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High resolution stable isotope analysis of a Tasmanian speleothem
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Desmarchelier, JM and Goede, A 1996
, 'High resolution stable isotope analysis of a Tasmanian speleothem'
, Papers and Proceedings of the Royal Society of Tasmania, vol. 130, no. 1
, pp. 7-13
, doi: https://doi.org/10.26749/rstpp.130.1.7.
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Abstract
High resolution oxygen and carbon isotope analyses of part of a uniform diameter stalagmite from a cave in northern Tasmania have been used to study the climatic transition from stadial to interstadial conditions during the early Last Glacial (109-95 ka). A significant change in oxygen isotope values suggests that temperature warmed rapidly by approximately 2°-3°C between 100 and 97 ka. A decrease in carbon isotope values between 101 and 98 ka indicates that moisture availability was increasing slightly in advance
of rising temperature.
Item Type: | Article |
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Authors/Creators: | Desmarchelier, JM and Goede, A |
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.130.1.7 |
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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