ライフサイエンスコーパス: biogenic

1 ointing to fires as major sources of primary biogenic aerosol particles in which lignin phenols occur

2 ur results prompt a better representation of biogenic aerosol sources in Arctic climate models.

3 ctions of OH radicals with three unsaturated biogenic alcohols, (E)-3-hexen-1-ol, (Z)-3-hepten-1-ol,

4 Biogenic alkenes, which are among the most abundant vola

5 is study aimed to assess lipid oxidation and biogenic amine (BA) development in "muxama", a dry-cured

6 During ripening, biogenic amine and free amino acid content, microbiologi

7 orebrain to increased concentrations of this biogenic amine and to specific alterations of crucially

8 udy, a model to assess fish quality based on biogenic amine contents using fuzzy logic model (FLM) is

9 ed from the retardation of microbial growth, biogenic amine formation and lipid oxidation during the

10 ed similar functional profiles for mammalian biogenic amine G protein-coupled receptor agonists and a

11 d RNAi assays indicate that males likely use biogenic amine neurotransmitters through the nervous sys

12 ndent in that focal axon modulation with the biogenic amine octopamine, abolished signal integration

13 ent in both samples with the addition of the biogenic amine producing strain almost evened out and th

14 ic acid bacteria (LAB) on tyramine and other biogenic amine production by different food borne-pathog

15 The aim of this study was to compare the biogenic amine production of two starter strains of Lact

16 ship drive and were controlled by tyramine-a biogenic amine related to dopamine, whose roles in most

17 Disruptions of biogenic amine signaling contribute to human neurologica

18 r and neural pathways through which parallel biogenic amine signaling tunes behavior appropriately to

19 or D4 against not only D1-3,5 but also other biogenic amine targets have emerged, and D4 is once agai

20 Histamine (HA) is a biogenic amine that can accumulate to high concentration

21 Histamine is a biogenic amine that is widely distributed and has multip

22 Na(+)/Cl(-)-coupled biogenic amine transporters are the primary targets of t

23 at distinguish substrates from inhibitors in biogenic amine transporters.

24 The biogenic amine tyramine (TA) regulates many aspects of i

25 Histamine is a biogenic amine with extensive effects on many cell types

26 In this study, the amino acid, biogenic amine, and trans- and cis-urocanic acid (UCA) c

27 hest concentrations of the amino acids and a biogenic amine.

28 Tyramine and histamine are the biogenic amines (BA) most commonly found at high concent

29 Free amino acids (AA) and biogenic amines (BA) were quantified for the first time

30 Tyramine and histamine, the most toxic biogenic amines (BA), are often found in high concentrat

31 for the extraction and determination of six biogenic amines (BAs) by NMR is presented.

32 The study evaluated the fatty acids and the biogenic amines (BAs) in 'Nduja of Spilinga stored in di

33 e chemiresistors in the detection of various biogenic amines (i.e. putrescine, cadaverine) and in the

34 Eight biogenic amines (spermine, spermidine, putrescine, hista

35 Only two biogenic amines (tryptamine and tyramine) and two polyam

36 The quantity of biogenic amines (tryptamine, phenylethylamine, putrescin

37 I then discuss the influence of several biogenic amines and neuropeptides on aggressive behavior

38 e compounds, such as phenolics, carotenoids, biogenic amines and phytosterols, which are highly desir

39 he optimal process parameters, regarding low biogenic amines and polyamines content, for "Futoski" ca

40 sed sensor was further tested with different biogenic amines and ratiometric response was obtained fo

41 pacity; ii) high contents of spermine, total biogenic amines and total polyamines; and iii) the highe

42 Biogenic amines are conserved signaling molecules that l

43 Biogenic amines are important for neurotransmission and

44 Biogenic amines are important signaling molecules, and t

45 gs link luminal conversion of amino acids to biogenic amines by gut microbes and probiotic-mediated s

46 The detection and monitoring of biogenic amines by NMR, upon fish storage, is informatio

47 A further 33 biogenic amines can be monitored in samples for relative

48 i-parameter approach: the trimethylamine and biogenic amines concentration changes were compared with

49 Total biogenic amines content ranged from 88.86 to 796.68mgkg(

50 , the intestinal concentrations of SCFAs and biogenic amines decreased with the dietary protein reduc

51 tanding the molecular pathways through which biogenic amines function in model organisms may improve

52 zed TiO2 thin film was used to determine the biogenic amines generated by pork during storage.

