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1 ) carotenoid and mediates photoprotection in cyanobacteria.
2 iles and alka/enes not naturally produced by cyanobacteria.
3 cting, and perhaps lysogenizing, filamentous cyanobacteria.
4 ns for improved yield from plants, algae and cyanobacteria.
5 d oomycetes to testate amoebozoans, and even cyanobacteria.
6 novel types of CO(2)-derived hydrocarbons in cyanobacteria.
7 NPQ) of the light-harvesting process in most cyanobacteria.
8 ntation products of metabolically engineered cyanobacteria.
9 tolerant, novel phylotypes of bundle-forming cyanobacteria.
10 differentiated climatic niches for distinct cyanobacteria.
11 was likely linked to the origins of oxygenic Cyanobacteria.
12 ellular resistance in the marine unicellular cyanobacteria.
13 n systems prone to contamination by invasive cyanobacteria.
14 -inducible protein early in the evolution of cyanobacteria.
15 a cryptic c-type heme protein widespread in cyanobacteria.
16 ws fast, sensitive, and in situ detection of cyanobacteria.
17 al blooms that often contain toxin-producing cyanobacteria.
18 protein that governs photoprotection in many cyanobacteria.
19 ch some are thermo-epilithic biofilm-forming cyanobacteria.
20 sity, and spatial distribution of Baltic Sea cyanobacteria.
21 en growth, gene expression, and cell size in cyanobacteria.
22 function gained following the acquisition of cyanobacteria.
23 trophic Thaumarchaeota, and photoautotrophic Cyanobacteria.
24 -subunit might have a regulatory function in cyanobacteria.
25 aving the fastest measured growth rate among cyanobacteria.
26 lants and bryophytes but absent in algae and cyanobacteria.
27 the light-harvesting phycobilisomes (PBS) in cyanobacteria.
28 esent two novel filament-forming proteins in cyanobacteria.
29 ich appears analogous to what is observed in cyanobacteria.
30 this to the extent required of desert crust cyanobacteria.
31 and copepod grazing on these picoplanktonic cyanobacteria.
32 cyanophycin (C(10)H(19)N(5)O(5)) granules in cyanobacteria.
33 ) governs photoprotection in the majority of cyanobacteria.
34 toxic natural products which are produced by cyanobacteria.
35 trogen fixation rates in pelagic unicellular cyanobacteria.
36 tic transcripts despite being outnumbered by Cyanobacteria.
37 the ALC is widely distributed among diverse cyanobacteria.
38 s cyanobacteria in comparison to unicellular cyanobacteria.
39 rated the highest productivity of sucrose in cyanobacteria.
40 nce of cobalt-dependent metabolism in marine cyanobacteria.
41 lect proliferation of nitrogen-fixing marine cyanobacteria.
42 iated with several bacterial taxa, including cyanobacteria.
43 e bacteria, nevertheless remained unclear in cyanobacteria.
44 thetic reaction centres and the evolution of Cyanobacteria.
45 gest and most ubiquitous groups of bacteria, cyanobacteria.
46 ciated fatty acids (FAs), and an increase in cyanobacteria.
47 2-methylhopanoid production by extant marine cyanobacteria.
48 carbonate coatings that entombed filamentous cyanobacteria.
49 except for a single lineage of endosymbiotic cyanobacteria.
54 e years, both treatments negatively affected cyanobacteria, although the effects of monsoon delay wer
57 ature, supporting the hypothesis that marine cyanobacteria and algae possess distinctive metabolomes.
