ライフサイエンスコーパス: cyanobacteria

1 ch some are thermo-epilithic biofilm-forming cyanobacteria.

2 eta-carboxysome biosynthesis and function in cyanobacteria.

3 chemoheterotrophic bacteria and mixotrophic cyanobacteria.

4 sity, and spatial distribution of Baltic Sea cyanobacteria.

5 rst BMCs discovered were the carboxysomes of cyanobacteria.

6 en growth, gene expression, and cell size in cyanobacteria.

7 in, produced by a group of late-successional cyanobacteria.

8 activators of nitrogenase gene expression in cyanobacteria.

9 c anhydrase to facilitate carbon fixation in cyanobacteria.

10 cluded Halobacteriaceae, Nanohaloarchaea and Cyanobacteria.

11 l components of this regulatory machinery in cyanobacteria.

12 -scale regulatory mechanisms that operate in cyanobacteria.

13 conversion mechanisms in algae, plants, and cyanobacteria.

14 recipitates form directly on the filamentous cyanobacteria.

15 e widely distributed in all phyla, including cyanobacteria.

16 omplexity of the uptake systems in different cyanobacteria.

17 ly of linear and cyclic peptides produced by cyanobacteria.

18 hways that facilitate dominance by different cyanobacteria.

19 rtain prokaryotes, including the majority of cyanobacteria.

20 teins found among ecophysiologically diverse cyanobacteria.

21 t is responsible for high light tolerance in cyanobacteria.

22 toacclimation (FaRLiP), which occurs in many cyanobacteria.

23 an important role in the regulation of GS in cyanobacteria.

24 tty acids are converted into hydrocarbons in cyanobacteria.

25 trophic Thaumarchaeota, and photoautotrophic Cyanobacteria.

26 the TCA cycle, is still poorly documented in cyanobacteria.

27 tor of photoprotective energy dissipation in cyanobacteria.

28 -subunit might have a regulatory function in cyanobacteria.

29 aving the fastest measured growth rate among cyanobacteria.

30 lants and bryophytes but absent in algae and cyanobacteria.

31 the light-harvesting phycobilisomes (PBS) in cyanobacteria.

32 ich appears analogous to what is observed in cyanobacteria.

33 this to the extent required of desert crust cyanobacteria.

34 and copepod grazing on these picoplanktonic cyanobacteria.

35 ) governs photoprotection in the majority of cyanobacteria.

36 toxic natural products which are produced by cyanobacteria.

37 0.51), Actinobacteria (10.21% +/- 0.37) and Cyanobacteria (1.96% +/- 0.21) that constituted 98.18% (

38 e accumulation of oxygen by the ancestors of cyanobacteria [1-3].

39 The invention of oxygenic photosynthesis by cyanobacteria 2.4 billion years ago forever transformed

40 onary history and gene content of primordial cyanobacteria [7, 8].

41 ents consisting of green algae combined with cyanobacteria able/unable of producing MC.

42 The surface of both mats were dominated by Cyanobacteria, accompanied with known or putative member

43 ated that ingestion of MC-producing algae of cyanobacteria accounted for most of the MC that accumula

44 e years, both treatments negatively affected cyanobacteria, although the effects of monsoon delay wer

45 e combined effects of the antibiotics to the cyanobacteria Anabaena flos-aquae.

46 ply, whereas Proteobacteria, Actinobacteria, Cyanobacteria and Acidobacteria decreased to different d

47 ature, supporting the hypothesis that marine cyanobacteria and algae possess distinctive metabolomes.

48 ansitions between an oxic state dominated by cyanobacteria and an anoxic state with sulfate-reducing

49 In cyanobacteria and chloroplasts, exposure to HL damages t

50 II, a large membrane-bound enzyme complex in cyanobacteria and chloroplasts, mediates light-induced o

51 ulated exchange of proteins and/or lipids in cyanobacteria and chloroplasts.

52 together, patterns suggest that increases in cyanobacteria and cryptophyte abundance reflect a combin

53 me functional groups such as nitrogen-fixing cyanobacteria and denitrifiers may be net beneficiaries

54 Cyanobacteria and diatoms formed distinctly coloured zon

55 imply that the expansion of nitrogen-fixing cyanobacteria and diversification of eukaryotes were del

56 Quite unexpectedly, cyanobacteria and Escherichia coli appear to share an in

57 hotspots, as a result of the degradation of cyanobacteria and extracellular organic matrix mediated

58 ion of nifH revealed that both heterocystous cyanobacteria and heterotrophic proteobacteria had the g

59 loride-binding characteristics exist between cyanobacteria and higher plants.

