论文

现代尘暴和非尘暴天气大气花粉特征及其环境意义——以北京地区为例

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  • 河北师范大学资源与环境科学学院,石家庄050016
王赞红(1967-),女,吉林省长春市人,副教授,博士。研究方向为大气颗粒物与环境变迁。

收稿日期: 2005-07-16

  修回日期: 2005-12-17

  网络出版日期: 2006-04-15

基金资助

国家自然科学基金资助项目(40571166);河北省自然科学基金资助项目(D2005000176)

Air pollen assemblage characteristics derived from duststorms and non-duststorms and its significance

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  • College of Resources and Environment Sciences,Hebei Normal University,Shijiazhuang 050016,China

Received date: 2005-07-16

  Revised date: 2005-12-17

  Online published: 2006-04-15

摘要

通过20012003年取得的尘暴和非尘暴天气大气花粉的对比研究,发现两类天气条件下大气花粉组合虽都以北京地区木本植物花粉为主,但尘暴天气样品中草本植物花粉数量有较多增加。根据尘暴活动和北京地区物候分析,推测这些草本植物花粉来自尘暴源区和路径区的表土沉积。基于上述认识,进一步对风成黄土古土壤层的花粉进行探讨,认为古土壤中草本植物花粉和木本植物花粉是同期沉积的,其木本植物花粉数量比较少可能是尘暴降尘导致草本植物花粉数增多所致。通过现代尘暴、非尘暴天气大气花粉特征的研究,对正确认识过去风成黄土和古土壤层中以草本植物花粉为主的孢粉组合特征提出了新的思路。

本文引用格式

王赞红, 许清海 . 现代尘暴和非尘暴天气大气花粉特征及其环境意义——以北京地区为例[J]. 地理研究, 2006 , 25(2) : 262 -267 . DOI: 10.11821/yj2006020009

Abstract

Pollen assemblage characteristics which have been used to reconstruct paleoenvironment are taken as an important agent based on modern climate conditions for plants growth.It is particularly so in the loess research.Nevertheless,there are still some problems in deducing paleoclimate by the pollen assemblage discovered in paleosols,which were supposed to have developed under relatively warm and wet climate conditions,thus containing more pollens of trees than of herbs,but it is reverse actually.The best way to probe into such a question period is to observe the process of pedogenesis which was presumed to happen in the interglacial period with the similar climate conditions of today.What happened on the soil surface today might be the same as that in the interglacial period.Therefore this research takes air pollen samples in Beijing under different weather conditions of duststorms and non-duststorms in spring to discuss the pollen assemblage characteristics.The results show that both samples derived from duststorms and non-duststorms contain pollens of trees and herbs,in the majority of trees,representing modern sedimentary environment.Samples of duststorms contain more herbs pollens than samples of non-duststorms,which is argued by the authors to be transported from the source and pathway of storms.Further on,based on the analyses of the amount of dustfall annually,this paper concludes that more pollens of herbs have been transported and deposited under duststorm weather conditions than pollens of trees under non-duststorm weather conditions,which possibly is partial reason for the presence of pollens assemblage in paleosols.Though limit to the samples number this paper's view needs more proof,a new thoughtway on pollen research of eolian sediments still has been put forward.

参考文献


[1] Webb R S,A nderson K H,W ebb!T Pol len res ponse s urface est imat es of lat e Q uat ernary ch anges in t he moist u re bal an ce of t he nort heast ern U ni ted S tat es Q uat ern ary R esear ch,1993,40:213~227

[2] 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):394~402

[3] Prent ice I C,Cramer W,H arrison S P A global biome model based on plant physi ol ogy and d om inan ce,s oil propert ies and climat e Journ al of Biogeography,1992,19(2):117~134

[4] G uo Z T,Ruddiman W F,Hao Z,et al O nset of A sian desertif icat ion by 22 M yr ago in ferred from loes s deposit sin C hina N at ure,2002,416:159~163

