长白山落叶松与鱼鳞云杉生长-气候关系的种间差异
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摘要
为阐明不同树种间树木径向生长对气候变化的响应及其时间稳定性,本研究以长白山北坡高海拔处(1600～1750 m)落叶松和鱼鳞云杉为研究对象,运用年轮年代学方法探究树木径向生长与气候的关系.结果表明:研究区落叶松生长与当年6月最高气温呈显著正相关,与当年6月降水呈负相关;鱼鳞云杉与当年5月最高温度呈显著正相关.冗余分析进一步表明,落叶松生长主要受夏季温度的影响,鱼鳞云杉生长主要受春季温度的制约.在1959—2014年,落叶松生长-夏季温度关系相对稳定;对于鱼鳞云杉,自1986年以来其与春季温度的相关性减弱,可能由于最高温度降低导致树木生长减慢.本研究结果可以为预测气候变化情景下长白山针叶树种生长的响应趋势提供数据支持和理论参考.
To clarify the responses of radial growth of different tree species to climate change and its stability, we explored the relationships between radial growth and climate factors of larch(Larix olgensis) and spruce(Picea jezoensis var. komarovii) distributed at high altitude(1600-1750 m) on the northern slope of Changbai Mountain, using the chronological method. The results showed that the growth of larch was significantly positively correlated with the maximum temperature in June and negatively correlated with the precipitation in June. The radial growth of spruce was significantly positively correlated with the maximum temperature in May. Results from redundancy analysis showed that larch growth was mainly affected by summer temperature, while spruce growth was significantly restricted by spring temperature. During 1959-2014, the relationship between larch growth and summer temperature was relatively stable. For spruce, the correlation between radial growth and spring temperatures had gradually weakened since 1986, mainly due to the growth slowdown because of decreased maximum air temperature. Our results provide theoretical references for predicting the growth response of conifers at Changbai Mountain region in the context of climate change.
To clarify the responses of radial growth of different tree species to climate change and its stability, we explored the relationships between radial growth and climate factors of larch(Larix olgensis) and spruce(Picea jezoensis var. komarovii) distributed at high altitude(1600-1750 m) on the northern slope of Changbai Mountain, using the chronological method. The results showed that the growth of larch was significantly positively correlated with the maximum temperature in June and negatively correlated with the precipitation in June. The radial growth of spruce was significantly positively correlated with the maximum temperature in May. Results from redundancy analysis showed that larch growth was mainly affected by summer temperature, while spruce growth was significantly restricted by spring temperature. During 1959-2014, the relationship between larch growth and summer temperature was relatively stable. For spruce, the correlation between radial growth and spring temperatures had gradually weakened since 1986, mainly due to the growth slowdown because of decreased maximum air temperature. Our results provide theoretical references for predicting the growth response of conifers at Changbai Mountain region in the context of climate change.
引文
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[8] van der Maaten-Theunissen M,Kahle HP,van der Maaten E.Drought sensitivity of Norway spruce is higher than that of silver fir along an altitudinal gradient in southwestern Germany.Annals of Forest Science,2013,70:185-193
[9] Franceschini T,Bontemps JD,Perez V,et al.Divergence in latewood density response of Norway spruce to temperature is not resolved by enlarged sets of climatic predictors and their non-linearities.Agricultural and Forest Meteorology,2013,180:132-141
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[11] Shao X-M (邵雪梅),Wu X-D (吴祥定).Reconstruction of climate change on Changbai Mountain,Northeast China using tree-ring data.Quaternary Sciences (第四纪研究),1997,3(1):76-85 (in Chinese)
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[13] Yu D-P (于大炮),Wang S-Z (王顺忠),Tang L-N (唐立娜),et al.Relationship between tree-ring chronology of Larix olgensis in Changbai Mountains and the climate change.Chinese Journal of Applied Ecology (应用生态学报),2005,16(1):14-20 (in Chinese)
[14] Kendall MG.Rank Correlation Methods.London:Griffin,1970
[15] Kolher MA.On the use of double-mass analysis for testing the consistency of meteorological records and for making required adjustments.Bulletin of the American Meteorology Society,1949,82:96-97
[16] Chen L (陈力),Yin Y-H (尹云鹤),Zhao D-S (赵东升),et al.Climate response of tree growth along an altitudinal gradient in the Changbai Mountains,Northeast China.Acta Ecologica Sinica (生态学报),2014,34(6):1568-1574 (in Chinese)
