ライフサイエンスコーパス: sheet

1 t the pace of mass loss of the Antarctic Ice Sheet.

2 etoplasts appear as a wrinkled hemispherical sheet.

3 42, which arranges into an antiparallel beta-sheet.

4 that may be used to reconfigure the origami sheet.

5 ated beneath the adjacent East Antarctic Ice Sheet.

6 a thickening and stratification of the cell sheet.

7 e motion at the margins of the Greenland Ice Sheet.

8 eriodic mechanical entanglements within each sheet.

9 ctrocatalytically active centers of the same sheet.

10 uence oceanic heat flux to the Greenland ice sheet.

11 on between adjacent molecules along the beta-sheet.

12 d species and suggested the presence of beta-sheets.

13 ic tendency of all polypeptides to form beta-sheets.

14 to complex filament aggregates and fibrillar sheets.

15 ar cardiomyocytes (NRVCMs) cultured on these sheets.

16 ture transformation from alpha-helix to beta-sheets.

17 y is established between adjacent epithelial sheets.

18 omer composed of 12 alpha-helices and 9 beta-sheets.

19 of cultivated human corneal epithelial cell sheets.

20 ring collective cell migration of epithelial sheets.

21 ssion necessarily persist in stratified cell sheets.

22 different financial risk in company balance sheets.

23 ted the fibrillation of HN and BAX into beta-sheets.

24 endemic clades south of the continental ice sheets.

25 , whereas BAX was converted entirely to beta-sheets.

26 meter-thick meandering and branching/merging sheets.

27 ted assemblies with polymer bilayers between sheets.

28 hobic interactions holding together the beta-sheets.

29 ing MSC chondrogenic differentiation as cell sheets.

30 progressive decay of Northern Hemisphere ice-sheets.

31 e a contribution from the East Antarctic Ice Sheet(3), which has been argued to have remained stable

32 terminal segment of the RCL into serpin beta-sheet A as a new strand.

33 likely by insertion of the peptide into beta-sheet A.

34 of ice shelves that buttress(11-13) the ice sheet accelerates ice flow and sea-level rise(14-16).

35 ermore, chondrogenically differentiated cell sheets adhere directly to cartilage surfaces via retenti

36 evealed that glycosylation stabilized a beta-sheet adjacent to the N130 GlcNAc and the N-terminal alp

37 on Pathway (RCP) scenarios and Antarctic Ice Sheet (AIS) melt propagate into uncertainties in project

38 of marine-based sectors of the Antarctic Ice Sheet (AIS)(1-3).

39 nland Ice Sheet (GrIS) and the Antarctic Ice Sheet (AIS).

40 Thus, this new magnesium sheet alloy is highly attractive for sheet applications

41 This new sheet alloy offers an excellent RT formability with a hi

42 Here we design a new magnesium sheet alloy-ZAXME11100 (Mg-1.0Zn-1.0Al-0.5Ca-0.4Mn-0.2Ce

43 rable to that of common 6xxx series aluminum sheet alloys.

44 perovskites, in which inorganic lead halide sheets alternate with naphthalene-based organic layers,

45 Two-layer beta-sheet amyloid structures predominate, but off-pathway be

46 ced by plasma, particularly contents of beta-sheet and beta-turn.

47 Advances in light-sheet and confocal microscopy now allow imaging of clear

48 onators with nanoscale footprint can support sheet and edge surface modes excited at the free space w

49 ecules reduces the voids within the graphene sheet and improves the alignment of graphene platelets,

50 bal soil erosion estimates (only considering sheet and rill erosion by water) with spatially distribu

51 Ric-8A binds to the exposed Galpha beta sheet and switch II to stabilize the nucleotide-free sta

52 eek to quantify interactions between the ice sheet and the ocean.

53 imum, leading to growth of the Antarctic ice sheet and the onset of Northern Hemisphere glaciation.

54 Flow models of the ice sheet and till-bedded glaciers elsewhere require a law t

55 and SAXS/WAXS measurements, reveals that the sheet and tube assemblies possess a similar underlying l

56 d comprising a four strand antiparallel beta-sheet and two helical turns stabilized by a complex disu

57 We employ long-term, rapid light-sheet and two-photon imaging of early zebrafish retinoge

58 secondary structures were measured in dough, sheeted and cooked pasta.

