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Phalacrocoracidae (3 Viewers)

Rawlence, N.J., A.T. Salis, H.G. Spencer, J.M. Waters, L. Scarsbrook, K.J. Mitchell, R.A. Phillips, L. Calderón, T.R. Cook, C.-A. Bost, L. Dutoit, T.M. King, J.F. Masello, L.J. Nupen, P. Quillfeldt, N. Ratcliffe, P.G. Ryan, C.E. Till, and M. Kennedy (2022)
Rapid radiation of Southern Ocean shags in response to receding sea ice
Journal of Biogeography (advance online publication)
doi: 10.1111/jbi.14360

Aim
Understanding how natural populations respond to climatic shifts is a fundamental goal of biological research in a fast-changing world. The Southern Ocean represents a fascinating system for assessing large-scale climate-driven biological change, as it contains extremely isolated island groups within a predominantly westerly, circumpolar wind and current system. Blue-eyed shags represent a paradoxical seabird radiation—a circumpolar distribution implies strong dispersal capacity yet their species-rich nature suggests local adaptation and isolation. Here we attempt to resolve this paradox in light of the history of repeated cycles of climate change in the Southern Ocean.

Location
Southern Ocean.

Taxa
16 species and subspecies of blue-eyed shags (Phalacrocoracidae; Leucocarbo spp.).

Methods
We use mitochondrial and nuclear sequence data from individuals across the geographical range of the genus to conduct the first comprehensive, time-calibrated phylogenetic analyses and ancestral-range biogeographical reconstructions of the blue-eyed shags.

Results
The origins of many island-endemic lineages are remarkably recent, consistent with a recent high-latitude circumpolar radiation in the Pliocene or Early Pleistocene. This recent sub-Antarctic expansion contrasts with significantly deeper lineages detected in South America and, to a lesser extent, New Zealand. These regions, particularly South America, acted as glacial refugia and sources for multiple waves of post-glacial dispersal.

Main conclusions
The blue-eyed shag paradox is resolved, with at least two waves of dispersal, linked to interglacial cycles, explaining the current distribution and diversity. Descendants of a Pliocene or Early Pleistocene wave of dispersal out of South America survive in the New Zealand region. In contrast, taxa distributed on sub-Antarctic islands originated much later, possibly since the Last Glacial Maximum. Blue-eyed shags therefore represent a powerful model system—comprising several natural replicates—for studying the early stages of founder-event speciation and adaptation in a Southern-Ocean bird group.
 
Martyn Kennedy, Alexander T Salis, Sampath S Seneviratne, Dilini Rathnayake, Lisa J Nupen, Peter G Ryan, Stefano Volponi, Pascale Lubbe, Nicolas J Rawlence, Hamish G Spencer. Phylogeny of the microcormorants, with the description of a new genus, Zoological Journal of the Linnean Society, 2023;, zlad041, Phylogeny of the microcormorants, with the description of a new genus


Abstract
The aptly named microcormorants (currently placed in the genus Microcarbo) form a morphologically diminutive and distinct clade sister to all other living cormorants and shags. However, the relationships within Microcarbo are largely speculative. Sequence data resolve these relationships unambiguously, with our phylogeny suggesting that the microcormorants separated from the other cormorants ~16 Mya and showing that the two African species [the reed (or long-tailed) cormorant, Microcarbo africanus, and the crowned cormorant, Microcarbo coronatus] are closely related sister taxa, forming a clade that diverged from the other microcormorants ~12 Mya. The deep split between the African microcormorants and the others is considerably older than many well-recognized generic splits within the cormorants (e.g. Leucocarbo and Phalacrocorax). Thus, we suggest that the African microcormorants warrant their own genus, and we erect Afrocarbo, with type species Pelecanus africanus. Within the reduced Microcarbo, we estimate that the little pied cormorant (Microcarbo melanoleucos of Australasia) separated from the sister pair of the Javanese and pygmy cormorants (respectively, Microcarbo niger from south/southeast Asia and Microcarbo pygmaeus from Europe) ~9 Mya and that the latter two species split ~2 Mya. Given the age of these splits, the microcormorants appear to represent another example of morphological conservatism in the Suliformes.
Genus Afrocarbo gen. nov
Type species: Pelecanus africanus Gmelin, 1789.

