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Australian Journal of Botany Australian Journal of Botany Society
Southern hemisphere botanical ecosystems
RESEARCH ARTICLE

Aquifers: the ultimate groundwater-dependent ecosystems

William F. Humphreys
+ Author Affiliations
- Author Affiliations

Western Australian Museum, 49 Kew Street, Welshpool, WA 6106, Australia. Email: bill.humphreys@museum.wa.gov.au

Australian Journal of Botany 54(2) 115-132 https://doi.org/10.1071/BT04151
Submitted: 21 September 2004  Accepted: 1 August 2005   Published: 5 April 2006

Abstract

Australian aquifers support diverse metazoan faunas comprising obligate groundwater inhabitants, largely crustaceans but also including insects, worms, gastropods, mites and fish. They typically comprise short-range endemics, often of relictual lineages and sometimes widely vicariant from their closest relatives. They have been confined to subterranean environments from a range of geological eras and may contain information on the deep history of aquifers. Obligate groundwater fauna (stygobites) occurs in the void spaces in karst, alluvial and fractured rock aquifers. They have convergent morphologies (reduction or loss of eyes, pigment, enhanced non-optic senses, vermiform body form) and depend on energy imported from the surface except in special cases of in situ chemoautotrophic energy fixation. In Australia, many stygofaunas in arid areas occur in brackish to saline waters, although they contain taxa from lineages generally restricted to freshwater systems. They may occur alongside species belonging to taxa considered typical of the marine littoral although far removed in space and time from marine influence. The ecological attributes of stygofauna makes them vulnerable to changes in habitat, which, combined with their taxonomic affinities, makes them a significant issue to biodiversity conservation. The interaction of vegetation and groundwater ecosystems is discussed and, in places, there are conservation issues common to both.


Acknowledgments

I have learnt a great deal about aquifers and hydrogeology from discussions with Philip Commander and Kevin Morgan. I thank Stefan Eberhard, Ivana Karanovic and Tomislav Karanovic for permission to cite from their unpublished works. Ken Grimes generously provided the karst map. I appreciate the use of photographs by Chris Watts, Stefano Taiti and Joo-Lae Cho. Various parts of the work reported here were conducted under grants from Australian Heritage Council, Australian Research Council, Australian Biological Resources Study and the Butler Trust. The constructive comments of two anonymous referees are appreciated and resulted in improvements to the manuscript.


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