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 rated under stable aerobic (+195 +/- 25 mV), anoxic (-15 +/- 50 mV), and anaerobic (-195 +/- 15 mV) c

4 n be photochemically oxidized by light under anoxic, abiotic conditions.

5 alysts using both doping and annealing under anoxic ambient.

6 ate and As species [As(III) and As(V)] under anoxic and circum-neutral pH conditions through scanning

7 from this study demonstrate that fluctuating anoxic and euxinic conditions could have been potentiall

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

9 ozoic (1.8-1.0 Ga), the ocean was suboxic to anoxic and multicellular organisms had not yet evolved.

10 s typically form at the interface of euxinic/anoxic and oxic conditions.

11 istory, the ocean's interior was pervasively anoxic and showed occasional shifts in ocean redox chemi

12 were mostly absent in sediments overlain by anoxic and sulfidic bottom waters, emphasizing their dep

13 e for deposition in marine environments with anoxic and sulfidic bottom waters.

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

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

16 tratum (4 m and below) that is euxinic (i.e. anoxic and sulphidic).

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

18 from the SUP05 clade under high DO (22 muM), anoxic, and low DO (3.8 muM) concentrations.

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

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

21 n active arsenic biogeochemical cycle on the anoxic Archean Earth.

22 Here we argue that, in the anoxic Archean oceans, pyrite could form in the absence

23 at 7 hPa, 0 degrees C, and a CO(2)-enriched anoxic atmosphere (called low-PTA conditions) was tested

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

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

26 I sediments incubated under fluctuating oxic/anoxic atmosphere.

27 balance calculations, constrained by modern anoxic basins, suggest that deep-water phosphate concent

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

29 The study reveals that anoxic bottom-water conditions, often with toxic hydroge

30 ized sedimentary record (1735-1999) from the anoxic-bottom waters of the Pettaquamscutt River basin,

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

32 ted hazard ratio, 0.98; 95% CI [0.96-0.99]), anoxic brain injury (3.55 [1.2-10.5]), aspiration (2.29

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

34 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 </=

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

36 s are more likely to arrive with more severe anoxic brain injury, but this does not account for all t

37 ified 36 ideal heart donors, 24 (66.7%) with anoxic brain injury.

38 Subsea hypersaline anoxic brine pools are among the most extreme habitable

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

40 depth transects in the Adriatic Sea, and the anoxic Cariaco Basin.

41 2-2015 (aHR, 0.58; P = 0.001) and donor with anoxic cause of death (aHR, 0.51; P = 0.007) were associ

42 012-2015 (aHR, 0.58; P=0.001) and donor with anoxic cause of death (aHR, 0.51; P=0.007) were associat

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

44 more likely to exhibit signs of early severe anoxic changes on CT or electroencephalogram, higher cre

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

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

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

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

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

50 ides is likely important under circumneutral anoxic conditions and in sunlit environments.

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

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

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

54 sands may be exposed to alternating oxic and anoxic conditions but the effect of this tidally induced

55 atlas of putative interactions, we show that anoxic conditions can promote mutualisms by providing mo

56 ng Mn(II)-bearing delta-MnO(2) at pH 8 under anoxic conditions for 25 d (dissolved Mn < 11 muM).

57 f N(2) O and NO increase significantly under anoxic conditions for AM soil (30- and 120-fold increase

58 ediment, where they were exposed to dark and anoxic conditions for ~75% of the day.

59 gradients of nitrate and ciprofloxacin under anoxic conditions in order to evaluate the ability of Sh

60 eous H(2)V(V)O(4)(-) (100 muM) removal under anoxic conditions in suspensions (2.0 g L(-1)) of magnet

61 n with Dehalococcoides mccartyi to establish anoxic conditions in the aquifer.

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

63 eservoirs that seasonally stratify, creating anoxic conditions in the hypolimnion that promote methyl

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

65 quencing (seq) of copepods exposed to nearly anoxic conditions showed differential expression of over

66 require sufficiently high organic loads and anoxic conditions to deliver a stable baseline current.

