4 Gagen M, McCarroll D, Loader N J et al. Stable isotopes in dendroclimatology:Moving beyond ''potential’ dendroclimatology. In:Hughes M K, Swetnam T W, Diaz H F eds. Dendroclimatology Progress and Prospects. Netherlands:Springer, 2011. 147~172
[2]
5 Young G H F, McCarroll D, Loader N J et al. A 500-year record of summer near-ground solar radiation from tree-ring stable carbon isotopes. The Holocene, 2010, 20 (3):315~324
[3]
6 van Der Sleen P, Groenendijk P, Vlam M et al. No growth stimulation of tropical trees by 150 years of CO2 fertilization but water-use efficiency increased. Nature Geoscience, 2015, 8 (1):24~28
[4]
7 Loader N J, Young G H F, Grudd H et al. Stable carbon isotopes from Tornetr？sk, Northern Sweden provide a millennial length reconstruction of summer sunshine and its relationship to Arctic circulation. Quaternary Science Reviews, 2013, 62 :97~113
[5]
8 Loader N J, Walsh R P D, Robertson I et al. Recent trends in the intrinsic water-use efficiency of ringless rainforest trees in Borneo. Philosophical Transactions of the Royal SocietyB: Biological Sciences, 2011, 366 (1582):3330~3339
[6]
9 Anchukaitis K J, Evans M N, Wheelwright N T et al. Stable isotope chronology and climate signal calibration in neotropical montane cloud forest trees. Journal of Geophysical Research:Biogeosciences, 2008, 113 (G3):G03030
[7]
10 Evans M N, Schrag D P. A stable isotope-based approach to tropical dendroclimatology. Geochimica et Cosmochimica Acta, 2004, 68 (16):3295~3305
[8]
11 Lévesque M, Siegwolf R, Saurer M et al. Increased water-use efficiency does not lead to enhanced tree growth under xeric and mesic conditions. New Phytologist, 2014, 203 (1):94~109
[9]
12 Keenan T F, Hollinger D Y, Bohrer G et al. Increase in forest water-use efficiency as atmospheric carbon dioxide concentrations rise. Nature, 2013, 499 (7458):324~327
[10]
13 Wang Guoan, Feng Xiahong. Response of plants'' water use efficiency to increasing atmospheric CO2 concentration. Environmental Science and Technology, 2012, 46 (16):8610~8620
[11]
14 Liu Xiaohong, Wang Wenzhi, Xu Guobao et al. Tree growth and intrinsic water-use efficiency of inland riparian forests in Northwestern China:Evaluation via δ 13 C and δ18O analysis of tree rings. Tree Physiology, 2014, 34 (9):966~980
[12]
16 De Kauwe M G, Medlyn B E, Zaehle S et al. Forest water use and water use efficiency at elevated CO2:A model-data intercomparison at two contrasting temperate forest FACE sites. Global Change Biology, 2013, 19 (6):1759~1779
[13]
17 Treydte K, Boda S, Graf Pannatier E et al. Seasonal transfer of oxygen isotopes from precipitation and soil to the tree ring:Source water versus needle water enrichment. New Phytologist, 2014, 202 (3):772~783
[14]
18 Larcher L, Hara-Nishimura I, Sternberg L. Effects of stomatal density and leaf water content on the 18 O enrichment of leaf water. New Phytologist, 2015, 206 (1):141~151
[15]
19 Hommel R, Siegwolf R, Saurer M et al. Drought response of mesophyll conductance in forest understory species-impacts on water-use efficiency and interactions with leaf water movement. Physiologia Plantarum, 2014, 152 (1):98~114
[16]
20 Saurer M, Spahni R, Frank D C et al. Spatial variability and temporal trends in water-use efficiency of European forests. Global Change Biology, 2014, 20 (12):3700~3712
[17]
21 Boucher, Guiot J, Hatté C et al. An inverse modeling approach for tree-ring-based climate reconstructions under changing atmospheric CO2 concentrations. Biogeosciences, 2014, 11 (12):3245~3258
[18]
22 Farquhar G D, Ehleringer J R, Hubick K T. Carbon isotope discrimination and photosynthesis. Annual Review of Plant Biology 1989, 40 (1):503~537
