Vascular Plants in Eastern Africa Rift Valley Saline Wetlands

2016 ◽  
pp. 285-293 ◽  
Author(s):  
Julius Kipkemboi
2021 ◽  
Author(s):  
Femke Augustijns ◽  
Nils Broothaerts ◽  
Gert Verstraeten

<p>Within eastern Africa, Ethiopia stands out for its steep topography, resulting in an altitudinal zonation of climate and vegetation. To understand future vegetation changes, we need information on past vegetation covers and vegetation responses to environmental and climatic changes. Pollen studies are available for low and high elevations in Ethiopia, but they are low in number and limited in spatial coverage. In addition, explicit research to altitudinal patterns of environmental changes are missing. However, archaeological evidence from SW Ethiopia suggests vertical migration of humans in response to humidity fluctuations, highlighting the need for research to spatial dynamics of human activities and vegetation in Ethiopia. On the other hand, sedimentological evidence suggests a millennia long agricultural history in Ethiopia’s highlands and several authors identify this region as a center of plant domestication. </p><p>It is clear that a thorough understanding of the past vegetation cover and its alteration by humans and climate is missing for Ethiopia. These research gaps impede identification of the timing and location of the onset of agriculture in the ancient Ethiopian landscape, resulting in poor understanding of e.g. contemporary degraded landforms. In our study, we aim to reconstruct and quantify the vegetation history along an altitudinal gradient in the Southern Ethiopian Rift Valley and to identify the role of man and climate on this evolution. Therefore, several lakes and swamps are selected as study sites along an altitudinal gradient (1100-3000 m a.s.l.) in the Gamo Highlands near the city of Arba Minch, along the Southern Ethiopian Rift Valley. Here, we will present the results of pollen, charcoal and NPP analyses from two wetland sites situated at 2300 and 3000 m a.s.l. The records show an increase of Afromontane forest taxa around 13 ka BP, at the expense of Montane ericaceous taxa. At 8 ka BP, a shift in the composition of the Afromontane forest is observed, together with a change in the fungal assemblage and decrease of grasses. Around 6 ka BP, Wooded grassland taxa increase simultaneously with <em>Delitschia</em> fungal spores. Montane forest taxa increase again at 2.5 ka BP, together with a shift in fungal spores, followed by an increase in charcoal accumulation during the last millennium. Most of the observed transitions can be linked to other vegetation records from Ethiopia, and reflect responses to climatic changes such as the African Humid Period. However, the exact timing and  nature of the vegetation changes differs substantially between records, and asks for a denser sampling of palaeoecological records across Ethiopia. In this study, we will link the reconstructed vegetation changes with anthropogenic and natural driving forces, and come up with a reconstruction of the long-term landscape development in the study area in SW Ethiopia.   </p>


2010 ◽  
Vol 83 (2_Suppl) ◽  
pp. 38-42 ◽  
Author(s):  
Wun-Ju Shieh ◽  
Robert F. Breiman ◽  
Fausta Mosha ◽  
Peter Bloland ◽  
Carol Y. Rao ◽  
...  

1986 ◽  
Vol 25 (3) ◽  
pp. 312-239 ◽  
Author(s):  
Claude Hillaire-Marcel ◽  
Odette Carro ◽  
Joel Casanova

During recent humid episodes, stromatolites were built along paleolake margins, some 60 m above the modern water level of Lakes Natron and Magadi (southern Gregory Rift Valley). Three generations of stromatolites are observed, the more recent ones frequently covering pebbles and boulders eroded from the older ones. The youngest one yielded 14C ages ranging from approximately 12,000 to 10,000 yr B.P. Their δ13C values (≥2.6%) suggest isotopic equilibrium between the paleolake total inorganic dissolved carbon and the atmospheric CO2, thereby lending credence to the reliability of the 14C. An initial 230Th/232Th ratio in the detrital component was determined by Th/U measurements on the 14C dated stromatolites. Using this value a 230Th/234U chronology for the older stromatolites was calculated. Ages of ≥240,000 and 135,000 ± 10,000 yr were obtained for the first and second generations, respectively. A humid episode apparently characterized eastern Africa during each glacial-interglacial transition. 18O and 13C measurements on stromatolites, when compared to values on modern waters and carbonates, provide paleohydrological information. Long residence time of the paleolake waters and less seasonally contrasted regimes are inferred.


