Chromaticity characteristics of the Last Glacial sediments in Houtian section of Nanchang city and its paleoenvironmental significance
-
摘要:
色度是古环境重建的重要指标之一，常用于黄土高原黄土古气候重建，但其在亚热带湿润区第四纪沉积中的研究十分少见且意义不明。选取鄱阳湖南岸之厚田沙地的沉积剖面为研究对象，进行了色度测试，结合光释光测年结果,将色度参数与其他气候代用指标进行对比，探讨MIS4—MIS2期间的古气候变化特征。结果表明：各色度参数曲线在剖面垂直方向上产生了较大波动，呈现出干冷→暖湿→干冷的多个冷暖震荡。其中L*值曲线的波峰段主要集中在沙丘砂层（HT6、HT4、HT1），指示MIS4阶段、MIS3b阶段和MIS2晚期阶段为干燥寒冷的气候环境，冬季风增强；a*、b*、C*和h*值曲线的波峰段主要集中在砂质古土壤层（HT5、HT3、HT2），指示MIS3c阶段、MIS3a阶段和MIS2早期阶段为温暖湿润的气候环境，夏季风增强，反映了该区域在末次冰期受冬季风和夏季风交替影响的气候演变格局。
-
关键词:
- 末次冰期 /
- 沙丘砂-砂质古土壤序列 /
- 色度 /
- 古环境 /
- 厚田沙地
Abstract:Chroma is one of the important indicators of paleoenvironment reconstruction, and is often used for paleoclimate reconstruction of the loess plateau, but its research in the Quaternary sediments in subtropical humid regions is rare and its significance is unclear. The sedimentary profile of Houtian sandy land on the south bank of Poyang Lake was selected as the research object and the chromaticity test was carried out. Combining with the results of optically stimulated luminescence (OSL), the chromaticity parameters were compared with other climatic proxies, and the paleoclimate changes during MIS2-MIS4 were discussed. Results show that the chromaticity parameter curves have large fluctuations in the vertical direction of the profile, showing multiple cold-warm oscillations from dry-cold → warm-wet → dry-cold. Among them, the peak sections of the L* (brightness) value curve are mainly concentrated in the dune sand layers of HT6, HT4, and HT1, indicating that the MIS4 stage, MIS3b stage, and early MIS2 stage, respectively, are dry and cold climate environment. The peak sections of the a*(redness), b* (yellowness), C* (saturation), and h* (hue) value curves are mainly concentrated in the sandy palaeosol layers of HT5, HT3, and HT2, representing the MIS3c stage, MIS3a stage and late MIS2 stage respectively, are warm and humid climate environment. The chromaticity index better reveals the characteristics of climate change in the Houtian area, and reflect the climate evolution pattern in the area affected by alternating winter monsoon and summer monsoon during the last glacial period.
-
-
表 1 厚田剖面地层特征描述
Table 1. Description of stratigraphic characteristics of the Houtian section
地层分层 深度/m 地层特征 HT1 0～0.50 黄红色沙丘砂层，松散，含较多植物根系 HT2 0.50～1.34 浅棕红色砂质古土壤层，较松散，含黄红色斑点 HT3 1.34～2.64 上部为黄红色砂质古土壤层，松散且无层理；下部为浅棕红色—黄红色中细砂，较紧实，
含较多铁质结核与斑点HT4 2.64～3.44 黄红色沙丘砂层，松散，含较多云母片 HT5 3.44～4.24 浅棕红色砂质古土壤层，紧实 HT6 4.24～5.74 灰白色沙丘砂层，松散 
下载: 导出CSV
表 2 厚田剖面色度分段变化规律
Table 2. Variation of chromaticity in different vertical sectors of the Houtian section
