| Literature DB >> 30159447 |
Alan C Hamilton1, Deborah Karamura2, Esezah Kakudidi3.
Abstract
The history of wild and cultivated plant diversity in Uganda is reviewed, taking forest species and bananas as examples. Palynological research into past human influences on forests is reassessed. The evidence suggests that crops were first introduced into the country at about 1000 BCE, farming communities practicing slash and burn agriculture started to significantly influence the floristic composition of forests during the 1st millennium BCE and there was a major episode of forest reduction at about 1000 CE related to socio-economic change. Bananas were probably introduced in the early centuries CE. The colonial era from 1894 saw the introduction of new concepts of land ownership and the establishment of forest reserves and agricultural stations. Forests and banana diversity are currently under threat, Uganda having a very high rate of deforestation and endemic banana varieties proving susceptible to introduced pests and diseases. It is suggested that, under these circumstances, conservationists take an opportunistic approach to field engagement, making use of favourable local conditions as they arise. Partnerships should be sought with elements of society concerned with sustainable use, provision of ecosystem services and cultural survival to widen the social base of plant conservation. International organisations involved in conservation of plant genetic resources and wild plant species should collaborate with one another to develop the conceptual basis of plant conservation, to make it more relevant to countries like Uganda.Entities:
Keywords: Ecosystem-based plant conservation; Indigenous knowledge; Pollen diagrams; Resource governance
Year: 2016 PMID: 30159447 PMCID: PMC6112125 DOI: 10.1016/j.pld.2016.04.001
Source DB: PubMed Journal: Plant Divers ISSN: 2468-2659
Fig. 1Locality map of Uganda.
Types of bananas found on farms in Uganda according to two surveys.
| Genome group or type | Genome | Survey 1 (1993–1994) | Survey 2 (2004–2005) | Main uses | Origin and history | |||
|---|---|---|---|---|---|---|---|---|
| Frequency (% farms) | Proportion of plants | Commoner varieties (% farms) | Number of varieties identified | Commoner varieties (% farms) | ||||
| Tetraploid hybrids | AAAA | 4 | All bred outside Uganda. | |||||
| Triploid hybrid | AAA | 1 | Received from IPGRI. | |||||
| Gros Michel | AAA | 63 | 2 | 2 | Dessert | Gros Michel (= | ||
| Kamaramasenge | AAB | 92 | 12 | 1 | Dessert | |||
| Ney Poovan | AB | 1 | Brewing | |||||
| Pisang Awak | ABB | 67 | 8 | 2 | Brewing | Pisang Awak and Bluggoe probably brought to East African coast from India by Arab traders possibly ca. 500 CE; probably introduced into Uganda by British in colonial times. | ||
| Bluggoe | ABB | 2 | Multiuse | |||||
| East African Highland | AAA-EA | 100 | 76 | 82 | Cooking (to make | Long present in Great Lakes region of East Africa (many endemic varieties); probably brought to East African coast by Indonesians (possibly later than ancestor of Plantains). | ||
| Plantain | AAB | 43 | 2 | 3 | Roasting | Long present in Central and West Africa (many endemic varieties); probably brought to East African coast by Indonesians. | ||
The wild species contributing the genomes are M. acuminata Colla (AA diploid) and M. balbisiana Colla (BB diploid).
Survey 1 (Gold et al., 2002); Survey 2 (Edmeades and Karamura, 2007).
This is the percentage of plants assigned to genome groups or types, averaged across farms.
Farmers call all these tetraploid hybrids Kawanda.
This triploid hybrid (Yangambi Km5) was received from the International Plant Genetic Research Institute (IPGRI) (Kikulwe et al., 2007).
The second Gros Michel type encountered in the survey was Bogoya Omumyufu (Red Bugoya), found on 3% of farms.
Taxonomy after (Onyango et al., 2011).
Assignment of Ndiizi to the Kamaramesenge subgroup is after (Pillay et al., 2003).
The number of varieties of AAA-EA bananas noted in the other survey (Survey 1) was 120.
The 3 types recognised in Survey 2 were Gonja, Majaga and Manjaya. Most Ugandans do not distinguish between different varieties of Plantains.
