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Pleistocene macro-and micro-plant fossils fromRosebery, western Tasmania
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Colhoun, EA and Van de Geer, G 1987
, 'Pleistocene macro-and micro-plant fossils fromRosebery, western Tasmania'
, Papers and Proceedings of the Royal Society of Tasmania, vol. 121
, pp. 89-92
, doi: https://doi.org/10.26749/rstpp.121.89.
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Abstract
Fossils of Microstrobos niphophilus and pollen in glacial lake clays that underlie till of the Penultimate Glaciation of western Tasmania indicate that an alpine heathland-herbfield environment occurred at 200 to 240 m altitude, and that the temperature was at least 4.5 to 5° C colder than at present. Charcoal in the deposits indicates that fires occurred adjacent to ice long before Man arrived in Tasmania.
Item Type: | Article |
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Authors/Creators: | Colhoun, EA and Van de Geer, G |
Keywords: | Royal Society of Tasmania, RST, Van Diemens Land, natural history, science, ecology, taxonomy, botany, zoology, geology, geography, papers & proceedings, Australia, UTAS Library |
Journal or Publication Title: | Papers and Proceedings of the Royal Society of Tasmania |
ISSN: | 0080-4703 |
DOI / ID Number: | https://doi.org/10.26749/rstpp.121.89 |
Collections: | Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania |
Additional Information: | Copyright Royal Society of Tasmania |
Item Statistics: | View statistics for this item |
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