ライフサイエンスコーパス: tide

1 impact because of their ability to form "red tides".

2 ated with harmful algal blooms known as 'red tides'.

3 s, surge flow, or air temperature during low tide).

4 where planetary gravity dominates over solar tides).

5 iberate plantation and seeds floating on the tide.

6 ity compared with the classical AKT(Thr-308)-tide.

7 (m) for MgATP but not on k(cat)/K(m) for FAK-tide.

8 tively higher concentrations observed at low tide.

9 nted a significant source of MeHg during low tide.

10 eristic of a tidal cycle, beginning with low tide.

11 and cool gulf water onto the bank during ebb tide.

12 ith larger measurements observed on outgoing tides.

13 ales-Verrucomicrobia group increased at high tides.

14 frequencies ranging from 20% to 0.5% of high tides.

15 he same as the principal lunar and lunisolar tides.

16 -dG and at C8 in all the guanine nucleosides/tides.

17 thquakes and the occurrence of the strongest tides.

18 erturbers such as passing stars and Galactic tides.

19 ffective in elucidating mechanisms caused by tides.

20 min and were generated on both ebb and flood tides.

21 rates containing abnormal and damaged nucleo-tides.

22 lanktonic ciliate which can form coastal red-tides.

23 into the backbone of a number of oligonucleo-tides.

24 ) have been linked to coral reefs during low tides.

25 and submerged due to periodic ebb and flood tides.

26 increased tidal range: spring ebb and flood tides.

27 terococci were elevated during ebb and flood tides.

28 inary complexes (Kd(ATP) = 0.6 microM and Kd(Tide) = 1 microM).

29 llowed by low affinity binding of Tide (K(d)(Tide)=180 microM), and values of K(m)(ATP)=5-6 microM an

30 and values of K(m)(ATP)=5-6 microM and K(m)(Tide)=4-5 microM were expressed in the active ternary co

31 croM), K(iMgATP) (1.3 +/- 0.2 microM), K(FAK-tide) (5.6 +/- 0.4 microM), and K(iFAK-tide) (6.1 +/- 1.

32 K(FAK-tide) (5.6 +/- 0.4 microM), and K(iFAK-tide) (6.1 +/- 1.1 microM) were obtained.

33 2-->Val) [DNA: C-to-T substitution at nucleo-tide 677 (677C-->T)] in methylenetetrahydrofolate reduct

34 omplex (alphaKd(ATP) = 40 microM and alphaKd(Tide) = 80 microM) from individual transitory binary com

35 dissolved organic matter (DOM) supply at low tide, a synchronous increase in numbers of bacteria and

36 aused by reflection of semi-diurnal internal tides affects sedimentation patterns and bottom gradient

37 systems that are found in the blooms of red tide algae.

38 Brevetoxins, the toxic components of "red tide" algae, all share one of two robust polycyclic ethe

39 Brown tide algal blooms, caused by the excessive growth of Aur

40 Karenia brevis is the dominant toxic red tide algal species in the Gulf of Mexico.

41 interaction of climate and the timing of low tides along the West Coast of the United States creates

42 Earth's body tide-also known as the solid Earth tide, the displacemen

43 (pre)biological building blocks (nucleosides/tides, amino acids and lipid precursors) under aqueous (

44 ave characteristics, and to a lesser extent, tides, amplify the resulting design heights by an averag

45 nhibitors, including 2'-modified nucleoside/-tide analogs such as PSI-6130, PSI-7977, INX-08189, and

46 1821 CE probably resulted in a similar storm tide and a significantly larger storm surge.

47 ansport warm water off the bank during flood tide and cool gulf water onto the bank during ebb tide.

48 enerated by the ocean lunar semidiurnal (M2) tide and demonstrate that magnetic fields of oceanic ori

49 inetic mechanism, for which both E-MgADP-FAK-tide and E-MgATP-P-FAK-tide dead-end complexes form.

50 ion PDK1-tide1 substrate versus AKT(Thr-308)-tide and kinase selectivity profiling revealed a novel s

51 n air temperature and relative humidity, and tide and wave actions dilute a fraction of the high sali

52 rate the combined effects of evaporation and tide and waves on subsurface salinity distribution on a

53 hour of day, day of year, minutes from high tide and year.

