Abstract
Global warming causes an unstable response in tree radial growth at high latitudes in the Northern Hemisphere. Additionally, different climatic responses of different age groups of trees have been found due to their different physiological mechanisms. In this study, the response stability and growth trend of three age groups (young < 100a, middle 100–200a, old ≥ 200a) of Picea schrenkiana (Schrenk spruce) to climate change and the causes of the different responses in different age groups were analyzed in the relatively dry climate of the eastern Tianshan Mountains. The results showed that: (1) With the abrupt increase in temperature in 1989, the annual mean minimum temperature became the dominant radial growth-limiting factor of the three age groups of Schrenk spruce. (2) The radial growth of the middle and young groups was more sensitive than that of the old group based on growth-climate correlation analysis. (3) The radial growth of the different age groups had different responses to climate factors, and all age groups were unstable on time scales. (4) The trend of the linear regression simulation of the basal area increment (BAI) indicated that the Schrenk spruce had the same growth trends in different age groups with growth first increased and then decreased; however, the decreased growth rate was higher in the middle and young age groups than in the old age group after the abrupt increase in temperature. Therefore, we should pay active attention to the impact of drought on Schrenk spruce in the eastern Tianshan Mountains and should particularly strengthen the conservation and management of the middle and young age groups.
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References
Biondi F, Waikul K (2004) DENDROCLIM2002: a program for statistical calibration of climate signals in tree-ring chronologies. Computers & Geosciences 30: 303–311. https://doi.org/10.1016/j.cageo.2003.11.004
Bond BJ (2000) Age-related changes in photosynthesis of woody plants. Trends in Plant Science 5: 349–353. https://doi.org/10.1016/S1360-1385(00)01691-5
Cahoon SMP, Sullivan PF, Brownlee AH, et al. (2018) Contrasting drivers and trends of coniferous and deciduous tree growth in interior Alaska. Ecology 99(6): 1284–1295. https://doi.org/10.1002/ecy.2223
Carrer M, Urbinati C (2004) Age-dependent tree-ring growth responses to climate in Larix decidua and Pinus cembra. Ecology 85: 730–740. https://doi.org/10.2307/3450399
Chen F, Yuan YJ, Wei WS, et al. (2014) Tree-ring recorded hydroclimatic change in Tienshan mountains during the past 500 years. Quaternary International, 358: 35–41. https://doi.org/10.1016/j.quaint.2014.09.057
Chen F, Shang HM, Yuan YJ, et al. (2016) Dry/wet variations in the eastern Tien Shan (China) since AD 1725 based on Schrenk spruce (Picea schrenkiana Fisch. et Mey) tree rings. Dendrochronologia 40: 110–116. https://doi.org/10.1016/j.dendro.2016.07.003
Cook ER, Peters K (1997) Calculating unbiased tree-ring indices for the study of climatic and environmental change. Holocene 7(3): 361–370. https://doi.org/10.1177/095968369700700314
Cox PM, Pearson D, Booth BB, et al. (2013) Sensitivity of tropical carbon to climate change constrained by carbon dioxide variability. Nature 494: 341–345. https://doi.org/10.1038/nature11882
D’Arrigo R, Jacoby G, Buckley B, et al. (2009) Tree growth and inferred temperature variability at the North American Arctic treeline. Global Planet Change 65: 71–82. https://doi.org/10.1016/j.gloplacha.2008.10.011
D’Arrigo R, Wilson R, Liepert B, et al. (2008) On the “Divergence Problem” in Northern Forests: A review of the tree-ring evidence and possible causes. Global and Planetary Change 60: 289–305. https://doi.org/10.1016/j.gloplacha.2007.03.004