[19]
23 Farquhar G D, O''leary M H, Berry J A. On the relationship between carbon isotope discrimination and the intercellular carbon dioxide concentration in leaves. Australian Journal of Plant Physiology, 1982, 9 (2):121~137
[20]
31 Anderson W T, Bernasconi S M, Mckenzie J A et al. Model evaluation for reconstructing the oxygen isotopic composition in precipitation from tree ring cellulose over the last century. Chemical Geology, 2002, 182 (2~4):121~137
[21]
32 Roden J S, Lin G, Ehleringer J R. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose. Geochimica et Cosmochimica Acta, 2000, 64 (1):21~35
[22]
33 Sternberg L, Pinzon M C, Anderson W T et al. Variation in oxygen isotope fractionation during cellulose synthesis:Intramolecular and biosynthetic effects. Plant, Cell and Environment, 2006, 29 (10):1881~1889
[23]
34 Craig H, Gordon L I. Deuterium and oxygen 18 variations in the ocean and marine atmosphere. In:Tongiogi E ed. Proceed of Stable Isotopes in Oceanographic Studies and Paleotemperatures. Italy:Pisa, 1965. 9~130
[24]
35 Sternberg L. Oxygen stable isotope ratios of tree-ring cellulose:The next phase of understanding. New Phytologist, 2009, 181 (3):553~562
[25]
36 Deniro M J, Epstein S. Isotopic composition of cellulose from aquatic organisms. Geochimica et Cosmochimica Acta, 1981, 45 (10):1885~1894
[26]
37 Leavitt S W, Danzer S R. Method for batch processing small wood samples to holocellulose for stable-carbon isotope analysis. Analytical Chemistry, 1993, 65 (1):87~89
[27]
38 Leavitt S W, Long A. Sampling strategy for stable carbon isotope ananlysis of tree in pine. Nature, 1984, 311 (5982):145~147
[28]
39 McCarroll D, Pawellek F. Stable carbon isotope ratios of latewood cellulose in Pinus sylvestris from Northern Finland:Variability and signal-strength. The Holocene, 1998, 8 (6):675~684
[29]
40 Daux V, Edouard J L, Masson-Delmotte V et al. Can climate variations be inferred from tree-ring parameters and stable isotopes from Larix decidua？Juvenile effects, budmoth outbreaks, and divergence issue. Earth and Planetary Science Letters, 2011, 309 (3~4):221~233
[30]
41 Liu Yu, Ma Limin, Leavitt S W et al. A preliminary seasonal precipitation reconstruction from tree-ring stable carbon isotopes at Mt. Helan, China, since AD 1804. Global and Planetary Change, 2004, 41 (3~4):229~239
[31]
42 Li？n I D, Gutiérrez E, Helle G et al. Pooled versus separate measurements of tree-ring stable isotopes. Science of the Total Environment, 2011, 409 (11):2244~2251
[32]
43 Szymczak S, Joachimski M, Br？uning A et al. Are pooled tree ring δ 13 C and δ18O series reliable climate archives？——A case study of Pinus nigra spp. laricio(Corsica/France). Chemical Geology, 2012, 308~309 :40~49
[33]
44 Shi Chunming, Masson-Delmotte V, Risi C et al. Sampling strategy and climatic implications of tree-ring stable isotopes on the southeast Tibetan Plateau. Earth and Planetary Science Letters, 2011, 301 (1~2):307~316
[34]
66 Liu Yu, Wang Ruiyuan, Leavitt S W et al. Individual and pooled tree-ring stable-carbon isotope series in Chinese pine from the Nan Wutai region, China:Common signal and climate relationships. Chemical Geology, 2012, 330~331 :17~26
[35]
83 Liu Xiaohong, Xu Guobao, Grieinger J et al. A shift in cloud cover over the southeastern Tibetan Plateau since 1600:Evidence from regional tree-ring δ18O and its linkages to tropical oceans. Quaternary Science Reviews, 2014, 88 :55~68
[36]
84 Aucour A M, Tao F X, Sheppard S M F et al. Climatic and monsoon isotopic signals(δD, δ 13 C)of Northeastern China tree rings. Journal of Geophysical Research, 2002, 107 (D9):4074
[37]
