祁连山中部祁连圆柏林干扰历史重建

doi:10.17521/cjpe.2024.0011

植物生态学报 ›› 2024, Vol. 48 ›› Issue (8): 967-976.DOI: 10.17521/cjpe.2024.0011 cstr: 32100.14.cjpe.2024.0011

祁连山中部祁连圆柏林干扰历史重建

董云焘¹^,²(), 贾恒锋¹^,², 杨晶¹^,², 李佩轩¹^,², 方欧娅¹^,^*()()

¹中国科学院植物研究所植被与环境变化国家重点实验室, 国家植物园, 北京 100093
²中国科学院大学, 北京 100049

收稿日期:2024-01-16 接受日期:2024-05-26 出版日期:2024-08-20 发布日期:2024-05-16
通讯作者: *方欧娅(oyfang@ibcas.ac.cn), ORCID:0000-0002-8287-9404
作者简介:董云焘 ORCID:0009-0007-1723-681X
基金资助:
国家自然科学基金(32271672)

Reconstruction of disturbance history on Juniperus przewalskii forests in middle Qilian Mountains

DONG Yun-Tao¹^,²(), JIA Heng-Feng¹^,², YANG Jing¹^,², LI Pei-Xuan¹^,², FANG Ou-Ya¹^,^*()()

¹State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, China National Botanical Garden, Beijing 100093, China
²University of Chinese Academy of Science, Beijing 100049, China

Received:2024-01-16 Accepted:2024-05-26 Online:2024-08-20 Published:2024-05-16
Contact: *FANG Ou-Ya(oyfang@ibcas.ac.cn), ORCID:0000-0002-8287-9404
Supported by:
National Natural Science Foundation of China(32271672)

摘要/Abstract

摘要：

重建区域干扰历史对于了解当地森林健康状况以及有针对性地指导森林管护具有重要意义。然而, 目前关于祁连山森林的干扰历史及主要干扰类型尚不清楚。该研究以主要分布于祁连山阳坡的树种——祁连圆柏(Juniperus przewalskii)为研究对象, 在8个采样点采集其树木年轮样芯并建立树轮宽度标准年表。通过分析气候因子与树轮指数的相关关系, 确定影响该区域祁连圆柏生长的主要气候因子。通过分析每株树木的生长变化率, 识别树木的生长释放和抑制现象, 从而判断干扰发生的时间和空间格局。结果表明冬季气温、夏季水分条件显著影响了祁连圆柏的生长。重建的干扰历史显示, 研究区在1930s、1970s发生过两次区域性的森林干扰事件, 两次干扰事件与冬季极端寒冷、夏季极端干旱密切相关, 与连续的厄尔尼诺事件发生时间相一致。两次干扰事件均显示出干扰在空间上的差异性, 体现出了不同森林抵抗力的差异。研究结果为预防和缓解森林衰退提供了重要参考。

关键词: 树木年轮, 生长释放, 生长抑制, 极端气候, 祁连山

Abstract:

Aims The reconstruction of regional disturbance history provides important information in understanding the health status of local forests and facilitating their management and protection. However, the history and regimes of disturbances in the Qilian Mountains remain poorly reported.

Methods In this study, we explored the disturbance history of Juniperus przewalskii, a dominant tree species on the sunny slope of the Qilian Mountains. Tree-ring cores were collected and the standard chronologies of tree-ring width from eight sites were established. We analyzed the correlation between climate factors and tree-ring index. By calculating the percentage growth change in each tree, we examined whether there had been tree-growth release or suppression, thereby identifying the historical course and spatial pattern of disturbances.

Important findings Winter air temperature and summer moisture conditions significantly affected the growth of the tree species. The reconstruction of disturbance history highlighted two major forest disturbance events that occurred during the 1930s and 1970s in our study area. These events were intimately linked to extreme cold winters and severe summer droughts, coinciding remarkably with the occurrence of El Niño. Both events showed spatial variability in disturbance, reflecting differences in resistance across forests. Our study results offer new perspectives in mitigating forest degradation and enhancing forest management in the future.

Key words: tree ring, growth release, growth suppression, extreme climate, Qilian Mountains

董云焘, 贾恒锋, 杨晶, 李佩轩, 方欧娅. 祁连山中部祁连圆柏林干扰历史重建. 植物生态学报, 2024, 48(8): 967-976. DOI: 10.17521/cjpe.2024.0011

DONG Yun-Tao, JIA Heng-Feng, YANG Jing, LI Pei-Xuan, FANG Ou-Ya. Reconstruction of disturbance history on Juniperus przewalskii forests in middle Qilian Mountains. Chinese Journal of Plant Ecology, 2024, 48(8): 967-976. DOI: 10.17521/cjpe.2024.0011

