ライフサイエンスコーパス: seawater

1 in serpentinizing fluids derived from modern seawater.

2 n edible mussels bred in polluted artificial seawater.

3 to grow in salt concentrations near that of seawater.

4 FA as hydrolysis products to the surrounding seawater.

5 he PAO fiber, in bacteria-containing natural seawater.

6 uct in the organic-rich interfacial layer of seawater.

7 s focardii, endemic of the Antarctic coastal seawater.

8 ontaminants in sea ice grown from artificial seawater.

9 serpentine alteration to authigenic clays by seawater.

10 es nonlinearly with the amount of biomass in seawater.

11 and fast detection of toxic contaminants in seawater.

12 r distinct layers of snow, sea ice brine and seawater.

13 factants in mPMA and those in the associated seawater.

14 of healthy coral reefs and their surrounding seawater.

15 mg g(-1) in 32 ppm uranium-spiked simulated seawater.

16 arine Vibrio species depend on for growth in seawater.

17 he atmosphere than to underlying sea ice and seawater.

18 e (e.g., Cu(2+)) ions naturally occurring in seawater.

19 by field observations of anthropogenic Fe in seawater.

20 ce and control mineralization separated from seawater.

21 regions relative to those in the associated seawater.

22 ltifunctional GBT uptake systems observed in seawater.

23 tion of their calcifying fluid above that of seawater.

24 n snowmelt due to snowpack releasing POPs to seawater.

25 ting oxygen deficiency and ammonification of seawater.

26 for the study of micro- and nanoplastics in seawater.

27 are the most abundant biological entities in seawater.

28 ies and the deep ocean than in the overlying seawater.

29 bent for uranium extraction from the natural seawater.

30 wide salinity range from fresh water to > 3x seawater.

31 for calcite or aragonite precipitating from seawater.

32 bundance, which differs from the surrounding seawater.

33 take and release of copper ions from natural seawater.

34 ugh the circulation of subseafloor fluids or seawater.

35 e samples, and model solutions of artificial seawater.

36 sociated with the analysis of Pb isotopes in seawater.

37 m (FTS) featuring partially filtered natural seawater.

38 Methylglyoxal slowly photodegraded in seawater (~0.001-0.03 nmol L(-1) h(-1)), whereas acetald

39 ase seawater (7)Li/(6)Li and retain constant seawater (10)Be/(9)Be over the past 16 million years.

40 or human feces, as the most abundant sterol (seawater: 45.1-20.3 ng L(-1); surface sediment: 90.2-70.

41 ecrease atmospheric carbon dioxide, increase seawater (7)Li/(6)Li and retain constant seawater (10)Be

42 Hormones associated with seawater acclimation (adrenocorticotropic hormone, corti

43 omatic hydrocarbons (PAHs) dispersed in LSMD seawater accommodated fractions (WAFs) and assesses the

44 However, seawater acidity alone provides an incomplete constraint

45 For the practical extraction of uranium from seawater, adsorbents with high adsorption capacity, fast

46 Seawater-air fugacity ratios were highly correlated with

47 a Y-maze chamber to test whether reduced-pH seawater altered the orientation of spiny lobster puerul

48 s of komatiites, these results indicate that seawater-altered lithosphere recycling into the deep man

49 ritea japonica) were incubated in autoclaved seawater amended with tetrapeptide alanine-valine-phenyl

50 ilm-forming 'species' that are undetected in seawater analyses, increasing the known microbial divers

51 nac as a potentially emerging contaminant in seawater and also than that of a conventional colorimetr

52 ntribute to the black carbon and nitrogen in seawater and are worthy of future investigation.

53 fully applied to quantify A. minutum AL9T in seawater and brackish water samples proving that it can

54 k to produce freshwater from brackish water, seawater and brine solutions, addressing the key environ

55 and seasons, being found at trace levels in seawater and gonads, with low risk for consumers.

