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2 tabolic rhythm that controls the alternating oxygenic and microoxic processes of Cyanothece sp. ATCC
4 ers, genomic arguments for cyanobacteria, an oxygenic atmosphere and any comparably diverse suite of
12 Glutathione metabolism is associated with oxygenic cyanobacteria and the oxygen-utilizing purple b
13 ring the Huronian glaciations, we argue that oxygenic cyanobacteria evolved and radiated shortly befo
16 a metabolically dormant spore to survive in oxygenic environments and be transmitted from host to ho
17 s essential for photosynthesis to proceed in oxygenic environments either by scavenging harmful react
18 , including very small molecules with single oxygenic groups, also strongly stimulated these posterio
20 tative APX-II crystals indicate a protonated oxygenic ligand at 1.88 angstrom from the heme iron.
22 Here, we have investigated the role of the oxygenic ligand in Av MoFeP, which natively contains a S
24 ree variants were generated in which (1) the oxygenic ligand was eliminated (betaSer188Ala), (2) the
25 one or two Fe centers in the absence of the oxygenic ligand, while still retaining wild-type-like di
27 rmance to reexamine the protonation state of oxygenic ligands of the inorganic core of X by directly
28 eP (betaPhe99Tyr/betaSer188Ala), and (3) two oxygenic ligands were simultaneously included (betaPhe99
30 tion of both anoxygenic light-dependent- and oxygenic light-independent CO2 fixation as well as anoxy
31 products indicates a consistent grouping of oxygenic lineages that are distinct and descendent from
32 us, more potent HSCs associated with the low-oxygenic niche can be isolated by selecting for the low
33 solate primitive HSCs located within the low-oxygenic niche due to difficulties of direct physical ac
38 Many attributes of primitive HSCs in the low-oxygenic osteoblastic niche, such as quiescence, and cal
39 e of biofuels derived from aquatic microbial oxygenic photoautotrophs (AMOPs), more commonly known as
40 nthetic competence and their relationship to oxygenic photoautotrophs on global scales are unknown.
44 growth, and up to a 340% enhancement of the oxygenic photocurrent compared to the first generation Q
46 us cyanobacteria are an essential element of oxygenic photogranules for granule-based wastewater trea
51 ified component to the regulatory network of oxygenic photosynthesis and conclude the more than 50-y-
53 n in Synechocystis 6803 is not essential for oxygenic photosynthesis and does not provide an importan
55 annot be invoked to support the emergence of oxygenic photosynthesis and eukaryotes by approximately
56 as key evidence supporting the early rise of oxygenic photosynthesis and eukaryotes, but the syngenei
57 tem I and photosystem II reaction centers of oxygenic photosynthesis and generates a transmembrane el
61 three billion years, the basic machinery of oxygenic photosynthesis and respiration has been perfect
62 sents a model membrane that can conduct both oxygenic photosynthesis and respiration simultaneously.
