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  • 1
    Online Resource
    Online Resource
    American Society for Microbiology ; 1989
    In:  Applied and Environmental Microbiology Vol. 55, No. 5 ( 1989-05), p. 1234-1241
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 55, No. 5 ( 1989-05), p. 1234-1241
    Abstract: Microzonation of denitrification was studied in stream sediments by a combined O 2 and N 2 O microsensor technique. O 2 and N 2 O concentration profiles were recorded simultaneously in intact sediment cores in which C 2 H 2 was added to inhibit N 2 O reduction in denitrification. The N 2 O profiles were used to obtain high-resolution profiles of denitrification activity and NO 3 − distribution in the sediments. O 2 penetrated about 1 mm into the dark-incubated sediments, and denitrification was largely restricted to a thin anoxic layer immediately below that. With 115 μM NO 3 − in the water phase, denitrification was limited to a narrow zone from 0.7 to 1.4 mm in depth, and total activity was 34 nmol of N cm −2 h −1 . With 1,250 μM NO 3 − in the water, the denitrification zone was extended to a layer from 0.9 to 4.8 mm in depth, and total activity increased to 124 nmol of N cm −2 h −1 . Within most of the activity zone, denitrification was not dependent on the NO 3 − concentration and the apparent K m for NO 3 − was less than 10 μM. Denitrification was the only NO 3 − -consuming process in the dark-incubated stream sediment. Even in the presence of C 2 H 2 , a significant N 2 O reduction (up to 30% of the total N 2 O production) occurred in the reduced, NO 3 − -free layers below the denitrification zone. This effect must be corrected for during use of the conventional C 2 H 2 inhibition technique.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 1989
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    detail.hit.zdb_id: 1478346-0
    SSG: 12
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  • 2
    Online Resource
    Online Resource
    American Society for Microbiology ; 1988
    In:  Applied and Environmental Microbiology Vol. 54, No. 9 ( 1988-09), p. 2245-2249
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 54, No. 9 ( 1988-09), p. 2245-2249
    Abstract: The construction of a microsensor which can be used to measure O 2 and N 2 O simultaneously is described. The microsensor exhibited a linear response to both O 2 and N 2 O, and the response to N 2 O was independent of the O 2 concentration and vice versa. The N 2 O detection limit of a microsensor with a tip diameter of 20 μm was around 1 μmol liter −1 . The signals for O 2 and N 2 O were affected by hydrogen sulfide, but other interfering agents were not observed in the biofilms and sediments analyzed. Microprofiles of O 2 and N 2 O were measured in a biofilm which was exposed to acetylene to block the N 2 O reductase activity of denitrifying bacteria. O 2 penetrated about 0.5 mm into the biofilm and was not affected by acetylene, but the N 2 O concentration at 1.4 mm depth increased from 32 to 411 μmol liter −1 after the addition of the inhibitor. The shape of the N 2 O profile after the addition of acetylene showed that denitrification (denitrifying activity) was detectable in all anoxic layers of the biofilm.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 1988
    detail.hit.zdb_id: 223011-2
    detail.hit.zdb_id: 1478346-0
    SSG: 12
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  • 3
    In: Water Research, Elsevier BV, Vol. 23, No. 7 ( 1989-7), p. 867-871
    Type of Medium: Online Resource
    ISSN: 0043-1354
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1989
    detail.hit.zdb_id: 202613-2
    detail.hit.zdb_id: 1501098-3
    SSG: 14
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  • 4
    Online Resource
    Online Resource
    Elsevier BV ; 1989
    In:  Journal of Microbiological Methods Vol. 9, No. 2 ( 1989-2), p. 111-122
    In: Journal of Microbiological Methods, Elsevier BV, Vol. 9, No. 2 ( 1989-2), p. 111-122
    Type of Medium: Online Resource
    ISSN: 0167-7012
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1989
    detail.hit.zdb_id: 1483012-7
    SSG: 12
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  • 5
    Online Resource
    Online Resource
    American Society for Microbiology ; 1988
    In:  Applied and Environmental Microbiology Vol. 54, No. 1 ( 1988-01), p. 176-182
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 54, No. 1 ( 1988-01), p. 176-182
    Abstract: The potential to carry out oxygenic photosynthesis after prolonged burial below the photic zone was studied at 0.1-mm depth intervals in the thick, laminated Microcoleus chthonoplastes mats growing in Solar Lake, Sinai. The buried mat community lost about 20% of its photosynthetic potential with depth per annual layer down to 8- to 10-year-old layers at a 14-mm depth. In some of the older layers, below a 30-mm depth, light-dependent oxygen consumption which increased with increasing light intensity was observed. Possible mechanisms for this phenomenon are (i) pseudocyclic electron transport (Mehler reaction), (ii) interactions between respiratory electron transport and photosynthetic electron transport, (iii) photorespiration, and (iv) photooxidation.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 1988
    detail.hit.zdb_id: 223011-2
    detail.hit.zdb_id: 1478346-0
    SSG: 12
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  • 6
    Online Resource
    Online Resource
    Elsevier BV ; 1988
    In:  Applied Geochemistry Vol. 3, No. 1 ( 1988-1), p. 118-
    In: Applied Geochemistry, Elsevier BV, Vol. 3, No. 1 ( 1988-1), p. 118-
