ライフサイエンスコーパス: equatorial

1 nce between couplings of the hydrides to the equatorial (31)P nuclei.

2 ow ingression initiates by contraction of an equatorial actin network with randomly oriented filament

3 s of known ecology from a single locality in equatorial Africa were sampled for tooth enamel and, tog

4 me drier, and monsoonal Asia, Venezuela, and equatorial Africa will become wetter.

5 uatorial South America compared with 8% over equatorial Africa.

6 imilar to those of previous EVD outbreaks in equatorial Africa.

7 high volume air samples and precipitation in Equatorial Africa.

8 e of the most prevalent pediatric cancers in equatorial Africa.

9 s, bonobos, and gorillas residing throughout equatorial Africa.

10 nals of strong selection in populations from equatorial Africa.

11 outbreak of Ebola virus disease (EVD) in the equatorial African country of the Democratic Republic of

12 rica who have considerably lighter skin than equatorial Africans.

13 consistent dry-season declines in GPP in the equatorial Amazon (Manaus K34, Santarem K67, and Caxiuan

14 cation lags between leaf and wood, dominated equatorial Amazon carbon flux dynamics and were deficien

15 aride aminoglycoside scaffolds containing an equatorial amine at the 2' sugar position with a beta-O-

16 Analogues with a bicyclic ring I carrying equatorial amino or hydroxyl groups mimicking the bound

17 r than as their more energetically favorable equatorial analogues.

18 Indeed, 1,2-cis-diols, having an equatorial and an axial hydroxy group, benzoyl cyanide o

19 d abruptly ~14,700 years ago in southeastern equatorial and northern Africa and continued into the Ho

20 At the interface between the equatorial and polar regions, we observe synchrotron emi

21 rcine eyes, 4 regions were obtained: cornea, equatorial and posterior sclera, and posterior pole cont

22 Simultaneous reports of EVD in equatorial and West Africa raised the question of whethe

23 antly, the CLASH model hints at latitudinal, equatorial, and hemispheric upgradings of climato-econom

24 antic Meridional Overturning Circulation and equatorial annual cycle.

25 gical trait shaped by microsporogenesis: the equatorial aperture pattern.

26 its implication in the determination of the equatorial aperture pattern.

27 Most eudicots have three equatorial apertures but several taxa have independently

28 The observed burst of variation upon loss of equatorial apertures shows that there are no strong deve

29 eudicots including species with and without equatorial apertures.

30 At the equatorial area, SD OCT imaging allowed visualization of

31 etinal tears in the pre with respect to post-equatorial areas (19 vs 7 eyes, p = 0.019).

32 ion to removal of these acids in terrestrial equatorial areas and in other regions where high CI conc

33 lity and population exposure of wildfires in Equatorial Asia during Fall 2015, which were the largest

34 f fires on future air quality and climate in Equatorial Asia will be decided in part by the conservat

35 tion of pollution sources and transport over Equatorial Asia.

36 e deaths across densely populated regions in Equatorial Asia.

37 elling planktonic foraminifera in an Eastern Equatorial Atlantic (EEA) sediment core from the Niger D

38 uranium-thorium-dated deep-sea corals in the Equatorial Atlantic and Drake Passage over the past 25,0

39 tmosphere models poorly simulate and predict equatorial Atlantic climate variability.

40 Prevailing theories on the equatorial Atlantic Nino are based on the dynamical inte

41 in coccolith biogeochemistry to reconstruct equatorial Atlantic sea surface temperature (SST) and at

42 Perturbations of the equatorial Atlantic trade winds ( approximately +/-1.53

43 By challenging the dynamical paradigm of equatorial Atlantic variability, our findings suggest th

44 ting nutrients for both the Amazon Basin and equatorial Atlantic.

45 Here we report on a bright equatorial atmospheric feature imaged in 2015 that moved

46 Three distinct oxygen environments (equatorial, axial, and interstitial) can be assigned on

47 ic acid adamantanylthioglycoside carrying an equatorial azide at the 5-position was also found to be

48 and where the active RhoA signal leads to an equatorial band of myosin overactivity.

49 ron-deficient sigma-hole and electronegative equatorial band.

50 and thereby actomyosin assembly, in a narrow equatorial band.

