Abstract
Soil fertility is largely a function of climate, parent material and management of the soils. Parent materials are derived from various rock types. Most of the rocks in Africa are of Precambrian age, more than 544 million years old. The oldest rocks in Africa, Archean granites and granite gneisses as well as old volcanic rocks, called greenstones, are more than 3.2 billion years old. They form the stable granite–greenstone nuclei of the continent. Folded Precambrian metamorphic belts, the so-called mobile belts, accreted around these nuclei. While the granite and granite gneiss-dominated areas are mineralogically and chemically more homogenous, the areas underlain by deeply eroded Precambrian fold belts vary widely in composition. The African post-Precambrian (<544 million years) history is marked by the development of sedimentary basins with varying sedimentary rocks at the perimeter of the igneous and metamorphic stable continent. Extensive parts of the interior of Africa are covered by Mesozoic to Cenozoic sandstone-dominated basins. Soil rejuvenating volcanic rocks extruded from lower parts of the earth crust and mantle mainly during Mesozoic and Cenozoic times in linear zones. Massive volcanic outpourings took place since about 30 million years, in Tertiary Rift environments. Soils derived from these rock types vary. Soils derived from silica oversaturated igneous and metamorphic rocks as well as sandstone-dominated lithologies form sandy soils with limiting, inherently low nutrient concentrations and low water-holding capacities. In contrast, soils derived from volcanic, silica-saturated or silica-undersaturated igneous rocks, young or old, contain higher concentrations of total Ca, Mg, P and micronutrients. Under suitable climatic conditions they weather into more clay-rich, fertile soils with high water-holding capacities. Examples of strong inherent soil differences related to the underlying parent materials are given from Zimbabwe and Uganda. Inherent differences in soil properties can spatially vary over short distances. The main nutrient constraints of African soils are N and P deficiencies. Most soils are also low in organic matter. There are many soil fertility restoration management strategies, making use of local organic and imported and local inorganic nutrient resources, such as phosphate rocks and fertilizers. Africa is endowed with large deposits of naturally occurring agrominerals and fertilizer raw materials. Natural gas, the principal feedstock for industrial N fertilizer production, is found in coastal zones of Africa, mainly at the northern and western sides of the continent. Extensive sedimentary phosphate rock resources occur along the west coast of Africa and in North Africa. Igneous phosphate rocks are found mainly in eastern and Central Africa and along linear zones in West and southwest Africa. Large gypsum deposits occur in Mesozoic strata in coastal sedimentary basins. Calcium–magnesium carbonates, in various forms, occur in almost every country of the continent.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Asumadu K, Weil RR 1988. A comparison of the USDA soil taxonomy and the Zimbabwe soil classification system with reference to some red soils of Zimbabwe. Proceedings of an international symposium, Harare, Zimbabwe, 24–27 Feb 1986, IDRC-MR 170e, International Development Research Centre, Ottawa, ON, Canada, 413–445
Baker BH, Mohr PA, Williams LAJ (1972) Geology of the eastern rift system of Africa. Geol Soc Am Spec Paper136:1–67
Bationo A, Hartemink A, Lungu O, Naimi M, Okoth PF, Smaling E, Thiombiano L (2006) African soils: their productivity and profitability of fertilizer use. Background paper prepared for the African Fertilizer Summit June 9–13, 2006, Abuja, Nigeria, 25p. http://www.africafertilizersummit.org/Background_Papers/05%20Bationo-African%20Soils%20-%20Their%20Productivity.pdf
Bermúdez-Lugo O (2003) The mineral industry of Egypt. US Geol. Surv. Minerals yearbook 2002. http://minerals.usgs.gov/minerals/pubs/country
Bosse HR, Gwosdz W, Lorenz W, Markwich H, Roth W, Wolff F (1996) Limestone and dolomite resources of Africa. Geol Jb D102, Hannover, Germany, 532p
Botswana Department of Geological Survey (2003) The Department of Geological Survey Coalbed Methane Study. http://www.gov.bw/docs/dgscbmstudy.pdf
De Ruiter PAC (1979) The gabon and congo basins salt deposits. Econ Geol 74:419–431
De Swardt AMJ (1964) Lateritisation and landscape development in parts of equatorial Africa. Zeitschr Geomorph (N S) 3:313–333
Fyfe WS, Kronberg BI, Leonardos OH, Olorufemi N (1983) Global tectonics and agriculture: a geochemical perspective. Agric Ecosyst Environ 9:383–399
Hoffman PF, Kaufman AJ, Halverston GP, Schrag DP (1998) A neoproterozoic snowball Earth. Science 281:1342–1348
