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A 23,000-yr Pollen Record from Lake Euramoo, Wet Tropics of NE Queensland, Australia

Published online by Cambridge University Press:  20 January 2017

Simon G. Haberle*
Affiliation:
Resource Management in Asia-Pacific Program, Research School of Pacific and Asian Studies, Australian National University, Canberra, ACT 0200, Australia

Abstract

A new extended pollen and charcoal record is presented from Lake Euramoo, Wet Tropics World Heritage rainforest of northeast Queensland, Australia. The 8.4-m sediment core taken from the center of Lake Euramoo incorporates a complete record of vegetation change and fire history spanning the period from 23,000 cal yr B.P. to present. The pollen record is divided into five significant zones; 23,000–16,800 cal yr B.P., dry sclerophyll woodland; 16,800–8600 cal yr B.P., wet sclerophyll woodland with marginal rainforest in protected pockets; 8600–5000 cal yr B.P., warm temperate rainforest; 5000–70 cal yr B.P., dry subtropical rainforest; 70 cal yr B.P.–AD 1999, degraded dry subtropical rainforest with increasing influence of invasive species and fire.

The process of rainforest development appears to be at least partly controlled by orbital forcing (precession), though more local environmental variables and human activity are also significant factors. This new record provides the opportunity to explore the relationship between fire, drought and rainforest dynamics in a significant World Heritage rainforest region.

