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New Zealand Land 
Formation 
Biology 
Ms Gibellini 
2014
How Was NZ formed? 
https://www.youtube.com/watch?v=pENq1ml2haA 
http://www.youtube.com/watch?v=IfDhY32vP-c
170 MYA 
• NZ was part of a land mass 
known as Gondwanaland 
• http://www.sciencelearn.org.nz/Contexts/ 
Ferns/Sci-Media/Animations-and- 
Interactives/Gondwana-animation
130 MYA 
• Africa, India and Madagascar detached and 
moved away from Africa and South America 
creating the Atlantic Ocean 
• Australia, NZ and Antarctica were attached 
to the southern end of South America and 
called Autralis. It straddled the South Pole 
BUT was ice free so temperate forests grew 
there for millions of years
80-60 MYA 
• Autralis began to break up, NZ or Zealandia as it 
was known broke away from Australia and the 
Antarctic and the Tasman Sea formed. 
• This took over 20 million years to occur! 
• As it separated the land was stretched and thinned 
out which is why much of the land is under the 
sea today 
• During this time period huge meteors and large 
scale volcanic activity resulted in the extinction of 
about half the plant and animals species on Earth 
including dinosaurs
23 MYA 
• Zealandia was at its lowest point, it is thought 
there were only a few scattered islands above sea 
level, the largest in the Canterbury area 
• As a result much of NZ is made from limestone 
(formed under the sea by shells of dead sea 
animals) 
• Therefore almost all of our flora and fauna 
arrived from other land masses 25 MYA. 
• NZ is currently rising out of the sea along the 
Alpine Fault as two tectonic plates collide
10 MYA 
The Pacific Plate began to sink into the 
Australian Plate. Pressure caused cracks 
to form…and eventually the Alpine Fault. 
NZ spilt in two and now lies across two 
plates and collide in sections creating new 
land, volcanic eruptions and uplift.
2.6 MYA 
• The Earth was exposed to periods of repeated cooling – 
ice ages 
• During glacial periods temperatures dropped as much as 
4.5’C, heavy snow fell on NZ mountains. The snow 
hardened into ice and glaciers moved downhill into 
lower regions. Glaciers once covered the valleys from 
Fiordland to west Nelson 
• Huge ice caps formed in the northern hemisphere 
locking up water and the sea level dropped by 100 
metres exposing more coastal land in NZ. When the ice 
caps melted the sea level then rose again
In the Last 1.8 MY 
• Sothern Alps have risen 
• Volcanic eruptions buried large areas of the 
North Island 
• Huge glaciers spread out from the mountains 
• The past 10 000 years has seen a fairly stable 
climate, temperatures have been rising for the 
past 7,000 years as a result so have sea levels.
Flora and Fauna 
• Up until several million years ago there were no terrestrial mammals except bats and 
seas, most of the fauna was made up of insects and birds, such as unusual frogs and the 
tuatara 
• The flora was mainly gondwanan plants such as giant kauri forests, podocarps and 
southern beech trees. 
• There is a high rate of interspecific and intraspecific hybridisation in NZ plants and 
animals 
• Following the separation from Gondwana species have came to NZ via the sea or 
airborne mostly from Australia. They arrived so long ago they are now almost 
unrecognisable as being decedents of Australian species. 
• Some species have also travelled to NZ from New Caledonia
NZ Flora and Fauna 
• https://www.youtube.com/watch?v=Tw7kx5dHii8 
• https://www.youtube.com/watch?v=KVSjtmtvF8M 
• https://www.youtube.com/watch?v=KVSjtmtvF8M&ytsession=pPvPZ-Sgl3oE8O8TNu5EuuoOYFlywimtWdew- 
4WICdIN3_kQI7og_2aaIPgrQ6ei1XCTbx6ze3mhdGT5VaOfP5TVflCxGaNf7PUeE 
TRZavaqFjMMaIv-FRgSqitxzZ0ufaA28YSC96ZdhTCvY9- 
XB4SijxtjuEYpxA2QNsGu4ewYiet0doaQ9feWuStr7oNdFM69v5X9hZRnEQbeVeli 
edSvKvXRp5R0BziKqqE3I05aNUw-pPho57w_ 
HLx86fUBjMq7XTMI3fYiSUolZm3CQLP7H3lNgYGnY4CQT4SVMbo 
GfaVUE-B_1LyW_1ybG6LKgQzIOj0eeog
Age of Man 
• NZ was one of the last land masses to be colonised by humans 
around 1250AD by Maori and then 1790 by Europeans. 
