长白山天然水曲柳径向生长对气候的响应

doi:10.17521/cjpe.2023.0231

植物生态学报 ›› 2024, Vol. 48 ›› Issue (8): 1011-1020.DOI: 10.17521/cjpe.2023.0231 cstr: 32100.14.cjpe.2023.0231

长白山天然水曲柳径向生长对气候的响应

李士杰¹^,², 王丽², 杜英军², 郑磊³, 曾凡锁¹^,⁴, 辛颖¹^,²^,^*()

¹林木遗传育种全国重点实验室(东北林业大学), 哈尔滨 150040
²东北林业大学林学院, 哈尔滨 150040
³辽宁省本溪市城市运行服务中心, 辽宁本溪 117099
⁴东北林业大学生命科学学院, 哈尔滨 150040

收稿日期:2023-08-11 接受日期:2024-04-08 出版日期:2024-08-20 发布日期:2024-04-09
通讯作者: *辛颖(xinying2004@126.com)
基金资助:
国家重点研发计划(2021YFD2200303);中央高校基本科研业务费(2572021DT06)

Radial growth response of natural Fraxinus mandshurica to climate in the Changbai Mountains

LI Shi-Jie¹^,², WANG Li², DU Ying-Jun², ZHENG Lei³, ZENG Fan-Suo¹^,⁴, XIN Ying¹^,²^,^*()

¹State Key Laboratory of Tree Genetics and Breeding (Northeast Forestry University), Harbin 150040, China
²School of Forestry, Northeast Forestry University, Harbin 150040, China
³Urban Operation Service Center of Benxi City, Benxi, Liaoning 117099, China
⁴College of Life Science, Northeast Forestry University, Harbin 150040, China

Received:2023-08-11 Accepted:2024-04-08 Online:2024-08-20 Published:2024-04-09
Contact: *XIN Ying(xinying2004@126.com)
Supported by:
National Key R&D Program of China(2021YFD2200303);Fundamental Research Funds for Central Universities(2572021DT06)

摘要/Abstract

摘要：

为了探究长白山天然水曲柳(Fraxinus mandshurica)径向生长与气候因子的关系, 探寻限制水曲柳生长的主要气象因子, 以红石、清原、桓仁和集安4个种源地的天然水曲柳为研究对象, 运用树木年代学方法, 研究天然水曲柳径向生长差异及其对气候因子的响应。结果表明: 4个种源地水曲柳在1960-1980年的轮宽指数都较低, 具有不同的变化趋势和波动特征。4个种源地水曲柳标准年表的相关性都达到了极显著水平, 这4个种源地水曲柳的径向生长具有较强的区域一致性。温度, 特别是生长季初期最低气温是红石、清原、桓仁和集安天然水曲柳径向生长的主要限制因子, 非生长季的水分状况也对来年水曲柳的径向生长有着重要影响, 而且长白山北麓水曲柳对气候的敏感性高于南麓和西南麓。方差分解分析也进一步印证了温度尤其是最低气温对长白山水曲柳径向生长的限制作用。在全球气候变化的背景下, 长白山集安水曲柳应对气候变化更加稳定, 是优良的水曲柳种质资源。

关键词: 水曲柳, 长白山, 径向生长, 气候响应, 种源, 方差分解

Abstract:

Aims To explore the relationship between the radial growth of natural Fraxinus mandshurica and climate factors in the Changbai Mountains, the response of natural F. mandshurica radial growth to climate factors was studied, which would further identify the main meteorological factors limiting the growth of F. mandshurica.

Methods Natural F. mandshurica in Hongshi, Qingyuan, Huanren, and Ji’an were selected. The dendrochronological method was used to establish the standard chronology to study the relationship between radial growth and climate factors.

Important findings The tree ring width index of four provenances was lower from 1960 to 1980, and these data had different trends and fluctuation characteristics. The correlation of four standard chronologies of F. mandshurica was extremely significant. The radial growth of F. mandshurica at these four provenances had strong regional consistency. Temperature, especially lowest air temperature in winter and early growing season, was the main limiting factor for the radial growth of natural F. mandshuricain Hongshi, Qingyuan, Huanren and Ji’an. Meanwhile, the water condition in non-growing season also had an important effect on the radial growth of F. mandshurica in the following year. The variance decomposition analysis further confirmed the limiting effect of temperature, especially lowest air temperature, on the radial growth of F. mandshurica from four provenances in the Changbai Mountains. In the context of global climate change, the F. mandshurica from Ji’an was more stable in responding to climate change. It’s an excellent germplasm resource of F. mandshurica.

