Climate-growth relationships of Pinus tabuliformis along an altitudinal gradient on Baiyunshan Mountain, Central China

doi:10.1007/s11676-023-01684-5

摘要/Abstract

Abstract:

A set of standard chronologies for tree-ring width (TRW), earlywood width (EWW) and latewood width (LWW) in Pinus tabuliformis Carr. along an altitudinal gradient (1450, 1400, and 1350 m a.s.l.) on Baiyunshan Mountain, Central China to analyze the effect of varying temperature and precipitation on growth along the gradient. Correlation analyses showed that at all three altitudes and the TRW and EWW chronologies generally had significant negative correlations with mean and maximum temperatures in the current April and May and with minimum temperatures in the prior July and August, but significant positive correlations with precipitation in the current May. Correlations were generally significantly negative between LWW chronologies and all temperatures in the prior July and August, indicating that the prior summer temperature had a strong lag effect on the growth of P. tabuliformis that increased with altitude. The correlation with the standardized precipitation evapotranspiration index (SPEI) confirmed that wet conditions in the current May promoted growth of TR and EW at all altitudes. Significant altitudinal differences were also found; at 1400 m, there were significant positive correlations between EWW chronologies and SPEI in the current April and significant negative correlations between LWW chronologies and SPEI in the current September, but these correlations were not significant at 1450 m. At 1350 m, there were also significant negative correlations between the TRW and the EWW chronologies and SPEI in the prior October and the current July and between LWW chronology and SPEI in the current August, but these correlations were not significant at 1400 m. Moving correlation results showed a stable response of EWW in relation to the SPEI in the current May at all three altitudes and of LWW to maximum temperature in the prior July–August at 1400 m from 2002 to 2018. The EWW chronology at 1400 m and the LWW chronology at 1450 m were identified as more suitable for climate reconstruction. These results provide a strong scientific basis for forest management decisions and climate reconstructions in Central China.

Key words: Tree rings, Climate response, Altitudinal gradient, Baiyunshan Mountain, Pinus tabuliformis Carr

Xiaoxu Wei, Jianfeng Peng, Jinbao Li, Jinkuan Li, Meng Peng, Xuan Li, Yameng Liu, Jiaxin Li. [J]. 林业研究(英文版), 2024, 35(1): 28-.

Xiaoxu Wei, Jianfeng Peng, Jinbao Li, Jinkuan Li, Meng Peng, Xuan Li, Yameng Liu, Jiaxin Li. Climate-growth relationships of Pinus tabuliformis along an altitudinal gradient on Baiyunshan Mountain, Central China[J]. JOURNAL OF FORESTRY RESEARCH, 2024, 35(1): 28-.

