Holocene to Middle last glaciation vegetation history at Tullabardine Dam, western Tasmania
Pollen analysis of 4 m of peat, swamp-soil and lake sediments dated from 0 to > 43800 years b.p. indicates the occurrence of three major pollen assemblage zones. During Zone 1 (11000-0 years b.p.) the area had temperate rainforest and the climate was warm, moist and interglacial. During Zone 2 (...
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| Veröffentlicht in: | Proceedings of the Royal Society of London. Series B, Biological sciences Biological sciences, 1986-11, Vol.229 (1255), p.177-207 |
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| container_title | Proceedings of the Royal Society of London. Series B, Biological sciences |
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| creator | Colhoun, E. A. Van De Geer, G. West, Richard Gilbert |
| description | Pollen analysis of 4 m of peat, swamp-soil and lake sediments dated from 0 to > 43800 years b.p. indicates the occurrence of three major pollen assemblage zones. During Zone 1 (11000-0 years b.p.) the area had temperate rainforest and the climate was warm, moist and interglacial. During Zone 2 ( ?25000-l 1000 years b.p.), correlated approximately with the last period of glaciation, the vegetation was mainly grassland and the climate was considerably colder than present. In late glacial times (14000-11000 years b.p.) pollen of shrub and tree taxa increased, especially during the later part of the period as the climate became warmer and moister. During Zone 3 (more than 4 3 0 0 0 -?25000 years b.p.) the vegetation was predominantly sub-alpine and alpine. This vegetation represents an interstadial assemblage for a lowland site. The climate was cool and moist. The results are compared with sites of similar age in Tasmania, and with sites from temperate forest environments in Chile and New Zealand. |
| doi_str_mv | 10.1098/rspb.1986.0081 |
| format | Article |
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A. ; Van De Geer, G. ; West, Richard Gilbert</creator><creatorcontrib>Colhoun, E. A. ; Van De Geer, G. ; West, Richard Gilbert</creatorcontrib><description>Pollen analysis of 4 m of peat, swamp-soil and lake sediments dated from 0 to > 43800 years b.p. indicates the occurrence of three major pollen assemblage zones. During Zone 1 (11000-0 years b.p.) the area had temperate rainforest and the climate was warm, moist and interglacial. During Zone 2 ( ?25000-l 1000 years b.p.), correlated approximately with the last period of glaciation, the vegetation was mainly grassland and the climate was considerably colder than present. In late glacial times (14000-11000 years b.p.) pollen of shrub and tree taxa increased, especially during the later part of the period as the climate became warmer and moister. During Zone 3 (more than 4 3 0 0 0 -?25000 years b.p.) the vegetation was predominantly sub-alpine and alpine. This vegetation represents an interstadial assemblage for a lowland site. The climate was cool and moist. The results are compared with sites of similar age in Tasmania, and with sites from temperate forest environments in Chile and New Zealand.</description><identifier>ISSN: 0080-4649</identifier><identifier>ISSN: 0962-8452</identifier><identifier>EISSN: 2053-9193</identifier><identifier>EISSN: 1471-2954</identifier><identifier>DOI: 10.1098/rspb.1986.0081</identifier><identifier>CODEN: PRLBA4</identifier><language>eng</language><publisher>London: The Royal Society</publisher><subject>Alpine glaciers ; Charcoal ; Climate models ; Earth sciences ; Earth, ocean, space ; ecological succession ; Exact sciences and technology ; forests ; glacial deposits ; Glacial lakes ; glaciology ; grasslands ; Marine and continental quaternary ; Paleobotany ; Paleontology ; Pollen ; Rain forests ; Shrubs ; Surficial geology ; Swamps ; Taxa ; Vegetation</subject><ispartof>Proceedings of the Royal Society of London. 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A.</creatorcontrib><creatorcontrib>Van De Geer, G.</creatorcontrib><creatorcontrib>West, Richard Gilbert</creatorcontrib><title>Holocene to Middle last glaciation vegetation history at Tullabardine Dam, western Tasmania</title><title>Proceedings of the Royal Society of London. Series B, Biological sciences</title><addtitle>Proc. R. Soc. Lond. B</addtitle><addtitle>Proc. R. Soc. Lond. B</addtitle><description>Pollen analysis of 4 m of peat, swamp-soil and lake sediments dated from 0 to > 43800 years b.p. indicates the occurrence of three major pollen assemblage zones. During Zone 1 (11000-0 years b.p.) the area had temperate rainforest and the climate was warm, moist and interglacial. During Zone 2 ( ?25000-l 1000 years b.p.), correlated approximately with the last period of glaciation, the vegetation was mainly grassland and the climate was considerably colder than present. In late glacial times (14000-11000 years b.p.) pollen of shrub and tree taxa increased, especially during the later part of the period as the climate became warmer and moister. During Zone 3 (more than 4 3 0 0 0 -?25000 years b.p.) the vegetation was predominantly sub-alpine and alpine. This vegetation represents an interstadial assemblage for a lowland site. The climate was cool and moist. The results are compared with sites of similar age in Tasmania, and with sites from temperate forest environments in Chile and New Zealand.