贵州草海湿地730ka来的环境变迁及草海未来的演化分析
详细信息   下载全文 | 推荐本文 |
摘要
本研究通过对草海湿地730 ka以来的气候、水域面积、植被等方面的研究,总结出草海湿地的生态环境演化规律。本研究认为草海盆地发育与环境演变的主要影响因素有地质构造作用、全球气候变迁和近代人类活动的影响三方面,且地质构造运动起控制作用。草海湿地现在处于第四纪间冰期,总的气候环境属于温湿气候,同时,其处于小气候旋回的干凉期末期,所以其总体上处于较差的自然生态环境。草海湿地在未来10 ka,其小气候旋回将从干凉期转变为温湿期,自然生态环境将会自然恢复,但要加强草海湿地生态保护,如减少人为取水、污水处理达标后排放等措施。草海湿地受到构造运动(青藏高原隆起)、全球气候变迁和近代人类活动影响,水域面积从600—700 ka BP期间的150km~2,减少到目前的20.98 km~2,草海湿地有不断向东南减小的趋势,它在几万年后有可能自然消失。
        On the basis of climatic change,distribution area and plant content of Caohai Lake,ecological environmental change of Caohai Lake,Guizhou Province from 730 ka to present was discussed in the paper.There were some conclusions that were showed as follows on this article.There are three main factors that influence the development and environmental evolution of the Caohai Lake basin,for instance,the geological tectonic movement effect,the global climate change and human beings activities in modern times;especially the tectonic movement is a main controlling factor.And then,climate belongs to Quaternary interval glacial epoch with warm and humid environment in present.At the same time,its climate is located at last epoch of second scale climate cycle(dry and cold climate).And the Caohai Lake's climate and ecology is generally odious in present,but the ecological environment of the Caohai Lake will return to well with climate changing from dry and cold to warm and humid after 10 ka.However,the ecological protection measures were put forward for the Caohai Lake,such as reducing artificial taken water and the domestic sewage and industrial wastewater treatment up to emission standard.Additionally,the Caohai Lake has been removing from west to east because of tectonic movement(such as the uplift of the Qinghai-Tibet Plateau),the global climate change and human beings activities.And distribution area of Caohai Lake has been reducing from 150 km~2 during 600—700 ka BP to 20.98 km~2 at present;there would have a slowly decreasing trend toward southeast in the distribution area of Caohai Lake as well.Therefore,the Caohai Lake would vanish on some day in the future.
引文
陈敬安,万国江,陈振楼,等.1999.洱海沉积物化学与古气候演化[J].地球化学,28(6):562-570.[Chen J A,Wan G J,Chen Z L,et al.1999.Chemical elements in sediments of Lake Erhai and palaeoclimate evolution[J].Geochimica,28(6):562-570.]
    陈佩英,林树基,周启永.1993.贵州草海地区赵家院子泥炭层剖面孢粉研究[J].贵州科学,11(3):31-39.[Chen P Y,Lin S J,Zhou Q Y.1993.Study of a peat-bed section near Zhaojiayuanzi in Caohai area,Guizhou[J].Guizhou Science,11(3):31-39.1
    陈佩英,周启承,林树基.1991.贵州威宁15000年来的古环境——南屯泥炭层剖面研究[J].贵州地质,8(2):141-154.[Chen P Y,Zhou Q C,Lin S J.1991.Palaeoenvironment from 15000 a.B.P.to the present in Weining County,Guizhou-A study of Nantun peat-bed section[J].Geology of Guizhou,8(2):141-154.]
    陈佩英.1987.贵州威宁草海CK17钻孔孢粉组合及古环境[J].贵州地质,4(3):381-388.[Chen P Y.1987.Palynological assemblages and palaeoenvironment of CK17 drilling hole in Caohai(Grassy Sea),Weining Country,Guizhou Province[J].Geology of Guizhou,4(3):381-388.]
    葛全胜,郑景云,满志敏,等.2002.过去2000a中国东部冬半年温度变化序列重建及初步分析[J].地学前缘,9(2):169-181.[Ge Q S,Zheng J Y,Man Z M,et al.2002.Reconstruction and analysis on the series of winter-half-year temperature changes over the past 2000years in eastern China[J].Earth Science Frontiers,9(2):169-181.]