85 Xu Chenxi, Zheng Huaizhou, Nakatsuka T et al. Oxygen isotope signatures preserved in tree ring cellulose as a proxy for April-September precipitation in Fujian, the subtropical region of Southeast China. Journal of Geophysical Research, 2013, 118 (23):2013JD019803
[38]
86 Leavitt S W. Regional expression of the 1988 U.S. midwest drought in seasonal δ 13 C of tree rings. Journal of Geophysical Research, 2007, 112 (D6):D06107
[39]
87 Leavitt S W, Woodhouse C A, Castro C L et al. The North American monsoon in the U. S. Southwest:Potential for investigation with tree-ring carbon isotopes. Quaternary International, 2011, 235 (1~2):101~107
[40]
88 Treydte K, Schleser G H, Schweingruber F H et al. The climatic significance of δ 13 C in subalpine spruces(Ltschental, Swiss Alps). TellusB, 2001, 53 (5):593~611
[41]
89 Fichtler E, Helle G, Worbes M. Stable-carbon isotope time series from tropical tree rings indicate a precipitation signal. Tree-Ring Research, 2010, 66 (1):35~49
[42]
90 刘晓宏, 秦大河, 邵雪梅等. 西藏喜马拉雅冷杉年轮δ 13 C与气候意义. 科学通报, 2003, 48 (11):1209~1213 Liu Xiaohong, Qin Dahe, Shao Xuemei et al. Climatic significance of stable carbon isotope in tree rings of Abies spectabibis in southeastern Tibet. Chinese Science Bulletin, 2003, 48 (11):1209~1213
[43]
91 刘晓宏, 秦大河, 邵雪梅等. 西藏林芝冷杉树轮稳定碳同位素对气候的响应. 冰川冻土, 2002, 24 (5):574~578 Liu Xiaohong, Qin Dahe, Shao Xuemei et al. Stable carbon isotope of Abies spectabibis from Nyingchi County of Tibet Autonomous Region and its response to climate change. Journal of Glaciology and Geocryology, 2002, 24 (5):574~578
[44]
92 Liu Xiaohong, Shao Xuemei, Zhao Liangju et al. Dendroclimatic temperature record derived from tree-ring width and stable carbon isotope chronologies in the middle Qilian Mountains, China. Arctic, Antarctic, and Alpine Research, 2007, 39 (4):651~657
[45]
93 Liu Xiaohong, Shao Xuemei, Liang Eryuan et al. Species-dependent responses of juniper and spruce to increasing CO2 concentration and to climate in semi-arid and arid areas of Northwestern China. Plant Ecology, 2007, 193 (2):195~209
[46]
94 Treydte K, Frank D C, Saurer M et al. Impact of climate and CO2 on a millennium-long tree-ring carbon isotope record. Geochimica et Cosmochimica Acta, 2009, 73 (16):4635~4647
[47]
95 Dansgaard W. Stable isotopes in precipitation. Tellus, 1964, 16 (4):436~468
[48]
96 Burk R L, Stuiver M. Oxygen isotope ratios in trees reflect mean annual temperature and humidity. Science, 1981, 211 (4489):1417~1419
[49]
97 Liu Xiaohong, An Wenling, Treydte K et al. Tree-ring δ18O in Southwestern China linked to variations in regional cloud cover and tropical sea surface temperature. Chemical Geology, 2012, 291 :104~115
[50]
98 Liu Xiaohong, Zeng Xiaomin, Leavitt S W et al. A 400-year tree-ring δ18O chronology for the southeastern Tibetan Plateau:Implications for inferring variations of the regional hydroclimate. Global and Planetary Change, 2013, 104 :23~33
[51]
99 Xu Guobao, Liu Xiaohong, Qin Dahe et al. Tree-ring δ18O evidence for the drought history of eastern Tianshan Mountains, Northwest China since 1700 AD. International Journal of Climatology, 2014, 34 (12):3336~3347
[52]
10 0Treydte K, Frank D, Esper J et al. Signal strength and climate calibration of a European tree-ring isotope network. Geophysical Research Letters, 2007, 34 (24):L24302
[53]
10 1Saurer M, Schweingruber F, Vaganov E A et al. Spatial and temporal oxygen isotope trends at the northern tree-line in Eurasia. Geophysical Research Letters, 2002, 29 (15):10~11
[54]
10 2Grieinger J, Br？uning A, Helle G et al. Late Holocene Asian summer monsoon variability reflected by δ18O in tree-rings from Tibetan junipers. Geophysical Research Letters, 2011, 38 (3):L03701
