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1 sor movement and current through the channel pore.
2 e once the capsid interacts with the nuclear pore.
3 he trypanosomal analogue of the Tom40 import pore.
4 an concur simultaneously in the hERG channel pore.
5 Pase rings (D1 and D2) surrounding a central pore.
6 in the setting of a narrow, cation-selective pore.
7 t, unlike the DNA, does not pass through the pore.
8 n that is then also translocated through the pore.
9 t with an impact on conformation of the KCNQ pore.
10 ate unfolding by threading through a central pore.
11 n, the influenza proton channel, and the MCU pore.
12 l saturation (ROS) and the fraction of micro-pores.
13 membranes without oligomerizing into visible pores.
14 s exclusively on the internal surface of the pores.
15 n clays include interlayer and interparticle pores.
16 TMEM16A forms a dimer with two pores.
17 hen concentrated as they are in pit membrane pores.
18 ese channels are composed of the ion-forming pore alpha1 and auxiliary subunits (beta and alpha2delta
19 cesses by conducting a time-resolved pore-by-pore analysis of the local curvature and capillary press
20 dopts a non-domain-swapped attachment to the pore and contacts the cytoplasmic Ca(2+)-binding domain
24 hiral sequences, assemble into antimicrobial pores and form contiguous helices that are biologically
25 he SILM, one in the IL phase in the membrane pores and the other in the supporting membrane polymer.
26 ytoplasm, docking of the capsid at a nuclear pore, and release of the viral genome into the nucleus.
27 ure-stable Ni-MOF-74 members with adjustable pore apertures, which exhibit excellent sorption capabil
29 with 3D printing, and indicate that scaffold pore architecture is a critical variable in additively m
31 lve translocation of peptides through capsid pores are associated with a subtle conformational change
33 ations of the IL (spectral diffusion) in the pores are slower than in the bulk IL by approximately 2-
35 th the Mlp1/2 role in gene gating to nuclear pores, artificial tethering to the nuclear periphery of
36 at when the proximity to the surface and the pore aspect ratio were included the actual initiating de
39 ntiviral drug, amantadine, at the N-terminal pore at low pH did not convert all histidines to the neu
44 sing on structures with methane-inaccessible pores blocked away from the main adsorption channels.
46 e influx was inhibited by MK-801, a specific pore blocker of N-Methyl-D-aspartic acid receptor (NMDAR
48 hese processes by conducting a time-resolved pore-by-pore analysis of the local curvature and capilla
49 thene-containing MOFs, the properties of the pore can be changed via an optical trigger without the p
50 urther demonstrate how the geometry of these pores can be altered beyond triangular by changing beam
52 ewise, the tomato CATION EXCHANGER 1 and TWO-PORE CHANNEL 1 (SlTPC1), key genes for Ca(2+) fluxes to
56 plasm to the periplasm via an inner-membrane pore complex (TraC and TraG) with homology to type IV se
57 t al. (2017) describe defects in the nuclear pore complex and impaired nucleocytoplasmic transport in
58 is expressed in cells of the developing air pore complex and the morphogenesis of the complex is def
59 Moreover, we provide evidence that a nuclear pore complex associates with the duplicating SPB and hel
61 e explore the hypothesis that the P2X7-PANX1 pore complex is a critical determinant of spreading depo
66 transcription complexes and show how nuclear pore composition changes can be exploited to regulate ge
68 ductivity for the case with aligned circular pores, confirming a significant thermal transport degrad
69 space, pore type, sample size and associated pore connectivity, as well as theoretical base and inter
70 ediate state to the activated state, the VSD-pore coupling has less efficacy in opening the pore, pro
71 ent mechanisms, other than the canonical VSD-pore coupling, are at work in voltage-dependent ion chan
72 he averages of the seven measurements from 8-pore devices are contrasted to single measurements from
74 age of the improved size resolution of the 8-pore devices to analyze in real time the assembly of Hep
76 hollow fibers not only possess a small mean pore diameter of 1.0-1.3 nm with a molecular weight cuto
77 to their difference in measurable ranges of pore diameter, pore space, pore type, sample size and as
79 rge value of inaccessible porosity occurs at pore diameters <10 nm, which we attribute to low connect
80 ances for porous copper inverse opals having pore diameters from 300 to 1000 nm by measuring the capi
81 capped PLGA displayed an osmotically induced/pore diffusion mechanism based on confocal micrographs o
82 vidence that, contrary to the time-dependent pore dilation model, ATP binding opens an NMDG(+)-permea
85 detergent and liposomes, for residues at the pore domain that agree with their location in the TRPV1
87 arly counterbalance hypokalaemia-induced two pore-domain K(+) channel isoform 1 (K2P1) leak cation cu
88 fies the interface between the catalytic and pore domains of CFTR and that this modification facilita
89 5 linker connects nearby voltage-sensing and pore domains to produce a non-domain-swapped transmembra
91 t the brine-oil interface jumps from pore-to-pore during imbibition at an approximately constant loca
93 show a strain-independent failure of fusion pore enlargement among H2 (A/Japan/305/57), H3 (A/Aichi/
