ライフサイエンスコーパス: anoxic

1 oxygenated (oxic) and redox stratified (oxic-anoxic).

2 Infected human tissues are hypoxic or anoxic.

3 Anoxic/aerobic and anaerobic/aerobic metabolic bioselect

4 alysts using both doping and annealing under anoxic ambient.

5 d abiotic production of hybrid N2 under both anoxic and 20% O2 atmosphere conditions.

6 Iron-speciation indicates deeper waters were anoxic and Fe-rich, while trace element concentrations i

7 in mid-Proterozoic oceans were predominantly anoxic and ferruginous (depleted in dissolved oxygen and

8 nd activates hypoxia marker genes under both anoxic and normoxic conditions.

9 roorganisms that can metabolize them in both anoxic and oxic zones.

10 when the atmosphere and oceans were largely anoxic and soluble Fe(2+) was abundant.

11 s in microbial mats found at 9-10 m depth in anoxic and sulfidic water in Little Salt Spring (Florida

12 Widespread euxinic (anoxic and sulfidic) oceanic conditions have been propos

13 However, there is no evidence for euxinic (anoxic and sulphidic) conditions for the fossiliferous s

14 Previous work has suggested that anoxic and/or reducing conditions are needed to synthesi

15 lains, which exhibited a succession of oxic, anoxic, and suboxic-oxic zones with increasing depth alo

16 m concurrent NO3(-) production by anammox in anoxic aquifers, a process that has been largely overloo

17 )] is an important biogeochemical process in anoxic aquifers.

18 se of a reduction in biomass in periodically anoxic areas.

19 violet C light by oxygen in Archaean earth's anoxic atmosphere followed by chirally selective damage

20 d for production of sulfur allotropes in the anoxic atmosphere of Archean Earth.

21 populations of self-cleaving ribozymes in an anoxic atmosphere with varying pH in the presence of eit

22 rite tailings comprise no requirement for an anoxic atmosphere, 1.8-fold less acid consumption than f

23 I sediments incubated under fluctuating oxic/anoxic atmosphere.

24 of NO2- by Fe(II)--chemodenitrification--in anoxic batch incubations at neutral pH.

25 ce the intracellular redox state of cells in anoxic biofilm subzones.

26 utcome data and reported the 1-year risks of anoxic brain damage or nursing home admission and of dea

27 Anoxic brain injury (odds ratio [OR], 3.80; 95% CI, 1.73

28 age (OR, 1.02; 95% CI, 1.01-1.04; P = .005), anoxic brain injury (OR, 3.49; 95% CI, 1.96-6.21; P </=

29 ndicated that the exclusion of patients with anoxic brain injury and refractory cardiogenic shock fro

30 0-541 million years ago, Ma) were dominantly anoxic, but may have become progressively oxygenated, co

31 Using the anoxic Cariaco Basin as a natural laboratory, particle a

32 eic breathing (p = 0.011) during the initial anoxic challenges.

33 We used steady-state oxic and anoxic chemostat cultures to demonstrate that the switch

34 ailable clinical tests for prognosis of post-anoxic coma are informative of poor outcome.

35 ical T1-weighted images were acquired in 126 anoxic coma patients ("learning" sample) 16 +/- 8 days a

36 An additional sample of 18 anoxic coma patients, recruited in Toulouse, was used to

37 Under an extreme anoxic condition (0.001%), survival fraction is calculat

38 , and under oxic, suboxic (0.2% oxygen), and anoxic conditions (oxygen-free with nitrate).

39 We incubated soils under cycles of oxic-anoxic conditions (tauoxic:tauanoxic = 1:6) at three fre

40 ted that incubation with 1 mm cysteine under anoxic conditions (to minimize sulphide oxidation) great

41 ionizing radiation damage to cytosine under anoxic conditions and also serving as a general model of

42 reduction transcript ratios increase during anoxic conditions and corresponded with the highest solu

43 ad an extremely narrow single EPR line under anoxic conditions and excellent oxygen sensitivity.

44 ings corroborate that BPA is not inert under anoxic conditions and suggest that MnO2-mediated coupled

45 nitrogenase can be oxidatively damaged under anoxic conditions and that the aforementioned conformati

46 tochondria) in producing acetate under dark, anoxic conditions and, surprisingly, also suggested that

47 at different initial Fe/S molar ratios under anoxic conditions at neutral pH.