60 only significant difference between PSII in cyanobacteria and higher plants.

61 Our findings implicate cyanobacteria and hydrocarbon degraders as key players i

62 y found in the genomes of phages that infect cyanobacteria and increase the fitness of the cyanophage

63 ifferent insecticides and binary mixtures of cyanobacteria and insecticides.

64 ystem I (PSI) is the dominant photosystem in cyanobacteria and it plays a pivotal role in cyanobacter

65 dverse health outcomes associated with toxic cyanobacteria and MCs.

66 for the label-free screening and sorting of cyanobacteria and microalgae in a microdroplet platform.

67 biophotovoltaic cells exploit the ability of cyanobacteria and microalgae to convert light energy int

68 degree showed a strong relationship between cyanobacteria and obligate anaerobes, from which cyanoba

69 olically engineered yeast, Escherichia coli, cyanobacteria and other microorganisms have been develop

70 taxa) and 18 fossil calibrations across all Cyanobacteria and photosynthetic eukaryotes.

71 It is general knowledge that cyanobacteria and plants oxidize carbohydrates via glyco

72 Cyanobacteria and plants provide aerobic life with oxyge

73 Cyanobacteria and plants provide the oxygen, food, fuel,

74 In photosynthetic organisms like cyanobacteria and plants, the main engines of oxygenic p

75 been observed in animals, plants, fungi and cyanobacteria and play a fundamental role in coordinatin

76 iruses infecting picophytoplankton, that is, cyanobacteria and prasinophytes, and heterotrophic bacte

77 the metabolic organization of multicellular cyanobacteria and provides a platform for further study

78 Swapping cyclases between cyanobacteria and purple phototrophic bacteria reveals t

79 xes found in the photosynthetic apparatus of cyanobacteria and rhodophyta that harvest solar energy a

80 totrophy was not an ancestral feature of the Cyanobacteria and that Oxyphotobacteria acquired the gen

81 Synteny among filamentous cyanobacteria and the similar expression patterns for hm

82 in the process of biofilm formation between cyanobacteria and well-studied type IV pili-producing he

83 ification and proliferation of nitrate-using cyanobacteria and, potentially, eukaryotic phytoplankton

84 representation of several genera such as YS2/Cyanobacteria, and Bacteroidales and underrepresentation

85 errocomicrobia but decreased Actinobacteria, Cyanobacteria, and Firmicutes as well as a reduced diver

86 oteobacteria, Actinobacteria, Bacteroidetes, Cyanobacteria, and Firmicutes were the top five phyla id

87 ed in a tripartite symbiosis system of moss, cyanobacteria, and fungus.

88 (biocrusts)-communities of mosses, lichens, cyanobacteria, and heterotrophs living at the soil surfa

89 ve [4Fe-4S] cluster protein, whereas plants, cyanobacteria, and some phototrophic bacteria possess an

90 are partially conserved in various archaea, cyanobacteria, and some proteobacteria, such as the ente

91 ion of MC and other secondary metabolites in cyanobacteria, and suggests interchangeable or complemen

92 es that the glyoxylate cycle exists in a few cyanobacteria, and that this pathway plays an important

93 d experiment comparing seawater amended with cyanobacteria- and diatom-derived DOM, metatranscriptome

94 of modern terrestrial and/or benthic coastal cyanobacteria appeared during the late Paleoproterozoic

95 Cyanobacteria are an integral part of Earth's biogeochem

96 We show that these printed cyanobacteria are capable of generating a sustained elec

97 Cyanobacteria are important contributors to primary prod

98 Cyanobacteria are important phytoplankton in the Baltic

99 rom atmospheric CO2 Growth and metabolism of cyanobacteria are inherently tied to the diurnal rhythm

100 Cyanobacteria are intricately organized, incorporating a

101 Cyanobacteria are major sources of oxygen, nitrogen, and

102 It is still unclear, however, which Cyanobacteria are most closely related to the chloroplas

103 Cyanobacteria are photosynthetic prokaryotes showing gre

104 Cyanobacteria are photosynthetic prokaryotes that make m

105 Phycocyanins from cyanobacteria are possible sources for new natural blue

106 Spherical cyanobacteria are probably the world's smallest and olde

107 importance of their primary metabolism, some cyanobacteria are prolific producers of unique and bioac

108 Microalgae and cyanobacteria are promising organisms for sustainable bi

109 Cyanobacteria are the ideal organisms for the production

110 Eukaryotic microalgae and prokaryotic cyanobacteria are the major components of the phytoplank

111 Filamentous and colonial cyanobacteria are widely regarded as trophic dead-ends m

112 Plants acquired many proteins from cyanobacteria as a result of the endosymbiotic event tha

113 The gene probably evolved in cyanobacteria as different species differ for its presen

114 nology while facilitating the development of cyanobacteria as highly modified biofactories.

