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气候变化是影响全球泥炭沼泽分布和演化的最重要的因子之一,而泥炭地由于自身的特点成为过去气候变化的良好地质档案。在介绍泥炭沉积过程及不同类型的泥炭沼泽的发育特点基础上,从过去气候变化的常用泥炭记录和泥炭地碳记录等方面总结了国际上针对泥炭地反演气候变化研究的若干重要进展,重点剖析了泥炭腐殖化度、植物残体、有壳变形虫、生物标志化合物、同位素和孢粉等泥炭地过去气候变化重建的代用指标的适用范围和优缺点,同时也分析了泥炭地碳累积和碳循环等热点研究问题。最后从泥炭地作为过去气候变化的记录档案、泥炭地对现在气候变化的响应与反馈及在泥炭地进行现场气候变化监测与实验等方面对泥炭地与气候变化研究进行了展望。
Abstract:Climate is the most important determinant of the distribution and character of peatlands,and its variation determines the location,typology and biodiversity of peatlands through the world;peatlands preserve,in the constantly accumulating peat,a unique record of their own development as well as of past climate changes,and are good geological archives of variation in climate and regional environment.Based on the discussion of peat deposition process and the development characteristics of different types of mires,this paper systematically reviewed international paleoclimatic studies about peat sediments from the two perspectives of the common climatic proxies and the carbon records in peatlands.The scopes of application as well as merits and demerits of six common climatic proxies including peat humification,peat macrofossils,testate amoebae,biomarker compounds,stable isotopes and pollen are analysed in detail,and the recent hot issues on carbon accumulation and carbon cycles in peatlands are also involved.Finally,the important research fields and contents in peatlands and climate changes are summarized based on four aspects:past climate variability reconstructed from peatlands,impacts of recent global climate variations on peatlands,potential feedbacks mechanisms of peatlands to climate change,and current direct observations and measurements on climatic and ecological conditions in peatlands.
鲍锟山,赵红梅,于晓菲,吕宪国,王国平.2011.大气环境变化的泥炭地质档案.地质论评,57(2):234-242
卜兆军,王升忠,谢宗航.2005.泥炭沼泽学若干基本概念的再认识.东北师范大学学报(自然科学版),37(2):105-110
柴岫.1990.泥炭地学.北京:地质出版社.1-312
洪冰,刘丛强,林庆华,Yasuyuki Shibata,冷雪天,王羽,朱泳煊,洪业汤.2009.哈尼泥炭δ18O记录的过去14000年温度演变.中国科学(D辑:地球科学),39(5):626-637
刘兴土,邓伟,刘景双.2006.沼泽学概论.长春:吉林科学技术出版社.1-88
林庆华,冷雪天,洪冰.2004a.大兴安岭近1000年来气候变化的泥炭记录.矿物岩石地球化学通报,23(1):15-18
林庆华,冷雪天,洪冰.2004b.小兴安岭过去5000年的泥炭δ13C记录.地球与环境,32(1):51-54
彭格林,刘光华,伍大茂,张则有.1999.泥炭沼泽化类型、控制因素及聚炭水文模式.地学前缘,6(增刊):125-132
王绍武,葛全胜,王芳,闻新宇,黄建斌.2010.全球气候变暖争议中的核心问题.地球科学进展,25(6):656-665
王燕,赵志中,乔彦松,王书兵,李朝柱,宋利峰.2006.川北若尔盖高原红原泥炭剖面孢粉记录的晚冰期以来古气候古环境的演变.地质通报,25(7):827-832
王琒瑜,宋长青,程全国,孙湘君.1998.利用花粉—气候响应恢复察素齐泥炭剖面全新世古气候的尝试.植物学报,40(11):1067-1074
王华,洪业汤,朱咏煊,林庆华,冷雪天,毛绪美.2003.红原泥炭腐殖化度记录的全新世气候变化.地质地球化学,31(2):51-56
鲜锋,周卫健,于学峰,卢雪峰,Jull A J,Franzen L G.2006.高原泥炭记录揭示的全新世季风快速变化.海洋地质与第四纪地质,26(1):41-45
夏玉梅,汪佩芳.2000.密山杨木3000多年来气候变化的泥炭记录.地理研究,19(11):53-59
谢树成,赖旭龙,黄咸雨,马相如,杨淑娟.2007.分子地层学的原理、方法及应用实例.地层学杂志,31(3):209-221
于学峰,周卫健.2004.全新世泥炭古气候记录研究进展.海洋地质与第四纪地质,24(4):121-126
朱芸,陈晔,赵志军,萧家仪,张茂恒,舒强,赵红艳.2009.神农架大九湖泥炭藓泥炭α-纤维素δ13C记录的1000-4000aBP间环境变化.科学通报,54(20):3108-3116
张欣利,贾继红,周静.2008.雨养泥炭沼泽古水文定量重建的代用指标——有壳肉足虫化石记录的应用与进展.海洋地质与第四纪地质,28(2):121-128
赵红艳,王升忠,白燕,冷雪天.2002.近10年来我国泥炭地学的研究进展,地球科学进展,17(6):848-854
周卫健,卢雪峰,武振坤,邓林,Jull A J,Donahue D,Beck W.2001.若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年.科学通报,46(12):1040-1044
