ライフサイエンスコーパス: ca.

1 meance of 3.5x10(-7) mol m(-2) s(-1) Pa(-1) (ca. 1000 GPU).

2 yield DeltaHf,298K = (325 +/- 8) kJ mol(-1), ca. 10 kJ mol(-1) below the previous value.

3 the relatively short lifetime of HFC-1447fz (ca. 8 days) implies that its global warming potential at

4 the substrates and pre-catalyst (NiCl2.6H2O, ca. $9.5/mol) bode well for the immediate widespread ado

5 m) increases dramatically from 0.45 to 3.79 (ca. 8-fold).

6 nsertion caused minimal change at pH 8 but a ca. 50 degrees C drop in the melting temperature (Tm ) w

7 Calculations confirm a ca. 17 kcal/mol barrier for the formation of 2-diazometh

8 taining one modification (10:15) displayed a ca. DeltaDeltaG degrees of +4 kcal/mol with respect to i

9 alamin EtPhCbl forms an excited state with a ca. 247 ps lifetime.

10 its represent a rich source of provitamin A (ca. 124 mug retinol-activity-equivalents/100g pulp, FW).

11 ved organic carbon (DOC) concentration above ca. 250 muM the binding capacity was only 50% of the the

12 isible and IR wavelengths at pressures above ca. 56 GPa, suggesting the imminent closure of its optic

13 phases of particularly rapid C accumulation (ca. 6.6-6.1 and ca. 4.9-3.9 ka BP), potentially resultin

14 e gonads were rich in essential amino acids (ca. 32.1% of total amino acids) with the most predominan

15 for carbon dioxide over nitrogen and adsorbs ca. 3 wt % of CO2 at ambient temperature and pressure.

16 archaeomagnetic curve from southern Africa (ca. 1000-1600 AD).

17 ularly rapid C accumulation (ca. 6.6-6.1 and ca. 4.9-3.9 ka BP), potentially resulting from increased

18 essed at the wildtype Michaelis complex, and ca. 50% is only expressed at the wildtype transition sta

19 stability for 50 charge/discharge cycles and ca. 7h at a discharge current density of 0.2mAcm(-2).

20 approximately 10,000 cal YBP in Labrador and ca. 6,000 cal YBP in Newfoundland [2, 3].

21 ystallization space than a random search and ca. 6 times more than humans and increases the crystalli

22 d with ca. 43 new species in the D world and ca. 39 new species in the H world.

23 al of terrestrial organisms at approximately ca. 20 and 6 Ma and corresponding events separating mari

24 assisted sampling of micrometer-sized areas (ca. 11 x 17 mum wide x 2.4 mum deep) from relatively low

25 de and longitude as co-variates explained as ca. 75% of the variability of the contaminant sediment c

26 ibits lattice thermal conductivity as low as ca. 0.5 W/mK near room temperature, owing to rattling dy

27 o exhibit negative water vapor adsorption at ca. 40-50% relative humidity (RH).

28 ophic drainage of proglacial Lake Agassiz at ca. 8.2 ka.

29 nction began at ca. 12,900-13,200 BP, and at ca. 12,600-13,900 BP in South America.

30 vation of displaced water libration bands at ca. 730 cm(-1) upon solvent replacement by adsorbed MOP.

31 ontiguous United States, extinction began at ca. 12,900-13,200 BP, and at ca. 12,600-13,900 BP in Sou

32 rollback from ca. 70 Ma and slab breakoff at ca. 53 Ma.

33 e and l-valine in pH 7.0 phosphate buffer at ca. 100 degrees C.

34 th 2 equiv of ethylene or t-butylethylene at ca. 25 degrees C to yield Sn2(Ar((i)Pr6))2R2(R = ethyl o

35 ed, or land use around Lake Sauce changed at ca. 800 cal.

36 wine and viniculture from the Near East, at ca. 6,000-5,800 BC.

37 -aryldiazenes in preheated diphenyl ether at ca. 150-250 degrees C for 5-25 min affords in most cases

38 itions for these complexes were all found at ca. 420 nm, their emission bands exhibited large Stokes

39 ugh flash vacuum pyrolysis of CF3 S(O)NCO at ca. 1200 K, sulfinyl isocyanate, bearing resonance struc

40 vee systems is estimated to have occurred at ca. 7 cal.

41 anisms in the Atlantic and Pacific oceans at ca. 23 and 7 Ma.

