ライフサイエンスコーパス: CO2

1 CO2 (+0.7%), core temperature (Tcore, +0.5 degrees C) an

2 CO2 concentration, and SO4 and nitrogen deposition on tw

3 CO2 ice sublimation mechanisms have been proposed for a

4 CO2 is a physiological gas normally produced in the body

5 e increase from net benefits of $2.7 ton(-1) CO2 to net costs of $8.5 ton(-1), leading the total SCC

6 meters were decreased for all species in 10% CO2 incubation.

7 pped, modified atmosphere packaged (70%O2/30%CO2) and maintained under retail conditions (4+/-0.5 deg

8 analytics exemplified for the analysis of a CO2 stream in a production plant for detection of benzen

9 mine several potential mechanisms of abiotic CO2 uptake in arid and semiarid soils: atmospheric press

10 ed [CO2] (E-[CO2]) by comparison to free-air CO2 enrichment (FACE) and chamber experiments.

11 experimental data from the Soybean Free-Air CO2 Enrichment site showing that the CFE declined with i

12 Although CO2 introduction is possible prior to hydroxide eluent g

13 owth from a population maintained in ambient CO2 and then transferred to elevated CO2 for 20 generati

14 noted with respect to lactate, alanine, and CO2 production.

15 ntury as indicated by an atmospheric CH4 and CO2 concentration model.

16 plasma synthesis of acetic acid from CH4 and CO2 is an ideal reaction with 100 % atom economy, but it

17 bounds for O2/N2, H2/N2, CO2/N2, H2/CH4 and CO2/CH4, with the potential for biogas purification and

18 oceanic factors (e.g., land cover change and CO2-induced warming) to the 2016 drought.

19 Coupled C-S cleavage and CO2 release to yield [(bpy)3Pd3(micro3-S)2](NO3)2 (bpy,

20 ons reduced model sensitivity to climate and CO2 , but only over the course of multiple centuries.

21 methanol, as well as the reactions of CO and CO2 over TMC surfaces.

22 n making related to investment decisions and CO2 emissions policy in the refining sector.

23 carboxylic acids from 1,6- and 1,7-enyes and CO2.

24 al species capable of using both HCO3(-) and CO2 had greater CO2 use as concentrations increased.

25 n and oxidation of organics, inorganics, and CO2 transformation.

26 which may have induced a surge in magma and CO2 fluxes from mid-ocean ridges and oceanic hotspot vol

27 ved from the arylamine starting material and CO2 in the presence of DBU, is dehydrated by activated s

28 D s decreases with increasing methane and CO2 injecting pressure for samples with high D s .

29 ane (DRM), i.e., the reaction of methane and CO2 to form a synthesis gas, converts two major greenhou

30 microbial communities for CCS monitoring and CO2 utilization, and, with examples, demonstrate how syn

31 while provided factorial additions of N and CO2 .

32 Here, multiple sensors tracked O2 and CO2, gas pressure (DeltaP) between internal silage and a

33 y and reduce emissions of air pollutants and CO2 from coal use, China is attempting to duplicate the

34 atin D-2 by synchronous extrusion of SO2 and CO2.

35 odel (PRELIM), that estimates energy use and CO2 emissions was modified to evaluate the environmental

36 methanol) directly from sunlight, water and CO2.

37 Recent field studies have reported anomalous CO2 uptake using eddy-covariance techniques in arid and

38 Anthropogenic CO2 is expected to drive ocean pCO2 above 1,000 muatm by

39 sion cross sections (Omega) with He, N2, Ar, CO2, and N2O were measured for the 20 common amino acids

40 and, Greece, are part of the largest arsenic-CO2-rich shallow submarine hydrothermal ecosystem on Ear

41 was reduced (P < 0.001) at constant arterial CO2 tension and pH (P = 0.27 and P = 0.23, respectively)

42 Although small changes in arterial CO2 are particularly potent to change CBF (1 mmHg variat

43 to change CBF (1 mmHg variation in arterial CO2 changes CBF by 3%-4%), the coupling mechanism is inc

44 Prospectively targeted arterial CO2 has the capability to evolve as an alternative to cu

45 azides, isocyantes, and nitriles, as well as CO2 and elemental sulfur (S8 ).

