Shenyang Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2024 Vol. 33, No. 5
Article Contents
Article navigation > Geology and Resources > 2024 > 33(5): 617-625
Next Article Previous Article

GAO Yuan, ZHOU Ye-ze, QIN Tian, HOU Hong-xing, PEI Yang, KOU Fu-jian, YAN Bo. SPOROPOLLEN ASSEMBLAGE OF BLACK SOIL SECTION IN EASTERN LIAOHE PLAIN: Age and Paleoclimatic Implication[J]. Geology and Resources, 2024, 33(5): 617-625. doi: 10.13686/j.cnki.dzyzy.2024.05.001
Citation: GAO Yuan, ZHOU Ye-ze, QIN Tian, HOU Hong-xing, PEI Yang, KOU Fu-jian, YAN Bo. SPOROPOLLEN ASSEMBLAGE OF BLACK SOIL SECTION IN EASTERN LIAOHE PLAIN: Age and Paleoclimatic Implication[J]. Geology and Resources, 2024, 33(5): 617-625. doi: 10.13686/j.cnki.dzyzy.2024.05.001
shu

SPOROPOLLEN ASSEMBLAGE OF BLACK SOIL SECTION IN EASTERN LIAOHE PLAIN: Age and Paleoclimatic Implication

  • Langfang Natural Resources Comprehensive Survey Center, CGS, Langfang 065000, Hebei Province, China

More Information
Received Date:  20 April 2023
Revised Date:  12 July 2023
Publish Date:  25 October 2024
    Abstract

  • By analysis of sporopollen in 0-1 m black soil profile PM25 in eastern Liaohe Plain, the fossils are divided into two sporopollen assemblages from bottom to top according to the sporopollen content change. The PM25-1 sporopollen assemblage is mainly Spiraea-Artemisia-Sanguisorba-Rosa-Echinate Asteraceae, with the climate changing from cold-dry to warm-wet; while the PM25-2 sporopollen assemblage is dominated by Pinus-Cyperaceae-Chenopodium, indicating the transition of climate from warm-wet to cold-dry. Combined with the 14C dating data, it is concluded that the black soil in eastern Liaohe Plain was mainly formed in Medieval Warm Period since 1335 a B.P.

    • FullText(HTML)
  • 加载中
    • References
  • [1] 陈铁梅. 14C测年与示踪用于研究四万年来的全球变化[J]. 第四纪研究, 1990, 2: 181-187. doi: 10.3321/j.issn:1001-7410.1990.02.009

    CrossRef Google Scholar

    Chen T M. Radiocarbon and Global Change[J]. Quaternary Sciences, 1990(2): 181-187. doi: 10.3321/j.issn:1001-7410.1990.02.009

    CrossRef Google Scholar

    [2] 陈铁梅, 李坤, 郭之虞, 等. 加速器质谱计在地球科学中的应用[J]. 海洋地质与第四纪地质, 1989, 9(1): 103-114.

    Google Scholar

    Chen T M, Li K, Guo Z Y, et al. Application of accelerator mass spectrometry to earth science[J]. Marine Geology & Quaternary Geology, 1989, 9(1): 103-114.

    Google Scholar

    [3] 程鹏, 周卫健, 余华贵, 等. 黄土-古土壤序列14C年代学研究进展[J]. 海洋地质与第四纪地质, 2007, 27(2): 85-89.

    Google Scholar

    Cheng P, Zhou W J, Yu H G, et al. Advances in radiocarbon dating researches in the loess-paleosol sequences[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 85-89.

    Google Scholar

    [4] 沈承德, 易惟熙, 孙彦敏, 等. 鼎湖山森林土壤14C表观年龄及δ13C分布特征[J]. 第四纪研究, 2000, 20(4): 335-344. doi: 10.3321/j.issn:1001-7410.2000.04.004

    CrossRef Google Scholar

    Shen C D, Yi W X, Sun Y M, et al. 14C apparent ages and δ13C distribution of forest soils in Dinghushan natural reserve[J]. Quaternary Sciences, 2000, 20(4): 335-344. doi: 10.3321/j.issn:1001-7410.2000.04.004

    CrossRef Google Scholar

    [5] 李汉鼎, 冷雪天, 白艳, 等. 泥炭样品14C年龄可靠性初步研究[J]. 海洋地质与第四纪地质, 1992, 12(2): 89-97.

