Free preview Natural history and biodiversity

Geology and deep history

📄 Introduction

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Aotearoa New Zealand’s culture is a product of a shared natural heritage, rich cultures, complex history, and objects and art that come together to inform our cultural identity.

Te Papa Tongarewa, the National Museum of New Zealand, is a unique place - part natural history museum, part museum, and part gallery - that preserves many of the stories that make up the narrative and shared identity of Aotearoa New Zealand. Its name, in its full Māori interpretation, means ‘our container of treasured things and people that spring from mother earth in New Zealand’.

Over a series of short units, we will peer into that container, and gain an insight into the breadth of Aotearoa New Zealand’s culture, history, and identity through the objects and stories that Te Papa stewards.

##Shaky isles

In this first unit, we will focus on the natural history of Aotearoa New Zealand; the geographical story that started 85 million years ago with continental plates, and continues today with earthquakes and volcanic activity.

This story dictated the unique biodiversity that makes Aotearoa the closest thing on Earth to looking at life in a parallel universe. We will see how the arrival of humans and other creatures to this land in more recent times has changed that story dramatically, and how present and future New Zealanders share a responsibility to protect the irreplaceable taonga (treasures) of this whenua (land).

##What to expect

We will begin with the continental and tectonic forces that formed this land as it broke away from Gondwanaland, sank almost completely beneath the waves then re-emerged, thrust upwards under the violent forces of immense tectonic plates colliding with one another. Then we will look at the creation of Lake Taupō by the supermassive volcano that still lurks smouldering beneath it.

Next we will touch on how mātauranga Māori (Māori knowledge) connects with these wild forces through the legend of Rūaumoko, god of earthquakes and volcanoes.

But before we get into it and immerse ourselves in what it means to be of this whenua (land) we call Aotearoa, the land of the Long White Cloud, let’s get to know each other!

###Introduce yourself in the comments, who are you, where are you from and why are you interested in this course?

Write your own comment, and respond to someone else, too.

📄 Prehistoric New Zealand

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In 2017, Earth's newest continent was declared. Long considered part of the Australian continent, [Zealandia](https://blog.tepapa.govt.nz/2017/06/01/a-right-continental-fuss-zealandia-explained/) was declared a distinct landmass, one that separated from the Gondwanaland supercontinent [85 million years ago](https://teara.govt.nz/en/evolution-of-plants-and-animals/page-2).

When Zealandia broke away from Gondwanaland, several species of dinosaur and their aquatic cousins, mosasaurs and plesiosaurs, came along for the ride. But that is just the beginning of the story; the land continued (and continues) to morph dramatically into the country we recognise as Aotearoa New Zealand today.

####Watch this video from The New Zealand History show for an introduction to both the very beginning of our story, and to some of the content we will consider more deeply throughout the rest of this course.

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###Transcript for the video above:

*Kia ora, I'm William Ray. Kia ora, I'm Leigh-Marama McLachlan and this is the Aotearoa History Show.*

*Over the next fourteen episodes we're going to run you through the story of these islands and their people. Lots of us go through life knowing bugger all about our past and if you don't know what's happened back in the day, you're going to have a really hard time understanding why things are the way they are now.*

*So that's where William and I come in. This show is going to reveal our history, warts and all. Some bits will make you super proud, others might make you feel pretty rubbish. Our history isn't just important, it's also super interesting.*

*We'll look at what the country was like before people arrived, the treaty those people signed, the wars they fought, and the people who led the way. Explorers. Innovators, prophets, warriors, diplomats. There's a lot of crazy stuff and we're gonna take you through everything. We don't have time for everything. We're gonna take you through most of the important stuff. That sounds pretty doable. But we have to meet you back here right after the titles.*

*“Whatungarongaro te tangata, toitū te whenua”, “people will perish but the land is permanent”. This is a whakataukī, a Māori saying, it symbolizes the importance of Papatūānuku, our land. Over the series we'll talk about the generations of people who have come and gone but first we need to tell the story of the land that sustained them. Māori legends have a lot to say about the origins of the land and sky this is the story of Ranginui and Papatūānuku - the sky father and earth mother how they were forced apart by their child Tāne Mahuta and how that separation gave space for new kinds of life.*

