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  • Other Sources  (88)
  • Springer  (49)
  • AGU (American Geophysical Union)  (39)
  • 1995-1999  (38)
  • 1990-1994  (50)
  • 1920-1924
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  • 1
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    Springer
    In:  Professional Paper, Super-Deep Continental Drilling and Deep Geophysical Sounding, Berlin, Springer, vol. 65, no. 16, pp. 372-376, (ISBN: 3-540-23712-7)
    Publication Date: 1990
    Keywords: Borehole geophys. ; Review article ; scientific drilling ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; Stress ; Stress measurements
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  • 2
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    Springer
    In:  Marine Biology, 106 (2). pp. 251-259.
    Publication Date: 2020-07-14
    Description: Rates of protein synthesis in the whole body and tissues ofOctopus vulgaris collected in September 1985 and 1986 from the Bay of Naples were measured following a flooding dose injection of3H phenylalanine. There were stable phenylalanine free pool-specific radioactivities and linear incorporation of radiolabel into arm-tip protein from 10 to 30 min after the injection. In starved individuals there were no significant differences between the fractional rates of protein synthesis of the following tissues: ventricle, brain, branchial heart, arm tip, gill, stomach, arm, renal appendage and mantle. The mean value (± SE) for all the tissues was 3.02 ± 0.17% d−1. In individuals fed varying amounts of crab, resulting in differing growth rates, there was a linear increase in fractional rates of whole-body protein synthesis with growth rate. A standard 148 g octopus growing at 3.0% d−1 synthesised 0.54 g of protein, with 0.43 g of this protein retained as growth. The proportion of the total protein synthesis which was retained as growth increased with increasing growth rate; at a maximum growth rate of 6% d−1, over 90% of the protein synthesised was retained as growth. The ventricle, arm tip, gill, arm and mantle also showed similar patterns of a linear increase in fractional rates of protein synthesis with increased growth rates. The RNA concentrations in the whole body and tissues increased with increasing growth rates, but the major change was an increase in the efficiency of translation. It is concluded that rapid growth rates inO. vulgaris are brought about by high rates of protein synthesis and high efficiencies of retention of synthesised protein and, therefore, little protein degradation.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    AGU (American Geophysical Union)
    In:  Paleoceanography, 8 (1). pp. 1-6.
    Publication Date: 2016-05-25
    Description: We present a method for determining the δ180 of seawater in the deep ocean during the last glacial maximum from the measured δ180 values of deep sea pore fluids. Using data from Deep Sea Drilling Project (DSDP) site 576 in the Western Pacific, this method yields a glacial to interglacial change in δ180swof 1.010.25 0/00. This value for ~δ180sw is the first direct measurement of deep ocean 8180 for the last glacial maximum and avoids the problems of spatial and temporal variability of the δ180 of surface water implicit in previous determinations. More precise, higher resolution pore fluid measurements are required to improve this determination.
    Type: Article , PeerReviewed
    Format: text
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  • 4
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    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Solid Earth, 100 (B11). pp. 22261-22282.
    Publication Date: 2021-06-15
    Description: Within the Australian-Antarctic Discordance (AAD), a boundary exists between isotopically defined “Pacific-type” and “Indian-type” mid-ocean ridge basalt (MORB) erupted along the Southeast Indian Ridge (SEIR). This boundary has migrated westward beneath the easternmost AAD spreading segment at a minimum rate of 25 mm/yr since 4 Ma; however, its long-term history remains a matter of speculation. To determine if Pacific-type upper mantle has migrated westward beneath the eastern Indian Ocean basin as Australia and Antarctica drifted apart during the last 70 m.y., we present new Sr-Nd-Pb isotope data, combined with trace element and 40Ar-39Ar radiometric age determinations, for samples from Legs 28 and 29 of the Deep Sea Drilling Project (DSDP). Basaltic basement at these DSDP sites provides a record of their upper mantle source composition and shows regional variations consistent with upper mantle flow in this region. East of the South Tasman Rise, all DSDP basalts have 87Sr/86Sr (0.7025–0.7029) and 206Pb/204Pb (18.80–19.48) ratios typical of Pacific-type MORB indicating that Pacific-type upper mantle existed east of the Australian-Antarctic continental margin and beneath the Tasman Sea during the early stages of seafloor spreading in this region. Basalts from DSDP sites west of the AAD have high 87Sr/86Sr (0.7030–0.7035), low 206Pb/204Pb (17.99–18.10) and trace element characteristics typical of present day Indian-type SEIR MORB. Between these two regions, DSDP basalts recovered along the western margin of the South Tasman Rise have isotopic characteristics that are, in one case consistent with an Indian-type MORB source (Site 280A) and, in the second case, transitional between Pacific-type and Indian-type mantle sources. The occurrence of seafloor basalts with transitional or Indian-type isotopic characteristics well to the east of the present Indian-Pacific MORB isotopic boundary within the AAD strongly implies that Pacific-type upper mantle has migrated westward into the region since the South Tasman Rise separated from Antarctica circa 40 Ma.