ライフサイエンスコーパス: bloom

1 ene copy number in seawater samples during a bloom event in Syracuse Bay (Mediterranean Sea) with an

2 not well constrained, in particular during a bloom formation and collapse.

3 nd prokaryotic community members following a bloom off southern California.

4 productivity, export and transcription in a bloom of Crocosphaera over eight days in the North Pacif

5 kton was consistently present, the lack of a bloom during the study period suggests a crucial depende

6 rients available in this new niche support a bloom of Salmonella serovars, thereby ensuring transmiss

7 ement for Si are absent from highly abundant bloom-forming coccolithophores, such as Emiliania huxley

8 ia, most notably during massive marine algae blooms.

9 ng the heat wave was accompanied by an algal bloom and chemically enhanced carbon uptake.

10 indicate that postfire ash loading and algal bloom stage may significantly affect DBP formation in so

11 f karlotoxin 2 (KmTx2; 1), the harmful algal bloom dinoflagellate Karlodinium sp. was collected and s

12 eattle during a cyanobacterial harmful algal bloom in the summer of 2014 were studied using a new app

13 con sequencing as a supporting tool in algal bloom monitoring or water-resource management.

14 erm self-regulation of available P for algal blooming in eutrophic lakes.

15 tely after the death of massive annual algal blooms showed that no selenomethionine or selenomethioni

16 nd North America show that controlling algal blooms and other symptoms of eutrophication depends on r

17 roliferation of cyanobacterial harmful algal blooms (CHABs), yet we have limited understanding of how

18 Cyanobacterial harmful algal blooms (CyanoHABs) have serious adverse effects on human

19 d magnitudes of cyanobacterial harmful algal blooms (CyanoHABs) in freshwater systems.

20 Harmful algal blooms (HABs) are frequently reported around the globe.

21 the impacts of such changes on harmful algal blooms (HABs) are not fully understood.

22 Harmful algal blooms (HABs) induced by eutrophication is becoming a se

23 Preventing harmful algal blooms (HABs) is needed to protect lakes and downstream

24 In freshwater lakes, harmful algal blooms (HABs) of Cyanobacteria (blue-green algae) produc

25 e released to the water during harmful algal blooms and are a serious threat to animals and humans.

26 phosphorus loading that drives harmful algal blooms and hypoxia.

27 Harmful algal blooms cause serious problems worldwide due to large qua

28 The occurrence of harmful algal blooms has resulted in growing worldwide concern about t

29 cent resurgence of hypoxia and harmful algal blooms in Lake Erie, driven substantially by phosphorus

30 es determine the prevalence of harmful algal blooms that threaten water quality.

31 may play a role in regulating harmful algal blooms, but little is known about the biochemical and ph

32 story, and six species causing harmful algal blooms, to determine the ecoregions most likely to be in

33 in contaminated water such as harmful algal blooms.

34 accelerate eutrophication and harmful algal blooms.

35 g the formation of large scale harmful algal blooms.

36 n regulating the occurrence of harmful algal blooms.

37 ion (MeHg burden per cell decreases in algal blooms), extending patterns of contaminant accumulation

38 in key ecological phenomena (including algal blooms and diel vertical migration) that shape the distr

39 algal interactions, control of massive algal blooms in the ocean, and the maintenance and degradation

40 ned high, increasing the likelihood of algal blooms in warming summer temperatures.

41 Postfire algal blooms can increase chlorine reactivity of fire-affected

42 sources of TONO and their precursors, algal blooms, and to a lesser degree agricultural or stormwate

43 DA-producing algal blooms are increasing in size and frequency.

44 e in snow albedo by red pigmented snow algal blooms over the course of one melt season can be 13%.

45 and reduced grazing each can stimulate algal blooms as shown by numerous experiments.

46 ted directly from Lake Erie during the algal blooms that affected 500000 residents in Toledo in 2014.

47 e most toxic compounds produced by the algal blooms, and reveal that the degradation efficiency can b

48 Toxic algal blooms may involve such eco-evolutionary feedbacks due t

49 r bio-hydrochar materials by utilizing algal blooms.

