西伯利亚落叶松树轮稳定碳同位素对气候的响应

Abstract

Abstract: Stable isotopes in tree rings are the important approaches in climate reconstruction and in studies on tree response to environmental factors in the past, such as the maximum latewood density, tree ring width and other tree ring parameters. In this paper, the tree ring samples of Larix sibirica Ledeb. collected in south slope of the Altay Mountains in 2009 were used to develop the treering width chronology and stable carbon isotope series based on the standard Dendrochronology methods and stable carbon isotope research achievements. It can establish the detrend series (DS) of stable carbon isotope of tree rings to eliminate atmospheric CO₂ effect from original δ¹³C. The stable carbon isotope series values of L. sibirica tree rings varied in a range of -22.8‰--25.4‰, The average value was -24.0‰, and the coefficient of variation was -0.017. Width chronology and stable carbon isotope detrend series were compared with monthly climatic factors (mean temperature, mean maximum temperature, mean minimum temperature, precipitation, relative humidity and sunshine duration) at Fuyun Meteorological Station. Correlation analysis revealed that there was a strong positive correlation between the stable carbon isotope detrend series and the mean temperature and mean maximum temperature but a negative one between it and the relative humidity in growing season. The correlation coefficient between the detrend series of stable carbon isotope and the monthly maximum temperature in June and July was as high as 0.611 (P<0.000 001), that between it and the monthly relative humidity in June and July was -0.493 (P<0.001), and that between it and monthly precipitation in July was -0.459 (P<0.01). The response of stable carbon isotope of L. sibirica tree rings to temperature and relative humidity in growing season was the most sensitive. The main factor affecting stable carbon isotope of L. sibiricawas the monthly maximum temperature in June and July.

Key words: Larix sibiricaLedeb, tree ring, stable carbon isotope (δ¹³C), climate response, Altay Mountains

ZHANG Rui-Bo, YUAN Yu-Jiang, WEI Wen-Shou, SHANG Hua-Ming, YU Shu-Long, ZHANG Tong-Wen, CHEN Feng, FAN Zi-Ang, QIN Li. Response of Stable Carbon Isotope of Larix sibirica Ledeb. Tree rings to Climate Change[J]., 2012, 29(2): 328-334.

References

Robertson I,Switsur V R,Carter A H C,et al.Signal strength and climate relationships in ¹³C/¹²C ratios of tree ring cellulose form oak in east England〔J〕.Journal of Geophysical Research,1997,106(D16):19 507-19 516.

Leavitt S W,Long A.Seasonal stable carbon isotope variability in tree-rings:Possible paleoenvironmental signals〔J〕.Chemical Geology：Isotope Geoscience Science,1991,87:59-70.

Wilson A T,Grinsted M J.¹³C/¹²C in cellulose and lignin paleathermometer〔J〕.Nature,1977,265:133-135.

Francey R J,Farquhar G D.An explanation of ¹³C/¹²C variations in tree rings〔J〕.Nature,1982,297(5):28-31.

Saurer M,Siegenthaler U.The climate-carbon isotope relationship in tree rings and the significance of site conditions〔J〕.Tellus,1995,46:320-330.

Hemming D L,Waterhouse J S.Climate variation and the stable carbon isotope composition of tree ring Cellulose: An intercomparison of three tree species of Quercus robur,Fagus sylvatica and Pinus silvestris〔J〕.Tellus,1998,50B:25-33.

Valerie A B,Glenn P J,Bruce P F,et al.Reconstruction of Summer temperatures in interior Alaska from tree-ring proxies: Evidence for changing synoptic climate regimes〔J〕.Climatic Change,2004,63:91-120.

Polona H, Tom L.Stable carbon isotopes in Norway Spruce Picea abies(L.) Karst.) tree rings at two sites in Slovenia〔J〕.Zbornik Gozdarstva in Lesarstva,2009,88:43-52.

Slawomira P,Anna P,Stanislaw H.Stable carbon isoptic composition of tree rings from a Pine tree from Augustow Wilderness,Poland,as a temperature and local environment conditions indicator〔J〕.Isotopes Environment Health Study,2004,40(2):145-154.

Alexander V K,Kerstin S T,Anatolii N,et al.Climate signals in treering width,density and δ¹³C from larches in Eastern Siberia(Russia) 〔J〕.Chemical Geology,2008,252:31-41.