48 itioning of associated As(V) and Sb(V) under anoxic conditions at pH 7.

49 In the eastern floodplain, the anoxic conditions at the intermediate horizon (55-80 cm)

50 ctivity, resists microbial degradation under anoxic conditions but is susceptible to abiotic transfor

51 oagulation at pH 6 and pH 8 at both oxic and anoxic conditions can be described by a new model that i

52 If the anoxic conditions characteristic of the studied sections

53 In addition, the anoxic conditions in the eastern floodplain coincided wi

54 all temperate lake over 1 year indicate that anoxic conditions in the hypolimnion and the autumn over

55 ranium and iron oxyhydroxides under oxic and anoxic conditions is essential for understanding uranium

56 Under anoxic conditions Mn(II) inhibited UO2 dissolution, whic

57 By contrast, the anoxic conditions prevented oleuropein from undergoing e

58 xcesses of dithionite to these samples under anoxic conditions produced small or negligible changes i

59 ns mediating inorganic carbon fixation under anoxic conditions suggests that SUP05 will become increa

60 ess undergoes frequent alternating anaerobic/anoxic conditions to achieve phosphate release and uptak

61 nd dissolved O2 concentration under oxic and anoxic conditions using amperometric microsensors.

62 ve the ability to oxidize NH4(+) to N2 under anoxic conditions using NO2(-).

63 ed on dithionite consumption by the HS under anoxic conditions were in good agreement with past elect

64 ivated sludge systems under both aerobic and anoxic conditions when operating under dynamic condition

65 ICLs are produced upon irradiation under anoxic conditions when the 4-bromopyridone is present in

66 hours in culture media at 37 degrees C under anoxic conditions with 3 mM glucose and 32 mug/mL dimeth

67 , the presence of either type of bag created anoxic conditions within the sediment along with reduced

68 itions) and, to a lesser degree, via direct (anoxic conditions) pathways.

69 on by (i) microbial processes under oxic and anoxic conditions, (ii) abiotic processes mediated by re

70 s mobilization potential under both oxic and anoxic conditions, as well as a high bioaccessibility of

71 at Miaohe there is geochemical evidence for anoxic conditions, but paleontological evidence for at l

72 Under anoxic conditions, certain anaerobic bacteria can oxidiz

73 Under anoxic conditions, nitrate is a preferential electron ac

74 Under anoxic conditions, nitrate reduction was accompanied by

75 ilable kinetic data for dechlorination under anoxic conditions, shows that sulfidation usually increa

76 Under anoxic conditions, the (reductive) dissolution of As-bea

77 he process of molybdenum precipitation under anoxic conditions, there is no information about their a

78 In the presence of 1 or 2 mM Fe(II), under anoxic conditions, U(VI) uptake by the smectites changed

79 Mn, Fe, and As were mobilized under anoxic conditions, whereas Sb, Se, and U were mobilized

80 ) rapidly consume DO and nitrate to maintain anoxic conditions, yielding Fe(II) from FeS oxidative di

81 d biofilm aggregate populations experiencing anoxic conditions.

82 germination and early seedling growth under anoxic conditions.

83 lize in the presence of aqueous Fe(2+) under anoxic conditions.

84 decomposed organic matter under waterlogged anoxic conditions.

85 ervoir of catotelm C is stable under current anoxic conditions.

86 robial activity, or biomass production under anoxic conditions.

87 that BPA is susceptible to degradation under anoxic conditions.

88 e waste repositories, was investigated under anoxic conditions.

89 minated floodplain soil (214 mg As/kg) under anoxic conditions.

90 on of As from Fe-rich aquifer sediment under anoxic conditions.

91 d generating ATP when it experiences hypoxic/anoxic conditions.

92 d vernadite (delta-Mn(IV)O2) at pH 7.5 under anoxic conditions.

93 mical systems can oscillate between oxic and anoxic conditions.

94 into microbial cholesterol metabolism under anoxic conditions.

95 conditions to mildly alkaline (pH 7-8.5) and anoxic conditions.

96 was rapidly biodegraded under oxic, but not anoxic conditions.

97 Sigma-Aldrich humic acid (HA), at pH 6 under anoxic conditions.

98 ycytidine and thymidine, respectively, under anoxic conditions.

99 and in combination, and under both oxic and anoxic conditions.

100 cross-links in duplex DNA selectively under anoxic conditions.