色度参数 层位 HT1 HT2 HT3 HT4 HT5 HT6 L* 范围 58.32～66.57 61.00～66.83 56.08～63.94 56.80～67.86 58.87～69.23 56.89～69.71 平均值 62.93 63.84 60.53 62.82 63.08 65.01 a* 范围 11.66～14.21 11.85～15.13 11.72～14.34 9.81～13.59 10.18～13.04 8.25～12.98 平均值 12.94 13.73 13.24 12.40 12.23 10.49 b* 范围 29.06～32.38 30.22～34.65 31.57～35.83 29.39～36.41 29.82～33.38 28.08～34.42 平均值 30.48 32.30 33.84 32.77 31.67 30.49 a*/b* 范围 0.390～0.448 0.389～0.443 0.371～0.412 0.333～0.403 0.341～0.401 0.279～0.385 平均值 0.424 0.425 0.391 0.378 0.386 0.343 C* 范围 31.66～35.20 32.46～37.81 33.68～38.50 31.01～38.85 31.51～35.80 29.47～36.79 平均值 33.11 35.10 36.34 35.04 33.96 32.25 h* 范围 0.372～0.421 0.371～0.417 0.355～0.390 0.321～0.383 0.329～0.381 0.272～0.367 平均值 0.401 0.402 0.373 0.361 0.368 0.330
下载: 导出CSV
表 3 色度参数L*、a*、b*与色饱和度C*、色调角h*的相关性分析
Table 3. Correlation between chromaticity indices L*, a*, b*, color saturation C* and hue angle h*
色度参数 L* a* b* C* h* L* 1 a* −0.7041 1 b* −0.8391 0.7829 1 C* −0.8398 0.8707 0.9876 1 h* −0.4707 0.9135 0.4643 0.5968 1
下载: 导出CSV
-
[1] 柯夫达 B A. 土壤学原理(上)[M]. 北京: 科学出版社, 1981: 19-20
KOVDA V A. Principles of Soil Science (One)[M]. Beijing: Science Press, 1981: 19-20.
[2] 苗运法, 杨胜利, 卓世新, 等. 我国西北干旱区现代地表沉积物颜色指标与降水关系[J]. 海洋地质与第四纪地质, 2013, 33(4):77-85 doi: 10.3724/SP.J.1140.2013.04077
MIAO Yunfa, YANG Shengli, ZHUO Shixin, et al. Relationship between the color of surface sediments and precipitation in arid northwest China [J]. Marine Geology and Quaternary Geology, 2013, 33(4): 77-85. doi: 10.3724/SP.J.1140.2013.04077
[3] Yang S L, Ding Z L. Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles [J]. Geophysical Research Letters, 2003, 30(20): 2058.
[4] 沈曼丽, 张军, 惠争闯. 兰州西津黄土色度指标记录的第四纪气候演化[J]. 冰川冻土, 2021, 43(3):809-817
SHEN Manli, ZHANG Jun, HUI Zhengchuang. Quaternary climate evolution recorded by loess chromatic proxy in Xijin, Lanzhou [J]. Journal of Glaciology and Geocryology, 2021, 43(3): 809-817.
[5] 莫东坡, 朱丽东, 李凤全, 等. 浙江曹娥江下游XYC孔色度特征及其全新世环境记录[J]. 古地理学报, 2018, 20(1):163-174 doi: 10.7605/gdlxb.2018.01.011
MO Dongpo, ZHU Lidong, LI Fengquan, et al. Chroma characteristics and its holocene environmental record of borehole XYC in the downstream area of Cao’e River, Zhejiang Province [J]. Journal of Palaeogeography, 2018, 20(1): 163-174. doi: 10.7605/gdlxb.2018.01.011
[6] 曹乐, 胡春生, 李文慧, 等. 宣城红土剖面色度特征及其古气候意义[J]. 安徽师范大学学报:自然科学版, 2019, 42(4):355-359 doi: 10.14182/J.cnki.1001-2443.2019.04.010
CAO Le, HU Chunsheng, LI Wenhui, et al. Chroma characteristics of Xuancheng red clay profile and its paleoclimatic significance [J]. Journal of Anhui Normal University (Natural Science), 2019, 42(4): 355-359. doi: 10.14182/J.cnki.1001-2443.2019.04.010
[7] 方小敏, 潘保田, 管东红, 等. 兰州约60 ka以来夏季风千年尺度不稳定性研究[J]. 科学通报, 1999, 44(24):2264-2267 doi: 10.3321/j.issn:0023-074X.1999.04.024
FANG Xiaomin, PAN Baotian, GUAN Donghong, et al. A 60 000-year loess-paleosol record of millennial-scale summer monsoon instability from Lanzhou, China [J]. Chinese Science Bulletin, 1999, 44(24): 2264-2267. doi: 10.3321/j.issn:0023-074X.1999.04.024
[8] 王千锁, 宋友桂, 李吉均, 等. 末次冰期-间冰期旋回朝那黄土颜色特征及古气候意义[J]. 地理科学, 2015, 35(11):1489-1494 doi: 10.13249/j.cnki.sgs.2015.11.019