97 ns which help lower the energetic barrier to pore expansion.IMPORTANCE Influenza A virus is an airbor
98 w (groundwater), with larger, well-connected pores filling before finer pore spaces, unlike groundwat
99 in a characteristically different pattern of pore-filling than wetting from below (groundwater), with
102 r, the molecular mechanisms for how stomatal pores form and how guard cell walls facilitate dynamic s
103 haviors and establish a link between peptide pore formation and both lipid-peptide charge and topolog
104 ts of ATP synthase that could participate in pore formation are e, f, g, diabetes-associated protein
105 of exogenous substrates upon inner membrane pore formation by alamethicin or Ca(2+)-induced PTP open
106 the founding member of this class, prevents pore formation by destabilizing the prepore into a poorl
107 tricts HIV-1 fusion at a step prior to small pore formation by selectively inactivating sensitive Env
113 nel is closed by a constriction of the inner pore formed by criss-crossing of the S6 segments at a co
114 vents of single-channel currents through the pore formed by recombinant ATOM40 were detected in elect
115 lts indicated that AG can be used as a novel pore-former, hydrophilizing and antifouling agent, as we
119 e-activated K(+)(BK) channel consists of the pore-forming alpha subunits (BKalpha) and auxiliary subu
120 Voltage-gated CaV2.1 channels comprise a pore-forming alpha1A subunit with auxiliary alpha2delta
121 ated potassium channels (BK) are composed of pore-forming BKalpha and auxiliary beta1 subunits in art
122 oL1 has been hypothesized to function like a pore-forming colicin and has been reported to have perme
124 osis requires cleavage and activation of the pore-forming effector protein gasdermin D by inflammator
125 rst evidence, to our knowledge, that StII, a pore-forming protein from a marine eukaryotic organism,
126 ed endosome-disrupting agent composed of the pore-forming protein Perfringolysin O (PFO), potent sile
128 anisms from all kingdoms of life, only a few pore-forming proteins have been successfully reconstitut
129 sins (CDCs) represent a family of homologous pore-forming proteins secreted by many Gram-positive bac
130 form a channel complex with the K(+) channel pore-forming subunit Kv4.3 in a subset of nociceptors to
137 is important for communications between the pore gate and the voltage sensor during deactivation.
138 occurs as a result of reconfiguration of the pore gate upon opening by a mechanism that is influenced
139 data also demonstrate that the mechanisms of pore gate-opening-induced and relaxation-induced voltage
141 yamide groups, open metal sites, appropriate pore geometry and cooperative binding between guest mole
142 orous hydrogel scaffolds to test how varying pore geometry, accomplished by manipulating the advancin
143 Several aromatic and hydrophobic residues in pore helix 1, helices S5 and S6, and helix S6 of a neigh
147 his depends on activation of the RyR1 Ca(2+) pore in the SR, under control of conformational changes
148 on of the diffusion barrier, an array of 100 pores in 0.2cm(2) area of nail permitting a 10(3)-fold i
152 audin-4) as receptors to form Ca2+-permeable pores in the membrane, damaging epithelial cells in smal
153 based on confocal micrographs of percolating pores in the polymer, not previously observed in vitro.
154 n diffuse easily through air- and gas-filled pores in the soil and likely play an important role in l
157 ed to monitor the shape and dimension of the pores in which water is confined, thus boosting the info
161 nts caused lipid bilayer destabilization and pore instability, limiting the total number of recorded
163 ete assembly intermediates and show that the pore is most probably a helix barrel that contains eight
167 conformation, the extracellular-half of the pore-lining M2 is splayed open, reminiscent of the open
168 adiol interaction with hERG mutations in the pore loop containing G604 or with common TdP-related blo
171 ermined by measuring their flux across large pore membranes and using dynamic light scattering, with
172 challenge the "drift and diffusion through a pore" model that dominates conventional explanatory sche
173 er size of only 82 amino acids, resemble the pore module of all complex K(+) channels in terms of str
176 in the vicinity of the gating region of the pore, namely between residues E90, E123, D253, N258, and
178 t thermal fluctuations enable rate-dependent pore nucleation, driving the dynamics of the swell-burst
179 We also observed that the duration of the pore obstruction event is more controlled by the knot tr
180 sing channel gating rather than blocking the pore of heterologously expressed human BK channels.
182 ught to unfold substrate through the central pore of their hexameric structures, but how this process
183 (GIP) is stored as an adsorbed phase in fine pores of coal matrix, the nano-pore structure directly i
184 es under transmission electron microscopy in pores of intervessel pit membranes and deposited on vess
185 the melting temperature of the polymer, the pores of the nanofibers collapse due to the nanofibers'
186 e attack complex (MAC), which forms a lethal pore on the cellular surface of pathogenic bacteria.
187 xchange that is controlled by stomata, small pores on plant leaves and stems formed by guard cells.
