铜川地区早中全新世黄土沉积特征及其古气候意义

周家兴, 于娟, 杨丽君, 吴利杰. 铜川地区早中全新世黄土沉积特征及其古气候意义[J]. 海洋地质与第四纪地质, 2020, 40(1): 160-166. doi: 10.16562/j.cnki.0256-1492.2018091901
引用本文: 周家兴, 于娟, 杨丽君, 吴利杰. 铜川地区早中全新世黄土沉积特征及其古气候意义[J]. 海洋地质与第四纪地质, 2020, 40(1): 160-166. doi: 10.16562/j.cnki.0256-1492.2018091901
ZHOU Jiaxing, YU Juan, YANG Lijun, WU Lijie. Sedimentary characteristics of the Early and Middle Holocene loess in Tongchuan area and their implications for paleoclimate[J]. Marine Geology & Quaternary Geology, 2020, 40(1): 160-166. doi: 10.16562/j.cnki.0256-1492.2018091901
Citation: ZHOU Jiaxing, YU Juan, YANG Lijun, WU Lijie. Sedimentary characteristics of the Early and Middle Holocene loess in Tongchuan area and their implications for paleoclimate[J]. Marine Geology & Quaternary Geology, 2020, 40(1): 160-166. doi: 10.16562/j.cnki.0256-1492.2018091901

铜川地区早中全新世黄土沉积特征及其古气候意义

  • 基金项目: 中国地质调查局地质科技调查项目“西北黄土堆积与中国古气候变化”(1212010911048)
详细信息
    作者简介: 周家兴(1992—),男,硕士研究生,研究方向为第四纪气候与环境,E-mail:970896733@qq.com
    通讯作者: 于娟(1982—),女,工程师,研究方向为环境地质,E-mail:48833488@qq.com
  • 中图分类号: P595;P532

Sedimentary characteristics of the Early and Middle Holocene loess in Tongchuan area and their implications for paleoclimate

More Information
  • 通过对铜川剖面黄土-古土壤沉积粒度的组成和变化特征及磁化率值进行分析,探讨了该地区11.4~1.5 kaBP期间的古气候变化特征。结果表明:(1)铜川剖面黄土-古土壤沉积以粉砂粒(4~63 μm)为主,黏粒(<4 μm)次之,砂粒(>63 μm)含量最低。(2)粒度和磁化率值在不同地层单元呈规律性变化:粉砂粒和砂粒在黄土层中较高,古土壤层中较低;黏粒和磁化率值在黄土层中较低,古土壤层中较高。(3)粉砂粒、黏粒和磁化率值的变化情况较好地记录了铜川地区11.4~1.5 kaBP期间的气候变化特征,可以将该地区的气候变化划分为4个阶段:11.4~10.2 kaBP寒冷干燥期,10.2~9.1 kaBP略温偏干期,9.1~4.4 kaBP温暖湿润期,4.4~1.5 kaBP较冷干期。

  • 加载中
  • 图 1  铜川剖面地理位置

    Figure 1. 

    图 2  铜川剖面粒度组成三角图

    Figure 2. 

    图 3  铜川剖面磁化率指标对降水和温度变化的响应(a,b)与东亚季风区年平均降水量(c)[25]及中国气温距平曲线(d)[26]

    Figure 3. 

    图 4  铜川剖面气候记录指标与东亚夏季风指标、降水记录及石笋记录对比

    Figure 4. 

    表 1  铜川剖面粒度及磁化率参数

    Table 1.  Magnetic susceptibility and grain size parameters of the samples from Tongchuan section