D’Arrigo R, Kaufman RK, Davi N, et al. (2004) Thresholds for warming-induced growth decline at elevational tree line in the Yukon Territory, Canda. Global Biogeochemical Cycles 18(3): GB3021. https://doi.org/10.1029/2004gb002249
Ewane BE, Lee HH (2017) Tree-ring reconstruction of streamflow for Palgong Mountain forested watershed in outheastern South Korea. Journal of Mountain Science 14(1): 60–76. https://doi.org/10.1007/s11629-016-3860-3
Franceschini T, Bontemps JD, Perez V, et al. (2013) Divergence in latewood density response of Norway spruce to temperature is not resolved by enlarged sets of climatic predictors and their nonlinearities. Agricultural and Forest Entomology 180: 132–141. https://doi.org/10.1016/j.agrformet.2013.05.011
Fritts HC (1976) Tree Rings and Climate. London: Academic Press, 1976: 11–14. https://doi.org/10.1038/scientificamerican0572-92
Gai XR, Yu DP, Wang SL, et al. (2017) Research progress on the formation mechanism of climate “divergence problem”. Chinese Journal of Ecology 36(11): 3273–3280. (In Chinese) https://doi.org/10.13292/j.1000-4890.201711.005
Gao LL, Gou XH, Deng Y, et al. (2013) Climate.growth analysis of Qilian juniper across an altitudinal gradient in the central Qilian Mountains, northwest China. Trees 27: 379–388. https://doi.org/10.1007/s00468-012-0776-6
Girardin MP, Bouriaud O, Hogg EH, et al. (2016) No growth stimulation of Canada’s boreal forest under half-century of combined warming and CO2 fertilization. Proceedings of the National Academy of Sciences USA 113(52): E8406–E8414. https://doi.org/10.1073/pnas.1610156113
Gómez-Guerrero A, Silva LCR, Barrera-Reyes M, et al. (2013) Growth decline and divergent tree ring isotopic composition (δ13C and δ18O) contradict predictions of CO2 stimulation in high altitudinal forests. Global Change Biology 19: 1748–1758. https://doi.org/10.1111/gcb.12170
Goossens C, Berger A (1987) How to Recognize an Abrupt Climatic Change? Abrupt Climatic Change 31–45. https://doi.org/10.1007/978-94-009-3993-6_3
Hadad MA, Juñent FAR, Boninsegna JA, et al. (2015) Age effects on the climatic signal in Araucaria araucana from xeric sites in Patagonia, Argentina. Plant Ecology & Diversity 8: 343–351. https://doi.org/10.1080/17550874.2014.980350
Holmes RL (1983) Computer-assisted quality control in Tree-ring dating and measurement. Tree-Ring Bulletin. https://doi.org/51-67.10.1006/biol.1999.0214
Huo YX, Gou XH, Liu WH, et al. (2017) Climate-growth relationships of Schrenk spruce (Picea schrenkiana) along an altitudinal gradient in the western Tianshan mountains, northwest China. Trees, 31: 429–439. https://doi.org/10.1007/s00468-017-1524-8
Jacoby GC, Darrigo RD (1995) Tree-ring width and density evidence of climatic and potential forest change in Alaska. Global Biogeochemical Cycles 9: 227–234. https://doi.org/10.1029/95GB00321
Jiang P, Liu HY, Wu XC, et al. (2016) Tree-ring-based SPEI reconstruction in central Tianshan Mountains of China since A.D. 1820 and links to westerly circulation. International Journal of Climatology 37: 2863–2872. https://doi.org/10.1002/joc.4884
Jiang Y, Zhang WT, Wang MC, et al. (2014) Radial growth of two dominant montane conifer tree species in response to climate change in north-central China. Plos One 9: e112537. https://doi.org/10.1371/journal.pone.0112537
Jiao L, Jiang Y, Wang M, et al. (2015) Divergent responses to climate factors in the radial growth of Larix sibirica in the eastern Tianshan Mountains, northwest China. Trees 29: 1673–1686. https://doi.org/10.1007/s00468-015-1248-6
Jiao L, Jiang Y, Wang MC, et al. (2016) Responses to climate change in radial growth of Picea schrenkiana along elevations of the eastern Tianshan Mountains, northwest China. Dendrochronologia 40: 117–127. https://doi.org/10.1016/j.dendro.2016.09.002