59 ansitions between an oxic state dominated by cyanobacteria and an anoxic state with sulfate-reducing
60 ke amino acids (MAAs) are widely reported in cyanobacteria and are known to be induced under ultra-vi
62 nd nutrient enrichment was detected for both cyanobacteria and chlorophyll-a demonstrating that ecolo
63 me functional groups such as nitrogen-fixing cyanobacteria and denitrifiers may be net beneficiaries
68 population growth rate across phytoplankton (Cyanobacteria and eukaryotic microalgae) and prokaryotes
69 ophic communities of photosynthetic algae or cyanobacteria and heterotrophic bacteria or fungi are pe
72 y found in the genomes of phages that infect cyanobacteria and increase the fitness of the cyanophage
74 biophotovoltaic cells exploit the ability of cyanobacteria and microalgae to convert light energy int
75 n (PCB), a phycobilin naturally occurring in cyanobacteria and only a few eukaryotic phototrophs, JSC
76 olically engineered yeast, Escherichia coli, cyanobacteria and other microorganisms have been develop
78 nt findings related to diurnal metabolism in cyanobacteria and present open questions in the field.
79 icrobiomes were dominated by Actinobacteria, Cyanobacteria and Proteobacteria but were heavily impact
82 xes found in the photosynthetic apparatus of cyanobacteria and rhodophyta that harvest solar energy a
84 2)-fixing organelles that are present in all cyanobacteria and some chemoautotrophs and that substant
85 totrophy was not an ancestral feature of the Cyanobacteria and that Oxyphotobacteria acquired the gen
88 Long-term coexistence between unicellular cyanobacteria and their lytic viruses (cyanophages) in t
89 ly, we quantify the relative contribution of cyanobacteria and viruses to photosystem-II psbA (reacti
90 in the process of biofilm formation between cyanobacteria and well-studied type IV pili-producing he
91 ification and proliferation of nitrate-using cyanobacteria and, potentially, eukaryotic phytoplankton
92 ve oligotrophic (e.g., phyla Nitrospirae and Cyanobacteria) and copiotrophic (e.g., phylum Proteobact
93 ae, Clostridiales, Christensenellaceae, YS2 (Cyanobacteria), and Victivallaceae are significantly ass
95 inococcus-Thermus, then Chlorobi/Chloroflexi/Cyanobacteria, and finally Bacteroidetes/Proteobacteria/
96 errocomicrobia but decreased Actinobacteria, Cyanobacteria, and Firmicutes as well as a reduced diver
97 anges during OCP-mediated photoprotection in cyanobacteria, and furnish a basis for understanding the
98 ve [4Fe-4S] cluster protein, whereas plants, cyanobacteria, and some phototrophic bacteria possess an
99 suggest the symbiosis of G. magellanica with cyanobacteria, and trees and shrubs with mycorrhizas, to
102 e within the carboxysome shell with Rubisco, cyanobacteria are able to overcome the limitations of Ru
106 cripts suggested that more living members of Cyanobacteria are associated with the photosynthetic lay
111 g, genetically amenable, and stress-tolerant cyanobacteria are desirable as chassis for such applicat
114 rom atmospheric CO2 Growth and metabolism of cyanobacteria are inherently tied to the diurnal rhythm