101 of paddy soil collected and processed under anoxic conditions.

102 to be mainly redox sensitive and promoted by anoxic conditions.

103 rm the strong retention of Sn(II) even under anoxic conditions.

104 s remain stable for at least 4 months, under anoxic conditions.

105 cherichia coli and purified the enzyme under anoxic conditions.

106 oparticles within 147 days when stored under anoxic conditions.

107 sumption by aerobic processes under apparent anoxic conditions.

108 that TMPD(*+) was formed from (3)CDOM* under anoxic conditions.

109 s growth substrates under oxic or even under anoxic conditions.

110 for debromination in the presence of nZVI in anoxic conditions; infinity in the case of catalytic oxi

111 by zero-valent iron nanoparticles (nZVI) in anoxic conditions; oxidative degradation by H2O2 in the

112 he P flux from the sediments under transient anoxic-conditions and to identify the relevant drivers.

113 urface layer fuel anaerobic processes in the anoxic core of AMZs, where 30-50% of global marine nitro

114 red how the physicochemistry and toxicity of anoxic Cu-amended sediments changed as they aged (i.e.,

115 H2 production was observed in dark anoxic cultures of diatoms (Fragilariopsis sp.) and a ch

116 ion of a bolus of nitric oxide injected into anoxic cultures without any other electron acceptors.

117 oxia, consistent with documented pathways of anoxic dark fermentation in microalgae.

118 and the existence of oxic shallow brine and anoxic deep brine layers.

119 ination of lethally warm, shallow waters and anoxic deep waters that acted to severely restrict the h

120 een well-oxygenated surface waters and fully anoxic deep waters.

121 tion, large amounts of methane accumulate in anoxic deep waters.

122 erature tolerant ostracods thrived except in anoxic deeper-waters.

123 stine/glutamate antiporter exhibited reduced anoxic depolarization and neuronal death in response to

124 depression, and provides novel insights into anoxic depolarization and the relevant cell swelling dur

125 h cortical spreading depression and terminal anoxic depolarization arose preferentially in the whiske

126 amics of seizures, spreading depression, and anoxic depolarization lie along a continuum of the reper

127 ng that demarcates spreading depression from anoxic depolarization.

128 At shallow anoxic depths, PA taxa were primarily affiliated with an

129 ulfide oxidation in waters mixed upward from anoxic depths.

130 2S oxidation in waters mixed upward from the anoxic depths.

131 As a method, anoxic dithionite titrations may further allow additiona

132 due to both a CO2-specific mechanism and an anoxic effect.

133 s significant amounts of O2 to the otherwise anoxic environment.

134 that HA can abiotically reoxidize sulfide in anoxic environments at rates competitive to sulfide oxid

135 th aqueous sulfide (termed sulfurization) in anoxic environments can substantially increase DOM's red

136 rends of U isotope fractionation in oxic and anoxic environments makes its isotope composition a usef

137 bacteria can adjust to life in both oxic and anoxic environments through differential expression of t

138 he interface of anaerobic/oxic and anaerobic/anoxic environments, and are often stimulated by an alte

139 recipitation of secondary Fe(II) minerals in anoxic environments, and suggest substantial complexity

140 eduction rates during the shift from oxic to anoxic environments, we found that AphB is also oxidized

141 e (Mn(3+) ) is a newly identified oxidant in anoxic environments, whereas acetate is a naturally abun

142 onditions as well as low oxygen, hypoxic and anoxic environments.

143 istributed organic matter into both oxic and anoxic environments.

144 bon cycling process that could take place in anoxic environments.

145 dissolved As(III) concentrations in suboxic-anoxic environments.

146 by which ethylene is produced by microbes in anoxic environments.

147 40 mEq/L, chronic liver disease, and hypoxic/anoxic episode.

148 significant degrader of hydrogen peroxide in anoxic Escherichia coli Intriguingly, ccp transcription

149 qPCR gene assays of samples spanning an oxic-anoxic-euxinic gradient.

150 The Toarcian Oceanic Anoxic Event (T-OAE) was characterized by a major distur

151 climatic warming across the Toarcian Oceanic Anoxic Event or T-OAE from an open ocean sedimentary suc

152 f enriched metals supports emerging 'oceanic anoxic event' models.

153 onmental upheaval, like the Cretaceous Ocean-Anoxic-Event-2 (OAE-2).