Type
Special issue articles
Copyright
University of Washington

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References

Anderson, D.M., Prell, W.L., and Barratt, N.J. (1989). Estimates of sea surface temperature in the Coral Sea at the last glacial maximum. Paleoceanography 4, 615627.CrossRefGoogle Scholar
Appleby, P.G., and Oldfield, F. (1983). Assessment of 210Pb from sites with varying sediment accumulation rates. Hydrobiologia 103, 2935.CrossRefGoogle Scholar
Barrows, T.T., and Juggins, S. (2005). Sea-surface temperatures around the Australian margin and Indian Ocean during the Last Glacial Maximum. Quaternary Science Reviews 24, 10171047.CrossRefGoogle Scholar
Bennett, K.D. (1994). ‘psimpoll’ version 2.23: a C program for analysing pollen data and plotting pollen diagrams. INQUA Commission for the study of the Holocene: working group on data-handling methods. Newsletter 11, 46.Google Scholar
Bennett, K.D. (1996). Determination of the number of zones in a biostratigraphical sequence. New Phytologist 132, 155170.CrossRefGoogle Scholar
Bennett, K.D., and Willis, K.J. (2001). Pollen. Smol, J.P., Birks, H.J.B., Last, W.M. Tracking Environmental Change Using Lake Sediments. Terrestrial, Algal, and Siliceous Indicators vol. 3, Kluwer, Dordrecht.532.CrossRefGoogle Scholar
Berger, A., and Loutre, M.F. (1991). Insolation values for the climate of the last 10 million of years. Quaternary Science Reviews 10, 297317.CrossRefGoogle Scholar
Birks, H.J.B., and Gordon, A.D. (1985). Numerical Methods in Quaternary Pollen Analysis. Academic Press, London.317pGoogle Scholar
Birks, H.J.B., and Line, J.M. (1992). The use of rarefaction analysis for estimating palynological richness from Quaternary pollen-analytical data. The Holocene 2, 110.CrossRefGoogle Scholar
Birtles, T. (1988). European interpretation of the Atherton-Evelyn vine scrub of tropical north Queensland, 1880–1920. Dargavel, J., Dixon, K., and Semple, N. Changing Tropical Forests: Historical Perspectives on Today's Challenges in Asia, Australasia and Oceania. Centre for Resource and Environmental Studies Publication, Australian National University, Canberra.197216.Google Scholar
Chen, Y. (1988). Early Holocene population expansion of some rainforest trees at Lake Barrine basin, Queensland. Australian Journal of Ecology 13, 225233.CrossRefGoogle Scholar
Clark, R.L., and Guppy, J.C. (1988). A transition from mangrove forest to freshwater wetland in monsoon tropics of Australia. Journal of Biogeography 15, 665684.CrossRefGoogle Scholar
Crowley, G.M. (1994). Quaternary soil salinity events and Australian vegetation history. Quaternary Science Reviews 13, 1522.CrossRefGoogle Scholar
Dai, A., and Wigley, T.M.L. (2000). Global patterns of ENSO-induced precipitation. Geophysical Research Letters 27, 12831286.CrossRefGoogle Scholar
Gagan, M.K., Hendy, E.J., Haberle, S.G., and Hantoro, W.S. (2004). Post-glacial evolution of the Indo-Pacific Warm Pool and El Niño-Southern Oscillation. Quaternary International 118–119, 127143.CrossRefGoogle Scholar
Godfred-Spenning, C.R., and Reason, C.J.C. (2002). Interannual variability of lower-tropospheric moisture transport during the Australian Monsoon. International Journal of Climatology 22, 509532.CrossRefGoogle Scholar
Haberle, S.G., and Chepstow-Lusty, A. (2000). Can climate influence cultural development?: a view through time. Environment and History 6, 349369.CrossRefGoogle Scholar
Haberle, S.G., and David, B. (2004). Climates of change: human dimensions of Holocene environmental change in low latitudes of the PEPII transect. Quaternary International 118–119, 165179.CrossRefGoogle Scholar
Haberle, S.G., Hope, G.S., and van der Kaars, W.A. (2001). Biomass burning in Indonesia and Papua New Guinea: natural and human induced fire events in the fossil record. Palaeogeography, Palaeoclimatology, Palaeoecology 171, 259268.CrossRefGoogle Scholar
Hayne, M., and Chappell, J. (2001). Cyclone frequency during the last 5000 years at Curacoa Island, north Queensland, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 168, 207219.CrossRefGoogle Scholar
Hill, R., and Baird, A. (2003). Kuku-Yalanji rainforest aboriginal people and carbohydrate resource management in the Wet Tropics of Queensland, Australia. Human Ecology 31, 2752.CrossRefGoogle Scholar
Hiscock, P., and Kershaw, A.P. (1992). Palaeoenvironments and prehistory of Australia's tropical Top End. Dodson, J. The Niave Lands: Prehistory and Environmental Change in Australia and the Southwest Pacific. Longman Cheshire, Melbourne.4375.Google Scholar
Horsfall, N. (1987). Aborigines and toxic north-eastern Queensland rainforest plants. Covacevich, J., Davie, P., and Pearn, J. Toxic Plants and Animals: A Guide for Australia. Queensland Museum, Brisbane.5763.Google Scholar
Kershaw, A.P. (1970). A pollen diagram from Lake Euramoo, North-East Queensland, Australia. New Phytologist 69, 785805.CrossRefGoogle Scholar
Kershaw, A.P. (1971). A pollen record from Quincan Crater, north-east Queensland, Australia. New Phytologist 70, 669805.CrossRefGoogle Scholar
Kershaw, A.P. (1975). Stratigraphy and pollen analysis of Bromfield Swamp, north-eastern Queensland, Australia. New Phytologist 75, 173191.CrossRefGoogle Scholar
Kershaw, A.P. (1978). The analysis of aquatic vegetation on the Atherton Tablelands, north-east Queensland, Australia. Australian Journal of Ecology 3, 2342.CrossRefGoogle Scholar
Kershaw, A.P. (1983). A Holocene pollen record from Lynch's Crater, north-eastern Queensland, Australia. New Phytologist 94, 669682.CrossRefGoogle Scholar
Kershaw, A.P. (1994). Pleistocene vegetation of the humid tropics of northeastern Queensland, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 109, 399412.CrossRefGoogle Scholar
Kershaw, A.P., and Nix, H.A. (1988). Quantitative palaeoclimatic estimates from pollen using bioclimatic profiles of extant taxa. Journal of Biogeography 15, 589602.CrossRefGoogle Scholar
Kershaw, A.P., van der Kaars, S., Moss, P.T., and Wang, X. (2002). Quaternary records of vegetation, biomass burning, climate and possible human impact in the Indonesian-Northern Australian region. Kershaw, A.P., David, B., Tapper, N.J., Penny, D., and Brown, J. Bridging Wallace's Line: The Environmental and Cultural History and Dynamics of the Southeast Asian-Australian Region. Catena Verlag, Reiskirchen, Germany.97118.Google Scholar
Maslin, M. (2004). Ecological versus climatic thresholds. Science 306, 21972198.CrossRefGoogle ScholarPubMed
Moss, P.T., and Kershaw, A.P. (2000). The last glacial cycle from the humid tropics of Australia: comparison of a terrestrial and marine record. Palaeogeography, Palaeoclimatology, Palaeoecology 155, 155176.CrossRefGoogle Scholar
Mueller-Dombois, D., and Fosberg, F.R. (1998). Vegetation of the Tropical Pacific Islands. Springer, New York.CrossRefGoogle Scholar
Powell, J.M. (1982). The history of plant use and man's impact on the vegetation. Gressitt, J.L. Biogeography and Ecology of New Guinea. Junk, The Hague.207227.Google Scholar
Rodbell, D.T., Seltzer, G.O., Anderson, D.M., Abbott, M.B., Enfield, D.B., and Newman, J.H. (1999). An ∼15,000-year record of El Niño-driven alluviation in southwestern Ecuador. Science 283, 516520.CrossRefGoogle ScholarPubMed
Sandweiss, D.H., Richardson, J.B. III Reitz, E.J., Rollins, H.B., and Maasch, K.A. (1996). Geoarchaeological evidence from Peru for a 5000 years B.P. onset of El Niño. Science 273, 15311533.CrossRefGoogle Scholar
Stuiver, M., and Reimer, P.J. (1993). Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, 215230.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., van der Plicht, J., and Spurk, M. (1998). INTCAL98 Radiocarbon age calibration 24,000-0 cal B.P.. Radiocarbon 40, 10411083.CrossRefGoogle Scholar
Thomas, M.F., Nott, J., and Price, D.M. (2001). Late Quaternary stream sedimentation in the humid tropics: a review with new data from NE Queensland, Australia. Geomorphology 39, 5368.CrossRefGoogle Scholar
Timms, B.V. (1976). Morphology of Lakes Barrine, Eacham and Euramoo, Atherton Tableland, North Queensland. Proceedings of the Royal Society of Queensland 87, 8184.Google Scholar
Turney, C.S.M., Kershaw, A.P., Clemens, S.C., Branch, N., Moss, P.T., and Fifield, L.K. (2004). Millennial and orbital variations of El Niño/Southern Oscillation and high-latitude climate in the last glacial period. Nature 428, 306310.CrossRefGoogle ScholarPubMed
Walker, D., and Chen, Y. (1987). Palynological light on tropical rainforest dynamics. Quaternary Science Reviews 6, 7792.CrossRefGoogle Scholar
Woodroffe, C.D., Kennedy, D.M., Hopley, D., Rasmussen, C., and Smithers, S.G. (2000). Holocene reef growth in Torres Strait. Marine Geology 170, 331346.CrossRefGoogle Scholar
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