56 Pu concentrations in seawater and groundwater samples, synthetic urine, and d

57 Isotope ratios of Pb in seawater and in the soluble fraction of Pb in atmospheri

58 palm seedlings were exposed to flooding with seawater and its major constituents under controlled con

59 Diel variability in concentrations of seawater and mPMA surfactants in some regions is consist

60 , we report new data for 21 targeted PFAS in seawater and plankton from the coast, shelf, and slope o

61 Air, snow, the fugacity in soils and snow, seawater and plankton were sampled concurrently from lat

62 e recoveries of 1 ng/g Se were obtained from seawater and river water, and 1 ng/g Se could be quantif

63 Marine microalgae within seawater and sea ice fuel high-latitude ecosystems and d

64 that bacteria are key DMSP producers in deep seawater and sediment.

65 These include exposure from polluted seawater and sediments and/or additional trophic transfe

66 s lower at etching sites compared to ambient seawater and the sponge's tissue.

67 d Zn) in subglacial meltwaters compared with seawater and typical riverine systems, together with the

68 Up to 42 out of 48 (in seawater) and 27 out of 37 (in biota) target analytes we

69 result in the entrainment of chemicals from seawater, and concentration profiles in bulk ice general

70 total suspended particulate (TSP) aerosols, seawater, and suspended and sinking particles in the Gul

71 sions were consistently lower for artificial seawater (AS) than buffered potassium iodide (KI) soluti

72 ; open-air, buried in soil, and submersed in seawater, as well as in controlled laboratory conditions

73 icantly higher than the oxygen saturation in seawater at the contemporary atmospheric pO(2) levels.

74 propriate for determination of diclofenac in seawater at the levels endorsed by the EU regulation.

75 large volume pumps by filtering 218-561 L of seawater at two to four depth strata (near-surface, ~300

76 of marine phytoplankton were inoculated with seawater bacterial assemblages, and communities were tra

77 s are distinct among sponge species and from seawater bacterial communities, indicating a key role of

78 A novel seawater-based pretreatment process was developed to imp

79 er 2016, model PMA (mPMA) were produced from seawater by bursting bubbles at two biologically product

80 pp. chemical cues than pueruli in ambient-pH seawater by comparing the proportion of individuals that

81 ural motifs are photo-oxidized on artificial seawater by the use of a solar simulator.

82 N (SSA) correlates weakly with seawater c(p,660) (R = 0.36, P << 0.01), but the correla

83 We find that seawater calcium concentration, by strongly influencing

84 We show that interstitial seawater can reduce fracture-driving stress by orders of

85 efore, reduced iodine emissions from natural seawater cannot be explained by chemical losses of I(2)

86 change drivers, such as temperature, pH and seawater carbonate chemistry, and dissolved oxygen, can

87 O(2)) emitted by human activities alters the seawater carbonate system.

88 to six locations across a natural mosaic in seawater chemistry throughout Hawai'i and fragmented int

89 Projected changes in seawater chemistry will have catastrophic biotic effects

90 nic carbon (DIC) allows them to modify local seawater chemistry, creating gradients in carbon, pH, an

91 patches retained the ability to alter local seawater chemistry.

92 his study, we combine a recent observational seawater CO(2) data product, i.e., the 6(th) version of

93 ynthesis are likely to benefit from elevated seawater CO(2) levels due to ocean acidification.

94 yi lysates, and were conducted using surface-seawater collected from the South Pacific Subtropical Gy

95 o atmospheric communities than to sea ice or seawater communities.

96 69.19 +/- 0.11% and 63.03 +/- 0.04% sugar in seawater compared with 52.82 +/- 0.16%, 45.93 +/- 0.37%

97 in these systems, and how secular changes in seawater composition may have modified serpentinization-

98 Surface seawater concentrations did not exhibit day-night differ

99 solutions between pH ~6.5 and >12 at modern seawater concentrations of NaCl, Mg(2+) and Ca(2+).

100 t uranium uptake may depend greatly upon the seawater concentrations of other elements such as vanadi

101 The results suggest that the variability in seawater concentrations of PFAAs has little influence on

102 ariability but remain relatively constant as seawater conditions change.

103 The assessment of antibiotics mobility under seawater conditions has been rarely studied, as an accur

104 mportance of physiological regulation versus seawater conditions in controlling coral calcifying flui

105 20 per mille) in the sample characterized by seawater conditions, whereas higher values (~25-27 per m

106 urface complexation constants obtained under seawater conditions.