*Then there's the story of the origin of Aotearoa, how the demigod Māui hauled up a great fish and how his brothers hacked that fish to pieces carving out valleys and mountains and forming the shape of the land these stories of powerful primeval forces have parallels in our modern understanding of plate tectonics. Tectonic forces have been around for at least 4 billion years. ever since the earth first formed but the story of Aotearoa is relatively recent. I mean recent in geological terms, we're still going to have to go back a hundred million years!*

*OK, so a hundred million years ago the old supercontinent of Gondwana and Laurasia were beginning to be torn to pieces. You can almost make out the outline of modern-day continents like Africa and North and South America. But down south, Australia and Antarctica were still fused together. The land which will one day become New Zealand was sitting at the eastern edge of Gondwana but things were about to change. Superheated magma was rising up against the bottom of the crust. Stretching it, opening up deep fissures and fault lines.*

*Sometimes magma reached all the way to the surface, forming long chains of volcanoes. Eventually a huge section of land broke away from Gondwana and went sailing into the Pacific Ocean. It was a brand new continent – Zealandia, Te Riu-a-Māui. This continent was enormous about 5 million square kilometers. That's 18 times bigger than modern-day New Zealand. And as Zealandia took off into the Pacific, it brought a whole lot of plants and animals along for the ride.*

*Zealandia separated from Gondwana right at the peak of the age of dinosaurs, the middle Cretaceous period. But this wasn't just the age of dinosaurs there were lots of huge marine reptiles living in the seas around Zealandia. Just a quick bit of paleontological pedantry - ancient flying reptiles like pterosaurs, and swimming reptiles like plesiosaurs, are not technically dinosaurs. Dinosaurs are mostly land animals.*

*We've found quite a few fossils of marine reptiles in New Zealand like Māuisaurus and Taniwhasaurus. Taniwhasaurus,? Yeah I know, it's cool, eh! But actual dinosaur fossils are much rarer, like if you got all of New Zealand’s dinosaur fossils together in one place they'd probably fit inside a shoebox. Like, we've got a rib from an armored ankylosaur, we've got a couple of vertebra from several different big meat-eating theropods, we've got a vertebra of a giant long necked titanosaur, plus a few extra bones which we can't quite identify. Bro, are these your toys? Yeah, I get a new one every year for Christmas.*

*Based on such limited evidence, it's hard to say much about what New Zealand's dinosaurs were like but we can make a few educated guesses. Back in the age of dinosaurs the world was much warmer. Antarctica was covered in forests instead of ice, but Zealandia was much closer to the South Pole than New Zealand is today. So our dinosaurs must have survived months of darkness every year. In these conditions they might have evolved large eyes to see in the dark and thick coats of feathers to protect them from the cold. According to our educated guesses, our dinosaurs must have been pretty weird. Hopefully, we'll find some more complete skeletons in the future so we can confirm just how weird they were.*

*Okay, so me with the killjoy, just like in the rest of the world Zealandia’s dinosaurs were driven to extinction when an asteroid hit the earth around 66 million years ago in the Gulf of Mexico. This asteroid was about 10 kilometres across and it left a crater 200 kilometers wide. Impact debris rained down all over the world and dust blocked out the Sun for weeks. 80% of life on Earth died out including all the non-avian dinosaurs, pterosaurs, and giant marine reptiles.*

*After the extinction of the dinosaurs, mammals quickly evolved to fill the niches they left behind. Mammals eventually became huge plant eaters, and apex predators - or at least that's what happened everywhere else in the world. What happened in Zealandia was very different. There were almost certainly mammals scurrying around in Zealandia when it separated from Gondwana. Mammals lived alongside dinosaurs for millions of years all over the world but by the time Māori arrived here about seven hundred years ago, New Zealand's mammals had vanished.*

*Today our only native mammals are three species of bat which seemed to have flown here relatively recently from Australia. So what happened to the rest of our mammals? One theory suggests that at some point Zealandia slipped completely beneath the sea, so all our mammals drowned. But nowadays most scientists think there was always some land above the surface which should have been enough to keep our mammals afloat. But still something wiped them out and we just have no idea what it was. It's one of the biggest mysteries of prehistoric New Zealand.*

