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Glacial-age water resources in inland
southeastern Australia
J Kemp
T Pietsch
J Olley
R Grun
C Pardoe
A Gontz
ARC (2013) Kiacatoo Man: biology, archaeology and
environment at the Last Glacial Maximum.
50 ka
Willandra Lakes – lake level record
?
?
34 ka
0 60 ka
50 ka?
?
?
0 60 ka
30 ka
0 60 ka
18 ka
16.2+1.6
20.3+1.5
0 60 ka
16 ka
16.2+1.9
13.1+1.5
18.8+1.4
0 60 ka
13 ka
13.4+1.3
0 60 ka
8 ka
7.7+1.0
8.3+0.8
5.2+0.4
5.5+0.4
9.2+1.1
0 60 ka
6 ka
0 60 ka
5 ka
0 60 ka
Fluvial reconstructions
Geophysical methods
ERT (Electrical Resistivity Tomography)– Schlumberger array, 2.5
m electrodes, d= 20 m
EM (Electromagnetic conductivity), d = 6 m
GPR (Ground Penetrating Radar), d= 0.1 m
EM ERT
131
132
133
134
135
136
0 50 100 150
Tocabil 1, Willandra Ck
Willandra Ck
132
134
136
138
0 50 100 150 200 250 300
E
Tocabil 2, Willandra Ck
Toc2
Toc1
Toc2
Toc1
Merrowie Ck
112
113
113
114
114
115
0 50 100 150 200
heightabovesealevel,metres
chainage in metres
Merrowie Ck palaeochannel,
Willandra
lake
levels
Lachlan-
Willandra
annual
floods
Conclusions
 Fluvial record allows quantitative record of water availability that complements
lake records in inland Australia
 Offer information about migration routes
 And the potential for archaeological finds.

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2018-08-31 - Tim Pietsch - Glacial age water resources in inland SE Australia

Editor's Notes

  1. Of course, land use change has complicated our interpretation of these events. And the present rate of increase in temperatures from the greenhouse effect is ten times faster than that which occurred in the post-glacial period, leading to questions about how quickly our landscapes can respond. But we need records of channel change in order to understand the lags in the system in order to successfully predict landscape (and climate) responses. Despite the transitions from arid to semi-arid and subhumid on the Riverine Plains over the past few thousand years, the channels reflect changes in the eastern highlands, through the complex and lagged effects of vegetation, soil and climate-controlled erosivity changes.