太白山北坡花粉通量与表土花粉研究

doi:10.11821/yj2008030007

地理研究 ›› 2008, Vol. 27 ›› Issue (3): 536-546.doi: 10.11821/yj2008030007

太白山北坡花粉通量与表土花粉研究

李月丛¹, 许清海¹, 曹现勇¹, 阳小兰², 李宜垠³, 周力平³

1. 河北省师范大学资源与环境学院, 石家庄 050016;
2. 河北省地理科学研究所,石家庄 050011;
3. 北京大学环境学院,北京 100871

收稿日期:2007-07-05 修回日期:2007-12-15 出版日期:2008-05-25 发布日期:2008-05-25
作者简介:李月丛,女,河北晋州人,研究员,博士。主要从事孢粉学与全球变化研究。 Email: lyczh@sohu.com, Tel: 0311-86269204
基金资助:
科学技术部基础研究重大项目前期研究专项项目(2003CCA01800),国家自然科学基金项目(40571166,40672107)、河北省博士基金项目(06547006-3)和教育部博士点专项科研基金项目(20050094004)联合资助。

Pollen influx and surface pollen assemblage on the northern slope of Taibai Mountain

LI Yue-cong¹, XU Qing-hai¹, CAO Xian-yong¹, YANG Xiao-lan², LI Yi-yin³, ZHOU Li-ping³

1. College of Resources and Environmental Sciences, Hebei Normal University, Shijiazhuang 050016,China;
2. Hebei Geography Institute, Hebei Academy of Sciences, Shijiazhuang 050011,China;
3. College of Environmental Sciences, Peking University, Beijing 100871,China

Received:2007-07-05 Revised:2007-12-15 Online:2008-05-25 Published:2008-05-25
Supported by:
科学技术部基础研究重大项目前期研究专项项目(2003CCA01800),国家自然科学基金项目(40571166,40672107)、河北省博士基金项目(06547006-3)和教育部博士点专项科研基金项目(20050094004)联合资助。

摘要/Abstract

摘要：

太白山北坡各森林植被带乔木花粉百分比多高于45%,与植被组成类似。高山草甸带捕捉器样品乔木花粉百分比低于15%,与植被组成一致,但表土花粉组合中乔木花粉百分比高于50%,外来花粉数量较多,进行高山带古环境研究应予注意。太白红杉林花粉通量最低,高山灌丛草甸最高。落叶栎林带表土花粉浓度最低,红桦林带最高。表土中松、冷杉属花粉百分比远高于花粉捕捉器,表明其在表土中有较好的保存能力。落叶松属和杜鹃花科花粉在表土及捕捉器中百分比均较低,表明对植被指示性良好。栎属与桦属花粉通量类似,但桦属花粉浓度大于栎属,表明栎属较桦属易于保存。

关键词: 太白山, 花粉捕捉器, 花粉通量, 花粉组合, 表土花粉, 花粉浓度

Abstract:

The pollen influx, pollen concentrations and pollen assemblages are studied based on pollen tauber traps and surface pollen samples coming from 6 different vertical vegetation zones on the northern slope of the Taibai Mountain. The results indicate that pollen influxes are more than 10000 grains /cm²/y, with the maximum in Larix Chinese belt and the minimum in shrub and meadows belt. Pollen concentrations are more than 25000 grains/g with the maximum in Betula albo-sinensis belt and the minimum in deciduous broad-leaved Quercus belt. The arboreal pollen percentages are mostly more than 45% in 5 forest belts both for pollen traps and surface samples, which are consistent with the vegetation composition. But the arboreal pollen percentages are less than 20% in pollen trap samples and more than 50% in surface samples coming from alpine shrub and meadows, indicating that more ex-local arboreal pollen appeared in surface pollen assemblages. The Abies and Pinus pollen percentages are much higher in surface samples than in pollen trap, suggesting that they can be easily preserved in moss or surface soil. Larix and Ericaceae have rather lower percentages both in pollen trap or in surface samples, compared with vegetation coverages, showing that they have not only lower pollen productions,short transported distance, but poor pollen preservation ability,and can indicate vegetation well. The study on pollen influx of Betula and Quercus shows that the pollen productions are similar, but Quercus pollen concentrations are much lower than Betula in respective forests, showing that Quercus pollen grains can not be preserved as well as Betula in moss or surface soil. The results are obtained from one year's experiments, so further research work should be done.

Key words: Taibai Mountain, pollen influx, pollen assemblages, pollen traps, surface samples, pollen concentrations

李月丛, 许清海, 曹现勇, 阳小兰, 李宜垠, 周力平. 太白山北坡花粉通量与表土花粉研究[J]. 地理研究, 2008, 27(3): 536-546.

LI Yue-cong, XU Qing-hai, CAO Xian-yong, YANG Xiao-lan, LI Yi-yin, ZHOU Li-ping. Pollen influx and surface pollen assemblage on the northern slope of Taibai Mountain[J]. GEOGRAPHICAL RESEARCH, 2008, 27(3): 536-546.

