Abiotic features
The past 7000 years, during the early to middle Holocene involved the formation of a linear barrier dune system, enclosing a long, narrow lagoon that stretched from Bunbury to Preston Beach. Strong winds and swell drove inland coastal erosion which moved a few kilometres east over approximately 7000 years. The Holocene barrier is stratigraphically complex due to being exposed to varying sea levels throughout time. 8000 years ago, Holocene sea levels were 6m below the modern present level and 7,500 years ago, levels rose dramatically by 4m. These intense fluctuations were driven by glacial and inter-glacial events. Coastal near-shore marine and coastal sedimentation took place over four stages, separated by glacial episodes (Department of Environment & Conservation, 2009). Semeniuk (1995) defined the Holocene coastal coquina as "white, cream, yellowish and tan shell beds, shell grit, shelly sand, and coarse to medium sand".