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Titlebook: Africa from MIS 6-2; Population Dynamics Sacha C. Jones,Brian A. Stewart Book 2016 Springer Science+Business Media Dordrecht 2016 African

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Human Evolution in Late Quaternary Eastern Africation of modern humans has roots that extend well before MIS 6, and propose four overlapping stages, making this a much more prolonged process than has traditionally been described. There is a broad relationship between evolutionary history and major climatic oscillations; nevertheless, a closer exam
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Follow the Senqu: Maloti-Drakensberg Paleoenvironments and Implications for Early Human Dispersals id linking highland population flux to prevailing climate. It is proposed that short-lived but acute episodes of rapid onset aridity saw interior groups disperse into the highlands to be nearer to the Orange-Senqu headwaters, perhaps via the river corridor itself.
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Across Rainforests and Woodlands: A Systematic Reappraisal of the Lupemban Middle Stone Age in Centring bifacial lanceolate points, core axes, and backed blades, are found across the region as the MSA Lupemban industry. As the earliest sustained archaeological signature in Central Africa, U-series dates of ~260 ka for the industry at Twin Rivers (Zambia) suggest the initial dispersal of pre-. homi
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The Later Pleistocene in the Northeastern Central African Rainforest. These include, for example, the role that riverine systems might have played in the patterning of both prehistoric and extant genetic relationships. Utilization of archaeologically perishable bone in lithic poor regions may also account for apparently disjunctive archaeological distributions.
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Africa from MIS 6-2: The Florescence of Modern Humans,m, behavioral florescence, and global dispersion. Over this ~200 kyr period, Africa experienced environmental changes on a variety of spatiotemporal scales, from the long-term disappearance of whole deserts and forests to much higher frequency, localized shifts. The archaeological, fossil, and genet
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Mid to Late Quaternary Landscape and Environmental Dynamics in the Middle Stone Age of Southern Sout are coastal sites, which contain evidence for varied occupational intensity and marine resource use, along with signs of notable landscape, environmental, and ecological change. Here, we review and synthesize evidence for Quaternary landscape and climatic change of relevance to the southern Cape MS
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