Variation of Tasmanian vegetation from East to West information
Tasmania can be broadly divided into two distinct regions, eastern and western, that exhibit major differences in climate, geology and vegetation. This divide, termed Tyler’s Corridor[1][2] (in recognition of Peter Tyler, a Tasmanian limnologist), runs from just south of the northwestern corner, and continues south, cutting roughly down the center of the island.[3] The vegetation changes occur principally due to variations in soil types, which are a result of the geological composition, and the vast difference in climate across the state. Generally, the west has a higher mean rainfall but poor acidic soil while the east has a lower mean rainfall but slightly more fertile soil. This results in a larger proportion of rainforest, moorland and wet sclerophyll vegetation dominating in the west and predominantly dry sclerophyll in the east.[3][4]
^Tyler, Peter (1992). "A lakeland from the dreamtime: the second founders' lecture". British Phycological Journal. 27 (4): 353–368. doi:10.1080/00071619200650301.
^Tyler, Peter (December 2007). "The distinctive limnological character of south west Tasmania". Australasian Plant Conservation. 16 (3): 27–28.
^ abRees, Andrew.B.H; Cwynar, Les.C (2010). "A test of Tyler's Line - response of chironomids to a pH gradient in Tasmania and their potential as a proxy to infer past changes in pH". Freshwater Biology. 55 (12): 2521–2540. doi:10.1111/j.1365-2427.2010.02482.x.
^Reid, James.B; Hill, Robert.S; Brown, Michael.J; Hovenden, Mark.J (2005). Vegetation of Tasmania. Tasmania: Australian Biological Resources Study. p. 108.
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