When people first arrived in Australia, they found unique plants and animals. It must have been like entering a new world. There were giant marsupials (mammals that carried their young in a pouch, such as kangaroos), giant monotremes (mammals that lay eggs, such as echidnas) and different types of birds (including emus and brolgas). There were also other giant animals that no longer exist. We call these extinct giant animals megafauna.
The name megafauna means 'big animals', generally animals with a body mass of over 40 kilograms. Much of the time, megafauna is a general term used to describe a particular group of large land animals that evolved during the Pleistocene epoch millions of years after the dinosaurs became extinct.
Australia’s megafauna were unique, and included giant marsupials such as Diprotodon, huge flightless birds such as Genyornis and giant reptiles such as Varanus ‘Megalania’.
Weight: About 110 kg
Length: 1.5 m from nose to tail
The marsupial lion was the largest of Australia’s marsupial carnivores, sporting an impressive set of teeth and a large claw on both front legs.
The Australian carnivore may have hunted other megafauna species, though scientists have varying theories about what it actually ate. As a marsupial, Thylacoleo carnifex had a pouch for rearing its young, much like a kangaroo or koala.
Weight: About 50kg
Length: Up to 5 m
Wonambi was a giant snake that took its name from an Aboriginal word for the rainbow serpents that inhabited waterholes in the Dreamtime.
It was non-venomous, instead killing its prey by constriction. It was related to the madtsoiids, an ancient group of snakes that were once common on all the continents that had been part of the super-continent of Gondwana, but which died out everywhere except Australia about 55 million years ago.
Weight: About 600 kg
Length: Up to 7m
This giant monitor lizard came from the same family as modern goannas and komodo dragons. No complete skeleton has ever been discovered, but the bones that have been found suggest it was a massive, heavily-built creature.
This ancient Australian carnivore probably competed for prey with the marsupial lion, and would have been capable of taking down an animal as large as diprotodon.
Weight: Up to 200 kg
Height: 2m
The giant short-faced kangaroo was the largest kangaroo in history. It was only a little taller than the red kangaroo, today’s current biggest kangaroo title-holder, but was much stockier and weighed more than twice as much.
Even though it was the biggest kangaroo ever, the short-faced giant kangaroo had a large, short head, compared to the more deer-like snout of modern kangaroos. It also had forward-facing eyes and chin, giving it an almost primate-like appearance, and only a single toe on its hind feet.
Like all kangaroos, it was herbivorous, though scientists believe it ate leaves rather than grass.
Weight: 1.5 to 2.5 tonnes
Length: 3 m
Diprotodon is often referred to as a giant wombat, and it did have a rear-facing pouch similar to a wombat.
However this prehistoric wombat was also closely related to modern koalas, as shown by its very koala-like nose. It was about the size of a white rhinoceros, making it the largest of all the marsupials, and like rhinos, it was herbivorous, probably living in grassy areas and open woodland, and eating a range of different plants.
What is the key historical finding discussed in this article?
Who conducted this research?
What scientific methods were used to come to this conclusion?
What argument is presented against the finding?
Who is making this counterpoint?
Megafauna were once widespread across Australia, but became extinct about 50,000 years ago – the same time as the first humans arrived.
Many megafauna fossils have been found in pitfall caves like the World Heritage-listed Naracoorte Caves on the Nullabor plain, where animals fell in through roof holes and were unable to escape. Animals became trapped in the caves at Naracoorte over a period of 500,000 years, leaving it with a rich fossil record covering more than 130 vertebrate species.
We have indisputable evidence that some early Aboriginal people were not only familiar with megafauna, in this case, Thylacoleo carnifex, but also recorded the salient features of this, now long extinct, animal in a manner that resonates across the millennia.
It is worth noting that not all megafauna are extinct – Australia has living megafauna in the form of Red and Eastern Grey Kangaroos and Saltwater Crocodiles
At the end of the last ice age, Australia's climate changed from cold-dry to warm-dry. As a result, surface water became scarce. Most inland lakes became completely dry or dry in the warmer seasons. Most large, predominantly browsing animals lost their habitat and retreated to a narrow band in eastern Australia, where there was permanent water and better vegetation. The diprotodon, one of Australia's megafauna, may have survived on the Liverpool Plains of New South Wales until about 7000 years ago.
As First Nations people have been in Australia over the past 50000 years, megafauna must have co-existed with humans for at least 30000 years. For social, spiritual and economic reasons, First Nations peoples harvested game in a sustainable manner.
Three potential drivers of the extinction of Australia's megafauna have been suggested.
The first is climate change that assumes an increase in arid conditions that eventually became lethal to megafauna.
The second proposed mechanism is that the early ancestors of Aboriginal people who either hunted megafauna species to extinction, or modified ecosystems to put the largest species at a disadvantage.
The third and most nuanced proposed driver of extinction is the combination of the first two.
Around 88 large vertebrate taxa disappeared from Sahul sometime during the Pleistocene, with the majority of losses (54 taxa) clearly taking place within the last 40,000 years. The largest was the 2.8-ton browsing Diprotodon optatum, whereas the ∼100- to 130-kg marsupial lion, Thylacoleo carnifex, the world’s most specialized mammalian carnivore, and Varanus priscus, the largest lizard known, were formidable predators. Explanations for these extinctions have centered on climatic change or human activities. Here, we review the evidence and arguments for both. Human involvement in the disappearance of some species remains possible but unproven. Mounting evidence points to the loss of most species before the peopling of Sahul (circa 50–45 ka) and a significant role for climate change in the disappearance of the continent’s megafauna.
Climate change frames debate over the extinction of megafauna in Sahul (Pleistocene Australia-New Guinea)Stephen Wroe, Judith H. Field judith.field@unsw.edu.au, Michael Archer, +6, and Scott D. MooneyAuthors Info & AffiliationsEdited by James O’Connell, University of Utah, Salt Lake City, UT, and approved April 9, 2013 (received for review February 12, 2013)May 6, 2013110 (22) 8777-8781https://doi.org/10.1073/pnas.1302698110Australian megafauna became extinct about 42,000 years ago at the same time that the Pleistocene epoch ended, and the people who arrived on the continent migrated from the north to the south, therefore a combination of these two factors is the most likely cause of extinction. Evidence that supports a nuanced interaction of both people and changing climate includes different rates of extinction. This is significant because the different patterns cannot be explained by people acting as ‘super-predators’ or climate change. Furthermore, there is a lack of reliable evidence that clearly points to either climate change or humans hunting and changing the ecosystem through fire management. Researchers often must rely on a single artefact such as a diprotodon tooth or a single site which limits the applicability of evidence to other situations. Ultimately, considering the research and evidence we have at the moment it seems as if it was a combination of both climate change and humans that led to the extinction of megafauna in Australia.