46 a natural ability to utilize and assimilate CO2 through different metabolic pathways.

47 changes, volcanic degassing and atmospheric CO2, which may have modulated the climate system's desce

48 d undergo N-dependent changes as atmospheric CO2 concentrations rise, having global-scale implication

49 Elevated atmospheric CO2 may widen the disparity in protein intake within cou

50 is of renewable bioproducts from atmospheric CO2 Growth and metabolism of cyanobacteria are inherentl

51 e orbitally driven variations in atmospheric CO2 concentration between [Formula: see text]150 and 700

52 d ecosystems to slow the rise in atmospheric CO2 concentrations may be smaller than previously assume

53 esponses of plants to changes in atmospheric CO2 concentrations, and fire, as well as what are likely

54 e responses to future changes in atmospheric CO2 concentrations, and thus feedbacks to climate change

55 Large amplitude variations in atmospheric CO2 were associated with glacial terminations of the Lat

56 y by the low partial pressure of atmospheric CO2 (Ca ) experienced during the last glacial period is

57 and higher partial pressures of atmospheric CO2 (pCO2 = 400 and 1000 ppmv).

58 ctly addressing global issues of atmospheric CO2 balance.

59 tions between the growth rate of atmospheric CO2 concentrations and the El Nino-Southern Oscillation

60 ictions on the potential role of atmospheric CO2 in inferred warmer conditions and valley network for

61 sponses to changing climate and atmospheric [CO2] in the boreal forest.

62 2 provides retrievals of the column-averaged CO2 dry-air mole fraction ([Formula: see text]) as well

63 tion for industrial packed and fluidized bed CO2 capture systems due to large particles with a diamet

64 pecies-specific developmental effects before CO2 and climate effects are inferred.Intrinsic water-use

65 espiration requires rapid conversion between CO2 and HCO3(-) Carbonic anhydrase II facilitates this r

66 wever, the electrochemical reactions between CO2 (0.04 % in ambient air) with Li anode may lead to th

67 pseudorevertant strains were not induced by CO2 , consistent with reports that CO2 directly stimulat

68 RelB is processed by CO2 in a manner dependent on a key C-terminal domain loc

69 However, greater values of CH4 -C:CO2 -C ratios lead to a greater global warming potential

70 Despite high simulated per-capita CO2 emissions from LUC in early phases of agricultural d

71 ion defective mutant, is sufficient to cause CO2 sensitivity, which can occur even in the absence of

72 o 11.8 ppm revealed that certain chemisorbed CO2 species are engaged in very strong HBs.

73 extends the understanding of the chemisorbed CO2 structures that are formed upon bonding of CO2 with

74 can be explained by declining chloroplastic CO2 concentration (cc ) at low PPFD.

75 ese climate anomalies by assimilating column CO2, solar-induced chlorophyll fluorescence, and carbon

76 d catalysts are found to exhibit competitive CO2 capacities (0.67-0.91 mmol g(-1) at 25 degrees C and

77 mines the cost of separating and compressing CO2 across 18 industrial processes.

78 n atmospheric carbon dioxide concentration ([CO2 ]) is critical for understanding and predicting the

79 However, converting CO2 to ethanol remains great challenge due to the low ac

80 e dry, such as finishing with super critical CO2 drying, or simple vacuum drying up to 95 degrees C.

81 by integrating components of a cyanobacteria CO2-concentrating mechanism will necessitate co-introduc

82 K (-11 mK to -335 mK) by 2100 due to delayed CO2 response.

83 rent gas-adsorption capacities and different CO2 versus CH4 selectivities.