    Type of Medium: Online Resource
    ISSN: 0883-2927
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1988
    detail.hit.zdb_id: 1499242-5
    SSG: 13
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  • 7
    Online Resource
    Online Resource
    Informa UK Limited ; 1989
    In:  Ophelia Vol. 31, No. 1 ( 1989-12), p. 29-49
    In: Ophelia, Informa UK Limited, Vol. 31, No. 1 ( 1989-12), p. 29-49
    Type of Medium: Online Resource
    ISSN: 0078-5326
    Language: English
    Publisher: Informa UK Limited
    Publication Date: 1989
    detail.hit.zdb_id: 417080-5
    detail.hit.zdb_id: 2668673-9
    SSG: 12
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  • 8
    Online Resource
    Online Resource
    American Society for Microbiology ; 1986
    In:  Applied and Environmental Microbiology Vol. 52, No. 2 ( 1986-08), p. 225-233
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 52, No. 2 ( 1986-08), p. 225-233
    Abstract: Recently developed techniques involving opposed, gel-stabilized gradients of O 2 and H 2 S permit cultivation of a marine Beggiatoa strain as a chemolithoautotroph which uses gliding motility to precisely track the interface between H 2 S and O 2 . In the current study with microelectrodes, vertical profiles of H 2 , O 2 , and pH were measured in replicate cultures grown for various intervals. After an initial period of exponential biomass increase (doubling time, 11 h), linear growth prevailed throughout much of the time course. This H 2 S-limited growth was followed by a transition to stationary phase when the declining H 2 S flux was sufficient only to supply maintenance energy. During late-exponential and linear growth phases, the Beggiatoa sp. consumed a constant 0.6 mol of H 2 S for each 1.0 mol of O 2 , the ratio anticipated for balanced lithoautotrophic growth at the expense of complete oxidation of H 2 S to SO 4 2− . Over the entire range of conditions studied, this consumption ratio varied by approximately twofold. By measuring the extent to which the presence of the bacterial plate diminished the overlap of O 2 and H 2 S, we demonstrated that oxidation of H 2 S by Beggiatoa sp. is approximately 3 orders of magnitude faster than spontaneous chemical oxidation. By integrating sulfide profiles and comparing sulfide consumed with biomass produced, a growth yield of 8.4 g (dry weight) mol −1 of H 2 S was computed. This is higher than that found for sulfide-grown thiobacilli, indicating very efficient growth of Beggiatoa sp. as a chemoautotroph. The methods used here offer a unique opportunity to determine the yield of H 2 S-oxidizing chemolithoautotrophs while avoiding several problems inherent in the use of homogeneous liquid culture. Finally, by monitoring time-dependent formation of H 2 S profiles under anoxic conditions, we demonstrate a method for calculating the molecular diffusion coefficient of soluble substrates in gel-stabilized media.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 1986
    detail.hit.zdb_id: 223011-2
    detail.hit.zdb_id: 1478346-0
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  • 9
    Online Resource
    Online Resource
    Wiley ; 1985
    In:  Soil Science Society of America Journal Vol. 49, No. 3 ( 1985-05), p. 645-651
    In: Soil Science Society of America Journal, Wiley, Vol. 49, No. 3 ( 1985-05), p. 645-651
    Abstract: An oxygen microelectrode was modified to measure O 2 concentrations in wet aggregates of a silt loam soil. The microelectrode tip had an O 2 ‐permeable membrane opening 3 µm in diameter, and O 2 measurements could be made in as little as 0.1‐mm increments to a depth of 12 mm. When aggregates were incubated in air, steep O 2 gradients usually occurred over very small distances from the aggregate surface. The smallest aggregate exhibiting an anaerobic center had a radius of 4 mm, although small aggregates (radius ≤ 6 mm) were generally oxic. Larger aggregates (radius ≥ 10 mm) often had measureable anaerobic centers, with the exception of those from a native prairie soil which exhibited irregular O 2 profiles and had aerobic centers, apparently due to O 2 intrusion caused by old root channels. Oxygen profiles obtained in 45 degree increments around an aggregate circumference were used to construct contour maps of O 2 concentrations within the aggregate. Oxygen gradients were somewhat asymmetric, suggesting nonuniformly distributed sites of O 2 consumption. An average intra‐aggregate O 2 diffusion coefficient of 8.5 × 10 −6 cm 2 · s −1 was measured for water‐saturated aggregates. The radii of anaerobic centers within several aggregates, measured directly with the electrode, correlated with those calculated from a model of radial diffusion using measured respiration rates and the intra‐aggregate O 2 diffusion coefficient. Anaerobic centers were present in all aggregates that denitrified, but not all aggregates with anaerobic zones denitrified. The denitrification rate did not correlate with the size of the anaerobic zone, indicating that factors other than anaerobic volume contributed to the observed rates.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1985
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 10
    Online Resource
    Online Resource
    Wiley ; 1989
    In:  Limnology and Oceanography Vol. 34, No. 2 ( 1989-03), p. 474-478
    In: Limnology and Oceanography, Wiley, Vol. 34, No. 2 ( 1989-03), p. 474-478
    Type of Medium: Online Resource
    ISSN: 0024-3590
    Language: English
    Publisher: Wiley
    Publication Date: 1989
    detail.hit.zdb_id: 2033191-5
    detail.hit.zdb_id: 412737-7
    SSG: 12
    SSG: 14
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