50 roximity to the sea concomitantly with algal blooms of Ostreopsis spp. in the Mediterranean area.

51 Algal-bloom dilution controlled the variability in the MeHg co

52 morphological analysis of the harmful-algal-bloom-forming raphidophyte Heterosigma akashiwo together

53 angeable or complementary functions allowing bloom-forming cyanobacteria to efficiently colonize and

54 l dispersant-degrading Colwellia, which also bloomed in situ in Gulf deep waters during the discharge

55 the universality of endolithic stages among bloom-forming microalgae spanning different phyla, some

56 recovery from frequent facultative anaerobe blooms, which may be driven by fluctuations in luminal r

57 trophic populations during diatom blooms and bloom collapse conditions, resulting in an increase in t

58 perties such as melting, crystallization and blooming were analyzed.

59 diversity, shifts in metabolic capacity, and blooms of pathogens.

60 rawberry was dependent on the stage of apple bloom.

61 During early and peak apple bloom, pollinator abundance and yield were reduced in la

62 Following peak apple bloom, pollinator abundance was greater on farms with hi

63 cides that were not sprayed during the apple bloom period.

64 We observe right-side asymmetric blooming shortly after the storms, attributed previously

65 utrient input therefore impact western basin bloom growth and central basin oxygen demand in distinct

66 reads and 11,807 OTUs were obtained in both bloom and control samples with Alpha-proteobacteria and

67 ndent receptors were highly abundant in both blooming phases.

68 nitial shift toward communities dominated by bloom-forming, short-lived seaweeds.

69 The production of toxins by bloom-forming cyanobacteria can lead to drinking water c

70 ne's microbiota, some of these organisms can bloom in the inflamed gut; expansion of enterobacteria i

71 r for opportunistic microorganisms that can 'bloom', significantly complicating diseases of barrier s

72 Classically, bloom response to horizontal stirring is regarded in ter

73 mporal overlap between mass flowering and co-blooming crops alters the strength and direction of thes

74 on the pollinator community and yield of co-blooming strawberry on farms spanning a gradient in cove

75 fects the pollination and yields of other co-blooming crops.

76 Viruses are a major cause of coccolithophore bloom demise in both temperate and sub-temperate oceanic

77 ntribute to the formation of coccolithophore blooms.

78 ance to solving the problem of cyanobacteria blooms in lakes.

79 at fish populations exposed to cyanobacteria blooms may potentially face several ecotoxicological iss

80 We caused a cyanobacterial bloom by gradually enriching an experimental lake while

81 econdary metabolites during a cyanobacterial bloom that emerged in a highly urbanized tropical reserv

82 thresholds needed to control cyanobacterial bloom formation.

83 were depleted during a dense cyanobacterial bloom, but were replaced by strains with only the high-f

84 as N may significantly impact cyanobacterial bloom size and toxicity.

85 Cyanobacterial blooms often occur in freshwater lakes and constitute a

86 Annual cyanobacterial blooms dominated by Microcystis have occurred in western

87 s can be strongly affected by cyanobacterial blooms, especially species of genus Daphnia, which are k

88 dramatic increases in harmful cyanobacterial blooms, creating serious threats to drinking water suppl

89 notype composition of harmful cyanobacterial blooms.

90 reventing the reoccurrence of cyanobacterial blooms in the following summer.

91 nificantly reduce the risk of cyanobacterial blooms in western Lake Erie but rather may promote a shi

92 Bay experiences annual toxic cyanobacterial blooms dominated by Planktothrix agardhii/suspensa.

93 genus that can develop toxic cyanobacterial blooms in many eutrophic lakes and reservoirs worldwide.

94 Although toxic cyanobacterial blooms in western Lake Erie threaten drinking water supp

95 ial community associated with cyanobacterial blooms is largely conserved at the phylum level, with Pr

96 oup of toxins associated with cyanobacterial blooms.

97 Diatom bloom events were observed in all enclosures, with enhan

98 an abundant microbial metabolite in a diatom bloom in the eastern North Pacific Ocean.

99 hypothesis that RNA viruses influence diatom bloom dynamics in Antarctic waters.

