Cushitic and Nilotic Prehistory: New Archaeological Evidence from North-West Kenya

1979 ◽  
Vol 20 (3) ◽  
pp. 319-328 ◽  
Author(s):  
B. M. Lynch ◽  
L. H. Robbins

Recent archaeological research conducted west of Lake Turkana, Kenya has shed new light on the prehistory of eastern Cushitic and Nilotic speakers in East Africa. The Namoratunga cemetery and rock art sites, dated to about 300 B.C., are clearly related to the prehistory of Eastern Cushitic speakers. The newly defined Turkwell cultural tradition, dated to the first millenniuma.d., is associated with eastern Nilotic prehistory. Lopoy, a large lakeside fishing and pastoralist settlement, is discussed in terms of eastern Nilotic prehistory. The archaeological data agrees with the independent findings of historical linguistics.

1987 ◽  
Vol 28 (2) ◽  
pp. 177-189 ◽  
Author(s):  
Peter Robertshaw

The results of recent archaeological research in the Upper Nile basin are summarized and placed within the context of the anthropological-historical debate concerning the origins of the Nuer, Dinka and Atuot as distinct ethnic groupings. The archaeological evidence demonstrates a considerable antiquity for cattle-keeping in the region, the existence of what appears to be a very widespread cultural tradition in the late first millennium a.d. characterized by a distinctive form of burial, and a hiatus in settlement in the area east of Rumbek early in the present millennium, possibly around the time when humped cattle were introduced further north. The implications of these data for the explanation of the origins of the Luo migrations are discussed.


Author(s):  
Atholl Anderson

Since the arrival of Europeans in the 16th century the observed ethnic complexity of the Malagasy, the Madagascan people, has been a subject of conjecture in several respects. When did people first reach Madagascar? Where did the different elements of the population originate? What was the sequence of their arrival? What was the nature of their maritime migrations? Early answers to these questions relied on the historical traditions of some Malagasy populations, especially of the Merina and highland groups, and on an extensive archive of historical and ethnographic observations. Recent approaches, through historical linguistics, palaeoecology, genomic history, and archaeology, especially in the last thirty years have provided new perspectives on the enduring issues of Madagascan population history. The age of initial colonization is still debated vigorously, but the bulk of current archaeological data, together with linguistic and genomic histories, suggest that people first arrived around the middle of the first millennium ce or later. Evidence of linguistic origins and human genetics supports the prevailing view that the first people came from Southeast Asia, the majority of them specifically from Borneo. Later Bantu migration from Africa was followed by admixture of those populations and other smaller groups from South Asia, in Madagascar. Admixture in East Africa before migration to Madagascar is no longer favored, although it cannot be ruled out entirely. Voyaging capability is a key topic that is, however, difficult to pin down. There is no necessity in the current data to envisage transoceanic voyages, and no evidence of Southeast Asian vessels in East Africa or Madagascar in the first millennium ce, although it is impossible to rule that out. The safest assumption at present is that contact between Southeast Asia and Madagascar during the period of colonization occurred through the established network of coastal and monsoon passages and shipping around the northern perimeter of the Indian Ocean.


2005 ◽  
Vol 46 (2) ◽  
pp. 209-241 ◽  
Author(s):  
PETER MITCHELL ◽  
GAVIN WHITELAW

Southernmost Africa (here meaning South Africa, Lesotho and Swaziland) provides an excellent opportunity for investigating the relations between farming, herding and hunting-gathering communities over the past 2,000 years, as well as the development of societies committed to food production and their increasing engagement with the wider world through systems of exchange spanning the Atlantic and Indian Oceans. This paper surveys and evaluates the archaeological research relevant to these communities and issues carried out in the region since the early 1990s. Among other themes discussed are the processes responsible for the emergence and transformation of pastoralist societies (principally in the Cape), the ways in which rock art is increasingly being incorporated with other forms of archaeological data to build a more socially informed view of the past, the analytical strength and potential of ethnographically informed understandings of past farming societies and the important contribution that recent research on the development of complex societies in the Shashe-Limpopo Basin can make to comparative studies of state formation.


2020 ◽  
Vol 86 (1) ◽  
pp. 203-205
Author(s):  
A.J. White ◽  
Samuel E. Munoz ◽  
Sissel Schroeder ◽  
Lora R. Stevens

Skousen and Aiuvalasit critique our article on the post-Mississippian occupation of the Horseshoe Lake watershed (White et al. 2020) along two lines: (1) that our findings are not supported due to a lack of archaeological evidence, and (2) that we do not consider alternative hypotheses in explaining the lake's fecal stanol record. We first respond to the matter of fecal stanol deposition in Horseshoe Lake and then address the larger issue, the primacy of archaeological data in interpreting the past.


