Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes

Research output: Contribution to journalArticleResearchpeer review

Authors

  • 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

Research Organisations

External Research Organisations

  • University of Münster
  • Kiel University
View graph of relations

Details

Original languageEnglish
Pages (from-to)166-179
Number of pages14
JournalIsotopes in Environmental and Health Studies
Volume48
Issue number1
Publication statusPublished - Mar 2012

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‰.

Keywords

    Baltic Sea, isotope biogeochemistry, isotope ecology, oxygen-18, pore water, sediments, sulphur turnover, sulphur-32, sulphur-33, sulphur-34

ASJC Scopus subject areas

Sustainable Development Goals

Cite this

Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes. / Strauss, Harald; Bast, Rebecca; Cording, Anja et al.
In: Isotopes in Environmental and Health Studies, Vol. 48, No. 1, 03.2012, p. 166-179.

Research output: Contribution to journalArticleResearchpeer review

Strauss, H, Bast, R, Cording, A, Diekrup, D, Fugmann, A, Garbe-Schönberg, D, Lutter, A, Oeser, M, Rabe, K, Reinke, D, Teichert, BMA & Westernströer, U 2012, 'Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes', Isotopes in Environmental and Health Studies, vol. 48, no. 1, pp. 166-179. https://doi.org/10.1080/10256016.2012.648930
Strauss, H., Bast, R., Cording, A., Diekrup, D., Fugmann, A., Garbe-Schönberg, D., Lutter, A., Oeser, M., Rabe, K., Reinke, D., Teichert, B. M. A., & Westernströer, U. (2012). Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes. Isotopes in Environmental and Health Studies, 48(1), 166-179. https://doi.org/10.1080/10256016.2012.648930
Strauss H, Bast R, Cording A, Diekrup D, Fugmann A, Garbe-Schönberg D et al. Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes. Isotopes in Environmental and Health Studies. 2012 Mar;48(1):166-179. doi: 10.1080/10256016.2012.648930
Download
@article{48f2d921d51348c9a8e6c0329e29e08a,
title = "Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes",
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‰.",
keywords = "Baltic Sea, isotope biogeochemistry, isotope ecology, oxygen-18, pore water, sediments, sulphur turnover, sulphur-32, sulphur-33, sulphur-34",
author = "Harald Strauss and Rebecca Bast and Anja Cording and David Diekrup and Artur Fugmann and Dieter Garbe-Sch{\"o}nberg and Andreas Lutter and Martin Oeser and Katharina Rabe and Debora Reinke and Teichert, {Barbara M.A.} and Ulrike Westernstr{\"o}er",
year = "2012",
month = mar,
doi = "10.1080/10256016.2012.648930",
language = "English",
volume = "48",
pages = "166--179",
journal = "Isotopes in Environmental and Health Studies",
issn = "1025-6016",
publisher = "Taylor and Francis Ltd.",
number = "1",

}

Download

TY - JOUR

T1 - Sulphur diagenesis in the sediments of the Kiel Bight, SW Baltic Sea, as reflected by multiple stable sulphur isotopes

AU - Strauss, Harald

AU - Bast, Rebecca

AU - Cording, Anja

AU - Diekrup, David

AU - Fugmann, Artur

AU - Garbe-Schönberg, Dieter

AU - Lutter, Andreas

AU - Oeser, Martin

AU - Rabe, Katharina

AU - Reinke, Debora

AU - Teichert, Barbara M.A.

AU - Westernströer, Ulrike

PY - 2012/3

Y1 - 2012/3

N2 - 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‰.

AB - 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‰.

KW - Baltic Sea

KW - isotope biogeochemistry

KW - isotope ecology

KW - oxygen-18

KW - pore water

KW - sediments

KW - sulphur turnover

KW - sulphur-32

KW - sulphur-33

KW - sulphur-34

UR - http://www.scopus.com/inward/record.url?scp=84858379241&partnerID=8YFLogxK

U2 - 10.1080/10256016.2012.648930

DO - 10.1080/10256016.2012.648930

M3 - Article

C2 - 22303924

AN - SCOPUS:84858379241

VL - 48

SP - 166

EP - 179

JO - Isotopes in Environmental and Health Studies

JF - Isotopes in Environmental and Health Studies

SN - 1025-6016

IS - 1

ER -

By the same author(s)