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2018-04-12
    Description: Petrologic and geochemical studies of vent solids from the Main Endeavour Field (MEF) and the High Rise Field (HRF), Juan de Fuca Ridge, demonstrate that the steep‐sided vent structures characteristic of these sites form dominantly by flange growth, combined with diffuse flow through sealed portions of structures, and incorporation of flanges into structures. Geochemical calculations suggest that the prevalence of amorphous silica and flanges in Endeavour deposits is the result of conductive cooling of vent fluids that have high concentrations of ammonia. At Endeavour, as the temperature of vent fluid decreases, ammonia‐ammonium equilibrium buffers pH and allows more efficient deposition of sulfide minerals and silica from fluids that have a higher pH than conductively cooled ammonia‐poor fluids present at most other unsedimented mid‐ocean ridge vent sites. Deposition of silica stabilizes flanges and allows structures to attain large size. It also leads to diffuse flow and further conductive cooling by reducing the permeability and porosity of the structures and of feeder zones, thus decreasing entrainment of seawater. Most inactive vent samples recovered from areas peripheral to the HRF and MEF are similar to barite + silica rich samples from the Explorer Ridge and Axial Seamount and likely formed from precipitation of silica and barite on a biological substrate. Active white smoker chimneys from the Clam Bed Field, located south of the HRF, are pyrrhotite rich and likely formed from vent fluids that are depleted in Zn and Cd and enriched in Pb and Ba relative to fluids exiting trans‐Atlantic geotraverse (TAG) and Cleft Segment white smoker chimneys.
    Type: Article , PeerReviewed
    Format: text
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  • 6
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    Springer
    In:  Springer
    Publication Date: 1996
    Keywords: Textbook of mathematics ; Data analysis / ~ processing ; Textbook of geophysics ; Chaotic behaviour
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  • 7
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    Springer
    In:  Amsterdam, 394 pp., Springer, vol. 46, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Publication Date: 1990
    Description: Consisting of more than 150 articles written by leading experts, this authoritative reference encompasses the entire field of solid-earth geophysics. It describes in detail the state of current knowledge, including advanced instrumentation and techniques, and focuses on important areas of exploration geophysics. It also offers clear and complete coverage of seismology, geodesy, gravimetry, magnetotellurics and related areas in the adjacent disciplines of physics, geology, oceanography and space science.
    Keywords: Textbook of geophysics ; Seismology ; Geodesy ; Gravimetry, Gravitation ; Electromagnetic methods/phenomena ; Applied geophysics ; PlanetologyT
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  • 8
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    Springer
    In:  Bull., Polar Proj. OP-O3A4, Super-Deep Continental Drilling and Deep Geophysical Sounding, Berlin, Springer, vol. 66, no. 2, pp. 134-140, (ISBN 0080419208)
    Publication Date: 1990
    Keywords: Geol. aspects ; scientific drilling ; Deep seismic sounding (espec. cont. crust) ; Earth model, also for more shallow analyses ! ; EUROPROBE (Geol. and Geophys. in eastern Europe)
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  • 9
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    Springer
    In:  Bull., Polar Proj. OP-O3A4, Super-Deep Continental Drilling and Deep Geophysical Sounding, Berlin, Springer, vol. 65, no. Subvol. b, pp. 353-363, (ISBN 0080419208)
    Publication Date: 1990
    Keywords: scientific drilling ; Borehole geophys. ; Mineralogy ; Geol. aspects ; EUROPROBE (Geol. and Geophys. in eastern Europe)
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  • 10
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    Springer
    In:  Berlin, Springer, vol. 4, no. Subvol. b, pp. 220, (ISBN: 1589480406)
    Publication Date: 1992
    Keywords: Fracture ; Handbook of geophysics ; Handbook of physics
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