Sökning: "foraminifera"

Visar resultat 11 - 15 av 21 avhandlingar innehållade ordet foraminifera.

  1. 11. Stratigraphic and taxonomic-phylogenetic studies of Upper Cretaceous and paleogene planktonic Foraminifera

    Författare :William A. Berggren; Stockholms universitet; []
    Nyckelord :;

    Sammanfattning : .... LÄS MER

  2. 12. Ecological studies of the meiobenthic fauna, especially Foraminifera, in some Swedish estuaries

    Författare :Ingemar Olsson; Uppsala universitet; []
    Nyckelord :NATURAL SCIENCES; NATURVETENSKAP;

    Sammanfattning : .... LÄS MER

  3. 13. Upper Cretaceous - Lower Tertiary deep-see benthic foraminifera from the Walvis Ridge, South Atlantic Ocean : taxonomy, paleobiogeography, and paleoecology

    Författare :Joen G. V. Widmark; Uppsala universitet; []
    Nyckelord :NATURAL SCIENCES; NATURVETENSKAP;

    Sammanfattning : .... LÄS MER

  4. 14. Marine conditions in middle Sweden during the Late Weichselian and Early Holocene as inferred from foraminifera, Ostracoda and stable isotopes

    Författare :Kristian Schoning; Stockholms universitet; []
    Nyckelord :NATURVETENSKAP; NATURAL SCIENCES;

    Sammanfattning : .... LÄS MER

  5. 15. A multimethod approach to dating Quaternary sediments from the Arctic Ocean

    Författare :Gabriel West; Matthew O'Regan; Darrell Kaufman; Helena Alexanderson; Guillaume St-Onge; Stockholms universitet; []
    Nyckelord :NATURVETENSKAP; NATURAL SCIENCES; NATURVETENSKAP; NATURAL SCIENCES; Arctic Ocean; Amino Acid Geochronology; Optically Stimulated Luminescence Dating; Palaeomagnetism; maringeologi; Marine Geology;

    Sammanfattning : The marine sedimentary environment in the polar regions is different from the rest of the world’s oceans, as it is greatly influenced by the cryosphere. In the Arctic, sea ice and icebergs can transport vast amounts of sediments, delivered by extensive fluvial systems from the surrounding continents, which have been shaped by the waxing and waning of large terrestrial ice sheets during the Quaternary period. LÄS MER