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  • 1
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    Radiolarians from the surface sediment in Lindåspollene, Western Norway (1973)
    Taylor & Francis
    In:  Sarsia, 53 (1). pp. 71-75.
    Details
    Publication Date: 2020-05-28
    Description: Sixtytwo species of radiolarians have been found in surface sediment in Lindåspollene. Some of these are common in deep-sea sediments from tropical and subtropical latitudes. These warm-water radiolarians are believed to have been introduced during a warm, postglacial period.
    Type: Article , PeerReviewed
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  • 2
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    Pleistocene palaeogeography of the Agulhas Bank (1972)
    Taylor & Francis
    In:  Transactions of the Royal Society of South Africa, 40 (3). pp. 155-165.
    Details
    Publication Date: 2020-05-04
    Description: Palaeogeographies of the Agulhas Bank for three low sea-level stages during the Pleistocene are presented (−140 m, −100 m and −50 m). Although they are specifically considered in relation to the last transgression (Flandrian, post-Weichsel/Würm), they are applicable to any of the previous glacial periods. In each case, the bedrock geology and expected superficial sediment cover are outlined, and general conclusions as to soil types, terrain, drainage, etc., are presented. The extended courses of local rivers in the Pleistocene are postulated from bathymetric and sedimentological data.
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  • 3
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    Cephalopoda from the eastern Mediterranean (1972)
    Taylor & Francis
    In:  Israel Journal of Zoology, 21 (2). pp. 83-97.
    Details
    Publication Date: 2021-04-29
    Description: Eighteen species of Cephalopoda collected off the coast of Israel and Cyprus are described and discussed.
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  • 4
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    Some Cretaceous ostracodal assemblages from the Agulhas Bank (South African continental margin) (1971)
    Taylor & Francis
    In:  Transactions of the Royal Society of South Africa, 39 (4). pp. 393-418.
    Details
    Publication Date: 2020-05-04
    Description: Four marine Cretaceous samples collected from the Agulhas Bank are discussed and their ostracodal assemblages described. Two of the samples are considered to be Lower Cretaceous, and the others Lower-Middle Senonian and Maastrichtian in age. Two new genera, twelve new species, and one new subspecies are described. Details of the foraminiferal assemblages are also given.
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