84 the environmental stress of carbon dioxide (CO2) anesthesia converts an asymptomatic rhabdovirus inf

85 cant drawdown of atmospheric carbon dioxide (CO2) at that time.

86 Trapping with carbon dioxide (CO2) gave the respective O-[Zr] bonded cyclic boratacarb

87 r hand, biological uptake of carbon dioxide (CO2) has the potential to offset the positive warming po

88 ater caused by anthropogenic carbon dioxide (CO2) is anticipated to influence the growth of dinitroge

89 to release large amounts of carbon dioxide (CO2) to the atmosphere in response to increasing tempera

90 Carbon dioxide (CO2) which constitutes a major part of the biogas is gen

91 ed for carbon monoxide (CO), carbon dioxide (CO2), and particulate matter (PM).

92 quilibrium between bicarbonate and dissolved CO2.

93 tially as an endolith when lacking dissolved CO2.

94 ing the effective concentration of dissolved CO2 near the electrode surface through rapid equilibrium

95 owth by Ca. P. anaerolimi whereby DPO drives CO2 reduction to formate, which is then assimilated into

96 Its dynamic CO2 uptake also matched well with its static condition.

97 Elevated (e)CO2 is expected to alter the biomass of fine, coarse and

98 rice yield in response to elevated [CO2] (E-[CO2]) by comparison to free-air CO2 enrichment (FACE) an

99 However, yield prediction in response to E-[CO2] varied significantly among the rice models.

100 Conversely, e[CO2] + HT during flowering and early grain filling signi

101 ood predictor of instantaneous net ecosystem CO2 exchange and 3) functional diversity of leaf N conce

102 solutions can provide 37% of cost-effective CO2 mitigation needed through 2030 for a >66% chance of

103 t for developing practical or cost-effective CO2 technologies.

104 the complex can selectively electrocatalyze CO2 reduction to CO in tetrahydrofuran at -0.48 V vs NHE

105 in the rate-limiting step of electrochemical CO2 reduction catalysis mediated by planar polycrystalli

106 Elevated CO2 can only weakly reduce these yield losses, in contra

107 Elevated CO2 had minimal effects on plant and soil N metrics and

108 ration rates, while +N addition and elevated CO2 concentrations increased growing-season soil CO2 eff

109 ical results suggest that combined, elevated CO2 and temperature will lead to long-term declines in t

110 onal soil C models and suggest that elevated CO2 might increase turnover rates of new soil C.

111 that the response of assemblages to elevated CO2 are correlated with inorganic carbon physiology.

112 ambient CO2 and then transferred to elevated CO2 for 20 generations (HC).

113 um tricornutum, after growing under elevated CO2 (1000 muatm, HCL, pHT : 7.70) for 1860 generations,

114 CO3(-)) increased in abundance with elevated CO2 whereas obligate calcifying species, and non-calcare

115 than HS93-4118 at both ambient and elevated [CO2 ].

116 aily C assimilation was greater at elevated [CO2 ] in both cultivars, while stomatal conductance was

117 r sites was due almost entirely to elevated [CO2 ].

118 edicting rice yield in response to elevated [CO2] (E-[CO2]) by comparison to free-air CO2 enrichment

119 surface temperatures and EGU air emissions (CO2, SO2, and NOX) using historical data.

120 7942 to improve glucose utilization, enhance CO2 fixation and increase chemical production.

121 The excess CO2 flux is resulted primarily from reduction in vegetat

122 ent in designing high-capacity but expensive CO2 sorbent for developing practical or cost-effective C

123 radigm to the emerging use of extracorporeal CO2 removal (ECCO2R) for ultraprotective ventilation in

124 at 25 degrees C and 0.15 bar), extraordinary CO2 /N2 selectivities (98-205 at 25 degrees C), and exce

125 Compared to significant climatic factors, CO2 had on average an approximately three-, four-, or fi

126 fficiently, many algae operate a facultative CO2 concentrating mechanism (CCM).

