Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes
- authored by
- Harald Strauss, Rebecca Bast, Anja Cording, David Diekrup, Artur Fugmann, Dieter Garbe-Schönberg, Andreas Lutter, Martin Oeser, Katharina Rabe, Debora Reinke, Barbara M.A. Teichert, Ulrike Westernströer
- Abstract
In this work, the biogeochemistry of marine sediments from the Kiel Bight, coastal SW Baltic Sea, is studied based on the abundance and isotopic composition of organic carbon and different forms of sedimentary sulphur. Active bacterial sulphate reduction, partly under sulphate-limiting conditions, is evident from paired δ 34S and δ 18O values of pore water sulphate. The resulting pore water sulphide is partly precipitated as acid-volatile iron sulphide and subsequently forms sedimentary pyrite, partly serves in later diagenetic sulphurisation of organic matter, or remains dissolved in the pore water, all evident from the respective δ 34S values. Microbial sulphate turnover is associated with an apparent isotopic fractionation between dissolved sulphate and dissolved sulphide (Δ 34S) that varies between 46 and 66‰.
- Organisation(s)
-
Institute of Mineralogy
- External Organisation(s)
-
University of Münster
Kiel University
- Type
- Article
- Journal
- Isotopes in Environmental and Health Studies
- Volume
- 48
- Pages
- 166-179
- No. of pages
- 14
- ISSN
- 1025-6016
- Publication date
- 03.2012
- Publication status
- Published
- Peer reviewed
- Yes
- ASJC Scopus subject areas
- Environmental Chemistry, General Environmental Science, Inorganic Chemistry
- Sustainable Development Goals
- SDG 14 - Life Below Water
- Electronic version(s)
-
https://doi.org/10.1080/10256016.2012.648930 (Access:
Unknown)