[55]
10 3Xu Hai, Hong Yetang, Hong Bin. Decreasing Asian summer monsoon intensity after 1860 AD in the global warming epoch. Climate Dynamics, 2012, 39 (7~8):2079~2088
[56]
10 4Shi Chunming, Daux V, Zhang Qibing et al. Reconstruction of southeast Tibetan Plateau summer climate using tree ring δ18O:Moisture variability over the past two centuries. Climate of the Past, 2012, 8 (1):205~213
[57]
10 5Xu Guobao, Liu Xiaohong, Qin Dahe et al. Drought history inferred from tree ring δ 13 C and δ18O in the central Tianshan Mountains of China and linkage with the North Atlantic Oscillation. Theoretical and Applied Climatology, 2014, 116 (3~4):385~401
[58]
10 6Xu Guobao, Liu Xiaohong, Qin Dahe et al. Relative humidity reconstruction for northwestern China''s Altay Mountains using tree-ring δ18O. Chinese Science Bulletin, 2014, 59 (2):190~200
[59]
10 7Xu Chenxi, Sano M, Nakatsuka T. A 400-year record of hydroclimate variability and local ENSO history in northern Southeast Asia inferred from tree-ring δ18O. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 386 :588~598
[60]
10 8Sano M, Tshering P, Komori J et al. May-September precipitation in the Bhutan Himalaya since 1743 as reconstructed from tree ring cellulose δ18O. Journal of Geophysical Research, 2013, 118 (15):8399~8410
[61]
10 9Sano M, Ramesh R, Sheshshayee M et al. Increasing aridity over the past 223 years in the Nepal Himalaya inferred from a tree-ring δ18O chronology. The Holocene, 2011, 22 (7):809~817
[62]
11 0Sano M, Xu C, Nakatsuka T. A 300-year Vietnam hydroclimate and ENSO variability record reconstructed from tree ring δ18O. Journal of Geophysical Research, 2012, 117 (D12):D12115
[63]
13 0Krepkowski J, Gebrekirstos A, Shibistova O et al. Stable carbon isotope labeling reveals different carry-over effects between functional types of tropical trees in an Ethiopian mountain forest. New Phytologist, 2013, 199 (2):441~451
[64]
1 Wilson A T, Grinsted M J. 12 C/13 C in cellulose and lignin as palaeothermometers. Nature, 1977, 265 (5590):133~135
[65]
2 Leavitt S W, Lone A. Seasonal stable-carbon isotope variability in tree rings:Possible paleoenvironmental signals. Chemical Geology, 1991, 87 (1):59~70
[66]
3 Treydte K S, Schleser G H, Helle G et al. The twentieth century was the wettest period in Northern Pakistan over the past millennium. Nature, 2006, 440 (7088):1179~1182
[67]
15 Walker X J, Mack M C, Johnstone J F. Stable carbon isotope analysis reveals widespread drought stress in boreal black spruce forests. Global Change Biology, 2015, doi:10.1111/gcb.12893
[68]
24 Deniro M J D, Epstein S. Relationship between oxygen isotope ratios of terrestrial plant cellulose, carbon dioxide and water. Science, 1979, 204 (4388):51~53
[69]
25 McCarroll D, Loader N J. Stable isotopes in tree rings. Quaternary Science Reviews, 2004, 23 (7~8):771~801
[70]
26 Waterhouse J S, Switsur V R, Barker A C et al. Oxygen and hydrogen isotope ratios in tree rings: How well do models predict observed values？Earth and Planetary Science Letters, 2002, 201 (2):421~430
[71]
27 Saurer M, Robertson I, Siegwolf R et al. Oxygen isotope analysis of cellulose:An interlaboratory comparison. Analytical Chemistry, 1998, 70 (10):2074~2080
[72]
28 Saurer M, Siegwolf R, Borella S et al. Environmental information from stable isotopes in tree rings of Fagus sylvatica. In:Beniston M, Innes J L eds. The Impacts of Climate Variability on Forests. Berlin Heidelberg:Springer, 1998. 241~253
[73]
29 Ehleringer J R, Dawson T E. Water uptake by plants: Perspectives from stable isotope composition. Plant Cell Enviroment, 1992, 15 (9):1073~1082
[74]