100 and catalytic rates during an intense diatom bloom in the Western Antarctic Peninsula (WAP) and in la

101 eptember 2010, an exceptionally large diatom bloom sedimentation event coincided with elevated sinkin

102 tile, oligotrophic populations during diatom blooms and bloom collapse conditions, resulting in an in

103 or the spatial and temporal extent of diatom blooms, thus impacting ecosystem productivity and ocean-

104 ia shaped their distinct niches in different bloom phases, and certain bacterial species from the Pse

105 of free-living bacterioplankton in different blooming phases of a dinoflagellate Prorocentrum donghai

106 cial for the termination of a dinoflagellate bloom.

107 ignificant genetic and functional diversity: bloom populations may undergo genetic differentiation ov

108 Here we identify dominant blooming patterns using 16 years of ocean-color data in

109 rinsic growth rates of Microcystis dominated blooms.

110 e and toxicity of the Planktothrix-dominated blooms to nutrient amendments with orthophosphate (PO4)

111 ns by a known Mimiviridae (AaV) occur during bloom peak and decline.

112 ns between bacteria and phytoplankton during bloom events are essential for both partners, which impa

113 he large-scale host-virus "arms race" during bloom succession and consequently the turnover of carbon

114 changes in cell division rate, with earlier blooms driven by warmer spring water temperatures.

115 idual cells or colonies under pre- and early-bloom conditions; however, the large-scale, ecosystem-le

116 ification, decreased turbulence and enhanced blooming.

117 enteric pathogens and reduce enterobacterial blooms.

118 io was not atypical of reoccurring Lake Erie blooms and thus may reoccur in the future.

119 o the same family indicated that P450 family blooming is possibly due to its members' duplications.

120 at the dominance of colonial and filamentous bloom-forming cyanobacteria (e.g. Microcystis, Planktoth

121 r phytoplankton growth, especially following bloom senescence.

122 om photosynthesis) acquired phototrophs form blooms.

123 cientific framework for management of future bloom events.

124 catalyst mechanism is capable of generating blooms for other endosymbiont-targeting viruses.

125 and photosynthesis rates are likely to give bloom-forming green seaweeds a competitive advantage in

126 e show that red snow, a common algal habitat blooming after the onset of melting, plays a crucial rol

127 Harmful blooms of the cyanobacterium Microcystis sp. have become

128 ical conditions prevailing during E. huxleyi blooms in the ocean, allowing potential dispersal and in

129 es is fundamental to assess future change in bloom frequency, duration, and magnitude and thus repres

130 Changes in bloom timing have been detected in some cases, but the u

131 The magnitude of the trends in bloom timing from 2006 to 2100 is very similar at high a

132 he priority is detecting long-term trends in bloom timing, data at a temporal resolution of 20 days a

133 ing to those with only a cursory interest in blooms as those deeply immersed in the challenge of unde

134 on fertilization experiments often result in blooms dominated by diatoms [2], indicating that diatoms

135 in the oil-amended communities that included blooms of recognized HCB (e.g., Thalassospira, Cycloclas

136 e (phytoplankton), which has shown increased blooms coincident with sea-ice losses.

137 Indeed, blooms often harbor significant genetic and functional d

138 ly unrecognized, critical role in TC-induced blooming, with potentially important implications for gl

139 e more important with increases in jellyfish blooms in some regions.

140 tributes to improve predictions of jellyfish blooms' magnitude and movements in coastal waters.

141 ilar to the unenriched lake, whereas a large bloom occurred in the continuously enriched lake.

142 the Pseudoalteromonadaceae only in the late-blooming phase, suggesting an active role of this group

143 carbon metabolism were abundant in the late-blooming phase.

144 monadaceae exclusively dominated in the late-blooming phase.

145 ommunity, defined initially by a short-lived bloom of Methylophaga (putative oil degraders) that was

146 The long bloom at SOI seems to drive considerable carbon immobili

147 r column from the atmosphere during the main bloom period but reached equilibrium after the bloom col

148 Mass bloom attracts pollinators and it is unclear how this af

149 c growth was mainly determined by microalgal bloom duration; each day, nanophytoplankton exceeded 200

150 c growth was mainly determined by microalgal bloom duration; each day, nanophytoplankton exceeded 200

151 mmunity diversity during a large Microcystis bloom (H' = 0.61) relative to periods preceding (H' = 2.