51 e been repeatedly reemerging across the vast equatorial belt of the African continent to cause epidem

52 This gives rise to a substantially enhanced equatorial bonding of the uranyl(VI) ions as elucidated

53 The equatorial C-F bond has a much greater destabilizing eff

54 ributes to the site selectivity and enhanced equatorial C-H bond reactivity for tertiary C-H bonds, a

55 The higher reactivity of tertiary equatorial C-H bonds was explained in terms of 1,3-diaxi

56 kH values for HAT from tertiary equatorial C-H bonds were found to be at least 1 order o

57 explanation of the higher reactivity of the "equatorial" C-H position of CB[n] compounds.

58 effective strategies are available for "all-equatorial" carbohydrates (glucose, etc.), the recogniti

59 actin complexes at the vertices of hexagonal equatorial cells for cell-to-cell alignment.

60 perturb ring geometries from the low-energy equatorial chair ((4)C1) conformation.

61 for lunar origin, the Moon accreted from an equatorial circum-terrestrial disk; however, the current

62 ffect on orbital mixing between the U 5f and equatorial Cl 3p orbitals.

63 passing less than 5000 kilometers above the equatorial cloud tops.

64 (-1) not measured since 1980-1981 with other equatorial clouds moving within an ample range of veloci

65 deficient in ER-PM contacts exhibit aberrant equatorial clustering of actin cables during ring assemb

66 al distance becomes less inverse for shorter equatorial CO distances: a decrease of 0.5 A results in

67 opics, impairing the developing economies of equatorial coastal cities and the habitability of low-ly

68 Our equatorial coccolith-derived geochemical record thus hig

69 rmocline altered the dynamics in the eastern equatorial cold tongue, resulting in reduced ENSO variab

70 ers revealed different combinations of axial-equatorial configurations of the anomeric oxygen.

71 here the trimethylsilyl group is in a pseudo equatorial conformation where it cannot migrate to the c

72 hiophene-S,S-dioxide exhibits only one quasi-equatorial conformer on both donor sites, with charge-tr

73 favorable orientation of bond dipoles in the equatorial conformer, a destabilizing electrostatic effe

74 of the phenyl ring in both the axial and the equatorial conformers of phenyl substituted 1,3-dioxanes

75 completion above a well-defined threshold of equatorial contractility.

76 ian region as an atmospheric response to the equatorial convective anomalies is seen advecting cold t

77 uired for spatially confined RhoA-GTP at the equatorial cortex of dividing cells, both the target spe

78 ein (INCENP), enhances CPC enrichment at the equatorial cortex, thus acting in tandem with MKlp2.

79 d cue to assemble the actomyosin ring at the equatorial cortex.

80 ase in nodes-precursor structures around the equatorial cortex.

81 nd localizes to midzone microtubules and the equatorial cortex.

82 ]thiophene-S,S-dioxide displays both a quasi-equatorial CT state and a higher-energy quasi-axial CT s

83 km along the path of relatively stable North Equatorial Current.

84 r example, flying insects typically increase equatorial curvature between the front and side of the e

85 ciliary muscle ring diameter (CMRD) or lens equatorial diameter (LED).

86 eclines at the range edge in the opposite or equatorial direction, mirrored by changes in the establi

87 the "axial" donor/acceptor distance and the "equatorial" distance to hydrogen-bond acceptors.

88 Whereas the equatorial domain displays almost perfect sevenfold symm

89 the distribution range, although towards the equatorial edges the magnitude of the amelioration provi

90 Src(-/-) equatorial epithelial cells also fail to form precisely

91 In Epha2(-/-) mouse lenses, equatorial epithelial cells fail to form precisely align

92 During lens development, equatorial epithelial cells undergo cell-to-cell alignme

93 The lability of the equatorial (eq) CH3CN groups in these complexes in solut

94 ons in weakening the SH monsoon, because the equatorial eruptions, despite reducing moisture content,

95 ment cells and in the retinular cells in the equatorial eye.

96 rong axial [Cp*](-) ligand field with a weak equatorial field consisting of the isocarbonyl ligands l

97 ds varying between 1.0 and 0.12 times recent equatorial field strengths.

