参考文献/References:
[1] GIRARDIN M P, HOGG E H, BERNIER P Y, et al. Negative impacts of high temperatures on growth of black spruce forests intensify with the anticipated climate warming [J]. Global Change Biology, 2016, 22(2): 627-643. DOI: 10.1111/gcb.13072
[2] CHARNEY N D, BABST F, POULTER B, et al. Observed forest sensitivity to climate implies large changes in 21st century North American forest growth [J]. Ecology Letters, 2016, 19(9): 1119-1128. DOI: 10.1111/ele.12650
[3] LIU H Y, WILLIAMS A P, ALLEN C D, et al. Rapid warming accelerates tree growth decline in semi-arid forests of Inner Asia [J]. Global Change Biology, 2013, 19(8): 2500-2510. DOI: 10.1111/gcb.12217
[4] WILLIAMS A P, ALLEN C D, MACALADY A K, et al. Temperature as a potent driver of regional forest drought stress and tree mortality [J]. Nature Climate Change, 2013, 3(3): 292-297.DOI: 10.1038/NCLIMATE1693
[5] TRANQUILLINI W, BENECKE U. Physiological ecology of the alpine timberline: Tree existence at high altitudes with special reference to the European Alps [M]. Berlin: Springer-Verlag, 1979. DOI: 10.1007/978-3-642-67107-4
[6] KÖRNER C, PAULSEN J. A world-wide study of high altitude treeline temperatures [J]. Journal of Biogeography, 2004, 31(5): 713-732. DOI: 10.1111/j.1365-2699.2003.01043.x
[7] 朱芬萌,安树青,关保华,等. 生态交错带及其研究进展[J]. 生态学报,2007,27(7):3032-3042. [ZHU Fenmeng, AN Shuqing, GUAN Baohua, et al. A review of ecotone: Concepts, attributes, theories and research advances [J]. Acta Ecologica Sinica, 2007, 27(7): 3032-3042]
[8] 李明财,罗天祥,朱教君,等. 高山林线形成机理及植物相关生理生态学特性研究进展[J]. 生态学报,2008,28(11):5583-5591. [LI Mingcai, LUO Tianxiang, ZHU Jiaojun, et al. Advances in formation mechanism of alpine timberline and associated physio-ecological characteristics of plants [J]. Acta Ecologica Sinica, 2008, 28(11): 5583-5591]
[9] HOFGAARD A, HARPER K A. Tree recruitment, growth, and distribution at the circumpolar forest-tundra transition: Introduction [J]. Canadian Journal of Forest Research, 2011,41(3): 435-436. DOI:10.1139/X10-238
[10] BATLLORI E, GUTIÉRREZ E. Regional tree line dynamics in response to global change in the Pyrenees [J]. Journal of Ecology, 2008, 96(6): 1275-1288. DOI: 10.1111/j.1365-2745.2008.01429.x
[11] ROSSLER O, BRÄUNING A, LOFFLER J, et al. Dynamics and driving forces of treeline fluctuation and regeneration in Central Norway during the past decades [J]. Erdkunde, 2008, 62(2): 117-128. DOI: 10.3112/erdkunde.2008.02.02
[12] LIANG E Y, WANG Y F, ECKSTEIN D, et al. Little change in the fir tree-line position on the southeastern Tibetan Plateau after 200 years of warming [J]. New Phytologist, 2011,190(3): 760-769. DOI: 10.1111/j.1469-8137.2010.03623.x
[13] 尚华明,洪建昌,张瑞波,等. 树轮记录的西藏东北部过去552 a上年10月至当年5月降水量变化[J]. 山地学报,2018, 36(6): 821-832. [SHANG Huaming, HONG Jianchang, ZHANG Ruibo, et al. Tree-ring recorded 522-year precipitation from previous October to May in northeastern Tibet, China [J]. Mountain Research, 2018, 36(6): 821-832] DOI: 10. 16089/j.cnki.1008-2786.000378
[14] 陈峰, 袁玉江, 喻树龙.闽中北柳杉树轮指示的气候信号与季风区不同地域干湿变化关系[J]. 山地学报,2015,33(6): 690-695. [CHEN Feng,YUAN Yujiang,YU Shulong. Drought signals in the tree-ring width record of Cedar(Cryptomeria
fortunei)trees from north central Fujian: Linkages to the monsoonal regions [J]. Mountain Research, 2015, 33(6): 690-695] DOI: 16089/j.cnki.1008-2786.000083
[15] COOK E R, KAIRIUKSTIS L A. Methods of dendrochronology: Applications in the environmental sciences [M]. London: Kluwer, 1990: 51-54. DOI: 10.1007/978-94-015-7879-0
[16] WOODCOCK H, BRADLEY R. Salix arctica(pall.): Its potential for dendroclimatological studies in the high arctic [J]. Dendrochronologia, 1994, 12: 11-22.
