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Kooyman, GL, Ponganis PJ.  2004.  The icing of external recorders during the polar winter. Memoirs of National Institute of Polar Research Special Issue. 58:183-187. AbstractWebsite
Ponganis, PJ, Meir JU, Williams CL.  2011.  In pursuit of Irving and Scholander: a review of oxygen store management in seals and penguins. Journal of Experimental Biology. 214:3325-3339.   10.1242/jeb.031252   AbstractWebsite

Since the introduction of the aerobic dive limit (ADL) 30 years ago, the concept that most dives of marine mammals and sea birds are aerobic in nature has dominated the interpretation of their diving behavior and foraging ecology. Although there have been many measurements of body oxygen stores, there have been few investigations of the actual depletion of those stores during dives. Yet, it is the pattern, rate and magnitude of depletion of O(2) stores that underlie the ADL. Therefore, in order to assess strategies of O(2) store management, we review (a) the magnitude of O(2) stores, (b) past studies of O(2) store depletion and (c) our recent investigations of O(2) store utilization during sleep apnea and dives of elephant seals (Mirounga angustirostris) and during dives of emperor penguins (Aptenodytes forsteri). We conclude with the implications of these findings for (a) the physiological responses underlying O(2) store utilization, (b) the physiological basis of the ADL and (c) the value of extreme hypoxemic tolerance and the significance of the avoidance of re-perfusion injury in these animals.

Kooyman, GL, Ponganis PJ.  2007.  The initial journey of juvenile emperor penguins. Aquatic Conservation-Marine and Freshwater Ecosystems. 17:S37-S43.   10.1002/aqc.930   AbstractWebsite

1. The first major journey of emperor penguins, among several in their lifetime, is the juveniles' dispersal from their natal colony on a trip that takes them beyond Antarctic waters. The route taken by fledglings from Cape Washington (74.5 degrees S; 165.4 degrees E) was Studied by applying satellite transmitters to ten individuals during December 1994-1996. In January 2001 transmitters with longer transmission capacity were also applied to six hand-fed fledglings, which had been held captive for one month while attaining a body mass exceeding that of wild birds. These post-captive birds were released at the ice edge of McMurdo Sound (77.5 degrees S; 165.0 degrees E), which is in the vicinity of other emperor penguin colonies, and 320km south of their natal colony of Cape Washington. 2. Independent of their parents, the wild birds travelled north-east for the next two months, reaching locations as low as 57 degrees S. The post-captive birds travelled north also, but their trek reached only to about 63 degrees S before they turned south, or remained near their most northerly position from March through May. 3. It was concluded that among colonies in the southern Ross Sea: (a) most healthy fledglings Survive at least the first two months at sea, feeding themselves as they go; (b) the Cape Washington fledglings travelled as far north as 57 degrees S, and much of this journey was in ice free waters; (c) by April, the post-captive birds reached at least as far as the large-scale pack ice edge and possibly beyond the edge Lit 63 degrees S; (d) by early March the trend north ends, and by about late March the birds travel to, or remain near the northern ice edge. 4. The reason the birds travel so far north remains a mystery. Copyright (c) 2008 John Wiley & Sons, Ltd.

McDonald, BI, Ponganis PJ.  2013.  Insights from venous oxygen profiles: oxygen utilization and management in diving California sea lions. Journal of Experimental Biology. 216:3332-3341.   10.1242/jeb.085985   AbstractWebsite