127 are W i across varying tree sizes at a fixed CO2 level and show that ignoring developmental changes i

128 ominent examples include the carboxysome for CO2 fixation and catabolic microcompartments found in ma

129 n, and may have significant implications for CO2 losses from tropical forest soils under future rainf

130 )') and heterogeneous rate constant (k0) for CO2 reduction were determined with different quaternary

131 enerally rely on two-electron mechanisms for CO2 activation and require highly activated reaction par

132 elopment of ultrathin GO-based membranes for CO2 capture.

133 dant enzyme in plants and is responsible for CO2 fixation during photosynthesis.

134 New materials with high selectivities for CO2 adsorption, large CO2 removal capacities, and low re

135 ce is key in controlling the selectivity for CO2 reduction over H2 evolution in aqueous solution.

136 tant information for the design of SILMs for CO2 capture.

137 imple molecular building blocks derived from CO2 and H2 are carbon sources in the initial stage of bi

138 e global food productivity, benefiting from [CO2] rich environments.

139 WTL reduced GWP from 337.3 to -480.1 g CO2 -eq m(-2) mostly because of decreased CH4 emissions,

140 A long-term net CO2 uptake of >200 g CO2 m(-2) yr(-1) is required to offset the positive radi

141 deposition reduced GWP from 21.0 to -163.8 g CO2 -eq m(-2) , mainly owing to increased net CO2 uptake

142 r-species energy currency even under gaseous CO2 -saturation.

143 findings support the hypothesis of a general CO2-fertilization effect on vegetation growth and sugges

144 one of the first to incorporate stream GHGs (CO2, CH4 and N2O) concentrations and emissions in rivers

145 Approximately 30%-40% of global CO2 fixation occurs inside a non-membrane-bound organell

146 le of using both HCO3(-) and CO2 had greater CO2 use as concentrations increased.

147 s would result in reductions of 0.19-0.53 Gt CO2 eqa(-1), 4.32-10.6 Gt [Formula: see text] eqa(-1), a

148 lion tonnes (MT) CH4 or 2.72 Gigatonnes (Gt) CO2 -eq (1 MT = 10(12) g, 1 Gt = 10(15) g) from ruminant

149 ons capable of featuring simultaneously high CO2 resistance and O2 permeability and the exploitation

150 s of water use by the vegetation in the high CO2 treatment could be contributing to elevation gain, e

151 of these materials, coupled with their high CO2 capacities and low projected energy costs, highlight

152 formance and survival probability under high CO2 experimental conditions do not show acclimatization

153 hocystis sp. PCC 6803 leads to a unique high-CO2-sensitive phenotype.

154 Developing rice cultivars with higher [CO2] responsiveness incorporated with increased toleranc

155 Human CO2 respiration requires rapid conversion between CO2 an

156 for use in organic solvents, can hydrogenate CO2 to formate in water with bicarbonate as the only add

157 oxygen, high pH, and enrichment of (13)C in CO2) indicate that upwelling of cold, nutrient-rich wate

158 ng the chemosensitive response to changes in CO2/H+ than previously thought.

159 he oxygen-18 isotopic ((18)O) composition in CO2 provides an important insight into the variation of

160 r test fleet, the measured 14.5% decrease in CO2 emissions from GDIs was much greater than the potent

161 d a new pathway for significant reduction in CO2 capture energy consumption.

162 ion-induced hypoxia and a subsequent rise in CO2 that drives fentanyl-induced increases in NAc glucos

163 We find that variability in CO2 and temperature sensitivity is attributable, in part

164 freezing, elevated temperature and increased CO2.

165 This challenges the idea that increasing CO2 would stimulate growth.

166 enhance synaptic transmission, mice inhaled CO2 to induce an acidosis and activate acid sensing ion

167 as much as half of the glacial-interglacial CO2 change.

