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  • Other Sources  (21)
  • Academic Press
  • Annual Reviews
  • Nature Publishing Group
  • 2005-2009  (1)
  • 1990-1994  (15)
  • 1980-1984  (5)
  • 2006  (1)
  • 1992  (11)
  • 1990  (4)
  • 1980  (5)
  • 1
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    Fault Mechanics and Transport Properties of Rocks: A Festschrift in Honor of W. F. Brace (1992)
    Academic Press
    In:  London, 524 pp., Academic Press, vol. special paper 359, ix + 190 pp., no. 2, pp. 527-553, (ISBN 0-8137-2359-0)
    Details
    Publication Date: 1992
    Keywords: Textbook of geophysics ; Fracture ; Rock mechanics ; Fluids ; Friction
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Image Reconstruction from Projections - the Fundamentals of Computerized Tomography (1980)
    Academic Press
    In:  New York, Academic Press, vol. III/12, Supplement to III/4, no. XVI:, pp. 1-14, (ISBN 0-87590-299-5 (soft cover))
    Details
    Publication Date: 1980
    Keywords: Inversion
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Tsunamis (1992)
    Academic Press
    In:  Bull., Open-File Rept., Encyclopedia of Earth System Science, London, Academic Press, vol. 231, no. 16, pp. 389-397, (ISBN 1-86239-165-3, vi + 330 pp.)
    Details
    Publication Date: 1992
    Keywords: Tsunami(s)
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Waves in Layered Media (1980)
    Academic Press
    In:  New York, Academic Press, vol. 173, pp. 503, (ISBN 0-444-50968-2)
    Details
    Publication Date: 1980
    Keywords: Textbook of geophysics ; Seismology ; Seismics (controlled source seismology)
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Brace-Goetze strength profiles, the partitioning of strike-slip and thrust faulting at zones of oblique convergence and the stress-heat flow paradox of the San Andreas fault (1992)
    Academic Press
    In:  Bull., Polar Proj. OP-O3A4, Fault Mechanics and Transport Properties of Rocks: A Festschrift in Honor of W. F. Brace, London, Academic Press, vol. 4, no. Subvol. b, pp. 435-459, (ISBN 0080419208)
    Details
    Publication Date: 1992
    Keywords: Geothermics ; Seismicity ; Strength ; Source parameters ; Stress ; Fault zone
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    Natural habitat of coelacanths (1990)
    Nature Publishing Group
    In:  Nature, 346 (6282). pp. 323-324.
    Details
    Publication Date: 2017-08-10
    Type: Article , PeerReviewed
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  • 7
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    Diets and dietary segregation of crested penguins (Eudyptes) (1990)
    Academic Press
    In:  In: Penguin Biology. Academic Press, pp. 131-156.
    Details
    Publication Date: 2017-02-27
    Type: Book chapter , PeerReviewed
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  • 8
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    Octopod 'ballooning' response (1992)
    Nature Publishing Group
    In:  Nature, 356 (6366). p. 199.
    Details
    Publication Date: 2017-03-14
    Type: Article , PeerReviewed
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  • 9
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    Erosion and Weathering (1992)
    Academic Press
    In:  In: Encyclopedia of Earth System Science. , ed. by Nierenberg, W. A. Academic Press, San Diego, pp. 177-185.
    Details
    Publication Date: 2018-02-06
    Type: Book chapter , NonPeerReviewed
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  • 10
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    Coelacanth tissue bank (1992)
    Nature Publishing Group
    In:  Nature, 357 (6374). p. 105.
    Details
    Publication Date: 2017-08-03
    Type: Article , NonPeerReviewed
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  • 11
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    14 The Phosphorus Cycle (1992)
    Academic Press
    In:  In: Global Biogeochemical Cycles. International geophysics series, 50 . Academic Press, London, pp. 301-315.
    Details
    Publication Date: 2018-06-01
    Description: This chapter discusses the phosphorus cycle. Phosphorus is one of the most important elements on Earth. It participates in or controls many of the biogeochemical processes occurring in the biosphere. Phosphate also plays a central role in the transmission and control of chemical energy within the cells, primarily, via the hydrolysis of the terminal phosphate ester bond of the adenosine triphosphate (ATP) molecule. The cycling of P is closely linked with biological processes. The chemical forms in which P is present in the environment is discussed. The processes that control its distribution in terrestrial, aquatic, and oceanic systems are described in the chapter. The chapter defines the major P reservoirs on the Earth's surface and the rate at which P is exchanged among these reservoirs. The chapter discusses the sub-global phosphorus cycles that includes freshwater terrestrial ecosystems, and the oceanic system and describes the global phosphorus cycle.