54 n geophysical fluctuations, such as internal tides and atmospheric-related inertial currents, rather

55 consider the joint effects of non-stationary tides and mean sea level (MSL) at multiple time scales.

56 te enterococci measurements may be biased by tides and other environmental factors, providing a flawe

57 X), the agent infamously associated with red tides and paralytic shellfish poisoning, is described.

58 lating to wavelengths that are controlled by tides and rotation, we suggest that Titan's moment of in

59 t long wavelengths that are not dominated by tides and rotation.

60 ), most commonly associated with oceanic red tides and shellfish poisoning, is a potent inhibitor of

61 gnitude and the relative influence of waves, tides and surge levels), we have performed a computer-ba

62 rcular orbit is unlikely to be the result of tides and therefore was probably present at formation.

63 Global curve-fitting analysis of ATP, Tide, and ADP titrations of pre-steady-state burst kinet

64 me on the flanks consistent with an internal tide, and high short-term variability in water temperatu

65 to combine sea-level projections with wave, tide, and storm surge models to estimate increases in co

66 ains can trap dry weather runoff during high tide, and then release it in a bolus during the falling

67 PDK1-catalyzed trans-phosphorylation of PDK1-Tide approximates a Rapid Equilibrium Random Bi Bi syste

68 r velocities caused by semi-diurnal internal tides are high enough to inhibit deposition of fine-grai

69 The resulting "@-tides", as these oligomers have been designated, show a

70 Basal pHi is improved and the "acid tide" associated with secretin returns, but there is sti

71 re, is useful as a quantitative measure of @-tide association and folding processes that involve this

72 inserted a double lox cassette a few nucleo-tides before the authentic ATG start of MHL-1, the gene

73 y; on varying Tide concentrations, ADP and p'Tide behaved as noncompetitive and competitive inhibitor

74 ct and the (T/E)-PDK1-Tide product analog (p'Tide) behaved as competitive and noncompetitive inhibito

75 uria (26/26) suggested MSE onset on a rising tide between 06:30 and 08ratio21 hrs (9 June).

76 K1 called the PDK1-interacting fragment (PIF)tide-binding site, or PIF pocket.

77 ocide hydrogen peroxide (H(2)O(2)) for brown tide bloom control.

78 When applied to brown tide bloom prone natural seawater in a microcosm study,

79 ent effectively removed the developing brown tide bloom, while the rest of phytoplankton assemblage (

80 nction and are associated with periodic "red tide" blooms.

81 ina brevis, an organism associated with 'red tide' blooms in the Gulf of Mexico.

82 Florida red tide brevetoxins are sodium channel neurotoxins produced

83 enhanced vertical mixing, perhaps driven by tides, brings abyssal nutrients to the surface and suppl

84 ltered and unfiltered groundwater during low tide, but were similar to seawater U-Hg(T) concentration

85 icated that enzymatic phosphorylation of FAK-tide by FAK1 was best described by a random bi bi kineti

86 step follows formation of the E-MgADP-P-FAK-tide complex.

87 etitive inhibitors, respectively; on varying Tide concentrations, ADP and p'Tide behaved as noncompet

88 Using both procedures, an oligonucleo-tide conjugate was prepared having the NDI intercalator

89 ms, and this may account for the high nucleo-tide conservation of this unusual gene structure from fi

90 Periodic ocean tides continually provide a cyclic load on Earth's surfa

91 Are perturbations to ocean tides correlated with changing sea-level and climate, an

92 ce of mud/seawater inhalation (11/26), local tide cycle, and the relative lack of renal myoglobinuria

93 evation higher than the highest astronomical tide datum - captured the biotic and edaphic marsh-uplan

94 hich both E-MgADP-FAK-tide and E-MgATP-P-FAK-tide dead-end complexes form.

95 GPS)-based measurements of semi-diurnal body tide deformation.

96 A pep- tide derived from the putative C-C' loop of FN3 (GSQRKHS

97 on Aureococcus anophagefferens bloom (brown tide) development.

