Duntroonornis parvus, also referred to as the Duntroon penguin, is a genus and species of extinct penguin from the Late Oligocene of New Zealand. The penguin was relatively small, similar in size to the Fiordland crested penguin. It was described by Brian Marples in 1952 from fossil material (a left tarsometatarsus) collected near Duntroon, from the Kokoamu Greensand Formation, near the border between the Canterbury and Otago regions of the South Island. Fossils found at the Hakataramea Valley may also be referrable to this species. The genus name Duntroonornis means "Duntroon bird". The specific epithet is the Latin parvus ("small").[2][3]
| Duntroonornis Temporal range: Late Oligocene,
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|---|---|
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Aves |
| Order: | Sphenisciformes |
| Family: | Spheniscidae |
| Genus: | †Duntroonornis Marples, 1952[1] |
| Species: | †D. parvus
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| Binomial name | |
| †Duntroonornis parvus Marples, 1952
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References
edit- ^ Marples, B.J. (1952). "Early Tertiary penguins of New Zealand". New Zealand Geological Survey, Paleontological Bulletin. 20: 42.
- ^ Gill, B.J. (Convener, OSNZ Checklist Committee) (2010). Checklist of the Birds of New Zealand, Norfolk and Macquarie Islands, and the Ross Dependency, Antarctica (4th ed.). Wellington: Te PaPa Press in association with the Ornithological Society of New Zealand. p. 329. ISBN 978-1-877385-59-9.
{{cite book}}: CS1 maint: multiple names: authors list (link) - ^ Miskelly, C.M. (2013). "Duntroon penguin". New Zealand Birds Online. Retrieved 24 May 2014.
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