59 ence by two orders of magnitude in ultrathin sheets and an unexpected thickness-dependent modulation

60 nd sheet size (model complexity) in learning sheets and compare them to counterparts in machine-learn

61 fines the structure and composition of these sheets and facilitates their precise characterization by

62 Quantifying changes in Earth's ice sheets and identifying the climate drivers are central t

63 ts in the mechanical equilibrium of confined sheets and in thermodynamic phases of superconductors an

64 e radiative forcing of greenhouse gases, ice sheets and mineral dust aerosols, this cooling translate

65 Leaves vary from planar sheets and needle-like structures to elaborate cup-shape

66 imp proteins, including the increase in beta-sheets, and the loss in turns.

67 gnesium sheet alloy is highly attractive for sheet applications in automotive and other industries.

68 perties and electrical conductivities of rGO sheets are limiting factors for the development of such

69 To achieve this goal, 3D MSC sheets are prepared, exploiting spontaneous post-detachm

70 the edge strands in one beta-sheet (the DAGH sheet) are particularly susceptible to conformational ch

71 hat fail to stabilize an intermolecular beta-sheet around a highly divergent beta-strand of the BTB d

72 animal embryos pull and close an epithelial sheet around the ellipsoidal egg surface during a gastru

73 rowth lead to the formation of an epithelial sheet around the yolk.

74 n its underside, the shape change of polymer sheet, as well as cell morphology, calcium (Ca(2+)) infl

75 s enable observation of successive stages of sheet assembly.

76 caspase-1 active site, an anti-parallel beta sheet at the caspase-1 L2 and L2' loops bound a hydropho

77 iate into long straight loose bundles and/or sheets at both pH 6.5 and pH 7.5, which had little effec

78 Sheet/barrel and mixed-alpha/beta proteins exhibit more

79 Furthermore, C(H)2 helical segments, beta-sheets, beta-turns, and random coil regions were less st

80 the stabilization of a remarkably short beta-sheet by incorporating N-(hydroxy)glycine (Hyg) residues

81 accelerate the retreat of the Antarctic Ice Sheet by increasing surface melting and facilitating 'hy

82 W) mica substrates and converted to 2D Janus sheets by surface plasma technique, and then integrated

83 Covalent long-range ordered (crystalline) sheets called 2D polymers have recently been synthesized

84 8 membrane was prepared on a commercial flat-sheet ceramic substrate.

85 dhesion molecules while maintaining the cell sheets' characteristics.

86 Results support 3D MSC sheets' chondrogenic differentiation to hyaline cartilag

87 he Eocene and the expansion of Antarctic ice sheets close to their modern size near the beginning of

88 ing ZPC and following ZPN subdomains by beta-sheet complementation.

89 nd that residues 11-42 and 69-102 adopt beta-sheet conformation in patient protein fibrils.

90 exploiting spontaneous post-detachment cell sheet contraction, and chondrogenically induced.

91 The two faces of the beta-sheet core are hydrophobic and surrounded by the membran

92 -terminus of Galpha is ejected from its beta sheet core, thereby dismantling the GDP binding site.

93 etramer, which comprises a six stranded beta-sheet core.

94 A 2D DNA sheet could be modularized into connected parts (e.g., t

95 We contend that ice sheets create highly geochemically reactive particulates

96 An accelerating Airy-beam light-sheet critically enabled imaging areas that were greater

97 in current understanding of algal-driven ice sheet darkening through quantification of the photophysi

98 tophagy receptor responsible for targeted ER sheet degradation.

99 es, the formation and function of epithelial sheets depends on classical cadherin-containing adherens

100 eta-strand is organized into a parallel beta-sheet despite the co-existence of an antiparallel beta-s

101 mphipathic hydrogen-bonded antiparallel beta-sheet dimer that binds chloride anions.

102 ation synchronous with rapid Cordilleran Ice Sheet discharge, indicating close coupling of ice-ocean

103 In particular, the West Antarctic Ice Sheet does not regrow to its modern extent until tempera

104 nificantly reduced surface area in the front sheet due to the non-canonical conformation of the CC' l

105 mperature, sea level and extent of polar ice sheets during Earth's past interglacial warm periods(1-3

106 ss loss from the Greenland and Antarctic ice sheets during the LIG, causing global mean sea level to

107 al that forms as stacks and clusters of thin sheets-each sheet up to hundreds of micrometres long and

108 f Earth's cryosphere, the East Antarctic Ice Sheet (EAIS), to global warming is poorly understood.

