黄河上游甘蒙柽柳生长对极端旱涝的响应

doi:10.17521/cjpe.2021.0020

植物生态学报 ›› 2021, Vol. 45 ›› Issue (6): 641-649.DOI: 10.17521/cjpe.2021.0020

所属专题：青藏高原植物生态学：种群生态学

黄河上游甘蒙柽柳生长对极端旱涝的响应

方欧娅¹^,^*(), 张永², 张启¹^,³, 贾恒锋¹^,³

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, 北京 100093
²中国科学院地理科学与资源研究所陆地表层格局与模拟院重点实验室, 北京 100101
³中国科学院大学, 北京 100049

收稿日期:2021-01-14 接受日期:2021-04-26 出版日期:2021-06-20 发布日期:2021-09-09
通讯作者: ORCID: *方欧娅: 0000-0002-8287-9404(oyfang@ibcas.ac.cn)
作者简介:^*E-mail: oyfang@ibcas.ac.cn
基金资助:
国家自然科学基金(31700412);第二次青藏高原综合科学考察研究项目(2019QZKK0301)

Growth responses of Tamarix austromongolica to extreme drought and flood in the upper Yellow River basin

FANG Ou-Ya¹^,^*(), ZHANG Yong², ZHANG Qi¹^,³, JIA Heng-Feng¹^,³

¹State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China
²Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
³University of Chinese Academy of Sciences, Beijing 100049, China

Received:2021-01-14 Accepted:2021-04-26 Online:2021-06-20 Published:2021-09-09
Contact: FANG Ou-Ya
Supported by:
National Natural Science Foundation of China(31700412);Second Tibetan Plateau Scientific Expedition and Research (STEP) Program, China(2019QZKK0301)

摘要/Abstract

摘要：

青藏高原黄河上游河岸带是典型的生态脆弱区, 然而近年来气候变暖加剧了该地极端旱涝事件的频繁发生, 高原河岸带生态脆弱区植被是否能够应对极端旱涝事件的干扰成为流域生态环境管理工作所关注的重点问题。为了研究黄河上游河岸林中主要树种对极端旱涝的响应, 该研究选取青海省同德县和兴海县3处河岸林中的47株甘蒙柽柳(Tamarix austromongolica), 分别从树干面向邻近山体一侧及与之垂直的一侧分别获取1根树轮样本, 分析其历史生长。通过对比两个方向上的生长速率判断甘蒙柽柳是否受到地质灾害影响从而将其划分为受伤组和对照组, 分析两组甘蒙柽柳在过去63年中径流极值年的抵抗力状况及两个方向的生长差异。研究发现, 甘蒙柽柳对干旱和洪涝均有着很强的抵抗力, 河岸带多样化的水分来源有助于甘蒙柽柳在极端干旱环境中较好地生长; 但洪涝伴随泥石流等地质灾害的频发使甘蒙柽柳面向山体侧面受到严重的生长抑制, 表现出显著的方向性差异, 从而影响甘蒙柽柳的形态。较长的创伤恢复期带来的遗留效应可能造成甘蒙柽柳对外界干扰的较高敏感性。研究黄河上游甘蒙柽柳生长对极端旱涝的响应, 将有助于评估生态脆弱区生态弹性过程, 同时为高原河岸带生态建设和恢复提供科学依据。

关键词: 生态弹性, 抵抗力, 生态脆弱区, 干旱, 洪涝, 气候变化, 甘蒙柽柳

Abstract:

Aims The riparian forests in the upper reaches of the Yellow River are typically fragile ecologically. However, the frequent extreme hydrological events induced by climate warming may pose increasing threats to ecological stability and security of this fragile ecosystem type. The ecological resilience and adaptation of riparian forests to extreme hydrological events are of key considerations in eco-environmental management of river basins. This paper aims to determine how Tamarix austromongolica, a major tree species in riparian forests of the upper Yellow River basin, responds to extreme drought and flood and explain the resistance and morphology of these riparian plants against environmental stresses.

Methods We selected 47 Tamarix austromongolica trees from three sampling sites along the upper reaches of the Yellow River. Two mutually perpendicular cores were taken from the trunk of the each sampling tree for estimation of the past annual growth, one from the direction facing the slope and the other along the contour of the nearby mountain. We compared the tree-ring growth between cores from the two sides and grouped them according to whether the growth was strongly affected by geohazards. We analyzed the resistance of the two groups to extreme hydrological events during the past 63 years. The statistical growth difference between two sampling directions from each group was performed by using paired test.

