Time course studies (protocol 1) showed small but measurable and approximately linear changes for three variables: PO2, pH, and BE.
Approximately 900,000 changes were found in E9 with an average of ∼67,000 per chromosome (~69,000 if the nonassembled chr 0 data are included); this represents approximately one sequence change every 1100 base pairs (bp).
Composite WOMAC scores at week 6 showed approximately equal changes in both groups (-270 versus -263, placebo versus AMG 108, respectively; P = 0.97).
South of approximately 55°S, changes in upwelling tend to increase DIC but are largely offset by stronger northward advection, increased carbon export, and outgassing of CO2.
The estimated rate of unrepaired DNA replication errors leading to SNPs in B. anthracis is approximately 10-10 changes per nucleotide per generation [ 38].
To address this, we have preliminary sequencing data that suggest that CC-125 has approximately 24,000 changes relative to the reference genome.
Finally, the repressive mark H3K27me3 was enriched approximately threefold changes in macroH2A-purified nucleosomes as compared to genomic chromatin (approximately 18% in macroH2A-purified vs. approximately 6% in genomic or approximately 5% in H2A.1-purified nucleosomes).
For comparison sake, a 1% change in AAI corresponds to only an approximately 5.7% change in genomic fluidity in the E. coli – Shigella group and an approximately 1.5% change in genomic fluidity in B. cereus (table 1).
Based on linear regression of genomic fluidity against AAI, within Y. pestis a change of 1% in AAI corresponds to an approximately 31% change in genomic fluidity; within the MTBC a similar 1% change in AAI corresponds to an approximately 26% change in genomic fluidity.
According to a GLMM analysis, a 1% change in weight was associated with an approximately 3% change in total diabetes-related costs (p ≪ 0.01).
