The Holocene history of the southwestern Baltic Sea as reflected in a sediment core from the Bornholm Basin
✍ Scribed by ELINOR ANDRÉN; THOMAS ANDRÉN; GUSTAV SOHLENIUS
- Book ID
- 109059843
- Publisher
- John Wiley and Sons
- Year
- 2000
- Tongue
- English
- Weight
- 595 KB
- Volume
- 29
- Category
- Article
- ISSN
- 0300-9483
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The occurrence of Mn carbonates in sapropelic sediments has been proposed to indicate that the host sediment originally accumulated under oxygenated bottomwaters. In the central Baltic Sea, Ca-rich rhodochrosite layers in sapropelic sediments have been related to in¯ows of oxic seawater from the Nor
I n three sediment cores from the Central Baltic Sea (Bornholm Basin, Gdansk Bay) correspondyng horizons with maximum abundance of remains of a limnetic fauna (Cladocera, Chironomidae) were found. These associations indicate the existence of an oligotrophic frcshwater hke. Ho\tever.. this horizon do