115 hat vitamin B12 is synthesized by planktonic cyanobacteria as pseudocobalamin, a form not bioactive i

116 that darkness triggers the same response in cyanobacteria as starvation in heterotrophic bacteria.

117 stage for bioengineering photoprotection in cyanobacteria as well as for developing new photoswitche

118 Biofilm communities were dominated by cyanobacteria at all temperatures (>91% of total biovolu

119 and genetic interactions between viruses and cyanobacteria at MIS, highlighting the value of parallel

120 In cyanobacteria, bacterial microcompartments, known as car

121 -2 mm thick red mat dominated by filamentous Cyanobacteria, below which Green Sulfur Bacteria (GSB, C

122 communities dominated by mosses, lichens and cyanobacteria (biocrusts) play a key role in supporting

123 ry of photosystem II (PSII) protein-films to cyanobacteria biofilms to derive: (i) the losses in ligh

124 r little relevance to solving the problem of cyanobacteria blooms in lakes.

125 lts suggest that fish populations exposed to cyanobacteria blooms may potentially face several ecotox

126 hwater lakes, harmful algal blooms (HABs) of Cyanobacteria (blue-green algae) produce toxins that imp

127 s not inherent to intracellularly calcifying cyanobacteria but was likely a genetically based trait o

128 rd the size of the genome of closely related cyanobacteria, but 10-fold larger than most plastid geno

129 key enzymes of the glyoxylate cycle in some cyanobacteria, but other studies concluded that these en

130 otics, are encoded by the genomes of diverse cyanobacteria, but their functions have not been investi

131 The production of toxins by bloom-forming cyanobacteria can lead to drinking water crises, such as

132 r increases (39-116%) in those from colonial cyanobacteria (canthaxanthin), but no response from biom

133 cal role of PntAB in oxygenic photosynthetic cyanobacteria capable of both autotrophic and heterotrop

134 The existence of cyanobacteria capable of performing photosynthesis using

135 range Carotenoid Protein (OCP) photoprotects cyanobacteria cells by quenching singlet oxygen and exce

136 used for rapid analysis of single algae and cyanobacteria cells with diameters ranging from 1 to 8 m

137 ured organisms related to the photosynthetic Cyanobacteria (class Oxyphotobacteria), including member

138 the class Melainabacteria and a new class of Cyanobacteria (class Sericytochromatia) that is basal to

139 hotosynthesis by integrating components of a cyanobacteria CO2-concentrating mechanism will necessita

140 rface communities of lichens, mosses, and/or cyanobacteria comprise up to 70% of dryland cover and he

141 Central carbon metabolism in cyanobacteria comprises the Calvin-Benson-Bassham (CBB)

142 hat predicts the effect of climate change on cyanobacteria concentrations in large reservoirs in the

143 ions more than 500-fold those found in other cyanobacteria, concomitantly and drastically lowering ph

144 Cyanobacteria contain multiple psbA genes that respond t

145 Marine planktonic cyanobacteria contributed to the widespread oxygenation

146 Complex internal membranes within cyanobacteria could disrupt this self-organization by st

147 ific analyses, the category with the highest Cyanobacteria counts was associated with respiratory ill

148 ical factors related to treatment effects on cyanobacteria cover and soil surface roughness following

149 genes have been found in viruses that infect cyanobacteria (cyanophages).

150 nd porewater ammonium and biomass of benthic cyanobacteria decreased.