Bothalia ◽  
1987 ◽  
Vol 17 (2) ◽  
pp. 237-256 ◽  
Author(s):  
P. B. Phillipson

A checklist of vascular plants of the Amatole Mountains is presented. The physical environment, climate and vegetation of the study area and the history of its botanical exploration are described. The mountains form part of the Winterberg Range in the eastern Cape/Ciskei region of south-eastern Africa, and cover an area of approximately 900 km2. The altitude ranges from about 700 m to 2 000 m above sea level, and the topography is very varied. The climate is warm temperate and supports various vegetation types including forest, sclerophyllous shrubland, grassland and marshland. The checklist records the occurrence of 1 215 taxa. The largest families and genera in the area contain predominantly grassland herbs. Many of the characteristic families of the Cape Floristic Region and of the arid areas of southern Africa are poorly represented in the Amatole Mountains.


Author(s):  
John Galaty

The Rift Valley is a stage on which the history of Eastern Africa has unfolded over the last 10,000 years. It served as a corridor for the southward migration from the Upper Nile and the Ethiopian highlands of Nilo-Saharan and Afro-Asiatic speakers and cultures, with their domestic animals, which over time defined and restructured the social and cultural fabric of East Africa. Genetic evidence suggests that, contrary to other regions in Africa where geography overrides language, the clustering of East African populations primarily reflects linguistic affiliation. Eastern Sudanic Nilotic speakers are dedicated livestock keepers whose identification with cattle over thousands of years is manifested in elaborate symbolism, networks created by cattle exchange, and the practice of sacrifice. The geographical attributes of rich grasslands in a semi-arid environment, close proximity of lowland and highland grazing, and a bimodal rainfall regime, made the Rift Valley an ideal setting for increasingly specialized pastoralism. However, specialized animal husbandry characteristic of East Africa was possible only within a wider socioeconomic configuration that included hunters and bee-keeping foragers and cultivators occupying escarpments and highland areas. Some pastoral groups, like Maasai, Turkana, Borana, and Somali, spread widely across grazing areas, creating more culturally homogeneous regions, while others settled near one another in geographically variegated regions, as in the Omo Valley, the Lake Baringo basin, or the Tanzanian western highlands, creating social knots that signal historical interlaying and long-term mutual coexistence. At the advent of the colonial period, Oromo and Maasai speakers successfully exploited the ecological potential of the Rift environment by combining the art of raising animals with social systems built out of principles of clanship, age and generation organizations, and territorial sections. Faced with displacement by colonial settlers and then privatization of rangelands, some Maasai pastoralists sold lands that they had been allocated, leading to landlessness amid rangeland bounty. Pastoral futures involve a combination of education, religious conversion, and diversified rangeland livelihoods, which combine animal production with cultivation, business, wage labor, or conservation enterprises. Pastoralists provide urban markets with meat, but, with human population increasing, per capita livestock holdings have diminished, leading to rural poverty, as small towns absorbing young people departing pastoralism have become critical. The Great East African Rift Valley has had a 10,000-year history of developing pastoralism as one of the world’s great forms of food production, which spread throughout Eastern Africa. The dynamics of pastoral mobility and dedication to livestock have been challenged by modernity, which has undermined pastoral territoriality and culture while providing opportunities that pastoralists now seek as citizens of their nations and the world.


