South Australia’s 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 of many iconic Australian megafauna species that became between 48,000 and 37,000 years ago.
Authors
Rieneke Weij
Postdoctoral researcher in Geochemistry/Palaeoclimatology, University of Cape Town
Jon Woodhead
Research Scientist
Kale Sniderman
Senior Research Fellow, The University of Melbourne
Liz Reed
Research Fellow, University of Adelaide
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.
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).
Palaeontologists have excavated and dated many of these fossil deposits and reconstructed the skeletons of a number of megafauna species.
The caves formed when groundwater percolated through cracks in limestone rocks, dissolving them and forming cavities. They were previously dated at between – 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 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.
What we did
The dating method 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.
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 at the complex.
Why this matters
There’s heated 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 and the 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.
Rieneke Weij receives funding from the Australian Research Council
Jon Woodhead receives funding from the Australian Research Council.
Kale Sniderman receives funding from the Australian Research Council
Liz Reed receives funding from the Australian Research Council.
