ライフサイエンスコーパス: carbon

1 s land area show abrupt shifts in vegetation carbon.

2 rolling the sequestration of sinking organic carbon.

3 efficiency under conditions of low inorganic carbon.

4 hilic substitution at an oxygenated tertiary carbon.

5 n pathways enabled by allylic versus vinylic carbons.

6 oxidizes 6:2 FTS by H-abstraction from ethyl carbons.

7 late-stage installation of both tritium and carbon-11 into the desired compounds via methylation of

8 ies measured at 1 s include methane, ethane, carbon-13 ((13)C) and deuterium (D) isotopes of methane,

9 AtGA2ox9 oxidizes carbon-20 to form tricarboxylic acid C(20)-GAs, whereas

10 ining a monosaccharide (glucose) attached at carbon-20.

11 Methylation of carbon-5 of cytosines (m(5) C) is a post-transcriptional

12 esents a level-1 identification of the seven carbon (7-C) sugar C-methyl-scyllo-inositol (mytilitol)

13 low concentrations of nutrients and organic carbon, abundant Prochlorococcus, and high microbial com

14 lic approach that combines two complementary carbon accounts, the physical carbon balance and the fos

15 ions across the areas for which we predicted carbon accumulation rates (except for northern Africa an

16 of information about depth, bulk density and carbon accumulation rates.

17 rgeable Zn-air batteries assembled with this carbon aerogel exhibit a remarkable specific capacity of

18 reviously reported on polymer-functionalized carbon-aerogels.

19 Transformations of biomass burning brown carbon aerosols (BB-BrC) over their diurnal lifecycle ar

20 that two molecules with tails made of alkyl carbon, alkylphosphocholines (APCs) and quaternary ammon

21 p a feedback between hydraulic controls over carbon allocation and the role of root growth on soil-pl

22 Cyclo[18]carbon (C(18), a molecular carbon allotrope) can be synthesized by dehalogenation o

23 ts attest to the input of isotopically light carbon, although the carbon sources remain debated.

24 ein, value-added materials such as activated carbon and carbon nanotubes were synthesized from low-va

25 by forming covalent bonds between molecular carbon and copper surface atoms.

26 ucosamine), using this beta-glucan to obtain carbon and energy for growth.

27 ant irreversible behaviour evident at glassy carbon and gold transducers - k(o) (standard heterogeneo

28 g robustness against mutations that increase carbon and nitrogen incorporation into protein sequences

29 These data, combined with the carbon and nitrogen isotope contents of the diamonds, in

30 etizing the results based on social costs of carbon and other air pollutant emissions highlights the

31 e show textural observations, backed up with carbon and oxygen isotope data, which indicate an intima

32 ained more elemental carbon but less organic carbon and was more sensitive to visible light by exhibi

33 centrations and stable isotope ratios of Hg, carbon, and nitrogen in the feathers and blood of geoloc

34 ally, soils store two to three times as much carbon as currently resides in the atmosphere, and it is

35 ummarizing the recent progress in nanoporous carbons, as the most commonly used EDLC electrode materi

36 e multiple autotrophic pathways of microbial carbon assimilation and fixation in paddy soils remain p

37 ate to substantial differences in total crop carbon assimilation.

38 erature controls the storage of soil organic carbon at mid and high latitudes(2,3), hydroclimate may

39 artial positive charge developing on the C-O carbon atom progressing C-H abstraction.

40 ion model that traces the fate of individual carbon atoms as they interact with their environment, un

41 distinguishing remote C-H bonds on adjacent carbon atoms is an extraordinary challenge due to the la

42 ntum chemical analysis, suggest that the two carbon atoms of the L->C(2) complex both have carbene ch

43 The functionalization occurs at C3 and C2 carbon atoms, respectively, at the indole scaffold in th

44 nterannual variability (IAV) of the net land carbon balance (S(net)) is important to predict future c

45 complementary carbon accounts, the physical carbon balance and the fossil fuel-derived gaseous carbo

46 med to have negligible impacts on the annual carbon balance but as data coverage increases and the Ar

47 Using a first-principles carbon balance model with a prescribed live woody biomas

48 ems are increasingly important to the annual carbon balance of these vulnerable ecosystems.

49 aphene has attracted attention for realizing carbon-based electronic devices.

50 al character which are potentially useful in carbon-based optoelectronics and spintronics.

51 , we show that the diffraction signal of the carbon-based pigment itself can be isolated.

