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  • Wiley  (3)
  • 1
    In: Biotechnology and Bioengineering, Wiley, Vol. 115, No. 6 ( 2018-06), p. 1450-1464
    Abstract: Harnessing the metabolic potential of uncultured microbial communities is a compelling opportunity for the biotechnology industry, an approach that would vastly expand the portfolio of usable feedstocks. Methane is particularly promising because it is abundant and energy‐rich, yet the most efficient methane‐activating metabolic pathways involve mixed communities of anaerobic methanotrophic archaea and sulfate reducing bacteria. These communities oxidize methane at high catabolic efficiency and produce chemically reduced by‐products at a comparable rate and in near‐stoichiometric proportion to methane consumption. These reduced compounds can be used for feedstock and downstream chemical production, and at the production rates observed in situ they are an appealing, cost‐effective prospect. Notably, the microbial constituents responsible for this bioconversion are most prominent in select deep‐sea sediments, and while they can be kept active at surface pressures, they have not yet been cultured in the lab. In an industrial capacity, deep‐sea sediments could be periodically recovered and replenished, but the associated technical challenges and substantial costs make this an untenable approach for full‐scale operations. In this study, we present a novel method for incorporating methanotrophic communities into bioindustrial processes through abstraction onto low mass, easily transportable carbon cloth artificial substrates. Using Gulf of Mexico methane seep sediment as inoculum, optimal physicochemical parameters were established for methane‐oxidizing, sulfide‐generating mesocosm incubations. Metabolic activity required 〉 ∼40% seawater salinity, peaking at 100% salinity and 35 °C. Microbial communities were successfully transferred to a carbon cloth substrate, and rates of methane‐dependent sulfide production increased more than threefold per unit volume. Phylogenetic analyses indicated that carbon cloth‐based communities were substantially streamlined and were dominated by Desulfotomaculum geothermicum . Fluorescence in situ hybridization microscopy with carbon cloth fibers revealed a novel spatial arrangement of anaerobic methanotrophs and sulfate reducing bacteria suggestive of an electronic coupling enabled by the artificial substrate. This system: 1) enables a more targeted manipulation of methane‐activating microbial communities using a low‐mass and sediment‐free substrate; 2) holds promise for the simultaneous consumption of a strong greenhouse gas and the generation of usable downstream products; and 3) furthers the broader adoption of uncultured, mixed microbial communities for biotechnological use.
    Type of Medium: Online Resource
    ISSN: 0006-3592 , 1097-0290
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 1480809-2
    detail.hit.zdb_id: 280318-5
    SSG: 12
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  • 2
    In: Rapid Communications in Mass Spectrometry, Wiley, Vol. 30, No. 16 ( 2016-08-30), p. 1857-1864
    Type of Medium: Online Resource
    ISSN: 0951-4198
    Language: English
    Publisher: Wiley
    Publication Date: 2016
    detail.hit.zdb_id: 2002158-6
    detail.hit.zdb_id: 58731-X
    SSG: 11
    Location Call Number Limitation Availability
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2019
    In:  Rapid Communications in Mass Spectrometry Vol. 33, No. 7 ( 2019-04-15), p. 678-682
    In: Rapid Communications in Mass Spectrometry, Wiley, Vol. 33, No. 7 ( 2019-04-15), p. 678-682
    Abstract: Different thermal conversion reactor packings result in distinct δ 2 H values in nitrogen‐containing materials, such as bone collagen. An older ‘traditional’ glassy carbon packing method causes incomplete conversion of N‐containing samples into H 2 gas, resulting in altered δ 2 H values compared with the complete conversion of hydrogen obtained with a chromium‐packed reactor. Given that δ 2 H values from collagen are gaining importance in palaeoecological and archaeological studies, a determination of the relationship between δ 2 H values produced with a glassy‐carbon‐packed and a chromium‐packed reactor is needed. Methods We obtained δ 2 H values (normalized on the VSMOW‐SLAP scale) from both glassy‐carbon‐packed (GP) and chromium‐packed (Cr) reactor configurations from bone collagen ( n  = 231) from a variety of archaeological sites, using a High‐Temperature Conversion Elemental Analyzer (TC/EA) coupled to a Delta Plus XP isotope ratio mass spectrometer. Results δ 2 H values from both methods are linearly correlated (r 2  = 0.934) and yield the following interconversion equation, δ 2 H(Cr) = 1.054 δ 2 H(GP) + 11.6‰ (95% conf. slope 1.020–1.090, intercept 10.6–12.6), and a mean difference of δ 2 H(Cr) –  δ 2 H(GP) = 10.1‰ (1 sd 5.2, 1 se 0.3, n  = 231). Conclusions We recommend adopting this interconversion between δ 2 H values produced with a glassy‐carbon‐packed and chromium‐packed reactor for bone collagen only, with appropriate propagation of uncertainty.
    Type of Medium: Online Resource
    ISSN: 0951-4198 , 1097-0231
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2019
    detail.hit.zdb_id: 2002158-6
    detail.hit.zdb_id: 58731-X
    SSG: 11
    Location Call Number Limitation Availability
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