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Since silk beta-sheet crystals play the role of physical crosslinks in silk materials, in their absence the crosslinking phenomenon we observed in the space-traveled silk samples were therefore due to chemical processes, and not to changes of secondary protein structure.
These samples were therefore classified as tidal channel October samples in the analyses (Table 2).
Wastewater samples were therefore not necessarily the most toxic when their fractions exhibited the highest inhibitory effects.
Duplicate samples were therefore taken from the larger iceberg samples (S1, S4, KG1 and KG2) to provide a rough estimate of sampling variations.
Samples were therefore transferred to 1 mL vials (Waters).
Samples were therefore pooled in 4 groups of years: 1900s, 1950s, 1970s and 2000s (Tables 2 and 3).
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The presence of 10Be and 26Al in these samples is therefore direct evidence for past deglaciation episodes at this location.
Testing for CD8+ reactivity toward other targets in NT1 blood samples is therefore an important next step for understanding NT1 pathogenesis.
This time integration of moss samples was therefore taken into account when building the constructed atmospheric 14C curves (see ref. 12).
Samples are therefore usually prepared and positioned to minimise the influence of other variables.
A rectangular sliding window of 128 samples was therefore used.
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