Table 3.
Responses of GC1 and GC2 to changes in GC3, by domain
n | R2 | Slope ± SE | Y at GC3 = 0 ± SE | Y at GC3 = 100 ± SE | ||
Bacteria | 311 | GC1 | 0.91 | 0.370 ± 0.007 | 0.367 ± 0.004 | 0.737 ± 0.003 |
GC2 | 0.80 | 0.219 ± 0.006 | 0.291 ± 0.004 | 0.510 ± 0.003 | ||
Archaea | 28 | GC1 | 0.85 | 0.38 ± 0.03 | 0.35 ± 0.02 | 0.73 ± 0.02 |
GC2 | 0.60 | 0.16 ± 0.03 | 0.30 ± 0.01 | 0.45 ± 0.01 | ||
Eukaryotes | 257 | GC1 | 0.57 | 0.24 ± 0.01 | 0.402 ± 0.008 | 0.643 ± 0.007 |
GC2 | 0.38 | 0.15 ± 0.01 | 0.334 ± 0.007 | 0.482 ± 0.006 |
Because there is error in both axes, but there should be a definite causal relationship between GC3 and GC1 or GC2, we use model I regression to predict specific values of GC1 or GC2 from a set value of GC3, and thus to calculate the most likely proportion and GC content of constant sites [73].