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  • Other Sources  (21)
  • Elsevier  (11)
  • American Geophysical Union
  • American Meteorological Society
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  • 2020-2023  (4)
  • 2020-2022
  • 1980-1984
  • 1975-1979  (17)
  • 1960-1964
  • 2022  (4)
  • 2022  (4)
  • 1978  (9)
  • 1975  (8)
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  • 2020-2023  (4)
  • 2020-2022
  • 1980-1984
  • 1975-1979  (17)
  • 1960-1964
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  • 1
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    The influence of dissipated stresswork on the rupture of materials (1975)
    Elsevier
    In:  Bull., Open-File Rept., Selected Papers on Rheology, New York, Elsevier, vol. 4, no. 1, pp. 158-167, (ISBN 0080419208)
    Details
    Publication Date: 1975
    Keywords: Textbook of geophysics ; Rheology ; Rock mechanics ; Inelastic ; Fracture
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Seismic pattern recognition (1978)
    Elsevier
    In:  Professional Paper, Computer-aided seismic analysis and discrimination, Washington, D. C., Elsevier, vol. 16, no. 16, pp. 133-146, (ISBN 1-86239-165-3, vi + 330 pp.)
    Details
    Publication Date: 1978
    Keywords: Data analysis / ~ processing ; Discrimination ; Seismics (controlled source seismology) ; Pattern recognition ; Detectors
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    High-resolution group velocity analysis (1978)
    Elsevier
    In:  Bull., Polar Proj. OP-O3A4, Computer-Aided Seismic Analysis and Discrimination, London, Elsevier, vol. 16, no. 4, pp. 97-109, (ISBN 0080419208)
    Details
    Publication Date: 1978
    Keywords: Earthquake ; Seismics (controlled source seismology) ; Discrimination ; Velocity analysis
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    The blind octopus, Cirrothauma (1978)
    Nature Publishing Group
    In:  Nature, 275 (5680). pp. 547-549.
    Details
    Publication Date: 2019-06-20
    Description: THE rare deep-sea octopod Cirrothauma murrayi Chun 1910 was first described from a single specimen caught during the Michael Sars Expedition of 1910 (ref. 1). Until now it has been caught only four more times2. We describe here three specimens of this species that were recently caught during biological cruises of RRS Discovery (Fig. 1). All of these animals, including the Discovery ones, have been caught at depths of more than 1,500 m, except one that was dip-netted through the ice of the Arctic Ocean3.
    Type: Article , PeerReviewed
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  • 5
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    Digenetic Trematodes in Cephalopods (1975)
    Cambridge University Press
    In:  Journal of the Marine Biological Association of the United Kingdom, 55 (4). pp. 893-910.
    Details
    Publication Date: 2020-07-23
    Type: Article , PeerReviewed
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  • 6
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    Volcanics from the Sierra Leone Rise (1978)
    Nature Publishing Group
    In:  Nature, 275 (5680). pp. 536-538.
    Details
    Publication Date: 2018-01-22
    Description: THE Sierra Leone Rise, located in the east equatorial Atlantic, forms a discontinuous chain of seamounts as shallow as 2 km extending with a general NE–SW trend from near the Sierra Leone coast of Africa, to the St Paul fracture zone near the Mid-Atlantic Ridge (Fig. 1). The origin of this feature has remained a topic of discussion. Sheridan et al.1 have hypothesised that the Sierra Leone Rise is a volcanic structure formed at the beginning of the opening of the Atlantic in the early Cretaceous period. The twin features of the Sierra Leone and the Ceara Rises are probably of oceanic origin and were created 80 Myr ago or later in their present-day position with respect to Africa and South America2. The Atlantic ocean exhibits several similar aseismic structures which appear symmetrically oriented with respect to the mid-oceanic ridge, such as the Walvis–Rio Grande Rise and the Iceland Faeroes–Iceland Greenland Ridges. These structures are volcanic edifices having a composition similar to that found in their associated islands3–7. Deep sea drilling of the Ceara Rise8,9 penetrated a basaltic basement of the upper Cretaceous period (Maestrichtian) (Leg 39, Site 354). Similarly, a DSDP hole (Leg 41, Site 366) on the Sierra Leone Rise, penetrated sediments of the same period, without reaching basement10. We report here the discovery of alkali-rich volcanics in an area of the Sierra Leone Rise. The sediment overlying the rock fragments is aged ∼45 Myr.