*Thanks to the lack of mammals, Aotearoa became dominated by birds. Most of which colonized New Zealand after flying here or after being blown across the ocean from other places. Once they arrived in New Zealand, these birds were safe from mammal predators so many species lost the ability to fly and took on radically different body shapes. The most radical change was the moa. The ancestors of the moa originally flew to New Zealand from Antarctica but over millions of years they completely lost their wings and grew much, much bigger.*

*The largest moa could stand more than 3 metres tall and weighed more than 200 kilos. Some birds kept their ability to fly, mostly these were smaller birds like the tūi and piwakawaka but there was one giant the pouākai or haast’s eagle, the largest bird of prey that's ever existed. The pouākai was the only animal big enough to take on a moa. They would dive out of the sky and hit with the force of a concrete block thrown from an eight story building – a concrete block with claws as big as a tiger.*

*Meanwhile, the land was still changing. At first Zealandia got stretched out and then it sank. Only a scattering of small islands were left above the surface. Then it was shoved up against the neighboring Australia plate and a bit of crust right on the boundary was pushed upwards. The land we call Aotearoa New Zealand rose from the sea. It's kind of like the story of Māui and his great fish.*

*There were also huge changes in the climate. Around 2.6 million years ago, the whole world fell into a series of ice ages. Glaciers grew over much of the central South Island, carving out huge valleys through the Southern Alps. Before the ice ages, Aotearoa was covered in the kinds of tropical plants you can see today in the forests of northern Queensland or Papua New Guinea but by the end of the last ice age, about 18,000 years ago, those plants had been replaced by rimu, totara, kauri, lots of ferns. The kind of plants we see in the bush today.*

*The huge glaciers in the South Island melted, leaving behind gigantic lakes like Wanaka, Tekapo, and Te Anau. But here's a funny thing about the ice ages; during the last ice age sea levels were a hundred and twenty-five meters lower than they are today. All the major islands of New Zealand were locked together in one big landmass. But global average surface temperatures were only about five degrees colder than today. That means every degree of warming over the last eighteen thousand years is translated to roughly twenty-five meters of sea level rise. Small changes in global temperature can translate to very big changes in the global climate and that's why scientists are really, really worried about global warming today.*

*OK, so that's the serious stuff, now let's talk about volcanoes. Sitting at the edge of a colliding plate boundary means that magma often finds weak points to bubble up through the crust under New Zealand. In over the last two million years, one of those weak points has set directly beneath the central North Island, the site of some of the world's most violent volcanic eruptions. The biggest was the oruanui eruption. About 25,000 years ago, it blanketed the entire North Island in ash and molten rock leaving behind the gigantic caldera which we now call Lake Taupō.*

*The Taupō super volcano has erupted many times but the last explosion happened in 232 AD, about the time the Roman Empire was at its height. This was much smaller than the oruanui event, but it's still the most violent volcanic eruption the world's seen in 5000 years. It covered most of the central North Island in a thick layer of ash and pumice - even a thousand kilometres away on the Chatham Islands, the ash fell half a metre deep.*

*Lake Taupō is still an active volcano and it will erupt again in the future, but you don't need to worry too much though because it's constantly monitored by scientists and we'd get a warning if it was winding up for another big explosion. The final major change in New Zealand's landscape happened after 1290, and if you dig down into the earth in many parts of Aotearoa you'll come across a thin layer of ash.*

*But this ash didn't come from a volcano, it came from a series of huge fires which ripped through New Zealand's forests. These fires were lit by human beings; the first humans ever to reach Aotearoa. Who were they? Where did they come from? That's a story for our next episode.*

*No reira tēnā koutou katoa, thank you so much for watching our very first episode of the Aotearoa History Show. We've got a bunch more coming - we're going all the way from a hundred million years ago up to pretty much the modern day. So make sure you subscribe at the bottom, give us a like, tell your friends about us, hit that little bell icon and then you'll get notified about all of our episodes as they come out.*

*Thanks for joining us on the Aotearoa History Show produced by RNZ and made possible by the RNZ New Zealand on Air Digital Innovation Fund.*

