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    湖北天门谭家岭遗址全新世中晚期气候变化及其对人类活动的影响

    毛欣 李长安 张玉芬 陈旭 刘辉

    毛欣, 李长安, 张玉芬, 陈旭, 刘辉, 2014. 湖北天门谭家岭遗址全新世中晚期气候变化及其对人类活动的影响. 地球科学, 39(10): 1445-1453. doi: 10.3799/dqkx.2014.137
    引用本文: 毛欣, 李长安, 张玉芬, 陈旭, 刘辉, 2014. 湖北天门谭家岭遗址全新世中晚期气候变化及其对人类活动的影响. 地球科学, 39(10): 1445-1453. doi: 10.3799/dqkx.2014.137
    Mao Xin, Li Chang'an, Zhang Yufen, Chen Xu, Liu Hui, 2014. Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province. Earth Science, 39(10): 1445-1453. doi: 10.3799/dqkx.2014.137
    Citation: Mao Xin, Li Chang'an, Zhang Yufen, Chen Xu, Liu Hui, 2014. Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province. Earth Science, 39(10): 1445-1453. doi: 10.3799/dqkx.2014.137

    湖北天门谭家岭遗址全新世中晚期气候变化及其对人类活动的影响

    doi: 10.3799/dqkx.2014.137
    基金项目: 

    国家自然科学基金项目 40971008

    详细信息
      作者简介:

      毛欣(1989-), 男, 硕士研究生, 主要从事第四纪地质学方面的研究.E-mail: maoxin02@gmail.com

      通讯作者:

      李长安, E-mail: chanli@cug.edu.cn

    • 中图分类号: P534.63+2;P595

    Impact of Middle to Late Holocene Climate Changes on Human Activities at Tanjialing Site, Tianmen, Hubei Province

    • 摘要: 石家河文化是长江中游地区早期文明演化进程中的重要阶段,然而目前对于石家河文化的绝对年代尚存有分歧,对该时期环境特征与人类文明相互关系的研究也较少.选择石家河文化典型遗址——谭家岭遗址为研究对象,经美国NSF-Arizona AMS实验室对该遗址剖面AMS 14C年龄的测定,并结合石家河文化的相对年代,可知石家河文化的绝对年代定在4 800~4 100 cal. a BP比较合适;通过对该遗址剖面的地球化学元素分析,借助主成分分析、环境C值等统计分析方法,结果表明:本区在4 850~4 300 cal. a BP间,元素的第二主成分、环境C值和Mg/Ca比值处于高值段,反映气候相对温暖湿润,同时反映人类活动的指标F1F3得分也处于高值段,表明人类活动较强;在4 300~4 124 cal. a BP间,元素的第二主成分、环境C值和Mg/Ca比值处于低值段,揭示气候进入相对寒冷干旱时期,同时F1F3得分显著降低,指示人类活动减弱,石家河文化走向衰败.本文研究结果表明距今4300a暖湿转为干冷气候背景下的洪水事件可能促使石家河文化走向衰败.

       

    • 图  1  谭家岭遗址位置图

      Fig.  1.  Location of the profile of Tanjialing site

      图  2  谭家岭遗址T0620剖面地层特征

      Fig.  2.  Stratigraphic characteristics of the profile T0620 on the Tanjialing site

      图  3  谭家岭遗址T0620探方东壁剖面地球化学元素含量随深度变化曲线

      Fig.  3.  Geochemistry element contents of the profile T0620 in the Tanjialing site

      图  4  谭家岭遗址剖面Mg/Ca、环境C值、PCA因子得分以及HS-4石笋的δ18O记录(Hu et al., 2008)

      Fig.  4.  The indexes of Mg/Ca, C value of the environment and the scores in PCA axes in the Tanjialing site and the record of δ18O for HS-4

      表  1  谭家岭遗址文化层AMS 14C测年及日历年龄校正

      Table  1.   AMS 14C dating and calendar calibration of chronology in the Tanjialing cultural layers

      样品 深度(m) 测定物质 14C年龄(a BP) 日历年龄(cal. a BP)
      TJL-2-14C-3 0.35 泥炭 3 769±39 4 124±38
      TJL-2-14C-1 1.95 泥炭 3 977±40 4 432±16
      TJL-1-14C-wood 2.80 古木 4 284±41 4 850±23
      下载: 导出CSV

      表  2  主要环境参数Pearson相关分析

      Table  2.   The Pearson correlation analyses between main environmental parameters

      Ca K Na Al Mg Mg/Ca C F1 F2 F3 δ18O
      Ca 1
      K -0.427* 1
      Na -0.757** 0.578** 1
      Al 0.728** -0.413** -0.529** 1
      Mg 0.590** -0.512** -0.699** 0.346 1
      Mg/Ca 0.172 -0.378 -0.451** 0.001 0.893** 1
      C 0.524** -0.526** -0.506** 0.899** 0.357** 0.138 1
      F1 0.156 -0.430** -0.378 0.001 0.156 0.580** 0.449** 1
      F2 -0.921** -0.499** -0.787** 0.803** 0.893** 0.200 0.586** 0.002 1
      F3 0.501** -0.621** -0.776** 0.506** 0.645** 0.512** 0.658** 0.586** 0.521** 1
      δ18O -0.306 -0.478** -0.461** -0.413** -0.578** -0.230 -0.454** -0.404** -0.282 -0.456** 1
      注:**相关性显著水平P < 0.01(双尾检验);*相关性显著水平P < 0.05(双尾检验).
      下载: 导出CSV
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    • 收稿日期:  2014-01-03
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