    Google Scholar

    Li H D, Leng X T, Bai Y, et al. A preliminary study on reliability of 14C ages of peat samples[J]. Marine Geology & Quaternary Geology, 1992, 12(2): 89-97.

    Google Scholar

    [6] 边叶萍, 翁成郁. 孢粉稳定碳同位素研究进展[J]. 海洋地质与第四纪地质, 2009, 29(3): 141-148.

    Google Scholar

    Bian Y P, Weng C Y. An overview of carbon stable isotope analysis of pollen[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 141-148.

    Google Scholar

    [7] 赵辰辰, 王永波, 胥勤勉. 2.5 Ma以来中国陆地孢粉记录反映的古气候变化[J]. 海洋地质与第四纪地质, 2020, 40(4): 175-191.

    Google Scholar

    Zhao C C, Wang Y B, Xu Q M. Climate changes on Chinese continent since 2.5 Ma: Evidence from fossil pollen records[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 175-191.

    Google Scholar

    [8] 孙湘君, 罗运利, 陈怀成. 中国第四纪深海孢粉研究进展[J]. 科学通报, 2003, 48(15): 1613-1621.

    Google Scholar

    Sun X J, Luo Y L, Chen H C. Deep-sea pollen research in China[J]. Chinese Science Bulletin, 2003, 48(20): 2155-2164.

    Google Scholar

    [9] 杨再宝, 李铁刚, 南青云. 8000 a BP以来珠江口西南部孢粉组合特征及其古气候意义[J]. 海洋地质与第四纪地质, 2012, 32(4): 33-40.

    Google Scholar

    Yang Z B, Li T G, Nan Q Y. Features of the sporopollen assemblages at southwestern Pearl River estuary over the past 8000 years and its paleoclimate implications[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 33-40.

    Google Scholar

    [10] 宋运红, 刘凯, 戴慧敏, 等. 松嫩平原东部典型黑土剖面孢粉组合、时代及其对古气候的指示[J]. 地质通报, 2022, 41(9): 1528-1538.

    Google Scholar

    Song Y H, Liu K, Dai H M, et al. Palynological assemblages of typical black soil profile in the eastern Songliao Plain and their age and paleoclimatic[J]. Geological Bulletin of China, 2022, 41(9): 1528-1538.

    Google Scholar

    [11] 范昊明, 蔡强国, 王红闪. 中国东北黑土区土壤侵蚀环境[J]. 水土保持学报, 2004, 18(2): 66-70. doi: 10.3321/j.issn:1009-2242.2004.02.017

    CrossRef Google Scholar

    Fan H M, Cai Q G, Wang H S. Condition of soil erosion in phaeozem region of Northeast China[J]. Journal of Soil and Water Conservation, 2004, 18(2): 66-70. doi: 10.3321/j.issn:1009-2242.2004.02.017

    CrossRef Google Scholar

    [12] 张新荣, 焦洁钰. 黑土形成与演化研究现状[J]. 吉林大学学报(地球科学版), 2020, 50(2): 553-568.

    Google Scholar

    Zhang X R, Jiao J Y. Formation and evolution of black soil[J]. Journal of Jilin University (Earth Science Edition), 2020, 50(2): 553-568.

    Google Scholar

    [13] 陆继龙, 周永昶, 周云轩. 吉林省黑土某些微量元素环境地球化学特征[J]. 土壤通报, 2002, 33(5): 365-368. doi: 10.3321/j.issn:0564-3945.2002.05.012

    CrossRef Google Scholar

    Lu J L, Zhou Y C, Zhou Y X. Environmental geochemical characteristics of some microelements in the black soil of Jilin Province[J]. Chinese Journal of Soil Science, 2002, 33(5): 365-368. doi: 10.3321/j.issn:0564-3945.2002.05.012

    CrossRef Google Scholar

    [14] 于磊, 张柏, 宋开山. 基于GIS的黑土区环境地球化学质量评价[J]. 干旱区资源与环境, 2004, 18(2): 23-26. doi: 10.3969/j.issn.1003-7578.2004.02.005

