To the top

Page Manager: Webmaster
Last update: 9/11/2012 3:13 PM

Tell a friend about this page
Print version

Late Holocene palaeoprodu… - University of Gothenburg, Sweden Till startsida
To content Read more about how we use cookies on

Late Holocene palaeoproductivity changes: a multi-proxy study in the Norwegian Trench and the Skagerrak, North Sea.

Journal article
Authors Irina Polovodova Asteman
Bjørg Risebrobakken
Matthias Moros
Anna Binczewska
Sławomir Dobosz
Eystein Jansen
Joanna Sławińska
Małgorzata Bąk
Published in Boreas
Volume in press
ISSN 0300-9483
Publication year 2017
Published at
Language en
Keywords North Sea, , Baltic Sea, palaeoceanography, foraminifera, diatoms, sediment geochemistry
Subject categories Earth and Related Environmental Sciences, Climate Research, Environmental Sciences, Oceanography, Hydrology, Water Resources, Geosciences, Multidisciplinary


To detect climatic linkages between the Baltic Sea, the Skagerrak and the Nordic Seas, we present multi-proxy reconstructions covering the last 4500 years from 3 sediment cores taken in the Skagerrak and along the SW Norwegian margin. Foraminiferal assemblages at all three sites show a distinct change at ~1700 years BP, associated with a transition from absence and rare occurrence of Brizalina skagerrakensis during ~4500–2300 years BP to its subsequent abundance increase, suggesting a stronger influence of nutrient-rich water masses during the last ~1700 years. Increased nutrient availability, which likely stimulated higher primary productivity, is further supported by an increase in diatoms, total organic carbon and benthic foraminiferal species indicative of high productivity and carbon fluxes during the last ~1700 years as compared to ~4500–2300 years BP. The amplitude of the B. skagerrakensis signal is largest in the central Skagerrak and gradually becomes smaller towards the Norwegian Sea suggesting that the dominant source of the nutrient-rich water was the brackish outflow from the Baltic Sea. The generally lower abundances of planktonic foraminifera since ~1700 years BP support the hypothesis of less saline surface water conditions in the Skagerrak. These results agree with other studies, which suggest a stronger Baltic outflow over the last 1700 years coinciding with a general cooling, increased wintertime westerlies bringing more winter precipitation to northern Europe, increased river runoff and higher frequency of floods. The increase in outflow also occurs during deposition of laminated sediments in the deep Baltic Sea. Leakage of dissolved inorganic phosphorus from anoxic sediments, as well as enhanced erosion due to deforestation in combination with higher runoff from Norway, coastal upwelling and more vigorous frontal dynamics may all have contributed to higher nutrient availability of the adjacent Skagerrak during the last 1700 years BP as compared to ~4500–2300 years BP, when low productivity prevailed in the study area.

Page Manager: Webmaster|Last update: 9/11/2012

The University of Gothenburg uses cookies to provide you with the best possible user experience. By continuing on this website, you approve of our use of cookies.  What are cookies?