Climate change in the dead heart of Australia

Joshua Larsen1,2, Gerald Nanson1, Tim Cohen1, Brian Jones1, John Jansen3, Jan-Hendrick May1
1University of Wollongong, Australia 2Australian Nuclear Science & Technology Organisation (ANSTO) 3University of Glasgow, Scotland
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Continent: Australia
Country: Australia
State/Province:South Australia, Queensland
City/Town: none
UTM coordinates and datum: none


Climate Setting: Arid
Tectonic setting: Intracratonic Basin
Type: Stratigraphy, Chronology

Figure 1. Location of the major rivers, lakes, and dunefields in southeast central Australia. Details


Despite the absence of large-scale glaciation, the Australian continent has experienced substantial environmental change throughout the Quaternary period. This is especially pronounced in central Australia, where one seventh of the continent is drained internally to the depocentre, and lowest point in Australia, Lake Eyre (Figure 1). Research has shown that at one time, large sandy braided and meandering rivers carried water through dunefields to a large freshwater lake system. Today, the rivers are hostage to the dunefield, and floodwaters might only reach Lake Eyre once every ten years or so. In order to understand the development of this arid desert landscape, and how changing climates have affected it, we need to find out when rivers and dunes were active, and how they are related to each other.

Large volumes of fluvial and aeolian quartz sand have been deposited and reworked within central Australia throughout the Quaternary. This is an ideal material for luminescence dating techniques, which allow us to determine the length of time these grains have been buried. If we combine this dating method with detailed stratigraphy of the rivers and dunes, a picture of changing wet and dry environments begins to emerge. This approach has been taken in the Strzelecki Desert, where Cooper and Strzelecki Creeks run through an expansive linear dunefield.

Looking from above, be it from a satellite image or from an aircraft, it is obvious that contemporary river patterns are affected by the position of the linear dunes (Figures 1 & 2). It is also apparent that the linear dunes are grouped into discrete clusters, with a flat muddy floodplain in between (Figures 2 & 3). Interestingly, if we dig beneath the linear dunes and floodplain, we find abundant fluvial sands, which stand in stark contrast to the mud dominated fluvial system of today (Figure 4).

Why then, do we have so much fluvial sand beneath muddy floodplains and linear dunes? Clearly Cooper and Strzelecki Creeks were much more active in the past, and the substantially higher discharges allowed transportation of coarse sands in braided and meandering streams. Most of this fluvial sand was transported during previous interglacials (i.e. warm stages), albeit with declining amounts with each successive interglacial. However these rivers also maintained active channels throughout glacial periods (i.e. cold stages) as well, suggesting that although rainfall and discharge had declined, central Australia was not completely dry during glacial periods.

It is also clear that fluvial transportation of sand was the dominant source of sand for the linear dunefields. The rivers were probably seasonal, and this allowed sand to be blown from the channel and into 'source bordering' or transverse dune features running parallel to the channel. These large source bordering dunes were then reworked into the linear dune clusters that cover the Strzelecki Desert. The ages of the linear dunes do not seem to reveal any significant growth during glacial or interglacial periods, in fact, they have a very steady, linear growth rate for at least the last 100,000 years. This suggests that the development of linear dunes in central Australia was not directly driven by changes in global climate, but rather by local and regional changes in sediment supply.

What does all this tell us about climate change and dead heart of Australia? Large rivers once flowed across the Strzelecki Desert delivering sand, which could then be used to build the dunes. Discharge has steadily declined over the Quaternary, such that today, the rivers are a shadow of their former selves. The linear dunes have probably been slowly accreting throughout this time, building first from fluvial sands, and then from the re-working of smaller dunes. Central Australia has, therefore, been able to build its dunefields for at least the last 100,000 years, and probably much longer. It was also much wetter, especially during interglacials, and the rivers would have supported a diverse riparian habitat and fed large freshwater lakes. However, during the current interglacial, central Australia is just as arid, if not more arid, than during any previous glacial period. Why is this so? No one is really sure. Some researchers believe human arrival dramatically altered the vegetation which in turn altered the climate, whereas others believe the climate has changed all on its own as the continent has slowly drifted northwards. Whichever the case, it seems the dead heart of Australia has much more to reveal about climate change.

Associated References

  • Cohen, T.J., Nanson, G.C., Larsen, J.R., Jones, B.G., Price, D.M., Coleman, M., and Pietsch, T.J. Late Quaternary aeolian and fluvial interactions on the Cooper Creek Fan and the development of linear and source-bordering dunes, Strzelecki Desert, Australia. Quaternary Science Reviews, (in press).
  • Fitzsimmons, K.E., Rhodes, E.J., Magee, J.W., and Barrows, T.T. (2007) The timing of linear dune activity in the Strzelecki and Tirari Deserts, Australia. Quaternary Science Reviews, 26 (19-21) p. 2598-2616.
  • Magee, J.W, Miller, G.H., Spooner, N.A., and Questiaux, D. (2004) Continuous 150 k.y. monsoon record from Lake Eyre, Australia: Insolation forcing and unexpected Holocene failure. Geology, 32, p. 885-888.
  • Miller, G.H., Mangan, J., Pollard, D., Thompson, S., Felzer, B., Magee, J.W. (2005) Sensitivity of the Australian Monsoon to insolation and vegetation: implications for human impact on the continental moisture balance. Geology, 33 (1), p. 65-68.
  • Nanson, G.C., Price, D.M., and Short, S.A. (1992) Wetting and drying of Australia over the past 300 ka. Geology, 20 (9), p. 791-794.
  • Nanson, G. C., Price, D. M., Jones, B. G., Maroulis, J. C., Coleman, M., Bowman, H., Cohen, T. J., Pietsch, T. J. and Larsen, J. R. (2008). Alluvial evidence for major climate and flow regime changes during the middle and late Quaternary for eastern central Australia. Geomorphology, 101 (1-2), p. 109-129.
  • Pitman, A. J., and Hesse, P.P. (2007) The significance of large-scale land cover change on the Australian palaeomonsoon. Quaternary Science Reviews, 26 (1-20), p. 189-200.