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    末次间冰期以来渭南黄土剖面高分辨率古气候时间标尺

    王文远 刘嘉麒 潘懋 刘东生

    王文远, 刘嘉麒, 潘懋, 刘东生, 2000. 末次间冰期以来渭南黄土剖面高分辨率古气候时间标尺. 地球科学, 25(1): 98-102.
    引用本文: 王文远, 刘嘉麒, 潘懋, 刘东生, 2000. 末次间冰期以来渭南黄土剖面高分辨率古气候时间标尺. 地球科学, 25(1): 98-102.
    WANG Wen-yuan, LIU Jia-qi, PAN Mao, LIU Dong-sheng, 2000. RECONSTRUCTION OF THE HIGH RESOLUTION TIMESCALE IN THE WEINAN LOESS SECTION OF THE LATE QUATERNARY. Earth Science, 25(1): 98-102.
    Citation: WANG Wen-yuan, LIU Jia-qi, PAN Mao, LIU Dong-sheng, 2000. RECONSTRUCTION OF THE HIGH RESOLUTION TIMESCALE IN THE WEINAN LOESS SECTION OF THE LATE QUATERNARY. Earth Science, 25(1): 98-102.

    末次间冰期以来渭南黄土剖面高分辨率古气候时间标尺

    基金项目: 

    国家自然科学基金重大资助项目 4929110001

    详细信息
      作者简介:

      王文远, 男, 博士后, 1969年生, 主要从事第四纪地质学研究

    • 中图分类号: P534.63;P532

    RECONSTRUCTION OF THE HIGH RESOLUTION TIMESCALE IN THE WEINAN LOESS SECTION OF THE LATE QUATERNARY

    • 摘要: 利用细颗粒热释光技术对渭南剖面重要地层界线处的7个样品进行了年龄测定, 并在此基础上, 结合已发表数据利用多项式回归方法建立了渭南剖面高分辨率的古气候时间标尺, 其中S0/ L1-1, L1-1/ L1-2, L1-4/ L1-5, L1-5/S1, S1/ L2的界线年龄分别为1.1, 2.5, 5.1, 7.6, 12.8 ka, 除了L1-4/ L1-5的界线年龄与氧同位素3阶段的起始年龄差距较大之外, 它们与SPECMAP深海氧同位素5以上各阶段的界线年龄可进行较好的对比, 而L1 -4/ L1-5的界线年龄与北太平洋风尘记录的氧同位素年龄却有很好的一致性.关键词: 黄土; 热释光; 高分辨率; 时间标尺.

       

    • 图  1  渭南剖面地层、已发表年龄数据[1]及其样品采集位置

      1.耕作土; 2.古土壤; 3.黄土

      Fig.  1.  Stratigraphy, ages-published and locations of sampling points of Weinan loess section

      图  2  第四纪沉积物热释光测年模型[7]

      图中Io为残留热释光; In=Io+Id

      Fig.  2.  Model of thermoluminescence dating of Quaternary sediments

      图  3  渭南黄土剖面样品WT2热释光实验

      a.热释光增光曲线; b.等效剂量的确定; c.“坪法试验”图

      Fig.  3.  Drawings for TL experiment from the sample WT2 of Weinan loess section

      图  4  末次间冰期以来渭南黄土剖面年代-深度时间模式

      Fig.  4.  Depth-age model of the Weinan loess section of Late Quaternary

      表  1  渭南热释光测年及放射性分析结果

      Table  1.   Thermoluminescence result from the fine grain and radioactivity data of Weinan loess section

    • [1] 刘嘉麒, 陈铁梅, 聂高众, 等. 渭南黄土剖面的年龄测定及15万年来高分辨率时间序列的建立[J]. 第四纪研究, 1994, 3: 193~202. doi: 10.3321/j.issn:1001-7410.1994.03.001
      [2] 丁仲礼, 余志伟, 刘东生. 中国黄土研究新进展(三): 时间标尺[J]. 第四纪研究, 1991, 4: 336~348. doi: 10.3321/j.issn:1001-7410.1991.04.005
      [3] Liu J Q, Nie G Z, Song C Y, et al. A high resolution time scale for the past 150 000 years at Weinan loess section, Central China[J]. Scientia Geologica Sinica, 1995, 1 (Suppl): 9~22.
      [4] Porter S C, An Z S. Correlation between climate events in the North Atlantic and China during the Last Glaciation[J]. Nature, 1995, 375: 305~308. doi: 10.1038/375305a0
      [5] Liu T S, Ding Z L. Chinese loess and the paleomonsoon[J]. Annu Rev Earth Planet Sci, 1998, 26: 111~145. doi: 10.1146/annurev.earth.26.1.111
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      [9] Singhvi A K, Sharma Y P, Agrawal D P. Thermoluminescence dating of sand dunes in Rajasthan, India[J]. Nature, 1982, 295: 313~315. doi: 10.1038/295313a0
      [10] Atiken M J. Thermoluminescence dating[M]. London: Academic Press, 1985. 24~29, 66~80.
      [11] Prescott J R, Stephan L G. The contribution of cosmic radiation to the environmental dose for thermoluminescent dating, latitude, attitude and depth dependences[J]. Council of Europe Journal PACT, 1982, 6: 17~25.
      [12] Fleming S J. Thermoluminescent techniques in archaeology[M]. Oxford: Clarendon Press, 1979. 30~33.
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      [14] Imbrie J, Hays J D, Martinson D G, et al. The orbital theory of Pleistocene climate: support from a revised chronology of the marine δ18O record[A]. In: BergerA, Imbrie J, Hays J D, et al, eds. Milankovtch and climate: understanding the response to astronomical forcing[C]. Netherland: Reidel Publishing, 1984. 269~305.
      [15] Forman S L. Late Pleistocene chronology of loess deposition near Luochuan, China[J]. Quaternary Research, 1991, 36: 19~28. doi: 10.1016/0033-5894(91)90014-V
      [16] Fang X M, Li J J, Derbyshire E, et al. Micromorphology of the Beiyuan loess_paleosol sequence in Gansu Province, China: geomorphological and paleoenvironmental significance[J]. Palaeogeography Palaeoclimatology Palaeoecology, 1994, 111: 289~303. doi: 10.1016/0031-0182(94)90069-8
      [17] Lu Y C, Zhang J Z, Xie J. Thermoluminescence dating of loess and paleosols from the Lantian section, Shanxi Province, China[J]. Quaternary Science Reviews, 1988, 7: 245~250. doi: 10.1016/0277-3791(88)90011-X
      [18] Hovan S A, Rea D K, Pisias N G, et al. A direct link between the China loess and marine δ18O records: aeolian flux to the North Pacific. Nature, 1989, 340: 296~298. doi: 10.1038/340296a0
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    出版历程
    • 收稿日期:  1999-08-31
    • 刊出日期:  2000-01-25

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