151 Lyngbyastatin 7 (1) is a marine cyanobacteria-derived lariat-type cyclic depsipeptide of

152 47)TiO2 NPs mixed with 1 x 10(6) cells/mL of cyanobacteria) despite the high natural Ti background, w

153 s on reproduction upon exposure to different cyanobacteria, different insecticides and binary mixture

154 Biologically diverse organisms (e.g., cyanobacteria, dinoflagellates, beetles) produce structu

155 Culture work demonstrates that many Cyanobacteria do not synthesize cobalamin but rather pro

156 Non-dinitrogen-fixing cyanobacteria dominated during the Medieval Climate Anom

157 tly inoculated with an alkalinity-generating cyanobacteria-dominated microbial consortium that was en

158 ster regulator of circadian transcription in cyanobacteria, driving genome-wide oscillations in mRNA

159 indicate that filamentous non-heterocystous cyanobacteria (e.g. Lyngbya, Microcoleus) were important

160 ce of colonial and filamentous bloom-forming cyanobacteria (e.g. Microcystis, Planktothrix, Anabaena

161 rt of microcystin, a hepatotoxin produced by cyanobacteria (e.g., Microcystis aeruginosa), to estuari

162 All sequenced cyanobacteria encode hydrocarbon biosynthesis pathways,

163 Cyanobacteria evolved a robust circadian clock, which ha

164 This study shows that marine planktonic cyanobacteria evolved from benthic marine and some diver

165 oterozoic (2,500-542 Mya), marine planktonic cyanobacteria evolved towards the end of the Proterozoic

166 Many cyanobacteria exhibit surface motility powered by type 4

167 a significant barrier to the exploitation of cyanobacteria for biotechnological and biomedical applic

168 for the sensitive and reliable detection of cyanobacteria for early warning and research purposes.

169 a spicata and Citrus limon were expressed in cyanobacteria for limonene production.

170 udy presents a feasible strategy to engineer cyanobacteria for photosynthetic production of isoprenoi

171 at relied on a single phylotype of Halothece cyanobacteria for primary production.

172 nit of the photosynthetic antenna complex in cyanobacteria, for STORM and SIM imaging.

173 Cyanobacteria forming one-dimensional filaments are para

174 nsitive detection of cyanopeptolin producing cyanobacteria from freshwater samples and hence shows a

175 Filamentous, N2 -fixing, heterocyst-forming cyanobacteria grow as chains of cells that are connected

176 Strong cyanobacteria growth was observed in all dialysis bags w

177 photosystem II (PS II) in plants, algae and cyanobacteria has generated most of the dioxygen in the

178 Cyanobacteria have attracted much attention as hosts to

179 Cryptogamic species and their associated cyanobacteria have attracted the attention of biogeochem

180 ent an overview of the unique chemistry that cyanobacteria have been co-opted to perform.

181 Although cyanobacteria have been engineered to produce various co

182 Plants, algae, and cyanobacteria have developed mechanisms to decrease the

183 Cyanobacteria have efficient carbon concentration mechan

184 Cyanobacteria have evolved effective adaptive mechanisms

185 Now it seems that even tiny cyanobacteria have what it takes to qualify for the most

186 ciations varied by phytoplankton group, with Cyanobacteria having the strongest and most consistent a

187 large quantities of cyanotoxins produced by cyanobacteria in eutrophic water.

188 Colonial nitrogen-fixing cyanobacteria in surface waters played a critical role i

189 Cyanobacteria in the Baltic Sea differed genetically fro

190 ocystin/nonmicrocystin (MC/non-MC) producing cyanobacteria in the diet of experimental Daphnia galeat

191 Nitrogen-fixing cyanobacteria in the genus Trichodesmium play a critical

192 of D. galeata clones to MC/non-MC-producing cyanobacteria in their diet, suggesting microevolutionar

193 fected abundance and composition of biocrust cyanobacteria in two grassland ecosystems.

194 eference for improving biofuel production in cyanobacteria, in which Ci is channeled off from central

195 These results indicate that cyanobacteria influence the fate and composition of iron

196 g mechanism and a faster Rubisco enzyme from cyanobacteria into higher plant chloroplasts may improve

197 that we can introduce a beam of aerosolised cyanobacteria into the focus of the Linac Coherent Light

198 osynthetic membranes, and its deprivation in cyanobacteria is accompanied by chlorophyll (Chl) deplet

199 The clock of cyanobacteria is driven by a three-protein oscillator co

200 Folding of the green-type RbcL subunits in cyanobacteria is mediated by the GroEL/ES chaperonin sys

201 I (PSII) complex located in chloroplasts and cyanobacteria is sensitive to light-induced damage(1) th

202 osynthesis of green plants, green algae, and cyanobacteria is the major provider of energy-rich compo