[17] BÄR A, BRÄUNING A, LÖFFLER J, et al. Dendroecology of dwarf shrubs in the high mountains of Norway: A methodological approach [J]. Dendrochronologia, 2006, 24(1): 17-27. DOI: 10.1016/j.dendro.2006.05.001
[18] BARICHIVICH J, SAUCHYN D J, LARA A, et al. Climate signals in high elevation tree-rings from the semiarid Andes of north-central Chile: Responses to regional and large-scale variability [J]. Palaeogeography, 2009, 281:320-333. DOI: 10.1016/j.palaeo.2007.10.033
[19] POORE R E, LAMANNA C A, EBERSOLE J J, et al. Controls on radial growth of mountain big sagebrush and implications for climate change [J]. Western North American Naturalist, 2009, 69(4): 556-562.
[20] XIAO Shengchuan, XIAO Honglang, KOBAYASHI O, et al. Dendroclimatological investigations of sea buckthorn(Hippophaer hamnoides)and reconstruction of the equilibrium line altitude of the July First Glacier in the western Qilian Mountains, northwestern China [J]. Tree-Ring Research, 2007, 63(1): 15-26.
[21] GRISSINO-MAYER H D. An updated list of species used in tree-ring research [J]. Tree-Ring Bulletin, 1993, 53: 17-43.
[22] SCHWEINGRUBER F H, POSCHLOD P. Growth rings in herbs and shrubs: Life span, age determination and stem anatomy [J]. Forest Snow and Landscape Research, 2005, 79(3): 195-415.
[23] LIANG E Y, ECKSTEIN D. Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau [J]. Annals of Botany, 2009, 104: 665 -670. DOI: 10.1093/aob/mcp158
[24] ETTL G J, PETERSON D L. Growth response of subalpine fir(Abies lasiocarpa)to climate in the Olympic Mountains, Washington, USA [J]. Global Change Biology, 1995,1(3):213-230.
[25] LIANG Eryuan, WANG Yafeng, XU Yan, et al. Growth variation in Abies georgei var. smithii along altitudinal gradients in the Sygera Mountains, southeastern Tibetan Plateau [J]. Trees-Structure and Function, 2010, 24: 363-373. DOI: 10.1007/s00468-009-0406-0
[26] SIDOR C G, POPA I, VLAD R, et al. Different tree-ring responses of Norway spruce to air temperature across an altitudinal gradient in the Eastern Carpathians(Romania)[J]. Trees-Structure and Function. 2015, 29: 985-997. DOI: 10.1007/s00468-015-1178-3
[27] CONLISK E, CASTANHA C, GERMINO M J, et al. Declines in low-elevation subalpine tree populations outpace growth in high-elevation populations with warming [J]. Journal of Ecology, 2017,105: 1347-1357. DOI: 10.1111/1365-2745.12750
[28] FRITTS H C. Tree rings and climate [M]. London: Academic Press,1976:77-82.
[29] SALZER M W, HUGHES M K, BUNN A G, et al. Recent unprecedented tree-ring growth in bristlecone pine at the highest elevations and possible causes [J]. Proceedings of the National Academy of Sciences of the United States of America, 2009,106(48): 20348-20353. DOI: 10.1073/pnas.0903029106
[30] PONOCNA T, SPYT B, KACZKA R, et al. Growth trends and climate responses of Norway spruce along elevational gradients in East-Central Europe [J]. Trees-Structure and Function, 2016, 30: 1633-1646. DOI: 10.1007/s00468-016-1396-3
[31] CONLISK E, CASTANHA C, GERMINO M J, et al. Declines in low-elevation subalpine tree populations outpace growth in high-elevation populations with warming [J]. Journal of Ecology. 2017, 105(5): 1347-1357. DOI: 10.1111/1365-2745.12750
[32] 石松林, 靳甜甜, 刘国华, 等. 气候变暖抑制西藏拉萨河大果圆柏树木生长[J]. 生态学报. 2018, 38(24): 8964-8972. [SHI Songlin, JIN Tiantian, LIU Guohua, et al. Climate warming decelerates growth of Sabina tibetica in Lhasa River area of Tibet [J]. Acta Ecologica Sinica, 2018, 38(24): 8964-8972] DOI: 10.5846 /stxb201807131522
[33] LIU Jingjing, QIN Chun, KANG Shuyuan. Growth response of Sabina tibetica to climate factors along an elevation gradient in south Tibet [J]. Dendrochronologia, 2013, 31(4): 255-265. DOI: 10.1016/j.dendro.2012.12.001
[34] LI Zongshan, LIU Guohua, FU Bojie, et al. The growth-ring variations of alpine shrub Rhododendron przewalskii reflect regional climate signals in the alpine environment of Miyaluo town in western Sichuan province, China [J]. Acta Ecologica Sinica, 2013, 33(1): 23-31. DOI: 10.1016/j.chnaes.2012.12.004
[35] FANG Ruizheng, MING Tianlu. The floristic study on the genus Rhododendron [J]. Acta Botanica Yunnanica, 1995, 17(4): 359-379.