Important findings Tamarix austromongolica trees were found to be very resistant to extreme drought events. The diverse sources of water in riparian zones attributed to their stable growth, which helps enhance their tolerance to hydrological drought events. But the trees injured by geohazards appeared to be more severely affected by droughts. The legacy effect in trauma-associated recovery might initiate high sensitivity to interferences. Moreover, T. austromongolica trees are adapted to a wide range of water conditions and their growth did not appear to be substantially affected by flooding. Well-watered condition along with fully hydrated shoots could promote the growth and counteract the potentially negative effects of submergence in T. austromongolica. However, flood induced geohazards, such as mudslides, could have significantly different impacts on growth in different directions, such that the side facing the nearby mountain slope suffered more growth suppression. These processes could lead to modification of morphology. Studying the growth response of T. austromongolica to extreme drought and flood on the upper reaches of the Yellow River will help assess the ecological resilience of ecologically fragile areas and provide a scientific basis for ecological construction and restoration in riparian zones on the Qingzang Plateau.

Key words: ecological resilience, resistance, ecological fragile region, drought, flood, climate change, Tamarix austromongolica

方欧娅, 张永, 张启, 贾恒锋. 黄河上游甘蒙柽柳生长对极端旱涝的响应. 植物生态学报, 2021, 45(6): 641-649. DOI: 10.17521/cjpe.2021.0020

FANG Ou-Ya, ZHANG Yong, ZHANG Qi, JIA Heng-Feng. Growth responses of Tamarix austromongolica to extreme drought and flood in the upper Yellow River basin. Chinese Journal of Plant Ecology, 2021, 45(6): 641-649. DOI: 10.17521/cjpe.2021.0020

导出引用管理器 EndNote|Ris|BibTeX

链接本文: https://www.plant-ecology.com/CN/10.17521/cjpe.2021.0020

https://www.plant-ecology.com/CN/Y2021/V45/I6/641

图/表 6

图1 甘蒙柽柳研究区地理位置(A)、采样方向说明(B)以及同德县然果村采样点实景图(C)。BD, 班多村; LQ, 上鹿圈村; RG, 然果村。

Fig. 1 Geographic location of the tamarisk (Tamarix austromongolica) research sites (A), explanation on sampling directions (B) and the real scenery of the sampling site at Ranguo village, Tongde County (C). BD, Banduo village; LQ, Shanglujuan village; RG, Ranguo village.

图2 1956-2018年唐乃亥水文站年实测总径流量及1956-2007年5-9月实测径流量。▲, 干旱年; ▼, 洪涝年。

Fig. 2 The measured annual total runoff from 1956 to 2018 and May-to-September runoff from 1956 to 2007 at the Tangnag Hydrological Station. ▲, drought year; ▼, flood year.

图3 黄河上游两组甘蒙柽柳在不同方向上对极端干旱(A)及洪涝(B)事件的抵抗力指数统计。

Fig. 3 Statistics of the resistance indices for two groups of Tamarix austromongolica in the upper Yellow River basin in different directions to extreme drought (A) and flood (B) events.

表1 黄河上游甘蒙柽柳在极端旱涝事件中A、B方向抵抗力指数差异检验

Table 1 Tests of differences in the resistance indices of Tamarix austromongolica in A and B directions to drought and flood events

事件 Event	组别 Group	配对t检验 Paired t-test			配对秩和检验 Wilcoxon signed rank test
事件 Event	组别 Group	t	df	p	V	p
干旱 Drought	受伤组 Injured group	0.824	19	0.420	132	0.330
干旱 Drought	对照组 Comparative group	1.526	25	0.139 (双侧) (two-sides) 0.069^* (单侧) (single-side)	238	0.116 (双侧) (two-sides) 0.058^* (单侧) (single-side)
洪涝 Flood	受伤组 Injured group	-2.204	18	0.041^ (双侧) (two-sides) 0.020^ (单侧) (single-side)	48	0.060^(双侧) (two-sides) 0.030^* (单侧) (single-side)
洪涝 Flood	对照组 Comparative group	-	-	-	157	0.895

图4 极端洪涝年两组甘蒙柽柳A、B方向抵抗力差值分布统计。

Fig. 4 Statistics distributions on of resistance differences between A and B directions in two groups of Tamarix austromongolica in extreme flood events.

