2012
DOI: 10.1016/j.jaridenv.2011.11.020
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Hydro-geospatial analysis of ancient pastoral/agro-pastoral landscapes along Wadi Sana (Yemen)

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Cited by 20 publications
(9 citation statements)
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References 21 publications
(26 reference statements)
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“…This 5 ka age is consistent with the cessation of silt accumulation in the wadi and onset of downcutting implying a local hydrological threshold, supporting this as a drying event (Oches et al, 2020). Although the midden stable isotopes are qualitative indicators, this supports evidence from other palaeoenvironmental work at Wadi Sana and elsewhere in Arabia linking decreased monsoon strength by 6 ka to increased rainfall variability (Harrower, 2008;Harrower et al, 2012) or the onset of widespread aridity before 6 ka (Enzel et al, 2015;Lézine et al, 1998Lézine et al, , 2010.…”
Section: Mid-holocene Vegetation and Hydrologysupporting
confidence: 81%
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“…This 5 ka age is consistent with the cessation of silt accumulation in the wadi and onset of downcutting implying a local hydrological threshold, supporting this as a drying event (Oches et al, 2020). Although the midden stable isotopes are qualitative indicators, this supports evidence from other palaeoenvironmental work at Wadi Sana and elsewhere in Arabia linking decreased monsoon strength by 6 ka to increased rainfall variability (Harrower, 2008;Harrower et al, 2012) or the onset of widespread aridity before 6 ka (Enzel et al, 2015;Lézine et al, 1998Lézine et al, , 2010.…”
Section: Mid-holocene Vegetation and Hydrologysupporting
confidence: 81%
“…6 ka; McCorriston et al, 2002). Furthermore, water management structures, such as canals and check dams, were constructed as further evidence of environmental management likely in use from at least 5.8 to 5 ka (Harrower et al, 2012). Although itinerant people persisted after 5 ka, their lifestyles and archaeological signatures changed significantly (McCorriston & Harrower, 2020).…”
Section: Discussionmentioning
confidence: 99%
“…They come from ethnographies of modern pastoral specialists, whose subsistence, material culture, sociopolitical organization, and histories reflect their interdependence with agricultural societies (e.g., Bonte 1981; Khazanov 1984; Khoury and Kostiner 1990; Lees and Bates 1974). These models have been valuable in understanding the archaeological record of specialized pastoralism and exchange in the Bronze Age (Khazanov 2009; McCorriston and Weisberg 2002; Porter 2002; Stein 2004) and in the interpretation of Levantine Neolithic and Chalcolithic groups who did have contact with farmers (Bar‐Yosef and Bar‐Yosef‐Mayer 2002; Bar‐Yosef and Khazanov 1992; Grigson 2006). They underscore the significance of segmentary tribal identities anchored in genealogy and kinship and the importance of emerging states in supporting specialized pastoral societies and in consolidating political tribes (Fleming 2009; McCorriston 1997; Porter 2009).…”
mentioning
confidence: 99%
“…The palaeo‐records for a strengthened south‐west Asian monsoon across Arabia have been frequently reviewed, pointing to a broader Early Holocene habitable geographic range and habitat diversity, including palaeolakes in today's desert areas, broader and heavier spring flow in the mountains and marshy wadi bottoms where there had previously only been harsh aridity (Lézine et al . ; Harrower et al ., ). Archaeological evidence from southern Arabia consists mostly of surface finds and points to industries now better understood in their technological and geographic distinctiveness than when earlier researchers pointed to far‐flung parallels with the Levant and Africa.…”
Section: Introductionmentioning
confidence: 97%