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Imperial shag

Species of bird

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Through South America, Taxonomy (biology) and Binomial nomenclature

Taxonomy

The imperial shag was formally described in 1828 by the Royal Navy officer Phillip Parker King based on a specimen that he had collected in the Strait of Magellan of southern Chile. He placed the species in the genus Phalacrocorax and coined the binomial name Phalacrocorax atriceps, where the specific epithet combines the Latin ater meaning "black" with -ceps meaning "-capped" or "-headed". The imperial shag was formerly usually retained in the genus Phalacrocorax, but has also sometimes been placed in its own genus Notocarbo. Based on a comprehensive molecular phylogeny of the cormorant family Phalacrocoracidae by Martyn Kennedy and Hamish Spencer that was published in 2014, the imperial shag is now one of nine species placed in the genus Leucocarbo that had been introduced by the French naturalist Charles Lucien Bonaparte in 1856.

Eight subspecies are recognised:

While some authorities consider all of the above — except albiventer — as separate species, others consider all as subspecies of a single species (as done in this article). Alternatively, some recognize two species, the white-cheeked L. atriceps (with subspecies bransfieldensis, nivalis and georgianus) and the black-cheeked L. albiventer (with subspecies melanogenis and purpurascens), or it has been suggested that three species should be recognized: L. atriceps (including albiventer), L. georgianus (with subspecies bransfieldensis and nivalis), and L. melanogenis (with subspecies purpurascens and possibly verrucosus, though the latter is more distinctive, and most consider it a separate species, the Kerguelen shag).

All these taxa are now treated as subspecies of the imperial shag based on a molecular phylogenetic study by Nicolas Rawlence and collaborators that was published in 2022. The authors found that despite their sedentary behaviour and the wide separation between the breeding colonies on the subantarctic islands, the genetic differences are small suggesting a circumpolar dispersal from South America after the Last Glacial Maximum around 21 thousand years ago.

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