Jiao L, Jiang Y, Wang M, et al. (2017) Age-Effect Radial Growth Responses of Picea schrenkiana to Climate Change in the eastern Tianshan Mountains, Northwest China. Forests 8: 294. https://doi.org/10.3390/f8090294
Jiao L, Jiang Y, Zhang WT, et al. (2019) Assessing the stability of radial growth responses to climate change by two dominant conifer trees species in the Tianshan Mountains, northwest China. Forest Ecology and Management 433: 667–677. https://doi.org/10.1016/j.foreco.2018.11.04
Joana V, Filipe C, Cristina N (2009) Age-dependent responses of tree-ring growth and intra-annual density fluctuations of Pinus pinaster to Mediterranean climate. Trees 23(2): 257–265. https://doi.org/10.1007/s00468-008-0273-0
Lebourgeois F, Mérian P, Courdier F, et al. (2012) Instability of climate signal in tree-ring width in Mediterranean mountains: a multi-species analysis. Trees 26: 715–729. https://doi.org/10.1007/s00468-011-0638-7
Li JF (1991) Climate of **njiang. China Meteorological Press P97–104. (In Chinese)
Li ZS, Liu GH, Fu BJ, et al. (2012) Anomalous temperature-growth response of Abies faxoniana to sustained freezing stress along elevational gradients in China’s Western Si-Chuan Province. Trees 26: 1373–1388. https://doi.org/10.1007/s00468-012-0712-9
Liang EY, Shao XM, Eckstein D, et al. (2006) Topography-and species-dependent growth responses of Sabina przewalskii and Picea crassifolia to climate on the northeast. Forest Ecology and Management 236(2–3): 268–277. https://doi.org/10.1016/j.foreco.2006.09.016
Malanson GP (2017) Mixed signals in trends of variance in high-elevation tree ring chronologies. Journal of Mountain Science 14(10): 62–69. https://doi.org/10.1007/s11629-017-4425-9
Oberhuber W, Kofler W, Pfeifer K, et al. (2008) Long-term changes in tree-ring-climate relationships at Mt. Patscherkofel (Tyrol, Austria) since the mid-1980s. Trees 22: 31–40. https://doi.org/10.1007/s00468-007-0166-7
Ogle K, Whitham TG, Cobb NS (2000) Tree-ring variation in pinyon predicts likelihood of death following severe drought. Ecology 81(11):3237–3243. https://doi.org/10.1890/0012-9658(2000)081[3237:TRVIPP]2.0.CO;2
Palombo C, Battipaglia G, Cherubini P, et al. (2014) Warming-related growth responses at the southern limit distribution of mountain pine (Pinus mugo Turra subsp. mugo). Journal of Vegetation Science 25: 571–583. https://doi.org/10.1111/jvs.12101
Peng JF, Gou XH, Chen FH, et al. (2005) Tree ring climate records of spruce and Siberian larch. Ecology and Environment 14(4): 460–465. (In Chinese)
Peng SS, Piao SL, Ciais P, et al. (2013) Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation. Nature 501: 88–92. https://doi.org/10.1038/nature12434
Pichler P, Oberhuber W (2007) Radial growth response of coniferous forest trees in an inner Alpine environment to heatwave in 2003. Forest Ecology and Management 242: 688–699. https://doi.org/10.1016/j.foreco.2007.02.007
Pompa-García M, Hadad MA (2016) Sensitivity of pines in Mexico to temperature varies with age. Atmósfera 29: 209–219. https://doi.org/10.20937/ATM.2016.29.03.03
Qi ZH, Liu HY, Wu XC, et al. (2015) Climate-driven speedup of alpine treeline forest growth in the Tianshan Mountains, Northwestern China. Global Change Biology 21: 816–826. https://doi.org/10.1111/gcb.12703
Richard W, Róisín CJ, William M, et al. (2017) Dynamics of canopy stomatal conductance, transpiration, and evaporation in a temperate deciduous forest, validated by carbonyl sulfide uptake. Biogeosciences 14: 389–401. https://doi.org/10.5194/bg-14-389-2017
Rossi S, Deslauriers A, Anfodillo T, et al. (2008) Age-dependent xylogenesis in timberline conifers. New Phytologist 177(1): 199–208. https://doi.org/10.1111/j.1469-8137.2007.02235.x
Rozas V, DeSoto L, Olano JM (2009) Sex-specific, age-dependent sensitivity of tree-ring growth to climate in the dioecious tree Juniperus thurifera. New Phytologist 182(3): 687–697.