98 rough-space coupling between the SF5-group's equatorial fluorines and proton/carbon nuclei of -H, -CH

99 spreading propagated northwards, opening an equatorial gateway to shallow and intermediate circulati

100 -position was also found to be selective for equatorial glycoside formation under the same conditions

101 sed 4O,5N-oxazolidinone group stabilizes the equatorial glycoside, i.e., reduces the anomeric effect,

102 ees C are selective for the formation of the equatorial glycosides, suggesting that the synthesis of

103 it covered families acting on both axial and equatorial glycosidic linkages, respectively.

104 ed point sources ranged between 8000 USD for Equatorial Guinea and 1.9 million USD for Ethiopia, depe

105 d children lower than 10%) included Burundi, Equatorial Guinea, Eritrea, and Rwanda.

106 urvey in Rio Muni, the mainland territory of Equatorial Guinea, which aimed to estimate the probabili

107 Central African Republic, Congo, Guinea, and Equatorial Guinea.

108 mechansm via Berry pseudorotation involving equatorial halides.

109 al ends and a matrix of N domains forming an equatorial hexamer-hexamer interface, with portals of ap

110 y group supported by hydrogen bonding of the equatorial hydroxy group to the axial oxygen.

111 One such bicyclic compound carrying an equatorial hydroxyl group has activity equal to that of

112 egioselectivity for the glycosylation on the equatorial hydroxyl group of the acceptor was obtained t

113 Its equatorial hydroxyl groups are hydrogen-bonded directly

114 ed by the coordination of calcium by the two equatorial hydroxyl groups, OH3 and OH4, at the non-redu

115 Compounds substituted with an equatorial hydroxyl or amino group in the newly formed r

116 dipole index of the SSSA between the central equatorial Indian Ocean (CEIO: 70 degrees E-90 degrees E

117 have potential to mitigate these effects for equatorial islands.

118 road westward flow rising to an axisymmetric equatorial jet and imparts an eastward-directed torque o

119 Saturn has an intense and broad eastward equatorial jet with a complex three-dimensional structur

120 ossibly mediated by the Miocene Indian Ocean Equatorial Jet, followed by back dispersal to Australasi

121 no evidence for glaciation, ice advanced to equatorial latitudes at least twice between 717 and 635

122 c pole that positions the Kaapvaal Craton at equatorial latitudes of 11 degrees +/- 6 degrees at this

123 y, these results highlight the utility of an equatorial ligand field for facilitating slow magnetic r

124 th N5 pentadentate ligands that modulate the equatorial ligand field of the Mn(IV) center, as assesse

125 s, with faster rates corresponding to weaker equatorial ligand fields.

126 ets (SIMs) with strong axial donors and weak equatorial ligands are attractive model systems with whi

127 stable conformers differing in the axial or equatorial location of the phenyl group and the angle of

128 d occurred in individuals who emigrated from equatorial locations.

129 stem exchange (NEE) and respiration (Re ) at equatorial locations.

130 an-GTP levels or tethering active Ran to the equatorial membrane affects anillin's localization and c

131 xide was fixed as carbonate and bound to the equatorial metal centers in both the Zn5 L6 and Cd5 L6 a

132 atially constrained arrangement of the three equatorial metal ions in the M5 L6 structures was found

133 anone is included more conventionally in the equatorial methyl conformation.

134 leading to the minor enantiomer involves the equatorial model.

135 nt, have weaker effects in weakening the off-equatorial monsoon circulation than the subtropical-extr

136 MTOCs, including the SPB and interphase and equatorial MTOCs.

137 ally related oxo-iron(IV) complex bearing an equatorial N-donor ligand, [L(TMC)Fe(IV)(O) (MeCN)](2+)

138 s possessing the chair conformation with the equatorial NMe group and differing by axial or equatoria

139 waves near the geomagnetic equator known as 'equatorial noise'.

140 en bonding to both hydroxy groups leading to equatorial O-acylation.

141 > GalPUGNAc) but preferred recognition of an equatorial O4 when the aglycon was absent (Ki for GalNGT

142 -nineteenth century and included an enhanced equatorial ocean response mechanism.

143 ducing the NH monsoon precipitation than the equatorial ones, and so do the SH eruptions in weakening

144 Whether equatorial or apical, the molecule is stabilized by a S.

145 ior margin location (iris, ciliary body, pre-equatorial or postequatorial choroid).

