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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 than 1 Ga after deposition of the Jack Hills sediment at 3 Ga.
17 the unoccupied calnexin behaved as a monomer sedimenting at 3.5 S20,W.
18 sediment at 10 to 20S, except for one, which sediments at 30 to 45S.
19 ndent RNA polymerase, and an unmapped factor sedimenting at 32 to 38 kDa.
20 arily at approximately 20S, a 90-kDa protein sediments at 35 to 40S, and a 25-kDa protein is present
21 a polypeptide were present in a complex that sedimented at 4.4 Svedberg units.
22 10 kDa on size exclusion chromatography, and sedimented at 4.5 S in glycerol gradients.
23 es was greatly reduced and the large subunit sedimented at 45S.
24 tured benthic Archaea recovered from estuary sediments at 48% to 95% completeness.
25 ino-terminal deletions of 29 and 61 residues sedimented at 4S.
26 e associated with calnexin in complexes that sedimented at 5-5.5 S20,W.
27 tin polymerised and actin filaments could be sedimented at 500,000g.
28 age in amphipods exposed to the contaminated sediment at 750 muatm pCO2 , as well as increased DNA da
29 ts in an increase in the amount of mRNA that sediments at 80 S and a decrease in the amount in polyso
30             In the most reduced intermediate sediments at 80-120 cm of the western floodplain, no Fe(
31 e suspended oil particles sank to underlying sediment (at a depth of approximately 1,300-1,700 m).
32 eanobacillus iheyensis, whose habitat is the sediment at a depth of 1050 m in the Pacific Ocean.
33 lding a high load of labile As sorbed to the sediment at a depth of 35.8 mbgl and concentrations of A
34 lution widely used along muddy coasts, traps sediment at a rate of less than 1.3 cm/y and typically l
35  a virion component and that 22/n199 virions sediment at a reduced density relative to wild-type viri
36 me in the Virginia barrier islands) accreted sediment at a significantly lower rate compared to other
37 ensity gradients revealed that the precursor sedimented at a density consistent with that of an HIV-1
38 rimentally the response of silica particles, sedimented at a wall, to active Pt/silica Janus particle
39 analyses show that this complex is large and sediments at a different fraction from known MRP RNA-con
40                             410-419 Myr old) sediments at a geological site in Shropshire (UK).
41 tically accreting thick sequences of organic sediments at a rate principally driven by the rate of RS
42 mperature and hydroclimate history from lake sediments at a site adjacent to a former Norse farm.
43 50S particles and to a 50S subunit precursor sedimenting at about 30S in sucrose gradients.
44 admixed with macrophages and red blood cells sedimented at an angle.
45     Furthermore, these editing activities co-sediment at approximately 20 S.
46  gradients made in low ionic strength, DHC1a sedimented at approximately 20S, and the anti-1b immunor
47 tive and required a membrane protein(s) that sedimented at approximately 4 S.
48  that the majority of the transport activity sedimented at approximately 4S, correlating with the pre
49 nd required a trypsin-sensitive protein that sedimented at approximately 4S.
50 t with dynein heavy chain, in a complex that sedimented at approximately 5S in a sucrose density grad
51                         The active factor(s) sedimented at approximately 7S on sucrose gradient centr
52 c loss of eIF4G and eIF2alpha from complexes sedimenting at approximately 40 S.
53 le to form distinct complexes, each of which sediments at approximately 20 S.
54 centrifugation shows that at neutral pH VacA sediments at approximately 22 S, whereas at acidic pH it
55 2 S, whereas at acidic pH it dissociates and sediments at approximately 5 S.
56 diments remained identifiable from post-Irma sediments at Blackwater Bay as a gray poorly sorted coar
57 ith multiple collectors effectively utilized sediment at both horizontal and vertical directions and
58 ed morphologic features of beta-retroviruses sedimenting at buoyant densities of 1.12 to 1.18 g/mL in
59 ated with potential CO2 leakage into shallow sediments at carbon sequestration sites.
60 for Tc(IV) to be oxidized and mobilized from sediments at coastal nuclear sites resulting from predic
61 e rise of continents and the accumulation of sediments at continental edges and in trenches has provi
62 (Fq'/Fm') was significantly reduced in oiled sediments at day 7, implying that the initial diatom-dom
63 superior for cases where large molecules are sedimented at faster rotor speeds, during which sediment
64 of an over-the-counter medication in aquatic sediments at five different locations.
65 ssess microbial diversity in tropical marine sediments at five shallow-water sites in Belize using bo
66 hic activity related to pathogens within bed sediment at freshwater beaches.