98 Measurements of @-tide dimerization and beta-hairpin folding equilibria no

99 n the maintenance of large blooms of the red-tide dinoflagellate Karenia brevis, which produces poten

100 nown as brevetoxins are produced by the 'red tide' dinoflagellate Karenia brevis.

101 How and where the ocean tides dissipate their energy are long-standing questions

102 e with reduced riverine influence located on tide-dominated sand islands), across elevation gradients

103 low probabilities (unbounded tails), 82% are tide-dominated, and almost 49% are highly susceptible to

104 incorporating the timing of semidiurnal high tide events throughout the breeding season, including ho

105 cintillans (Noctiluca) is a cosmopolitan red tide forming heterotrophic dinoflagellate.

106 trogen or phosphorus deficiency in the brown tide-forming alga Aureococcus anophagefferens.

107 er increased approximately 7-fold during low tide (from 0.5 to 3.6 pM).

108 Therefore, either the tide gauge estimates are too high, as has been suggested

109 sed on a modified Kalman smoother, for using tide gauge observations to estimate the individual sourc

110 Our synthetic tests indicate that when all tide gauge records are used in the analysis, it should b

111 The analysis of long-term tide gauge records identified an extreme sea-level rise

112 However, the brevity of tide gauge records result in significant uncertainties w

113 ng an area-weighting technique for averaging tide gauge records that both incorporates up-to-date obs

114 PS-derived radial motions with Fennoscandian tide gauge records to estimate a regional sea surface ri

115 year event) during the entire history of the tide gauge records.

116 e of sea-level rise recorded by the New York tide gauge.

117 Numerical model simulations, combined with tide-gauge and satellite altimetry data, reveal that wav

118 proxy relative sea-level reconstructions and tide-gauge data.

119 USArray Transportable Array inland and NOAA tide gauges along the coast recorded the pressure anomal

120 ent an analysis of sea level measurements at tide gauges combined with observations of temperature an

121 egory 4 storm, passed directly over six wave-tide gauges deployed by the Naval Research Laboratory on

122 Most direct estimates from tide gauges give 1.5-2.0 mm yr(-1), whereas indirect est

123 Here, we survey 152 tide gauges in the Pacific Ocean and South China Sea and

124 and our use of a common reference datum for tide gauges may explain the lower rates compared with ea

125 cing at the surface associated with Saturn's tides, geology, and/or surface composition.

126 During low tide, groundwater appeared to transport MMHg to the coas

127 e active; with an increased salinity at high tide, halotolerant clusters III, V, and X were predomina

128 After decades of disappointment, the tide has finally changed due to the success of recent pr

129 Remarkably, the tide has now turned again: the most important calcium tr

130 tuents, a proxy for the highest astronomical tide (HAT), changes over seasonal and interannual time s

131 Tides have been recognized as a major driving forcing af

132 ed of higher affinity, moth cytochrome c pep-tide I-Ek tetramer-binding cells resulted in substantial

133 nces in tumor immunology have now turned the tide in favor of immunotherapy for the treatment of many

134 ave a comparable role in deep circulation to tides in areas with complex topography.

135 This study demonstrates the importance of tides in regulating the dynamics of dissimilatory nitrat

136 --comparable with levels caused by winds and tides--in the vicinity of large populations of planktoni

137 e we propose that the dissipation of extreme tides increases vertical mixing of sea water, thereby ca

138 he sediment-tidal water interface and at the tide-induced groundwater fluctuating layer.

139 es associated with the solid-earth and ocean tides influence the genesis of tremor much more effectiv

140 stress optimized mangrove development along tide-influenced tropical coastlines.