63 ell types, the vegetative cells that perform oxygenic photosynthesis and the dinitrogen-fixing hetero
64 a, the only known bacterial clade capable of oxygenic photosynthesis and the only group of organisms
66 yanobacteria and plants, the main engines of oxygenic photosynthesis are the pigment-protein complexe
67 tical to those used to date the evolution of oxygenic photosynthesis before the Great Oxidation Event
68 rd respiring microbial communities fueled by oxygenic photosynthesis before the oxygenation of the at
69 n achieve simultaneous nitrogen fixation and oxygenic photosynthesis by cooperation between two cell
71 aging, we demonstrate substantial NIR-driven oxygenic photosynthesis by endolithic, Chl f-containing
75 xic world with high-Fe oceans indicates that oxygenic photosynthesis could have destroyed a methane g
78 ection (ATCC) 51142 is capable of performing oxygenic photosynthesis during the day and microoxic nit
79 al clades are thought to have evolved before oxygenic photosynthesis emerged, including the Chlorofle
80 otopic evidence have been used to claim that oxygenic photosynthesis evolved by 2.8 giga-annum before
81 d provided the evolutionary stock from which oxygenic photosynthesis evolved ca. 2.3 billion years ag
83 s an artefact of lateral gene transfer after oxygenic photosynthesis evolved, an alternative is a geo
85 ever, does not resolve the time of origin of oxygenic photosynthesis from its anoxygenic photosynthet
86 oligomeric dimeric cytochrome b6f complex of oxygenic photosynthesis from the thermophilic cyanobacte
88 Ca(1)Cl(y)) of the water oxidizing enzyme of oxygenic photosynthesis generates O(2) evolution capacit
91 ormation by the manganese-calcium cluster of oxygenic photosynthesis has shaped the biosphere, atmosp
99 is indicates an important role of NIR-driven oxygenic photosynthesis in primary production of endolit
102 e we report the presence of genes central to oxygenic photosynthesis in the genomes of three phages f
106 sible Glc-dependent repression/activation of oxygenic photosynthesis in the unicellular green alga Ch
109 D1 of the photosystem II reaction center of oxygenic photosynthesis is expressed in precursor form (
110 sed for transmembrane free energy storage in oxygenic photosynthesis is generated by the cytochrome b
111 that conducts the light-driven reactions of oxygenic photosynthesis is hosted within specialized pai
113 Light regulation of enzyme activities in oxygenic photosynthesis is mediated by ferredoxin:thiore
114 Our results indicate that the existence of oxygenic photosynthesis is not a sufficient condition fo
116 icrobial innovations in Earth's history, and oxygenic photosynthesis is the largest source of O2 in t
124 on, suggesting a significant effect of local oxygenic photosynthesis on Pacific AMZ biogeochemical cy
125 ty to reconstruct events in the evolution of oxygenic photosynthesis on the scale of entire genomes.
132 ear to have evolved during the transition to oxygenic photosynthesis to play various roles in chlorop
133 espite this, Anthocerotibacter is capable of oxygenic photosynthesis under a wide range of light inte
134 d the electrostatics of P680(+) reduction in oxygenic photosynthesis using histidine-tagged and histi
135 iological/organic nanoconstruct over in vivo oxygenic photosynthesis validates the concept of tetheri
136 easurements on retrieved samples showed that oxygenic photosynthesis was fully but reversibly inhibit
138 subunits of the cytochrome b(6)f complex of oxygenic photosynthesis was measured by stopped-flow mix
141 bacteria (the only microorganisms capable of oxygenic photosynthesis), their co-occurrence with anoxy
143 dation of the global ocean by cyanobacterial oxygenic photosynthesis, about 2,100 Myr ago, is presume
144 se ancient evolutionary innovations, such as oxygenic photosynthesis, can be corroborated with fossil
148 f (cytb(6) f ) complex has a central role in oxygenic photosynthesis, linking electron transfer betwe
150 ous phototrophs, they are used as models for oxygenic photosynthesis, nitrogen fixation, circadian rh
151 late that in the early evolutionary phase of oxygenic photosynthesis, nitrogenase served as an electr
152 eria are unique among bacteria in performing oxygenic photosynthesis, often together with nitrogen fi
153 s a large membrane protein complex vital for oxygenic photosynthesis, one of the most important biolo
159 ario, we demonstrated that a nuclear gene of oxygenic photosynthesis, psbO, is expressed in the sea s
163 ia are the only known prokaryotes capable of oxygenic photosynthesis, the evolution of which transfor
165 anobacteria, algae, and plants is pivotal in oxygenic photosynthesis, the process that powers life on
