全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
湖泊科学  2012 

13.8ka以来内蒙古吉兰泰盐湖的演化过程

DOI: 10.18307/2012.0418

Keywords: 吉兰泰盐湖,矿物组成,演化过程

Full-Text   Cite this paper   Add to My Lib

Abstract:

通过系统分析吉兰泰盐湖JLT-2010孔蒸发盐类矿物、碳酸盐矿物、碎屑岩矿物等,结合AMS14C测年获得的年代序列,研究该湖13.8ka以来的演化过程.结果表明:吉兰泰盐湖13.8-11.7calkaBP期间水体较淡;11.7-10.2calkaBP期间湖泊开始萎缩、咸化,进入咸水湖阶段;10.2-5.5calkaBP期间湖泊进入硫酸盐沉积阶段,其中9.0-8.2calkaBP经历了一个明显的淡化过程;5.5calkaBP以来,湖泊成盐作用进一步加强,由前期的硫酸盐沉积转变为氯化物沉积,其中3.7-2.0calkaBP达到全面氯化物沉积阶段,2.0-1.7calkaBP又经历了一个短暂而明显的淡化过程;目前,该盐湖已进入干盐湖发展阶段.总体而言,吉兰泰盐湖蒸发盐类矿物主要是在全新世增温的背景条件下逐步萎缩形成的,由于区域性干旱气候的持续影响,吉兰泰盐湖逐步萎缩、咸化,进而析盐.