Holwerda JG, Hutchinson RW (1968) Potash-bearing evaporites in the Danakil area, Ethiopia. Econ Geol 63:124–150
Kampunzu AB, Popoff M (1991) Distribution of the main African rifts and associated magmatism. In: Kampunzu AB, Lubala RT (eds) Magmatism in extensional structural settings – the phanerozoic African plate. Springer, New York, NY, pp 2–10
King LC (1967) The morphology of the Earth, 2nd edn. Oliver and Boyd Ltd, Edinburgh
King BS (1978) Structural and volcanic evolution of the Gregory Rift. In: Bishop WW (ed) Geological background to fossil man. Geol Soc London. Scottish Academic Press, Edinburgh, pp 29–54
Laval M, Hottin AM (1992) The Mlindi ring structure: an example of an ultrapotassic pyroxenite to syenite differentiated complex. Geol Rdsch 81:737–757
Michalski B (1997) The mineral industry of Egypt. US Geol Surv Minerals Yearbook 1997. http://minerals.usgs.gov/minerals/pubs/country
Mitchel CJ, Simukanga S, Shitumbanuma V, Banda D, Walker B, Steadman EJ, Muibeya B, Mwanza M, Mtonga M, Kapindula D (2003) http://www.mineralsuk.com/britmin/farmlime_summary.pdf
Mobbs PM (2004) The mineral industry of Libya. US Geol Surv Minerals Yearbook 2004. http://minerals.usgs.gov/minerals/pubs/country
Nyamapfene K (1991) Soils of Zimbabwe. Nehanda Publishers, Harare
Retallack GJ, Dugas DP, Bestland EA (1990) Fossil soils and grasses of a Middle Miocene East African grassland. Science 247:1325–1328
Sanchez PA (2002) Soil fertility and hunger in Africa. Science 295:2019–2020
Sanchez PA, Shepherd KD, Soule MJ, Place FM, Buresh RJ, Izac AN (1997) Soil fertility replenishment in Africa: an investment in natural resource capital. In: Buresh RJ, Sanchez PA, Calhoun F (eds) Replenishing soil fertility in Africa. SSSA Spec Publ 51, Madison, WI, pp 1–46
Schlueter T (2006) Geological Atlas of Africa. Springer, New York, NY
Sheldon RP (1980) Episodicity of phosphate deposition and deep ocean circulation – a hypothesis. Soc Econ Paleont Mineral, Spec Publ 29:239–247
Slansky M (1986) Geology of sedimentary phosphates. North Oxford Academic Press, London
Stamford NP, Santos PR, Santos CRS, Freitas ADS, Dias SHL, Lira MA Jr (2007) Agronomic effectiveness of biofertilizers with phosphate rock, sulphur and Acidithiobacillus for yam grown on a Brazilian tableland acidic soil. Biores Techn 98:1311–1318
Theodoro SHa, Leonardos OH (2006) The use of rocks to improve family agriculture in Brazil. Ann Braz Acad Sci 78:721–730
Tromp PL, O’Hare AM, Martin A (1995) Coalbed methane exploration in developing countries: Integration of proven technology and sub-Saharan coal. In: Blenkinsop TG, Tromp PL (eds) Sub-Saharan economic geology. Geol Soc Zimbabwe, Spec Publ 3, Balkema, Rotterdam/Brookfield, pp 55–83
U.S. Geological Survey (2007) Mineral commodity summaries 2007: U.S. Geological Survey. United States Government Printing Office: Washington, 195p
Van Kauwenbergh SJ (2006) Fertilizer raw material resources of Africa. Reference Manual IFDC R-16, IFDC, Muscle Shoals, AL
van Straaten P (1989) Nature and structural relationships of carbonatites from Southwest and West Tanzania. In: Bell K (ed) Carbonatites, genesis and evolution. Unwin Hyman, London, pp 177–199
van Straaten P (2002) Rocks for crops – Agrominerals of sub-Saharan Africa. International Centre for Research in Agroforestry – ICRAF, Nairobi
van Straaten P (2007) Agrogeology – the use of rocks for crops. Enviroquest Ltd, Cambridge, ON
Weil RR, Mughogho SK (2000) Sulfur nutrition of maize in four regions of Malawi. Agr J 92:649–656
Williams LAJ, Chapman GR (1986) Relationships between major structure, salic volcanism and sedimentation in the Kenya Rift from the equator northward to Lake Turkana. In: Frostick LE, Renault RW, Reid I, Tiercelin JJ (eds) Sedimentation in the African Rifts. Geol Soc Spec Publ, 25, 59–74
Zeese R, Schwerdtmann U, Tietz GF, Jux U (1994) Mineralogy and stratigraphy of three deep lateritic profiles of the Jos plateau (Central Nigeria). Catena 21:195–214
Zingore S, Manyame C, Nyamufagata P, Giller KE (2005) Long-term changes in organic matter of woodland soils cleared for arable cropping in Zimbabwe. Eur J Soil Sci 56:727–736
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2011 Springer Science+Business Media B.V.
About this paper
Cite this paper
van Straaten, P. (2011). The Geological Basis of Farming in Africa. In: Bationo, A., Waswa, B., Okeyo, J., Maina, F., Kihara, J. (eds) Innovations as Key to the Green Revolution in Africa. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-2543-2_3
Download citation
DOI: https://doi.org/10.1007/978-90-481-2543-2_3
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-2541-8
Online ISBN: 978-90-481-2543-2
eBook Packages: Biomedical and Life SciencesBiomedical and Life Sciences (R0)