52 Black carbon (BC) aerosols perturb climate and impoverish air

53 y subducted oceanic lithosphere destabilizes carbon-bearing metals to form diamond, without disturbin

54 oceanic crust, not sediment, is the primary carbon-bearing reservoir in slabs subducted to deep-lith

55 In recent years, carbon black has been re-discovered in the design of ele

56 we present an overview of the literature on carbon black-based electrochemical (bio)sensors, highlig

57 , with a special focus on the fabrication of carbon black-based electrodes in the realisation of sens

58 For each fragment, the carbon-black pigment found in the ink is identified as f

59 Here we demonstrate the formation of a boron-carbon bond between these substances in a two-step proce

60 to convex side due to a difference in metal-carbon bonding at the curved surfaces as confirmed by de

61 ghly selective and sequential activations of carbon-bromine (C-Br) and carbon-fluorine (C-F) bonds an

62 the marine primary productivity and organic carbon burial.

63 soot, high-A/F soot contained more elemental carbon but less organic carbon and was more sensitive to

64 Cyclo[18]carbon (C(18), a molecular carbon allotrope) can be synt

65 uncertainty in projecting future climate and carbon (C) cycle feedbacks.

66 Blue carbon (C) ecosystems are among the most effective C sin

67 Fire also reduced rates of carbon (C) mobilisation by soil biota.

68 Soil carbon (C) pools and plant community composition are reg

69 The magnitude of the terrestrial carbon (C) sink may be overestimated globally due to the

70 ion by plants may be symmetrically linked to carbon (C) transfer from plant to fungus or governed by

71 ies the potential opportunities for low-cost carbon capture and storage (CCS) scenarios with process

72 Despite carbon-carbon (C-C) bonds providing the central framewor

73 te efforts for beta-C-H functionalization in carbon-carbon and carbon-heteroatom bond-forming reactio

74 organic halides via selective cleavage of a carbon-carbon bond between the skeleton of the molecule

75 eriments to study in detail the mechanism of carbon-carbon bond formation in Ni bipyridine- and diket

76 cus marinus MC-1 (MmOGOR), which catalyzes a carbon-carbon bond formation reaction.

77 Carbon-carbon bond forming reactions are essential trans

78 egioselective oxygen radical addition to the carbon-carbon double bond.

79 lly installing extended pai-rich alternating carbon-carbon linkages between the rotational electron d

80 Ni,N-doped carbon catalysts have shown promising catalytic performa

81 ck of an effect of ligands, the formation of carbon-centered radicals with long lifetimes, and the de

82 nstruction of C-O bonds at fully substituted carbon centers in the synthesis of chiral 2,2-disubstitu

83 ic position to forge tertiary and quaternary carbon centers.

84 l-derived gaseous carbon footprint, to track carbon coming into, being added to urban stocks, and eve

85 droplets through polydimethylsiloxane (PDMS)-carbon composite membranes.

86 undamental pai functions are unique to sp(2) carbon-conjugated frameworks and cannot be accessible by

87 Inventorying carbon consumed and stored for urban metabolism should b

88 are otherwise freely moving in an ultralight carbon container floating above an air-dispensing base.

89 During the activity tests, the only carbon-containing products were DME and CO(2) .

90 s for PM transition from low to high organic carbon content were characterized based on the maximum f

91 ortality from wildfire, but at an increasing carbon cost for forest management.

92 he anode is composed of an elastic outermost carbon covering, a nonfilling porous structure, and a gr

93 ur models show that these extinction-related carbon cycle changes would have allowed the ocean to abs

94 net)) is important to predict future climate-carbon cycle feedbacks.

95 n predicting stomatal behavior and improving carbon cycle modeling.

96 , signalling a reorganization of the climate-carbon cycle system.

97 gae and is a critical parameter in the ocean carbon cycle.

98 groups that play a major role in the global carbon cycle.

99 and discuss implications on the terrestrial carbon cycle.

100 subsidy to distant habitats and for inshore carbon cycling and (potentially) carbon sequestration.

101 t the dominant mechanisms that determine the carbon cycling are different between the consolidated gu

102 otentially important consequences for global carbon cycling.

103 Managing the carbon debt with prescribed fire will help reduce the ri

104 sions were primarily fuelled by contemporary carbon decomposition.