    Type: Book chapter , NonPeerReviewed
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  • 12
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    Particulate organic carbon flux in the oceans-surface productivity and oxygen utilization (1980)
    Nature Publishing Group
    In:  Nature, 288 (5788). pp. 260-263.
    Details
    Publication Date: 2016-03-01
    Description: Organic detritus passing from the sea surface through the water column to the sea floor controls nutrient regeneration, fuels benthic life and affects burial of organic carbon in the sediment record. Particle trap systems have enabled the first quantification of this important process. The results suggest that the dominant mechanism of vertical transport is by rapid settling of rare large particles, most likely of faecal pellets or marine snow of the order of 〉200 μm in diameter, whereas the more frequent small particles have an insignificant role in vertical mass flux4–6. The ultimate source of organic detritus is biological production in surface waters of the oceans. I determine here an empirical relationship that predicts organic carbon flux at any depth in the oceans below the base of the euphotic zone as a function of the mean net primary production rate at the surface and depth-dependent consumption. Such a relationship aids in estimating rates of decay of organic matter in the water column, benthic and water column respiration of oxygen in the deep sea and burial of organic carbon in the sediment record.
    Type: Article , PeerReviewed
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  • 13
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    The Cenozoic palaeoenvironment of the Arctic Ocean (2006)
    Nature Publishing Group
    In:  Nature, 441 . pp. 601-605.
    Details
    Publication Date: 2019-07-03
    Description: The history of the Arctic Ocean during the Cenozoic era (0–65 million years ago) is largely unknown from direct evidence. Here we present a Cenozoic palaeoceanographic record constructed from 〉400 m of sediment core from a recent drilling expedition to the Lomonosov ridge in the Arctic Ocean. Our record shows a palaeoenvironmental transition from a warm 'greenhouse' world, during the late Palaeocene and early Eocene epochs, to a colder 'icehouse' world influenced by sea ice and icebergs from the middle Eocene epoch to the present. For the most recent approx14 Myr, we find sedimentation rates of 1–2 cm per thousand years, in stark contrast to the substantially lower rates proposed in earlier studies; this record of the Neogene reveals cooling of the Arctic that was synchronous with the expansion of Greenland ice (approx3.2 Myr ago) and East Antarctic ice (approx14 Myr ago). We find evidence for the first occurrence of ice-rafted debris in the middle Eocene epoch (approx45 Myr ago), some 35 Myr earlier than previously thought; fresh surface waters were present at approx49 Myr ago, before the onset of ice-rafted debris. Also, the temperatures of surface waters during the Palaeocene/Eocene thermal maximum (approx55 Myr ago) appear to have been substantially warmer than previously estimated. The revised timing of the earliest Arctic cooling events coincides with those from Antarctica, supporting arguments for bipolar symmetry in climate change.
    Type: Article , PeerReviewed
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  • 14
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    Diminishing oxygen (1992)
    Nature Publishing Group
    In:  Nature, 358 (6389). pp. 710-711.
    Details
    Publication Date: 2016-06-10
    Type: Article , PeerReviewed
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  • 15
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    Interhemispheric transport of carbon dioxide by ocean circulation (1992)
    Nature Publishing Group
    In:  Nature, 356 (6370). pp. 587-589.
    Details
    Publication Date: 2016-06-10
    Description: ALTHOUGH anthropogenic emissions of carbon dioxide have today created a greater atmospheric CO2concentration in the Northern than in the Southern Hemisphere, a comparison of interhemispheric CO2 profiles from 1980 and 1962 led Keeling and Heimann1,2 to conclude that, before the Industrial Revolution, natural CO2 sources and sinks acted to set up a reverse (south to north) gradient which drove about one gigatonne of carbon each year through the atmosphere from the Southern to the Northern Hemisphere. At steady state, this flux must have been balanced by a counter flow of carbon from north to south through the ocean. Here we present a means to estimate this natural flux by a separation of oceanic carbon anomalies into those created by biogenic processes and those created by CO2 exchange between the ocean and atmosphere. We find that before the Industrial Revolution, deep water formed in the northern Atlantic Ocean carried about 0.6 gigatonnes of carbon annually to the Southern Hemisphere, providing support for Keeling and Heimann's proposal. The existence of this oceanic carbon pump also raises questions about the need for a large terrestrial carbon sink in the Northern Hemisphere, as postulated by Tans et al.3, to balance the present global carbon budget.
