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Ponganis, PJ, Meir JU, Williams CL.  2010.  Oxygen store depletion and the aerobic dive limit in emperor penguins. Aquatic Biology. 8:237-245.   10.3354/ab00216   AbstractWebsite

The aerobic dive limit (ADL), dive duration associated with the onset of post-dive blood lactate elevation, has been widely used in the interpretation of diving physiology and diving behavior. However, its physiological basis is incompletely understood, and in most studies, ADLs are simply calculated with an O(2) store/O(2) consumption formula. To better understand the ADL, research has been conducted on emperor penguins diving at an isolated dive hole. This work has revealed that O(2) stores are greater than previously estimated, and that the rate of depletion of those O(2) stores appears to be regulated primarily through a diving bradycardia and the efficiency of swimming. Blood and respiratory O(2) stores are not depleted at the 5.6 min ADL determined by post-dive blood lactate measurements. It is hypothesized that muscle, isolated from the circulation during a dive, is the primary source of lactate accumulation. To predict this 5.6 min ADL for these shallow dives at the isolated dive hole with the classic O(2) store/O(2) consumption formula, an O(2) consumption rate of 2x the predicted metabolic rate of a penguin at rest is required. In contrast, if the formula is used to calculate an ADL that is defined as the time for all consumable O(2) stores to be depleted, then a 23.1 min dive, in which final venous partial pressure of oxygen (P(O2)) was 6 mm Hg (0.8 kPa), represents such a maximum limit and demonstrates that an O(2) consumption rate of about 0.5x the predicted rate of an emperor penguin at rest is required in the formula.

Ponganis, PJ, Stockard TK, Meir JU, Williams CL, Ponganis KV, Howard R.  2009.  O-2 store management in diving emperor penguins. Journal of Experimental Biology. 212:217-224.   10.1242/jeb.026096   AbstractWebsite

In order to further define O-2 store utilization during dives and understand the physiological basis of the aerobic dive limit (ADL, dive duration associated with the onset of post-dive blood lactate accumulation), emperor penguins (Aptenodytes forsteri) were equipped with either a blood partial pressure of oxygen (P-O2) recorder or a blood sampler while they were diving at an isolated dive hole in the sea ice of McMurdo Sound, Antarctica. Arterial P-O2 profiles (57 dives) revealed that (a) pre-dive P-O2 was greater than that at rest, (b) P-O2 transiently increased during descent and (c) post-dive P-O2 reached that at rest in 1.92 +/- 1.89 min (N=53). Venous P-O2 profiles (130 dives) revealed that (a) pre-dive venous P-O2 was greater than that at rest prior to 61% of dives, (b) in 90% of dives venous P-O2 transiently increased with a mean maximum P-O2 of 53 +/- 18 mmHg and a mean increase in P-O2 of 11 +/- 12 mmHg, (c) in 78% of dives, this peak venous P-O2 occurred within the first 3 min, and (d) post-dive venous P-O2 reached that at rest within 2.23 +/- 2.64 min (N=84). Arterial and venous P-O2 values in blood samples collected 1-3 min into dives were greater than or near to the respective values at rest. Blood lactate concentration was less than 2 mmol l(-1) as far as 10.5 min into dives, well beyond the known ADL of 5.6 min. Mean arterial and venous P-N2 of samples collected at 20-37 m depth were 2.5 times those at the surface, both being 2.1 +/- 0.7 atmospheres absolute (ATA; N=3 each), and were not significantly different. These findings are consistent with the maintenance of gas exchange during dives (elevated arterial and venous P-O2 and P-N2 during dives), muscle ischemia during dives (elevated venous P-O2, lack of lactate washout into blood during dives), and arterio-venous shunting of blood both during the surface period (venous P-O2 greater than that at rest) and during dives (arterialized venous P-O2 values during descent, equivalent arterial and venous P-N2 values during dives). These three physiological processes contribute to the transfer of the large respiratory O-2 store to the blood during the dive, isolation of muscle metabolism from the circulation during the dive, a decreased rate of blood O-2 depletion during dives, and optimized loading of O-2 stores both before and after dives. The lack of blood O-2 depletion and blood lactate elevation during dives beyond the ADL suggests that active locomotory muscle is the site of tissue lactate accumulation that results in post-dive blood lactate elevation in dives beyond the ADL.

Kooyman, GL, Ponganis PJ.  1994.  Emperor penguin oxygen consumption, heart rate and plasma lactate levels during graded swimming exercise. Journal of Experimental Biology. 195:199-209. AbstractWebsite

Oxygen consumption (V-O2), heart rate and blood chemistry were measured in four emperor penguins, Aptenodytes forsteri (Gray), during graded swimming exercise. The maximum V-O2, obtained, 52ml O-2 kg(-1) min(-1), was 7.8 times the measured resting V-O2 of 6.7 ml O-2 kg(-1) min(-1) and 9.1 times the predicted resting V-O2. As the swimming effort rose, a linear increase in surface and submerged heart rates (fH) occurred. The highest average maximum surface and submersion heart rates of any bird were 213 and 210 beats min(-1), respectively. No increase in plasma lactate concentrations occurred until V-O2 was greater than 25 ml O-2 kg(-1) min(-1). At the highest V-O2 values measured, plasma lactate concentration reached 9.4 mmol l(-1). In comparison with other animals of approximately the same mass, the aerobic capacity of the emperor penguin is less than those of the emu and dog but about the same as those of the seal, sea lion and domestic goat. For aquatic animals, a low aerobic capacity seems to be consistent with the needs of parsimonious oxygen utilization while breath-holding.