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地理学报  2010 

史前人类向青藏高原东北缘的三次扩张与环境演变

DOI: 10.11821/xb201001007, PP. 65-72

Keywords: 史前人类,青藏高原,环境演变

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Abstract:

晚更新世以来,史前人类有3次向青藏高原东北缘扩张的历程,均与环境演变有密切的关系,第一次进军高原发生在40-30kaBP暖湿的气候背景下,其后由于LGM严酷的自然环境,人们在高原的活动极大萎缩,出现文化断层;末次冰消期迅速好转的自然环境驱动了向高原的第二次进军,其后持续暖湿的自然环境,保证了人们能在高原生存与扩散;6~4kaBP东部毗邻地区的马家窑居民,在全新世暖期的气候背景下再次进入东北缘,促使原先生活在高原的居民告别了旧石器时代,进入新石器时代,社会性质发生巨大提升。

References

[1]  HuangWeiwen,ChenKezao,YuanBaoyin.PaleolithicsofXiaoQaidamLakeinQinghaiProcinceinChina//ProceedingsoftheSino-AustralianQuaternaryMeeting.Beijing:SciencePress,1987:168-175.[黄慰文,陈克造,袁宝印.青海小柴达木湖的旧石器//中国科学院中澳第四纪合作研究组//中国—澳大利亚第四纪学术讨论会论文集.北京:科学出版社,1987:168-175.]
[2]  BrantinghamPJ,GaoXing.PeoplingofthenorthernTibetanplateau.WorldArchaeology,2006,38(3):387-414.
[3]  CuiZhijiu,WuYongqiu,LiuGengnian.DiscoveryandenvironmentalsignificanceofneolithictraceinKunlunMountainsPassarea.ChineseScienceBulletin,1995,40(17):1451-1455.
[4]  ZhouDujun,MaHaizhou,BrantinghamPJetal.HumanactivitiesandlakeevolutioninthenorthQinghaisincelatePleistocene.JournalofSaltLakeResearch,2003,11(2):8-13.[周笃珺,马海州,BrantinghamPJ等.晚更新世以来青海北部的人类活动与湖泊演变.盐湖研究,2003,11(2):8-13.]
[5]  BaiYongshan,WangJinshou,ChangGehongetal.DiscoverytheancienthumanactivitiestraceintheQimantageregionofTibetanPlateau.GeologicalBulletinofChina,2003,22(5):369-370.[拜永山,王进寿,常革红等.青藏高原北部祁漫塔格地区发现古人类活动遗迹.地质通报,2003,22(5):369-370.]
[6]  BrantinghamPJ,GaoX,OlsenJWetal.AshortchronologyforthepeoplingoftheTibetanPlateau//MadsenDB,ChenFahu,GaoXing//LateQuaternaryClimateChangeandHumanAdaptationinAridChina(DevelopmentsinQuaternaryScience).Amsterdam:Elsevier,2007:129-150.
[7]  GaiPei,WangGuodao.ExcavationreportonaMesolithicsiteatLayihai,UpperYellowRiver.ActaAnthropologicaSinica,1983,2(1):49-59.[盖培,王国道.黄河上游拉乙亥中石器时代遗址发掘报告.人类学报,1983,2(1):49-59.]
[8]  GaoXing,ZhouZhenyu,GuanYing.HumanculturalremainsandadaptationstrategiesintheTibetanPlateaumarginregioninthelatePleistocene.QuaternarySciences,2008,28(6):970-977.[高星,周振宇,关莹.青藏高原边缘地区晚更新世人类遗存与生存模式.第四纪研究,2008,28(6):970-977.]
[9]  XieJunyi.NewdiscoveryandlookforwardonthePaleolithicinwestern-centerofGansuProvince.ActaAnthropologicaSinica,1991,10(1):27-33.[谢骏义.甘肃西部和中部旧石器考古的新发现及其展望.人类学报,1991,10(1):27-33.]
[10]  RhodeD,ZhangHaiying,DavidBMadsenetal.Epipaleolithic/earlyNeolithicsettlementsatQinghaiLake,westernChina.JournalofArchaeologicalScience,2007,34:600-612.