107 an has been documented on reefs under normal seawater conditions.

108 by these phytoplankton to extract iron from seawater constrain carbon flux into higher trophic level

109 mPMA from biologically productive seawater contained higher concentrations of surfactants

110 Preadult copepods were incubated in seawater containing a mixed assemblage of cultured micro

111 ment is predominantly controlled by enhanced seawater content in suture zones, rather than by enhance

112 ice-penetrating radar data can quantify the seawater content of suture zones and their modification

113 e exchange of calcifying fluid with external seawater, contributes to some variability but remain rel

114 high-temperature hot-spring fluids with cold seawater creates intermediate-temperature diffuse fluids

115 pe fractionation, suggesting that increasing seawater delta(18)O over time was the primary cause of t

116 ns of paleo-oceanographic reconstructions of seawater delta(26)Mg and Mg/Ca ratios.

117 These new data, along with the constant seawater delta(26)Mg over the past ~20 Myr, require a si

118 water samples (groundwater, river water, and seawater) demonstrated the applicability of the method.

119 This study provides evidence that ambient seawater density influences calcification and may accoun

120 ody extends up to 60 km from the coast and a seawater depth of 110 m.

121 h's accretion and by subsequent recycling of seawater-derived neon in plate tectonic processes.

122 The rising use of seawater desalination for fresh water production is driv

123 2) s(-1)), good cycling stability, and rapid seawater desalination performance under typical OLC-FCDI

124 great potential for wastewater treatment and seawater desalination with high energy conversion and ut

125 en energy, but also of great significance to seawater desalination.

126 ormula: see text]C-decoupling between global seawater DIC and shallow carbonate, without burying orga

127 We designed seawater dilution experiments to assess the effect of pC

128 The naturally elevated seawater dissolved inorganic carbon concentration at thi

129 nd use them to calculate relative changes in seawater-dissolved inorganic carbon (DIC) concentration,

130 reflects the [Formula: see text]C of global seawater-dissolved inorganic carbon (DIC).

131 , our Mariana Trench study reveals a typical seawater DMSP/dimethylsulfide (DMS) profile, with highes

132 etabolisms are likely supported by shallower seawater-dominated circulation.

133 ached chemicals from plastic into artificial seawater during simulated UV-induced weathering.

134 ry significantly advances the development of seawater electrolysis for large-scale hydrogen productio

135 The implementation of seawater electrolysis requires robust and efficient elec

136 gen evolution reaction catalyst for alkaline seawater electrolysis.

137 terrenal axis, and that relaxed selection on seawater entry traits has decreased this stimulation in

138 migration and pre-adapts juvenile salmon for seawater entry.

139 Seawater exposure increased Na and Cl contents in leaves

140 Reduced transpiration upon seawater exposure may contribute to controlling the move

141 hat date palm seedlings are tolerant towards seawater exposure to some extent, and highly tolerant to

142 intain plasma homeostasis in fresh water and seawater fish are well known, the corresponding molecula

143 Seawater flooding significantly reduced CO(2) assimilati

144 ltured in (13)C-labelled enriched artificial seawater for 0-12 h, and the algae were collected every

145 octanoic acid (PFOA), was detected in Arctic seawater for the first time.

146 mperature and oxygen isotopic composition of seawater from 1982 to 2016, based on paired oxygen isoto

147 reduce the boron concentration in synthetic seawater from 2.91 to <0.5 ppm in less than 3 min at an

148 ons were observed in biologically productive seawater from Georges Bank and coastal Rhode Island comp

149 Seawater from the highly protected 'crown jewel' offshor

150 Seawater from the less protected system of Los Canarreos

151 ts (WBCs) redistribute heat and oligotrophic seawater from the tropics to temperate latitudes, with s

152 hytoplankton-derived sulfur metabolites into seawater, from which they are rapidly assimilated by mar

153 n reducing hydrothermal fluids and oxidizing seawater, harnessing this energy to fix inorganic carbon

154 The Nd isotope composition of seawater has been used to reconstruct past changes in th

155 By contrast, the seawater-Hephaestus brine interface has been shown to ac

156 rifying abundant alternative sources such as seawater, high-salinity processed water, or underground

157 sses of methyl halides (CH(3)X) in fresh and seawater: hydrolysis and halide exchange.

