Demographic Effects of Severe Fire in Montane Shrubland on Tasmania’s Central Plateau
Australian montane sclerophyll shrubland vegetation is widely considered to be resilient to infrequent severe fire, but this may not be the case in Tasmania. Here, we report on the vegetative and seedling regeneration response of a Tasmanian non-coniferous woody montane shrubland following a severe...
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Published in | Fire (Basel, Switzerland) Vol. 4; no. 3; p. 32 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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01.09.2021
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Abstract | Australian montane sclerophyll shrubland vegetation is widely considered to be resilient to infrequent severe fire, but this may not be the case in Tasmania. Here, we report on the vegetative and seedling regeneration response of a Tasmanian non-coniferous woody montane shrubland following a severe fire, which burned much of the Great Pine Tier in the Central Plateau Conservation Area during the 2018–2019 fire season when a historically anomalously large area was burned in central Tasmania. Our field survey of a representative area burned by severe crown fire revealed that more than 99% of the shrubland plants were top-killed, with only 5% of the burnt plants resprouting one year following the fire. Such a low resprouting rate means the resilience of the shrubland depends on seedling regeneration from aerial and soil seedbanks or colonization from plants outside the burned area. Woody species’ seedling densities were variable but generally low (25 m−2). The low number of resprouters, and reliance on seedlings for recovery, suggest the shrubland may not be as resilient to fire as mainland Australian montane shrubland, particularly given a warming climate and likely increase in fire frequency. |
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AbstractList | Australian montane sclerophyll shrubland vegetation is widely considered to be resilient to infrequent severe fire, but this may not be the case in Tasmania. Here, we report on the vegetative and seedling regeneration response of a Tasmanian non-coniferous woody montane shrubland following a severe fire, which burned much of the Great Pine Tier in the Central Plateau Conservation Area during the 2018–2019 fire season when a historically anomalously large area was burned in central Tasmania. Our field survey of a representative area burned by severe crown fire revealed that more than 99% of the shrubland plants were top-killed, with only 5% of the burnt plants resprouting one year following the fire. Such a low resprouting rate means the resilience of the shrubland depends on seedling regeneration from aerial and soil seedbanks or colonization from plants outside the burned area. Woody species’ seedling densities were variable but generally low (25 m−2). The low number of resprouters, and reliance on seedlings for recovery, suggest the shrubland may not be as resilient to fire as mainland Australian montane shrubland, particularly given a warming climate and likely increase in fire frequency. Australian montane sclerophyll shrubland vegetation is widely considered to be resilient to infrequent severe fire, but this may not be the case in Tasmania. Here, we report on the vegetative and seedling regeneration response of a Tasmanian non-coniferous woody montane shrubland following a severe fire, which burned much of the Great Pine Tier in the Central Plateau Conservation Area during the 2018–2019 fire season when a historically anomalously large area was burned in central Tasmania. Our field survey of a representative area burned by severe crown fire revealed that more than 99% of the shrubland plants were top-killed, with only 5% of the burnt plants resprouting one year following the fire. Such a low resprouting rate means the resilience of the shrubland depends on seedling regeneration from aerial and soil seedbanks or colonization from plants outside the burned area. Woody species’ seedling densities were variable but generally low (25 m −2 ). The low number of resprouters, and reliance on seedlings for recovery, suggest the shrubland may not be as resilient to fire as mainland Australian montane shrubland, particularly given a warming climate and likely increase in fire frequency. |
Author | Leonard, Steven W. J. Prior, Lynda D. Foulkes, Judy A. Bowman, David M. J. S. |
Author_xml | – sequence: 1 givenname: Judy A. surname: Foulkes fullname: Foulkes, Judy A. – sequence: 2 givenname: Lynda D. orcidid: 0000-0002-5511-2320 surname: Prior fullname: Prior, Lynda D. – sequence: 3 givenname: Steven W. J. surname: Leonard fullname: Leonard, Steven W. J. – sequence: 4 givenname: David M. J. S. orcidid: 0000-0001-8075-124X surname: Bowman fullname: Bowman, David M. J. S. |
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CitedBy_id | crossref_primary_10_1007_s10113_024_02358_6 crossref_primary_10_1016_j_foreco_2021_119922 crossref_primary_10_1007_s10980_022_01558_x crossref_primary_10_1080_03736245_2025_2481851 crossref_primary_10_1071_BT23085 crossref_primary_10_3390_fire4040092 crossref_primary_10_1016_j_tfp_2024_100695 crossref_primary_10_3390_fire5020033 crossref_primary_10_1071_BT23069 crossref_primary_10_1007_s10113_022_01954_8 |
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SubjectTerms | buried seeds climate Climate change Colonization Conservation areas crown fire fire frequency fire season fire severity Forest & brush fires Grasslands Livestock montane shrubland Orites revoluta Plant populations post-fire regeneration response Precipitation Regeneration Resilience Seed banks Seedlings Seeds Shrublands surveys Tasmania Vegetation woody plants |
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Title | Demographic Effects of Severe Fire in Montane Shrubland on Tasmania’s Central Plateau |
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