152 Direct and indirect effects Microcystis blooms may have on the Delta food web were investigated.

153 ponse were frequently detected in the middle-blooming phase while proteins participating in proteolys

154 ely to the bacterial community in the middle-blooming phase while the Pseudoalteromonadaceae exclusiv

155 ses, and of a Microcystis aeruginosa natural bloom.

156 se intensifies, toxic and unsightly nuisance blooms of algae are becoming larger and more frequent in

157 -4) in microbial richness despite observable blooms of lithoautotrophic iron-oxidizing Betaproteobact

158 ial mean annual growth rates and duration of bloom seasons significantly increased within many coasta

159 ream primary production via the mechanism of bloom dilution (MeHg burden per cell decreases in algal

160 The spatial patterns of bloom timing are similar in both low (monthly) and high

161 bundance representatives, and local peaks of bloom-forming heterocystous taxa.

162 s were conducted to document the response of bloom-forming phytoplankton to submarine groundwater dis

163 succession, and the delay or suppression of bloom events.

164 hus, predicted increases in the frequency of blooms of A. fundyense could affect C. finmarchicus popu

165 t this behavior is key to the maintenance of blooms and essential to reduce the probability of strand

166 Extending beyond the traditional view of blooms being controlled primarily by physics and inorgan

167 ed in temperate lakes, where N2 fixers often bloom when N is replete, and non-fixers (e.g. Microcysti

168 on and production of dimethyl sulfide, often blooms in mid-latitude at the beginning of summer when i

169 vestigate the influence of spatial scales on bloom timing and find that trends are generally more rap

170 Its increasing detection during Ostreopsis blooms and in seafood highlights the need to characteriz

171 changes detected during a natural P. parvum bloom in the source system.

172 s of strong genetic drift caused by periodic blooms of a subset of genotypes, which may have reduced

173 Diatoms are single-celled, photosynthetic, bloom-forming algae that are responsible for at least 20

174 mum 5 days) to investigate how phytoplankton bloom timing changes in response to projected 21st centu

175 focused on a temperate spring phytoplankton bloom in subtropical waters.

176 occasions throughout a summer phytoplankton bloom (November-March).

177 gnitude and composition of the phytoplankton bloom.

178 Strong phytoplankton blooming in tropical-cyclone (TC) wakes over the oligotr

179 Phytoplankton blooms are a worldwide problem and can greatly affect ec

180 Phytoplankton blooms are elements in repeating annual cycles of phytop

181 Phytoplankton blooms beneath snow-covered ice might become more common

182 Phytoplankton blooms caused an increase of Gammaproteobacteria (Altero

183 freshwater-borne nutrients and phytoplankton blooms.

184 sea spray aerosol impacted by phytoplankton blooms.

185 water abruptly triggered dense phytoplankton blooms in the nutrient-poor environment of the upper lay

186 sinking organic matter during phytoplankton blooms and the filter-feeding behavior of the blue musse

187 ntially linked with eukaryotic phytoplankton blooms.

188 d in the literature to explain phytoplankton blooms, but over time the basic tenets of these hypothes

189 tudies have reported extensive phytoplankton blooms beneath ponded sea ice during summer, indicating

190 (NASG), which hosts extensive phytoplankton blooms.

191 In line with our findings, phytoplankton blooms downstream of South Georgia are more intensive an

192 shelf losses (resulting in new phytoplankton blooms which are eaten by benthos) are the only signific

193 Spatial characteristics of phytoplankton blooms often reflect the horizontal transport properties

194 ts the timing and magnitude of phytoplankton blooms that fuel marine food webs and influence global b

195 peak or integrated biomass) of phytoplankton blooms, both in directly sampled, local scale data and a

196 nding of ecological impacts of phytoplankton blooms.

