2022
DOI: 10.1130/abs/2022am-381322
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Reconstruction of Holocene Vegetation, Climate, and Land Use Changes Based on Pollen Analysis of Cores From Lake Khargal Mongolia

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“…In contrast, the regional perspective available from Egiin Gol, in conjunction with faunal, archaeobotanical, isotopic, and lake sediment analyses, demonstrates the integration of mobile herding with the new productive emphasis on agriculture. Cores from nearby Khargal Lake reveal the coeval appearance of pollens associated with agriculture but also a notable uptick in Sporormiella sp., a fungal spore that is found on the dung of domestic livestock [74]. From a settlement perspective, survey results show fewer upper tributary valley habitations in areas where protection from winter conditions would have been optimal; however, these winter sites are indeed present.…”
Section: Discussionmentioning
confidence: 97%
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“…In contrast, the regional perspective available from Egiin Gol, in conjunction with faunal, archaeobotanical, isotopic, and lake sediment analyses, demonstrates the integration of mobile herding with the new productive emphasis on agriculture. Cores from nearby Khargal Lake reveal the coeval appearance of pollens associated with agriculture but also a notable uptick in Sporormiella sp., a fungal spore that is found on the dung of domestic livestock [74]. From a settlement perspective, survey results show fewer upper tributary valley habitations in areas where protection from winter conditions would have been optimal; however, these winter sites are indeed present.…”
Section: Discussionmentioning
confidence: 97%
“…Even though local climate regimes have been variable, this has not imposed major changes in geomorphological regimes [72,73]. Lake core analysis at Khargal Lake (75 km to the northwest) indicates that the Xiongnu period local climate began to ameliorate around 250-200 BC and by the turn of the millennium became more like the contemporary climate experienced over the past few decades [74]. This reinforces observations by archaeobotanists that the same vegetation types and arboreal species seen today at Egiin Gol also appear as macroand microbotanical remains in burials and habitation sites of the Xiongnu period [75,76].…”
Section: The Egiin Gol Valley Study Areamentioning
confidence: 99%