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

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

69 The biological consumption of ethane under anoxic conditions was suggested by geochemical profiles

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

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

72 However, by retaining nitrates in anoxic conditions within the soil profile, SI could pote

73 deteriorating environments (cool, arid, and anoxic conditions) and climate fluctuations across the P

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

75 3 was subject to microbial degradation under anoxic conditions, and chlorotrifluoroethene (CTFE) was

76 The catalytic effect persisted under anoxic conditions, but decreased as soon as air or phena

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

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

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

80 ion products with 50 muM of antimonite under anoxic conditions.

81 lay minerals did not reduce PCE or TCE under anoxic conditions.

82 sumption by aerobic processes under apparent anoxic conditions.

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

84 cherichia coli and purified the enzyme under anoxic conditions.

85 oparticles within 147 days when stored under anoxic conditions.

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

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

88 d biofilm aggregate populations experiencing anoxic conditions.

89 germination and early seedling growth under anoxic conditions.

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

91 decomposed organic matter under waterlogged anoxic conditions.

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

93 robial activity, or biomass production under anoxic conditions.

94 that BPA is susceptible to degradation under anoxic conditions.

95 e waste repositories, was investigated under anoxic conditions.

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

97 silica at pH = 9, room temperature and under anoxic conditions.

98 oil decomposition rates even after prolonged anoxic conditions.

99 luxes and in situ primary productivity under anoxic conditions.

100 ioneine also plays physiological roles under anoxic conditions.

101 hanolic fermentation as the severely hypoxic/anoxic core became a progressively greater proportion of

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

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

104 es in oil-contaminated sediments during oxic-anoxic cycles in laboratory chambers that closely emulat

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

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

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

108 betaine, we demonstrate that MtpB catalyzes anoxic demethylation of proline betaine.

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

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

111 2S oxidation in waters mixed upward from the anoxic depths.

112 ulfide oxidation in waters mixed upward from anoxic depths.

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

114 recipients of organs from donors who died of anoxic drug overdose and recipients of organs from donor

115 the current opioid epidemic, utilization of anoxic drug overdose DCD donor grafts does not increase

116 ure at 5 years was similar for recipients of anoxic drug overdose donor grafts and recipients of othe

117 Grafts from anoxic drug overdose donors were less frequently used co

118 ents received grafts from donors who died of anoxic drug overdose.

119 The Archean Eon was a time of predominantly anoxic Earth surface conditions, where anaerobic process

120 and assembled core metabolic pathways on an anoxic Earth.

121 Anoxic encephalopathy was most frequent and P-PASS highe

122 arachnoid hemorrhage, and postcardiac arrest anoxic encephalopathy were selected.

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

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

125 or of this toxic redox-sensitive oxyanion in anoxic environments is poorly constrained.

126 e ammonia to nitrite, whereas in hypoxic and anoxic environments reduction of both ammonia-derived ni

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

128 o facilitate microbial goethite reduction in anoxic environments where electron transfer between cell

129 In anoxic environments, soluble hexavalent uranium (U(VI))

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

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

132 should be effectively irreversible in these anoxic environments, which differ greatly from shallow o

133 on the electron transfer process in natural anoxic environments.

134 management facility (TMF) featuring oxic and anoxic environments.

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

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

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

138 erefore, limit dissolved V concentrations in anoxic environments.

139 and diversification of the group in various anoxic environments.

140 open ocean waters appears less restricted to anoxic environments.

141 40 mEq/L, chronic liver disease, and hypoxic/anoxic episode.

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

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

144 tense deoxygenation such as Cretaceous ocean anoxic event (OAE) 2, a few regional sedimentary delta(1

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

146 f the supposed hyperthermal Toarcian Oceanic Anoxic Event (T-OAE, Early Jurassic, c.