189 e-binding site of complex II (site IIf); (b) pore opening in the inner membrane resulting in rapid ef
190 oach of kiri-kirgami, and their actuation of pore opening via both mechanical stretching and temperat
191 cate that G100V/C103V retards initial fusion-pore opening, hinders its expansion and leads to prematu
193 ymorphic activated forms with very different pore openings, markedly different gas-adsorption capacit
194 ctions either by conducting ions through the pore or by phosphorylating downstream proteins via its k
197 s approach, we discovered that a pair of two-pore potassium channel (K2P) subunits, largely dispensab
198 ke CP structure that occlude substrate entry pores, preventing unregulated degradation of substrates
201 y target of the compounds as the T3SS needle pore protein EspD, which is essential for effector prote
203 centerline approximation leads to an optimum pore radius of about 8-12A, depending on the model chose
204 ese motions result in a minimum open-channel pore radius of approximately 3 A formed by Gln-4933, rat
205 The impacts by individual parameter such as pore radius, half cone angle, and surface charges are sy
207 ANLAAF motif orient toward the center of the pore region and most likely lead to disturbance of the g
209 pectedly, the extracellular mouth of the ion pore remains closed, indicating that local movements of
212 antecedent soil moisture conditions to alter pore-scale, core-scale, and field-scale C dynamics.
213 cific OprP and the diphosphate-specific OprO pores show structural differences in their binding sites
218 99.6%), light weight (5 mg/cm(3)) and narrow pore size distribution ( 2 to 5 nm), the ECF anode exhib
219 icroscopic characteristics of the substrate (pore size distribution, porosity, permeability, and depo
220 showed that this transition occurs when the pore size is <3x the maximum of molecular dimensions.
224 ferent electrolyte composition and effective pore size to elucidate their influence on separation mec
226 ith an event size of the order of an average pore size, again much smaller than the large bursts seen
229 ons during CO2 sequestration will change the pore-size distribution and pore surface characteristics,
230 el is presented that incorporates a range of pore sizes to more accurately predict the capillary tran
231 In conjunction with a tight control over pore sizes, inverse opal scaffolds have found widespread
236 tion, with larger aggregates containing less pore space than under control conditions, and water rete
237 rence in measurable ranges of pore diameter, pore space, pore type, sample size and associated pore c
241 rmeability sediments that are sequestered in pore spaces too small for cell passage can be reduced by
242 r, well-connected pores filling before finer pore spaces, unlike groundwater rise in which capillary
244 phase in fine pores of coal matrix, the nano-pore structure directly influences gas storage and trans
247 Based on our results, we postulate that the pore structure of many mineral soils could undergo N-dep
248 ach method probes a unique aspect of complex pore structure of shale, the discrepancy between pore st
249 structure of shale, the discrepancy between pore structure results from different methods is explain
250 ly affected the crystallinity, surface area, pore structure, and luminescence properties of the polym
253 cognition approach to quantify similarity of pore structures and classify them using topological data
254 nanocarbon-based materials with controllable pore structures and hydrophilic surface show great poten
256 ratory experiments on mixed micro- and macro-pore suggest that there is a systematic relationship bet
257 n will change the pore-size distribution and pore surface characteristics, complicating permeability
259 between discrete organic molecules or on the pore surfaces of MOFs, in a very fast (1-2 s) and contin
260 ted biochar that covers the outer and inner (pore) surfaces of biochar particles using high-resolutio
261 nel gating coupling junction and the channel pore (T288N), which are functionally coupled during rece
264 leased through fluctuating exocytotic fusion pores that can flicker open and shut multiple times.
270 olved within each monomer with a constricted pore; this is likely to correspond to a closed state, be
271 cting ACT segments, a proteolipidic toroidal pore through which AC domain transfer could directly tak
272 nts exit the bacterial cell through the ComE pore through which the NTHI type IV pilus is expressed.
273 ied by incorporating Ni(2+) cations into the pores through coordination to the amino groups, and the
274 imilarly, standard deviations of the pore-to-pore time distributions decrease by 3.2-fold when the av
275 show that the brine-oil interface jumps from pore-to-pore during imbibition at an approximately const
277 molecular dynamics simulations to study the pore translocation of 10-kbp-long DNA rings that are kno
278 surable ranges of pore diameter, pore space, pore type, sample size and associated pore connectivity,
279 ulate and retain AITC molecules within their pores under low (30-35%) relative humidity (RH) conditio
280 e-selectivity in terms of smooth cylindrical pores using the centerline approximation leads to an opt
281 ere, we probed the dilation of single fusion pores using v-SNARE-reconstituted 23-nm-diameter discoi
285 lev's equations afforded the evaluation of a pore volume variation from 10 to 110 cm(3)/g by cobalt i
286 ed, which showed higher surface area, larger pore volume, stronger acidity and higher surface area co
288 ates that low chloride concentrations in the pore water of the corresponding sediments can only be ex
292 d unexpectedly low DOC concentrations in the pore waters, reflecting the combined effect of thermal d
293 experiments on controlled migration through pores, we show that squeeze-out of the fluid, and hence
297 ct can increase protein concentration inside pores, which enables crystal nucleation even under condi
298 hannel constitutes the actual protein-import pore wide enough to allow the passage of polypeptides wi
299 O, -OH) polyhedra supporting one-dimensional pores with apertures and internal diameters of 7.8 and 9
300 ablish the metastable nature of the inserted pore, yielding a force profile with barriers for membran
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