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The drying shrinkage could be explained by the cumulative pore volume in the gel pores and was larger in most samples with low RM content than that in the samples without RM.
Most samples with higher parasitemias remained positive upon re-examination (55/59 =93%).
Components 22 and 24 were dominant in most samples with contents that ranged 2.28 4.92‰ and 0.87 3.00‰, respectively.
The number of contigs detected was similar for most samples, with the exception of those from seeds, despite generation of a similar number of reads.
Most samples with PIK3CA mutations (80%) also had mutations in other genes, the most frequent of which was KRAS; other mutated genes were BRAF, MET, NRAS, and a second PIK3CA mutation (Table 2, last column).
Most samples with too few sequences to be included in the final datasets (i.e., failures) were collected at early time points (e.g., days 0 and 3) when microbial biomass was likely low.
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Furthermore, the surface areas (Table 1) of most samples decrease with increase in the crystallization time of the samples obtained by different acids because the high temperature causes the further condensation of Si OH species.
Most samples associated with the basal-like subtype clustered together, showing a distinctive genetic profile, characterized by the overexpression of KRT genes and TRIM29, among others.
We found that most samples cluster with the North-Central European populations (likely to correspond to the largest cluster on our PCA plot), but that there is also a distinct group stemming from Mediterranean populations.
At a 60 40 mixture, most samples erroneously grouped with the reference with longer branch lengths.
In contrast, most samples were undersaturated with respect to mackinawite (FeS s)).
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