豬野澤

豬野澤及河西走廊晚第四紀文獻索引及引用指南
ReferenceguideoftheLateQuaternaryclimatechangeforZhuyeLakeandtheHexiCorridorintheAsianmonsoonmarginalzones,northwestChina
河西走廊及豬野澤位於青藏高原北緣的祁連山南麓，處於戈壁大漠和高原之間的過渡地帶。在氣候上，該區域處於亞洲夏季風的西北緣，部分夏季降水來源於夏季風水汽輸送，同時主要受控於中緯度西風帶環流，是季風-西風相互作用的關鍵區域。近年來，該區域晚第四紀環境變化研究取得了大量進展，推動了長時間尺度季風和西風演化的研究，但還存在一些爭議。一個主要問題就是該區域文獻量比較大，與第四紀相關的論文較多，且學科較雜，不利於相關學者了解該區域的研究狀況。本索引旨在整理該區域近年來各相關學科的主要文獻，便於第四紀科學研究者了解該區域狀況，同時該索引也代表了蘭州大學晚第四紀研究在該區域的進展情況。
ZhuyeLakeandtheHexiCorridorarelocatedinthenorthernedgeoftheQinghai-TibetanPlateau,onthenorthernsideoftheQilianMountains,whileinatransitionzonebetweentheGobidesertandhighland.TheareaisinthenorthwestmarginoftheAsiansummermonsoon.Somesummerprecipitationisfromthesummermonsoonmoisturetransport,whiletheareaismainlycontrolledbythemid-latitudewesterlycirculation,whichisakeyareaforstudiesontheinteractionsbetweenthesummermonsoonandthewesterlies.Inrecentyears,scientistshavemadealotofprogressonthelateQuaternaryenvironmentalchangesinthearea,andpromotedthestudyoflong-termmonsoonandwesterlywindschanges,buttherearestillsomecontroversies.AmajorproblemisthattherearealargevolumeofpapersintheareathatarerelatedtotheQuaternarysciencewhilevarioussubjectsareinvolved.ThatisnotconduciveforscholarstounderstandthelateQuaternaryconditionsinthearea.Thereferenceguideisdesignedtoorganizeliteraturesinrelevantdisciplines,whichisgoodforscientiststounderstandthelateQuaternaryenvironmentseasily,whiletheguidealsorepresentstheresearchprogressofLanzhouUniversityonthelateQuaternaryenvironments.
1豬野澤千年尺度環境變化
豬野澤湖泊沉積物環境代用指標記錄顯示，豬野澤地區早全新世環境相對濕潤，中全新世階段水熱組合較為適宜，而晚全新世環境趨於乾旱。中全新世期間存在一次百年尺度的乾旱事件，不同位置的沉積剖面的砂層沉積是這次乾旱事件的主要標誌物。豬野澤全新世環境變化主要受亞洲夏季風演化控制，同時也受到中緯度西風帶氣候變化的影響，體現了季風邊緣區湖泊演化的特殊性。
[1]Chen,F.,Zhu,Y.,Li,J.,Shi,Q.,Jin,L.,Wünemann,B.,2001.AbruptHolocenechangesoftheAsianmonsoonatmillennial–andcentennial–scales:EvidencefromlakesedimentdocumentinMinqinBasin,NWChina.ChineseScienceBulletin46,1942–1947.
[2]Chen,F.,Cheng,B.,Zhao,Y.,Zhu,Y.,Madsen,D.B.,2006.Holoceneenvironmentalchangeinferredfromahigh–resolutionpollenrecord,LakeZhuyeze,aridChina.TheHolocene16,675–684.
[3]Li,Y.,Wang,N.,Cheng,H.,Long,H.,Zhao,Q.,2009.HoloceneenvironmentalchangeinthemarginalareaoftheAsianmonsoon:ArecordfromZhuyeLake,NWChina.Boreas38,349–361.
[4]Li,Y.,Wang,N.,Morrill,C.,Cheng,H.,Long,H.,Zhao,Q.,2009.Environmentalchangeimpliedbytherelationshipbetweenpollenassemblagesandgrain–sizeinNWChineselakesedimentssincetheLateGlacial.ReviewofPalaeobotanyandPalynology154,54–64.
