1987
DOI: 10.1016/0378-1097(87)90021-8
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Structure of a microbiol mat at Great Sippewissett Marsh, Cape Cod, Massachusetts

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Cited by 29 publications
(41 citation statements)
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“…Nevertheless, the molecular approach used here has demonstrated the presence of this group in the studied ecosystem. Furthermore, P. aestuarii has been observed forming a thin layer in the microbial mats at Great Sippewissett salt marsh [8]. Green and brown Prosthecochloris have previously been detected and isolated in axenic cultures from Ebro Delta microbial mats [12].…”
Section: Green Sulfur Bacteria Diversity In Microbial Mats In the Ebrmentioning
confidence: 99%
“…Nevertheless, the molecular approach used here has demonstrated the presence of this group in the studied ecosystem. Furthermore, P. aestuarii has been observed forming a thin layer in the microbial mats at Great Sippewissett salt marsh [8]. Green and brown Prosthecochloris have previously been detected and isolated in axenic cultures from Ebro Delta microbial mats [12].…”
Section: Green Sulfur Bacteria Diversity In Microbial Mats In the Ebrmentioning
confidence: 99%
“…Anoxygenic phototrophic bacteria are of significance for the biogeochemical cycling of carbon and sulfur in stratified ecosystems like meromictic lakes and microbial mats [40,41,63–66]. In the chemocline of some lakes, phototrophic consortia contribute significantly (i.e.…”
Section: Implications For the Microbial Ecology Of Sulfuretamentioning
confidence: 99%
“…In other environments, availability of oxygen is often transient and forms steep chemical gradients in sediments due to high biological demand (Glud, ; Jørgensen & Revsbech, ). Such variation is a hallmark of both shallow marine environments, impacted by regular diel photosynthetic and/or tidal forcing (Dillon et al., ; Fike et al., ; Nicholson, Stolz, & Pierson, ) and marine hydrothermal systems, where advection can abruptly change on unpredictable temporal and spatial scales (Gilhooly et al., ; Houghton et al., ; Yücel et al., ). The plethora of micro‐organisms capable of oxidizing intermediate valence sulfur species (e.g., thiosulfate, sulfite, elemental sulfur) in pure culture (Giovannelli, d'Errico, Manini, Yakimov, & Vetriani, ; Habicht, Canfield, & Rethmeier, ; Sievert, Hügler, Taylor, & Wirsen, ) suggests high turnover rates for these compounds, despite the lack of field‐based evidence for a sustained, long‐term pool of intermediates within the sediments (Brune, Frenzel, & Cypionka, ; D'Hondt et al., ; Jørgensen, ; Luther et al., ).…”
Section: Introductionmentioning
confidence: 99%