Rozas V, Olano JM, DeSoto L, et al. (2008) Large-scale structural variation and long-term growth dynamics of Juniperus thurifera trees in a managed woodland in Soria, central Spain. Annals of Forest Science 65: 809. https://doi.org/10.1051/forest:2008066
Rubino DL, McCarthy BC (2000) Dendroclimatological analysis of white oak (Quercus alba L., Fagaceae) from an old-growth forest of southeastern Ohio, USA. Journal of the Torrey Botanical Society 127: 240–250. https://doi.org/10.2307/3088761
Ruiz-Benito P, Madrigal-González J, Young S, et al. (2015) Climatic stress during stand development alters the sign and magnitude of age-related growth responses in a subtropical mountain pine. Plos One 10: e0126581. https://doi.org/10.1371/journal.pone.0126581
Schuster R, Oberhuber W (2013a) Age-dependent climate-growth relationships and regeneration of Picea abies in a drought-prone mixed-coniferous forest in the Alps. Canadian Journal of Forest Research 43: 609–618. https://doi.org/10.1139/cjfr-2012-0426
Schuster R, Oberhuber W (2013b) Drought sensitivity of three co-occurring conifers within a dry inner Alpine environment. Trees 27: 61–69. https://doi.org/10.1007/s00468-012-0768-6
Shao XM (1997) Advancements in dendrochronology. Quaternary Sciences 17(3): 265–271.
Sun J, Liu Y (2015) Age-independent climate-growth response of Chinese pine (Pinus tabulaeformis Carrière) in North China. Trees 29: 397–406. https://doi.org/10.1007/s00468-014-1119-6
Szeicz JM, MacDonald GM (1994) Age-dependent tree-ring growth responses of subarctic white spruce to climate. Canadian Journal of Forest Research 24(1): 120–132. https://doi.org/10.1139/x94-017
Vicente-Serrano SM, Beguería S, López-Moreno JI (2010) A multiscalar drought index sensitive to global warming: The Standardized Precipitation Evapotranspiration Index. Journal of Climate 23: 1696–1718. https://doi.org/10.1175/2009JCLI2909.1
Vieira J, Campelo F, Nabais C (2009) Age-dependent responses of tree-ring growth and intra-annual density fluctuations of Pinus pinaster to Mediterranean climate. Trees 23: 257–265. https://doi.org/10.1007/s00468-008-0273-0
Wang XC, Zhang YD. McRae DJ (2009) Spatial and age-dependent tree-ring growth responses of Larix gmelinii to climate in ortheastern China. Trees 23: 875–885. https://doi.org/10.1007/s00468-009-0329-9
White PB, Soule P, Gevel S (2014) Impacts of human disturbance on the temporal stability of climate-growth relationships in a red spruce forest, southern Appalachian Mountains, USA. Dendrochronologia 32: 71–77. https://doi.org/10.1016/j.dendro.2013.10.001
Marchand W, Girardin MP, Hartmann H, et al. (2019) Taxonomy, together with ontogeny and growing conditions, drives needleleaf species’ sensitivity to climate in boreal North. Global Change Biology. https://doi.org/10.1111/gcb.14665
Wu GJ, Liu XH, Chen T, et al. (2015) Long-term variation of tree growth and intrinsic water-use efficiency in Schrenk spruce with increasing CO2 concentration and climate warming in the western Tianshan Mountains, China. Acta Physiologiae Plantarum 37: 150. https://doi.org/10.1007/s11738-015-1903-y
Wu GJ, Xu GB, Chen T, et al. (2013) Age-dependent tree-ring growth responses of Schrenk spruce (Picea schrenkiana) to climate-A case study in the Tianshan Mountain, China. Dendrochronologia 31(4): 318–326. https://doi.org/10.1016/j.dendro.2013.01.001
Xu GB, Liu XH, Qin DH, et al. (2014a) Tree-ring δ18O evidence for the drought history of eastern Tianshan Mountains, northwest China since 1700 AD. International Journal of Climatology 34: 3336–3347. https://doi.org/10.1002/joc.3911