[5]Long,H.,Lai,Z.,Wang,N.,Li,Y.,2010.HoloceneclimatevariationsfromZhuyezeterminallakerecordsinEastAsianmonsoonmargininaridnorthernChina.QuaternaryResearch74,46–56.
2鹽池千年尺度氣候變化
鹽池晚冰期以來湖泊演化過程與青藏高原區和典型季風區的古氣候記錄具有一致性，晚冰期及早全新世湖泊擴張，中、晚全新世期間湖泊退縮明顯，這種變化顯示了千年尺度亞洲夏季風對該區域的影響，證明了夏季風北部邊界擺動的事實。
[1]Li,Y.,Wang,N.,Morrill,C.,Anderson,D.M.,Li,Z.,Zhang,C.,Zhou,X.,2012.Millennial–scaleerosionratesinthreeinlanddrainagebasinsandtheircontrollingfactorssincetheLastDeglaciation,aridChina.Palaeogeography,Palaeoclimatology,Palaeoecology365–366,263–275.
[2]Li,Y.,Wang,N.,Li,Z.,Zhou,X.,Zhang,C.,2013.ClimaticandenvironmentalchangeinYanchiLake,NorthwestChinasincetheLateGlacial:Acomprehensiveanalysisoflakesediments.JournalofGeographicalSciences23,932–946.
[3]Yu,Y.,Yang,T.,Li,J.,Liu,J.,An,C.,Liu,X.,Su,X.,2006.Millennial–scaleHoloceneclimatevariabilityintheNWChinadrylandsandlinkstothetropicalPacificandtheNorthAtlantic.Palaeogeography,Palaeoclimatology,Palaeoecology233,149–162.
[4]李育,王乃昂,李卓侖,周雪花,張成琦,2013.河西走廊鹽池晚冰期以來沉積地層變化綜合分析——來自夏季風西北緣一個關鍵位置的古氣候證據.地理學報68(7),933–944.[Li,Y.,Wang,N.,Li,Z.,Zhou,X.,Zhang,C.,2013.AcomprehensiveanalysisofYanchisedimentarystratachangessincetheLateGlacialinHexiCorridor——paleoclimateevidencefromakeypositionofsummermonsoonnorthwestedge.ActaGeographicaSinica68,933–944.(inChinese)]
[5]申建梅,張光輝,聶振龍,王金哲,嚴明疆,張俊牌,瑞林,2008.西北內陸高台鹽池孢粉組合與古氣候變化.中國生態農業學報16(2),323–326.[Shen,J.,Zhang,G.,Nie,Z.,Wang,J.,Yan,M.,Zhang,J.,Guo,R.,2008.Characteristicsofspore–pollenandancientclimatechangesininlandsofNorthwestChina.ChineseJournalofEco–Agriculture16,323–326.(inChinese)]
3花海千年尺度氣候變化
花海沉積物記錄的千年尺度環境變化表現為，早全新世環境流域徑流較大，流域性侵蝕及沉積過程較劇烈；中全新世有效濕度較高，晚全新世環境趨於乾旱。這種水分條件的變化與早全新世較強的亞洲季風所帶來的較多降水有關，從而增加了徑流量和流域性的侵蝕量。這種全新世水分條件變化模式，也受到了中緯度西風帶的影響。
[1]Li,Y.,Wang,N.,Morrill,C.,Anderson,D.M.,Li,Z.,Zhang,C.,Zhou,X.,2012.Millennial–scaleerosionratesinthreeinlanddrainagebasinsandtheircontrollingfactorssincetheLastDeglaciation,aridChina.Palaeogeography,Palaeoclimatology,Palaeoecology365,263–275.
[2]Wang,N.,Li,Z.,Li,Y.,Cheng,H.,Huang,R.,2012.YoungerDryaseventrecordedbythemirabilitedepositioninHuahaiLake,HexiCorridor,NWChina.QuaternaryInternational250,93–99.