Aaby B.1976.Cyclic climatic variations in climate over the past5500yr reflected in raised bogs.Nature,263:281-284
Anderson D E,1998.A reconstruction of Holocene climatic changes from peat bogs in north-west Scotland.Boreas,27:208-224
Aravena R,Warner B G,Charman D J,Belyea L R,Mathur S P&Dinel H.1993.Carbon isotopic composition of deep carbon ga-ses in an ombrogenous mire,northwestern Ontario,Canada.Radiocarbon,35:271-276
Asada T&Warner BG.2005.Surface peat mass and carbon balancein a hypermaritime peatland.Soil Science Society of AmericaJournal,69:549-562
Avsejs L A,Nott C J,Xie S,Maddy D,Chambers F M&EvershedR P.2002.5-n-Alkylresorcinols as biomarkers of sedges in anombrotrophic peat section.Organic Geochemistry,33:861-867
Baas M,Pancost R,van Geel B&Sinninghe DamstéJ S.2000.Acomparative study of lipids in Sphagnum species.Organic Geo-chemistry,31:535-541
Bao K S,Xia W L,Lu X G&Wang G P.2010a.Response to comment by Craig Loehle(MRD Vol30No3)on Bao et al(2010):Recent carbon accumulation in Changbai Mountain peatlands,Northeast China.Mountain Research and Development,30(4):411-412
Bao K S,Yu X F,Jia L&Wang G P.2010b.Recent carbon accu-mulation in Changbai Mountain peatlands,Northeast China.Mountain Research and Development,30(1):33-41
Barry G W&Daniel J C.1994.Holocene changes on a peatland innorth western Ontario interpreted from testate amoebae(Proto-zoa)analysis.Boreas,23:270-279
Barber K E.1993.Peatlands as scientific archives of past biodiversity.Biodiversity and Conservation,2:474-489
Barber K E,Chambers F M,Maddy D,Stoneman R&Brew J S.1994.A sensitive high-resolution record of late Holocene cli-matic change from a raised bog in northern England.The Hol-ocene,4:198-205
Barber K E,Battarbee R W,Brooks S J,Eglinton G,Haworth EY,Oldfield F,Stevenson A C,Thompson R,Appleby P G,Austin W E Net al.1999.Proxy records of climate change inthe UK over the last two millennia:documented change andsedimentary records from lakes and bogs.Journal of the Geo-logical Society,London,156:369-380
Barber K E,Chambers F M&Maddy D.2004.Late Holocene climatic history of northern Germany and Denmark:Peat macro-fossil investigations at Dosenmoor,Schleswig-Holstein,and Sv-anemose,Jutland.Boreas,33:132-144
Beilman D W,MacDonald G M,Smith L C&Reimer P J.2009.Carbon accumulation in peatlands of West Siberia over the last2000years.Global Biogeochemical Cycles,23(GB1012):1-12
Belyea L R&Baird A J.2006.Beyond“The limits to peat boggrowth”:cross-scale feedback in peatland development.Ecolog-ical Monographs,76(3):299-322
Blackford J J&Chambers F M.1991.Blanket peat humification:evidence for a Dark Age(1400BP)climatic deterioration in theBritish Isles.The Holocene,1:63-67
Blackford J.1995.Proxy climate record for the last1000years from Irish blanket peat and possible link to solar variability.Earthand Planetary Science Letters,133:145-150
Blackford J.2000.Palaeoclimatic records from peat bogs.Trends in Ecology&Evolution,15(5):193-198
Blundell A,Charman D J&Barber K E.2007.Multiproxy late Holocene peat records from Ireland:Towards a regional palaeo-climate curve.Journal of Quaternary Science,23:59-71
Borgmark A.2005.Holocene climate variability and periodicities insouth-central Sweden,as interpreted from peat humification a-nalysis.The Holocene,15:387-395
