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    Volume 43 Issue 11
    Nov.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(11): 4138-4148
    Liu Linjing, Li Chang'an, Jie Dongmei, Zhang Ruchun, Wang Jiangyong, Zhang Yufen, Mao Xin, Jiang Gaolei, Wang Panli, 2018. Paleoclimate Recorded by Phytolith in Anguli-Nuur Lake since Mid-Late Holocene. Earth Science, 43(11): 4138-4148. doi: 10.3799/dqkx.2018.614
    Citation: Liu Linjing, Li Chang'an, Jie Dongmei, Zhang Ruchun, Wang Jiangyong, Zhang Yufen, Mao Xin, Jiang Gaolei, Wang Panli, 2018. Paleoclimate Recorded by Phytolith in Anguli-Nuur Lake since Mid-Late Holocene. Earth Science, 43(11): 4138-4148. doi: 10.3799/dqkx.2018.614
    shu

    Paleoclimate Recorded by Phytolith in Anguli-Nuur Lake since Mid-Late Holocene

    doi: 10.3799/dqkx.2018.614
    • 1.

      School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 2.

      Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China

    • 3.

      Key Laboratory of Quaternary Chronology and Hydrological Environment Evolution, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China

    • 4.

      State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

    • 5.

      School of Geographical Sciences, Northeast Normal University, Changchun 130024, China

    • 6.

      Key Laboratory of Vegetation Ecology, Ministry of Education, Northeast Normal University, Changchun 130024, China

    • 7.

      Institute of Geographical Sciences, Hebei Academy of Sciences, Shijiazhuang 050011, China

    • 8.

      Hebei Engineering Research Center for Geographic Information Application, Shijiazhuang 050011, China

    • Received Date: 2018-04-17
    • Publish Date: 2018-11-15
      Abstract
    • Bashang area of Hebei Province is located in the East Asian monsoon-margin region and the ecotone between agriculture and animal husbandry. East Asian monsoon variability significantly affects the development of human civilization within its area of influence. In order to reconstruct the climate changes in Bashang area and understand the interactions between past climate and human civilization, a continuous 120 cm sediment profile was recovered from Anguli-Nuur Lake based on phytolith and pollen analysis. The results show that the climate in this region was gradually becoming cold and dry during the last 5 000 years, which is related to the weakening of East Asian monsoon produced by gradual variations of solar radiation. However, the climate was relatively wet during the periods of 5 030-3 074 cal. a BP. On the centennial scale, Anguli-Nuur has experienced seven obvious cold and dry events, which occurred during ~4 500 cal. a BP, 4 100-3 800 cal. a BP, ~3 500 cal. a BP, ~3 000 cal. a BP, ~2 100 cal. a BP, ~1 100 cal. a BP and 800-270 cal. a BP. The cold and dry events are consistent with the weakening stage of East Asian monsoon that is probably affected by high latitude climate and the solar activities. In this region, the development of human civilization is sensitive to climate change. Agriculture civilization is relatively developed during warm and humid stage, and grassland civilization appears during cool and arid stage.

       

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