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Study Finds Famous Australian Caves Are Up To 500,000 Years Older Than We Thought - And It Could Help Explain A Megafauna Mystery
South Australia’s Naracoorte Caves is one of the world’s best fossil sites, containing a record spanning more than half a million years. Among the remains preserved in layers of sand are the bones of many iconic Australian megafauna species that became extinct between 48,000 and 37,000 years ago.
The reasons for the demise of these megafauna species are intensely debated. But the older the fossils we can find, the better we can understand the species’ evolution and extinction.
To date, determining the precise age of the caves has been difficult. However our research demonstrates, for the first time, how old Naracoorte’s caves really are – and the answer is up to 500,000 years older than previously thought.
Our findings shed new light on the antiquity of this important place. We hope this will aid understanding of how biodiversity responds to a changing climate over time.
Artist’s impression of extinct Pleistocene megafauna in Australia by Julian Hume. Lower left: enormous short-faced kangaroos. Lower right: Thylacoleo carnifex and Wonambi naracoortensis.
Centre left and right: Diprotodon optatum and Zygomaturus trilobus. Author provided
A moment in geologic time
Caves can be extraordinary time capsules, often preserving the remains of long extinct plants and animals in exquisite detail. The Naracoorte Caves in South Australia is one such example.The cave complex is South Australia’s only World Heritage site. Among the remarkably diverse and complete fossil record are the remains of iconic megafauna such as:
- Thylacoleo carnifex (marsupial predator)
- Zygomaturus tribolus (huge herbivore)
- Wonambi naracoortensis (giant constrictor snake)
- Procoptodon goliah (browsing sthenurine kangaroo).
The caves formed when groundwater percolated through cracks in limestone rocks, dissolving them and forming cavities. They were previously dated at between 0.8 and 1.1 million years old – an estimate generated by dating a fossil dune ridge that lies over the cave complex.
But the methods used to date the dune ridge were not entirely suitable for the task. As such, a precise age of the caves had not been obtained, until now.
This intricate work involved in our study has taken five years, but it was worth the wait.
Layers of flowstones overlying sandy layers with fossil bone material in Specimen Cave, Naracoorte. Jon Woodhead, Author provided
What we did
The dating method we used involved examining the beautiful calcite formations inside the caves. Collectively, these are called “speleothems” and they include stalagmites, stalactites and flowstones.When speleothems form, tiny amounts of uranium – a radioactive element – are locked inside them. Over time, uranium slowly decays into the element lead. This occurs at a known, constant rate – which means we can use uranium in speleothems as a natural clock to date them.
Doing so involved extracting uranium and lead from the speleothem in a laboratory. We then measured each element and calculate the sample’s age very precisely.
Whale Bone Cave, one of the oldest caves at Naracoorte. Steve Bourne, Author provided
Because speleothems only start to grow once a subterranean cavity is formed and above the groundwater table, the oldest speleothem age reveals the minimum age of the cave itself.
From this, we found the caves began to form at least 1.34 million years ago – making them 250,000 to 500,000 years older than previous estimates.
The second part of our study sought to determine when the caves first opened to the surface, allowing both air and animals in. We did this by examining microscopic particles of charcoal and pollen captured in the calcite formations as they grew.
We found charcoal and pollen first appeared in the caves around 600,000 years ago. This suggests the caves may harbour exciting new vertebrate fossil material up to 600,000 years old – more than 100,000 years older than the oldest known fossil deposits at the complex.
Lead author Rieneke Weij descending into a cave at Naracoorte. Liz Reed, Author provided
Why this matters
There’s heated debate about whether the extinction of Australia’s megafauna was the result of humans or the climate.A good chronology is key to understanding when and how quickly natural processes occurred over time. Without precise ages, we cannot know the rate of change to landscapes, climate or biodiversity.
So while the Naracoorte Caves formed at least 1.34 million years ago, they did not open to the surface until 600,000 years ago. This sheds new light on the vast separation in time between landforms evolving and fossils accumulating.
Our findings will also help palaeontologists target new excavation sites to find older fossils – hopefully providing valuable further evidence of how our continent’s unique biodiversity has changed.
Our new approach can help to unravel how old fossil deposits at other cave complexes in Australia and around the world where both speleothems and vertebrate fossils are found.
Australia’s richness of plant and animal species faces an uncertain future, due to climate change and other human impacts. Studying important sites such as the Naracoorte Caves helps us understand not just how climate change influenced biodiversity in the past, but what might happen in future.
This article was first published on The Conversation, and was written by Brett Farmer, Rieneke Weij Postdoctoral researcher in Geochemistry/Palaeoclimatology from University of Cape Town, Jon Woodhead Research Scientist, Kale Sniderman Senior Research Fellow from The University of Melbourne, Liz Reed Research Fellow from University of Adelaide