The management and depletion of O-2 stores underlie the aerobic dive capacities of marine mammals. The California sea lion (Zalophus californianus) presumably optimizes O-2 store management during all dives, but approaches its physiological limits during deep dives to greater than 300. m depth. Blood O-2 comprises the largest component of total body O-2 stores in adult sea lions. Therefore, we investigated venous blood O-2 depletion during dives of California sea lions during maternal foraging trips to sea by: (1) recording venous partial pressure of O-2 (PO2) profiles during dives, (2) characterizing the O-2-hemoglobin (Hb) dissociation curve of sea lion Hb and (3) converting the PO2 profiles into percent Hb saturation (SO2) profiles using the dissociation curve. The O-2-Hb dissociation curve was typical of other pinnipeds (P-50=28 +/- 2mmHg at pH 7.4). In 43% of dives, initial venous SO2 values were greater than 78% (estimated resting venous SO2), indicative of arterialization of venous blood. Blood O-2 was far from depleted during routine shallow dives, with minimum venous SO2 values routinely greater than 50%. However, in deep dives greater than 4. min in duration, venous SO2 reached minimum values below 5% prior to the end of the dive, but then increased during the last 30-60s of ascent. These deep dive profiles were consistent with transient venous blood O-2 depletion followed by partial restoration of venous O-2 through pulmonary gas exchange and peripheral blood flow during ascent. These differences in venous O-2 profiles between shallow and deep dives of sea lions reflect distinct strategies of O-2 store management and suggest that underlying cardiovascular responses will also differ.

Ponganis, PJ, Stockard TK, Levenson DH, Berg L, Baranov EA.  2006.  Intravascular pressure profiles in elephant seals: Hypotheses on the caval sphincter, extradural vein and venous return to the heart. Comparative Biochemistry and Physiology a-Molecular & Integrative Physiology. 145:123-130.   10.1016/j.cbpa.2006.05.012   AbstractWebsite

In order to evaluate bemodynamics in the complex vascular system of phocid seals, intravascular pressure profiles were measured during periods of rest-associated apnea in young elephant seals (Mirounga angustirostris). There were no significant differences between apneic and eupneic mean arterial pressures. During apnea, venous pressure profiles (pulmonary artery, thoracic portion of the vena cava (thoracic vena cava), extradural vein, and hepatic sinus) demonstrated only minor, transient fluctuations. During eupnea, all venous pressure profiles were dominated by respiratory fluctuations. During inspiration, pressures in the thoracic vena cava and extradural vein decreased -9 to -21 mm Hg, and -9 to -17 mm Hg, respectively. In contrast, hepatic sinus pressure increased 2-6 mm Hg during inspiration. Nearly constant hepatic sinus and intrathoracic vascular pressure profiles during the breath-hold period are consistent with incomplete constriction of the caval sphincter during these rest-associated apneas. During eupnea, negative inspiratory intravascular pressures in the chest ("the respiratory pump") should augment venous return via both the venae cavae and the extradural. vein. It is hypothesized that, in addition to the venae cavae, the prominent para-caval venous system of phocid seals (i.e., the extradural vein) is necessary to allow adequate venous return for maintenance of high cardiac outputs and blood pressure during eupnea. (c) 2006 Elsevier Inc. All rights reserved.

Houser, DS, Dankiewicz-Talmadge LA, Stockard TK, Ponganis PJ.  2010.  Investigation of the potential for vascular bubble formation in a repetitively diving dolphin. Journal of Experimental Biology. 213:52-62.   10.1242/jeb.028365   AbstractWebsite

The production of venous gas emboli (VGE) resulting from altered dive behavior is postulated as contributing to the stranding of beaked whales exposed to mid-frequency active sonar. To test whether nitrogen gas uptake during repetitive breath-hold diving is sufficient for asymptomatic VGE formation in odontocetes, a bottlenose dolphin (Tursiops truncatus Montagu) was trained to perform 10-12 serial dives with 60s surface intervals to depths of 30, 50, 70 or 100m. The dolphin remained at the bottom depth for 90s on each dive. Doppler and/or two-dimensional imaging ultrasound did not detect VGE in the portal and brachiocephalic veins following a dive series. Van Slyke analyses of serial, post-dive blood samples drawn from the fluke yielded blood nitrogen partial pressure (P(N2)) values that were negligibly different from control samples. Mean heart rate (HR; +/-1. s.d.) recorded during diving was 50+/-3. beats min(-1) and was not significantly different between the 50, 70 and 100 m dive sessions. The absence of VGE and elevated blood P(N2) during post-dive periods do not support the hypothesis that N(2) supersaturation during repetitive dives contributes to VGE formation in the dolphin. The diving HR pattern and the presumed rapid N(2) washout during the surface-interval tachycardia probably minimized N(2) accumulation in the blood during dive sessions.