[36] PETERS R L, GROENENDIJK P, VLAM M, et al. Detecting long-term growth trends using tree rings: A critical evaluation of methods [J]. Global Change Biology, 2015, 21: 2040-2054. DOI: 10.1111/gcb.12826
[37] WILLIAMS A P, ALLEN C D, MACALADY A K, et al. Temperature as a potent driver of regional forest drought stress and tree mortality [J]. Nature Climate Change, 2013, 3: 292-297. DOI: 10.1038/NCLIMATE1693
[38] HUGHES M K, SWETNAM T W, DIAZ H F. Dendroclimatology: Progress and prospects: Volume 11 [M]. Berlin: Springer, 2011:101-105. DOI: 10.1007/978-1-4020-5725-0
[39] JUMP A S, HUNT J M, PENUELAS J. Rapid climate change-related growth decline at the southern range edge of Fagus sylvatica [J]. Global Change Biology, 2006, 12: 2163-2174. DOI: 10.1111/j.1365-2486.2006.01250.x
[40] WIGLEY T M L, BRIFFA K R, JONES P D. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology [J]. Journal of Climate and Applied Meteorology, 1984, 23(2): 201-213.
[41] WANG Wenzhi, JIA Min, WANG Genxu, et al. Rapid warming forces contrasting growth trends of subalpine fir(Abies fabri)at higher- and lower-elevations in the eastern Tibetan Plateau [J]. Forest Ecology and Management, 2017, 402:135-144. DOI: 10.1016/j.foreco.2017.07.043
[42] ERIKSSON M. Book review of methods of dendrochronology: Applications in the environmental sciences edited by COOK E R and KAIRIUKSTIS L A [J]. Forest Science, 1991,37(2): 734-735. DOI: 10.1093/forestscience/37.2.734
[43] FRITTS H C, DEAN J S. Dendrochronological modeling of the effects of climatic change on tree-ring width chronologies from the Chaco Canyon area,southwestern United States [J]. Tree-Ring Bulletin, 1992, 52: 31-58.
[44] LIANG Eryuan, SHAO Xuemei, QIN Ningsheng, et al. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau [J]. Global and Planetary Change, 2008, 61: 313-320. DOI: 10.1016/j.gloplacha.2007.10.008
[45] SHI C, MASSON-DELMOTTE V, DAUX V, et al. Unprecedented recent warming rate and temperature variability over the east Tibetan Plateau inferred from Alpine treeline dendrochronology [J]. Climate Dynamic, 2015, 45: 1367-1380. DOI: 10.1007/s00382-014-2386-z
[46] KRONER Y, WAY D A. Carbon fluxes acclimate more strongly to elevated growth temperatures than to elevated CO2 concentrations in a northern conifer [J]. Global Change Biology, 2016, 22(8): 2913-2928. DOI: 10.1111/gcb.13215
[47] KÖRNER C. A re-assessment of high elevation treeline positions and their explanation [J]. Oecologia, 1998,115: 445-459. DOI: 10.1007/s004420050540
[48] PENG S, PIAO S, CIAIS P, et al. Asymmetric effects of daytime and night-time warming on northern Hemisphere vegetation [J]. Nature, 2013, 501: 88-92. DOI: 10.1038/nature12434
[49] SIDOR C G, POPA I, VLAD R, et al. Different tree-ring responses of Norway spruce to air temperature across an altitudinal gradient in the Eastern Carpathians(Romania)[J]. Trees, 2015, 29: 985-997. DOI: 10.1007/s00468-015-1178-3
[50] 时兴合, 秦宁生, 朱海峰, 等. 青海杂多大果圆柏年轮指示的公元1360—2005年5—6月最高气温变化 [J]. 科学通报, 2010, 55(19): 1924-1931.[SHI Xinghe, QIN Ningsheng, ZHU Haifeng, et al. May-June mean maximum temperature change during 1360—2005 as reconstructed by tree of Sabina Tibetica in Zaduo, Qinghai province [J]. Chinese Science Bulletin, 2010, 55(19): 1924-1931] DOI: 10.1007/s11434-010-3237-x
[51] DUAN Jianping, ZHANG Qibin, LYU Lixin, et al. Regional-scale winter spring temperature variability and chilling damage dynamics over the past two centuries in southeastern China [J]. Climate Dynamics, 2012, 39: 919-928. DOI: 10.1007/s00382-011-1232-9
[52] ZHU H F, FANG X Q, SHAO X M, et al. Tree ring-based February-April temperature reconstruction for Changbai Mountain in northeast China and its implication for east Asian winter monsoon [J]. Climate of the Past, 2009,5: 661-666. DOI: 10.5194/ cp-5-661-2009
[53] TAKAHASHI K, TOKUMITSU Y, YASUE K, et al. Climatic factors affecting the tree-ring width of Betula ermanii at the timberline on Mount Norikura, central Japan [J]. Ecological Research, 2005, 20(4): 445-451. DOI: 10.1007/s11284-005-0060-y
[54] 吴普, 王丽丽, 邵雪梅. 采用高山松最大密度重建川西高原近百年夏季气温[J]. 地理学报, 2005, 60(6): 998-1006. [WU Pu, WANG Lily, SHAO Xuemei. Reconstruction of summer temperature from maximum latewood density of Pinus densata in west Sichuan [J]. Acta Geographica Sinica, 2005, 60(6): 998-1006]
[55] LIU Y, AN Z, LINDERHOLM H W, et al. Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings [J]. Science in China Series D: Earth Sciences, 2009, 52(3): 348-359. DOI: 10.1007/s11430-009-0025-z
[56] FRITTS H C. Tree rings and climate [M]. London: Academic Press, 1976: 376-412, 534.