42 ity (including ignimbrite and mafic rock) at ca. 52-51 Ma corresponds to a sudden decrease in the Ind

43 curve and the Late Pleistocene time-scale at ca. 40 ka.

44 racterized by a broad (1)H chemical shift at ca. 12-15 ppm that is reported here for the first time.

45 a first-order structural phase transition at ca. 4 GPa similar to previous reports on other Cu(II)-Cl

46 a previously unreported phase transition at ca. 8 GPa and dramatic piezochromism from translucent re

47 Ongeluk Formation volcanism at ca. 2,426 Ma was part of a large igneous province (LIP)

48 109 degrees , distance N(zeta)-acceptor atom ca. 2.7-3.0 A).

49 30 400 copies per haploid genome, averaging ca. 1900 copies per telomere, and synthesized by telomer

50 ca. 30-150 nm derived from Ni wire backbone (ca. 2 mum in diameter) is directly synthesized on commer

51 ercentage of stacking faults was found to be ca. 10%.

52 Several such compounds proved to be ca. 10- to 100-fold catalytically superior to the diaryl

53 ts at 298 K are consistently predicted to be ca. 25 kcal/mol, whereas barriers for 1,5- and 1,6-shift

54 ch loss of gene function had occurred before ca. 1650.

55 k of regeneration of these populations began ca. 165 ya (around 1850) after major anthropogenic distu

56 t near a critical point (contact angle being ca. 153 degrees ) the bulk thermal resistance has the le

57 on and the onset of the GOE occurred between ca. 2,460 and 2,426 Ma, approximately 100 My earlier tha

58 Brief (ca. 2 min) application of an electrochemical potential a

59 quantum yields (ca. 0.5-0.7) and brightness (ca. 35000-40000 M(-1) cm(-1)).

60 hat dilute alloying decreases 1's bandgap by ca. 0.5 eV.

61 eir visible absorption and emission bands by ca. 200 nm compared to the unsubstituted parent compound

62 itionally understood to have fully closed by ca. 3.5 million years ago (Ma), and this date has been u

63 nts show that increasing heme E degrees ' by ca. 210 mV results in increases in electron transfer (ET

64 change in oxygen atom transfer reactivity by ca. two orders of magnitude.

65 the lagoon were equivalent to, or reduced by ca. 30-40% compared to those from the reef.

66 t rates, such as 20C and 50C with capacities ca. 164 and 75 mAh g(-1), respectively.

67 ofossils of aquatic plants are in many cases ca. 2 degrees C warmer in the early Holocene (11,700-7,5

68 zing bimetallic PtCo nanoparticle catalysts (ca. 1.5 nm) highly dispersed in the framework of nitroge

69 abilize ultra-small ruthenium (Ru) clusters (ca. 0.8 nm) at a high loading density up to 5 wt %.

70 Species subsets that comprised ca. 85% of the original set can be considered reliable s

71 naked eye well below sub-ppm concentrations (ca. 30 ppb) with analytical detection limits of 5.4 ppb

72 oximately 800-1300 CE) and wetter conditions ca. 2 ka were caused by changes in the El Nino/Southern

73 ibits ultralow lattice thermal conductivity (ca. 0.18 Wm(-1) K(-1) ) and a high figure of merit of ab

74 in at both pH 7.0 and 3.0 (binding constants ca. 1.0x10(5) at 25.0 degrees C).

75 ions up to 100 mg/kg U as U(IV) and contains ca. 286 g of U in total.

76 urrent with human dispersal on the continent ca. 47,000 years ago.

77 e [ca. 661 (597-736) Ma], Corallinophycidae [ca. 579 (543-617) Ma], and the split of Ahnfeltiophycida

78 on the time scale of the hyperfine coupling (ca. 100 ns).

79 The algorithm-based search is able to cover ca. 9 times more crystallization space than a random sea

80 rmite species preserved in Early Cretaceous (ca. 100 mya) amber from Myanmar, one described as Krishn

81 North America during the latest Cretaceous (ca. 80-66 million years ago).

82 14 is highly enriched in the binary culture (ca. 10% genomic reads) and its ungapped 0.95 Mbp genome

83 ions on carbon ultramicroelectrodes (CUMEs), ca. 500 nm radii.

84 reased thermal denaturation values (DeltaTm, ca. 2.5-11.5 degrees C).