197 Intense annual spring phytoplankton blooms and thermohaline stratification lead to anoxia in

198 such successions during spring phytoplankton blooms in the southern North Sea (German Bight) for four

199 nnual variation between spring phytoplankton blooms, the accompanying succession of bacterial clades

200 ly bioavailable and stimulates phytoplankton blooms.

201 Expansive ice cover supported phytoplankton blooms of filamentous diatoms.

202 iability, we demonstrated that phytoplankton blooms in spring and autumn correspond to the annual max

203 incided with the second of two phytoplankton blooms, signifying the influence of ocean biology on sel

204 nt scyphozoan jellyfish producing population blooms in the Mediterranean probably due to pelagic ecos

205 he microbial population sampled during a pre-bloom period (June-July 2009).

206 These marked fluctuations in pre-bloom silicate inventories will likely have important co

207 lantic Ocean, clear evidence of a marked pre-bloom silicate decline of 1.5-2 microM throughout the wi

208 Overall, the pre-bloom cyanobacterial population was more genetically div

209 ns in August 2014 for comparison to previous bloom communities.

210 compared with the denser summer productivity blooms.

211 with intestinal dysbiosis of proteobacterial blooms, translocation of living bacteria across the inte

212 Replicated blooms were simulated by deep seawater (DSW) addition to

213 from Xiamen sea during an Akashiwo sanguine bloom using Illumina MiSeq sequencing of 16S rRNA gene a

214 ealed the great influence of an A. sanguinea bloom on free-living bacterial communities, and provided

215 rea in response to a 2011 Akashiwo sanguinea bloom.

216 neration of patchiness following large-scale bloom initiation.

217 re evolution may have enhanced the seasonal 'bloom' nature of primary productivity and fundamentally

218 Such blooms can trigger secondary blooms of planktonic bacteria that consist of swift succ

219 inoflagellate functional groups in simulated blooms were unique, with diatoms and haptophytes signifi

220 es spp. utilize enterobactin as iron source, bloom in Lcn2(-/-)/Il10(-/-) mice, and are sufficient to

221 Here, we cultured several seaweed species (bloom forming/nonbloom forming/perennial/annual) in the

222 nmental cues that were driving this specific bloom to provide a scientific framework for management o

223 he Mediterranean Sea, toxic Alexandrium spp. blooms, especially of A. minutum, are frequent and inten

224 by gliders during the North Atlantic spring bloom reveal anomalous features at depths of 100 to 350

225 occus, during which the timing of its spring bloom varied by 4 weeks.

226 he timing of the annual phytoplankton spring bloom is likely to be altered in response to climate cha

227 unique time-series of a phytoplankton spring bloom observed beneath snow-covered Arctic pack ice.

228 if pinpointing the start date of the spring bloom is the priority, the highest possible temporal res

229 During the spring bloom, which accounted for more than half of the seasona

230 is characterized by diatom-dominated spring blooms that results in significant transfer of carbon to

231 overpredicted flowering responses in spring-blooming species, relative to our warming experiment, an

232 to the most frequent cyanobacterial strains blooming in freshwater ecosystems, some of which are tox

233 Such blooms can trigger secondary blooms of planktonic bacter

234 and physiological mechanisms that allow such blooms, we examined how the proteome of E. huxleyi (stra

235 h effort to understanding the causes of such blooms and how they can be prevented or reduced.

236 sses the resilience of coral reefs suffering blooms of macroalgae.

237 the pulses associated with spring and summer blooms.

238 um Trichodesmium spp. form extensive surface blooms and contribute significantly to marine carbon and

239 cause this species can form large, sustained blooms that can generate intense propagule pressures for

240 We find that bloom timing generally shifts later at mid-latitudes and

241 Our results showed that bloom growth and microcystin (MC) concentrations respond

242 and those of free-living Cycloclasticus that bloomed during the Deepwater Horizon oil spill.

243 The bloom altered the overall community functional structure

244 The bloom decreased bacterial diversity, increased species e

245 The bloom was probably stimulated by low salinity and ended

246 The bloom's progression revealed potential impacts to nc-bac

247 The bloom, dominated by the haptophyte algae Phaeocystis pou

248 The bloom-forming dinoflagellate Alexandrium minutum respond

249 ing (H' = 2.32) or following (H' = 3.71) the bloom.