146 evolution model starting with the Moon in an equatorial orbit around an initially fast-spinning, high

147 rberos and Hydra--follow near-circular, near-equatorial orbits around the central 'binary planet' com

148 hydroxyphenyl group locked in the piperidine equatorial orientation had potencies equal to or better

149 milar to one another, with only the axial or equatorial orientation of two hydroxyl groups differenti

150 enzyme active site selectively activates the equatorial oxo for transfer, and allows facile structura

151 veals that the adsorbed uranyl ions share an equatorial oxygen atom with a phosphate tetrahedron of t

152 orner-sharing complex, in which two adjacent equatorial oxygen atoms are shared with the vertices of

153 ial surface monolayer became disordered, and equatorial oxygen atoms were displaced towards the surfa

154 d not change in spite of the displacement of equatorial oxygen atoms.

155 I) with coordination of uranium to axial and equatorial oxygen, similar to uranyl.

156 nt over the last deglaciation in the eastern equatorial Pacific (EEP) using benthic and planktonic fo

157 ombine new radiocarbon data from the Eastern Equatorial Pacific (EEP) with chronostratigraphic calend

158 e southern lobe of the NPO, the state of the equatorial Pacific 9-12 months later.

159 Our results suggest that the equatorial Pacific acts as a nonlinear amplifier that al

160 and decreased precipitation over the western equatorial Pacific and Atlantic.

161 arm water volume (WWV) variability along the equatorial Pacific and El Nino-Southern Oscillation (ENS

162 m the sub-Antarctic Atlantic and the eastern equatorial Pacific as a more direct tracer of oceanic CO

163 150 to 110 ka at three sites in the central equatorial Pacific at sub-millennial time resolution.

164 estern boundary currents and the interlinked equatorial Pacific circulation system were among the fir

165 cooperative mode--linking the El Nino basin (equatorial Pacific corridor) and the rest of the ocean--

166 Southern Ocean, we propose that the central equatorial Pacific data are consistent with more nutrien

167 could induce an El Nino-like anomaly, in the equatorial Pacific during the first 8-9 mo after the sta

168 ent concentrations were lower in the central equatorial Pacific during the LGP.

169 nd delta(15)N) from six cores in the central equatorial Pacific for the Holocene (0-10,000 years ago)

170 The efficiency of iron recycling in the equatorial Pacific implies the evolution of ecosystem-le

171 The equatorial Pacific is one of the three principal high-nu

172 Biological productivity in the equatorial Pacific is relatively high compared with othe

173 The equatorial Pacific Ocean is one of the major high-nutrie

174 Today, sea-surface temperatures in the equatorial Pacific Ocean modulate rainfall variability i

175 of redox-sensitive uranium from the central equatorial Pacific Ocean to identify intervals associate

176 y at three sites spanning the breadth of the equatorial Pacific Ocean to test the dust fertilization

177 istent picture of glacial carbon storage and equatorial Pacific Ocean watermass structure.

178 Rather, the thermocline of the eastern equatorial Pacific played a decisive role in the ENSO re

179 layed a greater role than dust in regulating equatorial Pacific productivity.

180 have ultimately worked to lower, not raise, equatorial Pacific productivity.

181 accounting for recent cooling in the eastern equatorial Pacific reconciles climate simulations and ob

182 e dust fluxes on primary productivity in the equatorial Pacific remains uncertain.

183 e reconstruct LGM temperature variability at equatorial Pacific sites using measurements of individua

184 Nitrate persists in eastern equatorial Pacific surface waters because phytoplankton

185 the trade winds over the western and central equatorial Pacific that favors the development of an El

186 to basin-wide uniform warm conditions in the equatorial Pacific the winter before the occurrence of a

187 th records from five previous studies in the equatorial Pacific to document the nonlinear relationshi

188 hat, although dust deposition in the central equatorial Pacific was two to three times greater in the

189 If equatorial Pacific winds resume their predicted weakenin

190 ic dust deposition could have fertilized the equatorial Pacific with iron during the last ice age--th

191 of particulate iron (measured in the eastern equatorial Pacific(30)) is bioavailable.