The Kenya rift valley is a sector of the rift system of eastern Africa which is marked by volcanic activity throughout its history from Miocene times to the present day. Activity is not confined to the rift zone but extends for distances of 200 km or more both to the west and east and is broadly centred on the Kenya ‘dome’, a topographic culmination in the course of the rift. The volcanic rocks show a considerable diversity of compositions ranging from basic to acid, but all are characteristically alkaline varying, however, from a mildly alkaline, alkali basalt-trachyte series, to strongly alkaline and undersaturated nephelinites and phonolites. The mode of extrusion and form of the volcanic accumulations are also very varied, evidently dependent in part on composition. There are thus the widespread ‘plateau’ phonolites of central and southern Kenya, possibly fissure eruptions; the large nephelinite central volcanoes of eastern Uganda, including Mt Elgon, and western Kenya; and the giant phonolite-trachyte or basalt-phonolite-trachyte volcanoes of Mts Kenya and Kilimanjaro. Extensive basalt fields were variously the products of fissure eruption, such as those of Samburu, or derived from numerous small centres as in the Nyambeni area or the Chyulu Hills. Large low-angle cones in the northern part of the rift are formed mostly of trachyte flows, whereas the axis of the rift is marked by a series of conspicuous trachyte-basalt volcanoes, often with spectacular calderas. The composition of the volcanic rocks shows variations with time, possibly indicating a dependence on the structural evolution of the rift, but sequences are not simple and cannot be easily defined. The nephelinite volcanoes of eastern Uganda are of Miocene age, but this composition also characterizes recent volcanoes of northern Tanzania. The basalt-basanite association dominates the earliest volcanic rocks of the rift zone itself, but has been repeatedly represented to the present. The flood phonolites were, however, largely confined to the upper Miocene; the Pliocene and earlier Pleistocene were marked by great eruptions of trachyte lavas and ignimbrite, whereas acid volcanic rocks, comendites and pantellarites, of Quaternary age are limited to a small area in the central part of the rift. The total volume of volcanic rocks cannot be estimated with any accuracy, but may be of the order of several 100 000 km 3 . The second part of this account presents in preliminary form the results of field mapping and chemical analytical programmes on the Cainozoic volcanics of the northern Kenya rift. It is shown that in this sector there is a distinct petrochemical evolution from the Miocene to the Pleistocene, the general trend being a decrease in silica undersaturation in both mafic and felsic rocks. The succession of lavas and sediments has a maximum thickness of 3 km and the main unconformities, indicating the major faulting episodes, coincide with the petrochemical changes.


2010 ◽  
Vol 203 (5) ◽  
pp. 655-665 ◽  
Author(s):  
Leonard Nderitu ◽  
John S. Lee ◽  
Jared Omolo ◽  
Sylvia Omulo ◽  
Monica L. O'Guinn ◽  
...  

1981 ◽  
Vol 22 (4) ◽  
pp. 435-456 ◽  
Author(s):  
Gadi G. Y. Mgomezulu

Research over the past five years or so indicates that in north-western and central Kenya and northern Tanzania pastoralism is much older than previously supposed. Radiocarbon dates from the central Rift valley and the Serengeti plains suggest the presence of domestic cattle by about the sixth millennium b.c. Early pottery traditions in the central Rift valley and around Lake Turkana have been more precisely identified. A continuing research project in the southern Sudan has revealed early pottery with possible northern affinities and rouletted pottery of the first as well as second millennia a.d. In north-western Tanzania, iron would still seem to have been smelted as early as the sixth century b.c. The use of iron, and perhaps of rouletted ware, by pastoral peoples in central Kenya is now dated to the late first millennium a.d. In Malawi, food-production would still seem to have been introduced early in that millennium, but the introduction of cattle has now been dated to the third or fourth century a.d., some centuries earlier than had previously been supposed. In Zambia, the surprisingly early dates for Situmpa pottery have apparently been confirmed. On the east coast, excavations at Hafun, Mogadishu and Manda have enabled more precise dating of the periods during which these ancient ports flourished, while a comprehensive survey programme has refined our knowledge of monumental sites along the Kenya coast.


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