53 Biogenic amines have been determined to be causal factor

54 ol tool for routine quantitative analysis of biogenic amines in beverages for the average laboratory.

55 able HPLC method for the determination of 11 biogenic amines in beverages has been performed.

56 ied for determination of the above mentioned biogenic amines in beverages, and permitted an undemandi

57 to evaluate concentrations and evolution of biogenic amines in Canadian pork destined for the Japane

58 Biogenic amines in Canadian pork for the chilled export

59 as led to a new approach in the detection of biogenic amines in complex matrices.

60 void the formation of high concentrations of biogenic amines in fermented food by bacteria, it is adv

61 re no significant differences in most of the biogenic amines including histamine, while there are sig

62 nce one-shot biosensors for determination of biogenic amines is described and compared with high-perf

63 However, biogenic amines observed in the other soybean products s

64 In the nematode Caenorhabditis elegans, the biogenic amines serotonin (5-HT) and octopamine regulate

65 The symporters for the biogenic amines serotonin (SERT), dopamine (DAT), and no

66 this study, we investigated the roles of the biogenic amines serotonin and octopamine in regulating l

67 sts were observed, including that vertebrate biogenic amines structurally related to octopamine acted

68 The effect of other potentially interfering biogenic amines was also evaluated.

69 In the control samples, the amount of biogenic amines was insignificant.

70 ardinella sp.) where the production of eight biogenic amines was monitored over fifteen days of stora

71 No biogenic amines were detected in the 300MPa treatments,

72 None of the 8 biogenic amines were detected in the final products, whi

73 The concentrations of ochratoxin A and biogenic amines were far below the health-hazardous thre

74 Glycoalkaloids, thiols and biogenic amines were generally stable, while 5-hydroxy-m

75 mum particle size) has been employed and the biogenic amines were identified and quantified in a tota

76 Individual biogenic amines were not correlated with their precursor

77 These biogenic amines were not detected in non-fermented soybe

78 inks, and by discriminating between multiple biogenic amines with remote structural differences six c

79 C method for simultaneously quantifying nine biogenic amines, 21 amino acids, and ammonium ions, in b

80 ant changes in plasma levels of amino acids, biogenic amines, acylcarnitines, and lipids.

81 tified metabolites, including sphingolipids, biogenic amines, amino acids and urea.

82 Various metabolites including biogenic amines, amino acids, lipids, were significantly

83 ranged between 0.03mg/L and 0.63mg/L for the biogenic amines, and 0.05mg/L and 5.19mg/L for other com

84 e amino acids, dipeptides, sugars, vitamins, biogenic amines, as well as different products of the AT

85 are not required for steady-state levels of biogenic amines, but become rate limiting in conditions

86 otal volatile base nitrogen (TVBN), K-value, biogenic amines, color, and texture.

87 sicochemical and microbiological parameters, biogenic amines, fatty acids and texture profiles and se

88 bolites (208 in total) included amino acids, biogenic amines, fatty acids, bile acids, sugars, and li

89 ites, including acylcarnitines, amino acids, biogenic amines, glycerophospholipids, hexose, and sphin

90 The neuromodulatory transmitters, biogenic amines, have profound effects on multiple neuro

91 Neuromodulators, including biogenic amines, neuropeptides, and hormones, are releas

92 cts storage: formation of trimethylamine and biogenic amines, proteolysis and different types of ferm

93 Biogenic amines, such as like serotonin, are conserved n

94 On the other hand, the bacterial-related biogenic amines, tyramine, histamine, tryptamine and bet

95 ned by food depletion nor is it modulated by biogenic amines, which suggest it is not an aversive beh

96 increase and the formation of the undesired biogenic amines.

97 ors namely total volatile basic nitrogen and biogenic amines.

98 embled and used as a separation platform for biogenic amines.

99 e presence of many of the common interfering biogenic amines.

100 include BrC primarily consider sources from biogenic and biomass combustion.

101 at ambient conditions, provide insight into biogenic and biomimetic pathways.