    葛肖虹,任收麦,马立祥,等.2006.青藏高原多期次隆升的环境效应[J].地学前缘,13(6):118-130.[Ge X H,Ren S M,Ma L X,et al.2006.Multi-stage uplifts of the Qinghai-Tibet Plateau and their environmental effects[J].Earth Science Frontiers,13(6):118-130.]
    顾兆炎,刘嘉麒,袁宝印,等.1994.湖相自生沉积作用与环境——兼论西藏色林错沉积物记录[J].第四纪研究,14(2):162-174.[Gu Z Y,Liu J Q,Yuan B Y,et al.1994.Lacustrine authigenic deposition expressive of environment and the sediment record from siling co,Xizang(Tibet),China[J].Quaternary Sciences,14(2):162-174.]
    郭媛,林昌虎,何腾兵,等,2012.草海表层沉积物有机碳、氮、磷分布特征及污染评价[J].贵州科学,30(1):27-32.[Guo Y,Lin C H,He T B,et al.2012.The distribution characteristics and pollution evaluation of organic carbon,nitrogen and phosphate in surface sediments of Caohai Lake[J].Guizhou Science,30(1):27-32.]
    韩淑媞,袁玉江.1990a.新疆巴里坤湖35 000年来古气候变化序列[J].地理学报,45(3):350-362.[Han S T,Yuan Y J.1990a.The sequence of paleoclimatic variation of Balikun lake of Xinjiang in the part 35000 years[J].Acta Geographic Sinica,45(3):350-362.]
    韩淑媞,钟巍.1990b.新疆巴里坤湖ZK0024孔微量元素变化的古气候意义[J].地理科学,10(2):150-158.[Han S T,Zhong W.1990b.Palaeoclimate significance from trace elemnt variation in Barkol lake in Xinjiang[J].Scientia Geographica Sinica,10(2):150-158.]
    吉汝安.1992.贵州第四纪自然环境的演变[J].贵州地质,9(1):59-62.[Ji R A.1992.Evolution of Quaternary natural environment in Guizhou[J].Geology of Guizhou,9(1):59-62.]
    孔凡翠,杨瑞东,韩晓彤,等.2011a.贵州威宁窑上组沉积物物源特征及沉积控制因素分析[J].现代地质,25(3):464-475.[Kong F C,Yang R D,Han X D,et al.2011a.Analysis of sediment provenance and sedimentary control factors in Yaoshang Formation,Weining County in Guizhou Province[J].Geoscience,25(3):464-475.]
    孔凡翠,杨瑞东,林树基.2010.从威宁草海的演化分析0.73Ma来贵州威宁地区喀斯特环境的演变[J].地球与环境,38(2):138-145.[Kong F C,Yang R D,Lin S J.2010.Analysis of the evolution of karst environment of Weining Region,Guizhou Province,West China:A proof from the sediment evolution of lake Caohai since about 73 million years[J].Earth And Environment,38(2):138-145.]
    孔凡翠,杨瑞东,沙占江.2013.贵州草海赵家院子全新世泥炭层地球化学特征及其环境意义[J].地质论评,59(4):716-730.[Kong F C,Yang R D,Sha Z J.2013.Geochemical characteristics and sedimentary environment of the epipleistocene peat on Zhaojiayuanzi sediment column in Caohai basin,Guizhou Province[J].Geological Review,59(4):716-730.]
    孔凡翠,杨瑞东,魏怀瑞,等.2011b.贵州威宁草海第四系窑上组沉积物微量元素地球化学特征及其古环境意义[J].海洋地质与第四纪地质,31(5):117-126.[Kong F C,Yang R D,Wei H R,et al.2011b.Geochemistry of trace elements of the Quaternary sediments of Yaoshang Formation in Weining Country,Guizhou Province and its paleoenvironmental implications[J].Marine Geology And Quaternary Geology,31(5):117-126.]
    李吉均,方小敏.1988.青藏高原隆起与环境变化研究[J].科学通报,43(15):1569-1574.[Li J J,Fang X M.1988.Study on plateau uplift and environmental change[J].Chin Sci Bull,43(15):1569-1574.]