Some major climatic events since 23 Myr BP that have moulded the floristic diversity of modern forests in Uganda.
| Time period | Climate | Rainforest |
|---|---|---|
| Last few centuries | Many climatic fluctuations, some geographically widespread, others apparently more local. | The influence of climatic events on rainforest in Uganda is difficult to discern against strong human influence on the vegetation. |
| From 4000 to 3500 BP | Drier than previously (but still wet compared with ice age aridity). | There was a transition to drier forest types at ∼4000–3500 BP in Uganda, experienced at all altitudes. |
| From 12,500 to 10,000 BP | Warmer and much wetter than previously. | The extent of forest expanded greatly in Uganda at ∼12,500–10,000 BP. |
| From 2.6 Myr BP | Marked climatic fluctuations in Africa, especially after 800,000 BP. | There were major contractions and expansions of forest in tropical Africa driven by the fluctuating climate. Differentiation and extinction of populations of forest species. |
| 23–2.6 Myr BP | Climate initially much wetter than now across tropical Africa, becoming progressively drier. | Forest was initially more extensive than now in tropical Africa, then retreating with species being lost. |
Dates are in years before present (BP), those based largely on radiocarbon dating (younger than ∼40,000 BP) being in 14C years before 1950 CE. Dates given in calendar years (BCE or CE) elsewhere in this paper are in calendar years, transposed from 14C years where necessary (Reimer et al., 2009).
The most detailed climatic records for the last ∼1000 years reveal fluctuations in climate of short to medium term duration (decades to centuries) (Ryves et al., 2011, Ssemmanda et al., 2005). A dry phase at ∼1750–1850 CE has been detected widely across East Africa. Similar short-term climatic fluctuations are likely to have occurred at all times.
A mid-Holocene shift to a drier climate has been widely recorded across equatorial and northern Africa, with the abruptness of the transition debated (McGlynn et al., 2013, Tierney et al., 2011). The date of ∼4000–3500 BP given here (equivalent to ∼2050–1850 BCE in calendar years) is one quoted in regional reviews (Hamilton, 1982, Hamilton, 1992, Jolly et al., 1997, Kiage and Liu, 2006). A notable feature seen in many pollen diagrams from Uganda is a rise in the very well dispersed pollen type Podocarpus (produced by the gymnosperm genera Afrocarpus and Podocarpus).
There is much evidence for a major transition from a relatively cool dry climate prevailing across equatorial Africa during the last global ice age (peaking at 18,000 BP) to warmer and much wetter conditions thereafter (the postglacial). The date of this transition given here is based on assessments of the pollen evidence for East Africa as a whole or parts thereof (Hamilton, 1982, Hamilton, 1992, Jolly et al., 1997, Kiage and Liu, 2006).
This is the Quaternary Period, marked by a series of ice ages in temperate parts of the world.
Several publications discuss climatic change during this period and its effects on the flora (Hamilton and Taylor, 1991, Harris et al., 2000, Jacobs, 2004, Plana, 2004, Sosef, 1994).
Fig. 2Archaeological and other sites in Uganda yielding evidence of pre-1900 AD influences of people on forests. Iron smelting areas after (Iles, 2009). The Luganda names of some geographical features are given in italics.
Sites of pollen diagrams from Uganda providing evidence (or possible evidence) of past influence of people on forest. Dates in calendar years, calibrated where necessary from radiocarbon dates (Reimer et al., 2009). Further explanatory notes in Appendix 1.
