A geomorphological based banded ('tiger') vegetation pattern related to former dune fields in Sokoto (Northern Nigeria)

Authors
Citation
Is. Zonneveld, A geomorphological based banded ('tiger') vegetation pattern related to former dune fields in Sokoto (Northern Nigeria), CATENA, 37(1-2), 1999, pp. 45-56
Citations number
23
Categorie Soggetti
Environment/Ecology
Journal title
CATENA
ISSN journal
03418162 → ACNP
Volume
37
Issue
1-2
Year of publication
1999
Pages
45 - 56
Database
ISI
SICI code
0341-8162(199909)37:1-2<45:AGBB(V>2.0.ZU;2-K
Abstract
A banded vegetation pattern has been observed on aerial photographs of Soko to province in Northern Nigeria. It was successfully used as a land mapping characteristic in the soil and vegetation (land unit) reconnaissance surve y see FAO (1969) [FAO, 1969. Soils Survey and Land Classification, Soils an d Water Resources Survey of the Sokoto Valley (Nigeria). Final report Vol. V, FAO/SF:67/Nr3.], Zonneveld et al. (1971) [Zonneveld, LS., de Leeuw, P.N. , Sombroek, W.G,, 1971. An ecological interpretation of aerial photographs in a savanna region in northern Nigeria. Publication of the International I nstitute for Aerial Survey and Earth Sciences (ITC) Enschede, The Netherlan ds, 41 pp.], The banded pattern is visible through vegetation density relat ed to differences in surface hydrology. The latter are caused by variation in soil sealing that is connected with a by sheet erosion (pediplanisation) levelled former early Holocene to late Pleistocene dune landscape (Sangiwa coversand landscape). The difference in sealing is related to a (very smal l) difference in silt content between the levelled former dunes and the fil led in valleys in combination with extreme low organic matter content. The lower silt content in the valley filling is connected with the re-sedimenta tion process, a feature well known in coversand formation. The sealing is a present day process. Fresh loosened soil material (by ploughing and soil p it digging) is after one rain shower already covered with a sealed crust of several millimetres through which no water penetrates, The orientation of the bands (about NNW-SSE) is perpendicular to the prevailing wind direction (ENE-WSW) during the period of formation of the former dunes, The genesis of this pattern of regional scale appears to be quite different from local scale banded patterns known to us in dry zones in Africa and Asia and descr ibed, in the same period of our study as 'Brousse tigree', being moving veg etation arcs related to sheet runoff and by consequence oriented perpendicu lar to that water flow. (C) 1999 Elsevier Science B.V. All rights reserved.