    李世杰,蔡德所,张宏亮,等.2009.桂林会仙岩溶湿地环境变化沉积记录的初步研究[J].广西师范大学学报(自然科学版),27(2):94-100.[Li S J,Cai D S,Zhang H L,et al.2009.Environmental changes record derived from sediment cores in Huixian Karst Wetlands,Guilin,China[J].Journal of Guangxi Normal University(Natural Science edition),27(2):94-100.]
    林瑞芬,卫克勤.2000.草海ZHJ柱样沉积物有机质的δ~(13)C记录及其古气候信息[J].地球化学,29(4):390-396.[Lin R F,Wei K Q.2000.Aδ~(13)C record of the organic matter in lacustrine sediments of the core ZHJ from Lake Caohai and its palaeoclimate implications[J].Geochemica,29(4):390-396.]
    林树基,刘爱民.1985.中新生代板块活动与贵州地貌之演化[J].贵州地质,2(2):123-130.[Lin S J,Liu A M.1985.Plate activities and evolution of Guizhou geomorphy in Mesozoic-Cenozoic[J].Geology of Guizhou,2(2):123-130.]
    林树基,郑洪汉.1987.草海的演化[M].贵阳:贵州人民出版社.[Lin S J,Zheng H H.1987.Evolution of Caohai[M].Guiyang:Guizhou People's Publishing House.]
    林树基,周启永,陈佩英.1990.贵州晚新生代冰期划分与古冰川问题[J].贵州地质,7(2):115-124.[Lin S J,Zhou Q Y,Chen P Y.1990.Glacial period divisions and palaeoglacial problems of late Cenozoic age in Guizhou[J].Geology of Guizhou,7(2):115-124.]
    刘凤英.2005.草海湿地生态系统影响因素分析[J].贵州环保科技,11(4):34-37.[Liu P Y.2005.Ansysis on Caohai wetland ecosystem influing factors[J],Environmental Protection and Technology,11(4):34-37.]
    刘平贵,范淑贤,李雪菊.2000.银川盆地第四纪地球化学元素特征及沉积环境[J].地质力学学报,6(4):43-50,94.[Liu P G,Fan S X,Li X J.2000.The geochemical element characteristics and paleosedimentary enviroment of the Quaternary deposits in Yinchuan basin[J].Journal of Geomechanics,6(4):43-50,94.]
    刘晓东,Dong Buwen.2013.青藏高原隆升对亚洲季风-干旱环境演化的影响[J].科学通报,58(28-29):2906-2919.[Liu X D,Dong B W.2013.Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution[J].Chinese Science Bulletin,58:4277-4291.]
    彭益书,付培,杨瑞东.2014.草海湿地生态系统健康评价[J].地球与环境,42(1):68-81.[Peng Y S,Fu P,Yang RD.2014.Assessment of wetland ecosystem health in Caohai lake of Guizhou Province[J].Earth And Environment,42(1):68-81.]
    齐建文,李矿明,黎育成,等.2012.贵州草海湿地现状与生态恢复对策[J].中南林业调查规划,31(2):39-40,56.[Qi J W,Li K M,Li Y C,et al.2012.Restoration strategies of Caohai wetland in Guizhou Province[J].Central South Forest Inventory And Planning,31(2):39-40,56.]
    史继扬,向明菊,林树基,等.1993.草海盆地、柴窝堡湖沉积物中甾醇类的分布特征及其地球化学意义[J].地球化学,(2):179-186.[Shi J Y,Xiang M J,Lin S J,et al.1993.Distribution characteristics of sterols in Chaiwobu lake sediments of the Caohai basin and their geochemical signification[J].Geochemica,(2):179-186.]
    陶发祥,洪业汤,姜洪波.1996.贵州草海地区最近8 ka的气候变化[J].科学通报,(16):1489-1492.[Tao F X,Hong Y T,Jiang H B.1996.The recently 8 ka climate change in Caohai,Guiahou Province[J].Chin Sci Bull,(16):1489-1492.]
    王俊达,李华梅,林树基,等.1986.贵州草海沉积物的古地磁地层学初步研究[J].地球化学,(4):329-335.[Wang J D,Li H M,Lin S J,et al.1986.A primary paleomagnetic stratigraphic study of Caohai lake sediments from Guizhou Province[J].Geochemica,(4):329-335.]