📄 Zealandia

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Zealandia (or [*Te Riu-a-Māui*](https://tetiniatangaroa.org.nz/projects/te-riu-a-m%C4%81ui-naming-a-continent)) is much larger than you might expect. Unlike other continents, it is [93% submerged](https://www.nationalgeographic.org/encyclopedia/zealandia/#:~:text=Most%20of%20that%20terrestrial%20land,also%20a%20part%20of%20Zealandia.) with only the three islands comprising Aotearoa New Zealand, New Caledonia, and a scattering of smaller islets peeking above the waves. But it was not always so, and that is the beginning of the story of how the geography and tectonic activity of this whenua (land) has led to flora and fauna so unique, it’s one of the closest things on Earth to imagining life on another planet, or in a parallel universe.

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As you walk through the Te Taiao exhibition in the Museum of New Zealand Te Papa Tongarewa (Te Papa), a colourful projection beams onto the floor, showing the shifting journey of Gondwanaland. Zealandia first breaks off then submerges and rises, shifting from a large continuous land area to the three islands we know today.

This had evolutionary impacts for the animals that became geographically separated by that submersion, or found themselves adapting from a mountainous to coastal environment shift (or vice-versa). There are species in New Zealand that millions of years ago had ancestors living in sub-tropical climates, and as the land beneath them rose, now dwell on mountains that once never existed.

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##Twisting Tectonic Plates

The Southern Alps are a mountain range that stretch almost the entire length of New Zealand’s South Island. They tell a geological story of New Zealand, where the Australian and Pacific tectonic plates meet. The collision twisted and pushed the earth up under their pressure, and caused a tension that continues today, causing the earthquakes that have earned the country one of its monikers - The Shaky Isles.

New Zealand experiences over [20,000 earthquakes a year](https://www.geonet.org.nz/earthquake/statistics) - though fewer than 150 are felt by its (human) inhabitants. These quakes are due to the meeting of these two giant plates, and is called [The Alpine Fault](https://www.otago.ac.nz/geology/research/alpine-fault/#:~:text=New%20Zealand%20lies%20at%20the,subducted%20below%20the%20Australian%20Plate.).

This fault delivers a bit of a double whammy to New Zealand, as in the South Island, the Australian plate is being subducted (forced downward by) the Pacific plate. As the land making up the Southern Alps is on the Pacific plate, these mountains are slowly being pushed upwards - by about 7mm a year!

Meanwhile, in the North Island, the opposite is happening- the Pacific plate is being subducted by the Australian plate. As the Australian plate pushes over the Pacific one, it has become thinner… creating the conditions for a lot of volcanic activity.

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For a more detailed explanation, you can check out [this](https://www.youtube.com/watch?v=POUwntNPFmc&ab_channel=OutThereLearning) video (7 mins) from GNS Science (NZ's geosciences Crown Research Institute).

##Volcanoes

The North Island abounds with [volcanic activity](https://www.learnz.org.nz/naturalhazards183/bg-standard-f/new-zealand-volcanoes), from the iconic Mount Taranaki cone volcano thrusting to the sky from an otherwise flat plateau, to the much bigger caldera “super volcanoes”, like the one that both formed and still lurks below the entirety of lake Taupō, and finally to the wide volcanic fields where one-off eruptions pepper large swathes of land like beneath the Auckland region.

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In the next section we will look a little closer at the supermassive caldera beneath Aotearoa New Zealand’s largest lake, Lake Taupō. This caldera is one of the world’s largest volcanoes and has had a dramatic impact on the shape of this whenua (land).

###Further Information (short videos):

The [sinking of Zealandia](https://www.youtube.com/watch?v=_qepWb_NVj4&ab_channel=AtlasPro) The [rise of Zealandia](https://www.youtube.com/watch?v=S_Ohu8KHkBs) [Alpine fault visual description](https://www.youtube.com/watch?v=1xfMcsErM_s) from GNS Science

###What have you learned so far? Share a list of 2-3 key points in the discussion below. Has anyone else shared similar points?

📄 The story of Lake Taupō

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Our biggest volcano isn’t the quintessential cone volcano you might imagine. It’s Lake Taupō, now bordered by a picturesque holiday town but formed about 25,500 years ago in the massive Ōruanui eruption. Taupō is a global star – the world’s most active supervolcano, and is studied by scientists from all over the world.