表2 RG、BD和LQ样点甘蒙柽柳抵抗力平均值比较

Table 2 Comparison of the mean resistance indices of Tamarix austromongolica at the RG, BD and LQ sites

采样点 Sampling site	组别(株数) Group (Number of plants)	干旱 Drought		洪涝 Flood
采样点 Sampling site	组别(株数) Group (Number of plants)	A方向 Direction A	B方向 Direction B	A方向 Direction A	B方向 Direction B
RG	受伤组 Injured group (8)	0.99	0.97	0.99	1.08
RG	对照组 Comparative group (9)	1.05	1.03	1.03	1.02
BD	受伤组 Injured group (7)	0.94	0.91	1.04	1.09
BD	对照组 Comparative group (13)	0.96	0.92	1.02	1.02
LQ	受伤组 Injured group (5)	0.87	0.85	1.00	1.15
LQ	对照组 Comparative group (4)	0.89	0.88	1.23	1.48

参考文献 43

[1]	Allen CD, Macalady AK, Chenchouni H, Bachelet D, Mc- Dowell N, Vennetier M, Kitzberger T, Rigling A, Breshears DD, Hogg EH, Gonzalez P, Fensham R, Zhang Z, Castro J, Demidova N, et al. (2010). A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests. Forest Ecology and Management, 259, 660-684. DOI URL
[2]	Anderegg WRL, Schwalm C, Biondi F, Camarero JJ, Koch G, Litvak M, Ogle K, Shaw JD, Shevliakova E, Williams AP, Wolf A, Ziaco E, Pacala S (2015). Pervasive drought legacies in forest ecosystems and their implications for carbon cycle models. Science, 349, 528-532. DOI PMID
[3]	Arbellay E, Fonti P, Stoffel M (2012). Duration and extension of anatomical changes in wood structure after cambial injury. Journal of Experimental Botany, 63, 3271-3277. DOI PMID
[4]	Bär A, Michaletz ST, Mayr S (2019). Fire effects on tree physiology. New Phytologist, 223, 1728-1741. DOI URL
[5]	DeSoto L, Cailleret M, Sterck F, Jansen S, Kramer K, Robert EMR, Aakala T, Amoroso MM, Bigler C, Camarero JJ, Čufar K, Gea-Izquierdo G, Gillner S, Haavik LJ, Hereş AM, et al. (2020). Low growth resilience to drought is related to future mortality risk in trees. Nature Communications, 11, 545. DOI: 10.1038/s41467-020-14300-5. DOI PMID
[6]	Devitt DA, Salal A, Mace KA, Smith SD (1997). The effect of applied water on the water use of saltcedar in a desert riparian environment. Journal of Hydrology, 192, 233-246. DOI URL
[7]	Dong ZW, Li SY, Zhao Y, Lei JQ, Wang YD, Li CJ (2020). Stable oxygen-hydrogen isotopes reveal water use strategies of Tamarix taklamakanensis in the Taklimakan Desert, China. Journal of Arid Land, 12, 115-129.
[8]	Fang OY, Jia HF, Qiu HY, Ren HB(2017). Age of arboreous Tamarix austromongolica and its growth response to environment in Tongde County of Qinghai, China. Chinese Journal of Plant Ecology, 41, 738-748. DOI URL
	[ 方欧娅, 贾恒锋, 邱红岩, 任海保(2017). 青海省同德县乔木状甘蒙柽柳的年龄及其生长对环境的响应. 植物生态学报, 41, 738-748.]
[9]	Fang OY, Zhang QB (2019). Tree resilience to drought increases in the Tibetan Plateau. Global Change Biology, 25, 245-253. DOI URL
[10]	Flores BM, Holmgren M, Xu C, van Nes EH, Jakovac CC, Mesquita RCG, Scheffer M (2017). Floodplains as an Achilles’ heel of Amazonian forest resilience. Proceedings of the National Academy of Sciences of the United States of America, 114, 4442-4446.
[11]	Gazol A, Camarero JJ, Anderegg WRL, Vicente-Serrano SM (2017). Impacts of droughts on the growth resilience of Northern Hemisphere forests. Global Ecology and Biogeography, 26, 166-176. DOI URL