154 nd) in sediments from the Cretaceous Oceanic Anoxic Events and the Archean Eon.

155 eses, excluding the volcanism-driven oceanic anoxic events of the Early-Middle Triassic and Toarcian

156 and were even a feature of Phanerozoic ocean anoxic events.

157 s ranging from small ponds to global oceanic anoxic events.The role of microbial communities in regim

158 ance of research regarding acute and chronic anoxic exposure and cold stress, the literature is lacki

159 d where the alternation of aerobic-feast and anoxic-famine conditions accomplished the selection of P

160 tablished during a 73-day period by using an anoxic Fe(II)-rich nutrient solution, a U(VI) amended nu

161 Life originated in an anoxic, Fe2+-rich environment.

162 ecrease in O2 concentration, resulting in an anoxic feature at the SWI.

163 redox gradient in Saanich Inlet-a seasonally anoxic fjord with biogeochemistry analogous to oxygen mi

164 ied by in situ (15)NO2(-) tracer tests along anoxic flow paths in areas of varying ammonium, nitrate,

165 rms of AMPA receptor (AMPAR) plasticity - an anoxic form of long-term potentiation and a delayed incr

166 At native pH of 8.6, the anoxic fraction, despite its significant Fe(II), approxi

167 Oxic and anoxic fractions differ significantly in Fe(II) natural

168 VII mainly focused on their role to regulate anoxic gene expression, little is known on the impact of

169 In anoxic groundwater aquifers, the long-term survival of D

170 tem, aerobic respiration generally maintains anoxic groundwater below an oxic vadose zone until seaso

171 tive Fe protein in the cytosol requires both anoxic growth conditions and co-expression of NifH and N

172 ing successful acclimation to high light and anoxic growth environments and gives new insights into a

173 se activity and that EutQ is required during anoxic growth of S. enterica on ethanolamine and tetrath

174 noxic storage of polyphosphate and four-step anoxic growth on PHA using nitrate, nitrite, nitric oxid

175 t microbial methanogenesis can only occur in anoxic habitats.

176 , the reservoir was strongly stratified, and anoxic hypolimnion water with high methylmercury levels

177 rences in DOC quality among oxic epilimnion, anoxic hypolimnion, and sediment porewater.

178 e in the vertical extent and duration of the anoxic hypolimnion, which can represent the main source

179 ine is also neuroprotective in vitro against anoxic/hypoxic damage.

180 Infiltrating river water becomes anoxic in the uppermost aquifer due to the oxidation of

181 Consistent with this, anoxic incubation of a sediment core resulted in an accu

182 At the oxic/anoxic interface (OAI) of hyporheic zones subjected to r

183 taxa in both size fractions across the oxic-anoxic interface is consistent with the cryptic sulfur c

184 encounters the overlying vadose zone an oxic/anoxic interface is created, often near the capillary fr

185 axis that allows them to compete at the oxic-anoxic interface.

186 Natural oxic-anoxic interfaces are often sulfidic, including the inte

187 biologically and abiotically at natural oxic/anoxic interfaces.

188 ination of enhanced phosphorus scavenging in anoxic, iron-rich oceans and a nutrient-based bistabilit

189 ong-term recovery potential in patients with anoxic-ischemic encephalopathy.

190 We used anoxic laboratory incubations to estimate anaerobic CO2

191 ductivity and by slow decomposition in cold, anoxic lake bottoms.

192 the oxycline (< 1-120 microM O2 ) and upper anoxic layer.

193 The deeper anoxic layers of smooth mats were dominated by Chlorofle

194 fera-like bacteria showed a distinct peak in anoxic layers that coincided with the zone of methane ox

195 ession of Dinoroseobacter shibae DFL12(T) to anoxic life by a combination of metabolome, proteome, an

196 ironmental conditions (temperature, pH, oxic/anoxic, light, and concentration and characteristics of

197 c AMPA receptor (AMPAR) plasticity - namely, anoxic long-term potentiation (a-LTP), and a delayed inc

198 from the hypoxic epithelium adjacent to the anoxic lumen to the relative higher tissue oxygenation a

199 r system was developed to assess oxic versus anoxic manipulations on in situ groundwater communities.