Diagnosis:
Small cormorants, with relatively short bills and long tails. They differ from the similarly proportioned Microcarbo (type species Pelecanus pygmaeus Pallas) in the adult possessing a more extensive area of bare skin on the face from the eye forwards in addition to under the bill, with prebreeding birds having a more obvious forehead crest and a red iris (dark brown or green in Microcarbo).

Included species:
Afrocarbo africanus (Gmelin, 1789) and Afrocarbo coronatus (Wahlberg, 1855).

Etymology:
The name refers to the African distribution of the included species. Gender masculine.
 
H&M online checklist footnote says:
Original spelling pygmeus was an incorrect Latin spelling; and spelling pygmaeus in Dorst & Mougin (1979) a justified emendation contra Dickinson & Remsen (2013)
 

I never really understood it either.

As Mike indicate above, pygmeus has been deemed to be a misspelled classical Latin word, and to be corrected on this base. Classical Latin dictionaries list only pygmaeus, indeed -- but pygmeus is a common spelling in post-classical Latin texts and, in my opinion, can not really be called an inadvertent error.
If we are to do this type of thing, should we not also immediately "correct" all these awful "littoralis" (a variant of litoralis, not listed in classical Latin dictionaries either), that are found all over the place in our nomenclature...?

(Note that the spelling of Platalea pygmea Linnaeus 1758 (now in Calidris) was similarly "corrected" to pygmaea on the Official List, without any comment or justification (Op. 67, Dir. 43).)
 
"Microcarbo pygmaeus" one reason is that Bonaparte spelled the species that way in the OD of Microcarbo??
t.43 (1856) - Comptes rendus hebdomadaires des séances de l'Académie des sciences - Biodiversity Heritage Library .

No, the reason is really only this : Latin Dictionary Headword Search Results
(But see this : pygmeus - Wiktionary, the free dictionary )

I would understand correcting an actual inadvertent misspelling -- e.g., 'pygmeaus' or 'pgymaeus' instead of pygmaeus. I have a much harder time with what was done here. Particularly as the use of the OS had become almost universal in the early 2000s, just before it happened...
 
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Not in the Phalacrocoracidae, but there is also Eurynorhynchus pygmeus (Spoon-billed Sandpiper). As far as I can see from my collection of data, it has never been "corrected" to pygmaeus.
 
Yes, it's now in Calidris, feminine, hence pygm[a]ea, not pygm[a]eus... and Clements and BirdLife, in any case, both switched to an -ae- spelling and broadened the genus Calidris to include this species simultaneously.
 
Theodore E. Squires and Alexander L. Bond (2024) Specimens of the extinct Spectacled Cormorant Urile perspicillatus. Bulletin of the British Ornithologists’ Club 144: 3-18.
Specimens of the extinct Spectacled Cormorant Urile perspicillatus

Abstract
In 1741, after reaching Alaska from eastern Russia and exploring the Aleutian Islands, the naturalist Wilhelm Steller became shipwrecked along with the rest of Vitus Bering's crew. During his struggle to ward off starvation on the unmapped Commander Islands, Steller discovered what would eventually be confirmed as the world's largest cormorant. Decades later, Peter Simon Pallas recognised the bird described in Steller's journal as a new species, naming it Phalacrocorax perspicillatus (now Urile perspicillatus) in his Zoographia Rosso-Asiatica. Within 41 years of its listing in the scientific literature, Leonhard Stejneger declared the cormorant had become extinct after finding only bones on Bering Island and conferring with indigenous Unangas regarding its decline. Here, we present an inventory of all known specimens (skins and osteological) of this poorly known seabird. There are six skins in four institutions and osteological material in four. Previous references to specimens in Senckenberg Natural History Collections, Dresden, and the American Museum of Natural History, New York, are incorrect. The original source of the skins remains elusive, but they all passed through Sitka, the then-capital of Russian America. All osteological specimens are from the species' only known breeding site, Bering Island in the Commander Islands.
 

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