192 larion-Clipperton Zone (CCZ, abyssal eastern equatorial Pacific) is the focus of a major research eff

193 understand the heat and mass balances of the equatorial Pacific, and possible changes associated with

194 -surface temperature, located in the central equatorial Pacific, based on oxygen isotopic time series

195 ns in sea surface temperature in the eastern equatorial Pacific, leading to major climatic and societ

196 e warming centers in the central and eastern equatorial Pacific, suppressing the positive Bjerknes fe

197 Throughout most of the equatorial Pacific, upwelling of water from the Equatori

198 pical flows and from time series data of the equatorial Pacific, we find that our analytical model re

199 des that upper ocean temperature bias in the equatorial Pacific, which becomes more intense with incr

200 or across the EOT from a site in the central equatorial Pacific.

201 ecords for East Asia and the central-eastern equatorial Pacific.

202 e maximum sea surface warming on the Central equatorial Pacific.

203 ubstantial iron fertilization to the central equatorial Pacific.

204 unities inside nodules from the northeastern equatorial Pacific.

205 d due to a lack of evidence from the eastern equatorial Pacific.

206 rth Pacific Subtropical Gyre and iron in the equatorial Pacific.

207 ost persistent conditions occurring over the equatorial Pacific.

208 al' for tropical corals, such as the eastern Equatorial Pacific.

209 , were preceded by La Nina conditions in the equatorial Pacific.

210 sponse to the intensified trade winds in the equatorial Pacific.

211 but several taxa have independently lost the equatorial pattern and have microsporogenesis decoupled

212 The species that have lost the equatorial pattern have highly variable microsporogenesi

213 If selection on the equatorial pattern limits variation, we expect to see in

214 rogenesis remains stable in species with the equatorial pattern.

215 nt and the electron-withdrawing group in the equatorial phenyl ring and/or an electron-donating group

216 identity of the coordinating ions within the equatorial plane and/or solution pH; therefore, spectral

217 f chromosomes to complete congression to the equatorial plane for proper mitotic separation.

218 itions and the pi-acidic ligand occupies the equatorial plane in an overall octahedral geometry about

219 splacement of two hydroxo/aquo groups at the equatorial plane of a single Fe octahedron.

220 stablished, the chromosomes are moved to the equatorial plane of the spindle and ultimately toward th

221 ting vesicles to a disk-shaped region at the equatorial plane precedes a primary rapid expansion phas

222 three nitrogens and a chloride in the psuedo-equatorial plane with the remaining pyridine nitrogen an

223 ghosts were oriented by a dense band in its equatorial plane, parallel to the centrifugal field.

224 while denser material drifted out along the equatorial plane, propelled by orbital motion.

225 he metastable, pseudoaxial position into the equatorial plane.

226 th highest levels of force on the apical and equatorial planes of the nucleus.

227 ered by activation of the GTPase RhoA at the equatorial plasma membrane.

228 Equatorial populations also face a potential dual burden

229 The final equatorial position of the Cu(II) is occupied by a water

230 This indicates that the equatorial position of the metaphase plate is essential

231 uatorial NMe group and differing by axial or equatorial position of the SiMe group.

232 , TPW), which is responsible for the present equatorial position of the volcanic province.

233 alkyl groups bound to the cyclohexyl ring in equatorial position, and other quite stable stereoisomer

234 Nonpolar and large 2-substituents prefer the equatorial position, and relatively large shift differen

235 e phenyl ring has a strong preference for an equatorial position.

236 ormation locating the phenyl substituents in equatorial position.

237 coordinated by four phosphorus atoms in the equatorial positions and two hydrogen atoms in the axial

238 The mobility of equatorial proteins was greatly reduced at the furrow co

239 cted by positive spin density, while the two equatorial protons experience negative spin density.

240 glycosides, suggesting that the synthesis of equatorial pseudaminic acid glycosides will be possible

241 organization due to the rigidity of the "all equatorial" pyranyl sugar backbone, alpha-L-HNA represen

242 ans-disposed tert-butoxide ligands with weak equatorial pyridine donors, approaching proposed schemes

243 speakers first moved southward, through the equatorial rainforest, before spreading toward eastern a

244 hese populations located west-to-east of the equatorial rainforest.

245 Case studies from populations at the equatorial range edge of a variety of woody species have

246 r predicted widespread growth decline at its equatorial range edge.

247 nd examined the availability of refugia near equatorial range limits.