[17] Fkiri S,Guibal F,Fady B,et al.Tree-rings to climate relationships in nineteen provenances of four black pines sub-species (Pinus nigra Arn.) growing in a common garden from Northwest Tunisia.Dendrochronologia,2018,50:44-51
[18] He MH,Shishov V,Kaparova N,et al.Process-based modeling of tree-ring formation and its relationships with climate on the Tibetan Plateau.Dendrochronologia,2017,42:31-41
[19] Zhang WT,Jiang Y,Wang MC,et al.Topography- and species-dependent climatic responses in radial growth of Picea meyeri and Larix principis-rupprechtii in the Luya-shan Mountains of North-Central China.Forests,2015,6:116-132
[20] Davi H,Dufrene E,Francois C,et al.Sensitivity of water and carbon fluxes to climate changes from 1960 to 2100 in European forest ecosystems.Agricultural and Forest Meteorology,2006,141:35-56
[21] Gai XR,Wang SL,Zhou L,et al.Spatiotemporal evidence of tree-growth resilience to climate variations for Yezo spruce (Picea jezoensis var.komarovii) on Changbai Mountain,Northeast China.Journal of Forestry Research,2018,https://doi.org/10.1007/s11676-018-0802-7
[22] Leonelli G,Pelfini M,Battipaglia G,et al.Site-aspect influence on climate sensitivity over time of a high-altitude Pinus cembra tree-ring network.Climatic Change,2009,96:185-201
[23] Chen ZJ,Zhang XL,He XY,et al.Extension of summer (June-August) temperature records for northern Inner Mongolia (1715-2008),China using tree rings.Quaternary International,2013,283:21-29
[24] Kharuk VI,Ranson KJ,Petrov IA,et al.Larch (Larix dahurica Turcz) growth response to climate change in the Siberian permafrost zone.Regional Environmental Change,2019,19:233-243
[25] Dulamsuren C,Khishigjargal M,Leuschner C,et al.Response of tree-ring width to climate warming and selective logging in larch forests of the Mongolian Altai.Journal of Plant Ecology,2014,7:24-38
[26] Walker X,Johnstone JF.Widespread negative correlations between black spruce growth and temperature across topographic moisture gradients in the boreal forest.Environmental Research Letters,2014,9,doi:10.1088/1748-9326/9/6/064016
[27] Zhu LJ,Cooper DJ,Yang JW,et al.Rapid warming induces the contrasting growth of Yezo spruce (Picea jezoensis var.microsperma) at two elevation gradient sites of Northeast China.Dendrochronologia,2018,50:52-63
[28] Sanchez-Salguero R,Camarero JJ,Gutierrez E,et al.Climate warming alters age-dependent growth sensitivity to temperature in Eurasian alpine treelines.Forests,2018,9,688
[29] Wang XC,Zhang MH,Ji Y,et al.Temperature signals in tree-ring width and divergent growth of Korean pine response to recent climate warming in northeast Asia.Trees:Structure and Function,2017,31:415-427
[30] Camarero JJ,Sanchez-Salguero R,Sanguesa-Barreda G,et al.Tree species from contrasting hydrological niches show divergent growth and water-use efficiency.Dendrochronologia,2018,52:87-95
[2] Colenutt ME,Luckman BH.Dendrochronological investigation of Larix lyallii at Larch Valley,Alberta.Canadian Journal of Forest Research,1991,21:1222-1233
[3] Chen L (陈力),Wu S-H (吴绍洪),Dai E-F (戴尔阜).Analysis of the tree-ring width chronologies of Pinus koraiensis and Larix olgensis on Changbai Mountains,Northeast China.Geographical Research (地理研究),2011,30(6):1147-1155 (in Chinese)
[4] Yu DP,Liu JQ,Lewis BJ,et al.Spatial variation and temporal instability in the climate-growth relationship of Korean pine in the Changbai Mountain region of Northeast China.Forest Ecology and Management,2013,300:96-105
[5] Babst F,Poulter B,Trouet V,et al.Site- and species-specific responses of forest growth to climate across the European continent.Global Ecology and Biogeography,2013,22:706-717
[6] Yu DP,Wang GG,Dai LM,et al.Dendroclimatic analysis of Betula ermanii forests at their upper limit of distribution in Changbai Mountain,Northeast China.Forest Ecology and Management,2007,240:105-113
[7] Li G-Q (李广起),Bai F (白帆),Sang W-G (桑卫国).Different responses of radial growth to climate warming in Pinus koraiensis and Picea jezoensis var.komarovii at their upper elevational limits in Changbai Mountain,China.Chinese Journal of Plant Ecology (植物生态学报),2011,35(5):500-511 (in Chinese)
[8] van der Maaten-Theunissen M,Kahle HP,van der Maaten E.Drought sensitivity of Norway spruce is higher than that of silver fir along an altitudinal gradient in southwestern Germany.Annals of Forest Science,2013,70:185-193
