地理科学进展 ›› 2014, Vol. 33 ›› Issue (6): 786-798.doi: 10.11820/dlkxjz.2014.06.007
郭超, 马玉贞, 胡彩莉, 伍永秋, 鲁瑞洁
收稿日期:
2013-12-01
修回日期:
2014-04-01
出版日期:
2014-06-25
发布日期:
2014-06-25
作者简介:
郭超(1988- ),陕西西安人,硕士生,主要研究方向为环境演变,E-mail:gc@mail.bnu.edu.cn。
基金资助:
GUO Chao, MAYuzhen, HU Caili, WU Yongqiu, LU Ruijie
Received:
2013-12-01
Revised:
2014-04-01
Online:
2014-06-25
Published:
2014-06-25
摘要: 湖泊沉积记录的环境演变是全球变化的重要研究领域之一,通过对中国内陆区中30 个湖泊研究成果的总结和梳理,探讨了全新世以来该地区干湿变化的规律和区域分异。通过降水量结合传统分区方法将中国内陆区分为西北干旱区、东亚季风边缘区和青藏高原区。对每个湖泊样点以500 年为时间间隔,以孢粉为主要干湿指标,综合氧同位素、有机质及碳酸盐等,将湖泊干湿状况划分3 个干湿等级(干旱,半湿润,湿润),建立区域干湿指数。结果表明,中国内陆不同区域全新世可能经历了不同的干湿变化过程:①西北干旱区基本上是早中全新世干旱,中晚全新世相对湿润,但区域差异明显;②东亚季风边缘区早全新世早期干旱,早全新世晚期和中全新世相对湿润,晚全新世干旱;③青藏高原区的湿润时期主要发生在早中全新世,但是不同地区有所不同。对比分析显示:西北干旱区的干湿变化可能受西风环流控制,但在时间和强度上区域内部差异较明显;东亚季风边缘区可能主要受东亚季风控制;青藏高原地区早中全新世的湿润可能与印度季风的增强相关。
中图分类号:
郭超, 马玉贞, 胡彩莉, 伍永秋, 鲁瑞洁. 中国内陆区湖泊沉积所反映的全新世干湿变化[J]. 地理科学进展, 2014, 33(6): 786-798.
GUO Chao, MAYuzhen, HU Caili, WU Yongqiu, LU Ruijie. Holocene humidity changes in inland China inferred from lake sediments[J]. PROGRESS IN GEOGRAPHY, 2014, 33(6): 786-798.
陈发虎, 黄小忠, 杨美临, 等. 2006. 亚洲中部干旱区全新世气候变化的西风模式: 以新疆博斯腾湖记录为例. 第四纪研究, 26(6): 881-887. [Chen F H, Huang X Z, Yang M L, et al. 2006. Westerly dominated Holocene climate model in arid central Asia: case study on Bosten Lake, Xinjiang, China. Quaternary Sciences, 26(6): 881-887.]高尚玉, 王贵勇, 哈斯, 等. 2001. 末次冰期以来中国季风区西北边缘沙漠演化研究. 第四纪研究, 21(1): 66-71. [Gao S Y, Wang G Y Ha S, et al. 2001. A case study on desert evolution in the northwestern fringe of monsoon area China since the last glacial epoch. Quaternary Sciences, 21(1): 66-71.]郭正堂, Petit-Maire N, 刘东生. 1999. 全新世期间亚洲和非洲旱区环境的短尺度变化. 古地理学报, 1(1): 68-74. [Guo Z T, N. Petit-Maire, Liu D S.1999. Holocene abrupt environmental changes in the arid regions in Africa and Asia. Journal of Palaeogeography, 1(1):68-74.]顾兆炎, 刘嘉麒, 袁宝印, 等. 1993. 12000 年来青藏高原季风变化: 色林错沉积物地球化学的证据. 科学通报, 38(1): 6l-64. [Gu Z Y, Liu J Q, Yuan B Y, et al. 1993. The evolution of the Qinghai-Xizang Plateau monsoon: evidence from the geochemistry of the sediments in Seling Co Lake. Chinese Science Bulletin, 38 (1): 61-64.]贾佳, 夏敦胜, 魏海涛, 等. 2009. 耀县黄土记录的全新世东亚冬夏季风非同步演化. 第四纪研究, 29(5): 966-975. [Jia J, Xia D S,Wei H T, et al. 2009. Asynchronous evolution of East Asia summer and winter monsoons of the Holocene recorded by Yao County loess. Quaternary Sciences, 29(5): 966-975.]蒋庆丰, 季峻峰, 沈吉, 等. 2013. 赛里木湖孢粉记录的亚洲内陆西风区全新世植被与气候变化. 中国科学: D 辑, 43(2): 243-255. [Jiang Q F, Ji J F, Shen J, et al. 2013. Holocene vegetational and climatic variation in westerlydominated areas of Central Asia inferred from the Sayram Lake in northern Xinjiang, China. Science China: series D, 56: 339-353.]李吉均. 1990. 中国西北地区晚更新世以来环境变迁模式. 第四纪研究, (3): 197-204. [Li J J. 1990. The patterns of environmental change since Late Pleistocene in northwestern China. Quaternary Sciences, (3): 197-204. ]刘林敬, 杨振京, 赵华, 等. 2012. 黄土高原平凉地区中全新世以来的植硅体记录与古气候研究. 地理与地理信息科学, 28(2): 104-107. [Liu L J, Yang Z J, Zhao H, et al. 2012. Holocene phytolith record and paleoclimate research in pingliang of the Loess Plateau. Geography and Geo-Information Science, 28(2): 104-107.]