2008
DOI: 10.1016/j.quaint.2007.06.033
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Climate, African and Beringian subaerial continental shelves, and migration of early peoples

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Cited by 10 publications
(3 citation statements)
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“…These relationships are consistent with a demographic history in which structure among EHG populations emerged before the Last Glacial Maximum (∼21 kya). This period has been identified as one of increased aridity and reduced temperatures in East Africa; these climatic conditions were accompanied by shifts in vegetation, particularly reduced forest coverage (101,102), and these environmental changes are thought to have triggered human dispersals into environmental refugia (103). Thus, we have uncovered a connection among geographically disparate HG populations in East Africa, consistent with a broad geographic distribution of their ancestors in the late Pleistocene before 30 kya.…”
Section: Discussionsupporting
confidence: 67%
“…These relationships are consistent with a demographic history in which structure among EHG populations emerged before the Last Glacial Maximum (∼21 kya). This period has been identified as one of increased aridity and reduced temperatures in East Africa; these climatic conditions were accompanied by shifts in vegetation, particularly reduced forest coverage (101,102), and these environmental changes are thought to have triggered human dispersals into environmental refugia (103). Thus, we have uncovered a connection among geographically disparate HG populations in East Africa, consistent with a broad geographic distribution of their ancestors in the late Pleistocene before 30 kya.…”
Section: Discussionsupporting
confidence: 67%
“…14 Nonetheless, in sub-Saharan Africa, glacial periods such as MIS 6 were often, but not exclusively, accompanied by aridity with expanding deserts and arid regions. 18,19 Such regions could have hampered interand/or intra-regional movement of humans and other animals. 17 Data for MIS 6 in South Africa indicate two dry phases, interspersed by a wet phase at ~140-130 ka ( Figure 3).…”
Section: Context Within the Mis Chronologymentioning
confidence: 99%
“…20 During such interglacial phases wetter climates and extended woodlands are expected, yet these remain general trends that might not apply equally to all regions or environmental niches. 18,19 As a whole, MIS 5 comprises a sequence of sub-stages alternating between warmer and cooler conditions ( Figure 3). 21 MIS 5e was an early warm interval, and was followed by irregular, but generally cooler, conditions culminating in the glacial conditions of MIS 4 (~71/74-60 ka).…”
Section: Context Within the Mis Chronologymentioning
confidence: 99%