30 Sternberg L, Deniro M J D. Biogeochemical implications of the isotopic equilibrium fractionation factor between the oxygen atoms of acetone and water. Geochimica et Cosmochimica Acta, 1983, 47 (12):2271~2274
[75]
45 Young G H F, Demmler J C, Gunnarson B E et al. Age trends in tree ring growth and isotopic archives:A case study of Pinus sylvestris L. from Northwestern Norway. Global Biogeochemical Cycles, 2011, 25 (2):GB2020
[76]
46 Dodd J P, Patterson W P, Holmden C et al. Robotic micromilling of tree-rings:A new tool for obtaining subseasonal environmental isotope records. Chemical Geology, 2008, 252 (1~2):21~30
[77]
47 Liu Xiaohong, An Wenling, Treydte K et al. Pooled versus separate tree-ring δD measurements, and implications for reconstruction of the Arctic Oscillation in Northwestern China. Science of the Total Environment, 2015, 511 :584~594
[78]
48 Liu Xiaohong, Shao Xuemei, Liang Eryuan et al. Climatic significance of tree-ring δ18O in the Qilian Mountains, Northwestern China and its relationship to atmospheric circulation patterns. Chemical Geology, 2009, 268 (1~2):147~154
[79]
49 Liu Yu, Wang Yanchao, Li Qiang et al. Tree-ring stable carbon isotope-based May-July temperature reconstruction over Nanwutai, China, for the past century and its record of 20th century warming. Quaternary Science Reviews, 2014, 93 :67~76
[80]
50 Leavitt S W, Long A. The global biosphere as net CO2 source or sink: Evidence from carbon isotopes in tree rings. In:Caldwell D E, Brierley J A, Brierley C L eds. Planetary Ecology. New York:Van Nostrand Reinhold, 1985. 89~99
[81]
51 Freyer H. On the 13 C record in tree rings. Part Ⅰ. 13 C variations in northern hemispheric trees during the last 150 years. Tellus, 1979, 31 (2):124~137
[82]
52 Gagen M, McCarroll D, Robertson I et al. Do tree ring δ 13 C series from Pinus sylvestris in Northern Fennoscandia contain long-term non-climatic trends？Chemical Geology, 2008, 252 (1~2):42~51
[83]
53 Francey R J, Farquhar G D. An explanation of 13 C/12 C variations in tree rings. Nature, 1982, 297 (5861):28~31
[84]
54 Saurer M, Cherubini P, Bonani G et al. Tracing carbon uptake from a natural CO2 spring into tree rings:An isotope approach. Tree Physiology, 2003, 23 (14):997~1004
[85]
55 Schleser G H, Jayasekera R. δ 13 C-variations of leaves in forests as an indication of reassimilated CO2 from the soil. Oecologia, 1985, 65 (4):536~542
[86]
56 Craig H. Carbon-13 variations in Sequoia rings and the atmosphere. Science, 1954, 119 (3083):141~143
[87]
57 Stuiver M, Burk R L, Quay P D. 13 C/12 C ratios in tree rings and the transfer of biospheric carbon to the atmosphere. Journal of Geophysical Research, 1984, 89 (D7):11731~11748
[88]
58 Gagen M, McCarroll D, Loader N J et al. Exorcising the ''segment length curse’: Summer temperature reconstruction since AD 1640 using non-detrended stable carbon isotope ratios from pine trees in Northern Finland. The Holocene, 2007, 17 (4):435~446
[89]
59 Xu Guobao, Chen Tuo, Liu Xiaohong et al. Summer temperature variations recorded in tree-ring δ 13 C values on the northeastern Tibetan Plateau. Theoretical and Applied Climatology, 2011, 105 (1~2):51~63
[90]
60 Leavitt S W, Long A. Stable carbon isotope chronologies from trees in the Southwestern United States. Global Biogeochemical Cycles, 1988, 2 (3):189~198
[91]
61 Saurer M, Siegenthaler U, Schweingruber F. The climate-carbon isotope relationship in tree rings and the significance of site conditions. TellusB, 1995, 47 (3):320~330
[92]
62 Marshall J D, Monserud R A. Co-occurring species differ in tree-ring δ18O trends. Tree Physiology, 2006, 26 (8):1055~1066
[93]
