The earliest prehistoric pottery in the Qinghai-Tibetan Plateau and its archaeological implications

被引:14
|
作者
Hou, GuangLiang [1 ]
Lai, ZhongPing [2 ]
Cao, Guangchao [1 ]
E, ChongYi [1 ]
Sun, YongJuan [3 ]
Rhode, David [4 ]
James, Feathers [5 ]
机构
[1] Qinghai Normal Univ, Key Lab Phys Geog & Environm Proc Qinghai Prov, Xining 810008, Qinghai, Peoples R China
[2] China Univ Geosci, Sch Earth Sci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
[3] Chinese Acad Sci, Qinghai Inst Salt Lakes, Xining 810008, Qinghai, Peoples R China
[4] Desert Res Inst, Earth & Ecosyst Sci, Reno, NV 89512 USA
[5] Univ Washington, Luminescence Lab, Seattle, WA 98195 USA
关键词
Prehistoric human activity; Qinghai-Tibetan Plateau (QTP); Pottery; Chronology and origin; Palaeolithic to Neolithic transition; SINGLE-ALIQUOT; LAKE AREA; LUMINESCENCE; CHRONOLOGY;
D O I
10.1016/j.quageo.2015.05.005
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Remains of prehistoric human activity in the Qinghai-Tibetan Plateau (QTP) were often found exposed in the surface due to strong erosion. Thus, archaeological sites containing continuous and integral cultural remains within stratigraphic layers are rare in the plateau. The Jiangxigou site, located in the south of Qinghai Lake basin and in the northeastern margin of the plateau, are such a site with ages ranging from the early to late Holocene, i.e. from the Paleolithic to the Neolithic. Our excavation disclosed remains including more than 700 pieces of microliths, 14 pottery pieces, and other cultural relics. The oldest pottery fragments were found at the depth of 75 cm in the section, and in particular, a painted pottery piece was found at the depth of 61 cm. In this study, both luminescence (TL and OSL) and radiocarbon dating were employed to establish the chronology for these remains. Two pieces of pottery were dated using thermoluminescence (TL), another two pieces of pottery were dated by OSL, and three charcoal samples by AMS C-14. TL age of pottery piece P14 from the depth of 75 cm is 7.06 +/- 0.51 ka, making it the earliest pottery in the Tibetan Plateau. The AMS 14C age of charcoals from the same depth of 75 cm is 6805 +/- 95 Cal a BP, in agreement with TL age of P14. OSL age of pottery P12 from the depth of 60-70 cm is 6.50 +/- 0.47 ka, and OSL age of pottery P9 from 54 cm is 4.97 +/- 0.25 ka. Thus, the age of the painted pottery piece at the depth of 61 cm should be similar to 5.50 ka by interpolation, making it the earliest painted pottery in the QTP. The pottery P14 has many common features similar to that of the Yangshao culture in China. We suggest that, before 7 ka, hunters using microlithic had been living in the northeastern margin of the QTP. Since 7 ka, these native microlithic hunters had been affected by the Neolithic Yangshao culture from the Loess Plateau, which was characterized by well-developed pottery. Agricultural growers migrated from the lower elevation of the Loess Plateau to the east of the QTP, leading to profound cultural exchanges with highland native microlithic hunters. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:431 / 437
页数:7
相关论文
共 50 条
  • [31] Computation of the present-day strain rate field of the Qinghai-Tibetan plateau and its geodynamic implications
    Zhu, SB
    Cai, YE
    Shi, YL
    [J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2005, 48 (05): : 1053 - 1061
  • [32] A synthesis of hydrogen isotope variability and its hydrological significance at the Qinghai-Tibetan Plateau
    Guenther, Franziska
    Aichner, Bernhard
    Siegwolf, Rolf
    Xu, Baiqing
    Yao, Tandong
    Gleixner, Gerd
    [J]. QUATERNARY INTERNATIONAL, 2013, 313 : 3 - 16
  • [33] Estimation of the Qinghai-Tibetan Plateau runoff and its contribution to large Asian rivers
    Liu, Zhaofei
    Yao, Zhijun
    Wang, Rui
    Yu, Guoan
    [J]. SCIENCE OF THE TOTAL ENVIRONMENT, 2020, 749
  • [34] Assessment of the vulnerability of alpine grasslands on the Qinghai-Tibetan Plateau
    Li, Meng
    Zhang, Xianzhou
    He, Yongtao
    Niu, Ben
    Wu, Jianshuang
    [J]. PEERJ, 2020, 8
  • [35] Plant phenology changes and drivers on the Qinghai-Tibetan Plateau
    Shen, Miaogen
    Wang, Shiping
    Jiang, Nan
    Sun, Jianping
    Cao, Ruyin
    Ling, Xiaofang
    Fang, Bo
    Zhang, Lei
    Zhang, Lihao
    Xu, Xiyan
    Lv, Wangwang
    Li, Baolin
    Sun, Qingling
    Meng, Fandong
    Jiang, Yuhao
    Dorji, Tsechoe
    Fu, Yongshuo
    Iler, Amy
    Vitasse, Yann
    Steltzer, Heidi
    Ji, Zhenming
    Zhao, Wenwu
    Piao, Shilong
    Fu, Bojie
    [J]. NATURE REVIEWS EARTH & ENVIRONMENT, 2022, 3 (10) : 633 - 651
  • [36] Evapotranspiration and Its Energy Exchange in Alpine Meadow Ecosystem on the Qinghai-Tibetan Plateau
    LI Jie
    JIANG Sha
    WANG Bin
    JIANG Wei-wei
    TANG Yan-hong
    DU Ming-yuan
    GU Song
    [J]. Journal of Integrative Agriculture, 2013, 12 (08) : 1396 - 1401
  • [37] Evapotranspiration and Its Energy Exchange in Alpine Meadow Ecosystem on the Qinghai-Tibetan Plateau
    Li Jie
    Jiang Sha
    Wang Bin
    Jiang Wei-wei
    Tang Yan-hong
    Du Ming-yuan
    Gu Song
    [J]. JOURNAL OF INTEGRATIVE AGRICULTURE, 2013, 12 (08) : 1396 - 1401
  • [38] Rangeland degradation on the Qinghai-Tibetan plateau: A review of the evidence of its magnitude and causes
    Harris, R. B.
    [J]. JOURNAL OF ARID ENVIRONMENTS, 2010, 74 (01) : 1 - 12
  • [39] STABILITY OF ALPINE MEADOW ECOSYSTEM ON THE QINGHAI-TIBETAN PLATEAU
    ZHOU Huakun1
    2. Graduate University of Chinese Academy of Sciences
    [J]. Science Bulletin, 2006, (03) : 320 - 327
  • [40] Snow effects on alpine vegetation in the Qinghai-Tibetan Plateau
    Wang, Kun
    Zhang, Li
    Qiu, Yubao
    Ji, Lei
    Tian, Feng
    Wang, Cuizhen
    Wang, Zhiyong
    [J]. INTERNATIONAL JOURNAL OF DIGITAL EARTH, 2015, 8 (01) : 56 - 73