    Type: Article , PeerReviewed
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  • 16
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    Upset for Milankovitch theory (1992)
    Nature Publishing Group
    In:  Nature, 359 (6398). pp. 779-780.
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    Publication Date: 2016-06-10
    Type: Article , PeerReviewed
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  • 17
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    Deep ocean circulation puzzle (1992)
    Nature Publishing Group
    In:  Nature, 356 (6372). pp. 744-746.
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    Publication Date: 2018-03-02
    Type: Article , PeerReviewed
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  • 18
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    Volatiles in submarine glasses as a discriminant of tectonic origin: application to the Troodos ophiolite (1990)
    Nature Publishing Group
    In:  Nature, 343 (6254). pp. 159-161.
    Details
    Publication Date: 2019-05-08
    Description: ISOTOPE ratios and concentrations of incompatible trace elements are remarkably successful in discriminating the tectonic origin and magmatic source components for basalts1–5. But problems remain with discriminating the tectonic origin of some tholeiites, especially where field relations and other geological evidence are ambiguous. For example, the tectonic origin of basalts from the Troodos ophiolite (Cyprus) has been debated for several decades. Most workers have been unable to distinguish between an island-arc and/or back-arc origin for the ophiolite6–8. Here we use volatile, K2O and TiO2 contents from ∼250 fresh submarine volcanic glasses to discriminate between tholeiites from different tectonic regimes. K2O÷H2O ratios are lower (〈0.70) in spread ing-centre glasses than in those from island arcs and intraplate oceanic islands. Back-arc-basin basalts can generally be separated from mid-ocean-ridge basalts by their high H2O contents. Using this information, we show that some fresh glasses from the Troodos ophiolite have a clear back-arc-basin affinity.
    Type: Article , PeerReviewed
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  • 19
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    The first fossil cephalopod statoliths to be described from Europe (1980)
    Nature Publishing Group
    In:  Nature, 287 (5783). pp. 628-630.
    Details
    Publication Date: 2016-11-15
    Description: Statoliths of cephalopods are small, hard calcareous stones which lie within the cartilaginous skulls of octopods, sepioids and teuthoids1. Fossil statoliths, clearly belonging to genera which are alive today, have previously been described from 11 Cenozoic deposits spanning from the Eocene to the Pleistocene in North America2–5. Such statoliths are of particular interest because they provide a means of studying the evolution of living cephalopod groups which have no calcareous shells, including the cosmopolitan and numerous teuthoids and octopods. Here, the first cephalopod statoliths to be recognized in European deposits are described and identified as Loligo sp. They are compared with the North American fossil Loligo species and statoliths removed from the two living Loligo species of Europe.
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  • 20
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    Sirius red-collagen interaction: A method for the measurement of collagen and bacterial collagenase activity (1980)
    Academic Press
    In:  Biochemistry International, 1 (5). pp. 455-462.
    Details
    Publication Date: 2018-11-20
    Description: The dye Sirius Red binds to collagens types I, II and III, giving red-colored products in which the bound dye is proportional to the amount of collagen present. Several other proteins also bind Sirius Red, in amounts 30-50 times less than collagen, on a weight basis. Because of this preferential binding to collagen, Sirius Red may be used for its quantitation even in presence of other proteins, as it occurs, for instance, in the culture medium of various types of cultured cells. When incubated at room temperature with bacterial collagenase, the Sirius Red-collagen complex is rapidly degraded while it is resistant to mammalian collagenase, trypsin and pepsin. Thus, the release of the bound dye may be used for quantitation of bacterial collagenase activity.
    Type: Article , PeerReviewed
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  • 21
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    Phytoplankton nutrient competition - from laboratory to lake (1990)
    Academic Press
    In:  In: Perspectives on plant competition. , ed. by Grace, J. B. and Tilman, D. Academic Press, San Diego, USA, pp. 193-213.
    Details
    Publication Date: 2019-08-07
    Type: Book chapter , NonPeerReviewed
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