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  5.     <title>UTas ePrints - The vegetation of an infrequently burned Tasmanian mountain region</title>
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  23. <meta content=" The Mt. Bobs-Boomerang area in southern Tasmania is rugged and mountainous
  24. (600-1080m above sea level), with a perhumid cool (Thornthwaire classification) climate and a range
  25. of geological substrates inclucling mudstone, sandstone, limestone and dolerite. 164 species of
  26. vascular plants, all native to Tasmania, have been recorded in the study area. The subalpine vegetation
  27. is composed primarily of rainforest and scrub communities. Fires have had major effects on these
  28. communities, but are rare; the period since the Last fire varies between about 50 and 500 years. A small
  29. area of herbland and heathland occupies the poorly drained valley fioors and different herbland
  30. communities are found on the flats and limestone cliffs around Lake Sydney.
  31. Above the treeline, which occurs at about 1000m on Mt. Bobs and the Boomerang, heathland
  32. is the major vegetation formation. Herblands are found in sheltered sites with the longest snowlie, and
  33. fjaeldmark, much of it associated with a pattern of non-sorted solifluction terraces, occupies the
  34. highest, most exposed part of the mudstone-capped Boomerang.
  35. Exposure to strong winds, snowlie, substrate type, degree of waterlogging and fire frequency
  36. appear to be major environmental delerminants of the plant communities.
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  53. <meta content=" The Mt. Bobs-Boomerang area in southern Tasmania is rugged and mountainous
  54. (600-1080m above sea level), with a perhumid cool (Thornthwaire classification) climate and a range
  55. of geological substrates inclucling mudstone, sandstone, limestone and dolerite. 164 species of
  56. vascular plants, all native to Tasmania, have been recorded in the study area. The subalpine vegetation
  57. is composed primarily of rainforest and scrub communities. Fires have had major effects on these
  58. communities, but are rare; the period since the Last fire varies between about 50 and 500 years. A small
  59. area of herbland and heathland occupies the poorly drained valley fioors and different herbland
  60. communities are found on the flats and limestone cliffs around Lake Sydney.
  61. Above the treeline, which occurs at about 1000m on Mt. Bobs and the Boomerang, heathland
  62. is the major vegetation formation. Herblands are found in sheltered sites with the longest snowlie, and
  63. fjaeldmark, much of it associated with a pattern of non-sorted solifluction terraces, occupies the
  64. highest, most exposed part of the mudstone-capped Boomerang.
  65. Exposure to strong winds, snowlie, substrate type, degree of waterlogging and fire frequency
  66. appear to be major environmental delerminants of the plant communities.
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  180.     <h1 class="ep_tm_pagetitle">The vegetation of an infrequently burned Tasmanian mountain region</h1>
  181.     <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Kirkpatrick, J.B.</span> and <span class="person_name">Harwood, C.E.</span> (1980) <xhtml:em>The vegetation of an infrequently burned Tasmanian mountain region.</xhtml:em> Proceedings of the Royal Society of Victoria, 91 . pp. 79-107. ISSN 0035-9211</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a onmouseover="EPJS_ShowPreview( event, 'doc_preview_2315' );" href="http://eprints.utas.edu.au/1843/1/03.01.05.pdf" onmouseout="EPJS_HidePreview( event, 'doc_preview_2315' );"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a><div class="ep_preview" id="doc_preview_2315"><table><tr><td><img alt="" src="http://eprints.utas.edu.au/1843/thumbnails/1/preview.png" class="ep_preview_image" border="0" /><div class="ep_preview_title">Preview</div></td></tr></table></div></td><td valign="top"><a href="http://eprints.utas.edu.au/1843/1/03.01.05.pdf"><span class="ep_document_citation">PDF</span></a> - Requires a PDF viewer<br />2462Kb</td></tr></table><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto"> The Mt. Bobs-Boomerang area in southern Tasmania is rugged and mountainous&#13;
  182. (600-1080m above sea level), with a perhumid cool (Thornthwaire classification) climate and a range&#13;
  183. of geological substrates inclucling mudstone, sandstone, limestone and dolerite. 164 species of&#13;
  184. vascular plants, all native to Tasmania, have been recorded in the study area. The subalpine vegetation&#13;
  185. is composed primarily of rainforest and scrub communities. Fires have had major effects on these&#13;
  186. communities, but are rare; the period since the Last fire varies between about 50 and 500 years. A small&#13;
  187. area of herbland and heathland occupies the poorly drained valley fioors and different herbland&#13;
  188. communities are found on the flats and limestone cliffs around Lake Sydney.&#13;
  189. Above the treeline, which occurs at about 1000m on Mt. Bobs and the Boomerang, heathland&#13;
  190. is the major vegetation formation. Herblands are found in sheltered sites with the longest snowlie, and&#13;
  191. fjaeldmark, much of it associated with a pattern of non-sorted solifluction terraces, occupies the&#13;
  192. highest, most exposed part of the mudstone-capped Boomerang.&#13;
  193. Exposure to strong winds, snowlie, substrate type, degree of waterlogging and fire frequency&#13;
  194. appear to be major environmental delerminants of the plant communities.&#13;
  195.  </p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/270799.html">270000 Biological Sciences &gt; 270700 Ecology and Evolution &gt; 270799 Ecology and Evolution not elsewhere classified</a></td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">1843</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Professor J.B. Kirkpatrick</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">26 Sep 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">09 Jan 2008 02:30</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=1843;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&amp;eprintid=1843">item control page</a></p>
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