刘兴起, 沈吉, 王苏民, 等. 2006. 晚冰期以来青海湖地区气候变迁受西南季风控制的介形类壳体氧同位素证据. 科学通报, 51(22): 2690-2694. [Liu X Q, Shen J, Wang S M, et al. 2006. An oxygen isotopic evidence form class shell of Qinghai lake area climate change controlled by the southwest monsoon since the late glacial. Chinese Science Bulletin, 51(22): 2690-2694.]刘浴辉, 孙霞, 郭彩青. 2013. 中国全新世4.2 ka BP 气候事件及其对古文明的影响. 地质科技情报, 32(1): 99-106. [Liu Y H, Sun X, Guo C Q. 2013. Records of 4.2 ka BP Holocene event from China and its impact on Ancient Civilizations. Geological Science and Technology Information. 32(1): 99-106.]邵晓华, 汪永进, 程海, 等. 2006. 全新世季风气候演化与干旱事件的湖北神农架石笋记录. 科学通报, 51(1): 80-86. [Shao X H, Wang Y J, Cheng H, et al. 2006. Longterm trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China. Chinese Science Bulletin, 51 (2): 221-228.]沈吉, 刘兴起, Matsumoto R, 等. 2004. 晚冰期以来青海湖沉积物多指标高分辨率的古气候演化. 中国科学: D 辑, 34(6): 582-589. [Shen J, Liu X Q, Matsumoto R, et al. 2004. A high resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake. Science China: Series D, 48(6): 742-751.]史正涛. 1996. 中国季风边缘带自然灾害的区域特征. 干旱区资源与环境, 10(4): 1-7. [Shi Z T. 1996. Regional characters of natural disaster in marginal monsoon belt of china. Journal of Arid Land Resources and Environment, 10 (4): 1-7.]宋长青, 王琫瑜, 孙湘君. 1996. 内蒙古大青山DJ 钻孔全新世古植被变化指示. 植物学报, 38(7): 568-575. [Song C Q, Wang B Y, Sun X J. 1996. Implication of paleovegetational changes in Diaojiao Lake, Inner Mongolia. Acta Botanica Sinica, 38(7): 568-575.]孙千里, 肖举乐. 2006. 岱海沉积记录的季风/干旱过渡区全新世适宜期特征. 第四纪研究, 26(5): 781-790. [Sun Q L, Xiao J L. 2006. Characteristics of the Holocene optimum in the monsoon/arid transition belt recorded by core sediments of Daihai Lake, North China. Quaternary Sciences, 26(5): 781-790.]王可丽, 江灏, 赵红岩. 2005. 西风带与季风对中国西北地区的水汽输送. 水科学进展, 16(3): 432-438 [Wang K L, Jiang H,Zhao H Y. 2005. Atmospheric water vapor transport from westerly and monsoon over the Northwest China. Advance inWater Science, 16(3): 432-438.]吴艳宏, Andreas L, Bernd W, 等. 2007. 青藏高原中部全新世气候变化的湖泊沉积地球化学记录. 中国科学: D 辑, 37(9): 1185-1191. [Wu Y H, Andreas L, Bernd W, et al. 2007. Holocene climate change of lakes sedimentary geochemical records in central Tibet Plateau. Science in China: series D, 37(9): 1185-1191.]徐袁, 钱维宏. 2003. 东亚季风边缘活动带研究综述. 地理学报, 58(7S): 1-9. [Xu Y, Qian W H. 2003. Review of East Asian monsoon margin region. Acta Geographica Sinica 58(7S): 1-9.]薛积彬, 钟巍. 2008. 新疆巴里坤湖全新世环境记录及区域对比研究. 第四纪研究, 28(4): 610-620. [Xue J B, Zhong W. 2008. Holocene climate chance record by lacustrine sediments in Barkol lake and its regional comparison. Quaternary Sciences, 28(4): 610-620.]杨肖肖, 孔昭宸, 姜文英, 等. 2012. 末次盛冰期以来渭源黄土剖面的孢粉记录. 地球环境学报, 3(2): 813-819. [Yang X X, Kong H C, Jiang W Y, et al. 2012. Pollen record for the Weiyuan loess sections since the Last Glacial Maximum. Journal of Earth Environment, 3(2): 813-819.]姚檀栋, 施雅风, Thompson L G. 1992. 祁连山敦德冰芯记录的全新世气候变化//施雅风, 孔昭宸. 中国全新世大暖期气候与环境. 北京: 海洋出版社: 206-211. [Yao T D, Shi Y F, Thompson L G. 1992. Holocene climate change recorded by ice core of Qilian mountain//Shi Y F, Kong Z C. Holocene warm period climate and environment in China. Beijing, China: Maritime Press: 206-211.]