63 Labuhn I, Daux V, Pierre M et al. Tree age, site and climate controls on tree ring cellulose δ18O:A case study on oak trees from south-western France. Dendrochronologia, 2014, 32 (1):78~89
[94]
64 Kress A, Saurer M, Siegwolf R T W et al. A 350 year drought reconstruction from Alpine tree ring stable isotopes. Global Biogeochemical Cycles, 2010, 24 (2):GB2011
[95]
65 Leavitt S W. Tree-ring C-H-O isotope variability and sampling. Science of the Total Environment, 2010, 408 (22):5244~5253
[96]
67 Woodley E J, Loader N J, McCarroll D et al. Estimating uncertainty in pooled stable isotope time-series from tree-rings. Chemical Geology, 2012, 294 :243~248
[97]
68 Boettger T, Friedrich M. A new serial pooling method of shifted tree ring blocks to construct millennia long tree ring isotope chronologies with annual resolution. Isotopes in Environmental and Health Studies, 2009, 45 (1):68~80
[98]
69 Mayr C, Frenzel B, Friedrich M et al. Stable carbon-and hydrogen-isotope ratios of subfossil oaks in Southern Germany:Methodology and application to a composite record for the Holocene. The Holocene, 2003, 13 (3):393~402
[99]
70 Gagen M, McCarroll D, Jalkanen R et al. A rapid method for the production of robust millennial length stable isotope tree ring series for climate reconstruction. Global and Planetary Change, 2012, 82~83 :96~103
[100]
71 Hangartner S, Kress A, Saurer M et al. Methods to merge overlapping tree-ring isotope series to generate multi-centennial chronologies. Chemical Geology, 2012, 294~295 :127~134
[101]
72 Wang Wenzhi, Liu Xiaohong, Shao Xuemei et al. A 200-yr temperature record from tree-ring δ13C at the Qaidam Basin of the Tibetan Plateau after identifying the optimum method to correct for changing atmospheric CO2 and δ 13 C. Journal of Geophysical Research, 2011, 116 (G4):G04022
[102]
73 Xu Guobao, Chen Tuo, Liu Xiaohong et al. Potential linkages between the moisture variability in the northeastern Qaidam Basin, China, since 1800 and the East Asian summer monsoon, as reflected by tree-ring δ18O. Journal of Geophysical Research, 2011, 116 :D09111
[103]
74 Wang Wenzhi, Liu Xiaohong, Xu Guobao et al. Moisture variations over the past millennium characterized by Qaidam Basin tree-ring δ18O. Chinese Science Bulletin, 2013, 58 (32):3956~3961
[104]
75 An Wenling, Liu Xiaohong, Leavitt S W et al. Specific climatic signals recorded in earlywood and latewood δ18O of tree rings in Southwestern China. TellusB, 2012, 64 :18703
[105]
76 Kern Z, Patkó M, Kzmér M et al. Multiple tree-ring proxies(earlywood width, latewood width and δ 13 C)from pedunculate oak(Quercus robur L.), Hungary. Quaternary International, 2013, 293 :257~267
[106]
77 Loader N J, Santillo P M, Woodman-Ralph J P et al. Multiple stable isotopes from oak trees in Southwestern Scotland and the potential for stable isotope dendroclimatology in maritime climatic regions. Chemical Geology, 2008, 252 (1~2):62~71
[107]
78 Young G H F, McCarroll D, Loader N J et al. A 500-year record of summer near-ground solar radiation from tree-ring stable carbon isotopes. The Holocene, 2010, 20 (3):315~324
[108]
79 Loader N J, Young G H F, Grudd H et al. Stable carbon isotopes from Tornetr？sk,Northern Sweden provide a millennial length reconstruction of summer sunshine and its relationship to Arctic circulation. Quaternary Science Reviews, 2013, 62 :97~113
[109]
80 McCarroll D, Loader N J, Jalkanen R et al. A 1200-year multiproxy record of tree growth and summer temperature at the northern pine forest limit of Europe. The Holocene, 2013, 23 (4):471~484
[110]
81 Liu Yu, Wu Xiangding, Leavitt S W et al. Stable carbon isotope in tree rings from Huangling, China and climatic variation. Science in China, 1996, 39 (2):152~161