Xu GB, Liu XH, Kang SC, et al. (2018) Age-dependent impacts of climate change and intrinsic water-use efficiency on the growth of Schrenk spruce (Picea schrenkiana) in the western Tianshan Mountains, China. Forest Ecology and Management 414: 1–14. https://doi.org/10.1016/j.foreco.2018.02.008
Xu Y, Li WJ, Shao XM, Xu ZH, et al. (2014b) Long-term trends in intrinsic water-use efficiency and growth of subtropical Pinus tabulaeformis Carr. and Pinus taiwanensis Hayata in central China. Journal of Soils and Sediments 14: 917–927. https://doi.org/10.1007/s11368-014-0878-4
Yao J, Chen Y, Zhao Y, et al. (2018) Response of vegetation NDVI to climatic extremes in the arid region of Central Asia: A case study in **njiang, China. Theoretical and Applied Climatology 131: 1503–1515. https://doi.org/10.1007/s00704-017-2058-0
Yu D, Liu J, Zhou L, et al. (2013) 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 300: 96–105. https://doi.org/10.1016/j.foreco.2012.06.032
Zhang QB, Cheng GD, Yao TD, et al. (2003) 2326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophysical Research Letters 30(14): 1739. https://doi.org/10.1029/2003GL017425.
Zhang RB, Yuan YJ, Gou XH, et al. (2016) Intra-annual radial growth of Schrenk spruce (Picea schrenkiana Fisch. et Mey) and its response to climate on the northern slopes of the Tianshan Mountains. Dendrochronologia 40: 36–42. https://doi.org/10.1016/j.dendro.2016.06.002
Zhang RB, Yuan YJ, Yu SL, et al. (2017) Past changes of spring drought in the inner Tianshan Mountains, China, as recorded by tree rings. Boreas 46: 688–696. https://doi.org/10.1111/bor.12238
Zhang RB, Qin L, Shang HM, et al. (2020) “Climatic change in southern Kazakhstan since 1850 C.E. inferred from tree rings”. International Journal of Biometeorology. https://doi.org/10.1007/s00484-020-01873-5
Zhang TW, Zhang RB, Yuan YJ, et al. (2015) Reconstructed precipitation on a centennial timescale from tree rings in the western Tien Shan Mountains, Central Asia. Quaternary International 358: 58–67. https://doi.org/10.1016/j.quaint.2014.10.054
Zhang TW, Lu B, Zhang RB, et al. (2019a) A 256-year-long precipitation reconstruction for northern Kyrgyzstan based on tree-ring width. International Journal of Climatology 40: 1477–1491. https://doi.org/10.1002/joc.6280
Zhang TW, Zhang RB, Jiang SX, et al. (2019b) On the ‘Divergence Problem’ in the Alatau Mountains, Central Asia: A Study of the Responses of Schrenk Spruce Tree-Ring Width to Climate under the Recent Warming and Wetting Trend. Atmosphere 2019, 10: 473. https://doi.org/10.3390/atmos10080473
Acknowledgments
This research was supported by the National Natural Science Foundation of China (Projects No. 41861006 and 41630750), the Scientific Research Program of Higher Education Institutions of Gansu Province (2018C-02) and the Research Ability Promotion Program for Young Teachers of Northwest Normal University (NWNU-LKQN2019-4). We also thank the anonymous referees for helpful comments on the manuscript.
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Jiao, L., Chen, K., Wang, Sj. et al. Stability evaluation of radial growth of Picea schrenkiana in different age groups in response to climate change in the eastern Tianshan Mountains. J. Mt. Sci. 17, 1735–1748 (2020). https://doi.org/10.1007/s11629-019-5703-5
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DOI: https://doi.org/10.1007/s11629-019-5703-5