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The pre-colonial distribution of grasslands, woodlands and forests on the Werribee plains, Victoria
(2012)
We use historic plans and recent field observations to reconstruct and describe the former (pre-1750) character and distribution of vegetation on the Werribee Plains, near Melbourne. The primary outcome of this research is a detailed vegetation map. The ecological factors controlling the distribution of trees and open-plains are also discussed. The results show that most of the area was treeless grassland at the time of European settlement (1835). This grassland was broken up by clearly-defined areas of Eucalypt forest, some of which remain. There is, in contrast, little remaining trace of the woodlands of Allocasuarina and Banksia, which we show were once widespread on the plains and stony rises beyond the Eucalypt forest. This work is timely, given the proposal for the creation of two large new reserves in the area, which contain many areas that may be subject to restoration.
European settlement in Australia has always been concentrated along or close to the coast. As a consequence, saltmarshes, mangroves and other coastal marshes have experienced a long history of modification and destruction. Depletion statistics are available for many coastal marshes in the Northern Hemisphere and, in Australia, for parts of New South Wales and Queensland. There are no equivalent State-wide data for Victoria. Using a suite of historical information, including extensive use of early surveyors’ maps, we aimed to provide a consistent view of the change in the extent of coastal marshes since European colonization in Victoria (i.e. the mid-19th century). Notwithstanding the difficulties of interpretation, we estimate that prior to European colonization Victoria supported approximately 346– 421 km2 of coastal marsh, of which approximately 80–95% remains. Although a simplistic interpretation suggests a net loss of 5–20% in wetland area over this time period, it is clear that some parts of the coast have experienced relatively little change since the mid 19th century whereas others have been severely depleted and, in a few sectors, there may have been an expansion of coastal marsh. The situation with the Gippsland Lakes is complex, and according to the method used to interpret the original data sources there has either been a substantial increase or a loss of up to 35% in wetland area around Lake Wellington. The largest absolute losses have probably been of EVC 140 Mangrove Shrubland and of coastal saltmarsh dominated by Tecticornia spp. Parts of the coast where significant losses have occurred include the Lonsdale Lakes, western shore of Port Phillip Bay, Anderson Inlet, Shallow Inlet, Powlett- Kilcunda, Corner Inlet and Nooramunga, and possibly Lake Wellington. With the exception of the Lonsdale Lakes, all these areas are situated along the Gippsland coast. Changes to coastal marshes have not stopped and are unlikely to cease in the near future. The destruction of coastal marshes for industrial development remains an ongoing threat in many regions (e.g. in Western Port) and is likely to be compounded by climate change and, in particular, sea-level rise.
We use historical information and extensive contemporary surveys to describe the pre-European vegetation of the Nepean Peninsula, an extensive area of calcareous sand dunes at the tip of the Mornington Peninsula, south of Melbourne, Victoria (38º19’S 144º43’E). We conclude that much of the area was once covered by open, grassy woodlands, variously dominated by Allocasuarina verticillata (Drooping Sheoak), Banksia integrifolia subsp. integrifolia (Coast Banksia), Acacia species (Wattles), and Melaleuca lanceolata subsp. lanceolata (Moonah), along with a range of other species. Some areas supported shrublands, woodlands, forests, grasslands and wetlands. This area was markedly distinct from most other nearby areas, and has ecological affinities with areas in western Victoria. Over 200 years of ‘European’ land use have left this landscape remarkably different today – even in places where native vegetation persists. We review and discuss the environmental factors that have influenced the pattern and structure of the vegetation.