Prolonged chemical restraint of walrus (Odobenus rosmarus) with etorphine supplemented with medetomidine

Physiological studies involving the use of isotopic water required chemical restraint of free- ranging walruses (Odobenus rosmarus) for several hours. In August 2000, six male walrus (total body mass: 1050–1550 kg) were immobilized in East Greenland by remote delivery of 8.0–9.8 mg of etorphine and subsequently restrained for up to 6.75 h by administration of medetomidine. The effects of etorphine were reversed with 10–24 mg diprenorphine. After termination of the etorphine-induced apnoea, lasting an average of 15.8 min (SD = 9.7, range = 9.5–35.2 min, n = 6), the animals were initially given 10–20 mg medetomidine intramuscularly. The initial dose was further augmented by 5 mg at intervals of 5 min. In two cases, when medetomidine was administered through a catheter inserted in the extradural vein, the animal became instantly apnoeic and regained respiratory function only after intravenous injection of the prescribed dose of the antagonist atipamezole and of the respiratory stimulant doxapram. After an average of 3.5 hours of immobilisation, rectal temperature began to increase and it is conceivable that this is the factor that will ultimately limit the duration of immobilisation. The animals became conscious and fully mobile shortly after an intravenous injection of a dose of atipamezole approximately twice the mass of the total dose of medetomidine given during the procedure followed by 400 mg of doxapram. It is concluded that medetomidine appears to be a suitable drug for chemical restraint of walruses for time-consuming procedures following initial immobilisation by etorphine. With animals of total body mass around 1,000–1,500 kg, the drug should be given intramuscularly in 10–20 mg increments (total mass 10–60 mg) until the breathing rate falls to approximately 1 min-1. At this level, breathing is maintained and animals do not respond to touch or injection

Total mercury in hair of polar bears (Ursus maritimus) from Greenland and Svalbard

Concentrations (ppm = ug/g dry weight) of total mercury (Hg) were determined in hair of polar bears (Ursus maritimus) from northwestern Greenland (N = 22; period of sampling: 1978-1989), eastern Greenland (N = 44: 1984-1989) and Svalbard (N = 31; 1980). For subadults (2-6 years of life), adults (7-10 years). and old bears (>10 years), concentrations of total Hg in hair were not found to be dependent on age or sex. A decreasing trend in Hg concentrations was found from west to east. The mean concentrations of total Hg in hair (cubs of the year and yearlings excluded) were: northwestern Greenland, x = 8.38 ppm (min.-max.: 4.71-14.19 ppm. N = 21); eastern Greenland: x = 4.58 ppm (min.-max.: 2.50-8.83 ppm. N = 41); and Svalbard, x = 1.98 ppm (min.-max.: 1.02-4.55 ppm, N = 29). Concentrations found in northwestern Greenland were similar to those reported by others from the hair of polar bears sampled within management zone F of the eastern Canadian High Arctic. Concentrations of total Hg in polar bear hair from eastern Greenland were similar to concentrations found by others in contemporary (1988) material collected during spring in western Svalbard. However, the mean concentration of total Hg in the 1980 Svalbard material, which was collected during July-September, was significantly lower than concentrations found in samples taken during late winter and spring in eastern Greenland and at Svalbard, respectively. Presumably the relatively low concentrations found in the 1980 Svalbard sample arc attributable to the period of moult and hence a larger proportion of newly grown hair in the individual samples. In a subsample consisting of internal tissues from 19 polar bears from eastern Greenland (1984-1987), concentrations of total Hg in hair correlated positively with concentrations of total Hg (wet weight) in muscle (N = 6), liver (N = 19) and kidney (N = 19) tissue. For liver and kidney tissue these relationships were statistically significant

Do Wild Polar Bears (Ursus maritimus) Use Tools When Hunting Walruses (Odobenus rosmarus)?

