罗霄山南部4个针叶树种生长特征及其气候响应对比分析

doi:10.17521/cjpe.2021.0289

植物生态学报 ›› 2021, Vol. 45 ›› Issue (12): 1303-1313.DOI: 10.17521/cjpe.2021.0289

罗霄山南部4个针叶树种生长特征及其气候响应对比分析

王兆鹏¹^,², 张同文², 袁玉江², 张瑞波², 喻树龙², 刘蕊², 石仁娜•加汗²^,³, 郭冬²^,³, 王勇辉¹^,^*()

¹新疆师范大学地理科学与旅游学院, 干旱区湖泊环境与资源重点实验室, 乌鲁木齐 830054
²中国气象局树木年轮理化研究重点实验室, 新疆树木年轮生态实验室, 乌鲁木齐 830002
³新疆大学资源与环境科学学院, 乌鲁木齐 830046

收稿日期:2021-08-11 接受日期:2021-10-08 出版日期:2021-12-20 发布日期:2021-11-11
通讯作者: 王勇辉
作者简介:^*(Wyhsd_3011@163.com)
基金资助:
国家自然科学基金(41975095);新疆维吾尔自治区重点实验室开放课题(2018D04028);天山青年计划-杰出青年科技人才项目(2019Q007)

Comparative analysis of growth characteristics and climate responses in four coniferous tree species of southern Luoxiao Mountains

WANG Zhao-Peng¹^,², ZHANG Tong-Wen², YUAN Yu-Jiang², ZHANG Rui-Bo², YU Shu-Long², LIU Rui², Shirenna JIAHAN²^,³, GUO Dong²^,³, WANG Yong-Hui¹^,^*()

¹Key Laboratory of Lake Environment and Resources in Arid Land, School of Geographical Science and Tourism, Xinjiang Normal University, Ürümqi 830054, China
²Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration, Xinjiang Laboratory for Tree Ring Ecology, Ürümqi 830002, China
³College of Resources and Environmental Sciences, Xinjiang University, Ürümqi 830046, China

Received:2021-08-11 Accepted:2021-10-08 Online:2021-12-20 Published:2021-11-11
Contact: WANG Yong-Hui
Supported by:
National Natural Science Foundation of China(41975095);Key Laboratory Opening Subject of Xinjiang Uygur Autonomous Region(2018D04028);Tianshan Youth Project of Xinjiang Uygur Autonomous Region-Outstanding Young Talent(2019Q007)

摘要/Abstract

摘要：

为了解影响罗霄山南部树木径向生长的主要气候要素, 该研究运用树木年轮气候学研究方法, 建立罗霄山南部4个针叶树种的树轮宽度标准化年表, 阐明影响该区域4个针叶树种径向生长的主要气候要素, 研究各树种在气温突变前后的径向生长特征及其对气候要素响应的异同。结果表明: 年表特征参数显示, 福建柏(Fokienia hodginsii)与其他树种相比, 其树轮宽度年表所包含的气候信息可能较少。与气候要素的相关分析显示, 铁杉(Tsuga chinensis)的径向生长同时受气温和降水的影响: 与上年10月的降水量呈显著正相关关系, 与气温的响应总体上呈负相关关系; 资源冷杉(Abies beshanzuensis var. ziyuanensis)仅与上年8月的降水量呈显著正相关关系; 马尾松(Pinus massoniana)与上年3月和当年1月的最高气温呈显著正相关关系, 与上年7月和当年8月的最低气温呈显著负相关关系; 福建柏仅与当年3月的降水量呈显著正相关关系。气温发生突变后, 4个树种树轮宽度指数的变化趋势相同, 均呈下降趋势, 除资源冷杉外, 各个树种的径向生长对气候要素的响应总体上有所增强, 且升温后产生的干旱胁迫抑制了各树种的生长。

关键词: 罗霄山, 树木年轮, 针叶树种, 气候因子

Abstract:

Aims In this study we constructed and analyzed the standardized chronology of tree-ring width in four coniferous tree species, Abies beshanzuensisvar. ziyuanensis, Fokienia hodginsii, Pinus massoniana and Tsuga chinensis, in southern Luoxiao Mountains, in order to investigate the radial growth characteristics of each species before and after the abrupt change in temperature, and to compare the similarities and differences among the four species in response to climate factors.

Methods Chronologies were developed from the cross-dated ring width series using the program ARSTAN, based on the standardized dendrochronological method. The time trend series of meteorological data from 1960 to 2013 and tree-ring chronologies were analyzed with a linear fitting method. The Mann-Kendall method was used to test the mutation of meteorological data. Growth-climate relationships were determined by calculating the Pearson correlation coefficients between tree-ring width chronologies and climatic factors.