124 Carboxysomes, protein-coated organelles in cyanobacteria, are important in global carbon fixation.
126 might be conserved in other differentiating cyanobacteria as HetL homologues are spread across the p
127 bionts, most dramatically in the unicellular cyanobacteria associated with haptophytes, which have lo
131 s the photogranules grow larger, filamentous cyanobacteria become enriched while other phototrophic m
132 pioneers were succeeded by, amongst others, cyanobacteria belonging to the genera Leptolyngbya, Lyng
133 -2 mm thick red mat dominated by filamentous Cyanobacteria, below which Green Sulfur Bacteria (GSB, C
134 ry of photosystem II (PSII) protein-films to cyanobacteria biofilms to derive: (i) the losses in ligh
137 Microcystins, as secondary metabolite of cyanobacteria (blue-green algae) and cyclic heptapeptide
138 hwater lakes, harmful algal blooms (HABs) of Cyanobacteria (blue-green algae) produce toxins that imp
139 (90)Sr and (226)Ra was not intrinsic to all cyanobacteria but was likely a specific biological trait
140 rd the size of the genome of closely related cyanobacteria, but 10-fold larger than most plastid geno
142 O(2) conditions in a manner similar to other cyanobacteria, but Prochlorococcus strains had significa
143 The production of toxins by bloom-forming cyanobacteria can lead to drinking water crises, such as
146 fect primary producers (i.e., plants, algae, cyanobacteria) can have particularly strong effects beca
147 cal role of PntAB in oxygenic photosynthetic cyanobacteria capable of both autotrophic and heterotrop
148 ured organisms related to the photosynthetic Cyanobacteria (class Oxyphotobacteria), including member
149 the class Melainabacteria and a new class of Cyanobacteria (class Sericytochromatia) that is basal to
150 hotosynthesis by integrating components of a cyanobacteria CO2-concentrating mechanism will necessita
152 rface communities of lichens, mosses, and/or cyanobacteria comprise up to 70% of dryland cover and he
153 hat predicts the effect of climate change on cyanobacteria concentrations in large reservoirs in the
154 y associate geosmin with microbes, including cyanobacteria consumed by larvae [2], who also find geos
155 anotoxins will allow a comprehensive risk of cyanobacteria-containing waters, preventing disease and
157 ical factors related to treatment effects on cyanobacteria cover and soil surface roughness following
160 ster regulator of circadian transcription in cyanobacteria, driving genome-wide oscillations in mRNA
161 in the adaptive strategies of Synechococcus cyanobacteria during the colonization of novel thermal n
164 teobacteria); is populated by photosynthetic Cyanobacteria exhibiting heterotrophic nutrition (Caloth
168 a significant barrier to the exploitation of cyanobacteria for biotechnological and biomedical applic
170 udy presents a feasible strategy to engineer cyanobacteria for photosynthetic production of isoprenoi
171 future biorefineries will deploy engineered cyanobacteria for the conversion of carbon dioxide to us
174 Here, we investigated resistance in marine cyanobacteria from the genera Synechococcus and Prochlor
175 ceeds by the Calvin-Benson-Bassham cycle, in Cyanobacteria, Gammaproteobacteria, and, surprisingly, G
176 and molecular physiology of Chl f-containing cyanobacteria has been unraveled in culture studies, the
179 Cryptogamic species and their associated cyanobacteria have attracted the attention of biogeochem
182 o-occurrence analysis of Hps orthologs among cyanobacteria identified an extended set of putative Hps
184 a higher proportion of CCRPs in filamentous cyanobacteria in comparison to unicellular cyanobacteria
188 Temporal variability of toxins produced by cyanobacteria in lakes is relatively unknown at time sca
189 e gut from the perspective of managing toxic cyanobacteria in lakes, and discuss practical aspects su
191 w concentrations of cobalt in marine waters, cyanobacteria in the genus Prochlorococcus retain the ge
194 ochrome c (6) in darkness (about 60% in both cyanobacteria, in our experiments), the conductivity of
195 articles (Cl NPs) in selectively eliminating cyanobacteria, including the universal bloom-forming spe
198 dents involving microcystins, are within the cyanobacteria (intracellular) until released into the su
200 g the origins of oxygenic photosynthesis and Cyanobacteria is key when piecing together the events ar
202 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
207 The origin of oxygenic photosynthesis in Cyanobacteria led to the rise of oxygen on Earth 2.3 bil