85 ciency (CE) of 90% and high current density (ca. 2 mA/cm(2) for the stripping peak).

86 ions into inorganic host materials developed ca. 40 years ago.

87 Local patches of strained material (diameter ca. 5 mum) form interwoven patterns seen in birefringenc

88 ted "corn-like" SnO2 nanoparticles (diameter ca. 5 nm) decorated along a "cob", addressed the irrever

89 n, NiO-decorated Ni nanowires with diameters ca. 30-150 nm derived from Ni wire backbone (ca. 2 mum i

90 an earlier colonization by Paleoeskimo dogs ca. 4500 years ago is unknown.

91 such varieties could be reduced drastically (ca. 80%) without affecting considerably the overall qual

92 ) influx through TRPA1 cation channels (EC50 ca. 200 nM), thereby explaining its ability to stimulate

93 oxicity, rapid drug decay, and low efficacy (ca. 20%).

94 acyclovir, with high entrapment efficiency (ca. 46-56%), could be prepared, and sustained release of

95 II) with reduced band gap; that is, enabling ca. 0.41 eV band gap modulation through introduction of

96 oduces each stereocenter with high enantio- (ca. 93% e.e.), diastereo- (up to 25:1 d.r.), and regiose

97 Larger enzymes (ca. 5 nm) can be encapsulated and retained within the ve

98 epopulation-following mission establishment (ca. 1775 CE)-reduced the self-limiting effect of Native

99 originated in the Early Miocene of Eurasia (ca. 19 Ma).

100 k from which oxygenic photosynthesis evolved ca. 2.3 billion years ago.

101 nd of the Lomagundi carbon isotope excursion ca. 2,060 Ma.

102 The as-prepared PtZn iNPs exhibited ca. 10 times higher mass activity in both acidic and bas

103 charged with KCN, transport is much faster (ca. 100 h) and higher K2MX4 equilibrium ratios are obtai

104 but fed at a faster rate when they did feed (ca. 26%).

105 mically smooth surfaces during the fleeting (ca. 20 ms) individual slip events.

106 NBS-LPE, only a small amount of apple flesh (ca. 10mg) was sampled directly using a syringe needle an

107 l assemblages precipitated from mixed fluids ca. 65 m below the Cretaceous paleo-seafloor at temperat

108 rous fishes consumed dramatically less food (ca. 90%) but fed at a faster rate when they did feed (ca

109 Here we use data for ca. 50,000 tropical seedlings representing 25 woody spec

110 of charge (SOC) under AM1.5 illumination for ca. 1.7 hours without any external bias.

111 lower impact, but were still responsible for ca. 9% of juvenile mortality on shags, whereas sport tro

112 nely-laminated sediments were deposited from ca. 5000 years ago until the present, and human activity

113 lk water protons increased dramatically from ca. 1.5 mm(-1) s(-1) to 13 mm(-1) s(-1) between pH 5 and

114 essive NMR shielding of the (1)H nuclei from ca. 4.70 to 1.25 ppm going away from the border of the r

115 nuclear phylogenomic datasets, ranging from ca. 25 Kb to 16.8 Mb and inferred topologies using both

116 antle input controlled by slab rollback from ca. 70 Ma and slab breakoff at ca. 53 Ma.

117 In situ hydrogel softening (from ca. 14 to 3.5 kPa) led to a decrease in the cell area an

118 of YAP/TAZ, and subsequent stiffening (from ca. 3.5 to 28 kPa) increased the cell area and nuclear l

119 verted the mixture from a liquid into a gel (ca. 0.1 mm min(-1)).

120 subset{Mo24 Fe12 } macrocycle forms a giant ca. 220 nm(3) unit cell containing 16 macrocycles cluste

121 -alignment of macro-nanodiscs (diameter of > ca. 40 nm) can be exploited for solid-state NMR studies

122 flow fractionation-ICPMS analyses to sizes > ca. 1 kDa.

123 Although the oxidation potential of BPAs (>ca. 1.80 V SHE) is significantly higher than the estimat

124 , respectively) and also for immature gulls (ca. 90% of mortality).

125 f Scopoli's shearwaters and Audouin's gulls (ca. 28% and 23% of total mortality, respectively) and al

126 home-made spread from ground bilberries had ca. 26% higher antioxidant activity.