109 ydrophilic residues located on the core beta-sheets edges of the oligomers.

110 nce on the mass balance of the Antarctic Ice Sheet, either indirectly, by its influence on air temper

111 Finally, the isolated sheets exhibit magnetic behaviours distinct from those o

112 Here we show that the Antarctic Ice Sheet exhibits a multitude of temperature thresholds bey

113 ass loss from glaciers and the Greenland Ice Sheet explains the high rates of global sea-level rise d

114 voidal geometry dictates that the epithelial sheet first expands and subsequently compacts.

115 combines an open-top, single-objective light sheet fluorescence microscope with an atomic force micro

116 Moreover, live light-sheet fluorescence microscopy and cultured PDGFRalpha+ c

117 plemented in multi-photon (two-photon) light-sheet fluorescence microscopy and, furthermore, can be a

118 res, immunostaining, H&E staining, and light-sheet fluorescence microscopy.

119 hin floral organs of Arabidopsis using light sheet fluorescence microscopy.

120 based fluorescent staining followed by light sheet fluorescent microscopy.

121 sive stability analysis of the Antarctic Ice Sheet for different amounts of global warming.

122 RPN1 and RPL26 and preferentially targets ER sheets for degradation, analogous to PINK1-Parkin regula

123 um in the Northern Hemisphere, expanding ice sheets forced a large number of plants, including trees,

124 n-T and Congo red binding and increased beta-sheet formation upon heat induction.

125 The Greenland Ice Sheet (GIS) has been losing mass at an accelerating rate

126 The Greenland Ice Sheet (GIS) is losing mass at a high rate(1).

127 in subglacial waters from the Greenland Ice Sheet (GrIS) and the Antarctic Ice Sheet (AIS).

128 wer the bare ice albedo of the Greenland Ice Sheet (GrIS), amplifying summer energy absorption at the

129 ring the rise and fall of the retreating ice sheet grounding line during successive tidal cycles.

130 ally, we document the transition to full ice-sheet growth over Scandinavia from the ice sheet's earli

131 ing cultivated human corneal epithelial cell sheets has been used successfully to treat limbal stem c

132 planar fragment containing a heterometallic sheet have remained elusive.

133 erforation and heteroatom doping of graphene sheets have been developed, patterning closely spaced ho

134 ture of a 2D-COF consists of two dimensional sheets held together through covalent bonds which are th

135 nism at different scales, we developed light-sheet illumination for fluorescence microscopy of small

136 g and broadband or monochromatic laser light-sheet illumination.

137 We used light-sheet imaging and automated cell segmentation and tracki

138 image analysis to identify the optimal light sheet imaging orientations.

139 open up enhanced depth penetration in light-sheet imaging to a wide range of end users.

140 st tumor induction model with inverted light-sheet imaging to study single-cell behavior for up to fo

141 ue advantages of combining Line Bessel light sheet imaging with AFM, we measured the forces exerted b

142 the gel for immunoprobing and confocal/light-sheet imaging.

143 ck of activity by showing loss of a key beta-sheet in a sequence known as the handle region that is c

144 ite the co-existence of an antiparallel beta-sheet in the same structure.

145 e, multi-walled carbon nanotubes and layered sheets in the coating.

146 argely driven by the growth and decay of ice sheets in the Northern Hemisphere.

147 BSA lost the alpha-helix and gain beta-sheets in the secondary structure during adsorption on h

148 ter crescentus SLP readily crystallizes into sheets in vitro via a calcium-triggered multistep assemb

149 y features typically associated with elastic sheets, including the development of radial wrinkles.

150 (hBN)(7,8) used to encapsulate the graphene sheets indicates the importance of the microscopic diele

151 These 3D cell sheets' initial thickness and cellular densities may als

152 erm partial collapse owing to the marine ice-sheet instability.

153 partially compensated by mass gains over ice sheet interiors (increased snow accumulation).