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链接本文: https://www.plant-ecology.com/CN/10.17521/cjpe.2024.0011

https://www.plant-ecology.com/CN/Y2024/V48/I8/967

图/表 7

表1 祁连山8个样点祁连圆柏树轮信息表

Table 1 Information of the eight Juniperus przewalskii tree-ring chronologies in Qilian Mountains

样点编号 Site ID	位置 Position	经度 Longitude (° E)	纬度 Latitude (° N)	海拔 Altitude (m)	定年样本量 Number of dated series	起止年 Period	年代长度 Time span (a)	平均序列长度 Mean length of series (a)	序列间相关系数 Series intercorrelation	平均敏感性 Average sensitivity	样本总体代表量 Express population signal (EPS)
YNG	野牛沟 Yeniugou	99.53	38.42	3 390	17	1772-2020	249	134.7	0.494	0.276	0.870
YHL	油葫芦 Youhulu	99.78	38.25	3 600	32	1500-2004	505	292.5	0.540	0.254	0.864
DG	东沟 Donggou	100.02	38.02	3 600	31	1630-2004	375	288.5	0.573	0.224	0.905
HZS	黄藏寺 Huangzangsi	100.25	38.26	3 340	34	1522-2020	499	234.0	0.447	0.248	0.859
AMDS	阿咪东索 Amidongsuo	100.25	38.07	3 353	19	1404-2017	614	390.7	0.452	0.210	0.854
DLD	大拉洞 Daladong	100.35	38.23	3 190	30	1268-2020	753	416.8	0.455	0.194	0.841
QYG	青阳沟 Qingyanggou	100.39	38.17	3 420	14	1758-2020	263	190.2	0.436	0.243	0.732
MZ	芒扎 Mangzha	100.73	38.21	2 950	30	1592-2020	429	107.5	0.472	0.275	0.880
QLB	-	-	-	-	207	1268-2020	753	259.1	0.430	0.230	0.971

图1 祁连山中部树轮采样点及气象站分布。各采样点名称见表1。

Fig. 1 Distribution of tree-ring sampling sites and meteorological stations in the middle Qilian Mountains. Site ID see Table 1.

图2 祁连山祁连圆柏树轮宽度标准年表。Num, 区域总样芯数量; QLB, 区域总年表; Sites, 各样点年表。

Fig. 2 Standardized tree-ring width chronologies of Juniperus przewalskii in Qilian Mountains. Num, the number of regional total sample cores; QLB, regional total tree-ring chronology; Sites, tree-ring chronologies of each sampling sites.

图3 祁连山祁连圆柏树轮年表与月平均气温(A)、月降水量(B)以及月平均相对湿度(C)的相关关系。QLB, 区域总树轮年表。红色表示正相关, 蓝色表示负相关, 颜色越深, 相关性越强。*, p < 0.05。“p”表示前一年, 例如“p9”表示前一年9月份。各采样点名称见表1。

Fig. 3 Correlation of Juniperus przewalskii tree-ring chronologies with monthly mean air temperature (A), monthly precipitation (B), and monthly mean relative humidity (C) in Qilian Mountains. QLB, the regional total tree-ring chronology. Red indicates positive correlation, blue indicates negative correlation, the darker the color, the stronger the correlation. *, p < 0.05. “p” indicates the previous year, for example, “p9” indicates September of the previous year. Site ID see Table 1.

图4 祁连山祁连圆柏树木生长的历史干扰状况。虚线标注为厄尔尼诺年。图例表示发生生长释放树木的百分比, 比例越高, 干扰强度越强。各采样点名称见表1。

Fig. 4 Juniperus przewalskii disturbance history in Qilian Mountains. The dashed lines denote El Niño years. The legend indicates the percentage of growth-release trees, the higher the percentage, the stronger the intensity of the disturbance. Site ID see Table 1.

图5 1908-1980年期间以20年为窗口时的干扰事件发生次数分布。虚线标注为厄尔尼诺年。彩色曲线表示各采样点干扰事件发生次数, 黑色曲线表示各采样点干扰事件发生次数的平均值。各采样点名称见表1。

Fig. 5 Number of disturbance events in a 20-year window for the period 1908-1980. The dashed lines are El Niño years. Colored curves indicate the frequency of sampling sites disturbances, the black curve indicates the average of the frequency of sampling sites disturbances. Site ID see Table 1.

图6 祁连山祁连圆柏在1930s和1970s干扰事件中受干扰程度的空间分布。A, 1930s干扰事件。B, 1970s干扰事件。各采样点名称见表1。

Fig. 6 Spatial distribution of Juniperus przewalskii disturbance levels in Qilian Mountains during the 1930s and 1970s disturbance events. A, Disturbance in 1930s. B, Disturbance in 1970s. Site ID see Table 1.

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祁连山中部祁连圆柏林干扰历史重建

Reconstruction of disturbance history on Juniperus przewalskii forests in middle Qilian Mountains

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