Eocene paleobotanical altimetry of Victoria's Eastern Uplands |
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| Authors: | D R Greenwood R L Keefe T Reichgelt J A Webb |
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| Institution: | 1. Department of Biology, Brandon University, Brandon, Manitoba, R7A 6A9, Canada;2. Sustainability Office, Melbourne Polytechnic, Preston, Victoria 3072, Australia;3. Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA;4. Environmental Geoscience, Department of Ecology, Environment and Evolution, La Trobe University, Victoria 3086, Australia |
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| Abstract: | On the high-elevation, low-relief Bogong Plateau, within the Eastern Uplands in Victoria, well-preserved diverse macrofloras and microfloras have been recovered from Eocene sediments at two sites underlying Eocene–Oligocene basalts. Estimates of mean annual temperature (MAT) were made from the floras at each site, using a novel method calculating probability density functions and maximum likelihood co-occurrence climate envelopes of the nearest living relatives of multiple fossil taxa, and the proportion of non-toothed rather than toothed leaf margins of all fossil leaves. The most likely scenario is an Eocene MAT at Bogong Plateau of 18°C, consistent with the cloudy mesothermal montane environment indicated by the abundance of tree ferns and other flora. From the MAT, the maximum Eocene paleo-elevation of the flora sites on the plateau can be calculated using the ‘lapse rate’ method, and was probably around 550?700 m above sea-level (～1000 m lower than at present), but with large uncertainties for these estimates. The macrofloras accumulated in stream valleys, so the maximum elevation of the Eastern Uplands at the time was greater, matching other estimates of >800 m. Uplift to the present elevation probably occurred ca 8–4 Ma, so the alpine environment on the high plains dates to this time, and the high-altitude biota has therefore developed in the last 8 million years. |
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| Keywords: | paleo-elevation Eocene Australia paleobotany paleoclimate |
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