| Site and altitude (m) | Type of site | Immediate surrounding landscape | Past human influences |
|---|---|---|---|
High altitude sites | |||
| Muhavura, Virunga Volcanoes, 4127 m | Summit crater lake | Afroalpine vegetation | Widespread forest clearance around mountains, very well dated at ∼1000 CE. Peaks in charcoal in the sediments accompany the palynological indicators of forest clearance. Floristic composition of montane forest or woodland altered at ∼1000 CE. The same results for the two sites inspires confidence. |
| Gahinga, Virunga Volcanoes, 3474 m | Summit crater bog | ||
| Kitandara, Rwenzori 3990 m | Lakes | Afroalpine vegetation | Widespread forest clearance in lowlands around mountains at ∼1000 CE (the date is interpolated from considerably older radiocarbon dates). Forest clearance greater to the east than the west. |
| Bujuku, Rwenzori 3920 m | |||
| Mahoma, Rwenzori 2960 m | Bamboo forest | ||
Sites in the Rukiga Highlands | |||
| Muchoya, 2260 m | Valley swamps and a lake (Bunyonyi) | Bamboo forest | Signs of forest disturbance from ∼225 BCE, more so from ∼1250 CE. Some forest always remaining. Change in swamp vegetation during first millennium CE. |
| Mubwindi, 2100 m | Broadleaved forest | Slopes around swamp forested throughout. Signs of human disturbance from ∼1650 CE. | |
| Katenga, 1980 m | Small-scale farming, scrub, pasture | Major forest clearance with soil erosion and swamp siltation. Two episodes of forest disturbance at Ahakakyezi, ∼1700–750 BCE and ∼700 CE-present; soil erosion with second episode; final clearance of ridge forest at ∼1150 CE. | |
| Bunyonyi, 1950 m | |||
| Ahakagyezi, 1830 m | |||
Crater sediments, Kasenda (Ndale) Volcanic Field | |||
| Kabata, 1370 m | Crater swamp | Small-scale farming, grassland; forest nearby | Some opening up of forest at ∼1600 CE; possible human disturbance earlier (sometime between 1350 BCE and 400 CE). Spread of papyrus over a lake sometime between 400 and 1400 CE. |
| Kasenda, 1260 m | Crater lakes | Forest around sites replaced by grassland, well dated at ∼900–1000 CE. Some shrub and forest tree regrowth from ∼1700 to 1750 CE (especially from late 1800s). | |
| Wandakara, 1170 m | |||
Swamp associated with a Later Iron Age settlement at Munsa | |||
| Munsa, 1220 m | Papyrus swamp | Small-scale farming, grass, forest patches | Forest clearance well dated at ∼1100 CE with soil erosion and swamp siltation. Economy established with cereal cultivation, cattle-keeping, iron-smelting. Some forest recovery from ∼1780 CE. |
Large lowland lake | |||
| Pilkington Bay, Lake Victoria, 1134 m | Huge lake | Farmland, savannah, forest | Major forest clearance, well dated at ∼1 CE, shown by a major decrease in the ratio of forest to grass pollen. Accompanied by changes in wetland vegetation. Absolute decline in forest tree pollen starts earlier, sometime between 1750 and 1250 BCE. |
Sources:
(McGlynn et al., 2013).
(Livingstone, 1967).
(Morrison, 1968).
(Taylor, 1990).
(Marchant et al., 1997).
(Morrison and Hamilton, 1974).
(Hamilton et al., 1986).
(Hamilton et al., 1989).
(Taylor et al., 1999).
(Ssemmanda et al., 2005).
(Lejja et al., 2005).
(Kendall, 1969).
Allocation of land in Buganda under the Uganda Agreement of 1900 (West, 1965).
| Beneficiary | Total area | Components | |||
|---|---|---|---|---|---|
| sq. mi. | km2 | sq. mi. | km2 | ||
| Protectorate Government | 10,550 | 27,324 | Forests | 1500 | 3885 |
| Waste and uncultivated land | 9000 | 23,310 | |||
| Government stations | 50 | 129 | |||
| One thousand chiefs and private landowners | 8000 | 20,720 | |||
| The Kabaka and other dignitaries | 958 | 2481 | Private property | 750 | 1942 |
| Land attached to their offices | 208 | 539 | |||
| Mission societies | 92 | 238 | |||
| Estimated total area of Buganda | 19,600 | 50,764 | |||
The Uganda Memorandum of Agreement (Forest) of 25th October 1907 defined the extent to which forest could be included in mailo land (the part allocated to ‘chiefs and private landowners’). In general, all patches of forest over 0.5 sq. mi. (1.3 km2) were to be assigned to the Protectorate Government.
The total area of ‘waste and uncultivated land’ became reduced to an estimated 8307 sq. mi. (21,515 km2) once the actual area of Buganda became better known and was reduced again to 6804 sq. mi. (17,622 km2) when the counties of Buyaga and Bugangazi (Bugangaizi) were transferred from Buganda to Bunyoro following a referendum in 1964. This land is sometimes known as mailo akenda (‘the nine thousand mailo land’) (Mutengesa, 2012).
The land distributed to ‘chiefs and landowners’ came to be known as mailo land (from English ‘mile’). It appears that the original intention of the British was that there would be about 1000–1030 recipients. However, distribution of mailo land was made the responsibility of the Buganda parliament (lukiiko) under the Uganda Agreement and land came to be distributed to many more people than the British had apparently intended. The first Allotment List had 3650 names, then, with yet more added, the total number of allotees rose to 4138 in the first authoritative list (1905). Many of these claims had little or nothing to justify them. Numerous transactions in mailo land then followed (many not officially documented), resulting in an estimated total of 100,000 holders of mailo land by 1963.