210 en compared to homologs in free-living alpha-cyanobacteria, likely reflecting the homogeneous intrace
213 hortest reported doubling time (2.1 h) among cyanobacteria, making it a promising platform for the so
216 Among the filamentous, heterocyst-forming cyanobacteria, motility is usually confined to specializ
219 hlights that this genus is distinctive among cyanobacteria, not only in the number of secondary metab
220 oteins (HCPs), have been found among diverse cyanobacteria, occurring as multiple paralogous groups,
224 responsible for triacylglycerol synthesis in cyanobacteria opens the possibility of using prokaryotic
227 tudinal distribution of marine Synechococcus cyanobacteria partly relies on the differentiation of li
230 The waterbody was largely dominated by the cyanobacteria Planktothricoides spp., together with the
238 ein level, starting with a primitive form in cyanobacteria, RCA of chlorophytes evolved by integratin
241 oreover, Synechocystis, a nonbiomineralizing cyanobacteria, removed only 14 and 25% of (226)Ra and (9
242 g diatoms, cryptophytes and greens to summer cyanobacteria) resulted in consumers evolving increasing
245 cterize a CRISPR-associated transposase from cyanobacteria Scytonema hofmanni (ShCAST) that consists
246 ersimplification of global change effects on cyanobacteria should be avoided; stressor gradients and
248 bundances of five phyla, namely Tenericutes, Cyanobacteria, Spirochaetes, Elusimicrobia and Lentispha
249 erse, with prevalence of UCYN-A (unicellular cyanobacteria, subcluster 1B) and non-cyanobacterial dia
250 cool-adapted by warm-adapted nitrogen-fixing cyanobacteria (such as Scytonema) and a switch in the do
251 teriaceae (Bacteriodetes), and the phylum of cyanobacteria (such as the Phormidium genus) can be iden
253 than the best-known free-living N(2)-fixing cyanobacteria, suggesting they may be equally or more im
254 of sigma factor in metabolic engineering of cyanobacteria, summarizes the challenges in the path tow
255 ce, ultimately killing the cell, while other cyanobacteria survive due to resistance to infection.
257 ding to carotenoid band shifts, in the model cyanobacteria Synechococcus elongatus PCC7942 and Synech
261 nin has demonstrated to be more selective to cyanobacteria than other pigments, such as chlorophyll-a
262 Cyanobacteriochromes are photoreceptors in cyanobacteria that exhibit a wide spectral coverage and
263 the chlorophyll-containing plants, algae and cyanobacteria that make up the oxygenic phototrophs and
267 onditions and inhibit the recruitment of the cyanobacteria, thereby preventing the reoccurrence of cy
268 Synechococcus, a globally important group of cyanobacteria, thrives in various light niches in part d
270 t recently discovered chlorophylls, enabling cyanobacteria to harvest near-infrared radiation (NIR) a
274 Irrigation with eutrophic water containing cyanobacteria toxins poses a potential risk to soil anim
275 he prominent marine dinitrogen (N(2))-fixing cyanobacteria Trichodesmium to ocean acidification (OA)
277 s oxygen-sensitive nitrogenase [11, 12], and cyanobacteria typically exhibit temperature-induced plas
279 increased the relative abundance of N-fixing cyanobacteria (up to 0.34 as fraction of total reads), c
282 underlie the regulation of photosynthesis in cyanobacteria using ensemble-based measurements remains
286 ignificantly decreased and Bacteroidetes and Cyanobacteria was increased compared to baseline and was
287 in both areas, but the relative abundance of Cyanobacteria was much higher in the emerged areas than
289 ion (qPCR), we discovered that toxin-forming cyanobacteria were present before visible blooms and tox
291 phic organisms, including plants, algae, and cyanobacteria, where it is referred to as photorespirati
292 e found broadly throughout eukaryotes and in cyanobacteria, where they generate circadian (about a da
293 far-red light photoacclimation in a range of cyanobacteria, which enables them to use near-infrared-r
294 ning (MoClo) system is not yet available for cyanobacteria, which lag behind other prokaryotes in syn
295 is balanced by nitrogen fixation mediated by cyanobacteria, which may form extensive blooms in surfac
296 tive cyanocidal compounds that can eliminate cyanobacteria while preserving algal members of the phyt
298 n of just a few heterologous genes can endow cyanobacteria with the ability to transform specific cen
299 otosynthesis by endolithic, Chl f-containing cyanobacteria within natural beachrock biofilms that are