[111]
82 徐国保. 北疆地区树轮稳定氧同位素比率(δ18O)气候意义. 北京: 中国科学院大学博士学位论文, 2014. 83~92 Xu Guobao. Climatic Significance of Stable Oxygen(δ18O)in Tree-ring in North Part of Xinjiang Uygur Autonomous Region. Beijing:The Doctoral Dissertation of University of Chinese Academy of Sciences, 2014. 83~92
[112]
11 1An Wenling, Liu Xiaohong, Leavitt S W et al. Relative humidity history on the Batang-Litang Plateau of Western China since 1755 reconstructed from tree-ring δ18O and δD. Climate Dynamics, 2014, 42 (9~10):2639~2654
[113]
11 2Liu Weiguo, Feng Xiahong, Liu Yu et al.δ18O values of tree rings as a proxy of monsoon precipitation in arid Northwest China. Chemical Geology, 2004, 206 (1~2):73~80
[114]
11 3Liu Yu, Cai Qiufang, Liu Weiguo et al. Monsoon precipitation variation recorded by tree-ring δ18O in arid Northwest China since AD 1878. Chemical Geology, 2008, 252 (1~2):56~61
[115]
11 4Miller D L, Mora C I, Grissino-Mayer H D et al. Tree-ring isotope records of tropical cyclone activity. Proceedings of the National Academy of Sciences of the United States of America, 2006, 103 (39):14294~14297
[116]
11 5Epstein S, Yapp C J. Climatic implications of the D/H ratio of hydrogen in CH groups in tree cellulose. Earth and Planetary Science Letters, 1976, 30 (2):252~261
[117]
11 6Gori Y, Wehrens R, Greule M et al. Carbon, hydrogen and oxygen stable isotope ratios of whole wood, cellulose and lignin methoxyl groups of Picea abies as climate proxies. Rapid Communications in Mass Spectrometry, 2013, 27 (1):265~275
[118]
11 7Yapp C J, Epstein S. Climatic significance of the hydrogen isotope ratios in tree cellulose. Nature, 1982, 297 (5868):636~639
[119]
11 8Feng Xiahong, Epstein S. Climatic temperature records in δD data from tree rings. Geochimica et Cosmochimica Acta, 1995, 59 (14):3029~3037
[120]
11 9Liu Xiaohong, An Wenling, Leavitt S W et al. Recent strengthening of correlations between tree-ring δ 13 C and δ18O in mesic Western China:Implications to climatic reconstruction and physiological responses. Global and Planetary Change, 2014, 113 :23~33
[121]
12 0Jahren A H, Sternberg L S L O. Annual patterns within tree rings of the Arctic middle Eocene(ca .45Ma):Isotopic signatures of precipitation, relative humidity, and deciduousness. Geology, 2008, 36 (2):99~102
[122]
12 1Helle G, Schleser G H. Beyond CO2-fixation by Rubisco——An interpretation of 13 C/12 C variations in tree rings from novel intra-seasonal studies on broad-leaf trees. Plant, Cell and Environment, 2004, 27 (3):367~380
[123]
12 2Kagawa A, Sugimoto A, Maximov T C. 13 CO2 pulse-labelling of photoassimilates reveals carbon allocation within and between tree rings. Plant, Cell and Environment, 2006, 29 (8):1571~1584
[124]
12 3Kagawa A, Sugimoto A, Maximov T C. Seasonal course of translocation, storage and remobilization of 13 C pulse-labeled photoassimilate in naturally growing Larix gmelinii saplings. New Phytologist, 2006, 171 (4):793~804
[125]
12 4Eglin T, Francois C, Michelot A et al. Linking intra-seasonal variations in climate and tree-ring δ 13 C:A functional modelling approach. Ecological Modelling, 2010, 221 (15):1779~1797
[126]
12 5Leavitt S W. Prospects for reconstruction of seasonal environment from tree-ring δ 13 C:Baseline findings from the Great Lakes area, USA. Chemical Geology, 2002, 192 (1~2):47~58
[127]
12 6Eilmann B, Buchmann N, Siegwolf R et al. Fast response of Scots pine to improved water availability reflected in tree-ring width and δ 13 C. Plant, Cell and Environment, 2010, 33 (8):1351~1360
[128]
12 7Barbour M M, Walcroft A S, Farquhar G D. Seasonal variation in δ 13 C and δ18O of cellulose from growth rings of Pinus radiata. Plant, Cell and Environment, 2002, 25 (11):1483~1499