158 (-2) h(-1) are achieved in purifying natural seawater in a closed system.

159 Overall, using seawater in hydrolysis of seaweed increased sugar hydrol

160 c acid inhibits aragonite precipitation from seawater in vitro, at the pH, saturation state and appro

161 Culture and seawater incubations, however, indicate oxygen isotopic

162 rvations of reservoir souring following cold seawater injection.

163 ng in subsurface oil reservoirs subjected to seawater injection.

164 iction of the fate of quinolones in sediment-seawater interface systems.

165 selective transfer of organic compounds from seawater into the atmosphere.

166 n-based assessment of the scope of potential seawater intrusion exists.

167 Seawater intrusion into coastal aquifers can increase gr

168 Seawater intrusion is particularly likely where water ta

169 water demands will exacerbate the threat of seawater intrusion.

170 along coast lines, date palms are exposed to seawater inundation and, hence, combined stress by salin

171 luid-buffered diagenesis that occurred where seawater invaded the sediment in response to geothermal

172 Increasing seawater iron brought about more robust bonding.

173 s were conducted using live mussels in which seawater iron levels were deficient, normal, or in exces

174 f HNTs, the cost for uranium extraction from seawater is close to the uranium price in the spot urani

175 Electrolysis of seawater is not only a promising approach to produce cle

176 Seawater is one of the most abundant natural resources o

177 y several hundreds of microliters of surface seawater is similar to that found in molecular surveys w

178 Abundance of the seawater isoform of gill Na(+)/K(+)-ATPase increased in

179 ng organic ligands that support more iron in seawater, leading to further macronutrient consumption u

180 thermal pretreatment of macroalgae, although seawater led to relatively higher yields.

181 system conditions, serpentine alteration by seawater led to the formation of authigenic phyllosilica

182 r concentrations at environmentally relevant seawater levels.

183 ar ionic strengths and, upon exocytosis into seawater, lysin and sp18 are dispersed to drive fertiliz

184 Pb concentrations in seawater measured in this study (max 76.8 pmol kg(-1)) w

185 d that P2 excision greatly hinders growth in seawater medium and inhibits biofilm formation.

186 in completely restores the growth defects in seawater medium and partially restores biofilm formation

187 ate 1990s and 2000s as a result of decreased seawater MeHg concentrations.

188 membranes, including 4 brackish water and 2 seawater membranes.

189 on organic carbon burial may lead to higher seawater methane concentrations over the coming centurie

190 Overall, seawater microbial composition and biogeochemistry were

191 Here, we examined the seawater microbial ecology of 25 Northern Caribbean reef

192 Therefore, coastal seawater mirrored the PCB congener profile and increased

193 t in Cuban coral reefs quantified background seawater-normalized extracellular superoxide concentrati

194 Uranyl capture from either seawater or nuclear waste has been well studied and typi

195 and synergetic effects of different ions in seawater over a large range of environmentally relevant

196 strial P input and biological utilization of seawater P in Phanerozoic.

197 tive Fe redox cycle favors the scavenging of seawater P through FeOOH absorption and authigenic phosp

198 d accordingly reduces the bioavailability of seawater P.

199 f wind speed, sea surface temperature (SST), seawater particle attenuation at 660 nm (c (p,660), a me

200 he phasing out of leaded gasoline on TSP and seawater Pb chemistry in the Northern GOA; the rate of c

201 ass spectrometry (MC-ICP-MS) measurements of seawater Pb isotope compositions following Pb separation

202 MS) double-spike method and produce unbiased seawater Pb isotope compositions with similar or improve

203 of similar quality when measuring 1-7 ng of seawater Pb, with reproducibilities (two standard deviat

204 e and alanine are positively correlated with seawater pCO(2) and inversely correlated with seawater p

205 Porites spp. corals cultured over different seawater pCO(2).

206 l conditions and examined for differences in seawater performance and its underlying physiological an

207 this altered lifecycle on traits underlying seawater performance have not been established.