References

[1]  郑绵平. 论盐湖学. 地球学报,1999,20(4):395-401.
[2]  Zheng MP,Meng YF,Wei LJ. Evidence of the pan-lake stage in the period of 40-28 ka BP on the Qinghai-Tibet Plateau. Acta Geologica Scinca,2000,74(2):266-272.
[3]  Smith GI. Subsurface stratigraphy and geochemistry of late Quaternary evaporates,Searles Lake,California,U. S. Geol Surv Prof Pap,1979,1043:130.
[4]  Spencer RJ,Eugster HP,Jones BF. Geochemistry of Great Salt Lake,Utah. Ⅱ:Pleistocene-Holocene evolution. Geochim Cosmochim Acta,1985,49:739-747.
[5]  Bowler JM,Huang Q,Chen KZ et al. Radiocarbon dating of Playa-Lake hydrologic changes:Examples from Northwestern China and central Australia. Palaeogeogr,Palaeoclimatol,Palaeoecol,1986,54:241-260.
[6]  Last WM,Slezak LA. The salt lakes of western Canada:a paleolimnological overview. Hydrobiol,1988,158:301-316.
[7]  张彭熹,张保珍. 柴达木地区近三百万年来古气候环境演化的初步研究. 地理学报,1991,46(3):326-335.
[8]  刘兴起,王永波,沈吉等. 16000 a 以来青海茶卡盐湖的演化过程及其对气候的响应. 地质学报,2007,(6):843-849.
[9]  更多...
[10]  魏乐军,郑绵平,刘喜方等. 西藏洞错硼砂芒硝层的发现及其古气候意义. 地质学报,2002,76(2):261-271.
[11]  魏乐军,郑绵平,马志邦. 西藏台错盐湖TT-1剖面的沉积特征和年代学研究. 地球学报,2004,23(4):1-10.
[12]  耿侃,陈育峰. 吉兰泰盐湖的形成、发育和演化. 地理学报,1990,45(3):341-349.
[13]  春喜. 晚第四纪吉兰泰盐湖古湖面与环境变化研究[学位论文]. 兰州:兰州大学,2006.
[14]  于松升,白福易,李浩基. 吉兰泰盐湖资源环境与可持续发展研究. 北京:科学出版社,2001:21-47.
[15]  Chung FH. Quantitative interpretation of X-ray diffraction patterns of mixtures. Ⅱ. Adiabatic principle of X-ray diffraction analysis of mixtures. Journal of Applied Crystallography,1974,7:526-531.
[16]  Jin ZD,Wu YH,Zhang XH et al. Role of late glacial to mid-Holocene climate in catchment weathering in the central Tibetan Plateau. Quaternary Research,2005,63(2):161-170.
[17]  Gasse F,Arnold M,Fontes JC et al. A 13,000-year climate record from western Tibet. Nature,1991,353:742-745.
[18]  Gasse F,Fontes JC,Campo EV et al. Holocene environmental changes in Bangong Co basin (Western Tibet):4. Discussions and conclusions. Palaeogeography,Palaeoclimatology,Palaeoecology,1996,120:79-92.
[19]  施雅风,孔昭哀,王苏民等. 中国全新世大暖期的气候与环境的基本特征. 见:施雅风编. 中国全新世大暖期气候与环境. 北京:海洋出版社,1992:1-19.
[20]  Shi YF,Kong ZC,Wang SM et al. Climates and environments of the Holocene Megathermal Maximum in China. Science in China:B,1994,37(4):482-493.
[21]  吴锡浩,安芷生,王苏民等. 中国全新世气候适宜期东亚夏季风时空变迁. 第四纪研究,1994,24(1):24-37.
[22]  秦伯强,施雅风,于革. 亚洲内陆湖泊在18ka BP 和6ka BP 的水位变化及其指示意义. 科学通报,1997,42(24):2586-2590.
[23]  Jia YL,Shi YE,Wang SM et al. Lake expending events in the Tibetan Plateau since 40 ka BP. Science in China:D, 2001,44(Suppl.):301-314.
[24]  于革,赖格英,刘健等. MIS3晚期典型阶段气候模拟的初步研究. 第四纪研究,2003,23(1):12-24.
[25]  Tarasov PE,Harrison SP. Lake status records from the former Soviet Union and Mongolia:a continental-scale synthesis. Palaeoklimaforschung,1998,25:115-130.
[26]  Grunert J,Lehmkuhlb K,Walther M. Paleoclimatic evolution of the Uvs Nuur basin and adjacent areas (Western Mongolia). Quaternary International,2000,65/66:171-192.
[27]  陈发虎,朱艳,李吉均等. 民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化. 科学通报,2001,46(17):1414-1419.
[28]  陈发虎,吴薇,朱艳等. 阿拉善高原中全新世干旱事件的湖泊记录研究. 科学通报,2004,49(1):1-9.
[29]  Chen FH,Shi Q,Wang JM. Environmental changes docmuenetd by sedimentation of Lake Yiema in arid China since the Late Glaciation. Journal of Paleolimnology,1999,22:159-169.
[30]  Chen FH,Wu W,Holmes JA et al. A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia,China. Chinese Science Bulletin,2003,48(14):1401-1410.
[31]  Sirocko F,Sarntheim M,Erlenkeuser H et al. Century-scale events in monsoonal climate over the past 24,000 years. Nature, 1993,364:322-324.
