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Treatise on Geomorphology 2013
DOI: 10.1016/b978-0-12-374739-6.00335-3
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12.19 Effects of Ants and Termites on Soil and Geomorphological Processes

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Cited by 30 publications
(30 citation statements)
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“…Published estimates indicate that >10 kyr are required to produce a stone layer at depths <1 m, with some evidence that these take 20–30 kyr to form. Field estimates for northern Australia (11.5 to greater than 17.7 kyr; Williams, ) are broadly consistent with global estimates of soil turnover by termites (Holt et al, ; Nye, ; Whitford & Eldridge, , table 2) and with experimental data on turnover rates (Salvador‐Blanes, Minasny, & McBratney, ).…”
Section: Modeling the Development Of Termite Stone Layerssupporting
confidence: 74%
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“…Published estimates indicate that >10 kyr are required to produce a stone layer at depths <1 m, with some evidence that these take 20–30 kyr to form. Field estimates for northern Australia (11.5 to greater than 17.7 kyr; Williams, ) are broadly consistent with global estimates of soil turnover by termites (Holt et al, ; Nye, ; Whitford & Eldridge, , table 2) and with experimental data on turnover rates (Salvador‐Blanes, Minasny, & McBratney, ).…”
Section: Modeling the Development Of Termite Stone Layerssupporting
confidence: 74%
“…There are no quantitative data on the relationship between termite abundance (population density) and soil turnover rate although these variables can be assumed to be positively correlated. In northern Australia, field estimates of turnover rates of 0.48 m 3 ·ha −1 ·year −1 (equivalent to 0.521 ton·km −2 ·year −1 ; Williams, ) are of the same order as experimental approximations (~1.1 ton·km −2 ·year −1 ) and global estimates (300–3000 kg·ha −1 ·year −1 ; Whitford & Eldridge, , table 2). Estimates of the rate of deposition of fine sediments on the ground surface in northern Australia vary but are mostly >2.5 mm/100 year (2.5–50 mm/100 year, Holt et al, ; 10 mm/100 year, Lee & Wood, , p. 251).…”
Section: Modeling the Development Of Termite Stone Layersmentioning
confidence: 74%
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“…This would likely extend the period over which decomposition and mineralization occur. Echidnas often burrow into the nests of ants and termites, which are themselves ecosystem engineers that enhance soil physical and chemical properties through their central place foraging (Whitford & Eldridge ). It is probable, therefore, that some of the chemical differences that we measured in echidna foraging pits could result from the build‐up of nitrogen and carbon due to invertebrate activity.…”
Section: Resultsmentioning
confidence: 99%