游海涛, 刘嘉麒. 2012. 14 ka BP 以来二龙湾玛珥湖沉积物记录的高分辨率气候演变. 科学通报, 57(24): 2322-2329. [You H T, Liu J Q. 2012. High-resolution climate evolution derived from the sediment records of Erlongwan Maar Lake since 14 ka BP. Chinese Science Bulletin, 57(24): 2322-2329.]张振克,王苏民. 1999. 中国湖泊沉积记录的环境演变: 研究进展与展望. 地球科学进展,14(4): 417-422. [Zhang Z K, Wang S M. 1999. Advance and prospects of lake sediments and environmental changes study in China. Advance in Earth Sciences, 14(4): 417-422.]周爱锋, 孙惠玲, 陈发虎, 等. 2010. 黄土高原六盘山天池记录的中晚全新世高分辨率气候变化及其意义. 科学通报, 55(22): 2263-2266. [Zhou A F, Sun H L, Chen F H, et al. 2010. High resolution climate change in mid-late Holocene on Tianchi Lake, Liupan Mountain in the Loess Plateau in central China and its significance. Chinese Sci Bull, 55(22): 2263-2266.]周卫建, 李小强, 董光荣, 等. 1996. 新仙女木期沙漠/黄土过渡带高分辨率泥炭记录: 东亚季风气候颤动的实例. 中国科学: B 辑, 26(2): 118-124. [Zhou W J, Li X Q, Dong G Y, et al. 1996. New younger dryas period high-resolution peat record in desert /loess transitional zone: a case for East Asia monsoon climate fibrillation. Science China: Series B, 26(2): 118-124.]朱立平, 王君波, 林晓, 等. 2007. 西藏纳木错深水湖芯反映的8.4 ka 以来气候环境变化. 第四纪研究, 27(4): 588-597. [Zhu L P, Wang J B, Lin X, et al. 2007. Environmental changes reflected by core sediments since 8.4 ka in Nam Co, Central Tibet of China. Quaternary Sciences, 27 (4): 588-597.]An C B, Feng Z D, Barton L. 2006. Dry or humid? Mid-Holocene humidity changes in arid and semi-arid China. Quaternary Science Reviews, 25(3): 351-361.An Z S, Porter S C, Kutzbach J E, et al. 2000. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews, 19(8): 743-762.Berger A, Loutre M F. 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 10(4): 297-317.Bond G, Kromer B, Beer J, et al. 2001. Persistent solar influence on north Atlantic climate during the Holocene. Science, 294: 2130-2136.Bond G, Showers W, Cheseby M, et al. 1997. A pervasive millennial: scale cycle in north Atlantic Holocene and glacial climates. Science, 278: 1257-1266.Chen C T A, Lan C H, Lou J Y, et al. 2003. The dry Holocene Megathermal in Inner Mongolia. Palaeogeography, Palaeoclimatology, Palaeoecology, 193(2): 181-200.Chen F H, Yu Z C, Yang M L. 2008. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews, 27: 351-364.Demske D, Tarasov P E, Wünnemann B, et al. 2009. Late glacial and Holocene vegetation, Indian monsoon and westerly circulation in the Trans-Himalaya recorded in the lacustrine pollen sequence from Tso Kar, Ladakh, NW India. Palaeogeography, Palaeoclimatology, Palaeoecology, 279(3): 172-185.Dykoski C A,Edwards R L,Cheng H, et al. 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave,China. Earth and Planetary Science Letters, 233: 71-86.El-Mosilimany A P. 1990. Ecological significance of common non-arboreal pollen: examples from drylands of the Middle East. Review of Palaeobotany and Palynology, 64: 343-350.Feng Z D, An C B, Wang H B. 2006. Holocene climatic and environmental changes in the arid and semi-arid areas of China: a review. Holocene ,16: 119-130.Gasse F, Fontes J C, Van Campo E, et al. 1996. Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: discussion and conclusions. Palaeogeography, Palaeoclimatology, Palaeoecology, 120(1): 79-92.Gupta A K, Anderson D M, Overpeck J T. 2003. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature, 421: 354-357.Hartmann K, Wünnemann B. 2007. Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses. Quaternary International, 194: 28-44.Herzschuh U. 2006. Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quaternary Science Reviews, 25: 163-178.Herzschuh U, Kramer A, Mischke S, et al. 2009. Quantitative climate and vegetation trends since the late glacial on the northeastern Tibetan Plateau deduced from Koucha Lake pollen spectra. Quaternary Research, 71(2): 162-171.Jiang Q F, Shen J, Liu X Q, et al. 2007. Holocene climate reconstruction of Ulungur Lake (Xinjiang, China) inferred from ostracod species assemblages and stable isotopes. Quaternary Sciences, 27(3): 382-391.Jiang W Y, Guo Z T, Sun X J, et al. 2006. Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia): Holocene variability of the East Asian monsoon. Quaternary Research, 65: 411-420.Jin L Y, Chen F H, Carrie Morrill, et al. 2012. Causes of early Holocene desertification in arid Central Asia. Climate dynamics, 38(7-8): 1577-1591.Kramer A, Herzschuh U, Mischke S, et al. 2009. Late glacial vegetation and climate oscillations on the southeastern Tibetan Plateau inferred from the Lake Naleng pollen profile. Quaternary Research, 73(2): 324-335.Lamb H F, Gasse F, Benkaddour A, et al. 1995. Relation between century-scale Holocene arid intervals in tropical and temperate zones. Nature, 373(6510): 134-137.Li Y, Wang N A, Cheng H, et al. 2009. Holocene environmental change in the marginal area of the Asian monsoon: A record from Zhuye Lake, NW China. Boreas, 38(2): 349-361.Liu H Y, Xu L H, Cui H T. 2002. Holocene history of desertification along the woodland-steppe border in Northern China. Quaternary Research, 57: 259-270.Lü X M, Zhu L P, Mitsugu N, et al. 2011. A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co, southern Tibet. Chinese Science Bulletin, 56 (27):2931-2940.Ma Y Z, Liu K B, Feng Z D, et al. 2008. A survey of modern pollen and vegetation along a south-north transect in Mongolia. Journal of Biogeography, 35: 1512-1532.Mason J A, Lu H, Zhou Y, et al. 2009. Dune mobility and aridity at the desert margin of northern China at a time of peak monsoon strength. Geology, 37: 947-950.Mojtahid M, Jorissen F J, Garcia J, et al. 2013. High resolution Holocene record in the southeastern Bay of Biscay: global versus regional climate signals. Palaeogeography,Palaeoclimatology, Palaeoecology, 377: 28-44. Moore P D, Webb J A, Collinson M E. 1991. Pollen analysis. 