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1 otein complexes that form with gRNA in vitro sediment at 10 to 20S, except for one, which sediments a
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
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
15 yzed by analytical ultracentrifugation, they sedimented at 230S compared with 273S for untreated viri
19 arily at approximately 20S, a 90-kDa protein sediments at 35 to 40S, and a 25-kDa protein is present
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
30 e suspended oil particles sank to underlying sediment (at a depth of approximately 1,300-1,700 m).
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
38 gradients made in low ionic strength, DHC1a sedimented at approximately 20S, and the anti-1b immunor
40 that the majority of the transport activity sedimented at approximately 4S, correlating with the pre
42 t with dynein heavy chain, in a complex that sedimented at approximately 5S in a sucrose density grad
46 centrifugation shows that at neutral pH VacA sediments at approximately 22 S, whereas at acidic pH it
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
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
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
62 red by enriching sulfur reducers from acidic sediments at low pH (from 2 to 5) with hydrogen, glycero
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
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
71 rofiles of the concentration versus depth of sediment at the two sites showed various patterns among
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
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
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