105 omography analysis revealed that SMAPs had a carbon-dense shell and were stored in multicore granules

106 velopment of novel carbon nanostructures and carbon-derived energy storage devices is presented with

107 issions and can offset summer photosynthetic carbon dioxide (CO(2) ) uptake.

108 faster rates of net H(2) oxidation and dark carbon dioxide (CO(2)) fixation than those from the carb

109 h a global warming potential 86-125x that of carbon dioxide (CO(2)) over a twenty-year period, is the

110 e global CDR goals of 0.5 to 2 gigatonnes of carbon dioxide (CO(2)) per year with extraction costs of

111 ironmental change factors (warming, elevated carbon dioxide [CO(2) ], increased precipitation, increa

112 de mixture) from two global warming gases of carbon dioxide and methane via dry reforming is environm

113 n dioxide reduction performances once a pure carbon dioxide feed is restored, indicating a negligible

114 romote arousal in response to elevated blood carbon dioxide levels, as seen in sleep apnea [3].

115 oxygen partial pressure (pO(2)), and a lower carbon dioxide partial pressure (pCO(2)).

116 ciency, the electrocatalysts exhibit similar carbon dioxide reduction performances once a pure carbon

117 in select patients receiving extracorporeal carbon dioxide removal is safe and feasible and avoids t

118 Initial arterial carbon dioxide tension tension was independently associa

119 )O/Cu(111) catalyst from carbon monoxide and carbon dioxide to methanol under a reaction environment

120 s using CO(2) and the catalytic reduction of carbon dioxide, including atmospheric CO(2), into methan

121 lowed the ocean to absorb massive amounts of carbon dioxide, thus limiting the global warming otherwi

122 RBCs) transport oxygen to tissues and remove carbon dioxide.

123 d the carboxylic group and the liberation of carbon dioxide.

124 ne-co-divinylbenzene) monolithic columns and carbon dioxide/methanol mobile phase.

125 This work aims to utilize diamond-like carbon (DLC) thin films for bioreceptor immobilization a

126 rly isomers with the ester bond at the 9(th) carbon due to decreased FAHFA hydrolysis activity.

127 nter ended, taking up roughly 90 g/m(2) more carbon during the winter to spring transition than in ot

128 ortant implications for forecasting mangrove carbon dynamics and the persistence of mangroves and oth

129 yet their biological communities and related carbon dynamics are highly sensitive to changes in clima

130 tically influence root productivity and soil carbon dynamics under future climate change scenarios.

131 bile ions, enabled by ionic screening of the carbon electrode.

132 ibe a convenient assembly for screen printed carbon electrodes (SPCE) suitable for analyses in gaseou

133 of capacitive deionization (CDI) with porous carbon electrodes is limited by the high ionic resistanc

134 s perspectives on managing drivers to reduce carbon emissions and make dentistry more environmentally

135 ected to reach 76.41% in 2050, both reducing carbon emissions and promoting eco-friendly development.

136 ate the economy-wide energy requirements and carbon emissions associated with future household consum

137 To assess whether the EU ETS reduced carbon emissions even as permits were cheap, we estimate

138 rmits were cheap, we estimate counterfactual carbon emissions using an original sectoral emissions da

139 nhance the rates of oceanic productivity and carbon export.

140 gher trophic-level production and additional carbon export.

141 Carbon fiber (CF) electrodes are thinner and more flexib

142 ciencies of raw and HNO(3)-treated activated carbon fiber cloth (ACFC) were examined.

143 running performance, many athletes race with carbon fiber plates embedded in their shoe soles.

144 ce synthetic fibers such as glass fibers and carbon fibers as well as to provide unique functionaliti

145 sulting in universal declines in the rate of carbon fixation with short-term increases in temperature

146 ial activations of carbon-bromine (C-Br) and carbon-fluorine (C-F) bonds and cyclodehydrogenation.

147 III)-catalyst allows the control of tertiary carbon-fluorine stereocenters with up to 96% ee.

148 The influence of terrestrial carbon flux on atmospheric CO(2) concentrations (DeltaCO

149 Using normalized daily carbon fluxes from the FLUXNET Network for 34 forest sit

150 locked together the regulation of water and carbon fluxes in vascular plants, finally examining spec

151 ic sites, model agreement for both water and carbon fluxes is typically higher on fine (daily-monthly

152 although climate change has an impact on the carbon fluxes of these ecosystems, the direct anthropoge

153 ages: in particular, they can have a massive carbon footprint, they are time-consuming, and the high

154 balance and the fossil fuel-derived gaseous carbon footprint, to track carbon coming into, being add

155 re, we evaluate the sensitivity of water and carbon footprints estimates among seven commonly used me

156 The sp(2) carbon frameworks are highly luminescent even in the sol

157 bed to different types of granular activated carbon (GAC).