Booth R K&Jackson S T.2003.A high-resolution record of late-Holocene moisture variability from a Michigan raised bog,USA.The Holocene,13(6):863-876
Booth R K.2008.Testate amoebae as proxies for mean annual waiter-table depth in Sphagnum-dominated peatlands of North A-merica.Journal of Quaternary Science,23:43-57
Caseldine C,Baker A,Charman D&Hendon D.2000.A compara-tive study of optical properties of NaOH peat extracts:Implica-tions for humification studies.The Holocene,10:649-657
Chambers F M,Barber K E,Maddy D&Brew J.1997.A5500-year proxy-climate and vegetation record from blanket mire atTalla Moss,Borders,Scotland.The Holocene,7:391-399
Chambers F M,Mauquoy D&Todd P A.1999.Recent rise todominance of Molinia caerulea in environmentally sensitive are-as:New perspectives from palaeoecological data.Journal of Ap-plied Ecology,36:719-733
Chambers F M&Charman D J.2004.Holocene environmental change:contributions from the peatland archive.The Hol-ocene,14(1):1-6
Chambers F M,Mauquoy D,Brain S A,Blaauw M&Daniell J RG.2007a.Globally synchronous climate change2800yearsago:Proxy data from peat in South America.Earth and Plane-tary Science Letter,253:439-444
Chambers F M,Mauquoy D,Gent A,Pearson F,Daniell J R G&Jones P S.2007b.Palaeoecology of degraded blanket mire inSouth Wales:Data to inform conservation management.Biolog-ical Conservation,137:197-209
Charman D J.1997.Modelling hydrological relationships of test ateamoebae(Protozoa:Rhizopoda)on New Zealand peatlands.Journal of the Royal Society New Zealand,27:465-483
Charman D J.2001.Biostratigraphic and palaeoenvironmental applications of testate amoebae.Quaternary Science Reviews,20:1753-1764
Charman D J,Aravena R,Bryant C L&Harkness D D.1999b.Carbon isotopes in peat,DOC,CO2,and CH4in a Holocenepeatland on Dartmoor,southwest England.Geology,27:539-542
Charman D J,Barber K E,Blaauw M,Langdon P G,Mauquoy D,Daley T,Hughes P D M&Karofeld E.2009.Climate driversfor peatland palaeoclimate records.Quaternary Science Re-views,28:1811-1819
Charman D J,Blundell A&Accrotelm members.2007.A new European testate amoebae transfer function for palaeohydrologicalreconstruction on ombrotrophic peatlands.Journal of Quaterna-ry Science,22:209-221
Charman D J&Garnett M H.2005.Chronologies for recent peat deposits using wiggle-matched radiocarbon ages:problems withold carbon contamination.Radiocarbon,47(1):135-145
Charman D J,Hendon D&Packman S.1999a.Multiproxy surfacere cords from replicate cores on an ombrotrophic mire:implications for Holocene palaeoclimatic records.Journal of Quaterna-ry Science,14:451-463
Charman D J&Warner B.1997.The ecology of testate amoebae(Protozoa:Rhizopoda)in oceanic peatlands in Newfoundland,Canada:Modelling hydrological relationships for paleoenviron-mental reconstruction.Ecoscience,4:555-562
Chanton J P,Bauer J E,Glaser P A,Siegel D I,Kelly C A,Tyler SC,Romanowicz E H&Lazrus A.1995.Radiocarbon evidencefor the substrates supporting methane formation within north-ern Minnesota peatlands.Geochimica.et Cosmochimica.Acta,59:3663-3668
Clark I&Fritz P.1997.Environmental isotopes in hydrogeology.Boca Raton,FL:CRC Press.