[12]	Ji P, Yuan X, Ma F, Pan M (2020). Accelerated hydrological cycle over the Sanjiangyuan region induces more streamflow extremes at different global warming levels. Hydrology and Earth System Sciences, 24, 5439-5451. DOI URL
[13]	Ji XM, Ning HS, Liang JY, Gao MY, Li L(2012). Comparison of drought resistance and photosynthetic characteristics of Haloxylon ammodendron and Tamarix hohenackeri at seedling stage under different moisture conditions. Journal of Desert Research, 32, 399-406.
	[ 吉小敏, 宁虎森, 梁继业, 高明月, 李磊(2012). 不同水分条件下梭梭和多花柽柳苗期光合特性及抗旱性比较. 中国沙漠, 32, 399-406.]
[14]	Kuang XX, Jiao JJ (2016). Review on climate change on the Tibetan Plateau during the last half century. Journal of Geophysical Research: Atmospheres, 121, 3979-4007. DOI URL
[15]	Li CF, Yang F, Zheng XQ, Han ZY, Pan HL, Zhou CL, Ji CR (2021). Changes in distribution and morphology of Tamarix ramosissima nebkhas in an oasis-desert ecotone. Geosciences Journal.DOI: 10.1007/s12303-020-0054-3. DOI
[16]	Li CJ, Chen T, Wang B, Xu GB, Zhang XW, Wu GJ(2019). Advances in research on the abnormal structure of tree-rings. Chinese Journal of Ecology, 38, 1538-1550.
	[ 李彩娟, 陈拓, 王波, 徐国保, 张轩文, 吴国菊(2019). 树轮异常结构的研究进展. 生态学杂志, 38, 1538-1550.]
[17]	Li CX, Lan HY(2021). Research progress in the stress tolerance mechanisms of desert plant Tamarix spp. Biotechnology Bulletin, 37, 17-29.
	[ 李彩霞, 兰海燕(2021). 荒漠植物柽柳抗逆机制的研究进展. 生物技术通报, 37, 17-29.]
[18]	Li D, Si JH, Zhang XY, Gao YY, Luo H, Qin J, Gao GL (2019). Comparison of branch water relations in two riparian species:Populus euphratica and Tamarix ramosissima. Sustainability, 11, 5461. DOI URL
[19]	Li XY, Liu LY, Gao SY, Shi PJ, Zou XY, Zhang CL (2005). Microcatchment water harvesting for growing Tamarix ramosissima in the semiarid loess region of China. Forest Ecology and Management, 214, 111-117. DOI URL
[20]	Liu HY, Williams AP, Allen CD, Guo DL, Wu XC, Anenkhonov OA, Liang EY, Sandanov DV, Yin Y, Qi ZH, Badmaeva NK (2013). Rapid warming accelerates tree growth decline in semi-arid forests of Inner Asia. Global Change Biology, 19, 2500-2510. DOI URL
[21]	Lloret F, Keeling EG, Sala A (2011). Components of tree resilience: effects of successive low-growth episodes in old ponderosa pine forests. Oikos, 120, 1909-1920. DOI URL
[22]	Moreno-Fernández D, Ledo A, Martín-Benito D, Cañellas I, Gea-Izquierdo G (2019). Negative synergistic effects of land-use legacies and climate drive widespread oak decline in evergreen Mediterranean open woodlands. Forest Ecology and Management, 432, 884-894. DOI
[23]	Mou YM, Fang OY, Cheng XH, Qiu HY (2019). Recent tree growth decline unprecedented over the last four centuries in a Tibetan juniper forest. Journal of Forestry Research, 30, 1429-1436. DOI URL
[24]	Nippert JB, Butler JJ, Kluitenberg GJ, Whittemore DO, Arnold D, Spal SE, Ward JK (2010). Patterns of Tamarix water use during a record drought. Oecologia, 162, 283-292. DOI PMID
[25]	Schurman JS, Trotsiuk V, Bače R, Cada V, Fraver S, Janda P, Kulakowski D, Labusova J, Mikoláš M, Nagel TA, Seidl R, Synek M, Svobodová K, Chaskovskyy O, Teodosiu M, et al. (2018). Large-scale disturbance legacies and the climate sensitivity of primary Picea abies forests. Global Change Biology, 24, 2169-2181. DOI URL