168 SPP) spectroscopies were used to investigate CO2 reorientation and spectral diffusion dynamics in SIL

169 piration across all sites, although invoking CO2 effects on vegetation (growth enhancement and increa

170 forcing of open-water fluxes (3.5 +/- 0.3 kg CO2 -eq m(-2) yr(-1) ) exceeded that of vegetated zones

171 eded that of vegetated zones (1.4 +/- 0.4 kg CO2 -eq m(-2) yr(-1) ) due to high ecosystem respiration

172 tude and interannual variability of the land CO2 sink.

173 ring the last 50 years has generated a large CO2 concentration in the atmosphere that has led to the

174 may be a key technology for achieving large CO2 emission reductions.

175 high selectivities for CO2 adsorption, large CO2 removal capacities, and low regeneration energies ar

176 activity of the cathode, the as-prepared Li-CO2 batteries exhibit high reversibility, low polarizati

177 and stable photocatalysts for visible light CO2 reduction.

178 midity, we estimated that most of the litter CO2 efflux and decay occurring in the dry season was due

179 3 and 298 K, JUC-62 showed 51% and 34% lower CO2 uptake, respectively, than when UV light was off.

180 monstrate how synthetic biology may maximize CO2 uptake within and above storage sites.

181 analyses are poorly constrained by measured CO2 exchange in drylands.

182 ivity may be involved in recycling metabolic CO2 Glandular trichomes cope with oxidative stress by pr

183 ntaining pyrenoid that is needed to minimise CO2 retro-diffusion for CCM operating efficiency.

184 thermal acclimation was tested by monitoring CO2 and CH4 production, CUE, and microbial biomass.

185 2008 Robeson upper bounds for O2/N2, H2/N2, CO2/N2, H2/CH4 and CO2/CH4, with the potential for bioga

186 absence of moisture stress resulting in net CO2 uptake increases in the shoulder seasons and decreas

187 O2 -eq m(-2) , mainly owing to increased net CO2 uptake.

188 A long-term net CO2 uptake of >200 g CO2 m(-2) yr(-1) is required to off

189 antly, PEDOT-C14-based SC pH sensors have no CO2 interference, an essential pH sensors property when

190 tock, which accounted for 47%-54% of all non-CO2 GHG emissions from the agricultural sector.

191 We argue that neither ice sheet dynamics nor CO2 change in isolation can explain the MPT.

192 Here, we identify several novel CO2-dependent changes in the NF-kappaB pathway.

193 us eddy covariance flux measurements of NOx, CO2, CO and non methane volatile organic compound tracer

194 with a precision better than 1% for N2, O2, CO2, He, Ar, 2% for Kr, 8% for Xe, and 3% for CH4, N2O a

195 which enables the simultaneous absorption of CO2 and SO2/SO3 from the flue gas.

196 d-basalt eruptions released large amounts of CO2 and CH4 into the atmosphere, causing severe global w

197 xt-generation adsorbents for a wide array of CO2 separations.

198 irst summarize the most important aspects of CO2 capture and green routes to produce H2.

199 Our results show partial re-assimilation of CO2 and H2 by n-butanol-producer C. beijerinckii.

200 2 structures that are formed upon bonding of CO2 with surface amines and readily released from the su

201 e experimental apparatus based on changes of CO2 partial pressures.

202 The concentration of CO2 in many aquatic systems is variable, often lower tha

203 Rising atmospheric concentrations of CO2 and O3 are key features of global environmental chan

204 seudonana, to high and low concentrations of CO2 at the level of transcripts, proteins and enzyme act

205 under elevated vs ambient concentrations of CO2.

206 The contrasting of CO2 fluxes between inland and coastal wetlands globally

207 lent activities for catalyzing conversion of CO2 into cyclic carbonate (conversion >95% at 100 degree

208 We use the correlations of CO2 with trace elements to define an average carbon abun

209 s seismic cluster records rapid degassing of CO2, suggesting an interval of anomalous fluid source.

