We measured the partial pressure of oxygen (Po-2) in the interstitial
gas surrounding the sand-swimming Namib mole Eremitalpa granti namiben
sis. At a sand temperature of 26 degrees C, which produced a nearly ma
ximal rate of oxygen consumption, the Po-2 near the noses of the anima
ls averaged only 0.9 kPa (6.7 Torr) below the level in the free atmosp
here. High oxygen availability was a result of the notably low metabol
ic rate in the 20 g mammals and the dry, porous and metabolically inac
tive nature of dune sand. A mathematical model indicated that normal m
ammals weighing 200 g or more could comfortably exist completely encas
ed in dune sand. We concluded that the moles' small size and low metab
olic rate are not adaptations to hypoxia or hypercapnia underground bu
t are probably related to low food availability and the energetic cost
of foraging in their desert environment. (C) 1996 Academic Press Limi
ted