Clymo R S.1984.The limits to peat bog growth.Philosophical Transactions of the Royal Society of London,Biological Sci-ences(Series B),303(1117):605-654
Clymo R S.1987.The ecology of peatlands.Science Progress(Ox-ford),71:593-614
Craft C B&Richardson C J.1993.Peat accretion and N,P,and organic C accumulation in nutrient-enriched and unenriched ever-glades peatlands.Ecological Applications,3(3):446-458
Gignac L D,Nicholson B J&Bayley S E.1998a.The utilization of bryophytes in bioclimatic modeling:present distribution of peat-lands in the Mackenzie River Basin,Canada.The Bryologist,101:560-571
Gignac L D,Nicholson B J&Bayley S E.1998b.The utilization of bryophytes in bioclimatic modeling:predicted northward migra-tions of peatlands in the Mackenzie River Basin,Canada as a re-sult of global warming.The Bryologist,101:572-587
Gignac L D&Vitt D H.1994.Responses of northern peatlands to climate change:Effects on bryophytes.Journal of the HattoriBotanical Laboratory,75:119-132
Gorham E.1991.Northern peatlands:role in the carbon cycle and probable responses to climatic warming.Ecological Applica-tions,1:182-195
Gorham E&Janssens J.1992.The paleorecord of geochemistry and hydrology in northern peatlands and its relation to globalchange.Suo,43:117-126
Heijmans M P D,Mauquoy D,van Geel B&Berendse F.2008.Longterm effects of climate change on vegetation and carbondynamics in peat bogs.Journal of Vegetation Science,19:307-320
Hughes P D M&Barber K E.2004.Contrasting pathways to om-brotrophy in three raised bogs from Ireland and Cumbria,Eng-land.The Holocene,14:65-77
Hughes P D M,Blundell A,Charman D J,Bartlett S,Daniell J RG,Wojatschke A&Chambers F M.2006.A9000cal yearmultiproxy climate record from a bog in eastern Newfoundland:Contributions of meltwater discharge and solar forcing.Quater-nary Science Reviews,25:1208-1227
Jackson S T&Charman D.2010.Editorial:peatlands—paleoenvir-onments and carbon dynamics.PAGES news,18(1):3-4
Joosten H&Clarke D.2002.Wise use of mires and peatlands-back-ground and principles including a framework for decision-mak-ing.International Mire Conservation Group and InternationalPeat Society,Finland.
Jouzel J,Hoffmann G,Koster R D&Masson V.2000.Water iso-topes in precipitation:data/model comparison for present-dayand past climates.Quaternary Science Reviews,19:363-379
Johnson L C&Damman A W H.1991.Species controlled Sphag-num decay on a south Swedish raised bog.Oikos,61:234-242
Korhola A,Tolonen K,Turunen J&Jungner H.1995.Estimatinglongterm carbon accumulation rates in boreal peatlands by radi-ocarbon dating.Radiocarbon,37:575-584
Kuhry P.1997.The palaeoecology of a treed bog in western boreal Canada:a study based on microfossils,macrofossils and physi-co-chemical properties.Review of Palaeobotany and Palynolo-gy,96:183-224
Lansdown J M,Quay P D&King S L.1992.CH4production viaCO2reduction in a temperate bog:a source of13C-depletedCH4.Geochimica et Cosmochimica Acta,56:3493-3503
Langdon P G,Barber K E&Hughes P D M.2003.A7500-yearpeat-based palaeoclimatic reconstruction and evidence for an1100-year cyclicity in bog surface wetness from Temple HillMoss,Pentland Hills,southeast Scotland.Quaternary ScienceReviews,22:259-274
Lamentowicz M,Lamentowicz M&Gabka M.2008a.Testateamoebae ecology and a local transfer function from a peatland inwestern Poland.Wetlands,28:164-175