[9] Franceschini T,Bontemps JD,Perez V,et al.Divergence in latewood density response of Norway spruce to temperature is not resolved by enlarged sets of climatic predictors and their non-linearities.Agricultural and Forest Meteorology,2013,180:132-141
[10] Wang H,Shao XM,Jiang Y,et al.The impacts of climate change on the radial growth of Pinus koraiensis along elevations of Changbai Mountain in northeastern China.Forest Ecology and Management,2013,289:333-340
[11] Shao X-M (邵雪梅),Wu X-D (吴祥定).Reconstruction of climate change on Changbai Mountain,Northeast China using tree-ring data.Quaternary Sciences (第四纪研究),1997,3(1):76-85 (in Chinese)
[12] Gao L-S (高露双),Wang X-M (王晓明),Zhao X-H (赵秀海).Response of Pinus koraiensis and Picea jezoensis var.komarovii to climate in the transition zone of Changbai Mountain,China.Chinese Journal of Plant Ecology (植物生态学报),2011,35(1):27-34 (in Chinese)
[13] Yu D-P (于大炮),Wang S-Z (王顺忠),Tang L-N (唐立娜),et al.Relationship between tree-ring chronology of Larix olgensis in Changbai Mountains and the climate change.Chinese Journal of Applied Ecology (应用生态学报),2005,16(1):14-20 (in Chinese)
[14] Kendall MG.Rank Correlation Methods.London:Griffin,1970
[15] Kolher MA.On the use of double-mass analysis for testing the consistency of meteorological records and for making required adjustments.Bulletin of the American Meteorology Society,1949,82:96-97
[16] Chen L (陈力),Yin Y-H (尹云鹤),Zhao D-S (赵东升),et al.Climate response of tree growth along an altitudinal gradient in the Changbai Mountains,Northeast China.Acta Ecologica Sinica (生态学报),2014,34(6):1568-1574 (in Chinese)
[17] Fkiri S,Guibal F,Fady B,et al.Tree-rings to climate relationships in nineteen provenances of four black pines sub-species (Pinus nigra Arn.) growing in a common garden from Northwest Tunisia.Dendrochronologia,2018,50:44-51
[18] He MH,Shishov V,Kaparova N,et al.Process-based modeling of tree-ring formation and its relationships with climate on the Tibetan Plateau.Dendrochronologia,2017,42:31-41
[19] Zhang WT,Jiang Y,Wang MC,et al.Topography- and species-dependent climatic responses in radial growth of Picea meyeri and Larix principis-rupprechtii in the Luya-shan Mountains of North-Central China.Forests,2015,6:116-132
[20] Davi H,Dufrene E,Francois C,et al.Sensitivity of water and carbon fluxes to climate changes from 1960 to 2100 in European forest ecosystems.Agricultural and Forest Meteorology,2006,141:35-56
[21] Gai XR,Wang SL,Zhou L,et al.Spatiotemporal evidence of tree-growth resilience to climate variations for Yezo spruce (Picea jezoensis var.komarovii) on Changbai Mountain,Northeast China.Journal of Forestry Research,2018,https://doi.org/10.1007/s11676-018-0802-7
[22] Leonelli G,Pelfini M,Battipaglia G,et al.Site-aspect influence on climate sensitivity over time of a high-altitude Pinus cembra tree-ring network.Climatic Change,2009,96:185-201
[23] Chen ZJ,Zhang XL,He XY,et al.Extension of summer (June-August) temperature records for northern Inner Mongolia (1715-2008),China using tree rings.Quaternary International,2013,283:21-29
[24] Kharuk VI,Ranson KJ,Petrov IA,et al.Larch (Larix dahurica Turcz) growth response to climate change in the Siberian permafrost zone.Regional Environmental Change,2019,19:233-243
[25] Dulamsuren C,Khishigjargal M,Leuschner C,et al.Response of tree-ring width to climate warming and selective logging in larch forests of the Mongolian Altai.Journal of Plant Ecology,2014,7:24-38
[26] Walker X,Johnstone JF.Widespread negative correlations between black spruce growth and temperature across topographic moisture gradients in the boreal forest.Environmental Research Letters,2014,9,doi:10.1088/1748-9326/9/6/064016
[27] Zhu LJ,Cooper DJ,Yang JW,et al.Rapid warming induces the contrasting growth of Yezo spruce (Picea jezoensis var.microsperma) at two elevation gradient sites of Northeast China.Dendrochronologia,2018,50:52-63
[28] Sanchez-Salguero R,Camarero JJ,Gutierrez E,et al.Climate warming alters age-dependent growth sensitivity to temperature in Eurasian alpine treelines.Forests,2018,9,688
[29] Wang XC,Zhang MH,Ji Y,et al.Temperature signals in tree-ring width and divergent growth of Korean pine response to recent climate warming in northeast Asia.Trees:Structure and Function,2017,31:415-427
[30] Camarero JJ,Sanchez-Salguero R,Sanguesa-Barreda G,et al.Tree species from contrasting hydrological niches show divergent growth and water-use efficiency.Dendrochronologia,2018,52:87-95