208 cies Carybdea xaymacana, compared to ambient seawater pH conditions (i.e. pH of 8.1).

209 Reductions in seawater pH constitute a conspicuous global change stres

210 Mean seawater pH decreased significantly at -0.009 +/- 0.0005

211 associated with rapid adaptation to reduced seawater pH in the Mediterranean mussel, Mytilus gallopr

212 cochemical and biological factors other than seawater pH must be considered.

213 dings support the development of coral-based seawater pH proxies, but suggest the influences of physi

214 t crustaceans are often resilient to reduced seawater pH, earlier ontogenetic stages can be physiolog

215 ion can facilitate adaptation to declines in seawater pH.

216 eawater pCO(2) and inversely correlated with seawater pH.

217 uent environmental fluctuations and reducing seawater pH.

218 ory conditions, and the PAE migration to the seawater phase was studied with varying light and bacter

219 ng utilising in situ measurements of optical seawater properties, we quantified artificial light expo

220 14.2-3.6 (delta(18)O(Halimeda )- delta(18)O(seawater)); r(2) = 0.92), comparing the temperatures mea

221 Carbonyl photoproduction rates in surface seawater ranged from 0.35-0.79, 0.06-0.2, and 0.02-0.07

222 5)N and delta(13)C values coupled with local seawater redox data for Mesoarchean shales of the Mozaan

223 for the analysis of (99)Tc in samples of the seawater reference material IAEA-443, a peat bog lake, a

224 aldehyde is likely supersaturated in surface seawater relative to its typical atmospheric concentrati

225 yper- (fresh water) and hypo-osmoregulation (seawater) remain mostly elusive.

226 e diversity of coliphages that is present in seawater remains largely unknown, with previous studies

227 etween net volatilization fluxes of PCBs and seawater salinity.

228 n oligotroph, isolated from the same surface seawater sample and utilizing the same proteinaceous sub

229 ranscripts were present in all of the tested seawater samples and Tara Oceans bacterioplankton datase

230 Here, by incubating natural seawater samples at three different temperatures, we ana

231 an eighteen-month (2015-2016) time-series of seawater samples from Monterey Bay, California.

232 Natural seawater samples showed the strongest reduction of I(2)

233 ughput and suitability for analyses of large seawater samples with high Si(OH)(4) contents.

234 ess, Ce-NPs were eventually detected in some seawater samples with low levels of lanthanum-NPs, sugge

235 lied to the detection of genomic DNA in real seawater samples.

236 sensor to detect E. fecalis from aqueous and seawater samples.

237 Reducing seawater saturation state and increasing [aspartic acid]

238 thought to have been abundant in early-Earth seawater, sediments, and hydrothermal systems.

239 onmental water samples including lake water, seawater, simulated water reference materials, and tap w

240 t sampling of freshwater (lakes and rivers), seawater, snow, air, and zooplankton for a range of lega

241 1.709 V, respectively, for overall alkaline seawater splitting at 60 degrees C.

242 efficient electrocatalysts that can sustain seawater splitting without chloride corrosion, especiall

243 ing artificial solutions, natural subsurface seawater (SSW), and, for the first time, samples of the

244 er were lower than those in the oligotrophic seawater suggesting that surfactant mixtures in the two

245 ave formed globally through the reduction of seawater sulfate or locally from hydrothermally supplied

246 indicating that neither flooding itself, nor seawater sulfate, contributed greatly to stomatal closur

247 ctants than those produced from oligotrophic seawater, supporting the hypothesis that seawater surfac

248 and compared with that of abiotic matrices (seawater, surface sediment, and suspended particulate ma

249 hic seawater, supporting the hypothesis that seawater surfactant properties modulate mPMA surfactant

250 A surfactants were weaker than corresponding seawater surfactants.

251 nchial expression of GHR increased following seawater (SW) exposure of juveniles, but expression of P

252 increase osmoregulatory capacity and acquire seawater (SW) tolerance.

253 Similarly, no enrichment of dominant seawater taxa such as Prochlorococcus, SAR11 or Synechoc

254 I show that external seawater temperature and buffering capacity exert the fi

255 actors, two equations model the influence of seawater temperature and mechanical forces.