127 designed sequence was found to activate HCII ca. 250-fold, while leaving aside antithrombin, a closel

128 idence for an economy based on goat herding, ca. 10,000 BP.

129 lved the emergence of Hildenbrandiophycidae [ca. 781 (681-879) Ma], Nemaliophycidae [ca. 661 (597-736

130 only partial photodecomposition of 5Me-HQE (ca. 1/3).

131 a decrease in radial growth before death in ca. 84% of the mortality events.

132 These are generated in ca. 90% yield on metathesis of methyl acrylate, styrene,

133 Occurring in ca. 10 ns, this NR red-shift was caused by the formation

134 if (TTTTTTAGGG)n in C. elegans, occurring in ca. 30 400 copies per haploid genome, averaging ca. 1900

135 s from four unique species, were prepared in ca. 70% isolated yields and fully characterized by multi

136 d as a catalyst and sorbent; this results in ca. 10% higher micropore volume with limited impact on i

137 versatility of the strategy is showcased in ca. 50 examples involving a plethora of electrophiles.

138 n early development of metabolic syndrome in ca. 25% of healthy male individuals suggesting a healthy

139 barriers was integrated with an inexpensive (ca. $300) electronic craft plotter/cutter for paper cutt

140 yet discovered in Amazonia (peat initiation ca. 8.9 ka BP), and developed in three stages: (i) peat

141 As agricultural activity intensified ca. 2200 cal.

142 ivity, the benzyl ester-containing analog is ca. 100-fold less active.

143 the strength of this second coordination is ca. 6-8 kJ mol(-1).

144 depth of ca. 100 nm and the bottom layer is ca. 900 nm.

145 The detection limit is ca. 20 fM, corresponding to 6pgL(-1) diclofenac, which i

146 The genome size is ca. 163 Mb with 19,222 predicted protein-coding genes.

147 at of the native enzyme, with a kcat that is ca. 3 times higher than that of the native enzyme, a kca

148 tion, e.g. the 'no-load' angular velocity is ca. 400 rad/s anticlockwise at 4 mM ATP.

149 polymer matrices with this method, which is ca. two to five times higher than that of phosphor-doped

150 thic sites, and in Nahal Hemar cave (Israel, ca. 8200 -7300 cal.

151 in the fossil record in the Middle Jurassic (ca. 170 million years ago).

152 specific surface area in a relatively large (ca. 750 nm overall diameter) stable structure, can be va

153 o facilitate characterization of very large (ca. 1-4 nm) anionic species.

154 their rates were symmetrical until the last ca. 6 Ma, when northern migration of South American line

155 nuclei concentration background by at least ca. 20%, supporting a marine biosphere-climate link thro

156 largely invariant for all foldamer lengths (ca. 60 ps), the subsequent hole transfer to the donor va

157 l except one mutant - which retained a level ca. 7% of the parent.

158 tant, low stiffness, and large strain limit (ca. 600% strain).

159 ss endophytes and diverged from that lineage ca. 100 MYA.

160 ), and the local carrier lifetimes are long (ca. 200 ns) and surprisingly homogenous among grains, an

161 ermittivity (ca. 102.30) and ultra-low loss (ca. 0.0042).

162 [1,5-a]pyridine 1T, the diazo compound lying ca. 5 kcal/mol above the triazole.

163 dly increased after the Last Glacial Maximum ca. 18 kya.

164 the same reaction in aqueous microdroplets (ca. 5 mum diameter) and find that the cycloaddition reac

165 n group Caragana, dated to the early Miocene ca. 18 Ma and onwards, can be linked to the Himalayan Mo

166 oon formation, in the middle to late Miocene ca. 12~6 Ma.

167 ve workers were known from just the Miocene (ca. 17-20 million years ago [mya]).

168 tivity in the hydrogenation of E/Z mixtures (ca. Z/E = 75:25) of alpha,beta-dialkylvinyl substrates,

169 nd 89 mug/L, respectively for doses of 2 mM (ca. 150 mg/L) PAA and [H2O2] < [PAA].

170 sets were strong (r >/= 0.8) with moderate (ca. 20%) species loss.

