Following the Holocene Warm Maximum, modern cooler and drier conditions were established in Australia by about:

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The establishment of modern cooler and drier conditions in Australia occurred around 4,500 years ago, according to climate records and archaeological evidence. This period is known as the mid-Holocene transition, marking a shift in climate patterns from the warmer and wetter conditions of the Holocene Warm Maximum to the current climate regime.

Following the Holocene Warm Maximum, Modern Cooler and Drier Conditions