Modern Pollen Assemblages of the Forest Communities and Their Relationships with Vegetation and Climate in Northern China

Expand
  • 1. College of Resources and Environment of Hebei Normal University, Shijiazhuang 050016, China;
    2. National Key Laboratory of Western China' s Environmental System, Ministry of Education, Lanzhou University, Lanzhou 730000, China;
    3. Hebei Institute of Geography Sciences, Shijiazhuang 050011, China

Received date: 2008-01-15

  Revised date: 2008-06-05

  Online published: 2008-09-25

Supported by

Preliminary Special Foundation for National Key Basic Research of China, No.2003CCA01800; Key National Natural Science Foundation of China, No. 40730103; National Natural Science Foundation of China, No.40672107; No.40571166

Abstract

In this paper, 53 pollen traps and surface samples were collected in order to detect the characteristics of pollen assemblages and their relationships with vegetation and climate in 16 forest communities located in 10 mountains in northern China. The results show that 72% of the pollen taxa (80 taxa) are the same between the traps and the surface samples. The dominant taxa in the plant communities are consistent with the main pollen taxa in the pollen assemblages at the same sites. In Pinus plant communities, both Pinus pollen influxes and concentrations are higher, indicating its higher pollen product and good pollen preservation ability. In Picea or Abies plant communities, Picea or Abies have lower pollen influx but high concentrations, suggesting their low pollen productivities but good pollen preservation abilities. In Betula or Quercus plant communities, Betula or Quercus have higher pollen influx but low concentrations, revealing their high pollen productivities but poor pollen preservation abilities. The study of the relationships between pollen and vegetation with discriminant analysis shows that pollen assemblages from both trap and surface samples can reflect the characters of different communities and distinguish different ecological areas, but the surface samples reflect the dominant components of communities much better than the traps. The study on the correlations between pollen assemblages and climate with DCCA reveals that significant correlations exist between pollen assemblages and mean temperature of the coldest month (R = 0.84 for trap samples, R = 0.72 for surface samples), and annual mean precipitation as well (R = 0.73 for trap samples, R = 0.71 for surface samples).

Cite this article

LI Yuecong1, XU Qinghai1, 2, WANG Xueli1, CAO Xianyong1, YANG Xiaolan3 . Modern Pollen Assemblages of the Forest Communities and Their Relationships with Vegetation and Climate in Northern China[J]. Acta Geographica Sinica, 2008 , 63(9) : 945 -957 . DOI: 10.11821/xb200809005

References


[1] Wu Yushu, Sun Xiangjun. Numerical characteristics of pollen assemblages of surface soil from the Xishan Mountains, Kunming. Acta Botanica Sinica, 1987, 29(2): 204-211.
[吴玉书, 孙湘君. 昆明西山林下表土花粉与植被间数量关系的 初步研究. 植物学报, 1987, 29(2): 204-211.]

[2] Yao Zuju. Surface pollen analysis in Zhongtiao Mountain. Acta Geographica Sinica, 1989, 44: 469-477.
[姚祖驹. 山西 中条山地区表土花粉分析. 地理学报, 1989, 44: 469-477.]

[3] Liu Guangxiu. Pollen analysis of surface samples from Dajiuhu Area, Hubei. Acta Botanica Boreali-Occidentalia Sinica, 1990, 10(3): 170-175.
[刘光琇. 神农架大九湖地区表土孢粉分析, 西北植物学报, 1990, 10(3): 170-175.]

[4] Yu Ge, Han Huiyou. A preliminary palynological study of the surface soil of modrn vegetation in the Zijin Mt., Nanjing. Acta Phytoecologica Sinica, 1995, 19(1): 79-84.
[于革, 韩辉友. 南京紫金山现代植被表土孢粉的初步研究, 植物生态 学报, 1995, 19(1): 79-84.]

[5] Zhang Jiahua, Kong Zhaochen, Du Naiqiu. Pollen analysis of surface samples from Baihua and Dongling Mountains in Beijing. Marine Geology & Quaternary Geology, 1996, 16(3): 101-112.
[张佳华, 孔昭宸, 杜乃秋. 北京地区百花山、 东灵山表土花粉的特征分析, 海洋地质与第四纪地质, 1996, 16(3), 101-112.]

[6] Yu Pengtao, Liu Hongyan. Surface pollen and its climatical significance of vertical zone in Beitai, Xiaowutai Mountain. Acta Scicentiarum Naturalum Universitis Pekinesis, 1997, 33(4): 475-483.
[于澎涛, 刘鸿雁. 小五台山北台北坡植被垂 直带的表土花粉及其气候意义研究, 北京大学学报, 1997, 33(4): 475-483.]