171 ate the critical distance between molecules (ca. 4.5 A) needed to explain the vibronic structure quen

172 ent ROS diffusion through ultrathin 2D MOLs (ca. 1.2 nm) enable highly effective X-PDT to afford supe

173 quantitatively evaluated by the exponent n (ca. 3) of the temperature dependence of the relaxation r

174 ly dispersed ultrafine MgO nanocrystallites (ca. 3 nm in size), together with the rGO sheets and in s

175 synthesis is described for Au nanoparticles (ca. 20 nm) supported on N-doped carbon (Au@NC), which wa

176 The CoMnP nanoparticles (ca. 5 nm in diameter) are nearly monodisperse and homoge

177 ispersed, silica-supported Cu nanoparticles (ca. 2 nm) prepared via surface organometallic chemistry

178 " approach for the synthesis of very narrow (ca. 0.5 nm) and soluble GNRs using a nonoxidative alkyne

179 dae [ca. 781 (681-879) Ma], Nemaliophycidae [ca. 661 (597-736) Ma], Corallinophycidae [ca. 579 (543-6

180 Herein, we introduce a novel ca. 1.6 kDa SMA-based polymer with styrene:maleic acid m

181 Armagh numbering ca. 140 mature trees.

182 -O close to 180 degrees , distance N(zeta)-O ca. 2.7-3.0 A).

183 , enables convenient structure assignment of ca. 200 components from wild-type and peroxisomal beta-o

184 ormed atropisomers separated by a barrier of ca. 15 kcal/mol, whose interconversion was studied by DF

185 4.6 F cm(-3) (and gravimetric capacitance of ca. 773.6 F g(-1) ) at a current density of 0.5 A g(-1)

186 dense monodisperse nanoparticles composed of ca. 50 POMs that were characterized by SAXS and transmis

187 um returns with this slower time constant of ca. 150 ms, indicating that the almost fully folded prot

188 protection occurring with a time constant of ca. 85 ms, but slower protection is observed around a re

189 f ca. 1.0 V, an attractive energy density of ca. 43 Wh kg(-1) based on both electrodes' active mass,

190 top layer of the nanojunction has a depth of ca. 100 nm and the bottom layer is ca. 900 nm.

191 10-100 pg), a relative standard deviation of ca. 7%, and an R(2) value of 0.9986.

192 oSUD micelles (particle average diameter of ca. 200 nm).

193 resulting in pSi particles with diameters of ca. 500 nm, composed of a porous network of Si nanocryst

194 ymers with molecular weight distributions of ca. 1.2-1.4 are obtained.

195 Molecular weight distributions of ca. 2 are observed.

196 and reaches a steady Faradaic efficiency of ca. 80 % at only -0.8 V vs. RHE.

197 , this fossil biota suggests an elevation of ca. 1,000 m.

198 s, this system enhances energy by factors of ca. 11 and 3.5, respectively, with a specific energy of

199 ic pre-exponential ln (A/min(-1)) factors of ca. 19-35 and 28-41, in the same order, depending on the

200 to monitor slow reactions at a frequency of ca. 180 h(-1) (on the Mini 12) with no sample carryover

201 th turnover number and turnover frequency of ca. 540 and 1.9 min(-1), respectively, and with 94% sele

202 ident photon-to-current efficiency (IPCE) of ca. 10 % at 400 nm.

203 ndamental photoluminescence (PL) lifetime of ca. 660 ns, which is very encouraging for photovoltaic a

204 Eventually, a detection limit of ca. 1 x 10(-9) M uranyl was achieved using a 5 min depos

205 ensor presents a very low detection limit of ca. 10 pM, (S/N=3) and a very high selectivity towards s

206 rrangements to a limit of detection (LOD) of ca. 15%.

207 The lowest LODs (of ca. 0.1% vol O2) were found on polished SPEs using LTCA,

208 3.3 % and carbon-13 polarization (%P13C ) of ca. 1.8 % were achieved in ethyl acetate utilizing 50 %

209 t proton nuclear spin polarization (%PH ) of ca. 3.3 % and carbon-13 polarization (%P13C ) of ca. 1.8

210 atalytic currents with an onset potential of ca. (-) 0.15 V vs Ag/AgCl, affording higher glucose sens

211 into N2H4, attendant with the production of ca. one molecule of NH3.