200 s indicate energy-based selection typical of anoxic marine sediments, 5-15% of taxa per sample exhibi

201 layer and the anaerobic core in nitrite-rich anoxic marine zones (AMZs), which constitute huge oxygen

202 m well-mixed holomictic lakes to stratified, anoxic, meromictic lakes that vary in their vertical ext

203 nd cannot be compensated by any other AEF or anoxic metabolic responses.

204 we primarily discuss the intricacies of dark anoxic metabolism in Chlamydomonas, but also discuss asp

205 imulation to achieve CF detoxification using anoxic microcosms established with aquifer material from

206 production of Arctic peat soil microbiota in anoxic microcosms over a temperature gradient from 1 to

207 In anoxic microcosms, 300 mug/L cis- and 150 mug/L trans-4-

208 ss and evenness was typically highest in the anoxic monimolimnion of meromictic lakes, with common ma

209 Elevated solution concentrations of As in anoxic natural systems are usually accompanied by microb

210 hesis that methane in bubbles is produced in anoxic near-stream sediment porewaters, and not in deepe

211 in the oxic zone, suggests putative surface anoxic niches in these microbial mats.

212 or these systems suggesting putative surface anoxic niches, differential nitrogen fixing niches, and

213 Coupled aerobic-anoxic nitrous decomposition operation (CANDO) is a prom

214 The coupled aerobic-anoxic nitrous decomposition operation is a new process

215 In contrast to elsewhere, we show that anoxic non-sulfidic (ferruginous), rather than euxinic,

216 Total ice cover would make an anoxic ocean likely, and would be a formidable barrier t

217 Circulation in an initially salty and anoxic ocean, restricted by the topography of the Falkla

218 or MBT and/or CBT for reconstructing pH, in anoxic or euxinic lakes, estuaries and ocean basins.

219 has focussed on the identification of fully anoxic or oxic conditions, rather than intermediate redo

220 gradation of various organic compounds under anoxic or oxic conditions.

221 ancient redox chemistries, extending from an anoxic origin through the GOE and ultimately to obligate

222 ed when assessing P mobility under transient anoxic-oxic conditions, which would derive from pH gradi

223 Anoxic peat samples were collected from a near-surface (

224 an Fe(II) concentration plateau within each anoxic period.

225 n of a lag phase in nitrate production after anoxic periods is a promising approach to suppress nitri

226 nitritation-anammox plants was subjected to anoxic periods of 5-60 min.

227 lag phase in nitrate production after short anoxic periods was performed with varied temperatures an

228 ion signatures at 20-day SRT: anaerobic-oxic-anoxic periods were the primary driver of rRNA similarit

229 were subject to alternating 48-h aerobic and anoxic periods, in which CH4 and NO2(-) were added toget

230 crease the contaminant concentrations in the anoxic plume beneath the vadose zone.

231 When anoxic polluted groundwater encounters the overlying vad

232 radual environmental changes can induce oxic-anoxic regime shifts mediated by microbial community dyn

233 tion or global warming can induce major oxic-anoxic regime shifts.

234 cation intermediate, from the aerobic to the anoxic regions of the biofilm.

235 In the anoxic regions, hydroxylamine oxidation by AOB provided

236 rocesses to sustain growth, development, and anoxic resistance of plants.

237 bohydrate reserves also led to a decrease in anoxic resistance, which was prevented by external Suc s

238 ed (5-60 degrees C) water quality changes in anoxic sandy sediments.

239 of the microbial community in the seemingly anoxic SCM revealed the enhanced expression of genes for

240 The degradation of organic matter in the anoxic seabed proceeds through a complex microbial netwo

241 also identified two small microniches in the anoxic sediment below the SWI, defined by elevated trace

242 ation, migrating Chaoborus spp. dwell in the anoxic sediment during daytime and feed in the oxic surf

243 Rates of Sb(V) reduction in anoxic sediment microcosms and enrichment cultures were

244 ion, we injected dissolved aluminum into the anoxic sediment of a eutrophic semienclosed bay in the B

245 s consisted of methane production within the anoxic sediment, followed by diffusive flux and ebulliti

246 es including an oral biofilm, freshwater and anoxic sediment.

247 trations of Sb(V) to Sb(III) was observed in anoxic sediments from two freshwater settings: (1) a Sb-

248 e minerals and the ferric Fe-bound P pool in anoxic sediments in the Chesapeake Bay.

