Missing rings of Larix sibirica associated with climatic elements on the Altai Mountains, China

doi:10.1007/s11676-024-01785-9

Abstract

Abstract:

The physiological structure and growth of trees in extreme environments (freezing temperatures, prolonged drought, wildfires, pest infestations, and diseases) can be inhibited, including radial growth, and stagnant growth or missing annual rings is highly possible. In this study, we analyzed the radial growth of Siberian larch (Larix sibirica) in the Hongshanzui area of the Altai Mountains, China. The overall missing ring rate at the sampling point was 2.39%, with years with the highest missing rings since meteorological site data were available (1960) identified as 1960, 1961, 1971, 1973, 1985, 1987, and 1995. Radial growth in high altitudes was mainly affected by temperatures in May and June (average temperature, average minimum temperature, and average maximum temperature). Frequent periods of freezing may lead to missing annual rings. However, while Larix sibirica shows resilience after prolonged freezing temperatures, it still requires time for the trees to return to normal growth levels.

Key words: Missing tree rings, Low growing season temperatures, Altai Mountains, Ecological resilience, Larix sibirica

Kailong Guo, Tongwen Zhang, Yonghui Wang, Xiaoxia Gou, Shulong Yu, Huaming Shang, Ruibo Zhang, Li Qin, Shengxia Jiang, Kexiang Liu, Dong Guo, Ruxianguli Abureheman, Yulin Guo. Missing rings of Larix sibirica associated with climatic elements on the Altai Mountains, China[J]. JOURNAL OF FORESTRY RESEARCH, 2024, 35(1): 134-.

