High-resolution measurements of sulphur isotope variations in sediment pore-waters by laser ablation multicollector inductively coupled plasma mass spectrometry

被引:19
作者
Widerlund, Anders [1 ]
Nowell, Geoff M. [2 ]
Davison, William [1 ]
Pearson, D. Graham [2 ]
机构
[1] Univ Lancaster, Dept Environm Sci, Lancaster Environm Ctr LEC, Lancaster LA1 4YQ, England
[2] Univ Durham, Dept Earth Sci, Sci Labs, Durham DH1 3LE, England
基金
英国自然环境研究理事会;
关键词
Diffusive gradients in thin films; Sediment microniches; Bacterial sulphate reduction; Sulphur isotope fractionation; Esthwaite Water; SULFATE-REDUCING BACTERIA; DIFFUSIVE GRADIENTS; THIN-FILMS; IN-SITU; SIMULTANEOUS RELEASE; MARINE-SEDIMENTS; SULFIDE; FRACTIONATION; MICRONICHES; ZN;
D O I
10.1016/j.chemgeo.2011.10.018
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A novel combination of the technique of diffusive gradients in thin films (DGT) and laser ablation high-resolution multicollector inductively coupled plasma mass spectrometry was developed to study sulphur isotope variations of dissolved pore-water sulphide in freshwater and marine sediments. The technique enables two-dimensional mapping of isotopic variations (delta S-34) in dissolved sulphide captured as solid Ag2S in DGT polyacrylamide gels. Measurements can be performed at a spatial resolution (similar to 100 pm) relevant to microbiological processes and formation of individual iron sulphide grains in surface sediments. Values of delta S-34 measured in BaSO4-DGT gel isotope standards (delta S-34 = 9.28 +/- 036 parts per thousand to 933 +/- 0.57 parts per thousand) are within 1 parts per thousand of the accepted value determined with conventional analytical techniques (delta S-34 = 10.13 +/- 0.29 parts per thousand). Sulphur isotope measurements were performed in sediments from a eutrophic lake (Esthwaite Water, UK) contained in laboratory mesocosms. Bacterial sulphate reduction and sulphide formation in this sediment are predominantly localized to discrete, mm-sized microniches, where oxidation of labile organic matter such as fresh algae and faecal pellets drives the reduction of sulphate. The results emphasize the importance of microniches as localized, highly dynamic reaction sites in sediments, where significant shifts in delta S-34 of up to +20 parts per thousand relative to the local background were measured across microniches. The improved spatial resolution for pore-water sulphur isotope measurements, compared to that of conventional sampling and analytical techniques, is essential for improving our understanding of the global biogeochemical cycling of sulphur as well as trace metal-sulphide interactions in modern sediments. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:278 / 285
页数:8
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