The total area of Buganda at the completion of the original mailo survey in 1936 was found to be 17,310 sq. mi. (44,833 km2). This resulted in a reduction in the area of land assigned to the Protectorate Government (in its position as recipient of the residue of the estate).
Institutional history of forestry in Uganda.
| 1898 | First director of a new Scientific and Forestry Department appointed. |
| 1917 | Forest Department created. |
| 1929 | First formulation of forest policy, concentrating on forest reservation for environmental protection and timber production. |
| 1929–1951 | Large forests made Central Forest Reserves (CFRs) under the central government and small forests made Local Forest Reserves (LFRs) under local governments. (However, a survey in 1956–1960 found that a considerable area of forest in Buganda had come to fall under private hands.) |
| 1967 | CFRs and LFRs merged into the unitary category of Forest Reserves under the central government. |
| 1971–1973 | Forest policy adjusted favouring enlargement of conifer plantations for volume wood production. Little emphasis given to natural forest, either for its protective functions or for productive purposes. |
| 1993 | All forest reserves decentralised to local government, except five of the larger forests (Bwindi-Impenetrable, Elgon, Kibale, Mgahinga, Rwenzori) which were made national parks and transferred to the Uganda Wildlife Authority. |
| 1995 | All forest reserves recentralised. |
| 1997 | All forest reserves decentralised. |
| 1998 | Forest reserves over 100 ha recentralised (and labelled CFRs); forest reserves under 100 ha remaining with local authorities (and labelled LFRs). |
| 2001 | New forest policy agreed, emphasising a greater role for the private sector in forestry operations. |
| 2003 | Forest Department replaced by: (1) National Forest Authority (NFA), responsible for CFRs; (2) District Forest Services (DFS), responsible for LFRs and advice to private forest owners; (3) Forest Sector Support Department (FSSD), responsible for coordination and regulation. |
| 2006 | Board members of NFA resign or summarily dismissed, relating to conflict with the government over allocating parts of Mabira CFR and forests on the Ssese Islands to investors. New board members appointed. |
Field collections of bananas in Uganda. Sources: (Biggs, 1940, Blomme et al., 2012, Karamura and Mgenzi, 2004, Kikulwe et al., 2007, Thomas, 1940, Tothill, 1940).
| Institute | History |
|---|---|
| Entebbe Botanic Gardens | Founded 1898, especially to test the local suitability of potential economic crops. Banana varieties were introduced from many countries. Work on bananas was transferred to agricultural stations from 1910. |
| Kampala Plantation | Banana varieties accumulated from Buganda and Ankole (1919–1925) and trials of cooking bananas started (1927). The collection no long exists, related to expansion of Kampala city. |
| Bukalasa Agricultural College (formerly Bukalasa Substation) | Trials on banana varieties started 1927 using materials obtained from Kampala Plantation. The work was largely transferred to Kawanda in about 1940. A banana collection was re-established in the 1960s, eventually containing 600 accessions, but lost by 1985. |
| Kawanda Agricultural Research Institute (KARI) | Banana collection started 1940, but later lost. It was restarted in 1989, triggered by concern over discovery of Black Sikokota in Uganda (1988). When Uganda started a banana breeding (2003), the Kawanda collection was transferred to MZARDI. Kawanda then became developed as a collection of breeding lines. |
| Makerere University Agricultural Research Institute – Kabanyolo | Banana collection established 1989, but lost by 2004. A few representative samples exist in tissue culture. |
| Namulonge Agricultural Research Institute | Collection established in 2006–8 as part of a plan to move all research on crops from Kawanda to Namulonge. It contains about 100 accessions. A banana collection belonging to the International Institute of Tropical Agriculture (IITA) was started at Sendusu, near Namulonge, in the 1990s. |
| Mbarara Zonal Agricultural Research and Development Institute (MZARDI) | Banana collection started 1998 as a reference collection and to duplicate the collection at Kawanda. The collection became a regional collection in 2008 (for DR Congo, Kenya, Tanzania, Uganda) within the framework of the Banana Research Network for Eastern and Southern Africa (BARNESA). It currently has 450 accessions. It is run by the National Banana Programme (based in KARI) of NARO, backstopped by Bioversity International. The altitude is 1410 m. |
Today under National Agricultural Research Organisation (NARO).
Today under Ministry of Agriculture, Animal Industry and Fisheries.