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The %S values of the clay phases in each sample were estimated using the approach outlined by Hillier (1993), where peak migration curves derived by Hower (1981) were used for regularly ordered (R = 1; i.e., free of any successive saponite saponite pairs within stacking %S < 50) C/S for peaks between 8.5 and 7.1 Å.
The PEDF concentrations (ng/ml) in each sample were estimated using internal PEDF standards.
The equivalent cDNA copies for each sample were estimated based on linear regression analysis.
Expression levels in each sample were estimated for 34 695 contigs from numbers of reads mapping to each contig.
Parametric estimates of OTU richness for each sample were estimated with Catchall (Bunge et al. 2012) and are displayed in Table 1.
Moreover, the amounts of cytochrome c present in the cytosolic extracts and cleaved caspase-9 or caspase-3 fragment and cleaved PARP fragment in each sample were estimated by western blot analyses as described above.
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In addition, the energy storage capacity of each sample is estimated using analytical formulae.
Then, the areal average precipitation of each sample is estimated and used as input to the Xinanjiang model.
The gold concentration in each sample was estimated using the ImageJ software (Fig. 12).
Colonies of more than 50 cells were scored as survivors, and the plating efficiency for each sample was estimated based on the initial number of seeded cells.
The maximum paleotemperature for each sample was estimated from the reported vitrinite reflectance values (Ro) in accompanying terrigenous rocks (Ohmori 1998) (Table 1).
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