[3]Wang,N.,Li,Z.,Li,Y.,Cheng,H.,2013.Millennial–scaleenvironmentalchangesintheAsianmonsoonmarginduringtheHolocene,implicatedbythelakeevolutionofHuahaiLakeintheHexiCorridorofnorthwestChina.QuaternaryInternational313,100–109.
[4]胡剛,王乃昂,羅建育,高順尉,李巧玲,2001.花海湖泊古風成砂的粒度特徵及其環境意義.沉積學報19(4),642–647.[Hu,G.,Wang,N.,Luo,J.,Gao,S.,Li,Q.,2001.Thegrainsizecharacteristicsofaeoliansandanditsenvironmentalsignificance.ActaSedimentologicaSinica19,642–647.(inChinese)]
[5]胡剛,王乃昂,趙強,程弘毅,諶永生,郭劍英,2003.花海湖泊特徵時期的水量平衡.冰川凍土25(5),485–490.[Hu,G.,Wang,N.,Zhao,Q.,Cheng,H.,Chen,Y.,Guo,J.,2003.WaterbalanceofHuahaiLakeBasinduringaspecialphase.JournalofGlaciologyandGeocryology25,485–490.(inChinese)]
4豬野澤氣候變化周期
豬野澤湖泊沉積物古環境代用指標記錄顯示，該區域有明顯的~256、~512、~1024年氣候循環周期，這與典型亞洲夏季風區全新世千年尺度和百年尺度氣候循環周期一致。同時，該區域湖泊沉積物中也記錄了明顯的北大西洋浮冰碎屑事件（BondEvents），這與該事件的全球性有關，體現了季風邊緣區環境變化對全球尺度氣候變化周期的回響。
[1]Li,Y.,Wang,N.,Li,Z.,Zhou,X.,Zhang,C.,2012.HoloceneclimatecyclesinnorthwestmarginofAsianmonsoon.ChineseGeographicalScience22,450–461.
[2]李育,李卓侖,王乃昂,2012.蒸發和環流因素對湖泊演化的影響——河西走廊豬野澤不同位置全新世沉積物古環境意義探討.湖泊科學24(3),474–479.[Li,Y.,Li,Z.,Wang,N.,2012.Impactsofevaporationandcirculationonlakeevolution:paleoenvironmentalimplicationsforHolocenesedimentsatdifferentlocationsofLakeZhuye,HexiCorridor.JournalofLakeSciences24,474–479.(inChinese)]
[3]Chen,F.,Zhu,Y.,Li,J.,Shi,Q.,Jin,L.,Wünemann,B.,2001.AbruptHolocenechangesoftheAsianmonsoonatmillennial–andcentennial–scales:EvidencefromlakesedimentdocumentinMinqinBasin,NWChina.ChineseScienceBulletin46,1942–1947.
[4]Chen,F.,Wu,W.,Holmes,J.A.,Madsen,D.B.,Zhu,Y.,Jin,M.,Oviatt,C.G.,2003.Amid–HolocenedroughtintervalasevidencedbylakedesiccationintheAlashanPlateau,InnerMongoliaChina.ChineseScienceBulletin48,1401–1410.
[5]靳立亞,陳發虎,朱艷,2004.西北乾旱區湖泊沉積記錄反映的全新世氣候波動周期性變化.海洋地質與第四紀地質24(2),101–108.[Jin,L.,Chen,F.,Zhu,Y.,2004.HoloceneClimaticPeriodicitiesRecordedfromLakeSedimentsinthe/Arid–SemiaridAreasofNorthwesternChina.MarineGeologyandQuaternaryGeology24,101–108.(inChinese)]
5豬野澤中全新世乾旱事件
季風邊緣區的湖泊沉積物中廣泛存在一次中全新世乾旱事件，但是關於這次事件的年代和機制還存在爭議。根據豬野澤湖泊沉積物的岩性、年代和待用指標探索，這次乾旱事件主要發生在~8.0-~7.0calkyrBP之間，其影響範圍主要在石羊河中、下游地區，對石羊河上游地區影響較小，這次乾旱事件可能主要受控於流域性水熱配比變化及季風與西風互動。
[1]Chen,F.,Zhu,Y.,Li,J.,Shi,Q.,Jin,L.,Wünemann,B.,2001.AbruptHolocenechangesoftheAsianmonsoonatmillennial–andcentennial–scales:EvidencefromlakesedimentdocumentinMinqinBasin,NWChina.ChineseScienceBulletin46,1942–1947.