    王克勇.1987.贵州草海第四纪介形类及其古环境[J].贵州地质,4(1):49-59.[Wang K Y.1987.Quaternary ostracoda and its palaeoenvironment in Caohai,Guizhou Province[J].Geology of Guizhou.4(1):49-57.]
    王苏民,窦鸿身.1998.中国湖泊志[M].北京:科学出版社,1-27.[Wang SM,DuHS.1998.The Journal of lake in China[M].Beijing:Science Press,1-27.]
    王苏民,刘健,周静.2003.我国小冰期盛期的气候环境[J].湖泊科学,15(4):369-376.[Wang S M,Liu J,Zhou J.2003.The climate of little Ice Age Maximum in China[J],Journal of Lake Sciences,15(4):369-376.]
    吴永红.2012.长江三角洲与贵州草海地区全新世环境变化对比研究[D].华东师范大学.[Wu Y H.2012.Comparative study on Holocene environmental change of Yangtze River Delta and Caohai in Cuizhou[D].East China Normal University.]
    于俊伟,赵广忠,田英.1991.威宁草海水体变化的气候效应[J].贵州科学,9(1):40-47.[Yu J W Zhao G Z,Tian Y.1991.The climatic effects of variation of the water body in Caohai,Weining[J].Guizhou Science,9(1):40-47.]
    余素华,文启忠.1995.试论青藏高原第四纪沉积地球化学演化与环境变迁[J].海洋地质与第四纪地质,15(4):97-106.[Yu S H,Wen Q Z.1995.Geochemical evolution and environment changes since Quaternary in Qingzang(Qinghai-Tibet)Plateau[J].Marine Geology And Quaternary Geology,15(4):97-106.]
    张乃娴,万国江,马玉光.2000.威宁草海沉积物中的粘土矿物及其环境记录[J].地质科学,35(2):206-211.[Zhang N X,Wan G J,Ma Y G.2000.The clay mineral and its environmental record in the sediment core of Caohai,Weining[J].Scientia Geologica Sinica,35(2):206-211.]
    张清海,李明晶,姚松林.2007.草海研究[M].贵阳:贵州科技出版社,1-293.[Zhang H H,Li M J,Yao S L.2007.Research in Caohai[M].Guiyang:Guizhou Scientific Press,1-293.]
    周启永,陈佩英.1989.沉积物中冷水碳酸盐的古气候意义——以贵州草海两个钻孔剖面为例[J].贵州地质,6(4):347-356.[Zhou Q Y,Chen P Y.1989.The palaeoclimate implication of the cold-water carbonate in sediments in two drilled hole sections of Caohai[J].Geology of Guizhou,6(4):347-356.]
    朱正杰,陈敬安,曾艳.2014.草海地区过去500年来古温度重建:来自沉积物纤维素结合碳酸盐氧同位素的证据[J].中国科学:地球科学,44(2):250-258.[Zhu Z J,Chen J A,Zeng Y.2014.Paleotemperature variations at Lake Caohai,southwestern China,during the past 500years:Evidence from combinedδ~(18)O analysis of cellulose and carbonates[J].Science China:Earth Sciences,doi:10.1007/s11430-014-4831-6]
    朱正杰,陈敬安,李航,等.2011.贵州草海沉积物碳酸盐碳同位素异常正值的发现及其环境指示意义[J].湖泊科学,23(5):681-685.[Zhu Z J,Chen J A,Li H,et al.2011.Discovery of abnormal positive values of carbon isotope of carbonate sediments from Lake Caohai,Guizhou Province and their implications[J].Journal of Lake Sciences,23(5):681-685.]
    朱正杰,莫建兵,张维,等.2010.贵州草海沉积物纤维素氧同位素研究及其古环境意义[J].地球与环境,38(1):8-13.[Zhu Z J,Mo J B,Zhang W,et al.2010.Oxygen isotopic composition of cellulose in sediments from Lake Caohai,and its paleoenvironmental implications[J].Earth And Environment,38(1):8-13.]
    竺可桢.1973.中国近五千年来气候变迁的初步研究[J].中国科学,(2):168-189.[Lan K Z.1973.A preliminary study on climate change in China in recently 5000 years[J].Scientia Sinica,(2):168-189.]