    地层单元平均粒径
    /μm
    黏粒
    (<4 μm)/%
    粉砂
    (4~63 μm)/%
    砂粒
    (>63 μm)/%
    低频磁化率
    χlf/(10−8 m3 /kg)
    频率磁化率
    χfd/%
    全新世黄土
    (LO,50~155 cm)
    范围14.01~28.6020.11~32.9965.77~78.230.84~6.89117.90~142.808.73~10.74
    均值19.3525.8071.452.75125.419.70
    全新世古土壤
    (S0,155~320 cm)
    范围11.22~20.2020.83~37.9061.20~76.770.01~3.54160.22~357.4510.02~11.36
    均值14.0831.6867.251.07268.2610.85
    过渡性黄土层
    (Lt,320~362 cm)
    范围13.25~18.3924.94~32.8266.12~72.981.06~2.6198.39~157.419.38~10.37
    均值16.7827.2470.791.97114.029.73
    马兰黄土层
    (L1,362~400 cm)
    范围16.38~29.4817.72~25.9672.57~79.101.47~6.4386.90~103.137.19~9.65
    均值20.3321.9875.152.8894.228.84
    全剖面
    (50~400 cm)
    范围11.22~29.4817.72~37.9061.20~79.100.01~6.8986.90~357.457.19~11.36
    均值16.6528.3569.781.87188.4110.16
    下载: 导出CSV
  • [1]

    Lu H Y, An Z S. Paleoclimatic significance of grain size of loess-palaeosol deposit in Chinese Loess Plateau [J]. Science in China Series D: Earth Sciences, 1998, 41(6): 626-631. doi: 10.1007/BF02878745

    [2]

    Guan H C, Zhu C, Zhu T X, et al. Grain size, magnetic susceptibility and geochemical characteristics of the loess in the Chaohu lake basin: implications for the origin, palaeoclimatic change and provenance [J]. Journal of Asian Earth Sciences, 2016, 117: 170-183. doi: 10.1016/j.jseaes.2015.12.013

    [3]

    杨石岭, 丁仲礼. 黄土高原黄土粒度的空间变化及其古环境意义[J]. 第四纪研究, 2017, 37(5):934-944 doi: 10.11928/j.issn.1001-7410.2017.05.02

    YANG Shiling, DING Zhongli. Spatial changes in grain size of loess deposits in the Chinese Loess Plateau and implications for palaeoenvironment [J]. Quaternary Sciences, 2017, 37(5): 934-944. doi: 10.11928/j.issn.1001-7410.2017.05.02

    [4]

    鹿化煜, 安芷生. 洛川黄土粒度组成的古气候意义[J]. 科学通报, 1997, 42(1):67-69

    LU Huayu, AN Zhisheng. Paleoclimatic significance of the composition of Luochuan loess [J]. Chinese Science Bulletin, 1997, 42(1): 67-69.

    [5]

    An Z S, Kukla G J, Porter S C, et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130, 000 years [J]. Quaternary Research, 1991, 36(1): 29-36. doi: 10.1016/0033-5894(91)90015-W

    [6]

    Sun Y B, An Z S, Clemens S C, et al. Seven million years of wind and precipitation variability on the Chinese Loess Plateau [J]. Earth and Planetary Science Letters, 2010, 297(3-4): 525-535. doi: 10.1016/j.jpgl.2010.07.004

    [7]

    于昊, 彭廷江, 李孟, 等. 西部黄土高原兰州黄土磁化率增强模式及其驱动机制[J]. 海洋地质与第四纪地质, 2018, 38(2):165-174

    YU Hao, PENG Tingjiang, LI Meng, et al. Magnetic susceptibility enhancement model and its driving mechanism of Lanzhou loess on the Western Loess Plateau [J]. Marine Geology & Quaternary Geology, 2018, 38(2): 165-174.

    [8]

    Zhao H, Chen F H, Li S H, et al. A record of Holocene climate change in the Guanzhong Basin, China, based on optical dating of a loess-palaeosol sequence [J]. The Holocene, 2007, 17(7): 1015-1022. doi: 10.1177/0959683607080530

    [9]

    黄春长, 庞奖励, 黄萍, 等. 关中盆地西部黄土台塬全新世气候事件研究[J]. 干旱区地理, 2002, 25(1):10-15 doi: 10.3321/j.issn:1000-6060.2002.01.003

    HUANG Chunchang, PANG Jiangli, HUANG Ping, et al. Holocene climatic events on the loess tableland in the Western Guanzhong Basin, China [J]. Arid Land Geography, 2002, 25(1): 10-15. doi: 10.3321/j.issn:1000-6060.2002.01.003

    [10]