167 of Earth's atmosphere since the evolution of oxygenic photosynthesis, thereby exerting key influence
168 tead, major innovations - from the origin of oxygenic photosynthesis, to the evolution of reefs or of
169 ria are the only prokaryotes to have evolved oxygenic photosynthesis, transforming the biology and ch
172 are necessary for the optimal functioning of oxygenic photosynthesis, we screened a large collection
173 e evolutionary transition from anoxygenic to oxygenic photosynthesis, which resulted in a substantial
227 core complex I subunits, as well as several oxygenic-photosynthesis-specific (OPS) subunits that are
228 Fe biomineralization may have protected oxygenic photosynthesizers against Fe(2+) toxicity durin
229 P pathway, in line with the observation that oxygenic photosynthesizers are nutrient-limited, rather
230 -microfossil Fe minerals are consistent with oxygenic photosynthesizers but not with other Fe-mineral
231 ecologically important prokaryotic group of oxygenic photosynthesizers that contain cyanobacteriochr
232 sites can expand the absorption spectrum of oxygenic photosynthetic and potentially modulate light h
233 a low concentration suggests that the first oxygenic photosynthetic bacteria in solitary form could
235 brane and intracellular proteins in isolated oxygenic photosynthetic cells are not subjected to exces
237 the photosynthetic membranes of functioning oxygenic photosynthetic cells was estimated using classi
238 the function and biological role of PntAB in oxygenic photosynthetic cyanobacteria capable of both au
239 ction center of photosystem II (PSII) of the oxygenic photosynthetic electron transport chain contain
240 e closest to the last common ancestor of all oxygenic photosynthetic lineages and that green sulfur b
241 ction is to protect the protein complexes in oxygenic photosynthetic membranes against toxic effects
242 al of photobiological hydrogen production by oxygenic photosynthetic microbes has attracted significa
244 However, only a few models are available for oxygenic photosynthetic microorganisms, particularly in
246 energy input, but the pigment composition of oxygenic photosynthetic organisms also reflects the spec
247 egulatory and catalytic functions of ChlH of oxygenic photosynthetic organisms and for a chaperoning
248 ical protein for disulfide bond formation in oxygenic photosynthetic organisms and required for their
249 s been conserved throughout the evolution of oxygenic photosynthetic organisms and suggest a role for
250 protein phosphorylation during evolution of oxygenic photosynthetic organisms and their colonization
254 mpared to other nonphotosynthetic organisms, oxygenic photosynthetic organisms such as cyanobacteria,
257 Photorespiration is an essential process in oxygenic photosynthetic organisms triggered by the oxyge
258 ) is a key component of this pathway in most oxygenic photosynthetic organisms(3,4) and is the last l
266 d type of flavin enzyme that is exclusive to oxygenic photosynthetic prokaryotes and that is based on
268 t the roles of glutathione in cyanobacteria, oxygenic photosynthetic prokaryotes that are the evoluti
270 ) has long been known as a micronutrient for oxygenic photosynthetic resulting from its role an essen
272 thrin, a novel rubrerythrin variant from the oxygenic phototroph Cyanophora paradoxa, at 1.20-1.40 A
273 anobacterium Prochlorococcus is the dominant oxygenic phototroph in the tropical and subtropical regi
274 57,990 base pairs, 1,716 genes) of any known oxygenic phototroph, whereas the genome of its low-light
276 ts, algae and cyanobacteria that make up the oxygenic phototrophs and a diversity of bacteriochloroph
277 s rubredoxin and its orthologs are unique to oxygenic phototrophs and distinct from rubredoxins in Ar
278 t and nutrients in the surface ocean between oxygenic phototrophs and Fe(II)-oxidizing, anoxygenic ph
279 pha-Tocopherol is synthesized exclusively in oxygenic phototrophs and is known to function as a lipid
282 ns in full solar exposure, light filtered by oxygenic phototrophs, and light filtered under seawater,
283 indicate that Ycf54 is a cyclase subunit in oxygenic phototrophs, and that different classes of the
284 subunit protein complex universally found in oxygenic phototrophs, as a reliable reporter protein to
286 emained elusive and paradoxical, in that, as oxygenic phototrophs, cyanobacteria tend to alkalinize t
292 ry, thereby precluding the possibility of an oxygenic prebiotic atmosphere caused by photodissociatio
293 ent increases in P bioavailability can raise oxygenic primary production and organic carbon burial, y
295 OX) state, whereby a backbone amidate and an oxygenic residue (Ser or Tyr) ligate to two of the clust