[2]Chen,F.,Wu,W.,Holmes,J.A.,Madsen,D.B.,Zhu,Y.,Jin,M.,Oviatt,C.G.,2003.Amid–HolocenedroughtintervalasevidencedbylakedesiccationintheAlashanPlateau,InnerMongoliaChina.ChineseScienceBulletin48,1401–1410.
[3]Chen,F.,Cheng,B.,Zhao,Y.,Zhu,Y.,Madsen,D.B.,2006.Holoceneenvironmentalchangeinferredfromahigh–resolutionpollenrecord,LakeZhuyeze,aridChina.TheHolocene16,675–684.
[4]Li,Y.,Wang,N.,Li,Z.,Zhang,H.,2011.HolocenepalynologicalrecordsandtheirresponsestothecontroversiesofclimatesystemintheShiyangRiverdrainagebasin.ChineseScienceBulletin56,535–546.
[5]李育,王乃昂,李卓侖,張華安,周雪花,張成琦,2012.豬野澤中全新世乾旱事件時空範圍和機制.地理科學32(6),731–738.[Li,Y.,Wang,N.,Li,Z.,Zhang,H.,Zhou,X.,Zhang,C.,2012.Thespatialandtimescalesforthedrymid–HoloceneeventinZhuyeLake.ScientiaGeographicaSinica32,731–738.(inChinese)]
6豬野澤年代學
豬野澤湖泊沉積物晚第四紀年代結果主要來自孢粉濃縮物、全樣有機質、全樣無機質、軟體動物殼體AMS14C和常規14C測年，光釋光測年也套用於部分湖泊沉積剖面。通過多種物質的測年物質和測年方法結果對比，豬野澤晚第四紀湖泊沉積物碳庫效應較小，部分層位年代有倒置現象，年代混亂現象主要集中在晚冰期和早全新世地層中，這主要受湖泊再沉積作用影響。根據豬野澤東北岸古湖泊岸堤光釋光及14C測年年代結果，豬野澤全新世高湖面期主要存在於早、中全新世，晚全新世體現了乾旱化趨勢。古湖泊岸堤年代結果所顯示的湖泊水位變化過程與湖泊沉積物指標研究一致。
[1]Li,Y.,Wang,N.,Li,Z.,Zhang,C.,Zhou,X.,2012.ReworkingeffectsintheHoloceneZhuyeLakesediments:AcasestudybypollenconcentratesAMS14Cdating.ScienceChinaEarthSciences55,1669–1678.
[2]Long,H.,Lai,Z.,Wang,N.,Li,Y.,2010.HoloceneclimatevariationsfromZhuyezeterminallakerecordsinEastAsianmonsoonmargininaridnorthernChina.QuaternaryResearch74,46–56.
[3]Long,H.,Lai,Z.,Fuchs,M.,Zhang,J.,Li,Y.,2012.TimingofLateQuaternarypalaeolakeevolutioninTenggerDesertofnorthernChinaanditspossibleforcingmechanisms.GlobalandPlanetaryChange92,119–129.
[4]Zhang,H.C.,Peng,J.,Ma,Y.,Chen,G.,Feng,Z.,Li,B.,Fan,H.,Chang,F.,Lei,G.,Wünemann,B.,2004.LateQuaternarypalaeolakelevelsinTenggerDesert,NWChina.Palaeogeography,Palaeoclimatology,Palaeoecology211,45–48.
[5]Zhang,H.C.,Wünemann,B.,Ma,Y.Z.,Pachur,H.-J.,Li,J.J.,Qi,Y.,Chen,G.J.,Fang,H.B.,2002.Lakelevelandclimatechangebetween40,000and18,00014CyearsBPinTenggerDesert,NWChina.QuaternaryResearch58,62–72.
