东北三江平原全新世火演化及其与植被和气候的关系

doi:10.13249/j.cnki.sgs.2005.02.177

地理科学 ›› 2005, Vol. 25 ›› Issue (2): 177-182.doi: 10.13249/j.cnki.sgs.2005.02.177

东北三江平原全新世火演化及其与植被和气候的关系

李小强¹, 赵宏丽¹, 闫敏华², 王升忠³

1. 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 陕西, 西安, 710075;
2. 中国科学院东北地理与农业生态研究所, 吉林, 长春, 130012;
3. 东北师范大学城市与环境学院, 吉林, 长春, 130024

收稿日期:2004-04-16 修回日期:2004-10-18 出版日期:2005-03-20 发布日期:2005-03-20
基金资助:
国家自然科学基金(40172064,40342077);中国科学院钻探工程项目(KZCX2-SW-118);创新群体基金(NSFC40121303);重大基础研究前期研究专项(2003CCC01500)的支持。

Fire variations and Relationship among Fire and Vegetation and Climate during Holocene at Sanjiang Plain,Northeast China

LI Xiao-Qiang¹, ZHAO Hong-Li¹, YAN Min-Hua², WANG Sheng-Zhong³

1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, Shaanxi 710075;
2. Northeast Institute of Geography and Agricultural Ecology, Chinese Academy of Sciences, Changchun, Jilin 130012;
3. urban and Environmental School of Northeast Normal University, Changchun, Jilin 130010

Received:2004-04-16 Revised:2004-10-18 Online:2005-03-20 Published:2005-03-20

摘要/Abstract

摘要： 通过勤得利泥炭剖面碳屑、花粉记录,重建东北三江平原地区全新世火演化与植被变化的历史;研究火演化与植被、气候的关系;探讨人类火活动及其环境效应的信息。三江平原最近9700aB.P.以来,疏林草原植被时期(9200-8500aB.P.)和疏林植被时期(9700-9200aB.P.)对应了暖干气候阶段,碳屑浓度出现峰值,而湿润时期的碳屑浓度均很低。显示在暖干气候阶段,火灾发生的频次高、强度大;湿润或相对湿润阶段。火灾力度相对较小或频次较低。同时,自然植被状况和植物类型同样制约了天然火发生的频次和强度。20世纪50年代三江平原开发与垦荒对火演化和环境产生重要影响。

Abstract: The records of charcoal and pollen from peat section at Qindeli, NortheastChina help us to reconstruct the fire variation and the vegetation history in the Holocene at Sanjiang Plain and to study their relationship among fire, vegetation and climate.The reconstruction of fire history also discusses the human activity of fire and the impact on environment.Two peak values of charcoal concentration appeared in the two periods of spares forest and grassland (9 200-8 500 a B.P.) and spares forest (9 700-9 200 a B.P.) corresponding to two climate epochs of warm-dry and relatively warm-arid respectively.In the wet period the charcoal concentration shows the low values.The frequency and intensity of fire are high in the dry period and low in the wet period.However, the characteristic of vegetation and the types of plant also restrict the frequency and intensity of fire in the Holocene at Sanjiang Plain.In the mean time, the exploitation to Sanjiang Plain influenced the fire variation and environment greatly after the 1950s.

中图分类号:

P467

李小强, 赵宏丽, 闫敏华, 王升忠. 东北三江平原全新世火演化及其与植被和气候的关系[J]. 地理科学, 2005, 25(2): 177-182.

LI Xiao-Qiang, ZHAO Hong-Li, YAN Min-Hua, WANG Sheng-Zhong. Fire variations and Relationship among Fire and Vegetation and Climate during Holocene at Sanjiang Plain,Northeast China[J]. SCIENTIA GEOGRAPHICA SINICA, 2005, 25(2): 177-182.

