Fig. 4. Final PO2 and dive duration. Final
PO2 values were recorded within the last 15 s
of each dive. (A) Final venous PO2 and dive
duration from nine emperor penguins (key shows individual symbols for each
penguin). The variability in final PO2 values
in relation to dive duration is presumably secondary to differences in
metabolic rates during dives. In addition, the span of
PO2 values at the aerobic dive limit (ADL)
clearly indicates that the blood O2 store is not depleted at this
limit, the dive duration associated with post-dive lactate accumulation. The
exponential regression
(y=96.416e–0.1216x,
r2=0.94, P<0.001) was constructed from the highest
final PO2 during each 1-min interval of dive
duration. This represents the minimum rate at which final
PO2 declines in relation to dive duration. (B)
Comparison of final venous PO2, arterial
PO2 and air sac
PO2
(Stockard et al., 2005)
demonstrates that air sac, arterial and venous
PO2 values become indistinguishable in longer
dives.