ライフサイエンスコーパス: bloom

1 nt plants, tetrapods and invertebrates and a bloom of microbially-induced sedimentary structures.

2 ure and global importance of E. huxleyi as a bloom-forming, calcifying, photoautotroph, E. huxleyi-Eh

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

4 of such blooms occur when the intensity of a bloom is too high, or when toxin-producing phytoplankton

5 This revealed a bloom, specifically of Enterobacter species, in immune-c

6 uced hepatic steatosis in association with a bloom in Akkermansia and increased Clostridium XIVa gene

7 eveals seasonal phytoplankton accumulation ('blooming') events occurring during periods of declining

8 two field campaigns revealed 1679 snow algae blooms, seasonally covering 1.95 x 10(6) m(2) and equati

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

10 s (P) loads from the MRW drive harmful algal bloom (HAB) severity in Lake Erie; hence changes in mana

11 e to a Karenia brevis red tide harmful algal bloom by examining sound spectrum levels recorded by two

12 In harmful algal bloom mitigation scenarios, the clustered ANN models rev

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

14 to harmful ecological events, such as algal blooms.

15 eds suggests greater potential to fuel algal blooms in coastal areas, especially given the likelihood

16 Cyanobacterial harmful algal blooms (cyanoHABs) are a serious environmental, water qu

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

18 , decreased water clarity, and harmful algal blooms (HAB).

19 Harmful algal blooms (HABs) caused by cyanobacteria in freshwater envi

20 lization of toxins from marine harmful algal blooms (HABs) has been well documented, the aerosolizati

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

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

23 Harmful algal blooms (HABs) produce potent neurotoxins that threaten h

24 n on their role in stimulating harmful algal blooms (HABs).

25 as experienced a resurgence of harmful algal blooms and hypoxia driven by increased nutrient loading

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

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

28 l research is needed regarding harmful algal blooms threatening ecosystem and human health, especiall

29 es including mass mortalities, harmful algal blooms, and declines in subtidal kelp beds.

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

31 pressures likely to influence harmful algal blooms, exposure to microcystin, a known hepatotoxin and

32 anagement decisions related to harmful algal blooms.

33 s the marine food chain during harmful algal blooms.

34 in contaminated water such as harmful algal blooms.

35 n regulating the occurrence of harmful algal blooms.

36 phication and it is plagued by harmful algal blooms.

37 episodic disturbances, such as harmful algal blooms.

38 Macro-algal blooms, eutrophication, and reduction in coral cover hav

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

40 n or decline, particularly in areas of algal blooms and near coral reefs, as well as in areas affecte

41 example, the increased persistence of algal blooms as observed in our mesocosm experiment.

42 ed to eutrophication and the spread of algal blooms with an increasing economic and environmental bur

43 )(1) and increases in the incidence of algal blooms.Although recent work has suggested that individua

44 rs, thus weakening top-down control on algal blooms in eutrophic lakes.

45 USA suffers from recurring late summer algal blooms that often contain toxin-producing cyanobacteria.

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

47 r bio-hydrochar materials by utilizing algal blooms.

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

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

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

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

52 e, we detected C. difficile colonization and blooms in people recovering from food poisoning and Vibr

53 However, after apple bloom, the abundance of known tree fruit pollinating bee

54 During apple bloom, the known tree fruit pollinators were more freque

55 tor species, and bees collected during apple bloom.

56 rawberry was dependent on the stage of apple bloom.

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

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

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

60 r related to the sensor, and referred to as "blooming", presumably in relation to the effect that can

61 s, low-abundant hydrocarbonoclastic bacteria bloom and rapidly prevail over the marine microbiota.

62 in behaviour ('animal personality') has been blooming for over a decade.

63 ndent receptors were highly abundant in both blooming phases.

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

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

66 colonize human oro-respiratory sites and can bloom in several human disorders.

67 Chocolate bloom is an off-white coating on the surface of chocolat

68 ability to detect and characterize chocolate bloom using portable laser spectroscopy could be used to

69 an spectrometer was used to detect chocolate bloom.

70 r the on-site chemical analysis of chocolate bloom and as an alternative laser-based chocolate decora

71 nvasive point-of-care detection of chocolate bloom has been an essential but challenging problem.