参考文献 53

1	Bao YY, Han YJ, Wang KK, Liu B. Growth response of coniferous trees to climate change in the Qinling Mountains. China Chin J Appl Ecol, 2021, 32(10): 3715-3723 In Chinese
2	Beguería S, Vicente-Serrano S, Reig F, Latorre B. Standardized precipitation evapotranspiration index (SPEI) revisited: parameter fitting, evapotranspiration models, tools, datasets and drought monitoring. Int J Climatol, 2014, 34: 3001-3023, DOI
3	Biondi F. Are climate-tree growth relationships changing in North-Central Idaho, U.S.A.?. Arct Antarct Alp Res, 2000, 32(2): 111-116, DOI
4	Bi SS, Hu JT, Fan PZ, Wang XY, Ye YZ. Plant community characteristics and spatial distribution of dominant tree species in Baiyun Mountain National Forest Park. J Henan Agric Univ, 2018, 52(2): 287-293 In Chinese
5	Cai QF, Liu Y, Song HM, Sun JY. Tree-ring-based reconstruction of the April to September mean temperature since 1826 AD for north-central Shaanxi Province, China. Sci China Ser D Earth Sci, 2008, 51(8): 1099-1106, DOI
6	Cai QF, Liu Y, Wang YC. Dendroclimatic investigation of Chinese pine in Taibai Mountain. Shaanxi Province J Earth Environ, 2012, 3(3): 874-880 In Chinese
7	Cai QF, Liu Y, Qian HJ, Liu RS. Inverse effects of recent warming on trees growing at the low and high altitudes of the Dabie Mountains, subtropical China. Dendrochronologia, 2020, 59: 10, DOI
8	Chen XJ, Yuan YJ, Chen F, Zhang RB, Zhang TW. Analysis of tree-ring width chronology characteristics from eastern area on north slope of Tianshan Mountains. J Desert Res, 2008, 28(5): 833-841 In Chinese
9	Cook ER. A time series analysis approach to tree-ring standardization, 1985 Tucson University of Arizona
10	Cook ER, Anchukaitis KJ, Buckley BM, D’Arrigo RD, Jacoby GC, Wright WE. Asian monsoon failure and megadrought during the last millennium. Science, 2010, 328(5977): 486-489, DOI
11	Cui JY, Peng JF, Li JR, Li X, Peng M, Yang L. Responses of tree-ring width of Pinus tabuliformis plantation to climatic factors in Songshan Mountains, central China. Chin J Appl Ecol, 2021, 32(10): 3497-3504 In Chinese
12	Fang KY, Gou XH, Chen FH, FranK D, Liu CZ, Li JB, Kazmer M. Precipitation variability during the past 400 years in the Xiaolong Mountain (central China) inferred from tree rings. Clim Dyn, 2012, 39(7–8): 1697-1707, DOI
13	Fritts HC. Tree rings and climate, 1976 London Academic Press
14	Gao J, Bao G, Wu ML, Liu N. Response of radial growth of planted Pinus tabuliformis in western Liaoning to climatic factors. J Earth Environ, 2020, 11(6): 629-638 In Chinese
15	Holmes RK. Dendrochronology program library. User’s manual, 1994 Tucson University of Arizona
16	Hou Y, Wang NA, Li G, Zheng F. Reconstruction of summer average temperature from tree-ring proxy data during 1751–2005 in Mr. Kongtong Clim Change Res, 2007, 13(3): 172-176
17	Jiao L, Jiang Y, Wang MC, Kang XY, Zhang WT, Zhang LN, Zhao SD. Responses to climate change in radial growth of Picea schrenkiana along elevations of the eastern Tianshan Mountains, northwest China. Dendrochronologia, 2016, 40: 117-127, DOI
18	Klesse S, DeRose RJ, Guiterman CH, Lynch AM, O’Connor CD, Shaw JD, Evans MEK. Sampling bias overestimates climate change impacts on forest growth in the southwestern United States. Nat Commun, 2018, 9(1): 5336, DOI
19	Li X, Peng JF, Li JR, Yang L, Cui JY, Peng M, Li CX. Climate-growth response of Pinus tabulaeformis in the south slope of Longchiman, Mt. Funiu, central China. Acta Ecol Sin, 2022, 42(7): 2865-2877 In Chinese
20	Liu Y, Ma LM, Cai QF, An ZS, Liu WG, Gao LY. Tree ring stable carbon isotope was used to reconstruct the temperature of Helan Mountain in summer (June–August) since 1890. Scientia Sinica (terrae), 2002, 32(8): 667-674
21	Liu Y, An ZS, Linderholm HW, Chen DL, Song HM, Cai QF, Sun JY, Tian H. Annual temperatures during the last 2485 years in the Eastern Tibetan Plateau inferred from tree rings. Sci China Ser D Earth Sci, 2009, 52(3): 348-359, DOI
22	Liu WZ. Illustrated Handbook of Common Medicinal Plants in Qinling Mountains, China (Rudin), 2015 Xi’an World Publishing Xi’an Co., Ltd 9 In Chinese
23	Liu Y, Wang YC, Li Q, Song HM, Linderholm HW, Leavitt SW, Wang RY, An ZS. Tree-ring stable carbon isotope-based May July temperature reconstruction over Nanwutai, China, for the past century and its record of 20th century warming. Quat Sci Rev, 2015, 117: 164-164, DOI
24	Mainali J, All J, Jha PK, Bhuju DR. Responses of Montane Forest to climate variability in the central Himalayas of Nepal. Mt Res Dev, 2015, 35(1): 66-77, DOI
25	McGregor S, Timmermann A, Timm O. A unified proxy for ENSO and PDO variability since 1650. Clim past, 2010, 6(1): 1-17, DOI
26	Nehrbass-Ahles C, Babst F, Klesse S, Nötzli M, Bouriaud O, Neukom P, Dobbertin M, Frank D. The influence of sampling design on tree-ring based quantification of forest growth. Glob Chang Biol, 2014, 20(9): 2867-2885, DOI
27	Peng XM, Xiao SC, Xiao HL. Advances in methods of building tree-ring width chronology. J Desert Res, 2013, 33(3): 857-865 In Chinese
28	Peng JF, Peng KY, Li JB. Climate-growth response of Chinese white pine (Pinus armandii) at different age groups in the Baiyunshan National Nature Reserve, central China. Dendrochronologia, 2018, 49: 102-109, DOI
