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1 otein complexes that form with gRNA in vitro sediment at 10 to 20S, except for one, which sediments a
2                    At high ionic strength it sediments at 10 S independent of Ca(2+), and its regulat
3 n form a catalytically inactive monomer that sediments at 10 Svedbergs (10 S).
4                                        Luv1p sediments at 100,000 x g and can be solubilized by salt
5 dimentation analysis demonstrated that trpL1 sedimented at 11S, while L1 proteins with amino-terminal
6  in a sucrose gradient, the altered particle sediments at 135S, has lost the coat protein VP4, and ha
7 ctious cell-entry intermediate particle that sediments at 135S.
8                      While the native virion sediments at 160S in a sucrose gradient, the altered par
9                Another molecular form, which sediments at 17 S, is also present in vivo.
10                       The purified material, sedimented at 20-25S, migrated in a blue native gel at 1
11 ATPase 6 (A6) guide RNA and unedited A6 mRNA sediments at 20 to 30S, with some sedimenting further in
12 ns are present in the immunoprecipitates and sediment at 20S along with the in vitro editing, and RNA
13                  In vivo, all cytosolic Arp1 sediments at 20S [7] suggesting that it assembles into o
14 ain the key enzymatic editing activities and sediment at ~20S on glycerol gradients.
15 yzed by analytical ultracentrifugation, they sedimented at 230S compared with 273S for untreated viri
16 the unoccupied calnexin behaved as a monomer sedimenting at 3.5 S20,W.
17 sediment at 10 to 20S, except for one, which sediments at 30 to 45S.
18 ndent RNA polymerase, and an unmapped factor sedimenting at 32 to 38 kDa.
19 arily at approximately 20S, a 90-kDa protein sediments at 35 to 40S, and a 25-kDa protein is present
20 a polypeptide were present in a complex that sedimented at 4.4 Svedberg units.
21 10 kDa on size exclusion chromatography, and sedimented at 4.5 S in glycerol gradients.
22 es was greatly reduced and the large subunit sedimented at 45S.
23 tured benthic Archaea recovered from estuary sediments at 48% to 95% completeness.
24 ino-terminal deletions of 29 and 61 residues sedimented at 4S.
25 e associated with calnexin in complexes that sedimented at 5-5.5 S20,W.
26 tin polymerised and actin filaments could be sedimented at 500,000g.
27 age in amphipods exposed to the contaminated sediment at 750 muatm pCO2 , as well as increased DNA da
28 ts in an increase in the amount of mRNA that sediments at 80 S and a decrease in the amount in polyso
29             In the most reduced intermediate sediments at 80-120 cm of the western floodplain, no Fe(
30 e suspended oil particles sank to underlying sediment (at a depth of approximately 1,300-1,700 m).
31 eanobacillus iheyensis, whose habitat is the sediment at a depth of 1050 m in the Pacific Ocean.
32 lding a high load of labile As sorbed to the sediment at a depth of 35.8 mbgl and concentrations of A
33  a virion component and that 22/n199 virions sediment at a reduced density relative to wild-type viri
34 ensity gradients revealed that the precursor sedimented at a density consistent with that of an HIV-1
35 analyses show that this complex is large and sediments at a different fraction from known MRP RNA-con
36 50S particles and to a 50S subunit precursor sedimenting at about 30S in sucrose gradients.
37     Furthermore, these editing activities co-sediment at approximately 20 S.
38  gradients made in low ionic strength, DHC1a sedimented at approximately 20S, and the anti-1b immunor
39 tive and required a membrane protein(s) that sedimented at approximately 4 S.
40  that the majority of the transport activity sedimented at approximately 4S, correlating with the pre
41 nd required a trypsin-sensitive protein that sedimented at approximately 4S.
42 t with dynein heavy chain, in a complex that sedimented at approximately 5S in a sucrose density grad
43                         The active factor(s) sedimented at approximately 7S on sucrose gradient centr
44 c loss of eIF4G and eIF2alpha from complexes sedimenting at approximately 40 S.
45 le to form distinct complexes, each of which sediments at approximately 20 S.
46 centrifugation shows that at neutral pH VacA sediments at approximately 22 S, whereas at acidic pH it
47 2 S, whereas at acidic pH it dissociates and sediments at approximately 5 S.
48 ith multiple collectors effectively utilized sediment at both horizontal and vertical directions and
49 ed morphologic features of beta-retroviruses sedimenting at buoyant densities of 1.12 to 1.18 g/mL in
50 ated with potential CO2 leakage into shallow sediments at carbon sequestration sites.
51 for Tc(IV) to be oxidized and mobilized from sediments at coastal nuclear sites resulting from predic
52 (Fq'/Fm') was significantly reduced in oiled sediments at day 7, implying that the initial diatom-dom
53 superior for cases where large molecules are sedimented at faster rotor speeds, during which sediment
54 of an over-the-counter medication in aquatic sediments at five different locations.
55 higher-order complexes containing Sec1p that sediment at greater than 20S.
56  eventually producing polymeric species that sediment at >> 10 000 S.
57 into the gradient, while most edited A6 mRNA sediments at >35S.
58 .9 Mb of genetic material was sequenced from sediments at horizons 1, 16, 32, and 50 m below the seaf
59 minin species discovered in Late Pleistocene sediments at Liang Bua (Flores, Indonesia), has generate
60 ing Ca2+-aggregated microsomes, which can be sedimented at low g forces.
61           The amount of cross-linked F-actin sedimenting at low centrifugal force also increased with
62 red by enriching sulfur reducers from acidic sediments at low pH (from 2 to 5) with hydrogen, glycero
63 ), which has not previously been verified in sediments at low temperature.
64 t remnants of ECNA sea water persist in deep sediments at many locations along the Atlantic margin.
65 natures for organic matter preserved in lake sediments at Olduvai Gorge during a key juncture in huma
66 (VI) adsorption to the quartz-sand dominated sediments at pH </= 4.0.
67  ultracentrifugation shows one main complex, sedimenting at s(20,)(w) = 7.2 +/- 0.1 S, together with
68 7 and 1.3) but accumulated preferentially in sediments at source-driven sites (BSAF = 0.2 and 0.4).
69 es present in the supernatant of this mutant sediment at the correct density for a retroviral particl
70 c rates similar to those in water, soil, and sediment at the same temperature.
71 rofiles of the concentration versus depth of sediment at the two sites showed various patterns among
72 d-type p51 (p66delta/p51WT and p66Ala/p51WT) sedimented at the dimeric position.
73 a3beta2alpha5 receptors expressed in oocytes sedimented at the same 11 S value as native alpha3-conta
74 tructing the former valley bottom and dating sediments at the base of the valley fill, we show that s
75            Microbial diversity in subsurface sediments at the Hanford Site 300 Area near Richland, Wa
76                Fullerenes (C60 to C200) from sediments at the PTB contain trapped helium and argon wi
77 microspectroscopy (mFTIR) analyses of intact sediments at the site of Wonderwerk Cave, Northern Cape
78 ts aberrant SH2 domain, the Dd-STATb protein sediments at the size expected for a homodimer and it is
79         The concentrations of PAH in surface sediments at the two locations were comparable and highe
80 ting advection of hydrothermal fluid through sediment at this site.
81 IV) accumulation in organic-enriched reduced sediments at three UCRB floodplains.
82          In sucrose density gradients, KIF3C sediments at two distinct densities, suggesting that it
83 ., but did not find a single spherule in YDB sediments at two previously reported sites.
84 corer to collect bottom seawater and surface sediments at vent sites.
85          They saltate like the wild type and sediment at wild-type rates upon gravistimulation.

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