154 ientation and aperture measurements from 519 sheet intrusions within Volcan Taburiente (La Palma, Can

155 The more stable East Antarctic Ice Sheet is larger and older, rests on higher topography, a

156 The Antarctic Ice Sheet is losing mass at an accelerating pace, and ice lo

157 The less stable West Antarctic Ice Sheet is smaller and younger and was formed on what was

158 The Greenland Ice Sheet is the largest land ice contributor to sea level r

159 cascaded subwavelength anisotropic impedance sheets is demonstrated.

160 The stacking arrangement of the 2D sheets is dictated by van der Waals interactions and is

161 ion and export in subglacial runoff from ice sheets is poorly constrained at present.

162 vel change as a result of mass loss from ice sheets is strongly nonuniform, owing to gravitational, d

163 ing were periodically weaved on the graphene sheet, leading to four different types of zones with dis

164 nd beta-sheet was observed, with higher beta-sheet levels in both pulses dried using CHD.

165 align well across parallel and antiparallel sheets, like rungs on a ladder.

166 yielded peptides 3a-c that preferred a beta-sheet-like conformation.

167 of ER tubules will lead to the formation of sheet-like ER, the action of atlastin GTPases must be ti

168 e warmest Pleistocene interglacials, the ice sheet margin at the Wilkes Basin retreated to near the p

169 in packing interactions within the same beta-sheet may play a critical role in the formation of polym

170 by tracing isochronous layers within the ice sheet measured from ice-penetrating radar between the tw

171 impossible to perform in a traditional light-sheet microscope geometry, including cell migration thro

172 on, including dual-view cleared-tissue light-sheet microscopes and reflective lattice light-sheet mic

173 eet microscopes and reflective lattice light-sheet microscopes.

174 plant organs imaged with confocal and light sheet microscopes.

175 , using high spatiotemporal resolution light-sheet microscopy (~1.4 volumes/second, 330 nm isotropic

176 ds were first combined with modernized light-sheet microscopy a decade ago, the performance of both t

177 the art of tissue-clearing methods and light-sheet microscopy and discuss applications of these techn

178 Light-sheet microscopy enables considerable speed and phototox

179 The revolution in light sheet microscopy enables the concurrent observation of t

180 We used tissue clearing and light-sheet microscopy for 3-dimensional (3D) profiling of the

181 Light-sheet microscopy revealed the temporal evolution of the

182 as detected by electron, confocal, and light sheet microscopy techniques.

183 We developed dual-view light-sheet microscopy to investigate the dynamics of biofilm

184 and immunolabeling in combination with light-sheet microscopy were applied to image carotid arteries

185 he square illumination mode of lattice light-sheet microscopy, but in a user friendly and versatile f

186 erabyte-sized multichannel images from light sheet microscopy, enabling the construction, analysis, a

187 using Adipo-Clear in combination with light-sheet microscopy.

188 M super-resolution imaging and lattice light-sheet microscopy.

189 intact cleared mouse brains imaged by light-sheet microscopy.

190 lar resolution by non-invasive NIR-IIb light sheet microscopy.

191 alaeodata(2) we find, using the Parallel Ice Sheet Model(3-5), that at global warming levels around 2

192 our experiments, we store a file containing sheet music of Mozart, and show perfect data recovery fr

193 A nanocrystalline diamond sheet (NDS) attached over the ZnO is described.

194 copyright holder of the image (the herbarium sheet of Arabidopsis thaliana) is the first author, Dere

195 Further, it is shown that the same sheet of AuNR/LCE film (100 um thick) can be morphed int

196 The incorporation of nanoscale pores into a sheet of graphene allows it to switch from an impermeabl

197 The L1 loop and beta2 sheet of HDA15HD are the essential interfaces for the te

198 d FRAP to create SPIM-FRAP, wherein we use a sheet of light to bleach a two-dimensional (2D) plane an

199 sensors themselves, in some cases leaving a sheet of Teflon as thin as 10 mum between the sample and

200 yl)-ethynyl)-benzene pillars that connect 2D sheets of 9,10-dicarboxytriptycene struts and Zn(2)(CO(2

201 r graphene (TBBG), consisting of two rotated sheets of Bernal-stacked bilayer graphene.

202 beta-Barrels are sheets of beta-strands wrapped into a cylinder, in which

203 re commonly composed of discrete cell layers-sheets of cells that are one-cell thick.