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 broadly regarded as a beneficial commensal, bloomed upon starvation and in a CD8 T cell-dependent ma

77 heated mesocosms with an increase in common bloom-forming taxa-Microcystis spp. and Dolichospermum s

78 OA, namely in regulating toxic cyanobacteria blooms on coral reefs.

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

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

81 5 during the development of a cyanobacterial bloom.

82 Intensified cyanobacterial bloom events are of increasing global concern because of

83 Cyanobacterial blooms are an increasing threat to water quality and glo

84 Cyanobacterial blooms produce hazardous toxins, deplete oxygen, and sec

85 Annual cyanobacterial blooms dominated by Microcystis have occurred in western

86 polysaccharides, likely from cyanobacterial blooms.

87 e global expansion of harmful cyanobacterial blooms (CyanoHABs) poses an increasing threat to public

88 reasing incidences of harmful cyanobacterial blooms (CyanoHABs), but little attention has been paid o

89 Harmful cyanobacterial blooms (HCBs) are becoming a major challenge for the man

90 severe and recurring harmful cyanobacterial blooms, especially by the non-N(2) -fixing Microcystis s

91 epatotoxin and a byproduct of cyanobacterial blooms can be a risk factor for NAFLD associated comorbi

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

93 e N(2) fixation efficiency of cyanobacterial blooms.

94 essive factor with effects on cyanobacterial blooms as source of microcystins.

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

96 ves of microbes involved in nitrogen cycling bloomed during times of ice cover as sequences related t

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

98 acid limitation terminates the spring diatom bloom in the AASP and the sinking of the senescent and d

99 The spring diatom bloom in the Arctic Ocean accounts for significant annua

100 tanding the future of the AASP spring diatom bloom requires models that explicitly consider changes i

101 Diatom blooms are important features of productive marine ecosy

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

103 trations than nitrate, which suggests diatom blooms may deplete Si before N.

104 During a 6-week study, diatoms bloomed and progressively consumed silicic acid to where

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

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

107 s, more individuals experienced C. difficile blooms.

108 cial for the termination of a dinoflagellate bloom.

109 Studies that document bloom conditions in lakes have either focused only on in

110 eria during the course of a diatom-dominated bloom in the German Bight, North Sea.

111 rogen, an early summer Microcystis-dominated bloom, a shift of dominance from Nostoc and Anabaena to

112 t acclimation strategies are employed during bloom dynamics.

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

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

115 ximity and abundance of almond pollen during bloom.

116 monly reported visual signs, such as earlier blooming or reduced floral display in early melting year

117 In the early bloom phase, selfish activity was accompanied by low ext

118 temperature-mediated floral bud break, early blooming in winter, and strong cold tolerance.

119 Ephemeral "blooms" of picoeukaryotic phytoplankton (PEUK) during sp

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

121 tributing respective metabolites, explaining bloom decline and community succession.

122 d by cyanobacteria, which may form extensive blooms in surface waters.

123 film on the chocolate surface, known as fat bloom.

124 trument was used to partially remove the fat bloom of the dark chocolate and to induce sugar bloom on

125 r phytoplankton growth, especially following bloom senescence.

126 en-fixing cyanobacterium that forms frequent blooms in freshwater habitats.

127 Freshwater blooms of phytoplankton affect public health and ecosyst

128 Freshwater blooms result in economic losses of more than US$4 billi

129 Raman spectra acquired from bloomed HERSHEY'S milk chocolate, Hawaiian Host milk cho

130 (FDP), defined as the duration between full bloom and maturity, are highly variable in peach [Prunus

131 cientific framework for management of future bloom events.

132 Their gigantic blooms play important ecological and biogeochemical role

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

134 amydomonas and Chlorella were found in green blooms but only Chloromonas was detected in red blooms.

135 present an indirect threat of freshwater HAB blooms in the St.

136 Harmful blooms of the cyanobacterium Microcystis sp. have become

137 However, bloom area and elevation were observed to increase at lo

138 st interactions in an ecologically important bloom-forming cyanobacterium.

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

140 erienced a significant (P < 0.1) decrease in bloom intensity are rare (8 per cent).

