第四纪研究
第四紀研究
제사기연구
2009年
4期
817-824
,共8页
李鸿凯%卜兆君%王升忠%安芷生%赵红艳%马云艳%陈旭
李鴻凱%蔔兆君%王升忠%安芷生%趙紅豔%馬雲豔%陳旭
리홍개%복조군%왕승충%안지생%조홍염%마운염%진욱
长白山%有壳变形虫%冗余分析%水位埋深
長白山%有殼變形蟲%冗餘分析%水位埋深
장백산%유각변형충%용여분석%수위매심
Changbai Mountains%testate amoebae%redundancy analysis%depth to water table
有壳变形虫(testate amoebae)是一种新的具有潜力的环境变化生物指标.对采集自长白山区哈泥(42°12'500N,126°31'05"E)、金川(42°20'47"N,126°21'35"E)、赤池(42°03'16"N,128°03'22"E)和圆池(42°01'55"N,128°25'58"E)等4个泥炭地不同生境的75个有壳变形虫样品,采用冗余分析方法(RDA)研究有壳变形虫种类组合变化与7个环境变量的关系,所有采样点均以泥炭藓(Sphagnum)为优势植被.结果表明水位埋深(depth to water table),pH值和泥炭湿度是影响长白山区泥炭地有壳变形虫种类变化的主要环境因子,显著性检验达到p<0.001的水平.这一结果与国外其他地区的研究结果相一致,这3个环境因子可以作为目标变量进行有壳变形虫-环境因子转换函数的构建.
有殼變形蟲(testate amoebae)是一種新的具有潛力的環境變化生物指標.對採集自長白山區哈泥(42°12'500N,126°31'05"E)、金川(42°20'47"N,126°21'35"E)、赤池(42°03'16"N,128°03'22"E)和圓池(42°01'55"N,128°25'58"E)等4箇泥炭地不同生境的75箇有殼變形蟲樣品,採用冗餘分析方法(RDA)研究有殼變形蟲種類組閤變化與7箇環境變量的關繫,所有採樣點均以泥炭蘚(Sphagnum)為優勢植被.結果錶明水位埋深(depth to water table),pH值和泥炭濕度是影響長白山區泥炭地有殼變形蟲種類變化的主要環境因子,顯著性檢驗達到p<0.001的水平.這一結果與國外其他地區的研究結果相一緻,這3箇環境因子可以作為目標變量進行有殼變形蟲-環境因子轉換函數的構建.
유각변형충(testate amoebae)시일충신적구유잠력적배경변화생물지표.대채집자장백산구합니(42°12'500N,126°31'05"E)、금천(42°20'47"N,126°21'35"E)、적지(42°03'16"N,128°03'22"E)화원지(42°01'55"N,128°25'58"E)등4개니탄지불동생경적75개유각변형충양품,채용용여분석방법(RDA)연구유각변형충충류조합변화여7개배경변량적관계,소유채양점균이니탄선(Sphagnum)위우세식피.결과표명수위매심(depth to water table),pH치화니탄습도시영향장백산구니탄지유각변형충충류변화적주요배경인자,현저성검험체도p<0.001적수평.저일결과여국외기타지구적연구결과상일치,저3개배경인자가이작위목표변량진행유각변형충-배경인자전환함수적구건.
Testate amoebae are unicellular organisms living in soils,wetlands and aquatic habitats which produce decay-resistant shells(tests).They are especially diverse and abundant in Sphagnum peatlands.In addition,testate amoebae show clear responses to the main environmental gradients in peatlands,such as depth to water table and pH.Many studies on modern ecology of testate amoeba have now been conducted in different regions of the world for their applications in paleoecology.However,most of them were conducted in Europe and North America,and none were in China,despite the presence of numerous peatlands here.In this study,75 samples were collected along hydrological gradients from 4 peatlands namely Hani (42°12'50"N,126°31 '05"E),Jinchuan(42°20'47"N,126°21 '35"E),Chichi(42°03'16"N,128°03'22"E)and Yuanehi(42°01 '55"N,128°25 '58"E),in the Changbai Mountains,North East China.All sampling spots were dominated by Sphagnum and covered different habitats including the hollow,the top,middle and low part of hummock.Depth to water table(DWT),moisture of peat,pH and conductivity were measured in situ.Latitude,longitude and altitude were recorded with GPS.33 testate amoebae taxa and 12984 tests were recorded.Detrended correspondence analysis(DCA)shows that 4 peatlands have similar testate amoebae assemblages.Since th e length of gradient is short than 3,a linear ordination model,redundancy analysis(RDA),was used tzo explore the relationship between testate amoebae assemblages and 7 environmental variables including latitude,longitude,altitude,pH,conductivity,DWT,and moisture of peat.The results show that the 7 environmental variables explain 31.8% of variation in species data.DWT,pH and moisture of peat have greater marginal effects,which are 10%,9% and 8%,respectively.All of these three variables are extremely significantly correlated with axis 1 of ordination.So they are principal factors which determine the assemblage of testate amoebae in peatlands in the Changbai Mountains.Monte Carol significance tests(999 permutation)of DWT,pH and soil moisture are all p < 0.001,which proves that they can be target variables in developing transfer functions for quantitative paleo-environmental reconstruction.The conclusion of this paper is consistent with ecological studies of testate amoeba conducted in other regions in the world.This convinces us that testate amoebae can be an extra method in paleoecological study on peat sediments in the Changbai Mountains.Coupling with other proxies such as pollen,plant macrofossil,humification degree,and isotope composition,we can recover a more integrated picture for the past.