• Humans burnt forests, converted land to agriculture and removed 
2/3 of the native forest, resulting in major ecological changes and 
erosion, 
• Hunting and introduction of pests resulted in the extinction of 
many native species
Diversity 
• Diversity – range of different species 
• NZ has had two main forest types for the past 190million years – 
podocarps (kauri) and the southern beech. 
• The rest of NZ was grassland and tussock in subalpine and low shrub 
land. 
• Many of NZ native birds descend from Gondwanan stock, in the absence 
of mammals birds have evolved to fill niches usually filled by mammals eg 
Moa 
• Others show clear links to Australian birds eg NZ Pigeon, Falcon and 
parrots
References 
• http://www.teara.govt.nz/en/geology-overview/page-11 
• http://www.gns.cri.nz/Home/Learning/Science-Topics/NZ-Geology/NZ-s-Geological-History 
• http://www.visitzealandia.com/what-is-zealandia/our-history/80-million-years-ago/ 
• http://en.wikipedia.org/wiki/Biodiversity_of_New_Zealand 
• http://www.teara.govt.nz/en/1966/geology-new-zealands-geological-history 
• http://www.teara.govt.nz/en/glaciers-and-glaciation/page-3 
• http://www.gns.cri.nz/Home/Learning/Science-Topics/NZ-Geology/NZ-s-Geological-History 
• http://www.teara.govt.nz/en/glaciers-and-glaciation/page-3 
• http://www.teara.govt.nz/en/geology-overview/page-6 
• http://www.visitzealandia.com/what-is-zealandia/our-history/80-million-years-ago/ 
• http://www.gns.cri.nz/Home/Learning/Science-Topics/Ocean-Floor/History-of-Zealandia 
• http://en.wikipedia.org/wiki/Biodiversity_of_New_Zealand

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How NZ's Unique Land and Life Evolved

  • 1. New Zealand Land Formation Biology Ms Gibellini 2014
  • 2. How Was NZ formed? https://www.youtube.com/watch?v=pENq1ml2haA http://www.youtube.com/watch?v=IfDhY32vP-c
  • 3. 170 MYA • NZ was part of a land mass known as Gondwanaland • http://www.sciencelearn.org.nz/Contexts/ Ferns/Sci-Media/Animations-and- Interactives/Gondwana-animation
  • 4. 130 MYA • Africa, India and Madagascar detached and moved away from Africa and South America creating the Atlantic Ocean • Australia, NZ and Antarctica were attached to the southern end of South America and called Autralis. It straddled the South Pole BUT was ice free so temperate forests grew there for millions of years
  • 5. 80-60 MYA • Autralis began to break up, NZ or Zealandia as it was known broke away from Australia and the Antarctic and the Tasman Sea formed. • This took over 20 million years to occur! • As it separated the land was stretched and thinned out which is why much of the land is under the sea today • During this time period huge meteors and large scale volcanic activity resulted in the extinction of about half the plant and animals species on Earth including dinosaurs
  • 6. 23 MYA • Zealandia was at its lowest point, it is thought there were only a few scattered islands above sea level, the largest in the Canterbury area • As a result much of NZ is made from limestone (formed under the sea by shells of dead sea animals) • Therefore almost all of our flora and fauna arrived from other land masses 25 MYA. • NZ is currently rising out of the sea along the Alpine Fault as two tectonic plates collide
  • 7. 10 MYA The Pacific Plate began to sink into the Australian Plate. Pressure caused cracks to form…and eventually the Alpine Fault. NZ spilt in two and now lies across two plates and collide in sections creating new land, volcanic eruptions and uplift.
