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We describe a new species of Polynesian sandpiper from Henderson Island, Prosobonia sauli sp. nov., based on multiple Holocene fossil bones collected during the Sir Peter Scott Commemorative Expedition to the Pitcairn Islands (1991–92). Prosobonia sauli is the only species of Prosobonia to be described from bone accumulations and extends the record of known extinct Polynesian sandpipers to four. It is readily differentiated from the extant Tuamotu Sandpiper P. parvirostris in several features of the legs and bill, implying ecological adaptations to different environments. The geographically nearest Prosobonia populations to Henderson Island were found on Mangareva, where it is now extinct. A previous record of a species of Prosobonia from Tubuai, Austral Islands, is here shown to belong to the Sanderling Calidris alba. Our analyses of newly sequenced genetic data, which include the mitochondrial genomes of P. parvirostris and the extinct Tahiti Sandpiper P. leucoptera, confidently resolve the position of Prosobonia as sister-taxon to turnstones and calidrine sandpipers. We present a hypothesis for the timing of divergence between species of Prosobonia and other scolopacid lineages. Our results further provide a framework to interpret the evolution of sedentary lineages within the normally highly migratory Scolopacidae.

Leucocarbo shags are a species-rich seabird clade exhibiting a southern circumpolar distribution. New Zealand's endemic Stewart Island shag, Leucocarbo chalconotus (G. R. Gray, 1845), comprises two regional groups (Otago and Foveaux Strait) that show consistent differences in relative frequencies between pied (black and white) and bronze (wholly dark) plumages, the extent and colour of facial carunculation, body size (based on postcranial morphometrics), and breeding season. Moreover, previous genetic research on modern and historical specimens utilizing mitochondrial DNA control-region sequences has also shown that the Otago and Foveaux lineages may not be sister taxa; instead, in several analyses the Otago lineage is sister to the endemic Chatham Island shag, Leucocarbo onslowi (Forbes, 1893). We present new ancient DNA analyses of the type specimens for the Otago and Foveaux Strait lineages of L. chalconotus, including a phylogenetic reanalysis of the available ancient, historical, and modern control-region sequence data for these lineages (including L. onslowi), and additional statistical analyses incorporating new morphometric characters. These analyses indicate that under the diagnosable species concept the two lineages of Stewart Island shag represent two separate species, which we now recognize as the Otago shag, L. chalconotus (G. R. Gray, 1845), and the Foveaux shag, Leucocarbo stewarti (Ogilvie-Grant, 1898).

Jamie R. Wood, Kieren J. Mitchell, R. Paul Scofield, Alan. J. D. Tennyson, Andrew E. Fidler, Janet M. Wilmshurst, Bastien Llamas, and Alan Cooper

The taxonomic affinities of the monotypic owl genus Sceloglaux Kaup, 1848 have been widely debated. Here, we present a high-coverage mitogenome for the sole member of the genus, New Zealand's extinct laughing owl (Sceloglaux albifacies Gray, 1845), and assess its phylogenetic relationships. Our results provide strong support for Sceloglaux being nested within Ninox Hodgson, 1837, as sister taxon to the clade containing the barking owl (Ninox connivens Latham, 1801), Sumba boobook (Ninox rudolfi Meyer, 1882), and morepork (Ninox novaeseelandiae Gmelin, 1788). Accordingly, we synonymize Sceloglaux with Ninox, and recommend that the laughing owl hereafter be referred to as Ninox albifacies. Osteological analyses and a comparison of the wing and leg proportions of the laughing owl with those of other owls supports Gould's (1865) contention that it was largely a terrestrial owl, and predominantly caught prey on the ground. This is further supported by the relatively high abundance of terrestrial prey remains preserved in sediment deposits at former laughing owl nest sites.

Although described as a distinct species in 1869, for more than a century now New Zealand's grey-faced petrel (Pterodroma macroptera gouldi Hutton, 1869) has been regarded as a subspecies of the great-winged petrel (P. macroptera A. Smith, 1840). However, several authors have recently questioned whether the taxon once again deserves full species status. Here, we demonstrate that the grey-faced petrel is sufficiently distinct in multiple facets of its biology (including mitochondrial DNA, plumage variation, morphometrics, osteology, vocalizations, external parasites, and feeding and breeding biology) to warrant reinstatement of full species status under the morphological, phylogenetic, and potentially biological species concepts. Moreover, we present new evidence from mitochondrial DNA (cytochrome c oxidase subunit 1 and cytochrome b) that suggests the great-winged petrel is actually more closely related to the white-headed petrel (Pterodroma lessonii Garnot, 1826) than to the grey-faced petrel. The reclassification of grey-faced petrel to full species status raises the degree of seabird endemism in New Zealand to 43%, emphasising the status of the archipelago as a hotspot for seabird diversity.