The research focused on the Biggenden banded snail (Figuladra bayensis) found at Coalstoun Lakes National Park in Queensland's Wide Bay region. Scientists took tiny samples from dead snail shells and used elevated levels of radiocarbon from 1960s nuclear tests to date growth bands, determining the snail lived about 4.5 years.
Analysis of oxygen and stable carbon isotopes revealed insights into rainfall. Instead of continuous growth, the shell showed periods of rapid growth separated by little or no growth. Lead researcher Nicholas Patton said: "What we saw was the shell did not grow continuously during the snail's life; there were periods of rapid growth separated by periods of little or no growth."
Honorary professor James Shulmeister said researchers initially assumed summer wet-season growth, but found two big growth spurts corresponding to cyclones that passed close to the site. "We realised that these were two cyclones or ex-cyclones that passed very close to the site and dumped a lot of water on Coalstoun Lakes," Mr Shulmeister said.
The research has been published in The Holocene. Mr Shulmeister expressed optimism about finding preserved snail shells in sediment cores to extend the record further back.
John Stanisic, honorary research fellow at the Queensland Museum, was not involved but called the work "quite incredible" and hoped it would spark more interest in land snails, which play a critical role in ecosystems. Dr Stanisic noted that snails are often overlooked despite being "part of that suite of invertebrate species that are so critical to the functioning of an ecosystem."
The study demonstrates that snail shells could be used to reconstruct past extreme rainfall events, offering a portal to historical weather data before official records began in 1900.