Lamentowicz M,Obremska M&Mitchell E A D.2008b.Autogenic succession,land-use change,and climatic influences on theHolocene development of a kettle hole mire in Northern Poland.Review of Palaeobotany and Palynology,151:21-40
Lamentowicz M,Van der Knaap P,Lamentowicz L,Van Leeuwen JF N,Mitchell E A D,Goslar T&Kamenik C.2009.A near-annual palaeohydrological study based on testate amoebae froman Alpine mire:Surface wetness and the role of climate duringthe instrumental period.Journal of Quaternary Science,24:190-202
Lottes A L&Ziegler A M.1994.World peat occurrence and the seasonality of climate and vegetation.Palaeogeography,Palaeo-climatology,Palaeoecology,106:23-37
Maltby E&Proctor M C F.1996.Peatlands:their nature and rolein the biosphere.In:Lappalainen E ed.Global peat resources.International Peat Society,Jysk,Finland.11-19
Mauquoy D&Barber K E.1999.A replicated3000yr proxy-climate record from Coom Rigg Moss and Felecia Moss,the Bor-der Mires,northern England.Journal of Quaternary Science,14:263-275
Mauquoy D,Engelkes T,Groot MHM,Markesteijn F,Oudejans MG,van der Plicht J&van Geel B.2002.High-resolution re-cords of late Holocene climate change and carbon accumulationin two north-west European ombrotrophic peat bogs.Palaeo-geography,Palaeoclimatology,Palaeoecology,186:275-310
Mauquoy D,van Geel B,Blaauw M,Speranza A&van der Plicht J.2004.Changes in solar activity and Holocene climate shifts derived from14C wiggle-match dated peat deposits.The Hol-ocene,14:45-52
Mauquoy D,Yeloff D,van Geel B,Charman D&Blundell A.2008.Two decadally resolved records from north-west Europe-an peat bogs show rapid climate changes associated with solarvariability during the mid-late Holocene.Journal of QuaternaryScience,23:745-763
Mazei Y A,Tsyganov A N&Bubnova O A.2009.The species composition and community structure of testate amoebae insphagnum bogs of northern Karelia(The White Sea Lowland).Journal of Zoology,88:1-12
McGlone M S&Wilmshurst J M.1999.A Holocene record of climate,vegetation change and peat bog development,East Ota-go,South Island,New Zealand.Journal of Quaternary Science,14(3):239-254
McMullen J A,Barber K E&Johnson B.2004.A palaeoecological perspective of vegetation succession on raised bog microforms.Ecological Monography,74:45-77
Meisterfeld R.2001a.Order Arcellinida,Kent1880.In:Lee J J,Leedale G F&Bradbury P eds.The illustrated guide to theProtozoa.Lawrence:Allen Press.827-860
Meisterfeld R.2001b.Testate amoebae with filopoda.In:Lee J J,Leedale G F&Bradbury P eds.The illustrated guide to theProtozoa.Lawrence:Allen Press.1054-1084
Mitchell E A D,Buttler A,Warner B G&Gobat J M.1999.Ecology of testate amoebae(Protozoa:Rhizopoda)in Sphagnumpeatlands in the Jura mountains,Switzerland and France.Eco-science,6:565-576
Mitchell E A D,van der Knaap W O,van Leeuwen J F N,ButtlerA,Warner B G&Gobat J M.2001.The palaeoecological his-tory of the Praz-Rodet bog(Swiss Jura)based on pollen,plantmacrofossils and testate moebae(Protozoa).The Holocene,11(1):65-80
Mitchell E,Charman D&Warner B.2008.Testate amoebae analysis in ecological and paleoecological studies of wetlands:Past,present and future.Biodiversity Conservation,17:2115-2137
Mitsch W J&Gosselink J G.2007.Wetlands(4th ed).New York:John Wiley&Sons
Morgan T J,Herod A A,Brain S A,Chambers F M&KandiyotiR.2005.Examination of soil contaminated by coal-liquids bysize-exclusion chromatography in1-methyl-2-pyrrolidinone solu-tion to evaluate interference from humic and fulvic acids and ex-tracta from peat.Journal of Chromatography,1095:81-88