7豬野澤孢粉
伴隨著流域性千年尺度環境變化和古生態-古植被變化，豬野澤沉積物孢粉記錄較好地反映了流域性植被的變化。但是豬野澤湖盆地形複雜，不同位置孢粉組合存在差異，湖盆西側受沖積相花粉影響較大，中、東部花粉組合較好的反映了湖泊水動力充分混合後的花粉組合。總體來講，早全新世上游喬木花粉含量較高，表現了較高的徑流量和降水量，中全新世花粉組合較豐富、孢粉濃度達到最高，晚全新世湖泊花粉組合變化現實了乾旱化趨勢。豬野澤地區全新世孢粉譜與其他指標對應較好，可靠地記錄了湖泊及流域的環境變化。
[1]Li,Y.,Wang,N.,Morrill,C.,Cheng,H.,Long,H.,Zhao,Q.,2009.Environmentalchangeimpliedbytherelationshipbetweenpollenassemblagesandgrain–sizeinNWChineselakesedimentssincetheLateGlacial.ReviewofPalaeobotanyandPalynology154,54–64.
[2]Li,Y.,Wang,N.,Li,Z.,Zhang,H.,2011.HolocenepalynologicalrecordsandtheirresponsestothecontroversiesofclimatesystemintheShiyangRiverdrainagebasin.ChineseScienceBulletin56,535–546.
[3]Chen,F.,Cheng,B.,Zhao,Y.,Zhu,Y.,Madsen,D.B.,2006.Holoceneenvironmentalchangeinferredfromahigh–resolutionpollenrecord,LakeZhuyeze,aridChina.TheHolocene16,675–684.
[4]Zhao,Y.,Yu,Z.,Chen,F.,Li,J.,2008.HolocenevegetationandclimatechangefromalakesedimentrecordintheTenggerSandyDesert,northwestChina.JournalofAridEnvironments72,2054–2064.
[5]ZhuY.,ChenF.,DavidM.,2002.TheenvironmentalsignalofanearlyHolocenepollenrecordfromtheShiyangRiverbasinlakesediments,NWChina.ChineseScienceBulletin47,267–273.
8豬野澤沉積物岩性、礦物及石英砂掃描電鏡分析
湖泊沉積物岩性、礦物及石英砂微形態也是反映湖泊演化過程的良好指標。豬野澤湖相沉積物以青灰色粉砂為主，部分層位夾雜褐色銹斑和黑色泥炭沉積層，湖相沉積層之間夾雜青灰色或黃褐色砂層，剖面頂部通常沉積了厚度不均的風成沉積物，這些岩性特徵指示了湖泊水動力條件的變化過程以及區域的風沙活動。碳酸鹽類礦物是該區域主要的鹽類礦物，其千年尺度鹽類礦物演化過程，體現了鹽湖演化的一般規律，與其他指標能形成良好對應。該區域沉積地層富含碳酸鹽類礦物，從而形成了一個巨大的無機碳庫。豬野澤地區砂層沉積物石英砂掃描電鏡分析揭示了該區域砂層沉積物來源的多元化，既帶有風成砂的特點，又經過水下環境的沉積，表明該區域砂層形成的複雜性。
[1]Li,Y.,Wang,N.,Morrill,C.,Cheng,H.,Long,H.,Zhao,Q.,2009.Environmentalchangeimpliedbytherelationshipbetweenpollenassemblagesandgrain–sizeinNWChineselakesedimentssincetheLateGlacial.ReviewofPalaeobotanyandPalynology154,54–64.
[2]Li,Y.,Wang,N.,Li,Z.,Zhou,X.,Zhang,C.,2012.HoloceneclimatecyclesinnorthwestmarginofAsianmonsoon.ChineseGeographicalScience22,450–461.
[3]Li,Y.,Wang,N.,Li,Z.,Zhou,X.,Zhang,C.,Wang,Y.,2013.Carbonateformationandwaterlevelchangesinapaleo–lakeanditsimplicationforcarboncycleandclimatechange,aridChina.FrontiersofEarthScience7,487–500.
[4]Li,Y.,Wang,N.,Li,Z.,Zhang,C.,Zhou,X.,2012.ReworkingeffectsintheHoloceneZhuyeLakesediments:AcasestudybypollenconcentratesAMS14Cdating.ScienceChinaEarthSciences55,1669–1678.