    CrossRef Google Scholar

    Yu L, Zhang B, Song K S. The geochemical environment quality evaluation on the black soil region based on GIS[J]. Journal of Arid Land Resources and Environment, 2004, 18(2): 23-26. doi: 10.3969/j.issn.1003-7578.2004.02.005

    CrossRef Google Scholar

    [15] 陆继龙, 周云轩, 周永昶, 等. 黑土农业区常量和微量元素环境地球化学特征[J]. 农业环境与发展, 2002, 19(1): 27-29. doi: 10.3969/j.issn.1005-4944.2002.01.014

    CrossRef Google Scholar

    Lu J L, Zhou Y X, Zhou Y C, et al. Environmental geochemical characteristics of major and trace elements in black soil agricultural areas[J]. Journal of Agricultural Resources and Environment, 2002, 19(1): 27-29. doi: 10.3969/j.issn.1005-4944.2002.01.014

    CrossRef Google Scholar

    [16] 余华贵, 祝一志, 程鹏, 等. 热解法用于礼村黄土-古土壤地层 14C测年[J]. 海洋地质与第四纪地质, 2009, 29(1): 73-78.

    Google Scholar

    Yu H G, Zhu Y Z, Cheng P, et al. Pyrolysis-combustion method used to do 14C dating of Holocene loess sequence at Licun profile[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 73-78.

    Google Scholar

    [17] 罗丽萍, 朱利东, 向芳, 等. 成都平原4000 a BP以来的孢粉记录与环境变化[J]. 古生物学报, 2008, 47(2): 195-202.

    Google Scholar

    Luo L P, Zhu L D, Xiang F, et al. Spore-pollen assemblage and environmental changes of the Chengdu Plain during the late Holocene[J]. Acta Palaeontologica Sinica, 2008, 47(2): 195-202.

    Google Scholar

    [18] 高瑞祺, 赵传本, 乔秀云, 等. 松辽盆地白垩纪石油地层孢粉学[M]. 北京: 地质出版社, 1999: 20-100.

    Google Scholar

    Gao R Q, Zhao C B, Qiao X Y, et al. Cretaceous oil strata palynology from Songliao Basin[M]. Beijing: Geological Publishing House, 1999: 20-100.

    Google Scholar

    [19] 裘善文, 李取盛, 夏玉梅, 等. 东北西部沙地古土壤与全新世环境[M]//施雅风. 中国全新世大暖期气候与环境. 北京: 海洋出版社, 1992: 153-160.

    Google Scholar

    Qiu S W, Li Q S, Xia Y M, et al. Paleosoil and Holocene environment of sandy land in western Northeast China[M]//Shi Y F. The climates and environments of Holocene Megathermal in China. Beijing: China Ocean Press, 1992: 153-160.

    Google Scholar

    [20] 高远, 秦天, 李瑞红, 等. 松辽盆地梨树断陷嫩江组孢粉记录及古气候特征[J]. 吉林大学学报(地球科学版), 2023, 53(5): 1391-1402.

    Google Scholar

    Gao Y, Qin T, Li R H, et al. Palynological records and paleoclimatic characteristics of Nenjiang Formation in Lishu fault depression, Songliao Basin[J]. Journal of Jilin University (Earth Science Edition), 2023, 53(5): 1391-1402.

    Google Scholar

    [21] 李徐生, 杨达源, 鹿化煜. 皖南风尘堆积序列氧化物地球化学特征与古气候记录[J]. 海洋地质与第四纪地质, 1999, 19(4): 75-82.

    Google Scholar

    Li X S, Yang D Y, Lu H Y. Oxide-geochemistry features and paleoclimatic record of the aeolian-dust depositional sequence in southern Anhui[J]. Marine Geology & Quaternary Geology, 1999, 19(4): 75-82.

    Google Scholar

    [22] 张玉芬, 李长安, 熊德强, 等. "巫山黄土"氧化物地球化学特征与古气候记录[J]. 中国地质, 2013, 40(1): 352-360.

    Google Scholar

    Zhang Y F, Li C A, Xiong D Q, et al. Oxide geochemical characteristics and paleoclimate records of "Wushan loess"[J]. Geology in China, 2013, 40(1): 352-360.