Since the late 1700s, reports of polar bears (Ursus maritimus) using tools (i.e., pieces of ice or stones) to kill walruses (Odobenus rosmarus) have been passed on verbally to explorers and naturalists by their Inuit guides, based on local traditional ecological knowledge (TEK) as well as accounts of direct observations or interpretations of tracks in the snow made by the Inuit hunters who reported them. To assess the possibility that polar bears may occasionally use tools to hunt walruses in the wild, we summarize 1) observations described to early explorers and naturalists by Inuit hunters about polar bears using tools, 2) more recent documentation in the literature from Inuit hunters and scientists, and 3) recent observations of a polar bear in a zoo spontaneously using tools to access a novel food source. These observations and previously published experiments on brown bears (Ursus arctos) confirm that, in captivity, polar and brown bears are both capable of conceptualizing the use of a tool to obtain a food source that would otherwise not be accessible. Based on the information from all our sources, this may occasionally also have been the case in the wild. We suggest that possible tool use by polar bears in the wild is infrequent and mainly limited to hunting walruses because of their large size, difficulty to kill, and their possession of potentially lethal weapons for both their own defense and the direct attack of a predator. Depuis la fin des années 1700, des signalements d’ours polaires (Ursus maritimus) se servant d’outils (comme des morceaux de glace ou des pierres) pour tuer des morses (Odobenus rosmarus) ont été communiqués verbalement par des guides inuits à divers explorateurs et naturalistes. Les guides en question se fondaient sur les connaissances écologiques traditionnelles (CET) locales de même que sur les interprétations de traces dans la neige ou les récits d’observations directes des chasseurs inuits ayant fait les signalements. Pour évaluer la possibilité que les ours polaires puissent parfois se servir d’outils pour chasser les morses en milieu sauvage, nous résumons : 1) les observations décrites aux premiers explorateurs et naturalistes par les chasseurs inuits au sujet de l’utilisation d’outils par les ours polaires; 2) la documentation récente attribuable aux chasseurs inuits et aux scientifiques; et 3) les récentes observations de l’ours polaire d’un zoo se servant d’outils spontanément pour avoir accès à une nouvelle source de nourriture. Ces observations, alliées à des expériences publiées au sujet d’ours bruns (Ursus arctos), permettent de confirmer qu’en captivité, tant les ours bruns que les ours polaires sont capables de conceptualiser l’utilisation d’un outil pour se procurer de la nourriture qui ne serait autrement pas accessible. D’après les renseignements prélevés auprès de toutes nos sources, cela aurait aussi pu être occasionnellement le cas en milieu sauvage. Nous suggérons que l’utilisation possible d’outils par les ours polaires en milieu sauvage n’est pas fréquente et qu’elle est surtout limitée à la chasse au morse en raison de la grande taille de cette espèce, de la difficulté à l’abattre et des armes potentiellement mortelles qu’elle possède, tant pour se défendre que pour attaquer un prédateur directement.&nbsp

Habitat Use of Ringed Seals (Phoca hispida) in the North Water Area (North Baffin Bay)

In conjunction with the International North Water Polynya Study in Smith Sound (northern Baffin Bay) in 1997-99, we examined the area use and diving activity of 23 ringed seals (Phoca hispida) that had been equipped with satellite transmitters on the Greenland side of the North Water (NOW) area. The study covered the period 12 August 1996-30 June 1999. Contact with the seals was maintained for an average of 108 days (range: 8-332 days). Four seals emigrated from the NOW area. During all seasons, the seals that remained in the area spent about 90% of the time in coastal (< 100 m deep) waters in the eastern parts of the NOW area. The total area visited by the seals during the open-water season ranged between 10 300 km² (1996) and 18 500 km² (1998), corresponding to about 15% to 25% of the entire NOW area. In winter, the total area visited by the seals varied between 2500 km² (1996-97) and 7000 km² (1998-99), and in spring, between 800 km² (1999) and 2100 km² (1997). Individual movement was significantly greater during the open-water season than during winter and spring. Maximum dive depths recorded were over 500 m (maximum for the instrument) outside and 376 m inside the NOW, for a 96 kg male seal. Non-adult seals spent about 99% of the time in waters less than 100 m deep, and more than 92% of the time in the upper 50 m. In contrast, adults tended to spend more time at greater depths. The study indicated that (1) the ringed seals took advantage of the generally lighter ice conditions in the eastern NOW, and (2) that non-adults likely exploited ice-associated amphipods and young polar cod (Boreogadus saida), and adults, mainly older polar cod and cephalopods taken at greater depths.Conjointement avec l'étude internationale sur la polynie de l'Eau du Nord dans le détroit de Smith (partie nord de la baie de Baffin) menée de 1997 à 1999, on a examiné l'utilisation de cette zone et l'activité de plongée de 23 phoques annelés (Phoca hispida) munis d'émetteurs-satellite du côté groenlandais de la région de l'Eau du Nord («NOW»). L'étude a couvert la période allant du 12 août 1996 au 30 juin 1999. Le contact avec les phoques a été maintenu pendant une moyenne de 108 jours (étendue: 8-332 jours). Quatre phoques ont émigré de la zone NOW. Durant toutes les saisons, les phoques qui restaient dans la zone passaient environ 90% du temps dans des eaux côtières (profondeur < 100 m) dans les secteurs orientaux de NOW. La superficie totale visitée par les phoques durant la saison d'eau libre allait de 10 300 km² (1996) à 18 500 km² (1998), correspondant à environ 15 à 25% de toute la zone NOW. En hiver, l'étendue totale fréquentée par les phoques allait de 2500 km² (1996-1997) à 7000 km² (1998-1999), et au printemps, de 800 km² (1999) à 2100 km² (1997). Les déplacements individuels étaient de beaucoup plus grands durant la saison d'eau libre qu'au cours de l'hiver et du printemps. Les profondeurs maximales de plongée enregistrées dépassaient 500 m (limite de l'instrument) à l'extérieur de la zone NOW et 376 m à l'intérieur, pour un phoque mâle de 96 kg. Les phoques non adultes passaient environ 99% du temps dans des eaux à une profondeur ne dépassant pas 100 m, et plus de 92% du temps dans les 50 m supérieurs. En revanche, les adultes avaient tendance à passer plus de temps à de plus grandes profondeurs. L'étude révèle 1) que les phoques annelés tiraient parti du fait qu'il y avait moins de glace dans la partie orientale de NOW, et 2) que, selon toute vraisemblance, les non-adultes exploitaient amphipodes et jeune morue polaire (Boreogadus saida) associés à la glace, les adultes se nourrissant surtout de morue polaire plus âgée et de céphalopodes prélevés à de plus grandes profondeurs