210 ing projections in response to a doubling of CO2-from 1.5 degrees C to 4.5 degrees C or greater -rema

211 However, the effects of CO2 enrichment on eutrophic coastal waters are still unc

212 Beneficial effects of CO2 on photosynthetic organisms will be a key driver of

213 complications because of electroreduction of CO2 to formate.

214 nd processes for the direct hydrogenation of CO2 to formate/formic acid, methanol, and dimethyl ether

215 rcing of the climate by increasing levels of CO2 and CH4.

216 10(8) M(-1) s(-1)) and half-life (10 ns) of CO2(*-) can be evaluated by fitting the collection effic

217 (MEA)-based postcombustion capture (PCC) of CO2 with distributed, humidity-swing-based direct air ca

218 tudy was to document the pharmacodynamics of CO2 for MBF using prospective end-tidal targeting to pre

219 of hydrogen without concurrent production of CO2 (unlike steam reforming) or CO (by complete methanol

220 nditions did not release a large quantity of CO2.

221 the complete orientational randomization of CO2 and structural fluctuations of the IL (spectral diff

222 hat inhibition is caused by the reduction of CO2 into CO, whose high affinity with platinum triggers

223 f modern energy challenges, the reduction of CO2 into fuels calls for electrogenerated low-valent tra

224 The electrochemical reduction of CO2 is known to be influenced by the identity of the alk

225 Electrochemical reduction of CO2 to ethanol, a clean and renewable liquid fuel with h

226 stable electrode for selective reduction of CO2 to ethanol.

227 ctrode for the electrocatalytic reduction of CO2 to formate.

228 achieve selective and efficient reduction of CO2 to specific hydrocarbons and oxygenates is to determ

229 matrix for the electrocatalytic reduction of CO2.

230 Direct releases of CO2 from litter layer only accounted for 19% increases

231 We report here on a new series of CO2-reducing molecular catalysts based on Earth-abundant

232 result of glaciation may act as a source of CO2 to the atmosphere.

233 demonstrate that the use of two standards of CO2 in air of known but differing delta(13)C and delta(1

234 tailed understanding of the initial steps of CO2 electroreduction on copper surfaces, the best curren

235 The utilization of CO2 as a carbon source for organic synthesis meets the u

236 he reaction mechanisms are reviewed based on CO2 capture literature as well as biological and atmosph

237 t Soil warming had a much stronger effect on CO2 flux than Air warming.

238 er volatile inventory, particularly of CO or CO2 ices, or contained amorphous ice, which could have t

239 racrine mechanisms, and via input from other CO2 -responsive neurons.

240 rhaps this is how a few corals survived past CO2 increases, such as the Paleocene-Eocene Thermal Maxi

241 system climate sensitivity is K (1sigma) per CO2 doubling, which is notably higher than fast-feedback

242 adjusts stomatal conductance, photosynthetic CO2 and photorespiratory O2 fixation, and starch synthes

243 equivalents, and recycling of N and possibly CO2 through refixation.

244 rown under current and elevated (550 [ppm]) [CO2 ] overinvest in leaves, and this is predicted to dec

245 o C-C bond breaking would produce protonated CO2, an energetically inaccessible species that can be a

246 attracted much attention as hosts to recycle CO2 into valuable chemicals.

247 rformance of a set of technologies to reduce CO2 emissions at refineries.

248 While the UK has committed to reduce CO2 emissions to 80% of 1990 levels by 2050, transport a

249 nsitization of molecular catalysts to reduce CO2 to CO is a sustainable route to storable solar fuels

250 rially important C1 chemicals while reducing CO2 emissions.

251 trial applications such as soil remediation, CO2 sequestration, and enhanced oil recovery.

252 the posttranslational control of respiratory CO2 refixation and anaplerotic photosynthate partitionin

253 Exponentially rising CO2 (currently 400 muatm) is driving climate change and

254 horter than that required by conventional SC-CO2 extraction and HRE, respectively.

