Grassroots Grassroots - Vol 20 No 1 | Page 6

FEATURE Figure 4: A functionally healthy valley sequence to its floodplain and then how the whole drainage ecosystem can become essentially a ”tiled roof with drain pipes”, etching out all the critical habitats in the process (Pringle & Tinley, 2003). Prevention is better than cure: If one believes that prevention is better than cure, it is imperative that all activities that involve the unnatural cutting of the nat- ural landscape are stopped, or planned very carefully. In particular, the sills that hold up the ponding of local wetlands should be protected on-site. For in- stance, by locating artificial watering points across slope rather than above or below wetland sills and avoiding track alignment near these fragile areas can minimise the threat of initiating gully head cuts into them from downslope or the diversion of flows elsewhere from upslope areas (Pringle et al., 2019). The key issue is to maintain critical natural landscape base levels that enable water retention, thereby supporting all of the key biodiversity values that result from nested patterns of small to very large wetlands, the “jewels in the crown” of any drainage ecosystem. Concluding comment: Landscape inci- sion is episodic but fast. It often works against natural, slow landscape succes- sion processes that create areas of great- er soil moisture balance and landscape productivity (Noy Meir, 1980) as well as critical, nested, drought buffering habi- tats (Newsome, 1980; McNaughton, 1983; Illius & O'Connor, 2000). Human- induced gullies and their devastating effects of landscape droughting and ecosystems’ drought buffering are not an issue specific to commercial land use as causative processes also affect lands set aside for biodiversity conservation. Gully development adheres to the laws of physics everywhere and can affect any land where a nick point is created by the cutting of the natural land sur- face. Generally, the effects of gully de- Figure 5: The unplugging of a wetland (Ken Tinley). velopment and expansion are at odds with most land management objectives, especially in relation to wetlands in their wide, arid context. Most importantly, gully head cuts are usually expanding their “stealing” of rangeland ecosys- tems’ most valuable resource: soil mois- ture. Acknowledgements Ken Tinley (D.Sc.) opened my eyes to the importance of physical landscape succession processes in ecological land management whatever the primary and other objectives of those managing the land. He also drew all the diagrams in this article, in cases with help from his wife Lynne. The Tinleys and Russell Grant kindly reviewed the initial drafts in detail. References 1. Clements, F.E. (1916) Plant Succession: An Analysis of the Development of Vegetation. In. Carnegie Institute of Washing- ton 2. Cole, M. (1963) Vegetation and geomorphology in northern Rhodesia: An aspect of the distribution of savanna of Cen- tral Africa. Geography Journal, 129, 290-310. 3. Cooke, R.U. & Reeves, R.W. (eds) (1976) Arroyos and Environmental Change in the American South-West. Clarendon Press, Oxford. 4. Cowles, C.C. (1901) The physiographic ecology of Chicago and vicinity: A study of the origin, development and classifi- cation of plant societies. Botanical Gazette, 31, 73-108. 5. Duguid, A., Barnetson, J., Clifford, B., Pavey, C., Albrecht, D., Risler, J. & McNellie, M. (2005) Wetlands in the North- ern Territory vol. 1. A report to the Austraian Government Department of Environment and Heritage on the inventory and significance of wetlands in the Northern Territory. In. Department of Natural Resources, Environment and the Arts, Northern Territory Government, Darwin. 6. Fanning, P. (1994) Long-term contemporary erosion rates in an arid rangelands environment in western New South Wales, Australia. Journal of Arid Environments, 28, 173-187. 7. Fynn, R.S. (2012) Functional resource heterogeneity increases livsetock and rangeland productivity. Rangeland Ecology 05 Grassroots Vol 20 No 1 March 2020