[5] S un X J,Song C Q,Wang F Y,et al V eget at ion hist ory of t h e Loess Plat eau of Ch ina du ring t he l as t 100 000years based on pollen dat a Q uat ernary Int ernati on al,1997,37:25~36

[6] 吴福莉,方小敏,等黄土高原中部. 5M a以来古生态环境演化的孢粉记录科学通报,2004,49(1):99~105

[7] K u kla G L oess st rat igraphy in Ch ina Q uat ernary Science R eview,1987,6:191~219

[8] 吕厚远,刘东生,郭正堂黄土高原地质、历史时期古植被研究状况科学通报,2003,48(1):2~7

[9] 唐克丽,贺秀斌黄土高原全新世黄土-古土壤演替及气候演变的再研讨第四纪研究,2004,24(2):129~140

[10] 庞奖励,黄春长,陈宝群黄土高原南部全新世土壤微结构形成机理探讨地理研究,2002,21(4):487~494

[11] 郭正堂,刘东生,安芷生渭南黄土沉积中十五万年的古土壤及其形成时的古环境第四纪研究,1994,(3):256~269

[12] 陈焕伟从古土壤看北京环境变迁土壤学报,2000,37(3):306~315

[13] 刘东生,郭正堂,吴乃琴,等史前黄土高原的自然植被景观-森林还是草原?地球学报,1994,(3-4):226~234

[14] 陈云,李铮华,赵景波,等全新世高温期气候不稳定性记录海洋地质与第四纪地质,1999,19(3):97~103

[15] 唐克丽,贺秀彬第四纪黄土剖面多元古土壤形成发育信息的揭示土壤学报,2002,39(5):609~617

[16] 谢树成,王志远,王红梅,等末次间冰期以来黄土高原的草原植被景观:来自分子化石的证据中国科学(D)辑,2002,(1):28~35

[17] 曲绍厚,李玉英,周明煜,等北京地区一次尘暴过程的来源环境科学学报,1984,4(1):80~85

[18] 宋之琛北京西郊空气中的孢粉组合中国第四纪研究,1959,2:69~74

[19] 张金谈北京西郊空气中的花粉植物学报,1964,12(3):282~285

[20] 吕新苗,刘惠清,王文杰,等北京周边地区沙尘暴时空分布特征及其环境背景地理研究,2004,23(1):38~44

[21] 何海娟,张德山,乔秉善北京城区空气中花粉含量与气象要素的关系初探中华微生物学和免疫学杂志,2004,21(增刊):31~33

[22] 张姝丽,张德山,何海娟北京城区花粉数量天气条件分析气象科技,2003,31(16):406~408

[23] M ullins J,Em berl in J S ampl ing pol len s Journal of A eros ol S cien ce,1997,28(3):365~370

[24] 徐雨晴,陆佩玲,于强近50年北京树木物候对气候变化的响应地理研究,2005,24(3):412~420

[25] 张志刚,陈万隆影响北京沙尘源地的气候特征与北京沙尘天气分析环境科学研究,2003,16(2):6~9

[26] 赵琳娜,孙建华,赵思雄2002年3月20日沙尘暴天气的影响系统、起沙和输送的数值模拟干旱区资源与环境,2004,18(1):72~80

[27] 康凤琴,李耀辉,吕世华2001年4月8日强沙尘暴天气的数值模拟研究中国沙漠,2003,23(6):681~685

[28] 郭正堂,刘东生,安芷生间冰期降尘与黄土中的加积型古土壤见:龚子同主编,土壤环境变化北京:中国科学技术出版社,1992:25~30

[29] 王赞红斋堂马兰黄土堆积与现代大气降尘对比研究北京大学博士研究生毕业论文,2003 52

[30] 刘东生,孙继敏,吴文祥中国黄土研究的历史、现状和未来一次事实与事故相结合的讨论第四纪研究,2001,21(3):185~207

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