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1 n a 2-coordinated Hg(Mem-RS)(2) structure in Geobacter.
2 availability of Fe(III) and the abundance of Geobacter.
4 ng, shows that bacteria related to the genus Geobacter, a known and commonly found ARB, dominate only
5 +/- 0.1, and 25.6 +/- 0.1, respectively, for Geobacter and 39.2 +/- 0.2, 38.2 +/- 0.1, and 25.7 +/- 0
6 osts a large population of current-producing Geobacter and attains a current density of 3 mA cm(-2) s
10 re selective to electroactive microbes (e.g. Geobacter) and more conducive for electroactive biofilm
12 s and were dominated by Deltaproteobacteria, Geobacter, and to a lesser extent, Clostridia, while low
13 icroorganisms (and relative abundances) were Geobacter anodireducens (89.3%) and Thauera sp. (5.5%).
15 ceptors and chemotaxis-like gene clusters of Geobacter appear to be responsible for a diverse set of
17 ntrophic interactions between fermenters and Geobacter at the anode and ferementers and hydrogenotrop
19 tu stimulation of Fe(III) oxide reduction by Geobacter bacteria leads to the concomitant precipitatio
20 ere are multiple types of redox cofactors in Geobacter biofilms spanning a range in oxidation potenti
22 zed with this capability were Shewanella and Geobacter, both reported to couple their growth to the r
25 ntrast, the enhanced decay model predicted a Geobacter cell density that was too low to allow recover
26 amount of current generated by an individual Geobacter cell in the absence of a biofilm and highlight
30 like the single gene cluster of E. coli, the Geobacter clusters are not all located near the flagella
31 monstrate a previously unrecognized role for Geobacter conductive pili in the extracellular reduction
35 cent discovery of a novel species Candidatus Geobacter eutrophica with the genetic potential of IHT a
36 16S-rDNA and -rRNA sequences showed that the Geobacter genus was less than 30% of the community of th
37 angstrom-resolution crystal structure of the Geobacter Hypr GGDEF domain was determined to understand
38 pili all appear important for the growth of Geobacter in changing environments and for electricity p
39 eatment include Legionella, Escherichia, and Geobacter in the lab-scale system and Mycobacterium, Sph
42 ted samples revealed the rapid enrichment of Geobacter-like environmental strains with strong similar
44 g Dehalococcoides mccartyi (Dhc) strains and Geobacter lovleyi strain SZ (GeoSZ), or inoculated with
45 -3.6 per thousand +/- 0.1 per thousand with Geobacter lovleyi strain SZ; -9.1 per thousand +/- 0.6 p
46 ntact cells of Sulfurospirillum multivorans, Geobacter lovleyi, Desulfuromonas michiganensis, Desulfi
47 c Methanothrix concilii, and exoelectrogenic Geobacter lovleyi, were successfully recovered for the r
48 we report that a bacterial SMUG1 ortholog in Geobacter metallireducens (Gme) and the human SMUG1 enzy
50 that laboratory evolution of a coculture of Geobacter metallireducens and Geobacter sulfurreducens m
51 mechanisms in the syntrophic association of Geobacter metallireducens and Geobacter sulfurreducens.
53 by the electrosyntrophic interaction between Geobacter metallireducens and Rhodopseudomonas palustris
54 enoyl-coenzyme A intermediate as observed in Geobacter metallireducens and Syntrophus aciditrophicus.
55 lity and key enabling metabolic machinery of Geobacter metallireducens GS-15 to carry out CO2 fixatio
57 GHI](2) complex from the anaerobic bacterium Geobacter metallireducens harboring 4 tungsten, 4 zinc,
60 investigated in resting cell suspensions of Geobacter metallireducens strain GS-15, a model Fe(III)-
61 inone-2,6-disulfonate (AH2QDS), (ii) resting Geobacter metallireducens strain GS-15, and (iii) a comb
64 GAC, they stimulated DIET in co-cultures of Geobacter metallireducens with Geobacter sulfurreducens
65 trons from electron donating organisms (eg., Geobacter metallireducens) to electron accepting organis
66 Here we report that another Fe(III)-reducer, Geobacter metallireducens, has an alternative strategy f
67 Using the exoelectrogenic nitrate reducer Geobacter metallireducens, the critical conditions contr
68 An orthologous frdCAB operon was present in Geobacter metallireducens, which cannot grow with fumara
71 g-range extracellular electron transport via Geobacter nanowires, and what mechanisms control this re
75 aining the observed conductive properties of Geobacter pili are a valuable tool to guide further inve
76 ltistep hopping as the mechanism that allows Geobacter pili to function as protein nanowires between
77 ment, theoretical energy-minimized models of Geobacter pili were constructed with a previously descri
78 eterologously expressed abundant, conductive Geobacter pili when grown aerobically in liquid culture.
