Microfossils in the upper quaternary sediments of the Norwegian Sea (biostratigraphy and paleoceanology)

Abstract

Diatom and nannoplankton microfossils in the samples of the surface bottom sediments and cores from the western part of the Norwegian Sea (64°–79°N) were studied. The abundance, distribution, taxonomic composition, and structure of the assemblages are determined by the productivity and temperature of the surface waters, by the distance from the shore, by the hydrological setting, and by the intensity of the supply of the Atlantic (from the south) and Arctic (from the north) waters to the Norwegian Sea. The repeated changes in the ecological structure of the diatom assemblages with time allowed us to distinguish five different ages and to estimate the changes in the paleoenvironment in the region under study during the past ∼19–21 ky. The nannofossil distribution is not universal over the entire area studied owing to the extreme northern location of the stations and low water temperatures. All the sediments examined refer to the Emiliania huxleyi zone of the Late Pleistocene-Holocene; in selected cases, narrower temperate and cold-water intervals were also recognized. The low species diversity and the poor preservation of nannofossils prove the dominating influence of the Arctic water masses.