203 ne obstacle to large-scale implementation of cyanobacteria is their limited growth rates as compared

204 ast to the well-studied uptake mechanisms in cyanobacteria, it is largely unknown how Mn is distribut

205 Some cyanobacteria, known as euendoliths, excavate and grow i

206 The origin of oxygenic photosynthesis in Cyanobacteria led to the rise of oxygen on Earth 2.3 bi

207 The photosynthetic capabilities of cyanobacteria make them interesting candidates for indus

208 Carbon fixation in cyanobacteria makes a major contribution to the global c

209 und 1 and DBL displayed activity against the cyanobacteria Microcystis aeruginosa with a half maximal

210 The cyanobacteria Microcystis proliferate in freshwater ecos

211 PSI-enriched domains in cyanobacteria might foreshadow the partitioning of PSI i

212 Chloroplasts arose from cyanobacteria, mitochondria arose from proteobacteria.

213 bly, suggest this is the form synthesized by cyanobacteria more broadly.

214 -phosphate (KDPG) aldolase, is widespread in cyanobacteria, moss, fern, algae, and plants and is even

215 These proteins are found in cyanobacteria, mosses, and microalgae, but have been los

216 Therefore, cyanobacteria must rely on unique adaptations to bore.

217 Marine photosynthesis is largely driven by cyanobacteria, namely Synechococcus and Prochlorococcus.

218 Plants, algae and cyanobacteria need to regulate photosynthetic light harv

219 In cyanobacteria, nitrogen homeostasis is maintained by an

220 hlights that this genus is distinctive among cyanobacteria, not only in the number of secondary metab

221 Finally, the network reveals that cyanobacteria occupy a unique position among prokaryotes

222 oteins (HCPs), have been found among diverse cyanobacteria, occurring as multiple paralogous groups,

223 The marine cyanobacteria of the genus Synechococcus are important p

224 granule dominated by filamentous and motile cyanobacteria of the order Oscillatoriales.

225 ically for groups of stressors (e.g., either cyanobacteria or insecticides) performed better than gen

226 red algae, whereas others were derived from cyanobacteria, other bacteria, and viruses.

227 Marine cyanobacteria perform roughly a quarter of global carbon

228 In cyanobacteria, photoprotection from overexcitation of ph

229 In plants, algae, and cyanobacteria, photosystem II (PSII) catalyzes the light

230 In plants, algae and cyanobacteria, Photosystem II (PSII) catalyzes the light

231 The waterbody was largely dominated by the cyanobacteria Planktothricoides spp., together with the

232 ding the activity of metabolically versatile cyanobacteria, played an important role in delaying the

233 recise nutrient regime that selects specific cyanobacteria populations is poorly understood.

234 sition as increases in pH favor more diverse cyanobacteria populations.

235 Cyanobacteria possess a family of one-helix high light-i

236 lted in a revised growth model where coccoid cyanobacteria predominate in mat communities forming lit

237 nsights gained from both the rock record and cyanobacteria presently living in early Earth analogue e

238 obacteria and obligate anaerobes, from which cyanobacteria presumably arose, for core functions that

239 l eight N pathways, whereas those within the Cyanobacteria primarily encoded three pathways.

240 The cyanobacteria Prochlorococcus and Synechococcus are impo

241 that strains of the two most abundant marine cyanobacteria, Prochlorococcus and Synechococcus, produc

242 Cyanobacteria produce structurally and functionally dive

243 e chronically and environmentally exposed to cyanobacteria producing hepatotoxins, such as microcysti

244 eltwater bacterial sequences were related to Cyanobacteria, Proteobacteria, Actinobacteria and Bacter

245 engineering BMCs because their expression in cyanobacteria provides a sensitive screen for form (appe

246 ent with the significantly greater number of cyanobacteria quantified by 16S rRNA reads and flow cyto

247 ein level, starting with a primitive form in cyanobacteria, RCA of chlorophytes evolved by integratin

248 rgence of oxygenic photosynthesis in ancient cyanobacteria represents one of the most impressive micr

249 Many cyanobacteria secrete siderophores to sequester iron.

250 eening experiments with green microalgae and cyanobacteria showed that all tested green microalgae sp

251 tentially involved in Daphnia acclimation to cyanobacteria: six protease genes, one ubiquitin-conjuga

252 They are found in all cyanobacteria, some purple photoautotrophs and many chem

253 physicochemical parameters of water column, cyanobacteria species explained the most variability of

254 bundances of five phyla, namely Tenericutes, Cyanobacteria, Spirochaetes, Elusimicrobia and Lentispha

255 Previous work on filamentous cyanobacteria suggested a very different mechanism, with

256 tness of competing clones in the presence of cyanobacteria, suggesting physiological plasticity.