158 ular potential sweep voltammetry on a glassy carbon (GC) electrode was developed to distinguish and q

159 Abnormalities of one carbon, glutathione and sulfide metabolisms have recentl

160 ase (Mthfr), which results in retention of 1-carbon groups in the folate cycle at the expense of tran

161 a-C-H functionalization in carbon-carbon and carbon-heteroatom bond-forming reactions, these have num

162 t, focusing on the role of sulfur structure, carbon host chemistry and porosity, and electrolytes in

163 lyzed enantioselective functionalizations of carbon-hydrogen (C-H) bonds represent a promising pathwa

164 important implications for the transport of carbon in aqueous fluids in the Earth's interior.

165 sive riparian canopy, high levels of organic carbon in soils, and suboxic conditions at shallow depth

166 o describes the relative amount of inorganic carbon in the algae and is a critical parameter in the o

167 Polar blue carbon increases with losses of marine ice over high lat

168 biocompatible gold electrodes modified with carbon ink or fumed silica can compete with the oxidatio

169 The increase in yields and associated carbon input to the SOC pool counteracted the increased

170 y of defect sites that promote adsorption of carbon intermediates and C-C coupling reactions while mi

171 nity to directly introduce a pulse of labile carbon into sediment, we traced a priming effect and ass

172 to the alkene, to the more substituted alpha-carbon is 3.6 kcal/mol lower than that to the beta-carbo

173 The quaternary carbon is a predominant feature of natural product struc

174 Negative carbon isotope excursions (CIEs) recorded in marine and

175 mation in groundwater at a field site, where carbon isotope fractionation of CFC-11 suggests naturall

176 ancient environments has depended heavily on carbon isotopic analysis of fossil bones and palaeosols.

177 ment found in the ink is identified as flame carbon (lampblack or soot).

178 renewable resources and energy, pursue a low-carbon lifestyle, and reduce energy intensity over the n

179 een plant water retention and EM fungi under carbon-limiting conditions.

180 upon replacing the ether-linked amines with carbon-linked morpholines, a modification motivated by f

181 etal single-atom catalysts on nitrogen-doped carbon (M(1)/CN, M = Pt, Ir, Pd, Ru, Mo, Ga, Cu, Ni, Mn)

182 nd 1b) exhibiting different scenarios of all-carbon magnetism.

183 spersed HEA-NPs on granular supports such as carbon materials, gamma-Al(2)O(3), and zeolite, which is

184 oparticles, metal carbide nanoparticles, and carbon materials.

185 ing cassette (ABC) transporters, and central carbon metabolic proteins) were positively correlated wi

186 usage and detect genetic changes involved in carbon metabolism and inter-specific interaction.

187 determine which genes involved in apicoplast carbon metabolism are required for blood-stage parasite

188 stable SACs on traditional supports (N-doped carbon, metal oxides, etc.) remains a formidable challen

189 under RCP 8.5 than simulations with moderate carbon mitigation (i.e., RCP 4.5).

190 above 1 m and adding diacids with oxygen-to-carbon molar ratio (O:C > 1) significantly reduced the r

191 ective and sensitive detection of endogenous carbon monoxide (CO) in live mammalian cells under normo

192 Carbon monoxide (CO) is a cell-signaling molecule (gasot

193 -defined CeO(2)/Cu(2)O/Cu(111) catalyst from carbon monoxide and carbon dioxide to methanol under a r

194 gly, immunomodulatory effects of HO-1 and/or carbon monoxide correlated with early induction of the l

195 lung capacity (P = .013) but not their lung carbon monoxide diffusion capacity (P = .12).

196 molecule into a dosage form for the goal of "carbon monoxide in a pill." This should enable non-inhal

197 he generation of synthesis gas (hydrogen and carbon monoxide mixture) from two global warming gases o

198 nzyme responsible for degradation of heme to carbon monoxide, bilirubin, and iron, is an important re

199 Photoactivatable carbon monoxide-releasing molecules (photoCORMs) are che

200 rography-enabled thermally transferred (XTT) carbon nanomaterial-based electrochemical sensors is pro

201 y enable the realization of devices based on carbon nanomaterials with exotic quantum properties.