    Atkinson T C,Briffa K R,Coope G R.1987.Seasonal temperatures in Britain during the past 22,000 years,reconstructed using beetle remains[J].Nature,325:581-92.
    Chambers,F.M.and Charman D.J.2004.Holocene environmental change:contributions from the peatland archive[J].Holocene,14(1):1-10.
    Chawchai S,Chabangborn A,Kylander M,et al.2013.Lake Kumphawapi-an archive of Holocene palaeoenvironmental and palaeoclimatic changes in northeast Thailand[J].Quaternary Science Reviews,68:59-75.
    Clague J J,Wohfarth B,Ayotte J,et al.2004.Late Holocene environmental change at treeline in the northern Coast Mountains,British Columbia,Canada[J].Quaternary Science Reviews,(23):2413-2431.
    Gasse F,Anold M,Fontes J C,et al.1991.A 13000 year climate record from Western Tibet[J].Nature,353(24):742-745.
    Grygar T,Kadlec J,Pruner P,et al.2006.Paleoenvironmental record in Lake Baikal sediments:environmental changes in the last 160 ky[J].Palaeogeography,Palaeoclimatology,Palaeoecology,237(2-4):240-254.
    Jin Z D,Wang S M,Shen J,et al.2001.Chemical Weathering since the Little Ice Age Record in Lake Sediments:A High-resolution Proxy of past Climate[J].Earth Surface Processes and Landforms,26:775-782.
    Jin Z D,Yu J M,Wang S M,et al.2009.Constraints on water chemistry by chemical weathering in the Lake Qinghai catchment,northeastern Tibetan Plateau(China):clues from Sr and its isotopic geochemistry[J].Hydrogeology Journal,17(8):2037-2048.
    Last W M,Smol J P.2001.Tracking environmental change using lake sediments Volume 1:Basin Analysis,Coring,and Chronological Techniques[M].Dordrecht,The Netherlands:Kluwer,1-599.
    Lerman A.1987.Lake:chemistry,geology,physics[M].Springer:Verlag Berlin Heidelberg,1-366.
    Lister G S,Kelts K,Chen K Z,et al.1991.Lake Qinghai China:closed-basin lake levels and the oxygen isotope record for ostracoda since the last Pleistocene[J].Palaeogeogr Palaeoclimatol Palaeoecol,84:141-162.
    Shen D F,Li S J.2013.Environment change of Sihu Lake in the past 450 years,southern China[J].Environmental Earth Sciences,70(7):2953-2962.
    Smol J.2002.Pollution of lakes and rivers:a paleoenvironmental perspective[M].Arnold,London:1-280.
    Wan G J,Bai Z G,Qing H,et al.2003.Geochemical records in recent sediments of Lake Erhai:implications for environmental changes in a low latitude-high altitude lake in southwest China[J].Journal of Asian Earth Sciences,21:489-502.
    Wohlfarth B,Hannon G,Feurdean A,et al.2001.Reconstruction of climatic and environmental changes in NW Romania duringthe early part of the last deglaciation(15,000-13,600 cal yr BP)[J].Quaternary Science Reviews,20:1897-1914.
    Wohlfarth B,Klubseang W,Inthongkaew S,et al.2012.Holocene environmental changes in northeast Thailand as reconstructed from a tropical wetland[J].Global and Planetary Change,92-93:148-161.
    Wohlfarth B,Lacourse T,Bennike O,et al.2007.Climatic and environmental changes in north-western Russia between15000 and 8000 cal yr BP:a review[J].Quaternary Science Reviews,(13-14):1871-1883.
    Wu L,Li F,Zhu C,et al.2012.Holocene environmental change and archaeology,Yangtze River Valley,China:Review and prospects[J].Geoscience Frontiers,3(6):875-892.
    Yu S Y,Clolmn S M,Lowell T V,et al.2010.Freshwater outbust from Lake Superior as a trigger for the cold event9300 years ago[J].Science,328(4):1262-1266.
    Zhu Z J,Chen J A,Zeng Y.2013.Abnormal positiveδ~(13)C values of carbonate in Lake Caohai,southwest China,and their possible relation to lower temperature[J].Quaternary International,286:85-93.
目录

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700