147 The Toarcian Oceanic Anoxic Event (TOAE, Early Jurassic, ~182 Ma ago) was cha

148 e rock represents the later stage of Oceanic Anoxic Event 2.

149 Characterization of the Hirnantian ocean anoxic event has focused on the onset of anoxia, with gl

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

151 sic-Jurassic transition and Toarcian Oceanic Anoxic Event, are well studied and largely associated wi

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

153 hylhopanoids deposited during Mesozoic ocean anoxic events (OAEs) and other intervals has been interp

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

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

156 ably longer than well-studied Mesozoic ocean anoxic events.

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

158 in the middle Atdabanian and after the Sinsk anoxic extinction event, starting ca. 513 Ma.

159 In the anoxic Fe(2+)-rich early oceans, these minerals would ha

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

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

162 Phosphorus speciation data show that, whilst anoxic ferruginous conditions were initially conducive t

163 osynthesis appeared, the atmosphere remained anoxic for hundreds of millions of years until the ~2.4

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

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

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

167 ts of the Belgium coastal zone (BCZ) and the anoxic Gotland basin (GB).

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

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

170 ng dissolved oxygen and nitrate with deeper, anoxic groundwater containing dissolved iron (Fe(II)) an

171 er, their possible role as sources of As for anoxic groundwaters remains unexplored.

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

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

174 form cohort of taxa adapted to thrive in the anoxic gut and disperse between anoxic patches as oxygen

175 nal step of microbial biomass degradation in anoxic habitats.

176 t microbial methanogenesis can only occur in anoxic habitats.

177 cells performing sulfide oxidation in deeper anoxic horizons have a high assimilation rate, whereas c

178 unrecognized role in MeHg production in the anoxic hypolimnion of freshwater lakes.

179 to 72 muM day(-1) ) methane oxidation in the anoxic hypolimnion of the temperate Lacamas Lake (Washin

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

181 tion of CFC-113 to cis-DFE is feasible under anoxic in situ conditions.

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

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

184 Oxic and anoxic incubations both showed active methane oxidation

185 In anoxic incubations, Methylobacter cell numbers increased

186 of the redoxcline and a reduced frequency of anoxic incursions onto the inner to mid-ramp is recorded

187 elation, Ni enrichments, and the absence of 'anoxic indicators' (no biomarkers, no framboids, low Mo

188 MYDGF mediates cardiac repair in mice after anoxic injury.

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

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

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

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

193 hemical oxidation of reduced species at oxic-anoxic interfaces, H(2) O(2) production by lactic acid b

194 biologically and abiotically at natural oxic/anoxic interfaces.

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

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

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

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

199 vo kidney perfusion (NEVKP) with hypothermic anoxic machine perfusion (HAMP) and static cold storage

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

201 o Basin subeuphotic zone, one of the largest anoxic marine basins worldwide.

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

203 In several modern anoxic marine systems concentrations of As(V) are higher

204 is a metabolic pathway actively utilized in anoxic marine water columns.

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

206 rahydrofolate represents the first described anoxic mechanism of proline betaine demethylation.

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

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

209 se results support the presence of localized anoxic microsites in the otherwise aerobic porous bulk s

210 inerals undergo reductive dissolution inside anoxic microsites of primarily unsaturated soil, which m

211 postulate that solid-phase iron reduction in anoxic microsites present in the rhizosphere of unsatura

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

213 r GAS skin tropism in which GAS generates an anoxic niche to evade phagocyte NADPH oxidase-mediated c

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

215 These results demonstrate that under anoxic, nitrate-reducing conditions, motility can contro

216 The coupling of anoxic nitrogen (N) cycling to the function of HSs as a

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

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

219 tent with an oxygen oasis in the Mesoarchean anoxic ocean, but delta(15)N data indicate a Mo-based di

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

221 largely in the form of As(III) in the early anoxic ocean.

222 In early anoxic oceans, especially during periods of high marine

223 this is normoxic (OHM1), hypoxic (OHM2), or anoxic (OHM3).