249 The majority of methane produced in many anoxic sediments is released via ebullition.

250 stal areas, permanent binding of mobile P in anoxic sediments may be needed together with measures in

251 The anoxic sediments of the White Oak River estuary comprise

252 bioremediation potential; however, the oxic-anoxic sediments supported a greater sea cucumber biomas

253 umulates in the tetravalent state, U(IV), in anoxic sediments, such as ore deposits, marine basins, a

254 g bacteria, which were prevalent in the oxic-anoxic sediments.

255 ric Fe-bound P pool can be a major P sink in anoxic sediments.

256 aringly soluble mineral uraninite (UO2+x) in anoxic sediments; however, studies now show that this is

257 Activated sludge was sampled from an anoxic selector of a municipal wastewater treatment plan

258 n liver and gills than fish reared in silty, anoxic sites.

259 By conducting anoxic slurry incubations with lake sediments amended wi

260 res of the drained areas were lower in deep, anoxic soil layers (below 30 cm), but higher in oxic top

261 A comparison of oxic to anoxic soils reveal up to ten times greater methane prod

262 In anoxic solution, CdTe dissolved at a finite rate.

263 Fe(II) added to anoxic solutions of as-received NOM oxidized to Fe(III)

264 oxic state dominated by cyanobacteria and an anoxic state with sulfate-reducing bacteria and phototro

265 ysteresis in the transition between oxic and anoxic states with similar changes in microbial communit

266 s are related to wine metal composition; (4) anoxic storage brings about an increase of free forms, a

267 In this model, the four-step anoxic storage of polyphosphate and four-step anoxic gro

268 lopment of H2S and methanethiol (MeSH) along anoxic storage of wines, 24 wines were stored in strict

269 t which free H2S (not MeSH) increases during anoxic storage.

270 g processing of tea leaves, a combination of anoxic stress and mechanical damage are essential for th

271 s of CsGAD2 mRNA induced by a combination of anoxic stress and mechanical damage.

272 We demonstrated fatal vulnerability to anoxic stress at a specific time in postnatal life induc

273 spectively, which were likely related to the anoxic stress on soil microbes and decreased photosyntha

274 , the literature is lacking evidence linking anoxic stress with variable environmental conditions suc

275 During exposure to anoxic stress, fruit flies and other poikilotherms enter

276 and wet environments increase resistance to anoxic stress.

277 ediments from this period, which requires an anoxic surface environment, implies that there may have

278 sorption of Fe(II) with As(III) and As(V) in anoxic suspensions of gamma-Al2O3 at pH 7.5 was investig

279 n the solubility and speciation of Zn(II) in anoxic suspensions of hexagonal birnessite at pH 6.5 and

280 ically lowered the availability of As in the anoxic systems studied.

281 d sites, on UO2 dissolution in both oxic and anoxic systems were investigated using batch and continu

282 ; 16 traumatic, 32 non-traumatic of which 13 anoxic, three mixed; 35 patients assessed >1 month post-

283 vious estimates that the deep ocean remained anoxic throughout the GOE.

284 e Earth's atmosphere as it transitioned from anoxic to highly oxic (1-2 billion years ago), a change

285 tipping points are a common feature of oxic-anoxic transitions, causing rapid drops in oxygen levels

286 no significant effect of thermocline depth, anoxic water volume, interface area of oxic-anoxic water

287 anoxic water volume, interface area of oxic-anoxic water, and sediment area in contact with anoxic w

288 xic water, and sediment area in contact with anoxic water.

289 ove the halocline and high concentrations in anoxic waters (1249 +/- 369 fM).

290 nthesis of acoustic data to show that, where anoxic waters occur within the water column, most migrat

291 nd micronekton migrating from the surface to anoxic waters.

292 oceans while the atmosphere itself remained anoxic with its attendant S-MIF signature.

293 ining delta(15)N trend that implies that the anoxic zone was shrinking for most of the 20th century.

294 carbon (C), mostly buried in deep, saturated anoxic zones (catotelm).

295 rate that worldwide expansion of euxinic and anoxic zones are symptoms of increased biological carbon

296 SMFC employment facilitated the formation of anoxic zones in sediments with oxygen loss and exudates

297 nvironment from consumer products, occurs in anoxic zones of urban wastewater systems and that sulfid

298 ry sulfide minerals are known to nucleate in anoxic zones, by reaction of the thiol-bound mercury wit

299 d by climate change and expansion of oceanic anoxic zones.

300 ater environments if nitrate is available in anoxic zones.