2nd ed. Oxford: Blackwell Scientific Publication: 216.Prentice I C, Guiot J, Huntley B, et al. 1996. Reconstructing biomes from palaeoecological data: a general method and its application to European pollen data at 0 and 6 ka. Climate Dynamics, 12: 185-194.Tang L Y, Shen C, Liu K, et al. 2000. Changes in South Asian monsoon: new high-resolution paleoclimatic records from Tibet, China. Chinese Science Bulletin, 45(1): 87-91.Thomas E R, Francoise G, Lin R F, et al. 1996. A Late Pleistocene-Holocene lacustrine record from Lake Manas, Zunggar (northern Xinjiang, western China). Palaeogeography, Palaeoclimatology, Palaeoecology, 120: 105-121.Thompson L G, Yao T, Davis M E, et al. 1997. Tropical climate instability: the Last Glacial Cycle from a Qinghai-Tibetan ice core. Science, 267: 1821-1825.Thornalley D J R, Elderfield H, McCave I N. 2009. Holocene oscillations in temperature and salinity of the surface subpolar North Atlantic. Nature, 457: 711-714.Van Campo E, Gasse F. 1993. Pollen-and diatom-inferred climatic and hydrological changes in Sumxi Co Basin (Western Tibet) since 13,000 yr BP. Quaternary Research, 39(3): 300-313.Wang W, Feng Z D. 2013a. Holocene moisture evolution across the Mongolian Plateau and its surrounding areas: a synthesis of climatic records. Earth-Science Reviews, 122: 38-57.Wang W, Feng Z D, Ran M, et al. 2013b. Holocene climate and vegetation changes inferred from pollen records of Lake Aibi, northern Xinjiang, China: a potential contribution to understanding of Holocene climate pattern in Eastcentral Asia. Quaternary International, 311: 54-62.Wang Y B, Liu X Q, Herzschuh U. 2010. Asynchronous evolution of the Indian and East Asian Summer Monsoon indicated by Holocene moisture patterns in monsoonal central Asia. Earth-Science Reviews, 103(3): 135-153.Weiss H, Courty MA, Wetterstrom W, et al. 1993. The genesis and collapse of third millennium north Mesopotamian civilization. Science, 261(5124): 995-995.Wen R L, Xiao J L, Chang Z G, et al. 2009. Holocene precipitation and temperature variations in the East Asian monsoonal margin from pollen data from Hulun Lake in northeastern Inner Mongolia, China. Boreas, 39: 262-272.Wischnewski J, Mischke S, Wang Y B, et al. 2011. Reconstructing climate variability on the northeastern Tibetan Plateau since the last late glacial-a multi-proxy, dual-site approach comparing terrestrial and aquatic signals. Quaternary Science Reviews, 30(1): 82-97.Xiao J L, Chang Z G, Si B, et al. 2009. Partitioning of the grain-size components of Dali Lake core sediments: evidence for lake-level changes during the Holocene. Journal of Paleolimnology , 42: 249-260.Zhao Y, Yu Z C. 2012. Vegetation response to Holocene climate change in East Asian monsoon-margin region. Earth-Science Reviews, 113: 1-10.Zhao Y, Yu Z C, Chen F H, et al. 2007. Holocene vegetation and climate history at Hurleg Lake in the Qaidam Basin, northwest China. Review of Palaeobotany and Palynology, 145(3): 275-288.Zhao Y, Yu Z C, Chen F H. 2009a. Spatial and temporal patterns of Holocene vegetation and climate changes in arid and semi-arid China. Quaternary International, 194: 6-18.Zhao Y, Yu Z C, Chen F H, et al. 2009b. Vegetation response to Holocene climate change in monsoon-influenced region of China. Earth-Science Reviews, 97: 242-256.Zhu L P, Zhen X L, Wang J B, et al. 2009. A ~30,000-year record of environmental changes inferred from Lake Chen Co, Southern Tibet. Journal of Paleolimnology, 42(3): 343-358. |
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