202 The macro-sized (meter-level) carbon nanostructured networks show extraordinary nanost

203 recent progress in the development of novel carbon nanostructures and carbon-derived energy storage

204 r immobilizing nIR-fluorescent single-walled carbon nanotube (SWCNT) sensors on seven different types

205 accase from white rot fungus on multi-walled carbon nanotube surface modified with a naphthalene grou

206 Carbon nanotubes (CNTs) embedded polymers are of increas

207 For carbon nanotubes (CNTs) in particular, the inability to

208 sition metal nucleated, high yield growth of carbon nanotubes (CNTs) is inhibited in electrolytes con

209 emerging electronic materials, single-walled carbon nanotubes (SWCNTs) are promising candidates for n

210 disulfide (MoS(2)) crystals on single-walled carbon nanotubes (SWCNTs).

211 doreductase enzymes enabled by single walled carbon nanotubes and colloidal clays, ii) the molecular

212 tions, demonstrating the potential of porous carbon nanotubes for atom sieving.

213 added materials such as activated carbon and carbon nanotubes were synthesized from low-value Miscant

214 ized fluorescent sp(3)-defect tailored (6,5) carbon nanotubes which, when excited at their first orde

215 by the CO(2) mineralised (i.e. samples were 'carbon negative', even when 10% w/w CEM 1 was used); fur

216 uted ionomer coverage throughout the fibrous carbon network in the catalyst.

217 ource of H(2), the process can be considered carbon-neutral.

218 Graphitic carbon nitride (g-C(3)N(4)) is a robust organic semicond

219 es with unique microenvironment on graphitic carbon nitride as "subnano reactors" to precisely confin

220 -earth single erbium (Er) atoms supported on carbon nitride nanotubes (Er(1) /CN-NT) with a tunable d

221 n, and relative supplies of resources (e.g., carbon, nitrogen, and phosphorus), leading to nonlinear

222 ental substitution on both the metal (M) and carbon/nitrogen (X) sites presents promising routes for

223 matic substitution reactions with oxygen and carbon nucleophiles to provide access to a variety of hi

224 The lower carbon number and aromaticity of the archipelago-derived

225 It yielded water-soluble compounds with carbon number and aromaticity up to 2-fold higher than t

226 We further show that RsaD redirects carbon overflow metabolism, contributing to stationary p

227 erent tunneling down to 10 K, indicating the carbon paint does not add spurious thermally activated c

228 th both dc and ac techniques, revealing that carbon paint protective layers provide a solution to thr

229 nophosphorus hydrolase (OPH) enzyme-modified carbon paste (CP) microneedle electrodes for square wave

230 f 8.2 +/- 4.2 (one standard error) tonnes of carbon per hectare per year from the breakdown of soil o

231 roclimate may be the dominant driver of soil carbon persistence in the tropics(4,5); however, the sen

232 The PIC (particulate inorganic carbon): POC (particulate organic carbon) ratio describe

233 novo lipogenesis in the liver(4-6), in which carbon precursors of acetyl-CoA are converted into fatty

234 the obtainment of stable polymer colloids as carbon precursors.

235 The biological carbon pump (BCP) comprises wide-ranging processes that

236 inorganic carbon): POC (particulate organic carbon) ratio describes the relative amount of inorganic

237 s secreted by fungal saprotrophs involved in carbon recycling.

238 lation (V-type proton ATPase), and inorganic carbon regulation (carbonic anhydrase).

239 ordered proteins control cell elongation and carbon reserves via an order-by-disorder mechanism, regu

240 f carbon through Earth's largest terrestrial carbon reservoir.

241 ple calculations based on typical 2D N-doped carbon/RuMo nanoalloys heterostructures demonstrate that

242 ion that is required to produce the distinct carbon scaffold of colchicine.

243 The implementation of soil carbon sequestration measures requires a diverse set of

244 for inshore carbon cycling and (potentially) carbon sequestration.

245 s of molecular tagging methods incorporating carbon, silicon, nitrogen, phosphorus, and deuterium int

246 explaining decadal-scale changes in the land carbon sink and highlight the importance of fire managem

247 hat turgor is a central driver of the forest carbon sink and should be considered in next-generation

248 growth and the ecosystem became a sustained carbon sink well before winter ended, taking up roughly

249 typically predict that this tropical forest 'carbon sink' will continue for decades(4,5).