##Taupō caldera

The huge Ōruanui eruption spat out so much magma that the ground collapsed kilometres downward and left a caldera – a gigantic collapsed block of land – in its wake. Water filled the hole, and Lake Taupō was formed.

###Watch a reconstruction of this event below.

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##Volcano factory

The Pacific Plate plunges beneath the eastern North Island, 4cm every year. Pressure builds. Rock melts. Hot magma rises and feeds a long chain of volcanoes.
The Earth’s crust is unusually thin in the Taupō Volcanic Zone. Magma gets close to the surface – and sometimes breaks through. Every now and then, huge eruptions leave giant holes in the landscape.

##Heaps of magma and falling ash

The volume of erupted material was 8–9 times the volume of water in Lake Taupō today.
Volcanic material filled the air. Most fell on the North Island, but some landed as far away as the Chatham Islands.
The ash coating the surrounding land was as much as 2m thick in neighbouring regions like Napier.

##Still active

After an eruption in the central North Island, volcanic ash could cover the entire island and beyond.
Since Ōruanui, there’ve been 28 smaller eruptions of Taupō. No super eruption will happen in your lifetime – the magma takes too long to build.
Thanks to monitoring by GNS Science, we can expect some warning before the next one.

##Legends

It's obvious that the presence of these vast natural forces has impacted on the course of life and evolution here in Aotearoa- indeed, it is this volcanic and tectonic activity that pushed Zealandia back up out of the sea millions of years ago. But it also shaped the stories and worldviews of its first people. We will look closer at this in the next step, with the Māori legend of Rūaumoko – the God of Earthquakes.

###Is there anything you're unsure of or would like to know more about? Your fellow learners might be able to help! Ask a question in the comments below. Help others by reading and responding to their questions if you can.

📄 The God of Volcanoes

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##Rūaumoko

Rūaumoko is the God of Earthquakes and Volcanoes (as well as of seasons) in pūrākau (Māori mythology).

The restless unborn child of Papatūānuku, Earth Mother, and Ranginui, Sky Father, Ruāumoko is said to make the Earth shake and roll in his stirrings within Papatūānuku's womb. Other versions say he is an infant at his mother’s breast, and his volcanic stirrings come from the fire gifted to him by Tama-kaka, to keep them both warm. Still others say that he is wedded to Hine-nui-te-po, goddess of death and night.

####In this video from Dr Huirangi Waikerepuru, you will hear how the legend of Rūaumoko and other Māori creation stories connect the mighty geothermal and tectonic forces at work in Aotearoa to te ao Māori (the Māori worldview), and connect its people to this whenua (land) in a spiritual way.

[[☃ video 1]]

Māori terms used in this video:
Tēna koe, ngā mihi, ki a koe | Greetings, acknowledgements to you
Whakapapa | genealogy, lineage

###Further Reading:

If you’d like to learn some other Māori pūrākau (myths, legends, stories), including the story of the world’s creation, the story of the formation of New Zealand, the seasons, or the length of the day, or more contemporary tales, the linked sites are good places to start. Many of these tales will differ between iwi (Māori tribes) and rohe (regions).

###After the last few steps, we'd love you to take a moment to pause and reflect on your learning experience so far. Share any thoughts you have below.

📄 Active Earth

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##Vigilance

New Zealand remains very much geologically active today. The devastating Christchurch earthquakes of 2011 are still fresh in the minds of New Zealanders, as large swathes of that city remain demolished and abandoned in what is known as the ‘red zone’. Wellingtonians live in uncomfortable awareness of the fault line they live on top of, Aucklanders of the volcanic heat of Rūaumoko beneath theirs. We must all remain vigilant.

##Active land, awesome forces

In its *Whakarūaumoko \| Active Land* exhibition at Te Papa Tongarewa, and with the support of Aotearoa New Zealand’s [Earthquake Commission](https://www.eqc.govt.nz/), all of the concepts and events we’ve learned about so far come together to allow Kiwi and International visitors alike to get an immersive and hands-on understanding of, and connection to, the whenua (land) beneath us.

This exhibition offers interactive installations that foster an understanding of the forces beyond our control and encourage visitors to think about how they can prepare themselves, their whanau (families), and their communities for the turbulent rumblings of Aotearoa, and the many ways in which they manifest.

