A stalagmite from a Western Australian (WA) cave has revealed that prior to European settlement in the state, low-intensity bushfires were quite frequent, whereas, from the late 1800’s infrequent but high-intensity bushfires have become common.
The stalagmite studied was extracted from Yonderup Cave in WA, and preserved a record of climate conditions and fires, enabling researchers to link-local fires with climatic precursors.
This is the first study to examine a stalagmite’s geochemistry in order to understand historical bushfires, and researchers speculate that this change in frequency and intensity of fires is associated with changes in land management practices.
“The intensity of this fire was likely caused, at least partially, by these dry conditions,” she said.
“We also know that this [the largest fire] occurred a few decades after Indigenous cultural burning would have been suppressed by Europeans, so the fire was also probably exacerbated by a build-up of understorey vegetation and dry combustible material on the forest floor due to the removal of Indigenous land management practices.”
Traditional Indigenous land management also involved burning the native grasses early in the dry season with small fires, whereas since European settlement, traditional burning practices have greatly declined, meaning savannah grasses are left to grow and become ideal fuel for uncontrollable fires late in the dry season.
The technique used to study the stalagmite’s geochemistry utilises its composition, the variation in its elements, and the order in which they were laid down.
“Nutrients such as phosphorus, and trace metals are found in bushfire ash and, in theory, can dissolve into waters that eventually infiltrate underground caves,” McDonough said.