Specimens of Nautilus pompilius were trapped at depths of 225 300 m off the
sunken barrier reef southeast of Port Moresby, Papua New Guinea. Animals t
ransported to the Motupore island laboratory were acclimated to normal habi
tat temperatures of 18 degrees C and then cannulated for arterial and venou
s blood sampling. When animals were forced to undergo a period of progressi
ve hypoxia eventually to encounter ambient partial pressure of oxygen (PO2)
levels Of similar to 10 mmHg land corresponding arterial PO2's of similar
to 5 mmHg), they responded by lowering their aerobic metabolic rates to 5-1
0% of those seen in resting normoxic animals. Coincident with this profound
metabolic suppression was an overall decrease in activity, with brief peri
ods of jet propulsion punctuating long periods of rest, Below ambient PO2 l
evels of 30-40 mmHg, ventilatory movements became highly periodic and at th
e lowest PO2 levels encountered, ventilation occasionally ceased altogether
. Cardiac output estimated by the Fick equation decreased during progressiv
e hypoxia by as much as 75 80%, and in the deepest hypometabolic states hea
rt rates slowed to one to two cycles of very low amplitude per minute. By t
he end of 500 min exposure to ambient PO2 levels of 10 mmHg or less, the an
aerobic end products octopine and succinate had increased significantly in
adductor muscle and heart, respectively. Increased concentrations of octopi
ne in adductor muscle apparently contributed to a small intracellular acido
sis and to the development of a combined respiratory and metabolic acidosis
in the extracellular compartment, On the other hand, increases in succinat
e in heart muscle occurred in the absence of any change in cardiac pHi. Tak
en together, we estimate that these anaerobic end products would make up le
ss than 2% of the energy deficit arising from the decrease in aerobic metab
olism. Thus, metabolic suppression is combined with a massive downregulatio
n of systemic O-2 delivery to match metabolic supply to demand.