255 and 31.6% more apigenin than conventional SC-CO2 extraction and HRE, respectively.

256 Large-scale CO2 hydrogenation could offer a renewable stream of indu

257 f rs4293393 was associated with higher serum CO2 level.

258 onsecutive supercritical carbon dioxide (SFE-CO2) pressurised liquid (PLE) and enzyme-assisted extrac

259 s influencing the biogeochemistry in shallow CO2-rich hydrothermal systems and the importance of coup

260 er only accounted for 19% increases in soil CO2 flux, suggesting that the leaching of dissolved orga

261 soil is the major cause of rain-induced soil CO2 pulse.

262 ed DOC input in regulating rain-induced soil CO2 pulses and microbial community composition, and may

263 concentrations increased growing-season soil CO2 efflux rates by increasing annual aboveground net pr

264 accompanies methane emissions and stimulates CO2 consumption by photosynthesizing phytoplankton.

265 As a climate mitigation strategy, CO2 capture from flue gases of industrial processes-much

266 igate if the interaction between sublimating CO2 ice blocks and a warm, porous, mobile regolith can g

267 ium europaeum fruits following supercritical CO2 extraction (at 30MPa and 40 degrees C).

268 Our results also indicate that CO2 component remains soluble in the melt at high pressu

269 Physiologists have long known that CO2 directly affects acid-base and ion regulation, respi

270 nduced by CO2 , consistent with reports that CO2 directly stimulates adenylyl cyclase.

271 isolated from green coffee beans showed that CO2 was generated from various green coffee components,

272 ong-term records at Barrow, AK, suggest that CO2 emission rates from North Slope tundra have increase

273 The CO2 solubility was measured using a home-made experiment

274 ive ensemble Monte Carlo simulations for the CO2 methanation reaction.

275 alysts have potential for application in the CO2 conversion industry.

276 RP may provide a molecular identifier of the CO2 arousal circuit.

277 About half of the CO2 produced came from plant tissue mineralization in in

278 sive and native communities; the rest of the CO2 was produced from SOM mineralization (priming).

279 ary amines, which, when oxidized, lose their CO2 capture capacity.

280 Over longer timescales, CO2 release could act as a negative feedback, limiting p

281 CGA is shown not a major contributor to CO2 formation, as heating of this compound under typical

282 boxylic acids measured indoors correlated to CO2 in daytime, suggesting that human occupants may cont

283 impacts the microbial respiration of DOC to CO2.

284 These have previously been linked to CO2 draw-down, but the severe cold climates of the Cryog

285 he upper branch of methyl group oxidation to CO2 as well as membrane-bound heterodisulfide reductase

286 Conversion of pyruvate to CO2 in the T. brucei bloodstream form provides new suppo

287 use many of the PBel neurons that respond to CO2 express calcitonin gene-related peptide (CGRP), we h

288 cluding exaggerated ventilatory responses to CO2 and prolonged circulation time, implicates the venti

289 pacts conclusions on trees' W i responses to CO2 or climate.

290 cles by exposing the colloidal suspension to CO2.

291 sides initial reactivity studies of 2 toward CO2 and methanol, different isomerization pathways depen

292 ith unprecedented catalytic stability toward CO2 reduction.

293 74-III results in a material that can uptake CO2 at low pressures through a chemisorption mechanism.

294 ion of the extraction rate and extent of USC-CO2 extraction.

295 ver, the extraction time required by the USC-CO2 procedure, which used milder conditions, was approxi

296 s and separation units as well as to utilise CO2 and recycle side-products in the process are describ

297 species, and non-calcareous macroalgae whose CO2 use did not increase consistently with concentration

298 r leaf area (Sm ) is closely associated with CO2 diffusion and photosynthetic rates.

299 activation of methane and its reforming with CO2 at relatively low temperatures (600-700 K).

300 In contrast, solutions without CO2 develop elongated convective channels known as wormh