WANG Qiansuo, SONG Yougui, LI Jijun, et al. Characteristics of color in Chaona section and its paleoclimatic significance during the Last Glacial-interglacial Cycle [J]. Scientia Geographica Sinica, 2015, 35(11): 1489-1494. doi: 10.13249/j.cnki.sgs.2015.11.019
[9] 陈一萌, 陈兴盛, 宫辉力, 等. 土壤颜色: 一个可靠的气候变化代用指标[J]. 干旱区地理, 2006, 29(3):309-313 doi: 10.3321/j.issn:1000-6060.2006.03.001
CHEN Yimeng, CHEN Xingsheng, GONG Huili, et al. Soil color: a new sensitive indicator for climatic change [J]. Arid Land Geography, 2006, 29(3): 309-313. doi: 10.3321/j.issn:1000-6060.2006.03.001
[10] 李越, 宋友桂, 王千锁. 新疆昭苏黄土剖面色度变化特征及古气候意义[J]. 地球环境学报, 2014, 5(2):67-75 doi: 10.7515/JEE201402003
LI Yue, SONG Yougui, WANG Qiansuo. Chroma characteristics in the Zhaosu loess section and its paleoclimatic significance [J]. Journal of Earth Environment, 2014, 5(2): 67-75. doi: 10.7515/JEE201402003
[11] 杨胜利, 方小敏, 李吉均, 等. 表土颜色和气候定性至半定量关系研究[J]. 中国科学:D辑, 2001, 44(1):218-226
YANG Shengli, FANG Xiaomin, LI Jijun, et al. Transformation functions of soil color and climate [J]. Science in China Series D:Earth Sciences, 2001, 44(1): 218-226.
[12] 石培宏, 杨太保, 田庆春, 等. 靖远黄土-古土壤色度变化特征分析及古气候意义[J]. 兰州大学学报:自然科学版, 2012, 48(2):15-23
SHI Peihong, YANG Taibao, TIAN Qingchun, et al. Chroma chracteristics in the loess-paleosol at Jingyuan section and its signification to paleocliamete [J]. Journal of Lanzhou University (Natural Sciences), 2012, 48(2): 15-23.
[13] 王志刚, 李志文, 黎武标, 等. 南昌市厚田沙地风沙沉积记录的末次冰期气候变化特征[J]. 中国沙漠, 2018, 38(6):1200-1208
WANG Zhigang, LI Zhiwen, LI Wubiao, et al. Climatic change recorded by Aeolian deposition in the Houtian section of Nanchang during the last glacial period [J]. Journal of Desert Research, 2018, 38(6): 1200-1208.
[14] 詹江振, 李志文, 王志刚, 等. 南昌市厚田剖面末次冰期风沙沉积的粒度分维特征及其揭示的古环境意义[J]. 热带地理, 2020, 40(6):1075-1084
ZHAN Jiangzhen, LI Zhiwen, WANG Zhigang, et al. Grain-Size fractal dimension of Aeolian sand during the last glacial period: The Houtian section of Nanchang and its paleoenvironmental significance [J]. Tropical Geography, 2020, 40(6): 1075-1084.
[15] 饶文波, 李晓彪, 高振敏, 等. 洛川黄土剖面中矿物固定态铵的分布[J]. 中国沙漠, 2004, 24(6):685-688 doi: 10.3321/j.issn:1000-694X.2004.06.004
RAO Wenbo, LI Xiaobiao, GAO Zhenmin, et al. Distribution of fixed-
$ {\rm{NH}}^{+} $ [16] 姚檀栋, THOMPSON L G, 施雅风, 等. 古里雅冰芯中末次间冰期以来气候变化记录研究[J]. 中国科学:D辑, 1997, 40(6):662-668 doi: 10.3321/j.issn:1006-9267.1997.05.006
YAO Tandong, THOMPSON L G, SHI Yafeng, et al. Climate variation since the Last Interglaciation recorded in the Guliya ice core [J]. Science in China Series D:Earth Sciences, 1997, 40(6): 662-668. doi: 10.3321/j.issn:1006-9267.1997.05.006
[17] 吴昊, 李志文, 郭福生, 等. 南昌市厚田乡风沙地貌形态特征与美学价值[J]. 华东地质, 2019, 40(4):264-272
WU Hao, LI Zhiwen, GUO Fusheng, et al. Morphological characteristics and aesthetic value of Aeolian landforms in Houtian township, Nanchang [J]. East China Geology, 2019, 40(4): 264-272.
