construction mechanism by non-diazotrophic cyanobacteria for their diazotrophic phylum group members (N2 fixers). Our observations may help to understand the prevalence of diazotrophy in low-phosphate, oligotrophic regions.
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