1972
DOI: 10.26749/rstpp.106.1.61
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Vegetation of the Central Plateau

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Cited by 31 publications
(14 citation statements)
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“…The high abundance of Lomatia in mixed sites may reflect its ability to resprout from lignotubers after low and intermediate levels of burning, and its tendency to grow in semi-shaded environments (Dickinson and Kirkpatrick, 1987). Lomatia is also relatively unpalatable to non-native and native browsers (Jackson, 1972). The low abundance of Lomatia in burned sites may reflect heat-caused mortality of belowground biomass or loss of soil organic matter from fire-caused erosion, both of which would favor herbaceous colonization over resprouting shrubs.…”
Section: Discussionmentioning
confidence: 99%
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“…The high abundance of Lomatia in mixed sites may reflect its ability to resprout from lignotubers after low and intermediate levels of burning, and its tendency to grow in semi-shaded environments (Dickinson and Kirkpatrick, 1987). Lomatia is also relatively unpalatable to non-native and native browsers (Jackson, 1972). The low abundance of Lomatia in burned sites may reflect heat-caused mortality of belowground biomass or loss of soil organic matter from fire-caused erosion, both of which would favor herbaceous colonization over resprouting shrubs.…”
Section: Discussionmentioning
confidence: 99%
“…The Central Plateau of Tasmania was extensively glaciated during the Pleistocene, and the present-day vegetation communities established at around 3000–4000 years ago (Dodson, 2001; Hopf et al, 2000; Stahle et al, 2016; Thomas and Hope, 1994). Modern vegetation is characterized by spatially heterogeneous patches of eucalypt woodlands at low elevations, coniferous forests and woodlands at higher elevations, and alpine heath above treeline (Jackson, 1972). Pure stands of Athrotaxis are characterized by low tree densities, with an understory of grass (e.g.…”
Section: Introductionmentioning
confidence: 99%
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