29	Peng JF, Li JB, Wang T, Huo JX, Yang L. Effect of altitude on climate-growth relationships of Chinese white pine (Pinus armandii) in the northern Funiu Mountain, central China. Clim Change, 2019, 154(1–2): 273-288, DOI
30	Peng JF, Li JB, Yang L, Li JR, Huo JX. A 216-year tree-ring reconstruction of April–July relative humidity from Mt. Shiren, central China. Int J Climatol, 2020, 40(14): 6055-6066, DOI
31	Peng JF, Li JB, Li X, Cui JY, Peng M. Climate-growth relationships of Chinese Pine (Pinus tabulaeformis Carr.) at Mt. Shiren in Climatic Transition Zone, Central China. Biology (basel), 2022, 11(5): 753
32	Qin J, Bai HY, Zhao P, Yang NJ, Yue JW. Age-dependent response of Abies fargesii tree radial growth to climatic factors in the Qinling Mountains. Acta Ecol Sin, 2022, 42(17): 7167-7176 In Chinese
33	Rai S, Dawadi B, Wang YF, Lu XM, Ru H, Sigdel SR. Growth response of Abies spectabilis to climate along an elevation gradient of the Manang valley in the central Himalayas. J for Res, 2020, 31(6): 2245-2254, DOI
34	Shao XM. Advancements in dendrochronology. J Quat Sci, 1997, 3: 265-271 In Chinese
35	Shi JF, Li JB, Cook ER, Zhang XY, Lu HY. Growth response of Pinus tabulaeformis to climate along an elevation gradient in the eastern Qinling Mountains, central China. Clim Res, 2012, 53(2): 157-167, DOI
36	Song HM, Yu L, Li Q, Gao N, Ma YY, Zhang YH. Tree-ring based May–July temperature reconstruction since AD 1630 on the Western Loess Plateau, China. PLoS ONE, 2014, 9(4): 0093504, DOI
37	Stahle DW, Cleaveland MK, Grissino-Mayer HD, Griffin RD, Fye FK, Therrell MD, Burnette DJ, Meko DM, DiazJ V. Cool- and warm-season precipitation reconstructions over western New Mexico. J Clim, 2009, 22(13): 3729-3750, DOI
38	Sun C, Liu Y. Climate response of tree radial growth at different timescales in the Qinling Mountains. PLoS ONE, 2016, 11(8): 0160938, DOI
39	Tian QH, Liu Y, Cai QF, Bao G, Wang WP, Xue WL, Zhu WJ, Song HM, Lei Y. The maximum temperature of May–July inferred from tree-ring in Funiu Mountain since 1874 AD. Acta Geogr Sin, 2009, 64(7): 879-887 In Chinese
40	Torbenson MCA, Stahle DW, Diaz JV, Cook ER, Griffin D. The relationship between earlywood and latewood ring-growth across north America. Tree Ring Res, 2016, 72(2): 53-66, DOI
41	Wang YF, Liang EY, Ellison AM, Lu XM, Camarero JJ. Facilitation stabilizes moisture-controlled alpine juniper shrublines in the central Tibetan Plateau. Glob Planet Change, 2015, 132(sep.): 20-30, DOI
42	Wang T, Li C, Zhang H, Ren SY, Li LX, Pan N, Yuan ZL, Ye YZ. Response of conifer trees radial growth to climate change in Baotianman National Nature Reserve, central China. Acta Ecol Sin, 2016, 36(17): 5324-5332 In Chinese
43	Wang SP, Wang N, Zhou ZY, Hu YC, Wang N, Chen Y, Ye YZ. Sprouting characteristics of woody plants and their correlation analysis with environmental factors in temperate deciduous broad-leaved forest in Baiyunshan, Henan Province. J Henan Agr Univ, 2020, 54(6): 970-977 In Chinese
44	Wu XD. Tree-ring and climatic change, 1990 Beijing China Meteorologieal Press In Chinese
45	Wu CY, Chen DS, Sun XM, Zhang SG. Influence of altitude and tree class on climate-growth relationships in a larch plantation in subtropical China. J for Res, 2023, 34: 1869-1880, DOI
46	Yang B, Qin C, Wang J, He M, Melvin TM, Osborn TJ, Briffa KR. A 3500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proc Natl Acad Sci USA, 2014, 111(8): 2903-2908, DOI
47	Yang JW, Zhang QL, Song WQ, Zhang X, Li ZS, Zhang YD, Wang XC. Response differences of radial growth of Larix gmelinii and Pinus sylvestris var. mongolica to climate change in Daxing’an Mountains, Northeast China. Chin J Appl Ecol, 2021, 32(10): 3415-3427 In Chinese
48	Yang L, Li JR, Peng JF, Huo JX, Chen L. Temperature variation and influence mechanism of Pinus tabulaeformis ring width recorded since 1801 at Yao Mountain, He’nan Province. Acta Ecol Sin, 2021, 41(1): 79-91 In Chinese
49	Yang YR, Zhang MS, Zhang LN, Lu QQ, Hong YX, Liu XH. Different responses of radial growth of Pinus tabuliformis to climate in the middle and western Qinling Mountain. Acta Ecol Sin, 2022, 42(4): 1474-1486 In Chinese
50	Yu J, Liu QJ. Larix olgensis growth-climate response between lower and upper elevation limits: an intensive study along the eastern slope of the Changbai Mountains, northeastern China. J for Res, 2020, 31(1): 231-244, DOI
51	Zhao YS, Shi JF, Shi SY, Wang BW, Yu J. Summer climate implications of tree-ring latewood width: a case study of Tsuga longibracteata in South China. Asian Geogr, 2017, 34(2): 131-146, DOI
52	Zhao YS, Shi JF, Shi SY, Yu J, Lu HY. Tree-ring latewood width based July–August SPEI reconstruction in South China since 1888 and its possible connection with ENSO. J Meteorol Res, 2017, 31(1): 39-48, DOI
53	Zhao YS, Shi JF, Shi SY, Ma XQ, Zhang WJ, Wang BW, Lu HY, Braeuning A, Sun XG. Early summer hydroclimatic signals are captured well by tree-ring earlywood width in the eastern Qinling Mountains, central China. Clim past, 2019, 15(3): 1113-1131, DOI