</description><subject>Alpine glaciers</subject><subject>Charcoal</subject><subject>Climate models</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>ecological succession</subject><subject>Exact sciences and technology</subject><subject>forests</subject><subject>glacial deposits</subject><subject>Glacial lakes</subject><subject>glaciology</subject><subject>grasslands</subject><subject>Marine and continental quaternary</subject><subject>Paleobotany</subject><subject>Paleontology</subject><subject>Pollen</subject><subject>Rain forests</subject><subject>Shrubs</subject><subject>Surficial geology</subject><subject>Swamps</subject><subject>Taxa</subject><subject>Vegetation</subject><issn>0080-4649</issn><issn>0962-8452</issn><issn>2053-9193</issn><issn>1471-2954</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1986</creationdate><recordtype>article</recordtype><recordid>eNp9Uk2P0zAQjRBIlMKVAxdy4EjK2E6c-ITY5aNIXYHYLkhwsKbJpHXJJpHt7lJ-PU6DKlWIvcSx5703z28cRU8ZzBio4pV1_WrGVCFnAAW7F004ZCJRTIn70SQcQZLKVD2MHjm3BUilUmIS_Zh3TVdSS7Hv4gtTVQ3FDTofrxssDXrTtfENrcmPvxvjfGf3Mfp4uWsaXKGtTCC_xeuX8S05T7aNl-iusTX4OHpQY-Poyd91Gl29f7c8nyeLTx8-nr9ZJCg5-KSoUiKeq-CnRq5SCN-yXAFwwZmo8pUkJZUgmbKcJGWlAKxJIpeKFwWQmEazUbe0nXOWat1bc412rxnoIRo9RKOHaPQQTSC8GAk9uhKb2mJbGndkFYyDCNlNIzHCbLcP_rvSkN_rbbezbdj-X9zdxfpy-fmMqUzdcK4M41mmoRAM8jRLc_3b9Ae5AaADQBvndqQPsNM2_3Z9NnbdDgM6XkVIlhWhmIzFMD36dSyi_allLvJMfy1SfbH4xue5-q4h4NmI35j15tZY0id3CZveutXB4MEay_PAeX0nZ7Bbdq2n1p8QdR3eke6rOig8HxVq7DSubZjI1SUHJoClAS1A_AEb8uSd</recordid><startdate>19861122</startdate><enddate>19861122</enddate><creator>Colhoun, E. A.</creator><creator>Van De Geer, G.</creator><creator>West, Richard Gilbert</creator><general>The Royal Society</general><general>Royal Society of London</general><scope>FBQ</scope><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19861122</creationdate><title>Holocene to Middle last glaciation vegetation history at Tullabardine Dam, western Tasmania</title><author>Colhoun, E. A. ; Van De Geer, G. ; West, Richard Gilbert</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a620t-8d4ee279993fa2940fa2ccb0023213d7b6e9693e6417e6e5c30afe6a2692880e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1986</creationdate><topic>Alpine glaciers</topic><topic>Charcoal</topic><topic>Climate models</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>ecological succession</topic><topic>Exact sciences and technology</topic><topic>forests</topic><topic>glacial deposits</topic><topic>Glacial lakes</topic><topic>glaciology</topic><topic>grasslands</topic><topic>Marine and continental quaternary</topic><topic>Paleobotany</topic><topic>Paleontology</topic><topic>Pollen</topic><topic>Rain forests</topic><topic>Shrubs</topic><topic>Surficial geology</topic><topic>Swamps</topic><topic>Taxa</topic><topic>Vegetation</topic><toplevel>online_resources</toplevel><creatorcontrib>Colhoun, E. A.</creatorcontrib><creatorcontrib>Van De Geer, G.</creatorcontrib><creatorcontrib>West, Richard Gilbert</creatorcontrib><collection>AGRIS</collection><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Proceedings of the Royal Society of London. Series B, Biological sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Colhoun, E. A.</au><au>Van De Geer, G.</au><au>West, Richard Gilbert</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Holocene to Middle last glaciation vegetation history at Tullabardine Dam, western Tasmania</atitle><jtitle>Proceedings of the Royal Society of London. Series B, Biological sciences</jtitle><stitle>Proc. R. Soc. Lond. B</stitle><addtitle>Proc. R. Soc. Lond. B</addtitle><date>1986-11-22</date><risdate>1986</risdate><volume>229</volume><issue>1255</issue><spage>177</spage><epage>207</epage><pages>177-207</pages><issn>0080-4649</issn><issn>0962-8452</issn><eissn>2053-9193</eissn><eissn>1471-2954</eissn><coden>PRLBA4</coden><abstract>Pollen analysis of 4 m of peat, swamp-soil and lake sediments dated from 0 to > 43800 years b.p. indicates the occurrence of three major pollen assemblage zones. During Zone 1 (11000-0 years b.p.) the area had temperate rainforest and the climate was warm, moist and interglacial. During Zone 2 ( ?25000-l 1000 years b.p.), correlated approximately with the last period of glaciation, the vegetation was mainly grassland and the climate was considerably colder than present. In late glacial times (14000-11000 years b.p.) pollen of shrub and tree taxa increased, especially during the later part of the period as the climate became warmer and moister. During Zone 3 (more than 4 3 0 0 0 -?25000 years b.p.) the vegetation was predominantly sub-alpine and alpine. This vegetation represents an interstadial assemblage for a lowland site. The climate was cool and moist. The results are compared with sites of similar age in Tasmania, and with sites from temperate forest environments in Chile and New Zealand.</abstract><cop>London</cop><pub>The Royal Society</pub><doi>10.1098/rspb.1986.0081</doi><tpages>31</tpages></addata></record> |
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| ispartof | Proceedings of the Royal Society of London. Series B, Biological sciences, 1986-11, Vol.229 (1255), p.177-207 |
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| language | eng |
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| source | JSTOR Archive Collection A-Z Listing |
| subjects | Alpine glaciers Charcoal Climate models Earth sciences Earth, ocean, space ecological succession Exact sciences and technology forests glacial deposits Glacial lakes glaciology grasslands Marine and continental quaternary Paleobotany Paleontology Pollen Rain forests Shrubs Surficial geology Swamps Taxa Vegetation |
| title | Holocene to Middle last glaciation vegetation history at Tullabardine Dam, western Tasmania |
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