Muller S,Bobrov A A,Schirrmeister L,Andreev A A&Tarasov PE.2009.Testate amoebae record from the Laptev Sea coast andits implication for the reconstruction of Late Pleistocene andHolocene environments in the Arctic Siberia.Palaeogeography,Palaeoclimatology,Palaeoecology,271:301-315
Nichols J E,Booth R K,Jackson S T,Pendall E G&Huang Y.2006.Paleohydrologic reconstruction based on n-alkane distri-butions in ombrotrophic peat.Organic Geochemistry,37:1505-1513
Nichols J E,Walcott M,Bradley R,Pilcher J&Huang Y.2009.Quantitative assessment of precipitation seasonality and summersurface wetness using ombrotrophic sediments from an ArcticNorwegian peatland.Quaternary Research,72(3):443-451
Nicholson B J,Gignac L D&Bayley S E.1996.Peatland distribution along a north-south transect in the Mackenzie River Basinin relation to climatic and environmental gradients.Vegetation,126:119-133
Nott C J,Xie S,Avsejs L A,Maddy D,Chambers F M&EvershedR P.2000.n-Alkane distribution in ombrotrophic mires as indi-cators of vegetation change related to climatic variation.OrganicGeochemistry,31:231-235
Oldfield F,Thompson R,Crooks P R J,Gedye S J,Hall V A,Har-kness D D,Housley R A,McCormac F G,Newton A J,Pil-cher J R,Renberg I&Richardson N.1997.Radiocarbon dat-ing of a recent high-latitude peat profile:Stormyran,north-ern Sweden.The Holocene,7:283-290
Pancost R,Baas M,van Geel B&Sinninghe Damste J S.2002.Biomarkers as proxies for plant inputs to peats:an example from asub-boreal ombrotrophic bog.Organic Geochemistry,33:675-690
Payne R J,Kishaba K,Blackford J J&Mitchell E A D.2006.Ecology of testate amoebae(Protista)in south-central Alaskapeatlands:Building transfer-function models for palaeoenviron-mental studies.The Holocene,16:403-414
Payne R&Mitchell E A D.2007.Ecology of testate amoebae from Mires in the Central Rhodope Mountains,Greece and develop-ment of a transfer function for palaeohydrological reconstruc-tion.Protist,158:159-171
Payne R J,Charman D J,Matthews S&Eastwood W J.2008.Testate amoebae as palaeohydrological proxies in SurmeneAgacbasi Yaylasi peatland(Northeast Turkey).Wetlands,28:311-323
Pellerin S&Lavoie C.2003.Reconstructing the recent dynamics ofmires using a multitechnique approach.Journal of Ecology,91:1008-1021
Pfadenhauer J,Schneekloth H,Schneider R&Schneider S.1993.Mire distribution.In:Heathwaite A L&Gttlich Kh eds.Mires:process,exploitation and conservation.Chichester.Wi-ley.71-121
Price G D,McKenzie J E,Pilcher J R&Hoper S T.1997.Carbon-isotope variation in Sphagnum from hummock-hollow comple-xes:implications for Holocene climate reconstruction.The Hol-ocene,7:229-233
Proctor M C F,Raven J A&Rice S K.1992.Stable carbon isotopediscrimination measurements in Sphagnum and other bryo-phytes:physiological and ecological implications.Journal ofBryology,17:193-202
Raghoebarsing A,Smolders A&Schmid M.2005.Methan otrophicsymbionts provide carbon for photosynthesis in peat bogs.Na-ture,436:1153-1156
Schrter D,Wolters V&De Ruiter P C.2003.C and N mineralization in the decomposer food webs of a European forest transect.Oikos,102:294-308
Shotyk W.1988.Review of the inorganic geochemistry of peats andpeatland waters.Earth-Science Reviews,25:95-176
Shurpali N J,Verma S B,Kim J&Arkebauer T J.1995.Carbondioxide exchange in a peatland ecosystem.Journal of Geophysi-cal Research,100(D7):14319-14326
Sukumar R,Ramesh R,Pant R K&Rajagopalan G.1993.Aδ13Crecord of late Quaternary climate change from tropical peats insouthern India.Nature,364:703-706