[11]  XieDuanju.Pre-historicalArchaeologyofGansuandQinghaiProvinces.Beijing:CulturalRelicsPress,2002.[谢端琚.甘青地区史前考古.北京:文物出版社,2002.]
[12]  ThompsonLG,YaoTandong,DavisMEetal.Tropicalclimateinstability:ThelastglacialcyclefromaQinghai-Tibetanicecore.Science,1997,276:1821-1825.
[13]  ShiYafeng,ZhaoJingdong.Thespecialwarm-humidclimateandenvironmentinChinaduring40-30kaBP:Discoveryandreview.JournalofGlaciologyandGeocryology,2009,31(1):1-10.[施雅风,赵井东.40~30kaBP中国特殊暖湿气候与环境的发现与研究过程的回顾.冰川冻土,2009,31(1):1-10.]
[14]  ShiYafeng,LiJijun,LiBingyuan.UpliftandEnvironmentChangesontheQinghai-XizangPlateauintheLateCenozoic.Guangzhou:GuangdongScienceandTechnologyPress,1998:422-431.[施雅风,李吉均,李炳元.青藏高原晚新生代隆升与环境变化.广州:广东科技出版社,1998:422-431.]
[15]  LoukasBarton,BrantinghamPJ,JiDuxue.LatePleistoceneclimatechangeandpaleolithicculturalevolutioninnorthernChina:Implicationsfromthelastglacialmaximum//MadsenDB,ChenFH,GaoX//LateQuaternaryclimatechangeandhumanadaptationinaridChina.Amsterdam.London:Elsevier,105-128.
[16]  TangLingyu,LiChunhai.Temporal-spatialdistributionoftheHolocenevegetationintheTibetanPlateau.JournalofGlaciologyandGeocryology,2001,23(4):367-374.[唐领余,李春海.青藏高原全新世植被的时空分布.冰川冻土,2001,23(4):367-374.]
[17]  WangJianlin,XiongWei.RelationshipbetweentheancientsmigrationclimatechangeinthelaterperiodoflatePleistoceneinTibet.ActaGeographicaSinica,2004,59(2):174-182.[王建林,熊伟,晚更新世以来西藏古人类迁移与气候变化关系,地理学报,2004,59(2):174-182.]
[18]  ShiYafeng,KongZhaochen,WangSuminetal.TheclimateandenvironmentofChinaMegathermalclimax.ScienceinChina:SeriesB,1993,23(8):865-873.
[19]  ZengYongnian,FengZhaodong,CaoGuangchao.DesertformationandevolutioninQaidambasinsincethelastglacialepoch.ActaGeographicaSinica,2003,58(3):452-457.[曾永年,冯兆东,曹广超.末次冰期以来柴达木盆地沙漠形成与演化.地理学报,2003,58(3):452-457.]
[20]  XuShuiying,ZhangWeixin,XuDefuetal.DiscussionontheperiglacialdevelopmentinthenortheastmarginalregionofQinghai-XizangPlateau.JournalofGlaciologyandGeocryology,1984,6(2):15-25.[徐叔鹰,张维信,徐德馥等.青藏高原东北边缘地区冰缘发展探讨.冰川冻土,1984,6(2):15-25.]
[21]  JiDuxue,ChenFahu,BettingeRLetal.HumanresponsetotheLastGlacialMaximum:EvidencefromnorthChina.ActaAnthropologicaSinica,2005,24(4):270-282.[吉笃学,陈发虎,BettingeRL等.末次盛冰期环境恶化对中国北方旧石器文化的影响.人类学学报,2005,24(4):270-282.]
[22]  XuShuying.ThepaleosolsandtheirreflectionoftheenvironmentalchangesinthenortheastregionoftheQinghai-XizangPlateau.ScientiaGeographicaSinica,1994,14(3):225-232.[徐叔鹰.青藏高原东北部的古土壤及其对环境变迁的反映.地理科学,1994,14(3):225-232.]