141 find, however, that lakes with a decrease in bloom intensity warmed less compared to other lakes, sug

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

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

144 considered, and that the role of viruses in bloom formation and decline may be governed by host phys

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

146 research identified the toxin microcystin in blooms, but we wanted to better understand how the algal

147 ncourage more studies on their occurrence in blooms, persistence, and potential toxicity.

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

149 ively blocks the striking irinotecan-induced bloom of Enterobacteriaceae in immune-deficient mice.

150 Hence, inflammation-induced blooms of E. coli LF82 are significantly blunted when am

151 le mechanistic link between viral infection, bloom termination, and mass carbon export events and hig

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

153 Contrasted to the known bloom-forming species U. prolifera growing at an approxi

154 We also found that a large bloom in August 2016 was highly anomalous both in its ov

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

156 hytoplankton communities and even form large blooms during favourable conditions.

157 The late bloom phase was characterized by high external hydrolysi

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

159 monadaceae exclusively dominated in the late-blooming phase.

160 All persistent strains have episodic local blooms to high abundance, crucial for their persistence

161 Lucie Estuary can result in lower bloom intensities.

162 sterols) of two chytrids infecting two major bloom-forming phytoplankton taxa of contrasting nutritio

163 These major blooms reflect the initiation of the arrival and upwelli

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

165 y be associated with a 50% reduction in mean bloom magnitude and annual primary productivity, assumin

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

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

168 re associated with low P and the Microcystis bloom.

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

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

171 Although Noctiluca blooms are non-toxic, they can cause fish mortality by e

172 ble with the hypothesis that recent nuisance blooms may be a consequence of climate change.

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

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

175 studied, revealing a global exacerbation of bloom conditions.

176 tudes, suggesting that parallel expansion of bloom area on larger landmasses, close to bird or seal c

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

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

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

180 colate were used to characterize the type of bloom.

181 ly rising levels of oxygen as a byproduct of blooming cyanobacterial photosynthesis resulted in a red

182 enced by marine nutrient inputs, with 60% of blooms less than 5 km from a penguin colony.

183 Antarctica may lose a majority of the 62% of blooms occupying small, low-lying islands with no high g

184 SV composition can change over the course of blooms.

185 New Zealand indicating prolonged periods of blooms of siliceous microorganisms starting ~36 million

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

187 roach, but has not been evaluated in situ on blooms of A. catenella, in which cell abundances may var

188 ommunities (SCs), which are composed of OTUs blooming at the same time of the year, and three environ

189 ynthesized by a natural Ostreopsis cf. ovata bloom, in suspension in the water and in the atmosphere.

190 sity and 68% more floral species during peak bloom, respectively, than non-affected stands; (2) bee c

191 environmental factors across a phytoplankton bloom using 16S rRNA gene amplicon community profiles.

192 ine snow formation following a phytoplankton bloom.

193 overall copepod abundance and phytoplankton bloom magnitude.

194 c parameters during the annual phytoplankton bloom cycle.

195 ), coinciding with a declining phytoplankton bloom.

196 mediated carbon cycling during phytoplankton bloom conditions in the marine environment.

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

198 reason behind the increase in phytoplankton bloom intensity remains unclear, however, as temporal tr

199 with the timing of the spring phytoplankton bloom resulting in increased prey availability in the Ca

200 rly summer after a late spring phytoplankton bloom, and were associated with high phosphorus and low

201 gnitude and composition of the phytoplankton bloom.

202 days to represent a transient phytoplankton bloom results in transient subsurface maxima or pulses i

203 Phytoplankton blooms are elements in repeating annual cycles of phytop

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

205 sea spray aerosol impacted by phytoplankton blooms.

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

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

208 ently form spatially extensive phytoplankton blooms, responding rapidly to increased availability of

209 eep waters stimulating massive phytoplankton blooms in the Southern Ocean.

210 gh their rapid exploitation of phytoplankton blooms and bulk egestion of rapidly sinking faecal pelle

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

212 benefiting from the decline of phytoplankton blooms.

213 Spring phytoplankton blooms in temperate environments contribute disproportio

214 ntense summertime near-surface phytoplankton blooms for 71 large lakes globally.

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

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

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

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

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

220 upregulated during the bloom compared to pre-bloom in Harsha Lake.

221 To prevent bloom appearance, the World Health Organization has esta

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

223 compared with the denser summer productivity blooms.