  • 8. 2.6 MYA • The Earth was exposed to periods of repeated cooling – ice ages • During glacial periods temperatures dropped as much as 4.5’C, heavy snow fell on NZ mountains. The snow hardened into ice and glaciers moved downhill into lower regions. Glaciers once covered the valleys from Fiordland to west Nelson • Huge ice caps formed in the northern hemisphere locking up water and the sea level dropped by 100 metres exposing more coastal land in NZ. When the ice caps melted the sea level then rose again
  • 9. In the Last 1.8 MY • Sothern Alps have risen • Volcanic eruptions buried large areas of the North Island • Huge glaciers spread out from the mountains • The past 10 000 years has seen a fairly stable climate, temperatures have been rising for the past 7,000 years as a result so have sea levels.
  • 10. Flora and Fauna • Up until several million years ago there were no terrestrial mammals except bats and seas, most of the fauna was made up of insects and birds, such as unusual frogs and the tuatara • The flora was mainly gondwanan plants such as giant kauri forests, podocarps and southern beech trees. • There is a high rate of interspecific and intraspecific hybridisation in NZ plants and animals • Following the separation from Gondwana species have came to NZ via the sea or airborne mostly from Australia. They arrived so long ago they are now almost unrecognisable as being decedents of Australian species. • Some species have also travelled to NZ from New Caledonia
  • 11. NZ Flora and Fauna • https://www.youtube.com/watch?v=Tw7kx5dHii8 • https://www.youtube.com/watch?v=KVSjtmtvF8M • https://www.youtube.com/watch?v=KVSjtmtvF8M&ytsession=pPvPZ-Sgl3oE8O8TNu5EuuoOYFlywimtWdew- 4WICdIN3_kQI7og_2aaIPgrQ6ei1XCTbx6ze3mhdGT5VaOfP5TVflCxGaNf7PUeE TRZavaqFjMMaIv-FRgSqitxzZ0ufaA28YSC96ZdhTCvY9- XB4SijxtjuEYpxA2QNsGu4ewYiet0doaQ9feWuStr7oNdFM69v5X9hZRnEQbeVeli edSvKvXRp5R0BziKqqE3I05aNUw-pPho57w_ HLx86fUBjMq7XTMI3fYiSUolZm3CQLP7H3lNgYGnY4CQT4SVMbo GfaVUE-B_1LyW_1ybG6LKgQzIOj0eeog
  • 12. Age of Man • NZ was one of the last land masses to be colonised by humans around 1250AD by Maori and then 1790 by Europeans. • Humans burnt forests, converted land to agriculture and removed 2/3 of the native forest, resulting in major ecological changes and erosion, • Hunting and introduction of pests resulted in the extinction of many native species
  • 13. Diversity • Diversity – range of different species • NZ has had two main forest types for the past 190million years – podocarps (kauri) and the southern beech. • The rest of NZ was grassland and tussock in subalpine and low shrub land. • Many of NZ native birds descend from Gondwanan stock, in the absence of mammals birds have evolved to fill niches usually filled by mammals eg Moa • Others show clear links to Australian birds eg NZ Pigeon, Falcon and parrots
  • 14.
  • 15. References • http://www.teara.govt.nz/en/geology-overview/page-11 • http://www.gns.cri.nz/Home/Learning/Science-Topics/NZ-Geology/NZ-s-Geological-History • http://www.visitzealandia.com/what-is-zealandia/our-history/80-million-years-ago/ • http://en.wikipedia.org/wiki/Biodiversity_of_New_Zealand • http://www.teara.govt.nz/en/1966/geology-new-zealands-geological-history • http://www.teara.govt.nz/en/glaciers-and-glaciation/page-3 • http://www.gns.cri.nz/Home/Learning/Science-Topics/NZ-Geology/NZ-s-Geological-History • http://www.teara.govt.nz/en/glaciers-and-glaciation/page-3 • http://www.teara.govt.nz/en/geology-overview/page-6 • http://www.visitzealandia.com/what-is-zealandia/our-history/80-million-years-ago/ • http://www.gns.cri.nz/Home/Learning/Science-Topics/Ocean-Floor/History-of-Zealandia • http://en.wikipedia.org/wiki/Biodiversity_of_New_Zealand