204 utilized novel electrospun fibrin microfiber sheets of different stiffnesses (50.0 +/- 11.2 kPa and 9

205 s required to maintain adhesion in confluent sheets of epithelial cells is not known.

206 nal system emerges upon stacking two twisted sheets of GeSe, in marked contrast to all moire systems

207 l discontinuities preserved in higher thrust sheets of the Himalaya, and in ancient orogens elsewhere

208 C terminus and interactions between the beta-sheets of the Ig domains.

209 t in secondary structure distribution, while sheeting only had a minor effect.

210 amide side groups out of plane with the COF sheets orienting the hydrogen bonds between the layers.

211 ls with distinct morphologies including thin sheets, orthorhombic tablets, acicular needles, and rose

212 minus of the largest Alaskan Cordilleran Ice Sheet outlet glacier during Last Glacial Maximum climate

213 the planet, from the hot ring current/plasma sheet outside.

214 localized surface plasmons (LSPs) on the NPG sheet, partially hybridized with graphene phonons and su

215 crystallographic structure of a cyclic beta-sheet peptide derived from the 19-36 region of medin tha

216 layer (denoted as RZx) on pyrolytic graphite sheets (PGS), which was then utilized as the sensing lay

217 on) is necessary and sufficient to seed beta-sheet polymerization, and BiP binding to this Aggron pre

218 as the presence of extensive continental ice sheets predicts a tidally energetic Snowball ocean due t

219 acids, alteration in the alpha-helical/beta-sheet protein ratio, structural changes in carbohydrates

220 thin the hydration shell than a similar beta-sheet protein, which may contribute to the high packing

221 ere have implications for the design of beta sheet proteins with tunable self-assembling properties a

222 ur super-tough MXene-functionalized graphene sheets provides a combination of energy and power densit

223 A higher proportion of beta sheets, random coils, alpha-helix and beta-turns for all

224 Each metal(II) halide sheet represents a fragment excised from a single layer

225 rom the instability of polar continental ice sheets represents a major socioeconomic hazard arising f

226 e intervening Bose metal state occurs if the sheet resistance of the film in the maximum, R(max) prio

227 The sheet resistance of the ink is approximately 600 Omega/s

228 These membranes are shown to have comparable sheet resistance to carbon-nanotube-composite membranes.

229 d requires the measurement of work function, sheet resistance, carrier concentration and mobility in

230 ed silver film with low optical loss and low sheet resistance.

231 uration of the temperature dependence of the sheet resistance.

232 derwater vehicle, enables calculation of ice sheet retreat rates from a complex of grounding-zone wed

233 increasing formation of intermolecular beta-sheets, revealed by second derivative spectra.

234 in solution to form ordered, insoluble, beta-sheet-rich amyloid fibrils.

235 ordered tau protein into highly ordered beta-sheet-rich fibrils is implicated in the pathogenesis of

236 tein (PrP), leading to the formation of beta-sheet-rich, insoluble, and protease-resistant self-repli

237 e-sheet growth over Scandinavia from the ice sheet's earliest position to the later pattern of debris

238 ntinental shelf, plays a key role in the ice sheet's mass balance.

239 l waters of East Antarctica recorded the ice sheet's response to MIS11 warming.

240 The ice sheet's temperature sensitivity is 1.3 metres of sea-lev

241 agate into fibrils that have a parallel-beta-sheet secondary structure.

242 evealed the adoption of a predominantly beta-sheet secondary structure.

243 Atomically thin graphene sheets serve as folding hinges during a process of 2D to

244 Furthermore, the Ir-decorated WO(3) sheets show excellent durability and H(2) S selectivity

245 on dynamics for both an alpha-helix and beta-sheet site of GB1, the immunoglobulin binding domain of

246 ship between training error, test error, and sheet size (model complexity) in learning sheets and com

247 tracted from selected articles into an excel sheet specifically designed for this review.

248 elix and one three-residue antiparallel beta-sheet stabilized by two disulfide bonds.

249 tal ions connected into two-dimensional (2D) sheets stacked on top of each other.

250 ide-based MOFs that allow fine tuning of the sheet stacking.

251 st of its time trapped in misregistered beta-sheet states connected by weakly bound states twith shor

252 This protein was designed to lack beta-sheet structure and is competitively inhibited by magnes

253 cross-seeded lRPT fibrils had a similar beta-sheet structured core, revealed by Raman spectroscopy, l

254 de-peptoid hybrids form unique parallel beta-sheet structures by self-assembly upon hydrogenation.

