A planet-defining point
In the dry creek bed of Enorama Creek, deep within Ikara-Flinders Ranges National Park, a small brass disc is set into the rock. This marker, known as a "Golden Spike," is a Global Boundary Stratotype Section and Point (GSSP). The International Union of Geological Sciences (IUGS) ratified this specific point in 2004, using it to officially define the start of the Ediacaran Period. This was the first new geological period added to the official time scale in 120 years.
The spike marks a precise boundary in the geological record dating to 635 million years ago. It sits at the base of a pale buff-colored layer of dolostone called the Nuccaleena Formation. This layer is a "cap carbonate," a distinctive type of rock deposited in warm, shallow seas as the planet rapidly warmed after a global ice age. Directly beneath this cap carbonate are glacial deposits of the Elatina Formation, evidence of the Marinoan glaciation when ice sheets may have covered the entire planet. The sharp transition from glacial debris to warm-water carbonate provides a clear, globally recognizable signal of the end of the Cryogenian "Snowball Earth" and the beginning of the Ediacaran. This is the only GSSP in the Southern Hemisphere.