224 ial communities ex vivo, with Proteobacteria blooming and Bacteroidetes declining in the presence of

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

226 remotely sensed data but not for quantifying bloom magnitude, information that would guide water qual

227 d duplication, are present in C. raciborskii blooms in Australia.

228 t and raising the possibility that recurrent blooms in the tropical Atlantic and Caribbean Sea may be

229 Therefore, we sampled one recurring bloom location throughout the entire open water season.

230 oms but only Chloromonas was detected in red blooms.

231 neration of patchiness following large-scale bloom initiation.

232 oratory cultures and mesocosms that simulate blooms.

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

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

235 ecosystem component and the ice algal spring bloom a critical event in the annual production cycle.

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

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

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

239 In the open Southern Ocean, the spring bloom magnitude is found to be greatest in areas with hi

240 he long-term average phenology of the spring bloom, but did not track contemporaneous green-up.

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

242 The combination of earlier spring blooms and lower summer food quantity and quality create

243 ummer-blooming species and herbaceous spring-blooming species.

244 didate Phyla Radiation) displayed successive blooms, potentially triggered by a period of methane fam

245 Harmful effects of such blooms occur when the intensity of a bloom is too high,

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

247 om of the dark chocolate and to induce sugar bloom on the milk chocolate.

248 he Cooper bill contained diatoms from summer bloom species suggesting that the money was not directly

249 the pulses associated with spring and summer blooms.

250 so applies to flowering durations for summer-blooming species and herbaceous spring-blooming species.

251 rmer areas, which is more obvious for summer-blooming species compared to spring-bloomers driven by t

252 ion pathway (RCP) 8.5, especially for summer-blooming species.

253 We find that peak summertime bloom intensity has increased in most (68 per cent) of t

254 s of laboratory cultures and oceanic surface blooms of Trichodesmium from the South Pacific Ocean tri

255 ed during the peak of multiple Synechococcus blooms, with this switch occurring in multiple clades, b

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

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

258 There is also a broad consensus that blooms are increasing with global warming, but the impac

259 The bloom of 2011 might be a result of Amazon River discharg

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

261 The bloom, dominated by the haptophyte algae Phaeocystis pou

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

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

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

265 As the bloom progressed, selfish uptake increased markedly, and

266 etwork, suggesting relationships between the bloom dominant species and other taxa could play a role

267 tive of a copy number difference between the bloom population and a culture used for assay calibratio

268 ng were significantly upregulated during the bloom compared to pre-bloom in Harsha Lake.

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

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

271 and N/Si increased significantly during the bloom.

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

273 e expression and biochemical activity in the bloom-forming, N(2) -fixing, marine cyanobacterium Trich

274 ionship was also observed in cultures of the bloom-forming diatom Chaetoceros tenuissimus, where Si s

275 We show that viral infection of the bloom-forming, planktonic diatom Chaetoceros socialis in

276 ater)(-1)) obtained at an early phase of the bloom.

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

278 nlight necessary to initiate and sustain the bloom.

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

280 the water column were stable throughout the bloom period.

281 o substrate structural complexity and to the bloom-stage dependent composition of the heterotrophic b

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

283 The blooming cosmopolitan coccolithophore Emiliania huxleyi

284 esponsive paper-like actuators can mimic the blooming of the Michelia flower and perform self-propell

285 These blooms are terminated by limiting silicate concentration

286 ithin this cyanobacterial genus during these blooms as well as further offshore in the Southern Calif

287 s showed particularly strong correlations to bloom dynamics.

288 tion in growing sea ice enabled M. rubrum to bloom at the ice-water interface despite the relative fl

289 Captured by profiling floats, two blooms were observed in the vicinity of the Antarctic Ci

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

291 ating cyanobacteria, including the universal bloom-forming species Microcystis aeruginosa, while havi

292 ial community and environment across various bloom stages.

293 and biogeochemical importance, forming vast blooms in aquatic ecosystems.

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 the collection of samples before any visible blooms were present.

297 ng cyanobacteria were present before visible blooms and toxins not previously detected in this region

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

299 tly replaced diatoms as the dominant winter, bloom forming organism.

300 abrupt shift in microbiome composition, with blooms of oral and disease-associated bacteria.