[18] 李向洁, 李志文, 杜建会, 等. 南昌市厚田沙地蔓荆灌丛沙堆的形态与沉积特征[J]. 地理科学, 2021, 41(11):2042-2051 doi: 10.13249/j.cnki.sgs.2021.11.017
LI Xiangjie, LI Zhiwen, DU Jianhui, et al. Morphology and sedimentary characteristics of Vitex trifolia Nebkhas in the Houtian sandy land of Nanchang City [J]. Scientia Geographica Sinica, 2021, 41(11): 2042-2051. doi: 10.13249/j.cnki.sgs.2021.11.017
[19] 邹学勇. 南昌地区风沙化土地风沙地貌发育规模和风沙活动预测[J]. 地理研究, 1991, 10(3):51-58
ZOU Xueyong. The forecasts of desert landform scale and shifting sand action degrees in Nanchang area [J]. Geographical Research, 1991, 10(3): 51-58.
[20] 张克旗, 吴中海, 吕同艳, 等. 光释光测年法: 综述及进展[J]. 地质通报, 2015, 34(1):183-203 doi: 10.3969/j.issn.1671-2552.2015.01.015
ZHANG Keqi, WU Zhonghai, LV Tongyan, et al. Review and progress of OSL dating [J]. Geological Bulletin of China, 2015, 34(1): 183-203. doi: 10.3969/j.issn.1671-2552.2015.01.015
[21] Lisiecki L E, Raymo M E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records[J]. Paleoceanography, 20(1): PA1003.
[22] 王海燕, 庞奖励, 黄春长, 等. 郧西县庹家湾黄土剖面色度参数特征及其古气候重建[J]. 水土保持学报, 2017, 31(2):151-156 doi: 10.13870/j.cnki.stbcxb.2017.02.026
WANG Haiyan, PANG Jiangli, HUANG Chunchang, et al. Chroma characteristics and paleoclimatic reconstruction of the loess-paleosol profile at Tuojiawan in Yunxi county, Hubei Province [J]. Journal of Soil and Water Conservation, 2017, 31(2): 151-156. doi: 10.13870/j.cnki.stbcxb.2017.02.026
[23] 冯力威, 吴克宁, 查理思, 等. 仰韶文化遗址区古土壤色度特征及其气候意义[J]. 生态环境学报, 2015, 24(5):892-897 doi: 10.16258/j.cnki.1674-5906.2015.05.026
FENG Liwei, WU Kening, ZHA Lisi, et al. Chroma characteristics and its climatic significance of Yangshao culture relic [J]. Ecology and Environmental Sciences, 2015, 24(5): 892-897. doi: 10.16258/j.cnki.1674-5906.2015.05.026
[24] 顾磊. 基于色度学的灵台剖面晚新生代地层序列研究[D]. 兰州大学硕士学位论文, 2011
GU Lei. A study on Lingtai section of late cenozoic era based on colorimetry[D]. Master Dissertation of Lanzhou University, 2011.