79 em, we monitored a carbon-stimulated in situ Geobacter population while iron reduction was occurring,
80 ntity, and 2) all biofilms were dominated by Geobacter populations, but the composition of -CH3-assoc
81 easurements suggest high carbon flux through Geobacter respiratory pathways, and the synthesis of ana
82 ) oxide reduction requires the expression of Geobacter's conductive pili, we evaluated their contribu
83 fferential gene expression analysis revealed Geobacter's transcriptional regulations to express more
84 enzyme from Geobacter sulfurreducens and the Geobacter S134P/V135K double mutant, which have been sho
85 SAPs based on 16S rRNA gene sequencing were Geobacter, Smithella and Syntrophobacter, but their rela
88 Here, we describe the isolation of a new Geobacter sp. strain Cd1 from a Cd-contaminated field si
90 nterspecies electron transfer (DIET) between Geobacter species and Methanosaeta species is an alterna
91 nities, the direct electron exchange between Geobacter species and Methanosaeta species might be an i
95 the electrically conductive pili (e-pili) of Geobacter species are of interest because of the importa
97 n (FISH) further confirmed that the dominant Geobacter species enriched belonged to Geobacter metalli
99 ached to the electrically conductive pili of Geobacter species in a manner reminiscent of the associa
103 insoluble electron acceptor may explain why Geobacter species predominate over other Fe(III) oxide-r
104 nt new insights into the mechanisms by which Geobacter species regulate their central metabolism unde
105 P in numerous Deltaproteobacteria, including Geobacter species that use extracellular insoluble metal
108 ed motility is considered to be critical for Geobacter species to locate fresh sources of Fe(III) oxi
110 on end products by exoelectrogens (typically Geobacter species) relieves feedback inhibition for the
111 ic compounds coupled to Fe(III) reduction in Geobacter species, but Fe(III) reduction with NADPH as t
112 -reducing bacteria, including Shewanella and Geobacter species, can reduce a wide range of high valen
114 The fgrM gene in the most studied strain of Geobacter species, Geobacter sulfurreducens strain DL-1,
122 rrent state of knowledge from Shewanella and Geobacter, specifically focusing on transfer across the
125 ould complement targeted knockout studies in Geobacter spp. and identify novel genes involved in this
126 ependent AOM in a biofilm anode dominated by Geobacter spp. and Methanobacterium spp. using carbon-fi
128 In this study, we confirm that 6-week-old Geobacter spp. dominated biofilms are by far more active
130 N2 and not facultative nitrate reduction by Geobacter spp. might be the primary response to perturba
131 bacterium spp. may work synergistically with Geobacter spp. to allow AOM, likely by employing interme
132 (13) C-acetate selected for ArrA related to Geobacter spp. whereas (13) C-lactate selected for ArrA
134 e an immediate influence on the stability of Geobacter spp.-dominated biofilms and may limit their pr
136 wo methyl-accepting chemotaxis proteins from Geobacter sulfurreducens (encoded by genes GSU0935 and G
137 -like conductivity in films of the bacterium Geobacter sulfurreducens and also in pilin nanofilaments
138 nserved among two species of Geobacteraceae, Geobacter sulfurreducens and Geobacter metallireducens.
139 cens) to electron accepting organisms (e.g., Geobacter sulfurreducens and Methanosarcina barkeri).
141 synergistic metabolisms of the exoelectrogen Geobacter sulfurreducens and the bacterium Clostridium c
142 lysis cell (MEC) driven by the exoelectrogen Geobacter sulfurreducens and the CBP bacterium Cellulomo
143 ly PFV to the recently described enzyme from Geobacter sulfurreducens and the Geobacter S134P/V135K d
146 ffort to mimic the T4P of the metal-reducing Geobacter sulfurreducens bacterium led to the design of
147 llular filaments in anaerobic bacteria, with Geobacter sulfurreducens being used as a model system.
150 with excess H(2), Shewanella oneidensis and Geobacter sulfurreducens both solubilized <0.001% of 0.5
152 ale protein wires harvested from the microbe Geobacter sulfurreducens can generate continuous electri
158 e we report that a pilus-deficient mutant of Geobacter sulfurreducens could not reduce Fe(iii) oxides
160 ngle-bacterium level current measurements of Geobacter sulfurreducens DL-1 to elucidate the fundament
161 t, for the first time, SERS of the bacterium Geobacter sulfurreducens facilitated by colloidal gold p
162 tum rate theory with a discussion focused on Geobacter sulfurreducens films as a reference standard o
163 crofluidic reactor that physically separates Geobacter sulfurreducens from the Mn(IV) mineral birness
166 d their contribution to uranium reduction in Geobacter sulfurreducens grown under pili-inducing or no
169 nome sequences for Shewanella oneidensis and Geobacter sulfurreducens has provided numerous new biolo
171 tive bacteria Shewanella oneidensis MR-1 and Geobacter sulfurreducens have developed electron transfe
177 dissimilatory Fe(III)-reducing microorganism Geobacter sulfurreducens is predicted to code for a smal
178 ng it with an electron transport specialist, Geobacter sulfurreducens KN400 (KN400), an adapted strai
180 a coculture of Geobacter metallireducens and Geobacter sulfurreducens metabolizing ethanol favored th
181 hird extracellular filament, formed from the Geobacter sulfurreducens octaheme cytochrome, OmcZ.