    Google Scholar

    [23] 冯志刚, 王世杰, 刘秀明, 等. 微地域搬运——碳酸盐岩红色风化壳形成过程的一种方式[J]. 地质学报, 2007, 81(1): 127-138.

    Google Scholar

    Feng Z G, Wang S J, Liu X M, et al. Micro-area transportation of residues: A style of forming the red weathering crusts of carbonate rocks[J]. Acta Geological Sinica, 2007, 81(1): 127-138.

    Google Scholar

    [24] 马晓晨, 王家生, 陈粲, 等. 华北房山景儿峪组顶部古风化壳常量元素地球化学特征及其古气候意义[J]. 地球科学, 2018, 43(11): 3853-3872.

    Google Scholar

    Ma X C, Wang J S, Chen C, et al. Major element compositions and paleoclimatic implications of paleo-regolith on top Jingeryu Formation in Fangshan, North China[J]. Earth Science, 2018, 43(11): 3853-3872.

    Google Scholar

    [25] 郭媛媛, 莫多闻, 毛龙江, 等. 澧阳平原岩板珰剖面地球化学特征与风化强度研究[J]. 地理科学, 2013, 33(3): 335-341.

    Google Scholar

    Guo Y Y, Mo D W, Mao L J, et al. Geochemical characteristics and weathering intensity of the Yanbandang profile in Liyang Plain, the middle reach of the Changjiang River[J]. Scientia Geographica Sinica, 2013, 33(3): 335-341.

    Google Scholar

    [26] 徐树建, 倪志超, 丁新潮. 山东平阴黄土剖面常量元素地球化学特征[J]. 矿物岩石地球化学通报, 2016, 35(2): 353-359.

    Google Scholar

    Xu S J, Ni Z C, Ding X C. Geochemical characteristics of major elements of the Pingyin loess in Shandong Province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2016, 35(2): 353-359.

    Google Scholar

    [27] 刘凯, 宋运红, 杨凤超, 等. 松嫩平原北部全新世黑土剖面孢粉组合及其对环境演化的制约[J]. 地质通报, 2023, 42(12): 2121-2131.

    Google Scholar

    Liu K, Song Y H, Yang F C, et al. Palynological assemblages of Holocene typical black soil profile from northern Songnen Plain and its restricts to environmental evolution[J]. Geological Bulletin of China, 2023, 42(12): 2121-2131.

    Google Scholar

    [28] 孔维翰. 下辽河平原第四纪微体古生物和气候[D]. 大连: 辽宁师范大学, 2014.

    Google Scholar

    Kong W H. Quaternary's micropalaeontology and climate of the Lower-Liaohe Plain[D]. Dalian: Liaoning Normal University, 2014.

    Google Scholar

    [29] 王强, 刘立军, 王卫东, 等. 环渤海地区及华北平原第四纪古环境变迁机制[J]. 地质调查与研究, 2004, 27(3): 129-138.

    Google Scholar

    Wang Q, Liu L J, Wang W D, et al. The mechanism of quaternary palaeoenvironmental change in circum-Bohai-sea region and North China plain[J]. Geological Survey and Research, 2004, 27(3): 129-138.

    Google Scholar

    [30] 冯丽杰, 郭伟静, 陈树良, 等. 松辽盆地南缘第四纪环境特征——以四平-双辽地区为例[J]. 地质与资源, 2007, 16(2): 81-85.

    Google Scholar

    Feng L J, Guo W J, Chen S L, et al. Quaternary environment characteristics in the southern margin of Song-Liao Basin: A case study of Siping-Shuangliao area[J]. Geology and Resources, 2007, 16(2): 81-85.

    Google Scholar

    [31] 刘祥, 侯兰英, 张志. 西辽河平原土地沙漠化地质环境演变研究[J]. 内蒙古农业大学学报, 2001, 22(3): 100-104.

    Google Scholar

    Liu X, Hou L Y, Zhang Z. Study on desertizational geological environment evolution in plain of Xi Liao River[J]. Journal of Inner Mongolia Agricultural University, 2001, 22(3): 100-104.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(6)

Tables(2)

Export Citation
PDF
XML

Article Metrics

Article views(81) PDF downloads(54) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020