257 The ancient fossil record of euendolithic cyanobacteria suggests that biological fixation of solid

258 Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to

259 s and point mutations in each of three model cyanobacteria; Synechococcus, Synechocystis and Anabaena

260 icrodroplets containing different species of cyanobacteria, Synechocystis PCC 6803 and Synechococcus

261 Even in the presence of cobalamin, Cyanobacteria synthesize pseudocobalamin-likely reflecti

262 radoxical, in that, as oxygenic phototrophs, cyanobacteria tend to alkalinize their surroundings, whi

263 ae, and plants and is even more common among cyanobacteria than phosphofructokinase (PFK), the key en

264 osystem II, abolished Chl f synthesis in two cyanobacteria that grow in far-red light.

265 aryochloris marina is a symbiotic species of cyanobacteria that is capable of utilizing far-red light

266 essential two-component system conserved in cyanobacteria that responds to multiple environmental si

267 rthermore, eutrophic lakes were dominated by Cyanobacteria that use little Si, so reservoirs did not

268 Here, we consider the physiology of cyanobacteria (the only microorganisms capable of oxygen

269 We propose that, in cyanobacteria, the CTDHs are carotenoid donors to HCPs.

270 In filamentous cyanobacteria, the mechanism of gliding motility is unde

271 In cyanobacteria, the orange carotenoid protein (OCP), when

272 In cyanobacteria, the photoactive Orange Carotenoid Protein

273 evolution of higher plant chloroplasts from cyanobacteria, the SRP pathway underwent striking adapta

274 In cyanobacteria, the trigger for this mechanism is the pho

275 onditions and inhibit the recruitment of the cyanobacteria, thereby preventing the reoccurrence of cy

276 In cyanobacteria, timing is generated by a posttranslationa

277 Unfortunately, the engineering of cyanobacteria to create efficient cell factories has bee

278 mplementary functions allowing bloom-forming cyanobacteria to efficiently colonize and dominate in fl

279 Chlorophyll f (Chl f) permits some cyanobacteria to expand the spectral range for photosynt

280 - but not always - limit the availability of cyanobacteria to filter feeding zooplankton (e.g. cladoc

281 gated cell division cycles are observed from cyanobacteria to mammals via intracellular molecular con

282 Irrigation with eutrophic water containing cyanobacteria toxins poses a potential risk to soil anim

283 Palyhtoa), dinoflagellates (Ostreopsis), and cyanobacteria (Trichodesmium).

284 udy, we generated a draft genome sequence of cyanobacteria Trichormus sp. NMC-1 in the QTP and perfor

285 Cyanobacteria typically colonize the surface of arid soi

286 Cyanobacteria use three major photosynthetic complexes,

287 Yet, the mechanism that euendolithic cyanobacteria use to excavate solid carbonates suggests

288 erating numerous markerless modifications in cyanobacteria using CRISPR technology and the alternativ

289 ignificantly decreased and Bacteroidetes and Cyanobacteria was increased compared to baseline and was

290 uity of a terrestrial biosphere populated by cyanobacteria well before the GOE.

291 icantly increased, whereas Bacteroidetes and Cyanobacteria were decreased.

292 exclusive hydrocarbon production pathways in cyanobacteria were discovered.

293 anabaenopeptins, cyclic peptides produced by cyanobacteria, were potent inhibitors of TAFIa with IC50

294 e blooms are predominantly blue-green algae (Cyanobacteria), which are favored by low ratios of nitro

295 In XJ1, and the most abundant phylum was Cyanobacteria, which also accounted for a large proporti

296 It is generally assumed that nitrogen-fixing cyanobacteria will dominate when nitrogen (N) is limitin

297 age, a factor that could have provided early cyanobacteria with an evolutionary benefit.

298 tinal and plasma LPC18:1, and Firmicutes and Cyanobacteria with plasma LPC 18:1.

299 Anabaenolysins are lipopeptides produced by cyanobacteria with potent lytic activity in cholesterol-

300 n of just a few heterologous genes can endow cyanobacteria with the ability to transform specific cen