    Type: Article , PeerReviewed
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  • 7
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    Molar Growth Yields, Respiration and Cytochrome Patterns of Beneckea natriegens when Grown at Different Medium Dissolved-oxygen Tensions (1975)
    Cambridge University Press
    In:  Journal of General Microbiology, 90 (2). pp. 237-246.
    Details
    Publication Date: 2020-07-24
    Description: The effect of medium dissolved-oxygen tension on the molar growth yield, respiration and cytochrome content of Beneckea natriegens in chemostat culture (D 0·37 hr-1) was examined. The molar growth yield (Y), the specific rate of oxygen (qo2) and glucose consumption, and the specific rate of carbon dioxide evolution were independent of the dissolved-oxygen tension above a critical value (〈 2 mmHg). However, the potential respiration rate increased with reduction in the dissolved-oxygen tension at values of the dissolved-oxygen tension well above the critical value. Changes in the cytochrome content occurred at dissolved-oxygen tensions well above the critical value. An increase in cytochrome c relative to cytochrome b was observed as the dissolved-oxygen tension was decreased. Reduction of the dissolved-oxygen tension to less than 1 mmHg caused a switch to fermentative metabolism shown by the apparent rise in Y o2 and decrease in the molar growth yield from glucose. At this point the potential respiration rate (q o2) increased to its highest value, while the cytochrome pattern reverted to that observed at dissolved-oxygen tensions above 96 mmHg. There appeared to be no correlation between cytochrome content, potential q o2, in situ q o2, and cyanide sensitivity of the organism at various dissolved-oxygen tensions.
    Type: Article , PeerReviewed
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  • 8
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    Bathymetry and stratigraphy of the northern Natal Valley (SW Indian Ocean): A preliminary account (1978)
    Elsevier
    In:  Marine Geology, 28 (1-2). pp. 89-106.
    Details
    Publication Date: 2016-04-12
    Description: Thick sediments (maximum of at least 4900 m) infill the Natal Valley, which lies between the coast of South Africa/Mozambique and the Mozambique Ridge. Eight physiographic provinces are recognised in the valley, and their boundaries can be related to well-defined sediment thickness or facies discontinuities within the basin infill. The acoustic stratigraphy of the area is established by reference to two regionally developed reflecting horizons, which, on the basis of previously published borehole and seismic data, are tentatively identified as mid-Cretaceous (McDuff) and mid-Cainozoic (Angus) hiatuses or important facies boundaries. Sedimentation began in the Natal Valley before mid-Cretaceous times and since then sediment dispersion has been strongly influenced by the disposition of large basement (? volcanic) highs: the approximately NE—SW Almirante Leite and Naudé ridges, and the larger N—S Mozambique Ridge. There is abundant evidence that sedimentation in the vicinity of these ridges has been current-controlled since at least mid-Cainozoic (Angus) times. The two main terrigenous sediment input points have been the Tugela and Limpopo rivers, which have large sediment cones adjacent to their mouths.
    Type: Article , PeerReviewed
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  • 9
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    The significance of the Mediterranean Sea to global climatology (1975)
    Elsevier
    In:  Ocean Management, 2 (4). pp. 323-332.
    Details
    Publication Date: 2016-07-19
    Description: Food production is affected by climate and by climate change. The indices for climate change may be recognized in long-term systematic observations of oceanic water columns at selected referential sites. The Mediterranean Sea, as part of the global oceanic circulation system, may be sensitive to climatic variation and may have an influence upon climate. The establishment of international referencestations for the Mediterranean area is suggested.
    Type: Article , PeerReviewed
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  • 10
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    The cephalopod statolithan-introduction to its form (1978)
    Cambridge University Press
    In:  Journal of the Marine Biological Association of the United Kingdom, 58 (03). p. 701.
    Details
    Publication Date: 2020-07-16
    Description: Terms, dimensions and ratios for statolith description are defined. The form of the calcareousstatoliths in the Teuthoidea, Sepiodea and Octopoda is described by reference to Loligo forbesi, Sepia officinalis and Eledone cirrosa. While statoliths change in form and size during the growth of a cephalopod, the adult form is often characteristic for a species, despite some variation. Description of statoliths is important in studies of the fossil remains of cephalopods lacking calcareous shells, and will probably become important in the taxonomy of living species, in food analysis of cephalopod predators and in the study of deep sea deposits.
    Type: Article , PeerReviewed
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