参考文献

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

[2] Peck B R M. Efficiency tests on the Tauber trap used as a pollen sampler in turbulent water flow. New Phytologist, 1972, 71:187~198.

[3] Davis M B, Brubaker L, Webb Ш. Calibration of absolute pollen influx. In: Birks H J B, West R G. Quaternary Plant Ecology.Oxford:Blackwell Science,1973.9~25.

[4] Davis M B, Spear R W, Shane L C K. Holocene climate of New England. Quaternary Research, 1980, 14:240~250.

[5] Craig A J. Pollen percentage and lnflux analyses in South-East Ireland: A contribution to the ecological history of the Late-Glacial Period.The Journal of Ecology, 1978, 66(1), 297~324

[6] Hicks S, Hyvarinen, V P. Sampling modern pollen deposition by means of 'tauber traps’: Some considerations. Pollen et Spores, 1986, 28:219~242.

[7] Cundill P R.A new design of pollen trap for modern pollen studies.Journal of Biogeography,1986,13(2):83~98.

[8] Faegri K, Iversen J. Textbook of Pollen Analysis. Oxford: Blackwell, 1989 (3rd. ). 1~295.

[9] Hall S A. Pollen deposition and vegetation in the southern Rocky Mountains and the southwest Plains, USA. Grana, 1990, 29:47~61.

[10] Bush M B. A simple yet efficient pollen trap for use in vegetation studies.Journal of Vegetation Science, 1992, 3(2):275~276.

[11] Hicks S, Ammann B, Latalowa M, et al. European Pollen Monitoring Programme: Project description and guidelines. University of Oulu, 1996, 28.

[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] Van Leeuwen J F N, Ammann B. Seven years of annual pollen influx at the forest limit in the Swiss Alps studied by pollen traps: Relations to vegetation and climate. Review of Palaeobotany and Palynology, 2001, 117: 31~52.

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

[16] Rsnen S, Hick 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: 103~116.

[17] 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.

[18] 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.

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

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

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

[22] 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.

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

[24] Rsnen S, Suutari H, Nielsen A B. A step further towards quantitative reconstruction of past vegetation in Fennoscandian boreal forests: Pollen productivity estimates for six dominant taxa.Review of Palaeobotany and Palynology, 2007, 146:208~220.

[25] 吕厚远, 王淑云, 沈才明,等.青藏高原现代表土中冷杉和云杉花粉的空间分布.第四纪研究,2004,24(1):39~49.

[26] 刘鸿雁, 王红亚, 崔海亭. 太白山高山带2000多年以来气候变化与林线的响应.第四纪研究, 2003, 23(3): 299~308.

[27] 许清海, 李月丛, 阳小兰, 等. 北方草原区主要群落类型表土花粉分析, 地理研究, 2005, 24(3): 585~597.

[28] 李宜垠, 张新时, 周广胜, 等. 中国北方几种常见表土花粉类型与植被的数量关系. 科学通报, 2000, 45(7): 761~764.

[29] 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.

[30] 赵景波, 岳应利, 岳明. 秦岭及黄土区现代栎林的孢粉组合研究. 西安工程学院学报, 1998, 20(1):46~50.

[31] 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.

[32] 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.

[33] 张俊牌, 童敏, 王书兵,等. 太白山芳香寺剖面孢粉记录的古气候重建. 地质力学学报, 2001,7(4):315~320.

[34] 崔之久, 唐元新, 李建江,等.太白山佛爷池剖面的全新世环境变化信息.地质力学学报,2003,9(4):330~336.

[35] 赵先贵, 肖玲. 秦岭地区15 ka BP以来的植被与环境. 西北植物学报, 2003, 23(4): 523~530.

[36] 童国榜, 张俊牌, 范淑贤,等.秦岭太白山顶近千年来的环境变化.海洋地质与第四纪地质,1996,16(4):95~104.

[37] Liu Hongyan, Cui Haiting, Tang Zhiyao, et al . Larch timberline and its development in temperate China. Mountain Research and Development , 2002 , 22(4) : 359~367.

[38] 傅志军, 郭俊理. 秦岭太白山植被的群落特征. 宝鸡师范学院学报(自然科学版), 1992, (1): 70~75.

[39] 方正. 秦岭太白山南北坡的植被垂直带谱. 植物生态学与地植物学丛刊, 1963, 1 (1/ 2): 162~163.

[40] 雷梅, 陈同斌, 冯立孝,等.太白山北坡成土因素及不同土壤垂直带谱的比较.地理研究,2001,20(5):583~592.

[41] 王开发, 王宪曾. 孢粉学概论. 北京: 北京大学出版社, 1983. 13~14.

[42] 李文漪.中国第四纪植被与环境. 北京: 科学出版社, 1998. 43~48.

[43] Kwaitowski A, Mianowska L. Badanie skladu chemicznego pylku II. Badania blon pylkowich. Acta Societatis Botanicorum Polonae, 1957, 26: 501~514.

太白山北坡花粉通量与表土花粉研究

Pollen influx and surface pollen assemblage on the northern slope of Taibai Mountain

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