Key words: Fraxinus mandshurica, Changbai Mountains, radial growth, climate response, provenance, variance decomposition

李士杰, 王丽, 杜英军, 郑磊, 曾凡锁, 辛颖. 长白山天然水曲柳径向生长对气候的响应. 植物生态学报, 2024, 48(8): 1011-1020. DOI: 10.17521/cjpe.2023.0231

LI Shi-Jie, WANG Li, DU Ying-Jun, ZHENG Lei, ZENG Fan-Suo, XIN Ying. Radial growth response of natural Fraxinus mandshurica to climate in the Changbai Mountains. Chinese Journal of Plant Ecology, 2024, 48(8): 1011-1020. DOI: 10.17521/cjpe.2023.0231

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链接本文: https://www.plant-ecology.com/CN/10.17521/cjpe.2023.0231

https://www.plant-ecology.com/CN/Y2024/V48/I8/1011

图/表 7

表1 长白山水曲柳种源地基本情况

Table 1 Information of Fraxinus mandshurica provenance land in the Changbai Mountains

采样点 Sampling point	经度 Longitude (E)	纬度 Latitude (N)	海拔 Altitude (m)
红石 Hongshi (HS)	127.07°	42.52°	270-350
清原 Qingyuan (QY)	124.92°	42.10°	230-290
桓仁 Huanren (HR)	125.35°	41.27°	250-280
集安 Ji’an (JA)	126.12°	41.12°	210-300

图1 长白山4个水曲柳种源地气象数据。T, 平均气温; Tmax, 最高气温; Tmin, 最低气温。HR, 桓仁; HS, 红石; JA, 集安; QY, 清原。

Fig. 1 Meteorological data of 4 Fraxinus mandshurica provenances in the Changbai Mountains. T, mean air temperature; Tmax, maximum air temperature; Tmin, minimum air temperature. HR, Huanren; HS, Hongshi; JA, Ji’an; QY, Qingyuan.

图2 长白山不同种源水曲柳标准年表。HR, 桓仁; HS, 红石; JA, 集安; QY, 清原。

Fig. 2 Standard chronology of Fraxinus mandshurica at different provenances in the Changbai Mountains. HR, Huanren; HS, Hongshi; JA, Ji’an; QY, Qingyuan.

表2 长白山不同种源水曲柳标准年表主要统计特征

Table 2 Main statistical characteristics of the standard chronology of Fraxinus mandshurica at different provenances in the Changbai Mountains

年表特征 Characteristic of chronology	红石 Hongshi	清原 Qingyuan	桓仁 Huanren	集安 Ji’an
时段(子样本信号强度>0.85) Time span (subsample signal strength > 0.85)	1959-2021	1963-2021	1961-2021	1964-2021
标准差 Standard deviation (SD)	0.211	0.161	0.208	0.177
信噪比 Signal-to-noise ratio (SNR)	11.923	5.217	4.631	4.435
平均敏感度 Mean sensitivity (MS)	0.180	0.164	0.160	0.152
一阶自相关 Autocorrelation order 1 (AC1)	0.655	0.442	0.521	0.543
样芯间平均相关系数 Mean interseries correlation (MC)	0.379	0.243	0.291	0.311
样本群体表达信号 Express population signal (EPS)	0.954	0.885	0.918	0.864
第一主成分所占方差量 Percentage of variance in first eigenvector (%)	44.56	24.18	37.52	32.31

表3 1970-2021年长白山不同种源水曲柳标准年表间的相关系数

Table 3 Correlation coefficients of standard chronology of Fraxinus mandshurica at different provenances in Changbai Mountains from 1970 to 2021

采样点 Sampling point	红石 Hongshi	清原 Qingyuan	桓仁 Huanren	集安 Ji’an
红石 Hongshi	1.000
清原 Qingyuan	0.471^**	1.000
桓仁 Huanren	0.370^**	0.496^**	1.000
集安 Ji’an	0.388^**	0.448^**	0.536^**	1.000

图3 长白山不同种源水曲柳标准年表与气候因子相关分析。P, 降水量; RH, 相对湿度; T, 平均气温; Tmax, 最高气温; Tmin, 最低气温。c, 当年; p, 上一年。*, p < 0.05; **, p < 0.01。

Fig. 3 Correlation analysis between standard chronology of Fraxinus mandshurica and climate factors at different provenances in the Changbai Mountains. P, precipitation; RH, relative humidity; T, mean air temperature; Tmax, maximum air temperature; Tmin, minimum air temperature. c, this year; p, last year. *, p < 0.05; **, p < 0.01.

图4 长白山不同种源水曲柳标准年表与气候因子的方差分解分析。P, 降水量; RH, 相对湿度; T, 平均气温; Tmax, 最高气温; Tmin, 最低气温; 气候因子后面的数字为月份。Adj R2,调整后的R2。*, p < 0.05。

Fig. 4 Variance decomposition analysis of standard chronology and climate factors of Fraxinus mandshurica at different provenances in the Changbai Mountains. P, precipitation; RH, relative humidity; T, mean air temperature; Tmax, maximum air temperature; Tmin, minimum air temperature; Number followed climate factors is month. Adj R2, adjusted R2. *, p < 0.05.

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长白山天然水曲柳径向生长对气候的响应

Radial growth response of natural Fraxinus mandshurica to climate in the Changbai Mountains

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