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Foraminifera, climatic change, and pollution

A study of late Holocene sediments in Drammensfiord, southeast Norway

Bibliographic Data

ID12267696
AuthorsElisabeth Alve (0000-0001-6692-7800, University of Oslo, corresponding author)
Year1991
Volume1
Issue3
Pages243-261
Publication date1991-10-01
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/095968369100100306
OpenAlexW2058886336
LanguageEN
Citations received6
References cited21

Benthic foraminifera are shown to reflect both natural (including climatic) and human- induced environmental alterations over the last 1500 years in Drammensfjord, Norway. Today, Drammensfjord is a 124 m deep, partly anoxic, hyposaline basin (salinity <32%o) separated from the adjoining Oslo Fjord by a sill at 10 m water depth. It has been affected by human-induced organic pollution for more than a century. Based on major faunal trends, sediment characteristics and concentrations of plant fragments and pollen grains, four environmental zones are distinguished. The faunal composition of zones 1-3 (before AD 500 to about AD 1850) reflects the natural environmental development from a period with frequent deep water renewals and diverse, calcareous dominated assemblages, to periods with increasing river flow which impeded effective deep water renewals, and gave rise to agglutinated assemblages of low diversity. Increasing human-induced organic flux over the last 130-140 years has elevated the redox cline. The general faunal responses as represented by zone 4 are: 1) development from agglutinated assemblages of zone 3 via assemblages dominated by Spiroplectammina biformis or Stainforthia fusiformis to the present anoxic, afaunal conditions, and 2) strongly increasing foraminiferal abundance with maximum values just prior to the afaunal intervals. The approach has considerable potential for differentiating the effects of pollution from the natural 'background

Anoxic waters · Benthic zone · Climate change · Environmental change · Foraminifera · Geochemistry · Holocene · Sediment · Sill · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Marine and environmental studies · Ecology · Geology · Oceanography · Paleontology

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    Open Access•Rienk H Smittenberg, Marianne Baas et al.•The Holocene•2005

  • Late Quaternary micropalaeontological record of a semi-enclosed marine basin, North Evoikos, central Aegean Sea

    Open Access•Hara Drinia, Assimina Antonarakou et al.•Quaternary International•2014

  • Late-Holocene climate and ecosystem history from Chesapeake Bay sediment cores, USA

    Open Access•Debra A Willard, Thomas M Cronin et al.•The Holocene•2003

  • Sewage history in the anoxic sediments of the fjord Nordåsvannet, western Norway

    Open Access•Matthias Paetzel, Hans Schrader et al.•The Holocene•1994

  • The impact of climate and shore-level displacement on the late-Holocene environmental development of Havstens Fjord and Koljö Fjord, Swedish west coast

    Open Access•Mikael Gustafsson, Kjell Nordberg•The Holocene•2002

  • Ecosystem turnover in an urbanized subtropical seascape driven by climate and pollution

    Open Access•Yuanyuan Hong, Moriaki Yasuhara et al.•Anthropocene•2021

  • Fundamentals of ecology

    Eugene Odum, Eugene Pleasants Odum et al.•Fundamentals of ecology•1959

  • The immigration and spread of spruce forest in Norway, traced by biostratigraphical studies and radiocarbon datings. A preliminary report

    Ulf Hafsten•Norsk Geografisk Tidsskrift -…•1985

  • Ur de sydsrenska skogarnas regionala historia under post-arktisk tid

    Lennart von Post•GFF•1924

Citations per year0.19
Citation span1994 - 2021 (28)
Highly citedNo

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