248 mblies differed in shape and position of the equatorial reflections, suggesting that the two peptides

249 the starspots are located, especially in the equatorial region and if the data quality is not optimal

250 orescent puncta of GFP-Kif15 move toward the equatorial region at a rate equivalent to microtubule gr

251 The equatorial region experiences strong seasonal insolation

252 One of its youngest terrains is the near-equatorial region informally named Sputnik Planum, which

253 a J-shaped motif with the carboxylate at the equatorial region of the dimeric capsule, and the revers

254 latitude section of the mid-Pacific and near-equatorial region of the east Pacific were identified as

255 rin receptor signaling complexes in the lens equatorial region, where lens epithelial cells initiate

256 In the eastern equatorial regions and the western boundary current exte

257 mic animals will increase from more polar to equatorial regions due to changing selective pressures i

258 uth bulges." Large numbers of adolescents in equatorial regions may account for observed relationship

259 ed deposits of sulfate-rich sediments in the equatorial regions of Mars have been suggested to be evi

260 ascending to top-tier predator guilds in the equatorial regions of Pangea prior to the dominance of d

261 onsible for the decreased incidence of MS in equatorial regions.

262 easing linearly ( 8 degrees C) from polar to equatorial regions.

263 ard the equator, maintaining the Sun's rapid equatorial rotation.

264 al circulation models suggest that a rise in equatorial sea surface temperature and related displacem

265 ion between Izumo1, a protein exposed on the equatorial segment of acrosome-reacted sperm, and the eg

266 ism in which the sperm protein IZUMO1 on the equatorial segment of the acrosome-reacted sperm recogni

267 des in excellent yield and good to excellent equatorial selectivity.

268 h hydride ions positioned exclusively at the equatorial site.

269 of the total variance of MCSs' lifetime over equatorial South America compared with 8% over equatoria

270 this study, we explored the role of the off-equatorial SST anomalies in the 2014 prediction.

271 We found significantly more variability in equatorial SSTs than previously reported, with pronounce

272 iling eastward and westward wind jets in the equatorial stratosphere (approximately 16 to 50 kilomete

273 tricted to the 30 degrees N and 30 degrees S equatorial strip.

274 First, the effect on guest binding of equatorial substitution on Q[6]'s was examined by compar

275 time involved in ocean transport, El Nino's equatorial subsurface 'heat reservoir', built up in bore

276 ion of cooler Pacific warm-pool SSTs and low equatorial temperature gradients in the past.

277 Seaway, a marine passage that connected the equatorial Tethys Ocean to the Boreal Sea.

278 Because the strongly donating equatorial tetracarbene pushes the Fe-dx(2)-y(2) orbital

279 y and systemic toxicity, was greater for the equatorial than for the axial pyranosides, and greater f

280 A deep equatorial thermocline altered the dynamics in the easte

281 otrophic prokaryotes and eukaryotes from the equatorial to temperate South Atlantic using an original

282 e-trans conformation (respectively, axial or equatorial to the bicyclic system).

283 atorial Pacific, upwelling of water from the Equatorial Undercurrent supplies far more dissolved iron

284 ade winds brings nutrient-rich waters of the Equatorial Undercurrent to the surface.

285 efs with higher nutrient availability (e.g., equatorial upwelling zones) were enriched in genes invol

286 istributions: NH volcanoes, SH volcanoes and equatorial volcanoes.

287 cific SST anomalies is nonlinear in terms of equatorial warming, because the enhanced meridional pres

288 r to the Cape Verde region, further south to equatorial waters in the central Atlantic, or to the Bra

289 Just to the south we distinguish an equatorial wave, bringing up ammonia gas from Jupiter's

290 This may result from stronger equatorial westerly ducts and subtropical jets during La

291 Upper tropospheric equatorial westerly ducts over the Pacific Ocean are the

292 d to a long-term trend in upper tropospheric equatorial westerly wind and subtropical jets during bor

293 the resulting atmospheric Kelvin wave drives equatorial westerly wind anomalies over the western Paci

294 imescale upper ocean heat content in the off-equatorial western tropical Pacific can provide conditio

295 ratios of the integrated intensities of the equatorial X-ray reflections (I(1,1)/I(1,0)) indicate th

296 acific warm pool temperatures and negligible equatorial zonal temperature gradients.

297 ch that the contractile ring assembles in an equatorial zone between the two spindle poles.

298 ring assembly by activating RhoA in a narrow equatorial zone.

299 ness that affects 22% people from tropic and equatorial zones.

300 ve a greater impact on shape change than the equatorial zonule and that choice of capsular thickness