The discovery of four new species of fossil penguins in New Zealand in 2025 sheds light on the long evolutionary journey of these captivating birds. Each fossil provides valuable insights into the environmental factors that influenced penguin evolution, from changes in habitat to climate. By piecing together these fossils, scientists can reconstruct the stages of development that led to the diverse penguins we know today, offering a glimpse into their evolutionary history. Additionally, studying these ancient penguins helps researchers understand their behavior, feeding habits, and adaptations to their environment. The unique geological history of New Zealand makes the study of fossil penguins particularly significant, providing a glimpse into how these birds have evolved and adapted over millions of years. Overall, the discovery of these new species is a thrilling find that contributes to our understanding of penguins and the natural world as a whole.
The question of penguin origins has long centered on New Zealand because the oldest known penguin fossils come from there. The islands sit on Zealandia, a largely submerged microcontinent that separated from Australia and Antarctica during the Cretaceous Period. Its geographic isolation, and the near-absence of native land mammals, meant birds dominated the ecosystem for tens of millions of years conditions that appear to have allowed early penguins to diversify with relatively few terrestrial threats.
Before the recent surge in fossil collection, the early stages of penguin evolution were understood in broad outline: the birds lost flight early in the Paleocene, probably filling marine niches left by the extinction of aquatic reptiles at the end of the Cretaceous, around 66 million years ago. What was less clear were the intermediate anatomical steps between a diving seabird and the upright, flipper-propelled animals seen today.
Excavations at the Waipara Greensand formation on New Zealand’s South Island have produced the bulk of the new material. The rock unit formed in shallow ocean waters a few million years after the Cretaceous mass extinction and is exposed along riverbeds and streambeds on the Canterbury Plains. Researchers have collected fossil bones from quarries, river cuts, and beachside cliffs, then prepared them by removing surrounding rock — in some cases from concretions, rounded stone structures that form around bones during sediment hardening. Digital laser scans of key specimens allowed comparative measurements against modern penguins and other diving birds.
The oldest species yet identified, Daniadyptes primaevus, is known only from a few flipper and leg bones, leaving much of its appearance uncertain. From the available material, researchers estimate it stood roughly one-third of a meter tall. Its bone density indicates it was already flightless. Daniel Ksepka, a paleontologist at the Bruce Museum who has worked extensively on New Zealand fossil penguins, notes that its estimated weight places it only slightly above the theoretical upper size limit for birds capable of both aerial and underwater wing-propelled flight — consistent with it representing a very early stage in the transition away from flight.
The Waipara fossils as a group show anatomical features that differ from modern penguins in several respects. Their beaks were notably elongated, which researchers have interpreted as suited to spearing large prey near the water’s surface — a method that requires surfacing to swallow. Their wing bones were longer, less flattened, and more flexible than those of modern penguins, and the joints allowed folding, something modern penguins cannot do. The lower-back vertebrae show flat joint surfaces similar to flying birds, rather than the ball-and-socket joints of later penguins. The tail bone, or pygostyle, was plate-shaped rather than the nearly triangular form seen in modern species. These birds likely walked with a forward-leaning posture rather than the upright waddle of living penguins.
Among the most studied later fossils is Kumimanu fordycei, named in 2023 and estimated to have lived approximately 58 million years ago. Using regression calculations based on humerus proportions the upper wing bone being nearly as long as that of an adult human the research team estimated its mass at around 155 kilograms, making it the largest penguin species yet documented. Ksepka and colleagues speculated that reaching such body sizes may have provided a thermoregulatory advantage. Early penguins, based on traces of blood vessels in fossilized bone, appear not yet to have evolved the countercurrent heat-exchange systems that modern penguins use to conserve body heat in cold water. Larger body mass reduces heat loss through scaling effects, which the researchers suggested could have enabled dispersal from Zealandia into colder Southern Hemisphere regions. They note this hypothesis is consistent with the fact that the earliest known penguin fossils from outside New Zealand found in 55-million-year-old Antarctic rocks also belong to large-bodied species. The researchers describe this as a speculative hypothesis, not a confirmed mechanism.
Giant penguins disappeared globally around 20 million years ago, with the last known large species persisting in Australia until roughly 15 million years ago. Paleontologists have proposed that the spread of pinnipeds seals, sea lions, and relatives through the Southern Hemisphere may have driven the giants out through food competition and displacement from breeding grounds, but the cause remains unresolved.
More recent fossil layers in New Zealand, dating to around three million years ago, have produced close relatives of modern species. A 2025 paper led by Alan Tennyson of Te Papa Tongarewa reported a fossilized skull from the Taranaki region of the North Island that researchers provisionally identified as likely belonging to Aptenodytes ridgeni a species previously known only from leg bones and ribs found in 1968. The skull is larger than that of a modern emperor penguin, with a longer, more robust beak. Because the skull was found in isolation, the species assignment is uncertain, as Ksepka acknowledges: “I speculate it represents the long-sought skull of Aptenodytes ridgeni.” The surrounding sediments date to the middle Pliocene, when New Zealand had subtropical ocean temperatures 10 to 20 degrees Celsius warmer than the Antarctic and subantarctic waters modern emperor and king penguins inhabit. The species did not survive to the present. The research team speculated without direct fossil evidence that foot-brooding behavior similar to that of modern Aptenodytes species may have left adults exposed to large raptors that arrived in New Zealand around two million years ago.
A contrasting pattern was found in Eudyptula wilsonae, a small fossil penguin reported in 2023, weighing under one kilogram and standing 0.3 meters tall. Its skull closely resembles those of two living species, the little penguin and the fairy penguin, except for a more slender beak, leading researchers to suggest it may be ancestral to both. The team speculated that burrowing nesting behavior and coming ashore at dusk behaviors shared with its modern relatives may have helped this genus avoid the large diurnal raptors that appear to have contributed to the disappearance of Aptenodytes from Zealandia.
Not all penguin extinctions in New Zealand trace to natural causes. DNA extracted from bones found in Chatham Islands dunes confirmed in a 2019 study that a genetically distinct crested penguin, named Eudyptes warhami, once bred there. Bones of the species appear in middens archaeological deposits containing food remains and radiocarbon dating places the youngest specimens at approximately 1500 CE, roughly coinciding with the first known human settlement of the Chatham Islands. Ksepka notes the timing suggests rapid extinction through hunting, “perhaps within a single generation.”
A limitation running through much of this work is the fragmentary nature of many specimens: several species are known from only partial skeletons, and behavioral inferences particularly for nesting and thermoregulation are drawn by analogy with living relatives rather than from direct fossil evidence. The causes of the giant penguin extinction and the disappearance of A. ridgeni specifically remain open questions.
References:
- Ksepka, D. T., et al. (2023). A giant stem penguin from the Paleocene of New Zealand (Kumimanu fordycei).
Journal of Paleontology / Alcheringa (Taylor & Francis) - Thomas, D. B., et al. (2023). A new species of small-bodied penguin (Eudyptula wilsonae) from New Zealand.
Journal of Vertebrate Paleontology - Tennyson, A. J. D., et al. (2025). A fossil skull of a large penguin (cf. Aptenodytes ridgeni) from the Pliocene of New Zealand.
Records of the Museum of New Zealand Te Papa Tongarewa - Cole, T. L., et al. (2019). Ancient DNA reveals extinct crested penguin (Eudyptes warhami) from the Chatham Islands.
Proceedings of the Royal Society B - Mayr, G., et al. (multiple years). Early Paleocene penguins from the Waipara Greensand, New Zealand.
Various publications (e.g., Alcheringa, Paleontological journals)