250 CO(2) fertilization as a driver of increased carbon sinks in global forests.

251 nking that the capacity of forests to act as carbon sinks will be generally enhanced under eCO(2), an

252 y alter spatial distribution of soil organic carbon (SOC) and total nitrogen (TN) concentrations in c

253 Soil organic carbon (SOC) concentration in WSA(0.106-0.25),WSA(2-5 mm

254 rophs in minimal media devoid of any organic carbon source, pointing to S. elongatus-E. coli K-12 as

255 a stationary phase with sucrose used as sole carbon source.

256 t of isotopically light carbon, although the carbon sources remain debated.

257 es cerevisiae growing in the presence of two carbon sources.

258 cular-based design of functionalized polymer/carbon spheres.

259 vival across treatments, expecting that both carbon stability and survival probability would increase

260 We assessed differences in carbon stability and tree survival across treatments, ex

261 We quantified the total ecosystem carbon stocks (TECS) in seagrass, emergent marshes, and

262 hewan to characterize above- and belowground carbon stocks and combustion rates in relation to histor

263 We found more carbon stocks in live trees, but a fewer number of stand

264 lifespan and thus recent increases in forest carbon stocks may be transient due to lagged increases i

265 that the deep Pacific is a site of respired carbon storage associated with periods of decreased glob

266 mutation that affected the gene encoding the carbon storage regulator CsrA.

267 ive mitigation strategies based on fostering carbon storage through increased tree diversity.

268 swamp forests (PSFs) are globally important carbon stores under threat.

269 A broad scope with all six-carbon-substituted arene motifs, control experiments, an

270 roph Rhodopseudomonas palustris, the type of carbon substrate influences the relative rates of diazot

271 The plant supplies carbon substrates and other nutrients to the bacteria in

272 unger than dissolved and particulate organic carbon, suggesting emissions were primarily fuelled by c

273 The bulk Earth's carbon/sulfur ratio is best explained by the delivery of

274 P) comprises wide-ranging processes that set carbon supply, consumption, and storage in the oceans' i

275 late (PET) is selectively depolymerized by a carbon-supported single-site molybdenum-dioxo catalyst t

276 lled from single vesicles onto an inner-wall carbon surface, where the duration of transmitter releas

277 Similar to carbon taxes, our model projects an optimal fee that ris

278 Mice were then given diethylnitrosamine and carbon tetrachloride (CCl(4)) to induce mutations, chron

279 albeit transient reduction in fibrosis after carbon tetrachloride injury, associated with increased H

280 ular injury in knockout mice despite ongoing carbon tetrachloride insult, associated with increased n

281 organic matter determines the proportion of carbon that is either stored or emitted to the atmospher

282 nd a metabolic mechanism for the recovery of carbon that would otherwise be lost as ethanol, for exam

283 ntaminated material, and modulates fluxes of carbon through Earth's largest terrestrial carbon reserv

284 is 3.6 kcal/mol lower than that to the beta-carbon, thus favoring the linear chiral aldehyde over th

285 e hydrogen transfer reaction from rhodium to carbon to form the H-C bond.

286 ently reported a linear relation between the carbon to zirconium atomic ratio (C/Zr) and the lattice

287 chondrial oxidation of glucose and glutamine carbons to support the bioenergetic demand of translatio

288 e, glutamine and fatty acids all contributed carbons to the TCA cycle.

289 Total organic carbon (TOC) mass concentrations are decreasing across t

290 Intriguingly, higher total organic carbon (TOC) removal was achieved when antibiotics and m

291 Under the low carbon transition scenario, China's urbanization rate is

292 ); however, the sensitivity of tropical soil carbon turnover to large-scale hydroclimate variability

293 scovered methyltransferase MtcB, sending one-carbon units into production of short-chain fatty acids.

294 The methionine salvage pathway recycles one-carbon units lost to polyamine biosynthesis to the methi

295 e precipitation decreases in the future, the carbon uptake capacity of boreal bogs may be threatened.

296 h a linear relationship between the heat and carbon uptake of the ocean in response to anthropogenic

297 chy of Escherichia coli to be ordered by the carbon-uptake flux rather than the identity of the subst

298 metrics to achieve due to trade-offs between carbon use for growth and production.

299 een 7.5 x 10(14) and 2.5 x 10(15) g of black carbon was released from the target and ejected into the

300 evertheless, nearly one-half billion tons of carbon were lost from both ITs and PNAs (-434 MtC and -4