The Utility of Harvest Recoveries of Marked Individuals to Assess Polar Bear (Ursus maritimus) Survival

Management of polar bear (Ursus maritimus) populations requires the periodic assessment of life history metrics such as survival rate. This information is frequently obtained during short-term capture and marking efforts (e.g., over the course of three years) that result in hundreds of marked bears remaining in the population after active marking is finished. Using 10 additional years of harvest recovery subsequent to a period of active marking, we provide updated estimates of annual survival for polar bears in the Baffin Bay population of Greenland and Canada. Our analysis suggests a decline in survival of polar bears since the period of active marking that ended in 1997; some of the decline in survival can likely be attributed to a decline in springtime ice concentration over the continental shelf of Baffin Island. The variance around the survival estimates is comparatively high because of the declining number of marks available; therefore, results must be interpreted with caution. The variance of the estimates of survival increased most substantially in the sixth year post-marking. When survival estimates calculated with recovery-only and recapture-recovery data sets from the period of active marking were compared, survival rates were indistinguishable. However, for the period when fewer marks were available, survival estimates were lower using the recovery-only data set, which indicates that part of the decline we detected for 2003 – 09 may be due to using only harvest recovery data. Nevertheless, the decline in the estimates of survival is consistent with population projections derived from harvest numbers and earlier vital rates, as well as with an observed decline in the extent of sea ice habitat.La gestion des populations d’ours polaires (Ursus maritimus) nécessite l’évaluation périodique des mesures du cycle biologique, tel que le taux de survie. Cette information est souvent obtenue dans le cadre des efforts de capture et de marquage à court terme (par exemple, sur une période de trois ans) qui se traduisent par le marquage d’une centaine d’ours au sein de la population une fois les travaux terminés. En nous appuyant sur dix années supplémentaires de données de récoltes de reprises suivant une période de marquage actif, nous aboutissons à des estimations actualisées de la survie annuelle des ours polaires faisant partie de la population de la baie de Baffin du Groenland et du Canada. Notre analyse suggère qu’il y a eu un déclin sur le plan de la survie des ours polaires depuis la période de marquage actif qui a pris fin en 1997. Une partie de ce déclin en matière de survie peut être attribuable à la diminution de la concentration de glace printanière sur le plateau continental de l’île de Baffin. La variance entourant les estimations de survie est comparativement élevée en raison du nombre à la baisse de marquages disponibles. Il y a donc lieu de faire preuve de prudence dans l’interprétation des résultats. La variance des estimations de survie augmentait considérablement au cours de la sixième année suivant le marquage. Lorsque nous avons comparé les estimations de survie avec les ensembles de données de reprise seulement et celles de recapture et de reprise pour la période de marquage actif, les taux de survie étaient indistinguables. Cependant, pour la période pendant laquelle un moins grand nombre de marquages était disponible, les estimations de survie étaient moins élevées lorsque nous nous sommes appuyés sur l’ensemble des données de reprise seulement, ce qui indique qu’une partie du déclin que nous avons constaté pour les années 2003 à 2009 pourrait être attribuable au fait que nous n’avons utilisé que les données des récoltes de reprises. Néanmoins, le déclin en matière d’estimations de survie est conforme aux projections de population dérivées des résultats des récoltes et des indices vitaux antérieurs, ainsi qu’à la diminution qui a été observée sur le plan de l’étendue de l’habitat de la glace de mer

Activity and Movement Patterns of Polar Bears Inhabiting Consolidated versus Active Pack Ice