250 In addition, the bloom coincided with a large shift in nc-bacterial commu

251 oom period but reached equilibrium after the bloom collapsed.

252 y, the short recovery of many taxa after the bloom indicates that bacterial communities may exhibit r

253 between benthic microbial assemblies and the bloom forming cyanobacterium Microcystis aeruginosa.

254 As the bloom develops, dissolved iron within the surface mixed

255 The interaction between the bloom-forming alga Emiliania huxleyi and its specific la

256 gross primary production observed during the bloom at Palmer Station may be characteristic of high la

257 ignificantly (p < 0.05) increased during the bloom included carbon degradation genes and genes involv

258 l, the increase in delta(13) Corg during the bloom results chiefly from decreasing ambient CO2 concen

259 omposition fluctuated dynamically during the bloom, but was dominated by Microcystis and Synechococcu

260 ile acI-A and acI-B OTUs declined during the bloom, providing evidence of niche partitioning at the s

261 and N/Si increased significantly during the bloom.

262 with phytoplankton were detected only in the bloom samples.

263 infect Microcystis sp. was implicated in the bloom's collapse.

264 half of the total microcystin content in the bloom, and ferintoic acids C (12) and D (13).

265 raint by breaking down filaments, making the bloom biomass available to other zooplankton species.

266 At the onset of the bloom, dissolved iron within the mixed layer was isotopi

267 We investigate the cellular response of the bloom-forming coccolithophore Emiliania huxleyi to phosp

268 nium (NH4), nitrate (NO3) and urea) over the bloom season (June - October).

269 background and set of tools for reading the bloom literature and to give some suggestions for future

270 nlight necessary to initiate and sustain the bloom.

271 aracteristics in the area indicated that the bloom developed in situ despite the snow-covered sea ice

272 the water column were stable throughout the bloom period.

273 varied over space and time, and whether the bloom affected non-cyanobacterial (nc-bacterial) diversi

274 Bacterial communities within the bloom were more homogeneous than those within the contro

275 novel insights at the crossroads between the blooming fields of landscape genetics, phylogeography, a

276 o neonicotinoids would occur only during the blooming period of flowering crops and that it may be di

277 ney, I have been witness and partaker in the blooming of a technique I love-cryo-electron microscopy.

278 In most cases, the blooms are predominantly blue-green algae (Cyanobacteria

279 marine dissolved organic matter (DOM), their blooms are a global problem that can greatly affect mari

280 y half of global carbon fixation, with their blooms contributing disproportionately to carbon sequest

281 These blooms are terminated by limiting silicate concentration

282 ajor source of the nutrients that fuel these blooms is the Maumee River.

283 The bacteria stimulated by this bloom included the SAR86 and SAR116 clades and the AEGEA

284 Overall results suggested that this bloom might enhance the microbial converting of nitrate

285 ridae and Myoviridae) may also contribute to bloom control, via their lytic activity underpinned by a

286 s showed particularly strong correlations to bloom dynamics.

287 derpin how E. huxleyi has found its niche to bloom in surface waters depleted of inorganic nutrients.

288 hic oil spills stimulate these organisms to "bloom" in a reproducible fashion, and although oil does

289 rrestrial communities, suggesting that toxic blooms may serve as useful models for eco-evolutionary d

290 In a typical bloom, diatoms dominate initially, transitioning over se

291 yi viruses (EhV) that infect the ubiquitous, bloom-forming phytoplankton E. huxleyi and show that EhV

292 community production, suggesting that under bloom conditions this diazotroph has a considerable impa

293 ccolithophore micro-alga that generates vast blooms in the ocean.

294 A viral 'bloom' was identified, and significant increases were de

295 rences in the magnitude of the virioplankton bloom; likely again mediated through changes in the bact

296 sh Sea and along the Alaskan coastline where blooms have recently emerged, and there have been signif

297 end beyond the aquatic environments in which blooms occur.

298 ient influx during mixing, leading to winter bloom formation.

299 em-level effects of toxicity associated with bloom states yield benefits that are necessarily 'public

300 Yet blooming has traditionally been discussed using anecdota