[5]李育,周雪花,李卓侖,王乃昂,2013.基於掃描電鏡分析的豬野澤全新世砂層成因探討.沉積學報31(1),149–156.[Li,Y.,Zhou,X.,Li,Z.,Wang.,N.,2013.FormationofHolocenesandlayersbySEManalysesintheZhuyeLakesediments.ActaSedimentologicaSinica31,149–156.(inChinese)]
9豬野澤沉積物地球化學
常用的湖泊沉積物有機地球化學指標有總有機碳（TOC）、碳氮比率（C/N）和有機碳同位素（δ13Corg）。它們可以反映湖泊及流域的初始生產力和植被類型，也反映了有機質隨沉積物沉積後的保存狀況，是湖泊及流域生態環境和古氣候、古環境變化信息的良好載體。豬野澤沉積物TOC與C/N變化趨勢一致，高值指示了較高的流域生產力，δ13Corg與其他兩種指標變化趨勢相反，其偏負指示較高的有效濕度。豬野澤沉積物地球化學指標研究結果與其他待用指標結果形成了良好對應，體現了早全新世徑流量及降水量較高，中全新世流域性初級生產力達到最大和晚全新世乾旱化的特點。
[1]Li,Y.,Wang,N.,Cheng,H.,Long,H.,Zhao,Q.,2009.HoloceneenvironmentalchangeinthemarginalareaoftheAsianmonsoon:ArecordfromZhuyeLake,NWChina.Boreas38,349–361.
[2]Li,Y.,Zhou,X.,Zhang,C.,Li,Z.,Wang,Y.,Wang,N.,2014.RelationshipbetweenpollenassemblagesandorganicgeochemicalproxiesandtheresponsetoclimatechangeintheZhuyeLakesediments.SciencesinColdandAridRegions.
[3]李育,王乃昂,李卓侖,程弘毅,2011.河西豬野澤沉積物有機地化指標之間的關係及古環境意義.冰川凍土33(2),334–341.[Li,Y.,Wang,N.,Li,Z.,Cheng,H.,2011.TherelationshipsamongOrganicGeochemicalProxiesandtheirpalaeoenvironmentalsignificancesintheZhuyeLakeSediments.JournalofGlaciologyandGeocryology33,334–341.(inChinese)]
[4]李育,周雪花,李卓侖,王乃昂,2013.豬野澤沉積物有機地球化學指標與花粉組合的關係及其對環境變化的回響.中國沙漠33(1),87–93.[Li,Y.,Zhou,X.,Li,Z.,Wang,N.,2013.RelationshipbetweenpollenassemblagesandorganicgeochemicalproxiesandtheresponsetoclimatechangeintheZhuyeLakesediments.JournalofDesertResearch33,87–93.(inChinese)]
[5]隆浩,王乃昂,李育,馬海州,趙強,程弘毅,黃銀洲,2007.豬野澤記錄的季風邊緣區全新世中期氣候環境演化歷史.第四紀研究27(3),371–381.[Long,H.,Wang,N.,Li,Y.,Ma,H.,Zhao,Q.,Cheng,H.,Huang,Y.,2007.Mid–HoloceneclimatevariationsfromlakerecordsoftheEastAsianmonsoonmargin:Amulti–proxyandgeomorphologicalstudy.QuaternarySciences27,371–381.(inChinese)]
10豬野澤晚第四紀古湖泊地貌學
古湖泊岸堤高程測量和OSL及14C測年可更好地了解中國西北地區晚第四紀高湖面的形成和演化。經實地調查表明，豬野澤東北緣有9級古湖泊岸堤和一級階地，這些古湖泊岸堤的年代結果體現了豬野澤從早、中全新世到晚全新世湖泊退縮的過程。全新世千年尺度上OSL及14C測年雖然存在差異，但共同現實了早、中全新世的高湖面。MIS3和MIS5階段高湖面的情況，兩種方法結果存在差異，有待進一步研究。
[1]Li,Y.,Wang,N.,Li,Z.,Zhang,C.,Zhou,X.,2012.ReworkingeffectsintheHoloceneZhuyeLakesediments:AcasestudybypollenconcentratesAMS14Cdating.ScienceChinaEarthSciences55,1669–1678.