Important findings The tree-ring width chronology of F. hodginsii provided less climatic signals than other three species. The radial growth of T. chinensis was affected by both temperature and precipitation: it was positively correlated with the precipitation in October of the previous year, but negatively with temperature. A. beshanzuensis var. ziyuanensis had a significant positive correlation with precipitation only in August of the previous year. P. massoniana was significantly positively correlated with the mean maximum air temperature in March of the previous year and January of the current year, and significantly negatively with the mean minimum air temperature in July of the previous year and August of the current year. F. hodginsii had a significant positive correlation with precipitation only in March of the current year. When temperature changed abruptly, the pattern of changes in the tree-ring width index was similar among the four species, all with a downward trend. The radial growth response to climate factors was enhanced in all species but A. beshanzuensis var. ziyuanensis, and their growth was inhibited by drought stress following warming. Results from this study provide information concerning the effects of climate change on tree growth and theoretical basis for forest ecosystem management and protection in the southern Luoxiao Mountains.

Key words: Luoxiao Mountains, tree-ring width, coniferous trees, climatic factor

王兆鹏, 张同文, 袁玉江, 张瑞波, 喻树龙, 刘蕊, 石仁娜•加汗, 郭冬, 王勇辉. 罗霄山南部4个针叶树种生长特征及其气候响应对比分析. 植物生态学报, 2021, 45(12): 1303-1313. DOI: 10.17521/cjpe.2021.0289

WANG Zhao-Peng, ZHANG Tong-Wen, YUAN Yu-Jiang, ZHANG Rui-Bo, YU Shu-Long, LIU Rui, Shirenna JIAHAN, GUO Dong, WANG Yong-Hui. Comparative analysis of growth characteristics and climate responses in four coniferous tree species of southern Luoxiao Mountains. Chinese Journal of Plant Ecology, 2021, 45(12): 1303-1313. DOI: 10.17521/cjpe.2021.0289

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链接本文: https://www.plant-ecology.com/CN/10.17521/cjpe.2021.0289

https://www.plant-ecology.com/CN/Y2021/V45/I12/1303

图/表 10

表1 罗霄山南部4个针叶树种采样点信息

Table 1 Information on sampling sites of four coniferous tree species in southern Luoxiao Mountains

项目 Item	NSP	HPA	SNM	SNB
纬度 Latitude (N)	26.42°	26.40°	26.45°	26.47°
经度 Longitude (E)	114.03°	114.03°	114.05°	114.07°
平均海拔 Mean altitude (m)	1 378.6	1 487.1	1 397.4	1 280.8
样本量(芯/树) Sample size (Number of cores/Number of trees)	72/24	66/22	60/20	60/20

图1 1960-2013年罗霄山南部地区气候特征。P, 降水量; T, 平均气温; Tmax, 最高气温; Tmin, 最低气温。

Fig. 1 Climatic characteristics of the southern Luoxiao Mountains from 1960 to 2013. P, precipitation; T, mean air temperature; Tmax, mean maximum air temperature; Tmin, mean minimum air temperature.

图2 罗霄山南部地区年平均气温(A)和年降水量(B)的Mann-Kendall检验结果(1960-2013)。UB, 统计量序列(下降趋势); UF, 统计量序列(上升趋势)。

Fig. 2 Results of Mann-Kendall tests for average temperature (A) and precipitation (B)(1960-2013). UB, sequence of statistics (downward trend); UF, sequence of statistics (upward trend).

表2 罗霄山南部4个针叶树种树轮宽度标准化年表主要特征参数

Table 2 Main characteristic parameters of tree-ring width standardized chronology of four coniferous tree species in southern Luoxiao Mountains

树种 Tree species	平均敏感度 Mean sensitivity	标准差 Standard deviation	一阶自相关系数 First-order auto-correlation	树间平均相关系数 Mean within- tree correlation	信噪比 Signal-to- noise ratio	样本代表性 Expressed population signal	子样本信号强度>0.85的第一年 The first year of subsample signal strength >0.85
NSP	0.135	0.241	0.702	0.256	16.849	0.944	1 877
HPA	0.182	0.282	0.404	0.212	12.886	0.928	1 913
SNM	0.271	0.247	0.610	0.295	15.905	0.941	1 898
SNB	0.217	0.221	0.560	0.241	13.993	0.933	1 923

图3 罗霄山南部4个针叶树种树轮宽度标准化年表。A, 铁杉。B, 资源冷杉。C, 马尾松。D, 福建柏。TRW, 树轮宽度标准化年表。

Fig. 3 Standardized chronology of tree-ring width of four coniferous tree species in southern Luoxiao Mountains. A, Tsuga chinensis. B, Abies beshanzuensis var. ziyuanensis. C, Pinus massoniana. D, Fokienia hodginsii. TRW, standardized chronology of tree-ring width.