The Holocene ◽  
2021 ◽  
pp. 095968362110116
Author(s):  
Tanzhuo Liu ◽  
Christopher J Lepre ◽  
Sidney R Hemming ◽  
Wallace S Broecker

Rock varnish is a manganiferous dark coating accreted on subaerially exposed rocks in drylands. It often contains a layered microstratigraphy that records past wetness variations. Varnish samples from latest Pleistocene and Holocene geomorphic features in the Lake Turkana basin, East Africa display a regionally replicable microstratigraphy record of Holocene millennial-scale wetness variability and a broad interval of wetter conditions during the African Humid Period (AHP). Three major wet pulses in the varnish record occurred during the generally wet interval of the early Holocene (11.5–8.5 ka) when the lake attained its maximum high stand (MHS) at 455–460 m. A >23 m drop from the MHS occurred between 8.5 and 8 ka. Subsequently two additional wet pulses occurred during the early to middle Holocene (8–5 ka) when the lake occupied its secondary high stand at 445 m. Collectively, these five wet phases represent an extended wet interval coincident with the AHP in the region. One moderate wet phase occurred during the subsequent climatic transition from the humid to arid regime (5–4.3 ka) after the lake level dropped rapidly from 445 m to <405 m. Five minor wet phases took place during the overall arid period of the late Holocene (4.3–0 ka) when the lake level oscillated below 405 m. These findings indicate that the AHP terminated rapidly around 5 ka in the Turkana basin in terms of lake level drop, but the regional shift in relative humidity from the AHP mode to its present-day condition lagged for about 700 years until 4.3 ka, hinting at a gradual phasing out in terms of moisture condition. These findings further suggest that Lake Turkana overflowed intermittently into the Nile drainage system through its topographic sill at 455–460 m during the early Holocene and has become a closed-basin lake thereafter for the past 8 ky.


Radiocarbon ◽  
2013 ◽  
Vol 55 (3) ◽  
pp. 1215-1221 ◽  
Author(s):  
Levy Figuti ◽  
Cláudia R Plens ◽  
Paulo DeBlasis

Sambaquis, famous Brazilian coastal shellmounds, represent a successful and long archaeological cultural tradition, with hundreds of sites spread over 2000 km of the Brazilian south-southeast coastline. These sites have many burials within a sequence of layers comprising a mix of faunal remains, charcoal, ashes, and sand, thus resulting in very complex stratigraphic structures. Several radiocarbon samples exhibit ages between 8000 and 1000 cal yr BP. In the Brazilian southeastern coastal hinterland, at the Ribeira de Iguape basin, 36 small mounds similar to the sambaquis were found, composed mostly of landsnail shells, bone remains of terrestrial fauna, lithic and osteodontological artifacts, and quite a few burials. Through the last decade an archaeological research project has accomplished extensive surveys and systematic 14C sampling, together with excavations in selected sites. A sequence of ages has been obtained from different samples (16 on shell, 10 on human bone, and 6 on charcoal) representing 19 sites. These dates range from 10,000 to 1000 cal yr BP, highlighting around 9000 yr of cultural continuity, contemporary to both the Paleoindian record over the hinterland plateau, and older than their coastal counterparts, the sambaquis. By presenting the 14C distribution and an overview of the archaeological features of these sites, we discuss briefly the dispersion and settlement processes of early peopling in this area of Brazil.


2016 ◽  
Vol 14 (1) ◽  
pp. 7-17 ◽  
Author(s):  
John Kinahan

Bones of domestic sheep dated to the early first millennium AD are described from the Dâures massif in the Namib Desert. The remains confirm earlier investigations which inferred the acquisition of livestock from indirect evidence in the rock art, suggesting a fundamental shift in ritual practice at this time. Dating of the sheep remains is in broad agreement with the dating of other finds in the same area and in southern Africa as a whole. The presence of suspected sheep bone artefacts, possibly used for ritual purposes, draws attention to the importance of livestock as more than a component of diet in the changing economy of hunter-gatherer society.


1995 ◽  
Vol 61 ◽  
pp. 347-370 ◽  
Author(s):  
Richard Bradley ◽  
Felipe Criado Boado ◽  
Ramón Fábregas Valcarce

This paper discusses the relationship between the earlier prehistoric pattern of settlement in Atlantic Europe and the creation of rock art. It investigates the organisation of the Copper Age and Early Bronze Age landscape of north-west Spain using the evidence provided by the distribution, siting, and composition of rock carvings. It presents the results of field survey in three sample areas extending from the centre to the outer edge of their distribution. Although these drawings cannot be interpreted as illustrations of daily life, they may have helped to define rights to particular resources in an area which experienced abrupt changes of ground conditions over the course of the year.


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