102 However, there are several biogenic and geogenic materials in natural waters that i

103 High-resolution biogenic and geologic proxies in which one increment or

104 The ice-nucleating material is probably biogenic and less than approximately 0.2 micrometres in

105 sess the effects of 2 different forms of AC (biogenic and petrogenic) on benthic organisms has been p

106 ndicate most of the methane in the wells was biogenic and produced by the CO2 reduction pathway, not

107 ve distribution on ACC was noted for several biogenic and synthetic systems, the molecular mechanisms

108 Large differences between biogenic and thermogenic sources are observed.

109 s involved in the reduction and oxidation of biogenic and xenobiotic carbonyls.

110 This biogenic-anthropogenic coupling expands the daily high-o

111 n which anthropogenic sulfate could regulate biogenic aqSOA formation, ways not presently included in

112 Nacre, a composite made from biogenic aragonite and proteins, exhibits excellent stre

113 bal secondary organic aerosol potential from biogenic benzenoids to be similar to that from anthropog

114 idate the origin of the superior hardness of biogenic calcite.

115 Maximizing the conversion of biogenic carbon feedstocks into chemicals and fuels is e

116 Therefore, among marine biogenic carbonate fossils, well-preserved acroporid ske

117 Reconstructing pH from biogenic carbonates using boron isotopic compositions re

118 Emerging evidence suggests that the miRNA biogenic cascade is tightly controlled.

119 Fe(II)-oxidizing bacteria form biogenic cell-mineral aggregates (CMAs) composed of micr

120 With the biogenic CH4 emissions omitted, the top-down estimates a

121 ion to the CH4 budget in addition to recent, biogenic CH4 is uncertain.

122 ine biosphere and to examine the capacity of biogenic CH4 to compensate for the faint young Sun durin

123 Proterozoic may have allowed large fluxes of biogenic CH4 to the atmosphere, enhancing the climatic s

124 d via biological activity, the reactivity of biogenic clay-Fe(II) toward reducible contaminants is pa

125 rs to assess the global warming potential of biogenic CO2 (GWPbio).

126 ting the primary anthropogenic, secondary or biogenic components of the species studied here.

127 Tyramine is a biogenic compound derived from the decarboxylation of th

128 t pairs) encompassing both anthropogenic and biogenic compounds and O3 and OH to examine the extent t

129 th possible but limited anthropogenic and/or biogenic contributions.

130 This climate-induced biogenic control also explains the puzzling fact that th

131 s (Arabidopsis thaliana) seedlings, exerting biogenic control of chloroplast functions.

132 content, reaching values equivalent to their biogenic counterparts.

133 of TFA from the atmosphere by reaction with biogenic Criegee intermediates.

134 Mitochondrial biogenic (cytochrome c, mitochondrial transcription fact

135 in water, and even discriminate between two biogenic diamines that are selectively detected over mon

136 igin of the organic layer covering colloidal biogenic elemental selenium nanoparticles (BioSeNPs) is

137 ficial topography contain elevated levels of biogenic elements and heavy metals, including C (and org

138 extent of interactions of anthropogenic and biogenic emissions and the resulting impact on atmospher

139 or new particles to form, particularly where biogenic emissions are important outdoors.

140 al organic compounds (HOMs) originating from biogenic emissions constitute a widespread source of org

141 seasonal cycle may be linked with increasing biogenic emissions in the Arctic, following the growing

142 ch human activities alter SOA formation from biogenic emissions in the atmosphere is largely undeterm

143 gs, which will provide a potential source of biogenic emissions near to air inlet systems.

144 ic aerosol formation in regions dominated by biogenic emissions with nearby SO2 sources.

145 Our results show that, in addition to biogenic emissions, abiotic processes could also be impo

146 Interactions between anthropogenic and biogenic emissions, and implications for aerosol product

147 ective mean TC contributions from wildfires, biogenic emissions, and other sources were 1.18, 0.12, a

148 driven by a combination of anthropogenic and biogenic emissions, and therefore their accurate represe

149 ants can impact the atmospheric oxidation of biogenic emissions, we investigated how sulfur dioxide (

150 These peaks are 13 times larger than typical biogenic emissions.

151 rosol due to wildfires and no clear trend in biogenic emissions.

152 sing the Shewanella exudate only, containing biogenic Fe(II), displayed rates of transformation that

153 both synthetic and environmentally relevant biogenic Fe(III) (oxyhydr)oxides.

