Sulfate reduction related to the early diagenetic degradation of organic matter and “black spot” formation in tidal sandflats of the German Wadden Sea (southern North Sea): stable isotope (13C, 34S, 18O) and other geochemical results
- 1 November 1998
- journal article
- Published by Elsevier in Organic Geochemistry
- Vol. 29 (5-7) , 1517-1530
- https://doi.org/10.1016/s0146-6380(98)00124-7
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Sulfur isotope fractionation during experimental precipitation of iron(II) and manganese(II) sulfide at room temperaturePublished by Elsevier ,1998
- Stable Sulfur Isotope Effects Related to Local Intense Sulfate Reduction in a Tidal Sandflat (Southern North Sea): Results from Loading ExperimentsIsotopes in Environmental and Health Studies, 1997
- Fate of elemental sulfur in an intertidal sedimentFEMS Microbiology Ecology, 1996
- Decay of plant detritus in organic-poor marine sediment: Production rates and stoichiometry of dissolved C and N compoundsJournal of Marine Research, 1995
- Physiology and ecology of the sulphate‐reducing bacteriaJournal of Applied Bacteriology, 1990
- Oxygen isotope exchange between sulphate and water during bacterial reduction of sulphateChemical Geology: Isotope Geoscience section, 1989
- Relationships between bacteria and grain surfaces in intertidal sediments1Limnology and Oceanography, 1983
- The bacteria of the sulphur cyclePhilosophical Transactions of the Royal Society of London. B, Biological Sciences, 1982
- Mineralization of organic matter in the sea bed—the role of sulphate reductionNature, 1982
- Seasonal variation in H2S emission to the atmosphere from intertidal sediments in denmarkAtmospheric Environment (1967), 1982