[2]Wang,N.,Li,Z.,Cheng,H.,Li,Y.,Huang,Y.,2011.HighlakelevelsonAlashanPlateauduringtheLateQuaternary.ChineseScienceBulletin56,1799–1808.
[3]Long,H.,Lai,Z.,Fuchs,M.,Zhang,J.,Li,Y.,2012.TimingofLateQuaternarypalaeolakeevolutioninTenggerDesertofnorthernChinaanditspossibleforcingmechanisms.GlobalandPlanetaryChange92,119–129.
[4]Zhang,H.C.,Wünemann,B.,Ma,Y.Z.,Pachur,H.-J.,Li,J.J.,Qi,Y.,Chen,G.J.,Fang,H.B.,2002.Lakelevelandclimatechangebetween40,000and18,00014CyearsBPinTenggerDesert,NWChina.QuaternaryResearch58,62–72.
[5]Zhang,H.C.,Peng,J.,Ma,Y.,Chen,G.,Feng,Z.,Li,B.,Fan,H.,Chang,F.,Lei,G.,Wünemann,B.,2004.LateQuaternarypalaeolakelevelsinTenggerDesert,NWChina.Palaeogeography,Palaeoclimatology,Palaeoecology211,45–48.
11豬野澤水量平衡及GIS
千年尺度湖泊演化除了受大氣環流特徵的影響外，蒸發也起了重要作用。湖泊蒸發量主要與相對濕度、溫度、水汽壓和日照時間有關。根據豬野澤地區現代觀測結果，溫度和相對濕度的變化可能在全新世千年尺度湖泊水位的變化中起重要作用。進一步研究顯示，豬野澤湖泊水位變化受控因素較多，流域及湖面降水是最主要的控制因素，但是流域性蒸散發和湖面蒸發也會影響千年尺度湖泊面積變化。
[1]Li,Y.,Wang,N.,Li,Z.,Ma,N.,Zhou,X.,Zhang,C.,2013.Lakeevaporation:Apossiblefactoraffectinglakelevelchangestestedbymodernobservationaldatainaridandsemi–aridChina.JournalofGeographicalSciences23,123–135.
[2]李育,李卓侖,王乃昂,2012.蒸發和環流因素對湖泊演化的影響——河西走廊豬野澤不同位置全新世沉積物古環境意義探討.湖泊科學24(3),474–479.[Li,Y.,Li,Z.,Wang,N.,2012.Impactsofevaporationandcirculationonlakeevolution:paleoenvironmentalimplicationsforHolocenesedimentsatdifferentlocationsofLakeZhuye,HexiCorridor.JournalofLakeSciences24,474–479.(inChinese)]
[3]Zhao,Q.,Li,X.,Wang,N.,2008.Lacustrinestratasedimentologyandlake–levelhistoryinancientZhuyezeLakesincetheLastDeglaciation.FrontiersofEarthScienceinChina2,199–208.
[4]郭曉寅,陳發虎,施祺,2000.GIS技術和水熱平衡模型在古湖泊水文重建研究中的套用——以石羊河流域為例.地理科學20(5),422–426.[Guo,X.,Chen,F.,Shi,Q.,2000.TheapplicationofGISandwaterandenergybudgettothestudyonthewaterrebuildingofPaleo–lake——acaseinShiyangRiverdrainage.ScientiaGeographicaSinica20,422–426.(inChinese)]
[5]頡耀文,王君婷,2006.基於TM影像和DEM的白鹼湖湖面變化模擬.遙感技術與套用21(4),284–287.[Xie,Y.,Wang,J.,2006.AStudyonthechangesofBaijianLakebasedonTMimageandDEM.RemoteSensingTechnologyandApplication21,284–287.(inChinese)]
12豬野澤及夏季風西北緣現代氣候過程
氣候變化的現代過程是研究古氣候變化的基礎。亞洲季風邊緣區受到季風與西風氣流的雙重影響，其古氣候變化體現出了一定的複雜性，通過該區域氣候現代過程的研究，短時間尺度上季風-西風相互作用明顯，而且這種短尺度的聯繫可以推測該區域長時間尺度氣候變化中兩大氣候系統的相互作用。
[1]Li,Y.,Wang,N.,Chen,H.,Li,Z.,Zhou,X.,Zhang,C.,2012.Trackingmillennial–scaleclimatechangebyanalysisofthemodernsummerprecipitationinthemarginalregionsoftheAsianmonsoon.JournalofAsianEarthSciences58,78–87.