[129]
12 8Livingston N J, Spittlehouse D L. Carbon isotope fractionation in tree ring early and late wood in relation to intra-growing season water balance. Plant, Cell and Environment, 1996, 19 (6):768~774
[130]
12 9Schulze B, Wirth C, Linke P et al. Laser ablation-combustion-GC-IRMS—A new method for online analysis of intra-annual variation of δ 13 C in tree rings. Tree Physiology, 2004, 24 (11):1193~1201
[131]
13 1Schubert B A, Jahren A H. Quantifying seasonal precipitation using high-resolution carbon isotope analyses in evergreen wood. Geochimica et Cosmochimica Acta, 2011, 75 (22):7291~7303
[132]
13 2Sheu D D, Kou P, Chiu C H et al. Variability of tree-ring δ 13 C in Taiwan fir:Growth effect and response to May-October temperatures. Geochimica et Cosmochimica Acta, 1996, 60 (1):171~177
[133]
13 3Klein T, Hemming D, Lin T et al. Association between tree-ring and needle δ 13 C and leaf gas exchange in Pinus halepensis under semi-arid conditions. Oecologia, 2005, 144 (1):45~54
[134]
13 4Managave S R. Model evaluation of the coherence of a common source water oxygen isotopic signal recorded by tree-ring cellulose and speleothem calcite. Geochemistry, Geophysics, Geosystems, 2014, 15 (4):905~922
[135]
13 5Zhu Mengfang, Stott L, Buckley B et al. Indo-Pacific Warm Pool convection and ENSO since 1867 derived from Cambodian pine tree cellulose oxygen isotopes. Journal of Geophysical Research, 2012, 117 :D11307
[136]
13 6Zhu Mengfang, Stott L, Buckley B et al.20th century seasonal moisture balance in Southeast Asian montane forests from tree celluloseδ18O. Climatic Change, 2012, 115 (3~4):505~517
[137]
13 7 Xu Chenxi, Sano M, Yoshimura K E I et al. Oxygen isotopes as a valuable tool for measuring annual growth in tropical trees that lack distinct annual rings. Geochemical Journal, 2014, 48 (4):371~378
[138]
13 8Managave S R, Ramesh R. Isotope dendroclimatology: A review with a special emphasis on tropics handbook of environmental isotope geochemistry. In: Baskaran M ed. Handbook of Environmental Isotope Geochemistry, Advances in Isotope Geochemistry. Berlin Heidelberg:Springer, 2011. 811~833
[139]
13 9Managave S R, Sheshshayee M S, Borgaonkar H P et al. Past break-monsoon conditions detectable by high resolution intra-annual δ18O analysis of teak rings. Geophysical Research Letters, 2010, 37 (5):L05702
[140]
14 0Managave S, Sheshshayee M, Bhattacharyya A et al. Intra-annual variations of teak cellulose δ18O in Kerala, India:Implications to the reconstruction of past summer and winter monsoon rains. Climate Dynamics, 2010, 37 (3~4):555~567
[141]
14 1Anchukaitis K J, Evans M N. Tropical cloud forest climate variability and the demise of the Monteverde golden toad. Proceedings of the National Academy of Sciences of the United States of America, 2010, 107 (11):5036~5040
[142]
14 2Johnstone J A, Roden J S, Dawson T E. Oxygen and carbon stable isotopes in coast redwood tree rings respond to spring and summer climate signals. Journal of Geophysical Research, 2013, 118 (4):1438~1450
[143]
14 3Berkelhammer M, Stott L D. Modeled and observed intra-ring δ18O cycles within Late Holocene Bristlecone pine tree samples. Chemical Geology, 2009, 264 (1~4):13~23
[144]
14 4Poussart P F, Schrag D P. Seasonally resolved stable isotope chronologies from Northern Thailand deciduous trees. Earth and Planetary Science Letters, 2005, 235 (3):752~765
[145]
14 5Poussart P F, Evans M N, Schrag D P. Resolving seasonality in tropical trees:Multi-decade, high-resolution oxygen and carbon isotope records from Indonesia and Thailand. Earth and Planetary Science Letters, 2004, 218 (3~4):301~316A