[32]  曹建廷,王苏民,沈吉等. 近千年来内蒙古岱海气候环境演变的湖泊沉积记录. 地理科学,2000,20(5):391-396.
[33]  王苏民,冯敏. 内蒙古岱海湖泊环境变化与东南季风强弱变化的关系. 中国科学:B 辑,1991,21(7):759-768.
[34]  郑绵平. 盐湖学的研究与展望. 地质评论,2006,52(6):737-746.
[35]  郑绵平,向军,魏新俊等. 青藏高原盐湖. 北京:科学技术出版社,1989:1-431.
[36]  郑绵平,赵元艺,刘俊英. 第四纪盐湖沉积与古气候. 第四纪研究,1998,(4):297-307.
[37]  胡东升,张华京,李炳元等. 青藏高原腹地湖泊沉积序列与古气候变化. 地质学报,2000,74(4):363-370.
[38]  Torgersen T,De deckker P,Chivas AR et al. Salt lakes:a discussion of processes influencing palaeoenvironmental interpretation and recommendations for future study. Palaeogeogr,Palaeoclimatol,Palaeoecol,1986,54:7-9.
[39]  中国科学院盐湖研究所. 青海柴达木盆地晚新生代地质环境演化. 北京:科学出版社,1986:1-156.
[40]  黄麒,陈克造. 七十三万年来柴达木盆地察尔汗盐湖古气候波动的形式. 第四纪研究,1990,3:205-212.
[41]  魏新俊,姜继学. 柴达木盆地第四纪盐湖演化. 地质学报,1993,67(3):255-265.
[42]  Liu XQ,Dong HL,Jason AR et al. Evolution of Chaka Salt Lake in NW China in response to climatic change during the Latest Pleistocene-Holocene. Quaternary Science Reviews,2008,27(7/8):867-879.
[43]  齐文,郑绵平. 西藏扎布耶湖ZK91-2钻孔沉积特征与气候环境演化. 湖泊科学,1995,7(2):133-140.
[44]  魏东岩,陈延成,王鉴津等. 内蒙古伊克昭盟盐湖最近23 ka 古气候波动模式的研究. 化工矿产地质,1995,17(4):239-247.
[45]  陈延成,魏东岩,王鉴津等. 内蒙古伊古昭盟盐湖晚第四纪氧碳同位素记录及古气候研究. 化工矿产地质,1995, 17(4):229-238.
[46]  江德昕,魏俊. 内蒙古查干诺尔盐湖晚更新世至全新世孢粉植物与古气候. 沉积学报(增刊),1997,A12:147-152.
[47]  春喜,王宗礼,夏敦胜等. 吉兰泰盐湖的形成及指示的环境意义. 盐湖研究,2008,(3):11-18.
[48]  耿侃,胡春元,刘佳. 吉兰泰地区第四纪湖泊的演变. 干旱区资源与环境,1989,3(2):26-33.
[49]  郑喜玉. 内蒙古盐湖. 北京:科学出版社,1992:95-210.
[50]  胡春元. 试论吉兰泰盐湖的发育与资源保护问题. 内蒙古林学院学报:自然科学版,1998,20(2):54-59.
[51]  庞西磊,胡东生. 近22 ka 以来吉兰泰盐湖的环境变化及成盐过程. 中国沙漠,2009,(2):193-199.
[52]  郑喜玉,张明刚,徐旭等. 中国盐湖志. 北京:科学出版社,2002:371-374.
[53]  Morrill C,Jonathan TO,Julia EC et al. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet. Quaternary Research,2006,65(2):232-243.
[54]  Shen J,Liu XQ,Wang SM et al. Palaeoclimatic changes in the Qinghai Lake area during the last 18000 years. Quaternary International,2005,136:131-140.
[55]  Yang XP,Ma NN,Dong JF et al. Recharge to the interdune lakes and Holocene climatic changes in the Badain Jaran Desert, Western China. Quaternary Research,2010,73:10-19.
[56]  Liu XQ,Shen J,Wang SM et al. A 16000-year pollen record of Qinghai Lake and its paleoclimate and paleoenvironment. Chinese Science Bulletin,2002,47(22):1931-1937.
[57]  耿侃,张振春. 内蒙古大贵诺尔全新世湖群地貌特征及其演化. 北京师范大学学报:自然科学版,1988,18(4):94-101.
[58]  顾兆炎,刘嘉麒,袁宝印等. 12000年来青藏高原季风变化——色林错沉积物地球化学证据. 科学通报,1993,38(1):61-64.
[59]  Kashiwaya K,Masuzawa T,Morinaga H et al. Changes in hydrological conditions in the central Qing-Zang (Tibetan) Plateau inferred from lake bottom sediments. Earth and Planetary Science Letters,1995,135:31-39.
[60]  Campo EV,Gasse F. Pollen and diatom inferred climatic and hydrological changes in Sunmxi Co Basion(Western Tibet) since 13, 000 yr B. P. Quaternary Research,1993,39:300-313.
[61]  Feng ZD,Wang WG,Guo LL et al. Lacustrine and eolian records of Holocene climate changes in the Mongolian Plateau:preliminary results. Quaternary International,2005,136:25-32.
[62]  于革,薛滨,刘健等. 中国湖泊演变与古气候动力学研究. 北京:气象出版社,2001:42-178.
[63]  Harrison SP,Yu G,Tarasov PE. Late Quaternary lake-level record from northern Eurasia. Quaternary Research,1996, 45:138-159.
[64]  Overpeck J,Anderson D,Trumbore S et al. The southwest Indian Monsoon over the last 18,000 years. Climate Dynamics, 1996,12:213-225.
[65]  Herzschuh U. Palaeo-moisture evolution in monsoonal Central Asia during the last 50, 000 years. Quaternary Science Reviews, 2006,25:163-178.

Full-Text

comments powered by Disqus

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133

WeChat 1538708413