154 We found that biogenic Fe(III) minerals were reduced faster and to an

155 ne the in situ transformation of OM-bearing, biogenic ferrihydrite stalks (Gallionella ferruginea-lik

156 This process is facilitated by soluble, biogenic flavins secreted by the organism for the purpos

157 The terrestrial biogenic fluxes of individual greenhouse gases have been

158 ification, potentially altering nutrient and biogenic gas cycling.

159 hotolysis is a major removal pathway for the biogenic gas dimethylsulfide (DMS) in the surface ocean.

160 age fluxes could distort the analysis of the biogenic gas kinetics.

161 lfur hexafluoride (SF6) and the investigated biogenic gases using enhanced Raman spectroscopy.

162 s further showed the superior selectivity of biogenic GNPs compared to chemically synthesized counter

163 The ability of self-functionalized biogenic GNPs towards highly selective colorimetric dete

164 sions) approaches to quantify the global net biogenic greenhouse gas balance between 1981 and 2010 re

165 s have been studied extensively, but the net biogenic greenhouse gas balance resulting from anthropog

166 nd waste management have altered terrestrial biogenic greenhouse gas fluxes, and the resulting increa

167 we record electron energy loss spectra from biogenic guanine crystals in their native state, resolvi

168 ple of how stress gradients generated across biogenic habitats can markedly alter ecological interact

169 Calcifying coralline macroalgae provide biogenic habitats colonised by epiphytic microalgae that

170 Kelp forests (Order Laminariales) form key biogenic habitats in coastal regions of temperate and Ar

171 aring conditions inside versus outside these biogenic habitats.

172 occurrence of ammonia oxidizers implies that biogenic HONO emissions are also possible in the urban a

173 The results suggest that biogenic HONO emissions will be important in soil enviro

174 rtant aerosol constituent in locations where biogenic hydrocarbon emissions mix with anthropogenic NO

175 sistent with the emission patterns of likely biogenic hydrocarbon precursors.

176 tive sites mitigate catalyst deactivation by biogenic impurities that are present during the producti

177 c acid in 94 % yield despite the presence of biogenic impurities.

178 h creates a microenvironment unfavorable for biogenic impurities.

179 ld's coalbed natural gas plays are secondary biogenic in origin, suggesting a potential for gas regen

180 es have not been exploited for anthropogenic-biogenic interaction studies until now.

181 n for regions with substantial anthropogenic-biogenic interactions and consequently improve air quali

182 About 90% of the lithogenic and biogenic iron ingested by krill is passed into their fec

183 Influent DO was effectively consumed by biogenic iron sulfides in the BRS+ column, while DO and

184 Biogenic iron sulfides produced in the BRS+ column, most

185 nic during the bioreduction of abiogenic and biogenic iron(III) (oxyhydr)oxides in arsenic-contaminat

186 t during bioreduction of arsenate(V)-bearing biogenic iron(III) (oxyhydr)oxides in phosphate-containi

187 lead to more active photochemistry, enhanced biogenic isoprene and fire emissions, an extension of th

188 ificant contributor is enhanced emissions of biogenic isoprene, a major ozone precursor, from water-s

189 urce in the U.S. is atmospheric oxidation of biogenic isoprene, but the corresponding HCHO yield decr

190 demonstrate that synergistic effects between biogenic ligands and a reductant (ascorbate) can occur i

191 nts were performed to quantify the effect of biogenic mackinawite on U(IV) stability in the presence

192 Bacterial magnetosomes (BMs) are a type of biogenic magnetic nanomaterials synthesized by magnetota

193 Biogenic magnetite (Fe3O4) in the form of giant (micron-

194 tal magnetization concentration of the giant biogenic magnetofossils to be only approximately 10% of

195 rogen peroxide (H2O2) was employed to remove biogenic material, and focal plane array (FPA)-based ref

196 ructure of functional peptides that engineer biogenic materials at this heterogeneous setting can be

197 r the formation of a wide range of so called biogenic materials that have unique properties that are

198 he product spectrum is not superimposed with biogenic metabolites and elevated substrate concentratio

199 he cumulative warming capacity of concurrent biogenic methane and nitrous oxide emissions is a factor

200 kill mechanisms that has been suggested is a biogenic methane burst triggered by the release of vast

201 n produced fluids and isotopic signatures of biogenic methane in this deep shale have recently been d

202 Together, these results suggest that some biogenic methane may be produced in these wells and that

203 nducted showing that considerable amounts of biogenic methane originating from shallow gas accumulati

204 While there is no doubt that biogenic methane production in the Arctic is an importan

205 on, confirming the complex processes driving biogenic methanol fluxes.