参考文献

[1] Bird M.A million-year record of fire in sub-Saharan Africa[J].Nature,1998,394(695):767-769.
[2] 周以良.中国东北植被地理(第一版)[M].北京:科学出版社,1997.1～233.
[3] 赵魁义.中国沼泽志(第一版)[M].北京:科学出版社,1999.181～278.
[4] 孔昭宸,杜乃秋.三江平原末次冰期的植物化石和孢粉组合[J].地理科学,1984,4(1):76～80.
[5] 夏玉梅.三江平原12 000年以来植物群发展和气候变化的初步研究[J].地理科学,1988,8(3):238～249.
[6] 夏玉梅,汪佩芳,王曼华.东北全新世温暖期气候变化的初步研究[A].见:张兰生(主编).中国生存环境历史演变规律研究(一)[C].北京:海洋出版社,1993.204～210.
[7] 叶永英.东北三江平原几个钻孔剖面的孢粉组合分析及其意义[J].地质科学,1983,(3):259～268.
[8] Moore P D,Webb J A.An Illustrated Guide to Pollen Analysis.London[M].Hodder and Stoughton,1978.5-50.
[9] 李小强,杜乃秋.第四纪花粉的无酸碱分析法[J].植物学报,1999,41(7):782～784.
[10] Tolonen K.Charred particle analysis.In:Berglund B.(Ed.).Handbook of Paleoecology and Paleohydrology[M].Wiley Chichester,1986.485-496.
[11] Peck R M.A comparison of four absolute pollen preparation techniques[J].New phytology,1974,73:67-87.
[12] Clark J S.Particle motion and the theory of charcoal analysis,source area,transport,deposition,and sampling[J].Quaternary Research,1988,30(1):67-80.
[13] 马学慧,夏玉梅,王瑞山.我国泥炭形成时期的探讨[J].地理研究,1987,6(1):31～41.
[14] 李取生,李崇玲.东北泥炭与中全新世降温事件的初步研究[A].张兰生(主编).中国生存环境历史演变规律研究(一)[C].北京:海洋出版社,1993.204～210.
[15] Morrison K D.Monitoring regional fire history through size-specific analysis of microscopic charcoal; the last 600 years in South India[J].Journal of Archaeological Science,1994,21(5):675-685.
[16] Whitlock C,Millspaugh S H.Testing the assumptions of firehistory studies; an examination of modern charcoal accumulation in Yellowstone National Park,USA[J].The Holocene,1996,6(1):7-15.
[17] Swain A M.A history of fire and vegetation in northeastern Minnesota as recorded in lake and sediments[J].Quaternary research,1973,(3):383-396.
[18] Earle C J.Charcoal in northcentral Alaskan lake sediments; relationships to fire and late-Quaternary vegetation history[J].Review of Palaeobotany and Palynology,1996,92(2):83-95.
[19] Carcaillet C,Thinon M.Pedoanthracological contribution to the study of the evolution of the upper treeline in the Maurienne Valley(North French Alps):methodology and preliminary data[J].Review of Palaeobotany and Palynology,1996,91(1):399-416.
[20] Filion L.A relationship between dunes,fire and climate recorded in the Holocene deposits of Quebec[J].Nature,1984,309(5968):543-546.
[21] 孙湘君,李逊,罗运利,等.南海北部最近37 ka以来天然火与气[J].中国科学(D辑),2000,30(2):163～168.
[22] Dodson J R,Intoh M,Prehistory and paheoecology of Yap:federated states of Micronesia[J].Quaternary International,1999,59:17-26.
[23] Clark J S.Effect of climate change on fire regimes in northwestem Minnesota[J].Nature,1988,334(6179):233-235.
[24] Behling H.Late Quaternary vegetation,climate and fire history of the Araucaria forest and Campos region from Serra Campos Gerais,Parana State(South Brazil)[J].Review of Palaeobotany and Palynology,1997,97(2):109-121.
[25] Burchard I.Anthropogenic impact on the climate since man began to hunt[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1998,139(1):1-14.
[26] Chandler C C.Problems and priorities for forest fire recarch[J].Journal of Forest 1973,71:625-628.
[27] 周道玮.草地火生态学研究进展(第一版)[M].长春:吉林科学技术出版社,1995.1～393.

东北三江平原全新世火演化及其与植被和气候的关系

Fire variations and Relationship among Fire and Vegetation and Climate during Holocene at Sanjiang Plain,Northeast China

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