67 nce of organic matter in lacustrine mudstone sediments at Gale crater was revealed by the Mars Scienc
68 higher-order complexes containing Sec1p that sediment at greater than 20S.
69  eventually producing polymeric species that sediment at >> 10 000 S.
70 into the gradient, while most edited A6 mRNA sediments at >35S.
71 .9 Mb of genetic material was sequenced from sediments at horizons 1, 16, 32, and 50 m below the seaf
72                          Sills intruded into sediment at least two times, first about 12-13 Ma (Middl
73 minin species discovered in Late Pleistocene sediments at Liang Bua (Flores, Indonesia), has generate
74 ing Ca2+-aggregated microsomes, which can be sedimented at low g forces.
75           The amount of cross-linked F-actin sedimenting at low centrifugal force also increased with
76 red by enriching sulfur reducers from acidic sediments at low pH (from 2 to 5) with hydrogen, glycero
77 ), which has not previously been verified in sediments at low temperature.
78 y be wider, slope more gently, and transport sediment at lower flows than rivers on Earth or Mars.
79 t remnants of ECNA sea water persist in deep sediments at many locations along the Atlantic margin.
80 were collected from the top 25 cm of surface sediment at ocean depths approaching 60 m over a ~2-km(2
81 natures for organic matter preserved in lake sediments at Olduvai Gorge during a key juncture in huma
82 (VI) adsorption to the quartz-sand dominated sediments at pH </= 4.0.
83  ultracentrifugation shows one main complex, sedimenting at s(20,)(w) = 7.2 +/- 0.1 S, together with
84 ing back to around 5800 cal BC found in lake sediments at Santovka, Slovakia, predated the earliest k
85 ntly found in bioretention media and forebay sediments at Sigma(35)PFAS concentrations of <0.03-19 an
86 7 and 1.3) but accumulated preferentially in sediments at source-driven sites (BSAF = 0.2 and 0.4).
87 ds to determine GrIS history from subglacial sediment at the base of the Camp Century ice core collec
88 le Bravo." Radioactive deposits in the ocean sediment at the bomb crater are widespread and high leve
89  near the water's surface or settle into the sediment at the bottom of the MSP, depending on their de
90 es present in the supernatant of this mutant sediment at the correct density for a retroviral particl
91 Samples from the sulphide body and overlying sediment at the Hakurei Site, Izena Hole, middle Okinawa
92   A higher abundance of MPs was found in the sediment at the inlet of the constructed wetland compare
93 c rates similar to those in water, soil, and sediment at the same temperature.
94 rofiles of the concentration versus depth of sediment at the two sites showed various patterns among
95 d-type p51 (p66delta/p51WT and p66Ala/p51WT) sedimented at the dimeric position.
96 a3beta2alpha5 receptors expressed in oocytes sedimented at the same 11 S value as native alpha3-conta
97 tructing the former valley bottom and dating sediments at the base of the valley fill, we show that s
98  trace metals, and pollution indices) in the sediments at the collection sites were evaluated.
99 ratios are similar to marine and terrestrial sediments at the ETE, and very different from potential
100 he sub-samples suggest that hydrate in silty sediments at the Gulf of Mexico is pore-invasive rather
101            Microbial diversity in subsurface sediments at the Hanford Site 300 Area near Richland, Wa
102                Fullerenes (C60 to C200) from sediments at the PTB contain trapped helium and argon wi
103 phorus and iron measurements of hydrothermal sediments at the same site.
104              Our results indicate that beach sediments at the sediment-water interface could serve as
105 microspectroscopy (mFTIR) analyses of intact sediments at the site of Wonderwerk Cave, Northern Cape
106 direct evidence for cold features in certain sediments at the site, Neandertals used the site predomi
107 ts aberrant SH2 domain, the Dd-STATb protein sediments at the size expected for a homodimer and it is
108 ME-2 and/or ANME-3 was abundant in down-core sediments at the ST site.
109         The concentrations of PAH in surface sediments at the two locations were comparable and highe
110 ting advection of hydrothermal fluid through sediment at this site.
111 IV) accumulation in organic-enriched reduced sediments at three UCRB floodplains.
112  ARG in Minnesota's waterbodies in water and sediment at two spatial scales: macro, throughout the st
113          In sucrose density gradients, KIF3C sediments at two distinct densities, suggesting that it
114                     Hurricane Ian's overwash sediments at two mangrove sites, including one directly
115 ., but did not find a single spherule in YDB sediments at two previously reported sites.
116 corer to collect bottom seawater and surface sediments at vent sites.
117 equences (units) of sandy, weakly stratified sediments at Wakulla Springs, Florida.
118          They saltate like the wild type and sediment at wild-type rates upon gravistimulation.

 
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