Martin Thoms

Prof. Martin Thoms

University of New England, Australia
orcid

Research Focus & Metrics

Academic Career Length

41Years (1986-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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7 February 2006 in River Research and Applications
Verified
Journal Article
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JTJames H. Thorp
James H. Thorp
Martin ThomsMartin Thoms
Martin Thoms
MDMichael D. Delong
Michael D. Delong

1 March 1999 in Freshwater Biology
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Journal Article
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PDF file
RNRichard H. Norris
Richard H. Norris
Martin ThomsMartin Thoms
Martin Thoms

7 February 2006 in River Research and Applications
Verified
Journal Article
Closed access
PDF file
SBStuart Bunn
Stuart Bunn
Martin ThomsMartin Thoms
Martin Thoms
SHStephen K. Hamilton
Stephen K. Hamilton
Samantha J. CaponSamantha J. Capon
Samantha J. Capon


1 May 1993 in Regulated Rivers: Research & Management
Verified
Journal Article
Closed access
PDF file
KWK. F. Walker
K. F. Walker
Martin ThomsMartin Thoms
Martin Thoms

4 February 2005 in Marine and Freshwater Research
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Journal Article
Closed access
PDF file
AAAngela H. Arthington
Angela H. Arthington
SBStephen R. Balcombe
Stephen R. Balcombe
GWGlenn A. Wilson
Glenn A. Wilson
Martin ThomsMartin Thoms
Martin Thoms
JMJon Marshall
Jon Marshall
Spatial and temporal variation in fish-assemblage structure within isolated waterholes on the floodplains of Cooper Creek, Australia, was studied during the 2001 dry season, a period of natural drought in this arid-zone river. Spatial variation in fish-assemblage structure and the abundance of five species in disconnected waterholes early in the dry season (April 2001) were related to the extent of floodplain inundation 14 months previously, and to the interconnectedness of waterholes and waterhole habitat structure. As the dry season progressed, waterhole volumes decreased owing to evaporative water loss and structural habitat elements (anabranches, bars, boulders) became exposed. Marked changes in fish assemblage structure between the early (April) and late (September) dry season were related to habitat loss but not to water chemistry. Interactions between flow and habitat across a nested hierarchy of spatial scales (the floodplain, the waterhole and habitat patches within waterholes) were crucial to the persistence of fish assemblages through the 2001 dry season. We conclude that the magnitude, timing and frequency of floodplain inundation and natural variations in waterhole volume must be maintained if we wish to sustain the distinctive habitats and fish assemblages of this arid-zone floodplain river.