Temporal range: Late Miocene to recent
|Crabeater seal, Lobodon carcinophaga|
The true seal tribe Lobodontini, collectively known as the lobodontine seals, consist of four species of seals in four genera: the crabeater seal (Lobodon carcinophaga), the leopard seal (Hydrurga leptonyx), the Weddell seal (Leptonychotes weddelli), and the Ross seal (Ommatophoca rossii). All lobodontine seals have circumpolar distributions surrounding Antarctica. They include both the world's most abundant seal (the crabeater seal) and the only predominantly mammal-eating seal (the leopard seal). While the Weddell seal prefers the shore-fast ice, the other species live primarily on and around the off-shore pack ice. Thus, though they are collectively the most abundant group of seals in the world, the combination of remote range and inaccessible habitat make them among the least well studied of the world's seals.
The Lobondontini are thought to have diverged from the elephant seals (Mirounga) in the late Miocene or early Pliocene after moving southward from the Atlantic to the Southern Ocean. All species share teeth adaptations including lobes and cusps useful for straining smaller prey items out of the water (the name "Lobodontini", meaning "lobe-toothed"). Nonetheless, they have diversified into specialized prey ecological niches, thereby illustrating the radiating sympatric speciation associated with colonization of a novel environment with multiple available niches. Thus, the crabeater seal, with the most specialized sieve-like dental features, is the only seal that feeds predominantly on Antarctic krill, while the leopard seal is the only seal which actively preys on other seals and penguins, while still retaining the ability to filter-feed on krill.
The lobodontine seals in aggregate are among the most successful of all marine mammal groups, collectively accounting for at least 50% of all seals on Earth and about 80% of the global biomass of pinnipeds. The extremely high abundance of crabeater seals in particular, with possibly over 30,000,000 individuals, is a testament to the high productivity of the Southern Ocean, especially with respect to krill. High numbers of seals may also be the indirect result of the wide-scale extermination of large baleen whales in the Antarctic due to commercial whaling in the 19th and 20th centuries, and the subsequent increase in krill densities. Genetic evidence suggests that Weddell and crabeater seal populations may have increased in size during the Pleistocene. None of the four species is currently thought to be declining in numbers.
Crabeater seal (Lobodon carcinophaga)
Leopard seal (Hydrurga leptonyx)
Ross seal (Ommatophoca rossii)
Weddell seal (Leptonychotes weddellii)
- Wozencraft, W.C. (2005). "Order Carnivora". In Wilson, D.E.; Reeder, D.M. Mammal Species of the World: A Taxonomic and Geographic Reference (3rd ed.). Johns Hopkins University Press. ISBN 978-0-8018-8221-0. OCLC 62265494.
- Fyler, C.A.; Reeder, T.W.; Berta, A.; Antonelis, G.; Aguilar, A.; Androukaki, E. (2005), "Historical biogeography and phylogeny of monachine seals (Pinnipedia: Phocidae) based on mitochondrial and nuclear DNA data", Journal of Biogeography, 32: 1267–1279, doi:10.1111/j.1365-2699.2005.01281.x
- Boyd, I. (2009). "Antarctic Marine Mammals". In Perrin, W. F.; Würsig, B.; Thewissen, J. G. M. Encyclopedia of Marine Mammals (2nd ed.). Academic Press. pp. 30–36. ISBN 978-0-12-373553-9.
- Laws, R.M. Seals. In: Laws, R.M. (ed) Antarctic Ecology, Vol. 2, Academic Press, London, pp. 621-675
- Erickson, A. W., Siniff, D. B., Cline, D. R. and Hofman, R. J. (1971). Distributional ecology of Antarctic seals. In: G. Deacon (ed.), Symposium on Antarctic Ice and Water Masses, pp. 55-76. Sci. Comm. Antarct Res., Cambridge, UK.
- Mori, M.; Butterworth, D. (2006). "A first step towards modelling the krill-predator dynamics of the Antarctic ecosystem". CCAMLR Science. 13: 217–277.
- Curtis, Caitlin; Stewart, Brent S.; Karl, Stephen A. (2009-05-01). "Pleistocene population expansions of Antarctic seals". Molecular Ecology. 18 (10): 2112–2121. doi:10.1111/j.1365-294X.2009.04166.x. ISSN 1365-294X. PMID 19344354.