255 there is an accumulation of random and beta-sheet structures that is mediated by small connecting se

256 t of experiments and simulations of floating sheets subjected to radial stretching.

257 GQDs self-assemble into mesoscale chains, sheets, supraparticles, nanoshells, and nanostars.

258 e show how a preTCR applies the concave beta-sheet surface of its single variable domain (Vbeta) to "

259 e) (PNIPAm) is widely used to fabricate cell sheet surfaces for cell culturing, however copolymer and

260 e investigate thiol-ene micropillar scaffold sheets ("synthetic paper") as the solid substrate in suc

261 This review aims to introduce cell sheet technology as a breakthrough cell therapy with dem

262 ther, these data support the utility of cell sheet technology for fabricating scaffold-free, hyaline-

263 technology to pattern single cells into ECM sheets that are >10x larger than previously described.

264 ork for supervised learning in thin, creased sheets that learn the desired force-response behavior by

265 inked COFs rapidly polymerize as crystalline sheets that subsequently reorganize to form stacked stru

266 sters and, occasionally, isolated individual sheets that, following demetallation, have slid apart fr

267 ations and that the edge strands in one beta-sheet (the DAGH sheet) are particularly susceptible to c

268 In contrast, beta-sheets, the main secondary structure in cooked pasta, ne

269 e, cobalt(II) chloride and iron(II) chloride sheets through the peripheral coordination of six chelat

270 ed, resettable structural conversion of a 2D sheet to a 3D architecture, due to the constraints induc

271 We employ a programmable polymer actuator sheet to autonomously synchronize thermal and mechanical

272 n in silico model of the developing cortical sheet to explore which factors could potentially constra

273 sary for oligomers with an antiparallel beta-sheet to propagate into fibrils that have a parallel-bet

274 f the contribution of the West Antarctic Ice Sheet to sea level rise.

275 Mass loss from the Antarctic Ice Sheet to the ocean has increased in recent decades, larg

276 ping from the linear folding motions of such sheets to force-bearing modes in conjunction with the Ma

277 s as stacks and clusters of thin sheets-each sheet up to hundreds of micrometres long and wide but on

278 During training, we fold the sheet using training forces, prompting local crease stif

279 origin of the switching mechanism in atomic sheets using monolayer MoS(2) as a model system.

280 of cultivated human corneal epithelial cell sheets using time-lapse imaging of the cell culture proc

281 ncluding collapses of the West Antarctic Ice Sheet (WAIS).

282 A MrGO sheet was crosslinked by a conjugated molecule (1-aminop

283 nd the presence of both alpha-helix and beta-sheet was observed, with higher beta-sheet levels in bot

284 e throughout at those points where the metal sheeting was absent and where the vegetation had overgro

285 nger peptide sequences that form stable beta-sheets was found to suppress superstructure formation.

286 brief interruptions, while the Antarctic ice sheet waxed and waned.

287 Extensive areas of polar ice sheets were grounded below sea level during both glacial

288 nanoparticles anchored onto the 2-D graphene sheets were synthesized using a two-step laser liquid so

289 brils (intermolecularly hydrogen-bonded beta-sheets) when the pH is lowered below 4.

290 234)U cycling observed in the Laurentide Ice Sheet, where (234)U accumulated during periods of ice st

291 ithelial monolayers are two-dimensional cell sheets which compartmentalize the body and organs of mul

292 ater resources are held by the Antarctic Ice Sheet, which thus represents by far the largest potentia

293 he supramolecular network into undulating 2D sheets, which then stack into a 3D network via a series

294 ectively inhibits the agglomeration of WO(3) sheets while maintaining well-dispersed ex-solved partic

295 s flipping to the other side of the graphene sheet with a relatively low activation energy of about 1

296 zero-energy deformations of periodic origami sheets with generic crease patterns.

297 ctica remains in the grip of continental ice sheets, with only about 0.2% of its overall area being i

298 r interaction acting between the paired beta-sheets within Tau fibrils.

299 an even mixture and distribution of the rGO sheets within the PCL matrix.

300 the mineral surface and an increase in beta sheets within the protein structure.