    庞奖励, 黄春长, 刘安娜, 等. 黄土高原南部全新世黄土-古土壤序列若干元素分布特征及意义[J]. 第四纪研究, 2007, 27(3):357-364 doi: 10.3321/j.issn:1001-7410.2007.03.007

    PANG Jiangli, HUANG Chunchang, LIU Anna, et al. Ba/Sr and Rb/Sr ratio of Holocene loess-palaeosol sequences and its significance in South Loess Plateau, China [J]. Quaternary Sciences, 2007, 27(3): 357-364. doi: 10.3321/j.issn:1001-7410.2007.03.007

    [11]

    贾耀锋, 庞奖励, 黄春长, 等. 关中盆地全新世黄土-土壤剖面微量元素的地球化学特征及其古气候意义[J]. 土壤通报, 2012, 43(3):513-520

    JIA Yaofeng, PANG Jiangli, HUANG Chunchang, et al. Geochemistry of trace elements and their paleoclimatic implications in the loess-soil section in Guanzhong basin [J]. Chinese Journal of Soil Science, 2012, 43(3): 513-520.

    [12]

    刘安娜, 庞奖励, 黄春长, 等. 甘肃庄浪全新世黄土-古土壤序列元素分布特征及意义[J]. 地球化学, 2006, 35(4):453-458 doi: 10.3321/j.issn:0379-1726.2006.04.013

    LIU Anna, PANG Jiangli, HUANG Chunchang, et al. Element distributions of the Zhuanglang Holocene loess-paleosol sequence, Gansu Province and its significance [J]. Geochimica, 2006, 35(4): 453-458. doi: 10.3321/j.issn:0379-1726.2006.04.013

    [13]

    王琳栋, 杨太保, 梁烨, 等. 会宁地区全新世黄土沉积粒度特征及其古气候意义[J]. 干旱区研究, 2016, 33(6):1150-1156

    WANG Lindong, YANG Taibao, LIANG Ye, et al. Grain size characteristics in the loess-paleosol at Huining section and its signification to paleoclimate during Holocene [J]. Arid Zone Research, 2016, 33(6): 1150-1156.

    [14]

    贾佳, 夏敦胜, 魏海涛, 等. 耀县黄土记录的全新世东亚冬夏季风非同步演化[J]. 第四纪研究, 2009, 29(5):966-975 doi: 10.3969/j.issn.1001-7410.2009.05.14

    JIA Jia, XIA Dunsheng, WEI Haitao, et al. Asynchronous evolution of East Asia summer and winter monsoons of the Holocene recorded by Yao County loess [J]. Quaternary Sciences, 2009, 29(5): 966-975. doi: 10.3969/j.issn.1001-7410.2009.05.14

    [15]

    Xia D S, Jia J, Li G H, et al. Out-of-phase evolution between summer and winter East Asian monsoons during the Holocene as recorded by Chinese loess deposits [J]. Quaternary Research, 2014, 81(3): 500-507. doi: 10.1016/j.yqres.2013.11.002

    [16]

    周家兴, 吴利杰, 于娟, 等. 铜川地区11.4~1.5 kaBP期间黄土地球化学风化特征及其古气候意义[J]. 地球与环境, 2019, 47(1):64-73

    ZHOU Jiaxing, WU Lijie, YU Juan, et al. Characteristics of geochemical weathering of loess in the Tongchuan area during 11.4~1.5 kaBP and its paleoclimatic implications [J]. Earth and Environment, 2019, 47(1): 64-73.

    [17]

    Zhao C L, Shao M A, Jia X U, et al. Particle size distribution of soils (0-500 cm) in the Loess Plateau, China [J]. Geoderma Regional, 2016, 7(3): 251-258. doi: 10.1016/j.geodrs.2016.05.003

    [18]

    Buggle B, Hambach U, Müller K, et al. Iron mineralogical proxies and Quaternary climate change in SE-European loess–paleosol sequences [J]. CATENA, 2014, 117: 4-22. doi: 10.1016/j.catena.2013.06.012

    [19]