[7] Zhao Xiangui, Xiao Ling, Chen Cungen et al. Pollen analysis of surface soil sample from the Qinling Mountains. Journal of Northwest Forestry College, 1999, 14(1): 1-5.
[赵先贵, 肖玲, 陈存根等. 秦岭表土的花粉分析. 西北林学院学报, 1999, 14(1): 1-5.]

[8] Li Yiyin, Zhang Xinshi, Zhou Guangsheng. Study of quantitative relationship between vegetation and pollen in surface samples in the eastern forest area of Northeast China Transect. Acta Botanica Sinica, 2000, 42(1): 81-88.
[李宜垠, 张新 时, 周广胜. 中国东北样带(NECT)东部森林区的植被与表土花粉的定量关系. 植物学报, 2000, 42(1): 81-88.]

[9] Yang Zhenjing, Xu Qinghai, Meng Lingyao et al. Quantitative relationship between pollen in the surface soil and vegetation in the Yanshan area. Acta Phytoecologica Sinica, 2003, 27(6): 804-809.
[杨振京, 许清海, 孟令尧等. 燕山 地区表土花粉与植被间的数量关系. 植物生态学报, 2003, 27(6): 804-809.]

[10] Xu Qinghai, Li Yuecong, Yang Xiaolan et al. Quantitative relationship between pollen and vegetation in northern China. Science in China (Series D), 2007, 37(2): 192-205.
[中国北方几种主要花粉类型与植被定量关系. 中国科学 (D 辑), 2007, 37(2): 192-205.]

[11] Davis M B, Brubaker L, Webb Ⅲ T. Calibration of absolute pollen influx. In: Birks, H J B, West R G (eds.). Quaternary Plant Ecology. Oxford: Blackwell Science, 1973. 9-25.

[12] Hicks S. Pollen analogues and pollen influx values as tool for interpreting the history of a settlement centre and its hinterland. PACT, 1997, 52: 137-150.

[13] Hicks S, Tinsley H, Huusko A et al. Some comments on spatial variation in arboreal pollen deposition: First records from the Pollen Monitoring Programme (PMP). Review of Palaeobotany and Palynology, 2001, 117(1-3): 183-194.

[14] Tonkov S, Hicks S, Bozilova E et al. Pollen monitoring in the central Rila Mountains, Southwestern Bulgaria: Comparisons bteween pollen trap and surface samples for the period 1993-1999. Review of Palaeobotany and Palynology, 2001, 117(1-3): 167-182.

[15] Rasanen S, Hicks S, Odgaard B V. Pollen deposition in mosses and in a modified 'Tauber trap' from Hailuoto, Finland: What exactly do the mosses record? Review of Palaeobotany and Palynology, 2004, 129(1-3): 103-116.

[16] Vermoere M, Vanhecke L, Waelkens M et al. A comparison between modern pollen spectra of moss cushions and Cundill pollen traps. Grana, 2000, 39: 146-158.

[17] Koff T. Pollen influx into Tauber traps in Estonia in 1997-1998. Review of Palaeobotany and Palynology, 2001, 117 (1-3): 53-62.

[18] Bunting M J, Armitage R, Binney H A et al. Estimates of 'relative pollen productivity' and 'relevant source area of pollen' for major tree taxa in two Norfolk (UK) woodlands. The Holocene, 2005, 15(3): 459-465.

[19] Soepboer W, Sugita S, Lotter A F et al. Pollen productivity estimates for the reconstruction of past vegetation cover in the cultural landscape of southern Sweden. The Holocene, 2004, 14(3): 368-381.

[20] Sugita S, Gaillard M J, Brostrom A. Landscape openness and pollen records: A simulation approach. The Holocene, 1999, 9: 409-421.

[21] Sugita S. Theory of quantitative reconstruction of vegetation I: Pollen from large sites REVEALS regional vegetation composition. The Holocene, 2007, 17(2): 229- 241.

[22] Bennett K D, Hick S. Numerical analysis of surface and fossil pollen spectra from northern Fennoscandia. Journal of Biogeography, 2005, 32: 407-423.

[23] Barnekow L, Loader N J, Hicks S et al. Strong correlation between summer temperature and pollen accumulation rates for Pinus sylvestris, Picea abies and Betula spp. in a high-resolution record from northern Sweden. Journal of Quaternary Research, 2007, 22(7): 653-658.

[24] Sugita S, Parshall T, Calcote R. Detecting differences in vegetation among paired sites using pollen records. The Holocene, 2006, 16(8): 1123-1135.

[25] R!s"nen S, Suutari H, Nielsen A B. A step further towards quantitative reconstruction of past vegetation in Fennoscandian boreal forests. Review of Palaeobotany and Palynology, 2007, 146: 208-220.