[25] 杜兰, 李志文, 杜丁丁, 等. 烟台芝罘黄土剖面末次间冰期沉积物色度特征及其古环境意义[J]. 热带地理, 2021, 41(2):423-430 doi: 10.13284/j.cnki.rddl.003328
DU Lan, LI Zhiwen, DU Dingding, et al. Chromatic characteristics of sediments in Zhifu loess section of Yantai during the last Interglacial period and its paleoenvironmental significance [J]. Tropical Geography, 2021, 41(2): 423-430. doi: 10.13284/j.cnki.rddl.003328
[26] 杨丹, 庞奖励, 周亚利, 等. 汉中盆地军王村黄土-古土壤剖面的色度特征及机理[J]. 中山大学学报:自然科学版, 2018, 57(1):93-101 doi: 10.13471/j.cnki.acta.snus.2018.01.013
YANG Dan, PANG Jiangli, ZHOU Yali, et al. Chroma characteristics and its significance of the Junwangcun loess-paleosol profile in the Hanzhong basin [J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2018, 57(1): 93-101. doi: 10.13471/j.cnki.acta.snus.2018.01.013
[27] 刘荔昀, 鲁瑞洁, 刘小槺. 风成沉积物色度记录的毛乌素沙漠全新世以来气候变化[J]. 中国沙漠, 2019, 39(6):83-89
LIU Liyun, LU Ruijie, LIU Xiaokang. Climate change in the Mu us desert since Holocene based on soil chromaticity [J]. Journal of Desert Research, 2019, 39(6): 83-89.
[28] 李杨, 方晶, 潘隆, 等. 沉积物色度在古环境重建中的应用[J]. 气象科技进展, 2018, 8(6):22-27 doi: 10.3969/j.issn.2095-1973.2018.06.003
LI Yang, FANG Jing, PAN Long, et al. Application of sediment chromaticity in paleo-environment reconstruction [J]. Advances in meteorological Science and Technology, 2018, 8(6): 22-27. doi: 10.3969/j.issn.2095-1973.2018.06.003
[29] 高鹏坤, 庞奖励, 黄春长, 等. 陕南丹凤茶房村黄土—古土壤剖面色度参数特征[J]. 沉积学报, 2015, 33(3):537-542 doi: 10.14027/j.cnki.cjxb.2015.03.011
GAO Pengkun, PANG Jiangli, HUANG Chunchang, et al. Chroma characteristics and its significances of the Chafangcun loess-paleosol profile in southeast Shaanxi, China [J]. Acta Sedimentologica Sinica, 2015, 33(3): 537-542. doi: 10.14027/j.cnki.cjxb.2015.03.011
[30] Sun Y B, He L, Liang L J, et al. Changing color of Chinese loess: geochemical constraint and paleoclimatic significance [J]. Journal of Asian Earth Sciences, 2011, 40(6): 1131-1138. doi: 10.1016/j.jseaes.2010.08.006
[31] 陈杰, 杨太保, 曾彪, 等. 中国帕米尔地区黄土上部色度变化特征及古气候意义[J]. 沉积学报, 2018, 36(2):333-342 doi: 10.14027/j.issn.1000-0550.2018.043
CHEN Jie, YANG Taibao, ZENG Biao, et al. Chroma characteristics and its paleoclimatic significance in Pamir Loess Section, China [J]. Acta Sedimentologica Sinica, 2018, 36(2): 333-342. doi: 10.14027/j.issn.1000-0550.2018.043
[32] 韩洪军, 陈海涛, 孔凡彪, 等. 山东章丘黄土剖面色度研究[J]. 枣庄学院学报, 2019, 36(5):59-64 doi: 10.3969/j.issn.1004-7077.2019.05.010
HAN Hongjun, CHEN Haitao, KONG Fanbiao, et al. Study on the Chroma of Zhangqiu loess in Shandong Province [J]. Journal of Zaozhuang University, 2019, 36(5): 59-64. doi: 10.3969/j.issn.1004-7077.2019.05.010
[33] 鹿化煜, 安芷生. 黄土高原黄土粒度组成的古气候意义[J]. 中国科学:D辑, 1998, 41(6):626-631 doi: 10.3321/j.issn:1006-9267.1998.03.002
LU Huayu, AN Zhisheng. 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: 10.3321/j.issn:1006-9267.1998.03.002
[34] 安芷生, PORTER S, KUKLA G, 等. 最近13万年黄土高原季风变迁的磁化率证据[J]. 科学通报, 1990, 35(7):529-532 doi: 10.1360/csb1990-35-7-529
AN Zhisheng, PORTER S, KUKLA G, et al. Magnetic susceptibility evidence for the 130000 year Loess Plateau monsoon variation [J]. Chinese Science Bulletin, 1990, 35(7): 529-532. doi: 10.1360/csb1990-35-7-529
-
图(5)
表(3)
计量
- 文章访问数: 1762
- PDF下载数: 79
- 施引文献: 0