    Liu Q S, Deng C L, Yu Y, et al. Temperature dependence of magnetic susceptibility in an argon environment: implications for pedogenesis of Chinese loess/palaeosols [J]. Geophysical Journal International, 2005, 161(1): 102-112. doi: 10.1111/j.1365-246X.2005.02564.x

    [20]

    An Z S, Liu T S, Lu Y C, et al. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China [J]. Quaternary International, 1990, 7-8: 91-95. doi: 10.1016/1040-6182(90)90042-3

    [21]

    陈璞皎, 郑祥民, 周立旻, 等. 宁镇地区下蜀黄土粒度特征及其古环境意义[J]. 地质科技情报, 2017, 36(5):7-13

    CHEN Pujiao, ZHENG Xiangmin, ZHOU Limin, et al. Grain size distribution and its significance of the Xiashu loess in Nanjing-Zhenjiang area [J]. Geological Science and Technology Information, 2017, 36(5): 7-13.

    [22]

    汪海斌, 陈发虎, 张家武. 黄土高原西部地区黄土粒度的环境指示意义[J]. 中国沙漠, 2002, 22(1):21-26 doi: 10.3321/j.issn:1000-694X.2002.01.005

    WANG Haibin, CHEN Fahu, ZHANG Jiawu. Environmental significance of grain size of loess-paleosol sequence in Western part of Chinese Loess Plateau [J]. Journal of Desert Research, 2002, 22(1): 21-26. doi: 10.3321/j.issn:1000-694X.2002.01.005

    [23]

    宋扬, 郝青振, 葛俊逸, 等. 黄土高原表土磁化率与气候要素的定量关系研究[J]. 第四纪研究, 2012, 32(4):679-689 doi: 10.3969/j.issn.1001-7410.2012.04.13

    SONG Yang, HAO Qingzhen, GE Junyi, et al. Quantitative relationships between modern soil magnetic susceptibility and climatic variables of the Chinese Loess Plateau [J]. Quaternary Sciences, 2012, 32(4): 679-689. doi: 10.3969/j.issn.1001-7410.2012.04.13

    [24]

    路彩晨, 贾佳, 高福元, 等. 全新世安塞剖面的磁学特征变化历史及其受控因子分析[J]. 海洋地质与第四纪地质, 2018, 38(5):178-184

    LU Caichen, JIA Jia, GAO Fuyuan, et al. Holocene variations of paleomagnetic characteristics along the loess section of Ansai and their controlling factors [J]. Marine Geology & Quaternary Geology, 2018, 38(5): 178-184.

    [25]

    Chen F H, Xu Q H, Chen J H, et al. East Asian summer monsoon precipitation variability since the last deglaciation [J]. Scientific Reports, 2015, 5: 11186. doi: 10.1038/srep11186

    [26]

    侯光良, 方修琦. 中国全新世气温变化特征[J]. 地理科学进展, 2011, 30(9):1075-1080 doi: 10.11820/dlkxjz.2011.09.001

    HOU Guangliang, FANG Xiuqi. Characteristics of Holocene temperature change in China [J]. Progress in Geography, 2011, 30(9): 1075-1080. doi: 10.11820/dlkxjz.2011.09.001

    [27]

    Wang Y B, Liu X Q, Herzschuh U. Asynchronous evolution of the Indian and East Asian Summer Monsoon indicated by Holocene moisture patterns in monsoonal central Asia [J]. Earth-Science Reviews, 2010, 103(3-4): 135-153. doi: 10.1016/j.earscirev.2010.09.004

    [28]

    Berger A, Loutre M F. Insolation values for the climate of the last 10 million years [J]. Quaternary Science Reviews, 1991, 10(4): 297-317. doi: 10.1016/0277-3791(91)90033-Q

    [29]

    Wang Y J, Cheng H, Edwards R L, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224, 000 years [J]. Nature, 2008, 451(7182): 1090-1093. doi: 10.1038/nature06692

  • 加载中

(4)

(1)

计量
  • 文章访问数:  2000
  • PDF下载数:  83
  • 施引文献:  0
出版历程
收稿日期:  2018-09-19
修回日期:  2018-12-19
刊出日期:  2020-02-25

目录