表3 罗霄山南部4个针叶树种树轮宽度标准化年表系数及气候因子在突变前后的平均值

Table 3 Standardized chronological coefficient of tree-ring width of four coniferous tree species in southern Luoxiao Mountains and the mean value of climatic variables before and after abrupt changes

时段 Time interval	年平均气温 Mean annual air temperature (℃)	年降水量 Annual precipitation (mm)	年表系数 Chronological coefficient
时段 Time interval	年平均气温 Mean annual air temperature (℃)	年降水量 Annual precipitation (mm)	铁杉 NSP	资源冷杉 HPA	马尾松 SNM	福建柏 SNB
突变前 Before abrupt change	17.397	1 521.133	0.969	0.899	0.865	1.141
突变后 After abrupt change	17.973	1 515.164	0.828	1.040	0.805	0.924

图4 1980-2013年时段内1996年前后罗霄山南部年气候资料及4个树种年轮指数变化趋势。A, 平均气温。B, 降水量。C, 铁杉。D, 资源冷杉。E, 马尾松。F, 福建柏。

Fig. 4 Annual climate data and change trend of tree-ring index of four tree species in southern Luoxiao Mountains before and after 1996 during 1980-2013. A, Mean air temperature. B, Precipitation. C, Tsuga chinensis. D, Abies beshanzuensis var. ziyuanensis. E, Pinus massoniana. F, Fokienia hodginsii.

图5 罗霄山南部4个针叶树种树轮宽度标准化年表与单月气候因子的相关分析。A, 铁杉。B, 资源冷杉。C, 马尾松。D, 福建柏。c, 当年; p, 上年; P, 降水量; T, 平均气温; Tmax, 最高气温; Tmin, 最低气温。

Fig. 5 Correlation analysis between standardized chronology of tree-ring width and monthly climate factors in four coniferous tree species of southern Luoxiao Mountains. A, Tsuga chinensis. B, Abies beshanzuensis var. ziyuanensis. C, Pinus massoniana. D, Fokienia hodginsii. c, current year; p, previous year; P, precipitation; T, mean air temperature; Tmax, mean maximum air temperature; Tmin, mean minimum air temperature.

图6 罗霄山南部4个针叶树种树轮宽度标准化年表与季节性气候因子的相关分析。A, 铁杉。B, 资源冷杉。C, 马尾松。D, 福建柏。c, 当年; p, 上年; P, 降水量; T, 平均气温; Tmax, 最高气温; Tmin, 最低气温。

Fig. 6 Correlation analysis between standardized chronology of tree-ring width and seasonal climate factors in four coniferous tree species of southern Luoxiao Mountains. A, Tsuga chinensis. B, Abies beshanzuensis var. ziyuanensis. C, Pinus massoniana. D, Fokienia hodginsii. c, current year; p, previous year; P, precipitation; T, mean air temperature; Tmax, mean maximum air temperature; Tmin, mean minimum air temperature.

图7 气温突变前后罗霄山南部4个针叶树种树轮宽度标准化年表与月气候要素的相关分析。A, 铁杉与降水量的相关。B, 铁杉与平均气温的相关。C, 铁杉与最高气温的相关。D, 铁杉与最低气温的相关。E, 资源冷杉与降水量的相关。F, 资源冷杉与平均气温的相关。G, 资源冷杉与最高气温的相关。H, 资源冷杉与最低气温的相关。I, 马尾松与降水量的相关。J, 马尾松与平均气温的相关。K, 马尾松与最高气温的相关。L, 马尾松与最低气温的相关。M, 福建柏与降水量的相关。N, 福建柏与平均气温的相关。O, 福建柏与最高气温的相关。P, 福建柏与最低气温的相关。p, 上年; c, 当年。

Fig. 7 Correlation analysis between standardized chronology of tree-ring width and monthly climate factors of four coniferous tree species in southern Luoxiao Mountains before and after abrupt temperature change. A, Correlation between Tsuga chinensis and precipitation. B, Correlation between T. chinensis and mean temperature. C, Correlation between T. chinensis and mean maximum temperature. D, Correlation between T. chinensis and mean minimum temperature. E, Correlation between Abies beshanzuensis var. ziyuanensis and precipitation. F, Correlation between A. beshanzuensis var. ziyuanensis and mean temperature. G, Correlation between A. beshanzuensis var. ziyuanensis and mean maximum temperature. H, Correlation between A. beshanzuensis var. ziyuanensis and mean minimum temperature. I, Correlation between Pinus massoniana and precipitation. J, Correlation between P. massoniana and mean temperature. K, Correlation between P. massoniana and mean maximum temperature. L, Correlation between P. massoniana and mean minimum temperature. M, Correlation between Fokienia hodginsii and precipitation. N, Correlation between F. hodginsii and mean temperature. O, Correlation between F. hodginsii and mean maximum temperature. P, Correlation between F. hodginsii and mean minimum temperature. p, previous year; c, current year.

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罗霄山南部4个针叶树种生长特征及其气候响应对比分析

Comparative analysis of growth characteristics and climate responses in four coniferous tree species of southern Luoxiao Mountains

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