[26] Sun Xiangjun, Wu Yushu. Modern pollen rain of needle and broadleaved mixed forest in Changbai Mountains. Acta Botanica Sinica, 1988, 30(5): 549-557.
[孙湘君, 吴玉书. 长白山针叶混交林的现代花粉雨. 植物学报, 1988, 30(5): 549-557.]

[27] Xu Qinghai, Li Yuecong, Zhou Liping et al. Pollen flux and vertical dispersion in coniferous and deciduous broadleaved mixed forest in the Changbai Mountains. Chinese Science Bulletin, 2007, 52(5): 568-571.
[许清海, 李月 丛, 周力平等. 长白山针阔混交林带花粉通量及垂直散布特征初步研究. 科学通报, 2007, 52(5): 568-571.]

[28] Tauber H. Investigations of the mode of pollen transfer in forested areas. Review of Palaeobotany and Palynology, 1967, 3: 277-286.

[29] Wu Zhengyi. Vegetation of China. Beijing: Science Press, 1980. 971-955.
[ 吴征益. 中国植被. 北京: 科学出版社, 1980. 917-955.]

[30] Faegri K, Iversen J. Textbook of Pollen Analysis. 3rd. Oxford: Blackwell, 1989. 1-295.

[31] Liu K B, Lam NS N. Paleovegetational reconstruction based on modern and fossil pollen data: An application of discriminant analysis. Annals of the Association of American Geographers, 1985, 75: 115-130.

[32] Lynch E A. The ability of pollen from small lakes and ponds to sense fine-scale vegetation patterns in the Central Rocky Mountains, USA. Review of Palaeobotany and Palynology, 1996, 94: 197-210.

[33] Kodela P G. Modern pollen rains from forest communities on the Robertson Plateau, New South Wales. Australian Journal of Botany, 1990, 38: 1-24.

[34] Horrocks M, Ogden J. Modern pollen spectra and vegetation of Mt. Hauhungatahi, central North Island, New Zealand. Journal of Biogeography, 1994, 21: 637-649.

[35] Reese C A, Liu K B. A modern pollen rain study from the central Andes region of South America. Journal of Biogeography. 2005, 32(4): 709-718.

[36] Brostr#m A, Gaillard M J, Ihse M et al. Pollen-landscape relationships in modern analogues of ancient cultural landscapes in southern Swede. Vegetation History and Archaeobotany, 1998, 7(4): 189-201.

[37] Sepp$ H, Birks H J B, Odland A et al. A modern pollen-climate calibration set from northern Europe: Developing and testing a tool for palaeoclimatological reconstructions. Journal of Biogeography, 2004, 31(2): 251-267.

[38] Finsinger W, Heiri O, Valsecchi V et al. Modern pollen assemblages as climate indicators in southern Europe. Global Ecology and Biogeography, 2007, 16(5): 567-582.

[39] Prentice I C. Multidimensional scaling as a research tool in Quaternary palynology. Review of Palaeobotany and Palynology, 1980, 31: 71-104.

[40] Zhang Wentong. Statistic Analysis Tutorial for SPASS 11 (Senior). Beijing: Hope Electronic Press, 2002. 64-89.
[ 张文 彤. SPASS11.0 统计分析教程(高级篇). 北京: 北京希望电子出版社, 2002. 64-89.]

[41] ter Braak C J F, Prentice I C. A theory of gradient analysis. Advances in Ecological Research, 1988, 18: 271-317.

[42] Lu Houyuan, Wu Naiqin, Yang Xiangdong et al. Phytoliths as quantitative indicators for the reconstruction of pastenvironmental conditions in China I. Quaternary Science Reviews, 2006, 25: 945-959.

[43] ter Braak C J F, Smilauer P. CANOCO Reference Manual and User's Guide to CANOCO for Windows: Software for Canonical Community Ordination Ithaca, NY. Microcomputer Power, 1998, 351.

[44] Li Yuecong, Xu Qinghai, Xiao Jule et al. Indication of some major pollen taxa in surface samples to their parent plants of forest in northern China. Quaternary Sciences, 2005, 25(5): 598-608.
[李月丛, 许清海, 肖举乐等. 中国北方森林 植被主要表土花粉类型对植被的指示性. 第四纪研究, 2005, 25(5): 598-608.]

[45] Jackson S T, Kearsley J B. Quantitative representation of local forest composition in forest-floor pollen assemblages. Journal of Ecology, 1998, 86: 474-490.

[46] Li Yuecong, Xu Qinghai, Yang Xiaolan et al. Pollen-vegetation relationship and pollen preservation on the Northeastern Qinghai-Tibetan Plateau. Grana, 2005, 44(3): 160-171.

[47] Dimbleby G W. Soil pollen analysis. Journal of Soil Science, 1961, 12: 1-11.

Outlines

/