References 46

1	Barbosa AC, Stahle DW, Burnette DJ, Torbenson MCA, Cook ER, Bunkers MJ, Garfin G, Villalba R. Meteorological factors associated with frost rings in rocky mountain bristlecone pine at Mt Goliath, Colorado. Tree Ring Res, 2019, 75(2): 101, DOI
2	Bisset IJW, Dadswell HE, Wardrop AB. Factors influencing tracheid length in conifer stems. Aust for, 1951, 15(1): 17-30, DOI
3	Cao SJ, Cao FX, Qi CJ, Xu QJ. Advances in research on the relationships between climatic change and pathological tree-rings structures. J Ecol Environ, 2010, 19(2): 494-498, DOI
4	Čufar K, De Luis M, Eckstein D, Kajfez-Bogataj L. Reconstructing dry and wet summers in SE Slovenia from oak tree-ring series. Int J Biometeorol, 2008, 52(7): 607-615, DOI
5	Cui Y (2014) Response of tree-rotation width chronology to climate and early summer temperature reconstruction in Altay region M.S Xinjiang University.
6	Cuny HE, Rathgeber CBK, Frank D, Fonti P, Fournier M. Kinetics of tracheid development explain conifer tree-ring structure. New Phytol, 2014, 203(4): 1231-1241, DOI
7	Fang OY, Zhang QB. Tree resilience to drought increases in the Tibetan Plateau. Glob Chang Biol, 2019, 25(1): 245-253, DOI
8	Fritts HC. Tree rings and climate, 1976 Xiii Academic Press, London 567
9	Gou XX, Zhang TW, Yuan YJ, Yu SL, Zhang RB, Jiang SX, Guo XL. Radial growth of dominant coniferous species and their responses to climate changes in the Altay Mountains, China. Chin J Appl Ecol, 2021, 32(10): 3594-3608, DOI
10	Hiratsuka Y, Zalasky H (1993) Frost and other climate-related damage of forest trees in the prairie provinces. For. Can., Northwest Reg., North. For. Cent., Edmonton, Alberta. Inf. Rep. NOR-X-331. https://doi.org/10.5555/19960612405
11	Hu YC, Yuan YJ, Wei WS, Zhang RB, Zhang TW, Shang HM, Chen F. Tree-ring reconstruction of mean June–July temperature during 1613–2006 in East Altay, Xinjiang of China. J Desert Res, 2012, 32(04): 1003-1009 (in Chinese)
12	Hu J, Yu SL, Yuan YJ, Zhang TW, Shang HM, Zhang RB. Characteristics of tree-ring width chronologies in the central Altay Mountains and climate response. Desert Oasis Meteorol, 2014, 8(3): 19-26 (in Chinese)
13	Hu M, Chen F, Chen YP. Responses of radial growth of Pinus sibirica to climate and hydrology in Altay, Xinjiang, China. Chin J Appl Ecol, 2021, 32(10): 3609-3617, DOI
14	Huang LP, Gao YQ, Zhang TW, Hu DY, Wang L. Growth of Siberia Larch in the middle east of Altay Mountains and its response to climate change. Arid Zone Geogr, 2015, 38(6): 1169-1178, DOI
15	Jiao L, Wang LL, Li L, Chen XX, Yan XX. Divergent responses of radial growth of Larix sibirica to climate change in Altay Mountains of Xinjiang. Chin J Plant Ecol, 2019, 43(4): 320-330, in Chinese) DOI
16	Jiao L, Ma L, Zhang TW, Wang SJ. Changes of mean minimum temperature in June–July since 1798 in central Altay Mountain recorded by tree rings. Acta Ecol Sin, 2021, 41(5): 1944-1958 (in Chinese)
17	Kang J, Liang HX, Jiang SW, Zhu HX, Zhou P, Huang JG. Effects of competition and climate on tree radial growth of Pinus sibirica in Altai Mountains, Xinjiang, China. Chin J Plant Ecol, 2020, 44(12): 1195-1202, in Chinese) DOI
18	Kokutse AD, Stokes A, Kokutse NK, Kokou K. Which factors most influence heartwood distribution and radial growth in plantation teak?. Ann for Sci, 2010, 67(4): 407, DOI
19	Li JF, Yuan YJ, Zhou WS J (1989) Hydrological studies of annual climate rings in Xinjiang. Beijing: Meteorological Publishing. pp 73.
20	Li JF, Yuan YJ, Yu XY (2000) Research and application of tree−rotation hydrology: Science Publishing. pp 27−33.
21	Li CJ, Chen T, Wang B, Xu GB, Zhang XW, Wu GJ. Advances in research on the abnormal structure of tree-rings. Chin J Ecol, 2019, 38(5): 1538-1550, DOI
22	Li YJ, Fang KY, Bai MW, Cao XG, Dong ZP, Tang WR, Mei ZP. Ecological resilience of ancient Pinus massoniana trees to climate change and insect infestation in southeastern Fujian, China. Chin J Appl Ecol, 2021, 32(10): 3539-3547, DOI
23	Liang EY, Eckstein D. Light rings in Chinese pine (Pinus tabulaeformis) in semiarid areas of North China and their palaeo-climatological potential. New Phytol, 2006, 171(4): 783-791, DOI
24	Liu Y, An ZS, Ma HZ, Cai QF, Liu ZY, Kutzbach JK, Shi JF, Song HM, Sun JY, Yi L, Li Q, Yang YK, Wang L. Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature. Sci China Ser D, 2006, 49(4): 408-420, DOI