206 distribution and speciation of Zn sorbed to biogenic Mn oxides forming in the hyporheic zone of Pina

207 , we compare the structure and reactivity of biogenic Mn oxides produced by the biofilm-forming bacte

208 ns where Cr(III)-minerals are colocated with biogenic Mn(III/IV)-oxides, suggesting Cr(VI) generation

209 Biogenic MnO2 minerals affect metal fate and transport i

210 ometry to determine the extent and nature of biogenic modification.

211 and uptake of dopamine (DA) as well as other biogenic molecules in viable brain tissue slices has gai

212 but could also contribute to the creation of biogenic molecules.

213 er (SERT) regulates neurotransmission by the biogenic monoamine neurotransmitter serotonin (5-HT, 5-h

214 These biogenic nanoparticles are promising developments for fu

215 NER are considered as a potential risk while biogenic NER from incorporation of labeled carbon into m

216 wth can be used to estimate the formation of biogenic NER.

217 18)O); and (4) stable but spatially variable biogenic NO3(-) concentrations, consistent with recharge

218 ersistent concentrations of blasting-related biogenic NO3(-) derived from nitrification of NH4(+) (lo

219 gated the mechanism and rate of oxidation of biogenic noncrystalline U(IV) by dissolved oxygen (DO) i

220 x transformation and implies the lability of biogenic noncrystalline U(IV) species in the subsurface

221 lfates (R-OS(O)2OH) previously designated as biogenic or of unknown origin in field studies might hav

222 e present-day atmosphere involves ammonia or biogenic organic compounds, in addition to sulfuric acid

223 -24 +/- 5 per thousand is consistent with a biogenic origin and may be evidence that a terrestrial b

224 66.2 +/- 6.4 per mil, consistent with a soil biogenic origin.

225 Post-2006 source increases are predominantly biogenic, outside the Arctic, and arguably more consiste

226 t the conclusion that many commonly measured biogenic oxidation products may be bound in low-volatili

227 al Sec-dependent system is the major protein-biogenic pathway for protein secretion across the cytopl

228 rlds: expediency and synthetic capability of biogenic pathways and chemical diversity enabled by orga

229 Biogenic polyamines are small organic polycations involv

230 determination of three of the most important biogenic polyamines; spermine (SPM), spermidine (SPD) an

231 Comparison of the biogenic precipitates to an abiotic sample shows mineral

232 esh SOA was generated by mixing ozone with a biogenic precursor (beta-pinene, limonene, alpha-pinene)

233 th structurally similar MW 212 C5-OSs, whose biogenic precursor is likely related to 3-Z-hexenal but

234 For the biogenic precursors and experimental conditions studied,

235 can help further the understanding of which biogenic precursors and which chemical processes drive p

236 secondary organic aerosol (SOA) derived from biogenic precursors are characterized with high-resoluti

237 ers link these frequent nucleation events to biogenic precursors released by open water and melting s

238 This finding implies that biogenic processes are more important to uranium ore gen

239 n the atmosphere that stems from abiotic and biogenic processes, including the activity of ammonia-ox

240 Biogenic production and release of methane (CH4 ) from t

241 ater coral Lophelia pertusa also forms large biogenic reefs, facilitated by skeletal fusion.

242 lective autoregulates its population through biogenic renewal and mitophagic culling; mitochondrial f

243 Fe signal residing, at least partially, in a biogenic reservoir.

244 ation in the preindustrial atmosphere and in biogenic-rich regions with limited anthropogenic impacts

245 Growth yields and rates on biogenic S(0) are comparable with those previously deter

246 wild-type strain of Cba. tepidum can grow on biogenic S(0) globules as the sole photosynthetic electr

247 etry and SDS-PAGE indicate that Cba. tepidum biogenic S(0) globules contain carbon, oxygen and nitrog

248 erosol liquid water facilitates formation of biogenic secondary organic aerosol (SOA) and that biogen

249 WS_DTT activity was least associated with biogenic secondary organic aerosol.

250 Biogenic selenium (Se) emissions play a major role in th

251 Biogenic selenium nanoparticles of strain ZYK(T) show a

252 imately 70 Myr-long record of early Mesozoic biogenic silica (BSi) flux from radiolarian chert in Jap