Swindles G T,Plunkett G&Roe H M.2007.A delayed climaticresponse to solar forcing at2800cal BP:Multiproxy evidencefrom three Irish peatlands.The Holocene,17:177-182
Tolonen K,Warner B G&Vasander H.1994.Ecology of Testaceans(Protozoa:Rhizopoda)in mires in Southern Finland:II.Multivariate analysis.Arch Protistenkunde,144:97-112
Tolonen K&Turunen J.1996.Accumulation rates of carbon inmires in Finland and implications for climate change.The Hol-ocene,6(2):171-178
Turetsky M R&Wieder R K.1999.Refixation of soil-produced orrespired14CO2by Sphagnum in a boreal bog.Ecoscience,6:587-591
Turetsky M R,Wieder R K,Willams,C J&Vitt D H.2000.Or-ganic matter accumulation,peat chemistry,and permafrostmelting in peatlands of boreal Alberta.Ecoscience,7:379-392
Turunen J,Roulet N T&Moore T R.2004.Nitrogen depositionand increased carbon accumulation in ombrotrophic peatlands ineastern Canada.Global Bioecological Cycles,18(GB3002):1-12
Ukonmaanaho L,Nieminen T M,Rausch N,Cheburkin A,LeRouxG&Shotyk W.2006.Recent organic matter accumulation inrelation to some climatic factors in ombrotrophic peat bogs nearheavy metal emission sources in Finland.Global and PlanetaryChange,53:259-268
Vliranta M,Korhola A,SeppH,Tuittila E-S,Sarmaja-KorjonenK,Laine J&Alm J.2007.High-resolution reconstruction ofwetness dynamics in a southern boreal raised bog,Finland,dur-ing the late Holocene:A quantitative approach.The Holocene,17:1093-1107
Vitt D H,Halsey L A,Bauer I E&Campbell C.2000.Spatial andtemporal trends in carbon storage of peatlands of continentalwestern Canada through the Holocene.Canadian Journal ofEarth Sciences,37:683-693
Warner B G&Charman D J.1994.Holocene soil moisture changeson a peatland in northwestern Ontario based on fossil testateamoebae(Protozoa)analysis.Boreas,23:270-279
White J W C,Clais P,Figge R A,Kenny R&Markgraf V.1994.A high-resolution record of atmospheric CO2content from car-bon isotopes in peat.Nature,367:153-156
Wieder R K,Turetsky M R&Vile M A.2009.Peat as an archiveof atmospheric,climatic and environmental conditions.In:Maltby E&Barker T eds.The wetlands handbook.Oxford:Blackwell Publishing Ltd.96-112
Williams T&Flannagan L.1996.Effect of changes in water content on photosynthesis,transpiration and discrimination agains13CO2and C18O16O in Pleurozium and Sphagnum.Oecologia,108:38-46
Wilkinson D M.2008.Testate amoebae and nutrient cycling:Peering into the black box of soil ecology.Trends Ecological Evolu-tion,23:596-599
Xie S,Nott C,Avsejs L,Maddy D,Chambers F.2004.Molecular and isotopic stratigraphy in an ombrotrophic mire for paleocli-mate reconstruction.Geochimica Cosmochimica Acta,68:2849-2862
Yeloff D&Mauquoy D.2006.The influence of vegetation composition on peat humification:Implications for palaeoclimatic studies.Boreas,35:662-673
Yeloff D,Charman D,van Geel B&Mauquoy D.2007.Recon-struction of hydrology,vegetation and past climate change inbogs using fungal microfossils.Review of Palaeobotany and Pal-ynology,146:102-145
Zhang W J,Xiao H A,Tong C L,Su Y R,Xiang W S,Huang DY,Syers J K&Wu J S.2008.Estimating organic carbon stor-age in temperate wetland profiles in Northeast China.Geoder-ma,146:311-316
基本信息:
DOI:10.19839/j.cnki.dcxzz.2012.01.014
中图分类号:P532
引用信息:
[1]鲍锟山,王国平,赵红梅,等.泥炭沉积与气候变化的泥炭记录[J].地层学杂志,2012,36(01):97-108.DOI:10.19839/j.cnki.dcxzz.2012.01.014.
基金信息:
国家重点基础研究发展计划项目(No.2012CB956100);; 国家自然科学基金资助项目(No.40830535,40871089)
2012-01-15
2012-01-15