141 , a function of bed surface depth below high tide, influences the rate of sediment deposition and slo

142 Generated primarily by the wind and the tides, internal waves can travel thousands of kilometres

143 tering by ocean-bottom topography of surface tides into internal waves, but estimates of the magnitud

144 roM) was followed by low affinity binding of Tide (K(d)(Tide)=180 microM), and values of K(m)(ATP)=5-

145 of enterococci in dry sands at the mean high-tide line was significantly positively related to sand m

146 samples came from sandy beaches at the high tide line, and most seawater samples were taken at the s

147 topographic and population data, local high tide lines, and regional long-term sea-level commitment

148 f energy propagation of semidiurnal internal tides may determine the average gradient of continental

149 e mechanism, we propose that extreme oceanic tides may produce changes in sea surface temperature at

150 f one of the moon's semi-diurnal gravimetric tides might have driven the patients' bipolar cycles, by

151 Here we propose a "tide" model to accommodate and interpret current experim

152 idge agrees with the predictions of internal tide models.

153 Earth tides modulate tremor and low-frequency earthquakes (LFE

154 hey are shredded by the strong gravitational tides near the white dwarf core.

155 Building on these lessons to turn the tide of biodiversity loss will require bold and innovati

156 ts have started to pull together in a rising tide of coherence and organization.

157 protect endangered wildlife against a rising tide of infectious disease?

158 health partnerships, which have stemmed the tide of infectious diseases in low- and middle-income co

159 tially dedicated exclusively to stemming the tide of infectious epidemics.

160 In this era of systems biology, the tide of information derived from "omic" technologies (ge

161 ities a legal avenue to help curb the rising tide of juvenile smoking without raising taxes, creating

162 latform for beginning to confront the rising tide of non-communicable diseases.

163 An incoming tide of research is now beginning to challenge this as y

164 effectiveness is now threatened by a rising tide of resistance.

165 We anticipate our work may turn the tide of the dogmatic view of CHOP and cause a reinvestig

166 own been shown to be sufficient to stem the tide of the epidemic.

167 he power of research in children to turn the tide of the growing burden of non-communicable, chronic,

168 ention and management strategies to stem the tide of this disease and its cost.

169 gent and immediate action to stem the global tide of tobacco-related death and suffering and to impro

170 ction of RFL cells showed slowly propagating tides of cGMP spreading across the cell in response to d

171 to develop novel therapies that may turn the tide on the continuing struggle to find effective cures

172 ombination prevention strategies to turn the tide on the HIV pandemic.

173 -wetland complexes located above the head-of-tide on the western shore of Chesapeake Bay.

174 en cycling microorganisms, but the effect of tides on dissimilatory nitrate reduction, including deni

175 proximately 13-14 bp on dsDNA, and no nucleo-tides on the single-stranded tail of the DNA product.

176 We propose that tides played a catalytic role in liberating iceberg arma

177 rients increased the biomass and evenness of tide pool macrophytes where consumer abundance and nutri

178 In this study, we used tide pool microcosms to demonstrate that the effects of

179 ndria from a patient heteroplasmic at nucleo-tide position 8993 of mitochondrial DNA (mtDNA) were int

180 trations, the ADP product and the (T/E)-PDK1-Tide product analog (p'Tide) behaved as competitive and

181 hat excessive Cu and Ni likely promote brown tides, provides evidence for trace metal linkages in alg

182 th with the Moon and Sun at times of extreme tide raising forces.

183 ations in the strength of the global oceanic tide-raising forces caused by resonances in the periodic

184 isance flooding," often associated with high tides, recent increases in frequency are more clearly li

185 Tide records going back to the 19th century show no meas

186 At low tide, representative of higher DOM and increased prey bu

187 We use it to measure the Earth tides, revealing the long-term stability of our instrume

188 ETV differs from the other nucleoside/tide reverse transcriptase inhibitors approved for HBV t

189 hosphorylation of a model peptide substrate (Tide, RRRLSSLRA).

190 d culturable enterococci populations in high-tide sands.

191 le violations), (ii) exons (including nucleo-tide sequence, length and GC content), (iii) protein cod

192 At Hong Kong, the increase in tides significantly amplifies the risk caused by sea-lev

193 s revealed distinct shifts such that, at low tide, significantly higher phylotype abundances were obs

194 -terminal amino acids within an 8-residue, @-tide-stabilized [in which @ denotes the 1,2-dihydro-3(6H

195 multiple drivers (e.g., extreme coastal high tide, storm surge, and river flow).

