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1 asured using quantitative Western blots, and radioisotopic (14) C uptake was used to characterize lig
2 d ages, provide the only extant independent, radioisotopic age constraint on glacial termination VI a
3 tional archaeological discoveries as well as radioisotopic age control and a magnetic polarity strati
5 nstrain the origin of dinosaurs, we produced radioisotopic ages for the Argentinian Chanares Formatio
7 s of Mars and the Earth, using an integrated radioisotopic and astronomical timescale from the Cretac
10 combinations of Fos immunocytochemistry and radioisotopic- and digoxigenin-labeled in situ hybridiza
18 le stable isotope biosignature detection and radioisotopic dating of vug- and fracture-filling assemb
19 scence has been considered an alternative to radioisotopic detection of materials in the life science
21 need for the waste disposal associated with radioisotopic, enzyme-linked, or fluorescence detection
24 istribution of Y1-R mRNA in rodents by using radioisotopic in situ hybridization histochemistry (ISHH
25 lular components and, using a combination of radioisotopic labeling and mass spectrometry, were shown
27 creases the stability of HOSCN/OSCN(-), that radioisotopic labeling provided evidence that under phys
29 has experienced a widespread transition from radioisotopic labeling to nonisotopic labeling over the
33 ts the application of whole-body noninvasive radioisotopic, magnetic, and optical imaging methods for
35 showed, for the first time, consistency with radioisotopic measurements of the affinity of the FeEnt-
36 epair in vivo, we developed a convenient non-radioisotopic method to directly detect DNA excision rep
37 determined with considerable precision using radioisotopic methodologies; however, complications asso
39 c placement via a combination of established radioisotopic methods and a recently developed dating me
40 e principles of molecular targeting based on radioisotopic methods and provide examples from the lite
42 an be by any number of highly sensitive, non-radioisotopic modalities, such as fluorescence resonance
44 antage of this capability, evaluation of the radioisotopic purity of 99mTc produced at medium energy
47 ns and geochemical, magnetostratigraphic and radioisotopic results that securely place the Chorora Fo
48 ach known to be functional to some degree in radioisotopic sequencing, on single-stranded M13mp18 tem
49 e accurate interpretation and attribution of radioisotopic signatures is only possible with a complet
53 he value calculated for in situ nerves using radioisotopic techniques, but less than the value report
56 e water residence time, determined using the radioisotopic tracer (222)Rn, with dissolved carbon and
57 es of a chemostat for strain improvement and radioisotopic tracers for the quantification of pathway
58 ne (OM) and the inner membrane, but existing radioisotopic uptake assays only measure its passage thr