253 dies, suggest that global reorganizations of biogenic silica burial over the Cenozoic reduced marine

254 Biogenic silica encapsulation was used to stabilize the

255 an intricately nanostructured, highly porous biogenic silica material derived from the shells of micr

256 (source of reactive aluminium) and reactive biogenic silica on or shallowly buried within the seaflo

257 the magnitude of anthropogenic influence on biogenic SOA formation based on comprehensive ambient me

258 into a global modeling framework shows that biogenic SOA formation in general, and ELVOC in particul

259 perimental conditions studied, HOMs in fresh biogenic SOA have molecular formulas more closely resemb

260 n HOMs in aged SOA, suggesting that aging of biogenic SOA is not a good surrogate for ambient LVOOA.

261 , were providing information on the aging of biogenic SOA produced under ambient solar conditions.

262 ontributes substantially to the formation of biogenic SOAs in the atmosphere.

263 uctivity and wind speed, suggesting a marine biogenic source for aerosol WSON.

264 y isotope content of methane points toward a biogenic source, while other studies propose a decrease

265 rogenitors made use of hydrogen sulfide from biogenic sources (e.g., decaying wood) rather than from

266 in mesocosm studies aimed at characterizing biogenic sources and linking them to indigenous microbia

267 Stable isotope data suggest that biogenic sources are the cause of this emission increase

268 Thermogenic and biogenic sources were compositionally distinct, and emis

269 gh methane concentrations from predominantly biogenic sources were found throughout the study area.

270 >50,000 years old and is mostly derived from biogenic sources, although a thermogenic contribution co

271 of deltaD-CH4 to distinguish thermogenic and biogenic sources.

272 Biogenic stalks lost approximately 30% of their initial

273 ich is twofold higher than any known organic biogenic structures.

274 by reaction of the thiol-bound mercury with biogenic sulfide, but not in oxic environments.

275 ane territories, allowing an adaptation from biogenic to barrier functions.

276 We have assessed dissolution of biogenic uraninite deployed in wells at the Rifle, CO, D

277 ranium release to (sub)oxic pore waters from biogenic uraninite produced by natural or engineered pro

278 In abiotic experiments with NAu-2 and biogenic uraninite, 16.4% of clay-Fe(III) was reduced in

279 on of aerosol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a la

280 imulations indicate that the contribution of biogenic VOC emissions to ozone formation is lower in Ju

281 Our study demonstrates that biogenic VOCs can considerably enhance air pollution dur

282 ion of secondary organic aerosols (SOA) from biogenic VOCs influences the Earth's radiative balance.

283 os where increased temperatures cause higher biogenic volatile organic compound (VOC) emissions, whic

284 dwater, showing the significant influence of biogenic volatile organic compound oxidation above the f

285 Nitrate radical (NO3) oxidation of biogenic volatile organic compounds (BVOC) is important

286 ribute 2.4% to the global carbon emission of biogenic volatile organic compounds (BVOCs) and can be r

287 Considerable amounts and varieties of biogenic volatile organic compounds (BVOCs) are exchange

288 rganic species in SOA formed by oxidation of biogenic volatile organic compounds (BVOCs) at the singl

289 Emissions of biogenic volatile organic compounds (bVOCs), are an impo

290 ass yields from NO3 oxidation of a series of biogenic volatile organic compounds (BVOCs), consisting

291 Biogenic volatile organic compounds (BVOCs), in particul

292 nic aerosol (SOA) formed by the oxidation of biogenic volatile organic compounds (BVOCs).

293 Emissions of biogenic volatile organic compounds (VOCs) form an impor

294 to enhance the emissions of climate-relevant biogenic volatile organic compounds (VOCs) from boreal a

295 sional model calculations show that sCI from biogenic volatile organic compounds composed the majorit

296 d rural environments and reacts rapidly with biogenic volatile organic compounds to form secondary or

297 Biogenic waste materials and biomass have historically b

298 technologies involved in the exploitation of biogenic wastes, in order to provide an introduction to

299 how technologies for managing and processing biogenic wastes--both established and novel--should be d

300 oad-spectrum inhibition of QS and biofilm by biogenic Zinc oxide nanoparticles and it is envisaged th