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The Chionoidea are a small, southern hemispheric shorebird clade that today includes the Magellanic Plover (Pluvianellidae) and two species of sheathbills (Chionidae). Here we describe the first fossil remains attributable to this group. The two newly described species, the early Miocene Neilus sansomae gen. et sp. nov. from New Zealand and the late Oligocene Chionoides australiensis gen. et sp. nov. from South Australia, are overall more similar to sheathbills, but the mosaic of characters shared with both Chionidae and Pluvianellidae preclude referral to either lineage. Attribution of fossils this age to these lineages also conflicts with divergence dates based on molecular data, as the split between the Magellanic Plover and sheathbills is hypothesised to be more recent. We therefore suggest that these Australasian, plover-size species represent the first record of stem-group taxa within Chionoidea.http://zoobank.org/urn:lsid:zoobank.org:pub:2A5A2FD1-C3B5-4BAB-88D8-5862FE9E7976

Cyanoramphus parakeets are a key biogeographic element of the Pacific. Many of these parakeets are, however, endangered, with ongoing conservation management hampered by the unresolved taxonomic status of some populations. We used modern and ancient DNA (mitochondrial DNA control region) to assess the taxonomy of the Auckland Islands populations of red-crowned (Cyanoramphus novaezelandiae novaezelandiae) and yellow-crowned (Cyanoramphus auriceps) parakeets. Our analyses show that both red-crowned and yellow-crowned parakeets on the Auckland Islands are nested within the mainland New Zealand diversity of the two species. However, we also found an orange-fronted parakeet (Cyanoramphus malherbi) mitochondrial DNA lineage within the genome of both of these species in the Auckland Islands population. Further sampling of historic orange-fronted parakeet museum skins showed that the orange-fronted morphotype is paraphyletic with respect to mitochondrial haplotype, which is probably caused by hybridisation or inc...

Historical museum skins are an important genetic resource for taxonomic, phylogeographic and conservation genetic research. However, their utility can be compromised by errors in specimen labels concerning taxonomic identity, collection locality and collector. Here we use morphological comparisons and ancient DNA analysis to show that two Auckland Island Shags (Leucocarbo colensoi) in the Sir Walter Buller collection of the Canterbury Museum, New Zealand, are mislabelled. Given that Buller was able to identify these taxa prior to their supposed collection dates, it suggests erroneous labelling and/or poor record keeping. Despite the importance of Buller's collections for ornithological research, our findings reinforce previous conclusions that caution is required when utilising these avian specimens.

The first pre-Quaternary anurans from New Zealand are reported from the Early Miocene (19–16 Ma) St Bathans Fauna based on 10 fossil bones. Four bones representing two new species differing in size are described in Leiopelma: Leiopelmatidae, and are the first Tertiary records for the family. Six indeterminate frog fossils are morphologically similar to leiopelmatids and represent two species consistent in size with those known from diagnostic material. These records are highly significant, as minimally, they reduce the duration of the leiopelmatid ‘ghost lineage’ by c.20 million years and demonstrate that a diversity of leiopelmatids has long been present on New Zealand, supporting the ancient dichotomy of the extant species based on molecular data.Leiopelma miocaenale Worthy, Tennyson, Scofield & Hand in pressurn:lsid:zoobank.org:act:83F24868-A212-435B-B892-AD510796B5BBLeiopelma acricarina Worthy, Tennyson, Scofield & Hand in pressurn:lsid:zoobank.org:act:D3955F53-37C2-4EAD-B0BC-CE8D23FCD51B

Herons (Aves: Ardeidae) are rare in the fossil record globally. Fossil taxa referred to Ardeinae and Nycticoracini are known from as early as the early Oligocene and ardeids undetermined to subfamily include some as old as the early Eocene. In Australasia, the pre-Pliocene record is restricted to one species from the early Miocene of New Zealand. On the basis of a tarsometatarsus and a coracoid we describe a new species of bittern (Ardeidae: Botaurinae) from the St Bathans Fauna, of early Miocene age, from Otago, New Zealand. This is only the third and the oldest pre-Quaternary record for Botaurinae globally.

Holocene New Zealand sea lion (Phocarctos hookeri) bones collected from the north of New Zealand's South Island strengthen existing evidence for the former Holocene presence of breeding colonies of P. hookeri on mainland New Zealand. The taxonomic identity of Phocarctos bones is confirmed using both morphology and ancient DNA analysis. Five radiocarbon dates on four adult and one pup bone from Creighton's Cave near Paturau, northwest Nelson, ranged from 1290±30 yr BP to 5430±30 yr BP. Three radiocarbon dates on pup bones spanning 200 14C yr (1550±30 yr BP to 1390±30 yr BP) reveal that a prehistoric breeding rookery was present at Delaware Bay, Nelson, until shortly before the time of human arrival c. AD 1280 (670 yr BP). The Delaware Bay site in particular provides a valuable ‘snapshot’ of coastal New Zealand faunas shortly before human arrival, one that has potential to enhance our understanding of changes in the endemic coastal fauna associated with human colonisation.

The ratite moa (Aves: Dinornithiformes) were a speciose group of massive graviportal avian herbivores that dominated the New Zealand (NZ) ecosystem until their extinction ≈600 years ago. The phylogeny and evolutionary history of this morphologically diverse order has remained controversial since their initial description in 1839. We synthesize mitochondrial phylogenetic information from 263 subfossil moa specimens from across NZ with morphological, ecological, and new geological data to create the first comprehensive phylogeny, taxonomy, and evolutionary timeframe for all of the species of an extinct order. We also present an important new geological/paleogeographical model of late Cenozoic NZ, which suggests that terrestrial biota on the North and South Island landmasses were isolated for most of the past 20–30 Ma. The data reveal that the patterns of genetic diversity within and between different moa clades reflect a complex history following a major marine transgression in the Oligocene, affected by marine barriers, tectonic activity, and glacial cycles. Surprisingly, the remarkable morphological radiation of moa appears to have occurred much more recently than previous early Miocene ( ca. 15 Ma) estimates, and was coincident with the accelerated uplift of the Southern Alps just ca. 5–8.5 Ma. Together with recent fossil evidence, these data suggest that the recent evolutionary history of nearly all of the iconic NZ terrestrial biota occurred principally on just the South Island.

Magenta Petrels Pterodroma magentae were caught at light-attraction stations on southwest Chatham Island, New Zealand, and most were fitted with transmitters. Of 52 captured since 1993, 71% were males, and all 36 tracked adequately proved to be non-breeders in the breeding season of capture. Our data indicated no sex bias in their probability of being captured at lights. Males provided 86% of trackings, and 87% of trackings of birds flying over the breeding area were males. Males landed 118 times; females 13 times. Only males were found on the ground, by night and day, apparently unassociated with burrows (three with and ten without transmitters), but subsequently digging burrows (n = 8). Of 19 birds banded as fledglings up to 2000, males were first recaptured nearing 4 years old [at lights and on the ground) and a female nearing 6 years old (in burrow). Among 37 fledglings, the sex ratio was even. Nine tracked males occupied burrows, as did two females, but the latter were older recaptures (10+ and 25+ years old). It appears that only males claimed existing, or dug new, burrows. They then attracted a mate to the burrow by means unknown, but from among females frequenting an inshore courtship area near the colony, or occasionally flying over the colony, at night. Females established in burrows, but then losing their mate, were able to re-mate there, by calling from near the burrow or by attracting a mate in flight or from the postulated inshore courtship area. Both sexes sometimes took years to pair or re-mate, possibly reflecting the dearth of available mates.