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
✦ LIBER ✦
On the calculation of release rates from stagnant basin sediments
✍ Scribed by David Dyrssen; Torbjörn Svensson
- Book ID
- 115813640
- Publisher
- Elsevier Science
- Year
- 1982
- Tongue
- English
- Weight
- 154 KB
- Volume
- 36
- Category
- Article
- ISSN
- 0009-2541
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