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

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

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

227 id/compact particles, and aggregates with an anoxic or oxic interior.

228 hrive in the anoxic gut and disperse between anoxic patches as oxygen-tolerant spores.

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

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

231 eterotrophic bacteria had a dual role in the anoxic phase and could be responsible for both net N(2)O

232 inly to the N(2)O production/emission in the anoxic phase and the accumulation of N(2)O to be signifi

233 Therefore, properly extending the length of anoxic phase could serve as a potential control means to

234 means to regulate N(2)O accumulation in the anoxic phase.

235 es promoted oil biodegradation in subsequent anoxic phases by microbially mediated reoxidation of alt

236 sed concepts of control over the aerobic and anoxic phases collectively.

237 were observed in the oxic as compared to the anoxic phases with a relatively constant ratio between a

238 When anoxic polluted groundwater encounters the overlying vad

239 ns and oxidative weathering under ostensibly anoxic Precambrian atmospheres.

240 e oxidation by a Methylobacter species, with anoxic rates being threefold higher.

241 This, in turn, further decreased anoxic recycling of bioavailable phosphorus to the water

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

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

244 No substantial change in the anoxic relaxation rate and a slight decrease in pO(2) se

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

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

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

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

249 es dominate the otolith (ear bone) record in anoxic sediment layers of the Santa Barbara Basin over t

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

251 Two lineages are widespread among anoxic, sedimentary environments, whereas Ca.

252 e most of the upward ammonium flux from deep anoxic sediments is being consumed.

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

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

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

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

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

258 ied two populations of U (dominantly +IV) in anoxic sediments.

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

260 crobial degradation of aromatic compounds at anoxic sites, catalyze a biological Birch reduction beyo

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

262 By conducting anoxic slurry incubations with lake sediments amended wi

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

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

265 noparticles (CoS.xH(2)O) that were stable in anoxic solution for 2 months, with estimated log K* valu

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

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

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

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

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

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

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 e impact of GR phases on As sequestration in anoxic subsurface environments.

275 otential locations of MeHg production in the anoxic, sulfidic hypolimnion of a freshwater lake.

276 r precipitates, peat NOM can sequester Sb in anoxic, sulfur-enriched environments.

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

278 and in higher concentrations in slow-flowing anoxic systems as degassing mechanisms are not strong.

279 occurrence of fine-grained Fe(3)S(4) in many anoxic terrestrial settings.

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

281 onation were observed in Fe(II)- and Mo-rich anoxic TMF seepage, while attenuation and isotope fracti

282 area of northeastern Panthalassa experienced anoxic to euxinic bottom water conditions in the direct

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

284 ophic bacteria are mostly active at the oxic-anoxic transition zone in stratified lakes, where they u

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

286 Cells were amended into anoxic tubes buffered at pH 7.0, with initial 100 muM DN

287 sociated with succinate accumulation in both anoxic turtles and ischemic mouse hearts.

288 nganese oxides in the photic zones of modern anoxic water bodies and sediments.

289 in groundwater are associated with shallow, anoxic water tables and soils enriched in organic carbon

290 etagenomes along a gradient of oxygenated to anoxic waters (<0.02 mumol/l O(2) ) in the Eastern Tropi

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

292 bacteria from the SUP05 clade often dominate anoxic waters within marine oxygen minimum zones (OMZs)

293 In anoxic waters, which composed most of the Paleoproterozo

294 inery and metabolic network stability in the anoxic world.

295 d beta diversity of viral communities in the anoxic zone were lower than in surface waters, which par

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

297 as a stabilizing feedback between expanding anoxic zones and atmospheric carbon dioxide.

298 n by partial and complete denitrification in anoxic zones in organic aggregates.

299 e examined across the oxycline, suboxic, and anoxic zones of the Cariaco Basin, Venezuela.

300 teria consortia in the pumping well oxic and anoxic zones, including autotrophic iron-oxidizing bacte