212 its of detection (LODs) were in the range of ca. 1-9 ppm, lower than the minimum exposure limit (25 p

213 he nakhlite-source volcano grew at a rate of ca. 0.4-0.7 m Ma(-1)-three orders of magnitude slower th

214 results show that, within our resolution of ca. 0.1 nm, slip of the surfaces is not correlated with

215 Because of the limiting exposure time of ca. 20 s of the membranes with the sample, this approach

216 an be extended to dipolar evolution times of ca. 80 mus, permitting distances up to 170 A to be acces

217 layed low micromolar activity (EC50 value of ca. 2 muM) and limited cytotoxic liability (CC50 > 100 m

218 osits, are marked by zircon Eu/Eu* values of ca. </=0.08.

219 o estimate the CBM, which provides values of ca. -4.0 eV versus vacuum on both ITO and TiO2 electrode

220 tored, with emission quantum yield values of ca. 0.54 in toluene.

221 potent MIF inhibitors bind with Kd values of ca. 50 nM; two are from our laboratory, and the other is

222 performance: an average operation voltage of ca. 1.0 V, an attractive energy density of ca. 43 Wh kg(

223 -symmetric cages having a confined volume of ca. 1300 A(3) .

224 A third drought phase centred on ca. 1.8-1.1 ka BP led to markedly reduced C accumulation

225 ding yeast, in high temporal resolution over ca. 2.5 cycles of the short-period respiratory oscillati

226 osing approximately 27% of its strength over ca. 30 y).

227 the two chemotypes show significant overlap (ca. 90 %) both qualitatively and semi-quantitatively, su

228 ed molecular hybrid organic-inorganic oxides ca. 4-9 nm in size, with molecular weights ranging 2-10

229 aving evolved well after the rise of oxygen (ca. 867 million years ago), and thus cannot be progenito

230 increased biological activity over the past ca. 50 years, in response to climate change.

231 egion, dating to the early Neolithic period (ca. 6,000-5,000 BC), provide the earliest biomolecular a

232 iferous (Pennsylvanian) and Permian Periods (ca. 323-252 Ma), when arborescent vascular plants relate

233 TiO2 THz dielectrics with high permittivity (ca. 102.30) and ultra-low loss (ca. 0.0042).

234 catalyst, ambient pressure, condensed phase, ca. 0.03 m monomer).

235 nd 1050 nm (fwhm approximately 145 meV, PLQY ca. 1.8%), which is the first observation of narrow near

236 ydrogen-bonded DMSO near the eutectic point (ca. 35 mol %) which also correlates with several abnorma

237 ur approach to co-occurring Late Precontact (ca. A.D. 1000-1600) monuments in Michigan: (i) mounds an

238 a high selectivity towards C2 /C3 products (ca. 60 %) for up to 5 h in 0.1 m KHCO3 at -1.0 V vs. RHE

239 In two natural waters, a high proportion (ca. 93-100%) of dissolved Zn was measured, and the resid

240 gh photoluminescence (PL) quantum yield (QY; ca. 15-55 %) and product yield have been synthesized usi

241 of transmission through the reaction region (ca. 20-200 ms), representing a 50-1000-fold improvement

242 PNTs via native chemical ligation, rendering ca. 100 nm-long nanotubes.

243 Recent estimates report ca. 200,000 seabirds killed annually by bycatch in Europ

244 nalyses on a molecular timetree representing ca. 82% of the extant families, and reassess the insect

245 e possesses low equivalent series resistance ca. 3.5 Omega, resulting in superior power performance a

246 of Ahnfeltiophycidae and Rhodymeniophycidae [ca. 508 (442-580) Ma].

247 lation following postglacial sea-level rise, ca. 2.5 ka, to characterize long-term change in insular

248 Herein we report a scalable (ca. 11.0 g per batch) and low-temperature colloidal proc

249 both of which provided similar sensitivity (ca. 0.2 mM(-1)) when normalized to the same standard.

250 the Gold Rush and Euro-American settlement (ca. 1865 CE), fire activity declined, and the strong mul

251 est swamp; and (iii) raised peat dome (since ca. 3.9 ka BP).

252 avelengths in spite of their identical size (ca. 2.5 nm).

253 kite nanocrystals (PNCs) of different sizes (ca. 2.5-100 nm) with high photoluminescence (PL) quantum

254 from the upper Permian (Changhsingian Stage, ca. 254-252 million-years ago) of China documenting a mi

255 ed after implementation of fire suppression (ca. 1904 CE).

256 declines in microbial decay in a long-term (ca. 20 yrs.) N deposition experiment have altered the bi

257 ere in terms of S/N at wavenumbers less than ca. 1400 cm(-1) despite the weaker signal enhancement de

258 y those organics with an IP value lower than ca. 9.0 eV can be oxidized in the CPPy-F-8/PMS system.