Rūaumokos story is also told in the permanent *Whakarūaumoko \| Active Land* exhibit. The mātauranga (knowledge) of te ao Māori (Māori worldviews) are interwoven throughout the exhibition, weaving together the spiritual and physical aspects of these phenomena. Visitors can follow the story of Zealandia, and create volcanic eruptions by building the pressure underground in an interactive display of magma flows.

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A display of the Indo Australian and Pacific plates tectonic plates (Aotearoa perched on top), can slide over each other as visitors learn about the sliding subduction that created our maunga (mountains).

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A tsunami tank gives visitors the power to unleash a wave across a diorama of the coastline - illustrating how far these devastating swells can climb the land.

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Earthquakes are an experience shared by all New Zealanders, and one that children are trained for from early schooling. The Quake House brings that home. Walk inside a tiny replica of a classic timber kiwi home, and experience the ground shaking beneath your feet. Feel the sharp jolts and deep rolls of quakes that speak to the depth and distance of the earthquake epicenter.

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This experience prompts visitors to consider many things; their rapid response to a quake for their immediate safety ([Drop, Cover, Hold](https://getready.govt.nz/emergency/earthquakes/drop-cover-hold), the preparations they need to make for the aftermath of a “big one” (food and water stockpiles, plans for locating loved ones), and how to quake-proof their home (securing objects like bookshelves, being aware of vulnerable structures like chimneys). It is simultaneously a thrilling, and sobering experience.

Partnered with this is a smaller “quake table” that mimics a tiny quake, complete with materials, and a challenge to build your own quake-proof structure atop it. Visitors can become a civil engineer, and see whether their creations have the structural integrity to withstand the forces of the Alpine Fault.

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####Further resources

Learn more about what goes on [inside the Quake House](https://blog.tepapa.govt.nz/2019/08/08/one-shot-capturing-the-heart-of-our-new-quake-house/), and how it was created.

📄 Brace Yourself

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Te Papa Tongarewa can be loosely translated as “Treasure Box” in acknowledgement of the more than 2.5 million priceless taonga (treasures) it holds. The museum, and its repository of treasures are in Wellington. A city sitting almost directly on a fault line, and in buildings that rest on soft reclaimed land that was once swamp and sea. It’s fair then, to ask how it can possibly hope to protect them in a land so vulnerable to devastating quakes.

The answer? 152 base isolators sit underneath the 50,000 tonne museum building. These are essentially giant shock absorbers, layers of steel, rubber, and lead, sitting between the building itself and the concrete slab it sits on.

These [ingenious devices](https://www.youtube.com/watch?v=GL5wEicECto) (invented in Aotearoa New Zealand!) mean that Te Papa can withstand a once-in 250 years quake unscathed, a once-in-500 years quake with minor repairs, and a once-in-2000 years quake by preserving the people, and taonga (treasures) within, if not the building itself.

####Further reading

[How Te Papa resists earthquakes](https://www.tepapa.govt.nz/discover-collections/read-watch-play/science/halting-jolts-how-te-papa-resists-earthquakes) [Te Papa’s ‘Quake Breaker’ exhibit](https://www.tepapa.govt.nz/quake-braker)

####Do you have earthquakes where you are? Or other natural disasters? How have you prepared for these? Comment below your experiences and how you have prepared for the natural disasters that can occur where you live.

📄 Reflection – Geography and deep history

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**We’ve covered 85 million years in this lesson! Since that first separation of Zealandia, this whenua | land has been in constant motion in response to massive and relentless forces within the earth. The dramatic rising, falling, sinking, grinding, pushing, and explosions have created a land like no other, and one that New Zealanders today learn to respect.**

These Shaky Isles may sound inhospitable, but nothing could be further from the truth. Next week we will cover a very different story, the story of how Aotearoa New Zealand has become home to a plethora of creatures so unique that they have been compared to life on another planet, or in a parallel dimension.

We’ll see you in the next lesson to learn just what makes the animals of Aotearoa so strange, and so precious.

###What did you learn in this lesson that you found the most interesting? Why?

**Post your comment, and react or respond to someone else.**

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