256 n tuna (Thunnus thynnus) due to increases in seawater temperature between a low point in 1969 and rec

257 Temporal variation in seawater temperature plays a crucial role in coral reef

258 Seawater temperature rise in French Polynesia has repeat

259 ion of the production efficiency of SSA with seawater temperature with a minimum around 6-10 degrees

260 one at a time: (1) air entrainment rate, (2) seawater temperature, and (3) biomass of phytoplankton.

261 er decreases almost linearly with increasing seawater temperature, and the production efficiency is s

262 -2011, exposing marine communities to summer seawater temperatures 2-5 degrees C warmer than average.

263 As seawater temperatures continue to rise and the incidence

264 normal or environmentally relevant elevated seawater temperatures.

265 nic cycles, the major-element composition of seawater, the marine phosphorus cycle, and atmospheric p

266 In seawater, the SSUP fiber achieved a breakthrough uranium

267 puts that typically dilute the alkalinity of seawater thereby resulting in reduced buffering, nutrien

268 well despite being constantly splashed with seawater, they represent a valuable genetic resource for

269 he flow of various tracers from the external seawater to within the cells of all tissues in living an

270 examine the effects of relaxed selection on seawater traits, anadromous and landlocked Atlantic salm

271 thylene, PE-bags), were incubated in natural seawater under laboratory conditions, and the PAE migrat

272 y and alkalinity (pH 2-14) and high-salinity seawater (up to 330 g kg(-1) ).

273 adsorbents have become highly promising for seawater uranium extraction.

274 dy will be used to inform future work on the seawater uranium production cost from a full-scale SMORE

275 ested whether a single PCR survey of eDNA in seawater using a broad metazoan primer could identify di

276 generated by detraining air into artificial seawater using a diffuser demonstrating that the product

277 contaminant that is difficult to remove from seawater using conventional reverse osmosis membranes.

278 f environmental DNA (eDNA) from sediment and seawater using metabarcoding offers a powerful molecular

279 Laboratory calibrations with filtered seawater verified instrument stability and precision.

280 environments, available copper from natural seawater was absorbed and electrochemically released bac

281 The lava-impacted seawater was characterized by high concentrations of met

282 NP behavior in synthetic wastewater and seawater was characterized during aging and exposure.

283 r- and polyfluoroalkyl substances (PFASs) in seawater was investigated along a sampling transect from

284 ygenic phototrophs, and light filtered under seawater, we derived optimal absorption characteristics

285 ion (given as normalized signal readouts) in seawater were <4% and <14%, respectively, as compared to

286 Free PAEs diluted in seawater were also studied for bacterial degradation.

287 ty tolerance, survival and initial growth in seawater were greater in anadromous than in landlocked s

288 Pueruli conditioned in reduced-pH seawater were less responsive and failed to select the L

289 Surfactant CMCs in biologically productive seawater were lower than those in the oligotrophic seawa

290 tions of surfactants extracted from mPMA and seawater were quantified and characterized via measureme

291 gy to produce H(2) and to extract CO(2) from seawater, where it is in equilibrium with the atmosphere

292 he high concentration of inorganic sulfur in seawater, which can readily be reduced by phytoplankton,

293 concentrated green seaweed hydrolysates and seawater with marine yeast Wickerhamomyces anomalus M15

294 g abiotic and biotic degradation behavior in seawater with physical properties and molecular structur

295 n, heavy and light oils were irradiated over seawater with simulated sunlight.

296 ter samples (i.e., tap water, rainwater, and seawater) with no sample preparation.

297 veal in situ evidence of anthropogenic Fe in seawater, with low delta(56)Fe (-0.23 per mille > delta(

298 dly attach to and release from substrates in seawater within a minute.

299 of diclofenac in high matrix samples, e.g., seawater, without any prior sample treatment was selecte

300 hesis that pueruli conditioned in reduced-pH seawater would be less responsive to Laurencia spp. chem

301 ted SiO(2)(aq) concentrations in Precambrian seawater would have generated serpentinites that produce