259 Our simplest model estimates that ca. 1130 +/- 137 N. cepedianus individuals consume 11,37

260 zed reactions of substrate pieces shows that ca. 50% of the wildtype TIM dianion binding energy, elim

261 Although the ca. 13 ppm chemical shift value is consistent with compu

262 ct the intermediate radical pairs within the ca. 8 ns laser pulse of our laser setup.

263 e were lower in colorectal carcinoma tissue (ca. 2.5- and 3.5-fold, respectively).

264 erator-collector distance (ranging from 3 to ca. 500 mum) on the collection efficiencies obtained at

265 The capacity can be recovered back to ca. 430 mAh g(-1) in 2 cycles when lowered to 0.2C and s

266 tilizing 50 % para-hydrogen corresponding to ca. 50 % polarization transfer efficiency.

267 result patterning of polymer brushes down to ca. 300 nm is reported.

268 e causative low-density structure extends to ca. 6 km depth, which we interpret as a shallow plumbing

269 .6 mug L(-1) and in treated wastewater up to ca. 1 mug L(-1).

270 ese substances occur in raw wastewater up to ca. 1.6 mug L(-1) and in treated wastewater up to ca. 1

271 The small-size nanodiscs (up to ca. 30 nm diameter) can be used for solution NMR spectro

272 ted U, but crystalline U(IV) comprises up to ca. 30% of total U at some locations.

273 perature dependencies remain unchanged up to ca. 700 bar.

274 is results in high doping densities of up to ca. 8 x 10(12) cm(-2) .

275 e isolated in moderate to good yields, up to ca. 90% based on the disproportionation reaction.

276 nanolimulus luopingensis, a Middle Triassic (ca. 244 million years old) horseshoe crab from Yunnan Pr

277 Bird fossils from Turonian (ca. 90 Ma) sediments of Axel Heiberg Island (High Canadi

278 f other skeletal elements from the Turonian (ca. 90-92 million years ago) of Uzbekistan.

279 n donor-acceptor distance (DAD) is typically ca. 2.7 A, considerably shorter than normal van der Waal

280 s in all three biodiversity attributes until ca. 2000, followed by a slow decline since.

281 ed, ice patches remained on the island until ca. 9,000 calibrated (cal) YBP [1].

282 ghest CO2 gravimetric and volumetric uptake (ca. 1.3 mmol/g and 51.4 cm(3) (STP) cm(-3)) for a physic

283 fluorescence quenching is demonstrated using ca. 200 nm diameter template-synthesized polyfluorene na

284 e most to tropical peatland area and volume (ca. 44% for both) partly related to some yet unaccounted

285 by light-weight (ca. 3 mg) and small volume (ca. 30 mm x 2 mm x 10 mum) is driven by a microcontrolle

286 ernative given the relatively small volumes (ca. 100 kt CO2/a).

287 the fraction retained on their surfaces, was ca. 90%.

288 etained to a remarkably high level of water (ca. 42 wt % H2 O) because of solvophobic sequestration o

289 he most active species is a high wavenumber (ca. 1685 cm-1) carbonate that we associate directly with

290 brid actuator characterised by light-weight (ca. 3 mg) and small volume (ca. 30 mm x 2 mm x 10 mum) i

291 the fact that circulating levels of JH were ca. 2 orders of magnitude higher in queens than those in

292 With ca. 3 log inactivation for both Escherichia coli and Bac

293 -MnP phase transition under compression with ca. 22 % unit-cell volume changes, which was found to be

294 ovoltaic tests demonstrate that devices with ca. 10% of mixed phases outperform pure-phase devices.

295 mensional (3D) supramolecular framework with ca. 2.8 nm diameter one-dimensional (1D) hexagonal chann

296 tion cryogenic localization microscopy, with ca. 9 nm between the centers of mass.

297 ey exhibit different open probabilities with ca. 90% in KcvNTS and 40% in KcvS.

298 nable untargeted (discovery) proteomics with ca. 25 amol lower limit of detection.

299 lent in the corresponding isotope world with ca. 43 new species in the D world and ca. 39 new species

300 terized by high fluorescence quantum yields (ca. 0.5-0.7) and brightness (ca. 35000-40000 M(-1) cm(-1