[23]  DuNaiqiu,KongZhaochen,ShanFashou.Apreliminaryinvestigationonthevegetioanlandclimaticchangesince11000yearsinQinghaiLake:AnanalysisbasedonpalynologyincoreQH85-14C.ActaBetanicaSinica,1989,31(10):803-814.[杜乃秋,孔昭宸,山发寿.青海湖QH85-14C钻孔抱粉分析及其古气候古环境的初步探讨.植物学报,1989,31(10):803-814.1994,14(3):225-232.]
[24]  DuShuisheng.StagediversionandareadivisionofNorthChinaOldStoneAgelatecultureandrelevantproblemsActaArchaeologicaSinica,2007,(2):127-152.[杜水生.中国北方旧石器时代晚期文化的分期分区及相关问题.考古学报,2007,(2):127-152.]
[25]  MadsenDB,MaHaizhou,BrantinghamPJetal.ThelateUpperPaleolithicoccupationofthenorthernTibetanPlateaumargin.JournalofArchaeologicalScience,2006,33(10):1433-1444.
[26]  NingxiaArchaeologicalInstitute.Shuidonggou:TheReportofExcavationin1980.Beijing:Sciencepress,2003:209-219.[宁夏文物考古研究所.水洞沟:1980发掘报告.北京:科学出版社,2003:209-219.]
[27]  StateAdministrationofCulturalHeritage.TheCultureRelicAtlasofChina:QinghaiBranch.Beijing:ChinaCartographicPublishingHouse,1996:15-23.[国家文物局.中国文物地图集·青海分册.北京:中国地图出版社,1996:15-23.]
[28]  ZhangZhiheng.PalaeolithicArchaeologyofChina.Nanjing:NanjingUniversityPress,2004.[张之恒.中国新石器时代考古.南京:南京大学出版社,2004.]
[29]  AnChengbang,WangLin,JiDuxueetal.ThetemporalandspatialchangesNeolithicculturesinGansu-Qinghairegionandpossibleenvironmentforcing.QuaternarySciences,2006,26(6):923-927.[安成邦,王琳,吉笃学等.甘青文化区新石器文化的时空变化和可能的环境动力.第四纪研究,2006,26(6):923-927.]
[30]  ChenHonghai,GeSangben,LiGuoling.DiscusstothenatureofZongrirelic.Archaeology,1998,(5):23-27.[陈洪海,格桑本,李国林.试论宗日遗址的文化性质.考古,1998,(5):23-27.]
[31]  LiuXingqi,ShenJi,WangSuminetal.A16000-yearpollenrecordandancientenvironmentevolution.ChineseScienceBulletin,2002,47(17):1351-1355.
[32]  WangYJ,ChengH,EdwardsRLetal.Ahigh-resolutionabsolute-datedLatePleistocenemonsoonRecordfromHuluCave,China.Science,2001,294(5550):2345-2348.
[33]  ChenKezao,BowlerJM.PreliminarystudyonsedimentarycharacteristicsandevolutionofpalaeoclimateofQarhansaltlakeinQaidamBasin.ScientiaSinica(SeriesB),1985(11):1218-1231.
[34]  WanHewen,TangLingyu,ZhangHucaietal.PollenrecordreflectsclimatechangesineasternQaidamBasinduring36-18kaBP.QuaternarySciences,2008,28(1):112-121.[万和文,唐领余,张虎才等.柴达木盆地东部36~18kaBP期间的孢粉记录及其气候环境.第四纪研究,2008,28(1):112-121.]
[35]  ShiYafeng,ZhengBenxing,YaoTandong.GlaciersandenvironmentsduringtheLastGlacialMaximumontheTibetanPlateau.JournalofGlaciologyandGeocryology,1997,19(2):97-113.[施雅风,郑本兴,姚檀栋.青藏高原末次冰期最盛时的冰川与环境.冰川冻土,1997,19(2):97-113.]

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