182 fate of As(V) during microbial reduction by Geobacter sulfurreducens of Fe(III) in synthetic arsenic
183 o-cultures of Geobacter metallireducens with Geobacter sulfurreducens or Methanosarcina barkeri in wh
184 Hg methylation by an iron-reducing bacterium Geobacter sulfurreducens PCA and a sulfate-reducing bact
185 ongrowing cultures of the anaerobic bacteria Geobacter sulfurreducens PCA and Desulfovibrio desulfuri
186 nsively studied Hg(II) methylating bacteria: Geobacter sulfurreducens PCA and Desulfovibrio desulfuri
192 The metallic-like electrical conductivity of Geobacter sulfurreducens pili has been documented with m
193 with the electrogenic and acetate-consuming Geobacter sulfurreducens produced electricity from PET o
194 We show that the iron reducing bacterium Geobacter sulfurreducens produces and exports appreciabl
195 discovered that the environmental bacterium Geobacter sulfurreducens produces cAG and uses a subset
196 um) transport of electrons along networks of Geobacter sulfurreducens protein filaments, known as mic
198 electrodes by the Fe(III)-reducing anaerobe Geobacter sulfurreducens requires proper expression of r
203 he most studied strain of Geobacter species, Geobacter sulfurreducens strain DL-1, is truncated by a
204 ria, Anaeromyxobacter dehalogenans strain K, Geobacter sulfurreducens strain PCA, and Shewanella putr
205 cing the sludge with humic acids), and (iii) Geobacter sulfurreducens to produce electrons from aceta
206 only up to 1 to 2 nanometers via tunneling, Geobacter sulfurreducens transports respiratory electron
208 , is vital during the growth and survival of Geobacter sulfurreducens under conditions typically enco
210 e structure of a cytochrome c(7) (PpcA) from Geobacter sulfurreducens was determined by X-ray diffrac
211 dium(II) reduction to Pd(0) nanoparticles by Geobacter sulfurreducens was explored under conditions o
213 cupancy or functionality, and that NifH from Geobacter sulfurreducens was more resistant to O(2) expo
215 tive appendages from the anaerobic bacterium Geobacter sulfurreducens were first observed two decades
216 of electron transport in actively respiring Geobacter sulfurreducens wild type biofilms using interd
217 y visualize charge propagation along pili of Geobacter sulfurreducens with nanometre resolution and u
219 naerobic Fe(III)-reducing bacterial species (Geobacter sulfurreducens) and the enzymatic reduction of
223 al structures of the 1,004-residue PutA from Geobacter sulfurreducens, along with determination of th
225 ysR family regulators of a model prokaryote, Geobacter sulfurreducens, and employed phylogenetic tree
226 ytochrome shares 80% identity with PpcA from Geobacter sulfurreducens, but their redox properties are
227 tris TIE-1 and the Fe(III)-reducing bacteria Geobacter sulfurreducens, comparing magnetite nanopartic
228 ype cytochrome abundant in Fe(III)-respiring Geobacter sulfurreducens, designated MacA, was more high
229 s an electron donor in chemostat cultures of Geobacter sulfurreducens, despite the fact that growth y
230 irectional integration by type I-G CRISPR in Geobacter sulfurreducens, in which Cas4 is naturally fus
231 standing of the interaction mechanisms among Geobacter sulfurreducens, Mo(VI), and iron oxyhydroxides
233 tive appendages from the anaerobic bacterium Geobacter sulfurreducens, recently identified as extrace
234 tional states of the sigma factor network in Geobacter sulfurreducens, revealing a unique network top
235 NA-Seq, we show that GacA, the Hypr GGDEF in Geobacter sulfurreducens, specifically regulates cyclic
236 otein nanowires harvested from the bacterium Geobacter sulfurreducens, that functions at the biologic
237 re typically iron-reducing bacteria, such as Geobacter sulfurreducens, that produce high power densit
238 ctural homology with their counterparts from Geobacter sulfurreducens, the results showed that the he
257 ortant source of elemental and methylmercury.Geobacter sulfurreducensPCA, a model bacterium predomina
258 omics improves the ability to understand how Geobacter thrives in natural environments and better the
259 tyostelium discoideum for methylation of the Geobacter tRNA-Asp and tRNA-Glu were determined showing
260 had only a weak activity toward its matching Geobacter tRNA-Asp, but methylated Geobacter tRNA-Glu wi
262 poS plays a role in regulating metabolism of Geobacter under suboptimal conditions in subsurface envi
265 ilaments on metal-reducing organisms such as Geobacter were composed of type IV pili, it has now been
266 sult, we show that tRNA-Glu is methylated in Geobacter while the methylation is absent in tRNA-Asp.
267 evealed that acetate/lactate mainly enriched Geobacter, while in situ OM supported growth and activit