25	Liu PX, Gou XH, Zhang QB, Chen FH. Advances in dendrohydrology around the world. J Glaciol Geocryol, 2004, 26(6): 720-728, DOI
26	Nabais C, Campelo F, Vieira J, Cherubini P. Climatic signals of tree-ring width and intra-annual density fluctuations in Pinus pinaster and Pinus pinea along a latitudinal gradient in Portugal. Forestry, 2014, 87(4): 598-605, DOI
27	Niu JQ, Yuan YJ, Zhang TW, Shang HM, Zhang RB, Yu SL, Chen F, Jiang SX. Characteristics of tree-ring width chronologies in Altay and their response to climate change. Desert Oasis Meteorol, 2016, 10(1): 59-67, DOI
28	Oberhuber W, Stumböck M, Kofler W. Climate-tree-growth relationships of Scots pine stands (Pinus sylvestris L.) exposed to soil dryness. Trees, 1998, 13(1): 19-27, DOI
29	Oberhuber W, Kofler W, Pfeifer K, Seeber A, Gruber A, Wieser G. Long-term changes in tree-ring–climate relationships at Mt Patscherkofel (Tyrol, Austria) since the mid 1980s. Trees, 2008, 22(1): 31-40, DOI
30	Payette S, Delwaide A, Simard M. Frost-ring chronologies as dendroclimatic proxies of boreal environments. Geophys Res Lett, 2010, 37(2): L02711, DOI
31	Rossi S, Deslauriers A, Anfodillo T, Carrer M. Age-dependent xylogenesis in timberline conifers. New Phytol, 2008, 177(1): 199-208, DOI
32	Sass-Klaassen U, Fonti P, Cherubini P, Gričar J, Robert EMR, Steppe K, Bräuning A. A tree-centered approach to assess impacts of extreme climatic events on forests. Front Plant Sci, 2016, 7: 1069, DOI
33	Shang HM, Wei WS, Yuan YJ, Yu SL, Zhang TW, Waheti A, Li XJ. Response of tree ring width to recent climate change, south slope of Altai Mountains. Acta Ecol Sin, 2010, 30(9): 2246-2253 (in Chinese)
34	Shi YG, Wen KG (2006) Dictionary of meteorological disasters in China (Xinjiang volume) Beijing: Meteorological Publishing.
35	Tardif JC, Salzer MW, Conciatori F, Bunn AG, Hughes MK. Formation, structure and climatic significance of blue rings and frost rings in high elevation bristlecone pine (Pinus longaeva D. K. Bailey). Quat Sci Rev, 2020, 244: 106516, DOI
36	Wang LL, Shao XM, Huang L, Liang EY. Tree-ring characteristics of Larix gmelinii and Pinus sylvestris var mongolica and their response to climate in Mohe, China. Chin J Plant Ecol, 2005, 29(3): 280-285, DOI
37	Wang XM, Zhao XH, Gao LS. Climatic response of Betula ermanii along an altitudinal gradient in the northern slope of Changbai Mountain, China. Dendrobiology, 2013, 70: 99-107, DOI
38	Wang CS, Zhou FF, Zheng ZP, Dong ZP, Bing XJ. Spatial distribution of missing ring rate in Asia and their influencing factors. J Subtrop Resour Environ, 2022, 17(2): 4551-4559, DOI
39	Wilmking M, Hallinger M, Van Bogaert R, Kyncl T, Babst F, Hahne W, Juday GP, de Luis M, Novak K, Völlm C. Continuously missing outer rings in woody plants at their distributional margins. Dendrochronologia, 2012, 30(3): 213-222, DOI
40	Wu GJ, Liu XH, Chen T, Xu GB, Wang B, Kang HH, Li CJ, Zeng XM. The positive contribution of iWUE to the resilience of schrenk spruce (Picea schrenkiana) to extreme drought in the western Tianshan Mountains, China. Acta Physiol Plant, 2020, 42: 1-16, DOI
41	Xie PP, Zhang BY, Dong YB, Lyu PC, Du MC, Zhang XL. Differences in ecological resilience of radial growth between Larix principis-rupprechtii and Picea meyeri after drought. Chin J Appl Ecol, 2023, 34(7): 1779-1786, DOI
42	Xue RH, Jiao L, Liu XP, Chen K. Evaluation of the stability of the radial growth of Larix sibirica at different altitudes in response to climate change in Altai Mountains, Xinjiang. Chin J Ecol, 2021, 40(5): 1275-1284, DOI
43	Yu J, Shah S, Zhou G, Xu ZZ, Liu QJ. Tree-ring-recorded drought variability in the northern Daxing’anling Mountains of Northeastern China. Forests, 2018, 9(11): 674, DOI
44	Zhang TW, Yuan YJ, Yu SL, Wei WS, Yang Q, Shang HM, Ding L. Development of two tree-ring width chronologies of the samples collected from the Baluntai Region. Arid Zone Res, 2008, 25(2): 288-294, DOI
45	Zhang TW, Yuan YJ, Yu SL, Wei WS, Yang Q, Shang HM. June to September precipitation series of 1481–2004 reconstructed from tree-ring in the western region of Altay prefecture, Xinjiang. J Glaciol Geocryol, 2008, 30(4): 659-667, DOI
46	Zhao SD, Jiang Y, Wen Y, Jiao L, Li WQ, Xu H, Ding MH. Frequent locally absent rings indicate increased threats of extreme droughts to semi-arid Pinus tabuliformis forests in North China. Agric for Meteor, 2021, 308, DOI