Effect of soil type on burrowing behavior and cocoon formation in the green-striped burrowing frog, Cyclorana alboguttata

Author:

Booth D.T.1

Affiliation:

1. School of Integrative Biology, The University of Queensland, Brisbane 4072, Australia.

Abstract

This study examined the effect of soil type on burrowing behaviour and cocoon formation during aestivation in the green-striped burrowing frog, Cyclorana alboguttata (Günther, 1867). Given a choice, frogs always chose to burrow in wet sand in preference to wet clay. Frogs buried themselves faster and dug deeper burrows in sandy soil. However, under my laboratory conditions, there was little difference in the pattern of soil drying between the two soil types. Frogs in both sand and clay soil experienced hydrating conditions for the first 3 months and dehydrating conditions for the last 3 months of the 6-month aestivation period, and cocoons were not formed until after 3 months of aestivation. After 6 months, there were more layers in the cocoons of frogs aestivating in sand than those aestivating in clay. Frogs were able to absorb water from sandy soil with water potentials greater than –400 kPa, but lost water when placed on sand with a water potential of –1000 kPa.

Publisher

Canadian Science Publishing

Subject

Animal Science and Zoology,Ecology, Evolution, Behavior and Systematics

Reference30 articles.

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2. Cogger, H.G. 1992. Reptiles and amphibians of Australia. Reed, Sydney, N.S.W.

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4. Gee, G.W., and Bauder, J.W. 1986. Particle-size analysis. In Methods of soil analysis. Part 1. Physical and mineralogical methods. Edited by A. Klute. Soil Society of America, Madison, Wis. pp. 383–412.

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