Tag Archives: Fossils

Using DNA forensics to determine the past distribution of the brown kiwi species rowi.

Yesterday was a special day for 20 rowi (a species of the flightless kiwi) who were flown from the South Island to their new home on Mana Island, near Wellington. It was reported that this was the first time that this species of kiwi had been in the North Island for over a century.

So how do we know that rowi used to be in the North Island?

Kiwi researcher Kristina Ramstad holding a rowi. Photo by Rachael Abbott.

Kiwi researcher Kristina Ramstad holding a rowi. Photo by Rachael Abbott.

Today kiwi are absent from large areas of New Zealand, including the southern North Island (North Island brown kiwi occur from the central North Island northwards).  We know that kiwi used to occur in the southern North Island because their bones have been found in caves and other deposits.  However, trying to identify kiwi species just by looking at the shape and size of their bones is tricky.

Little spotted kiwi is the only species that can be identified from its bones because they are much smaller than the other kiwi species.  The bones of great spotted kiwi and the three species of brown kiwi (rowi, North Island brown kiwi and tokoeka) can’t be identified to species because they overlap in size and shape.

This is the kind of puzzle that DNA can solve. As part of my PhD I examined the past distribution of each kiwi species by sequencing DNA from kiwi bones that had been collected from throughout New Zealand.  Some of these bones were up to several thousand years old, but they still contained small amounts of DNA!

Surprisingly I found that the bones in the southern North Island were most closely related to rowi, rather than the geographically closer North Island brown kiwi.  Today rowi only naturally occur in one small population at Okarito on the West Coast of the South Island and they are the rarest species of  kiwi.  My DNA work showed that they used to occur as far north as the southern Hawke’s Bay. You can read the published results here.

Fossils uncovered!

Sphenodontid

Sphenodontid, collected 13 Dec 2001, St Bathans. Vinegar Hill, Site 1, New Zealand. Field Collection 2002-2004. Te Papa.

Normally fossils are found in the field but in this case Te Papa technicians and I have been rediscovering an early accumulation of fossil reptiles and fish held in Te Papa’s collections that have not been examined for decades.

When the Colonial Museum opened in 1865, the Director James Hector, wanted to show New Zealanders natural wonders from around the world, so he set about acquiring all sorts of natural history objects from museums in other countries. Some spectacular fossils were among his acquisitions and Te Papa still has these today.

The fossils that we have now registered and re-housed include skulls and teeth of long extinct reptiles – ichthyosaurs (“fish lizards”) and plesiosaurs (think Loch Ness Monster) – as well as remains of ancient fish – particularly shark’s teeth.

Plesiosauria

Plesiosauria, collected Lyme Regis, Dorset, England. Te Papa.

Dozens of the ichthyosaur, plesiosaur and fish remains originate from the Jurassic Lyme Regis fossil beds in Dorset, England. This site is one of the most famous fossil localities in the world because the giant reptile remains found here in the early 1800s, most famously by Mary Anning, were clearly of extinct species – yet at the time the concept of extinction was virtually unheard of. Dinosaurs, for example, were only discovered later. Te Papa’s fossil reptile and fish collection also includes more recently acquired specimens, such as dinosaur footprint casts from North America, dinosaur eggs and fragments of a 19 million year old ancestral tuatara from Central Otago.

Te Papa’s Natural Environment Imaging Supervisor Jean-Claude Stahl has been photographing many of these fossils and examples of them are shown here. Many others can be accessed through Te Papa’s Collections On-line browser.

Fossils in Te Papa’s Collections Online

Posted by Alan Tennyson, Curator of Fossil Vertebrates

Tales from Te Papa: Iguanodon tooth

In 1825, Gideon Mantell described fossil teeth and bones from a quarry near Cuckfield in Sussex, England. He named these remains ‘Iguanodon’ meaning ‘having teeth like those of an Iguana’ (a lizard), but he correctly determined that they were quite unlike the teeth of any known lizard or mammal.

He is credited with being the first person to recognise the prior existence of a group of animals that were neither mammal nor lizard and that were subsequently named ‘dinosaurs’ in 1842 (by Richard Owen).

Dr Hamish Campbell writes about Gideon Mantell below:

Gideon Mantell (1790-1852) lived in Lewes near Brighton where he practised as a doctor. He enjoyed a reputation as an outstandingly successful obstetrician; very few mothers or babies lost their lives due to childbirth when he was involved. He was highly intelligent, well-educated and a skilled artisan. However, to the detriment of his marriage (1816-1839) to Mary Anne, he developed an abiding interest in natural history and, in particular, paleontology.

The Country of the Iguanodon, 1837 by John Martin (1789–1854), watercolour. Gift of Mrs Mantell-Harding, 1961. Image © Te Papa.

The Country of the Iguanodon, 1837 by John Martin (1789–1854), watercolour. Gift of Mrs Mantell-Harding, 1961. Image © Te Papa.

On his death, his sons inherited his estate but it was the younger Walter Mantell who ultimately acquired many of his father’s fossil collections, including the famous ‘Iguanodon tooth’ that resides here at Te Papa.

Walter first came to New Zealand in 1839 with the New Zealand Company. He was to spend much of his adult life here and played a significant role in the early colonial development of New Zealand, including the establishment of the Colonial Museum, the original fore-runner to Te Papa. Many descendents of Walter Mantell reside in New Zealand to this day.

The deluge and the ark

The lower jaw of a tuatara (sphenodon). Three teeth are visible along the top. This was the first fossil bone found at St Bathans. Image copyright Te Papa

Recently, a group of researchers in New Zealand suggested that the absence of fossils between 25 and 22 million years ago indicated that the islands completely disappeared under water, and then later re-emerged. But a newly discovered fossil reptile suggests this theory does not hold water. Alan Tennyson, Curator of Fossil Vertebrates at Te Papa, and colleagues, found the remains of a fossilized reptile jaw at St Bathans in Otago.

Curator of Fossil Vertebrates, Alan Tennyson, excavating the St Bathans site in Otago. Image copyright Te Papa

Curator of Fossil Vertebrates, Alan Tennyson, excavating the St Bathans site in Otago. Image copyright Te Papa

The teeth in the fossil jaw and their wear patterns is unique to the tuatara and its ancestors. But what is most exciting about Alan’s fossil is its age: it dates to just 3 million years after a time when other researchers have suggested the land mass sank beneath the waves.

After the ancestral New Zealand continent broke away from Australia and Antarctica, it drifted northwards and, due to a combination of tectonic movements and rising sea-levels, the total land area shrank considerably, but just how small the land area was reduced to is open to debate.

If the entire land area was submerged, the ancestral tuatara discovered by Alan and his colleagues, and all of New Zealand’s biodiversity, could only have arrived after the land re-emerged. To do this, the ancient reptile would have had to cross vast oceans – an unlikely feat for an animal that is a poor swimmer that would have rapidly dehydrated in salt water.

It’s not just the tuatara fossil that suggests New Zealand did not fully drown.

There are many different species in the St Bathans fossil deposit – about 24 species of birds, as well as plants, insects, and freshwater fish. There is no evidence that these species lived in Australia at the time, and most would not have been able to survive a lengthy sea journey. This suggests that ancient New Zealand did not disappear, but remained as an isolated island chain, allowing many species to survive and then repopulate as the continental crust re-emerged.

Reference: Jones, M, E.H.; Tennyson, A.J.D.; Worthy, J.; Evans, S.E.; Worthy, T.H. (2009). A sphenodontine (Rhynchocephalia) from the Miocene of New Zealand and paleobiogeography of the tuatara (Sphenodon). Proceedings of the Royal Society B

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