[2]Li,Y.,Wang,N.,Li,Z.,Ma,N.,Zhou,X.,Zhang,C.,2013.Lakeevaporation:Apossiblefactoraffectinglakelevelchangestestedbymodernobservationaldatainaridandsemi–aridChina.JournalofGeographicalSciences23,123–135.
[3]Li,Z.,Wang,N.,Li,Y.,Zhang,Z.,Li,M.,Dong,C.,Huang,R.,2013.RunoffsimulationsusingwaterandenergybalanceequationsinthelowerreachesoftheHeiheRiver,northwestChina.EnvironmentalEarthSciences70,1–12.
[4]李育,李卓侖,王乃昂,2012.蒸發和環流因素對湖泊演化的影響——河西走廊豬野澤不同位置全新世沉積物古環境意義探討.湖泊科學24(3),474–479.[Li,Y.,Li,Z.,Wang,N.,2012.Impactsofevaporationandcirculationonlakeevolution:paleoenvironmentalimplicationsforHolocenesedimentsatdifferentlocationsofLakeZhuye,HexiCorridor.JournalofLakeSciences24,474–479.(inChinese)]
[5]李卓侖,王乃昂,李育,來婷婷,路俊偉,2012.近50年來黑河出山徑流對氣候變化的回響.水土保持通報32(2),7–11.[Li,Z.,Wang,N.,Li,Y.,Lai,T.,Lu,J.,2012.VariationsofrunoffinrespondingtoclimatechangeinmountainousareasofHeiheRiverduringlast50years.BulletinofSoilandWaterConservation32,7–11.(inChinese)]
13季風邊緣區湖泊演化模擬
古氣候模擬與湖泊所記錄的古氣候信息提取是研究過去全球變化的兩種重要手段。模擬方法側重於古氣候變化機制研究，而湖泊記錄主要用於古氣候重建，將二者結合起來靈活運用是理解古氣候變化和長尺度水循環過程及機制的重要途徑。根據CCSM3.0古氣候模式、湖泊水量&能量平衡模型結果，季風邊緣區末次盛冰期以來的湖泊演化過程與模擬結果匹配較好。豬野澤湖泊記錄是季風邊緣區的典型記錄，其與模擬結果匹配較好，模擬方法進一步解釋了豬野澤千年尺度演化的機制問題。
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[2]Li,Y.,Wang,N.,Chen,H.,Li,Z.,Zhou,X.,Zhang,C.,2012.Trackingmillennial–scaleclimatechangebyanalysisofthemodernsummerprecipitationinthemarginalregionsoftheAsianmonsoon.JournalofAsianEarthSciences58,78–87.
[3]Li,Y.,Morrill,C.,2013.LakelevelsinAsiaattheLastGlacialMaximumasindicatorsofhydrologicsensitivitytogreenhousegasconcentrations.QuaternaryScienceReviews60,1–12.
[4]Li,Y.,Wang,N.,Li,Z.,Ma,N.,Zhou,X.,Zhang,C.,2013.Lakeevaporation:Apossiblefactoraffectinglakelevelchangestestedbymodernobservationaldatainaridandsemi–aridChina.JournalofGeographicalSciences23,123–135.
[5]李育,李卓侖,王乃昂,2012.蒸發和環流因素對湖泊演化的影響——河西走廊豬野澤不同位置全新世沉積物古環境意義探討.湖泊科學24(3),474–479.[Li,Y.,Li,Z.,Wang,N.,2012.Impactsofevaporationandcirculationonlakeevolution:paleoenvironmentalimplicationsforHolocenesedimentsatdifferentlocationsofLakeZhuye,HexiCorridor.JournalofLakeSciences24,474–479.(inChinese)]