We investigated the influence of ice conditions on activity and movement patterns of polar bears in the Canadian-West Greenland Arctic. We used radiotelemetry data gathered over 11 years (1989-99) from 160 adult female polar bears to test for differences in movement and activity of bears inhabiting active ice and consolidated ice. Bears inhabiting active ice moved more than those inhabiting consolidated ice (12 versus 8 km/day), but their activity throughout the year did not differ (bears of both groups were active for 21% of the day). Differences in activity and movement of bears in the two study areas appeared to be related to differences in predominant ice conditions and presumed prey availability. Seals, particularly juveniles, are most plentiful in spring and summer, when polar bears moved more and were most active. During winter, when juvenile seals were less available in consolidated ice areas, bears in that habitat were less active and moved less than bears in active ice areas. Polar bears have evolved flexible patterns of seasonal activity, movements, and facultative den use as adaptations to different sea-ice environments.On a étudié l'influence des conditions de glace sur le régime de l'activité et du déplacement de l'ours polaire dans l'Arctique canadien de l'ouest du Groenland. On s'est servi de données prélevées par radiomesure sur une période de 11 ans (de 1989 à 1999) portant sur 160 ourses polaires adultes afin de déterminer s'il existe des différences dans le déplacement et l'activité des ourses entre celles qui vivent sur la glace mobile et celles qui vivent sur la glace soudée. Les ourses vivant sur la glace mobile se déplaçaient plus que celles vivant sur la glace soudée (12 km/jour contre 8), mais leur activité tout au long de l'année ne différait pas (les ourses des deux groupes étaient actives 21 p. cent de la journée). Les différences dans l'activité et le déplacement des ourses entre les deux zones d'étude semblaient être reliées à des différences dans les conditions de glace prédominantes et dans la disponibilité présumée des proies. L'abondance des phoques, en particulier les jeunes, atteint son maximum au printemps et en été, au moment où les ourses polaires étaient souvent le plus actives et se déplaçaient le plus. Durant l'hiver, quand les phoques juvéniles étaient moins disponibles dans les zones de glace soudée, les ourses vivant dans cet habitat étaient moins actives et se déplaçaient moins que les ourses vivant dans les zones de glace mobile. L'ourse polaire a développé une certaine flexibilité de comportement dans son activité, son déplacement et son utilisation facultative d'une tanière, pour s'adapter à différents environnements de glace de mer

Are liver and renal lesions in East Greenland polar bears (Ursus maritimus) associated with high mercury levels?

BACKGROUND: In the Arctic, polar bears (Ursus maritimus) bio-accumulate mercury as they prey on polluted ringed seals (Phoca hispida) and bearded seals (Erignathus barbatus). Studies have shown that polar bears from East Greenland are among the most mercury polluted species in the Arctic. It is unknown whether these levels are toxic to liver and kidney tissue. METHODS: We investigated the histopathological impact from anthropogenic long-range transported mercury on East Greenland polar bear liver (n = 59) and kidney (n = 57) tissues. RESULTS: Liver mercury levels ranged from 1.1–35.6 μg/g wet weight and renal levels ranged from 1–50 μg/g wet weight, of which 2 liver values and 9 kidney values were above known toxic threshold level of 30 μg/g wet weight in terrestrial mammals. Evaluated from age-correcting ANCOVA analyses, liver mercury levels were significantly higher in individuals with visible Ito cells (p < 0.02) and a similar trend was found for lipid granulomas (p = 0.07). Liver mercury levels were significantly lower in individuals with portal bile duct proliferation/fibrosis (p = 0.007) and a similar trend was found for proximal convoluted tubular hyalinisation in renal tissue (p = 0.07). CONCLUSION: Based on these relationships and the nature of the chronic inflammation we conclude that the lesions were likely a result of recurrent infections and ageing but that long-term exposure to mercury could not be excluded as a co-factor. The information is important as it is likely that tropospheric mercury depletion events will continue to increase the concentrations of this toxic heavy metal in the Sub Arctic and Arctic marine food webs

Liquid state properties from first principles DFT calculations: Static properties

In order to test the Vibration-Transit (V-T) theory of liquid dynamics, ab initio density functional theory (DFT) calculations of thermodynamic properties of Na and Cu are performed and compared with experimental data. The calculations are done for the crystal at T = 0 and T_m, and for the liquid at T_m. The key theoretical quantities for crystal and liquid are the structural potential and the dynamical matrix, both as function of volume. The theoretical equations are presented, as well as details of the DFT computations. The properties compared with experiment are the equilibrium volume, the isothermal bulk modulus, the internal energy and the entropy. The agreement of theory with experiment is uniformly good. Our primary conclusion is that the application of DFT to V-T theory is feasible, and the resulting liquid calculations achieve the same level of accuracy as does ab initio lattice dynamics for crystals. Moreover, given the well established reliability of DFT, the present results provide a significant confirmation of V-T theory itself.Comment: 9 pages, 3 figures, 5 tables, edited to more closely match published versio