Micron-scale mapping of sulfur cycling across the oxycline of a cyanobacterial mat: a paired nanoSIMS and CARD-FISH approach

被引:111
作者
Fike, David Andrew [1 ]
Gammon, Crystal Lynn [1 ]
Ziebis, Wiebke [2 ]
Orphan, Victoria Jeanne [1 ]
机构
[1] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[2] Univ So Calif, Dept Biol Sci, Los Angeles, CA 90089 USA
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
Guerrero Negro; in situ hybridization; microcoleus; nanoSIMS; sulfate-reducing bacteria; sulfur isotopes;
D O I
10.1038/ismej.2008.39
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The metabolic activities of microbial mats have likely regulated biogeochemical cycling over most of Earth's history. However, the relationship between metabolic activity and the establishment of isotopic geochemical gradients in these mats remains poorly constrained. Here we present a parallel microgeochemical and microbiological study of micron-scale sulfur cycling within hypersaline microbial mats from Guerrero Negro, Baja California Sur, Mexico. Dissolved sulfide within the mats was captured on silver discs and analyzed for its abundance and delta S-34 isotopic composition using high-resolution secondary ion mass spectrometry (nanoSIMS). These results were compared to sulfide and oxygen microelectrode profiles. Two-dimensional microgeochemical mapping revealed well-defined laminations in sulfide concentration (on scales from 1 to 200 mu m), trending toward increased sulfide concentrations at depth. Sulfide delta S-34 decreased from similar to+10%omicron to -20%omicron in the uppermost 3mm and oscillated repeatedly between -10%omicron and -30%omicron down to a depth of 8mm. These variations are attributed to spatially variable bacterial sulfate reduction within the mat. A parallel examination of the spatial distribution of known sulfate-reducing bacteria within the family Desulfobacteraceae was conducted using catalyzed reporter deposition fluorescence in situ hybridization. Significant concentrations of Desulfobacteraceae were observed in both oxic and anoxic zones of the mat and occurred in several distinct layers, in large aggregates and heterogeneously dispersed as single cells throughout. The spatial distribution of these microorganisms is consistent with the variation in sulfide concentration and isotopic composition we observed. The parallel application of the methodologies developed here can shed light on micron-scale sulfur cycling within microbially dominated sedimentary environments.
引用
收藏
页码:749 / 759
页数:11
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