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Crabeater seal
The crabeater seal (''Lobodon carcinophaga'' or ''carcinophagus'') is a true seal with a circumpolar distribution around the coast of Antarctica. They are medium- to large-sized (over 2 m in length), relatively slender and pale-colored, found primarily on the free-floating pack ice that extends seasonally out from the Antarctic coast, which they use as a platform for resting, mating, social aggregation and accessing their prey. They are by far the most abundant seal species in the world. While population estimates are uncertain, there are at least 7 million and possibly as many as 75 million individuals. This success of this species is due to its specialized predation on the abundant Antarctic krill of the Southern Ocean, for which it has uniquely adapted, sieve-like tooth structure. Indeed, its scientific name, translated as "lobe-toothed (''lobodon'') crab eater (''carcinophagus'')", refers specifically to the finely lobed teeth adapted to filtering their small crustacean prey.〔Bengtson, J. A. (2002). Crabeater seal ''Lobodon carcinophaga''. In: W. F. Perrin, B. Wursig, and J. G. M. Thiewissen. (eds), Encyclopedia of marine mammals, pp. 302-304. Academic Press, London, UK.〕 Despite its name, crabeater seals do not eat crabs. As well as being an important krill predator, the crabeater seal is an important component of the diet of leopard seals (''Hydrurga leptonyx''), which consume about 80% of all crabeater pups.
== Taxonomy and evolution ==
The crabeater seal shares a common recent ancestor with the other Antarctic seals, which are together known as the lobodontine seals. These include the Ross seal (''Ommatophoca rossii''), leopard seal (''H. leptonyx'') and Weddell seal (''Leptonychotes weddelli''). These species, collectively belonging to the Lobodontini tribe of seals, share teeth adaptations including lobes and cusps useful for straining smaller prey items out of the water column. The ancestral Lobodontini likely diverged from their sister clade, the Mirounga (elephant seals) in the late Miocene to early Pliocene, when they migrated southward and diversified rapidly in relative isolation around Antarctica.〔
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