[57] LIANG E Y, LEUSCHNER C, DULAMSUREN C, et al. Global warming-related tree growth decline and mortality on the north-eastern Tibetan plateau [J]. Climatic Change, 2016, 134:163-176.DOI: 10.1007/s10584-015-1531-y
相似文献/References:
[1]马华,王云琦,王力,等.近20a广西石漠化区植被覆盖度与气候变化和农村经济发展的耦合关系[J].山地学报,2014,(01):38.
MA Hua,WANG Yunqi,WANG Li,et al.Vegetation Cover and Climate Change and Rural Economic Development in Relations during Last 20 Years in Karst Region of Guangxi,China[J].Mountain Research,2014,(5):38.
[2]刘军会,高吉喜,王文杰,等.青藏高原植被覆盖变化及其与气候变化的关系[J].山地学报,2013,(02):234.
LIU Junhui,GAO Jixi,WANG Wenjie().Variations of Vegetation Coverage and Its Relations to Global Climate Changes on the Tibetan Plateau during 1981—2005[J].Mountain Research,2013,(5):234.
[3]刘伟龙,赵 慧,王小丹,等.气候变化下西藏高寒湿地生态系统研究的意义和特点[J].山地学报,2014,(04):481.
LIU Weilong,ZHAO Hui,WANG Xiaodan,et al.Review and Evaluation of the Effect of the Climate Change on the High Altitude Wetland Ecosystem in Tibet Plateau[J].Mountain Research,2014,(5):481.
[4]姜永见,李世杰,沈德福,等.青藏高原江河源区近40年来气候变化特征及其对区域环境的影响[J].山地学报,2012,(04):461.
JIANG Yongjian,LI Shijie,SHEN Defu,et al.Climate Change and Its Impact on the Regional Environment in the Source Regions of the Yangtze, Yellow and Lantsang Rivers in Qinghai-Tibetan Plateau during 1971—2008[J].Mountain Research,2012,(5):461.
[5]蓝永超,胡兴林,丁宏伟,等.气候变暖背景下祁连山西部山区水循环要素的变化——以疏勒河干流上游山区为例[J].山地学报,2012,(06):675.
LAN Yongchao,HU Xinglin,DIN Hongwei,et al.Variation of Water Cycle Factors in the Western Qilian Mountain Area under Climate Warming——Taking the Mountain Watershed of the Main Stream of Shule River Basin for Example[J].Mountain Research,2012,(5):675.
[6]陈剑,崔之久,戴福初,等.金沙江奔子栏-达日河段大型泥石流堆积扇的成因机制[J].山地学报,2011,(03):312.
CHEN Jian,CUI Zhijiu,Dai Fuchu,et al.Genetic Mechanism of the Major Debrisflow Deposits at BenzilanDari Segment, the Upper Jinsha River[J].Mountain Research,2011,(5):312.
[7]王晓东,刘惠清.长白山突变型林线岳桦对气候变化的响应[J].山地学报,2011,(05):551.
WANG Xiaodong,LIU Huiqing.Climatic Response of Betula ermanii from Closed Treeline in Changbai Mountains[J].Mountain Research,2011,(5):551.
[8]熊尚发,刘东生,丁仲礼.南方红土的剖面风化特征[J].山地学报,2000,(01):7.
[9]刘文杰.西双版纳近40年气候变化对自然植被净第一性生产力的影响[J].山地学报,2000,(04):296.
[10]闫淑君,洪伟,吴承祯,等.福建近41年气候变化对自然植被净第一性生产力的影响[J].山地学报,2001,(06):522.