196 ion when incorporated in an oligopeptide ("@-tide") strand.

197 Daily tide stresses were previously thought to be insufficient

198 orrelations between smaller events and daily tide stresses.

199 ped using a biotinylated version of the PDK1-tide substrate containing the activation loop of AKT fus

200 Our results suggest that internal tides, substrate heterogeneity and oceanographic interfa

201 d 1 mol of tightly bound heme per mol of pep tide subunit.

202 controlled by comparable contributions from tides, surface winds and passing eddies.

203 oreover, depth and frictional changes affect tide, surge, and wave characteristics, altering the rela

204 pically consider the superimposed effects of tides, surges, waves, and relative sea-level rise (SLR),

205 we describe the synthesis of a variety of @-tide-templated hairpins and the NMR and CD characterizat

206 ophagefferens populations from a dense brown tide that occurred in Long Island, NY, in 2009 were assa

207 The regenerative process may tide the loss of overall beta-cell function, but it also

208 th's body tide-also known as the solid Earth tide, the displacement of the solid Earth's surface caus

209 itude of the moon's semi-diurnal gravimetric tides: the 14.8-day spring-neap cycle, the 13.7-day decl

210 All of these devices can observe the Earth tides: the elastic deformation of the Earth's crust as a

211 Going against the current tide, this paper argues that there is indeed a systemati

212 1(deltaPH)-catalyzed phosphorylation of PDK1-Tide (Tide), which contains an extended "PIF" sequence C

213 d during the peak spawning period after high tide to produce a linear relationship.

214 The ability of damaged nucleo-tides to inhibit exonucleolytic digestion differs signif

215 The cascade from tides to turbulence has been hypothesized to serve as a

216 Given these major elements in the tides-to-turbulence cascade, an energy budget approaches

217 plitude and steepness as internal waves from tide-topography interactions observed elsewhere, and is

218 ed frequently in the absence of any apparent tide-topography interactions.

219 Tides transport warm water off the bank during flood tid

220 roundwater discharge to the ocean during low tide transported mercury offshore.

221 Inundation by spring tides was the primary rewetting mechanism that sustained

222 2+) concentrations lower than those in brown tide waters enhance A. anophagefferens growth, but Zn se

223 d Ni(2+) concentrations, e.g. those of brown tide waters in the northeastern US, greatly stimulated A

224 lobal sea level and sedimentation, including tide, wave and fluvial processes.

225 an normal ocean-level fluctuations caused by tides, waves, and storm surge.

226 times larger than those associated with the tides, we argue that tremor occurs on very weak faults.

227 These oligonucleo-tides were constructed from novel monomeric units (2'- t

228 hen release it in a bolus during the falling tide when drainpipe outlets are exposed; (3) nearshore t

229 e substrate (Ac-RRRRRRSETDDYAEIID-NH(2), FAK-tide) which corresponds to the sequence of an autophosph

230 aPH)-catalyzed phosphorylation of PDK1-Tide (Tide), which contains an extended "PIF" sequence C-termi

231 ng the climatic influence of the lunar nodal tide, which has been detected with its modern 18.6-yr pe

232 analyze the LFE response to the fortnightly tide, which modulates the amplitude of the daily tidal s

233 vent viscosity had no effect on k(cat)/K(FAK-tide), while k(cat) and k(cat)/K(MgATP) were both decrea

234 owing to constant changes in river inflows, tides, wind, and water height, all of which combine to a

235 e of 1 mM [gamma-(18)O(4)]ATP and 1.5 mM FAK-tide with a progressive time course which was commensura

236 and III and assayed incorporation of nucleo-tides with modified sugars by these variants, all of whi

237 ater (3.3-5.2 pM) decreased during a falling tide, with groundwater U-Hg(T) concentrations typically

238 ate is highest during the waxing fortnightly tide, with LFEs most strongly promoted when the daily st

239 one-half could therefore be provided by the tides, with the other half coming from action on the sur

240 Here we show that ocean tides within the Labrador Sea were exceptionally large o