Saurer M,Siegenthaler U. ¹³C/¹²C isotope ratios in tree rings are sensitive to relative humidity〔J〕. Dendrochronologia,1989,7:9-13.

Sonninen E,Jungner H.Stable carbon isotope in treerings of a Scots alpine pine (Pinus sylvestris L.) from northern Finland〔J〕.Palaoklimaforschung,1995,15:121-128.

Sheu D D,Kou P,Chiu C H,et al. Variability of tree ring δ¹³C in Taiwan fir:Growth effect and response to May-October temperatures〔J〕. Geochimica et Cosmochimica Acta,1996,60(1):171-177.

Saurer M,Borella S,Schweingruber F,et al.Stable carbon isotope relations in tree-rings of beech:Climatic versus site-related influences〔J〕.Trees,1997,11:291-297.

Liu Yu,Wu Xiangding,Steven W Leavitt,et al.Stable carbon isopote in tree ring from Huangling,China and climatic variation〔J〕.Science in China:Series D,1996,39(2):152-160.

Liu Yu,Ma Limin,Cai Qiufang,et al.Reconstruction of summer temperature (June-August) at Mt.Helan,China,from tree-ring stable carbon isotope values since AD 1890 〔J〕.Science in China:Series D,2002,45(12):1 127-1 136.

Qian Junlong,Lv Jun,Tu Qipu,et a1.Reconstruction of the climate in the Tianmu Mountain area,Zhejiang Province,in the last 160 years by δ¹³C sequence of tree ring αcellulose.〔J〕.Science in China:Series D,2002,45(5):409-419.

Liu Xiaohong,Shao Xuemei,Wang Lili,et al.Climatic significance of the stable carbon isotope composition of tree-ring cellulose:Comparison of Chinese hemlock (Tsuga chinensis Pritz) and alpine pine (Pinus densata Mast) in a temperate-moist region of China〔J〕.Science in China:Series D,2007,50(7):1 076-1 085.

Nuerlan H.Hydrological features of rivers in Altai prefeture〔J〕. Hydrology,2001,21(4):53-55.

Holmes R L.Computer-assisted quality control in tree-ring dating and measurement〔J〕.Tree-Ring Bulletin,1983,43:69-75.

Cook E R.A time series analysis approach to tree-ring atandardization〔D〕. Tucson:The University of Arizona,1985.

Beerling D J,Heath J,Mansfield T A. Drought CO₂ interactions in trees observations and mechanism〔J〕. New Phytol,1996,134(2):235-242.

Leavitt S W,Lara A.South American tree rings show δ¹³C declining trend〔J〕.Tellus,1994,46:152-157.

Danny M C,Neil J L.Stable isotopes in tree rings〔J〕.Quaternary Science Reviews,2004,23:771-801.

Keeling C D,Mook W M,Tans P.Recent trends in the ¹³C/¹²C isotopes of atmosphere dioxide〔J〕.Nature,1979,277(11):121-123.

O’Leary M H.Carbon isotopes in photosynthesis〔J〕.BioScience,1988,38(5):328-336.

Porte A,Loustau D.Seasonal and interannual variations in carbon isotope discrimination in a maritime pine(Pinus pinaster) stand assessed from the isotopic composition of cellulose in annual rings〔J〕. Tree Physiology,2001,21 (12/13):861-868.

Duquesnay A,Breda N,Stievenard M,et al. Changes of tree ring δ¹³C and water-use efficiency of beech (Fagus sylvaticaL.) in Northwestern France during the past century〔J〕. Plant Cell and Environment,1998,21:565-572.

Lipp J,Trimborn P,Fritz P. Stable isotopes in tree ring cellulose and climate change〔J〕. Tellus,1991,43(B):322-330.

McCarroll D,Pawellek F.Stable carbon isotope ratios of Pinus sylvestris from northern Finland and the potential for extracting a climate signal from long Fennoscandian chronologies〔J〕.The Holocene,2001,11:517-526.

Schleser G H,Frielingsdorf J,Blair A.Carbon isotope behaviour in wood and cellulose during artifcial aging〔J〕.Chemical Geology,1999,158:121-130.

Beerling D J.Predicting leaf gas exchange and δ¹³C response to the past 30 000 years of global environmental change〔J〕.New Phytologist,1994,128:425-433.

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Response of Stable Carbon Isotope of Larix sibirica Ledeb. Tree rings to Climate Change

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