[26]	Sher A, Quigley MF (2013). Tamarix: a Case Study of Ecological Change in the American West. Oxford University Press, Oxford.
[27]	Snyder KA, Scott RL (2020). Longer term effects of biological control on tamarisk evapotranspiration and carbon dioxide exchange. Hydrological Processes, 34, 223-236. DOI URL
[28]	Stoffel M (2008). Dating past geomorphic processes with tangential rows of traumatic resin ducts. Dendrochronologia, 26, 53-60. DOI URL
[29]	Stromberg JC, Tluczek MGF, Hazelton AF, Ajami H (2010). A century of riparian forest expansion following extreme disturbance: spatio-temporal change in Populus/Salix/ amarix forests along the Upper San Pedro River, Arizona, USA. Forest Ecology and Management, 259, 1181-1189. DOI URL
[30]	Wang PL, Wang LQ, Liu ZY, Zhang TQ, Wang YY, Li YB, Gao CQ (2019). Molecular characterization and expression profiles of GRAS genes in response to abiotic stress and hormone treatment in Tamarix hispida. Trees, 33, 213-225. DOI URL
[31]	Wang TS, Sun BP, Feng L, Hu SJ, Yu MH(2013). Effects of different soil moisture contents on root growth characteristics of Tamarix austromongolica seedlings. Chinese Journal of Ecology, 32, 591-596.
	[ 王同顺, 孙保平, 冯磊, 胡生君, 于明含(2013). 不同水分处理对甘蒙柽柳幼苗根系生长特性的影响. 生态学杂志, 32, 591-596.]
[32]	Wang WQ, Ma ZJ, Feng LZ(2003). Plant for protecting ridge of terrace fields in hilly area of Qinghai: Tamarix austremongolica Nakai. Research of Soil and Water Conservation, 10, 112-115.
	[ 王文卿, 马占杰, 冯玲正(2003). 青海浅山区梯田护埂植物——甘蒙柽柳. 水土保持研究, 10, 112-115.]
[33]	Wei J, Zhang XM, Ma WD, Shan LS, Yan HL(2007). Seedling growth dynamics of Tamarix austromongolica and its acclimation strategy in hinterland of desert. Arid Land Geography, 30, 666-673.
	[ 魏疆, 张希明, 马文东, 单立山, 闫海龙(2007). 甘蒙柽柳幼苗生长动态及其对沙漠腹地生境条件的适应策略. 干旱区地理, 30, 666-673.]
[34]	Xia JB, Lang Y, Zhao QK, Liu P, Su L (2021). Photosynthetic characteristics of Tamarix chinensis under different groundwater depths in freshwater habitats. Science of the Total Environment, 761, 143221. DOI: 10.1016/j.scitotenv.2020.143221. DOI URL
[35]	Xiao SC, Xiao HL, Peng XM, Tian QY (2014). Intra-annual stem diameter growth of Tamarix ramosissima and association with hydroclimatic factors in the lower reaches of China’s Heihe River. Journal of Arid Land, 6, 498-510. DOI URL
[36]	Xu H, Li Y, Xie JX, Cheng L, Zhao Y, Liu R(2010). Influence of solar radiation and groundwater table on carbon balance of phreatophytic desert shrub Tamarix. Chinese Journal of Plant Ecology, 34, 375-386.
	[ 许皓, 李彦, 谢静霞, 程磊, 赵彦, 刘冉(2010). 光合有效辐射与地下水位变化对柽柳属荒漠灌木群落碳平衡的影响. 植物生态学报, 34, 375-386.]
[37]	Yang GY, Yu LL, Zhang KM, Zhao YL, Guo YC, Gao CQ (2017). A ThDREB gene from Tamarix hispida improved the salt and drought tolerance of transgenic tobacco and T. hispida. Plant Physiology and Biochemistry, 113, 187-197. DOI URL
[38]	Yang Y, Saatchi SS, Xu L, Yu YF, Choi S, Phillips N, Kennedy R, Keller M, Knyazikhin Y, Myneni RB (2018). Post- drought decline of the Amazon carbon sink. Nature Communications, 9, 3172. DOI: 10.1038/s41467-018-05668-6. DOI PMID
[39]	Yao TD, Thompson LG, Mosbrugger V, Zhang F, Ma YM, Luo TX, Xu BQ, Yang XX, Joswiak DR, Wang WC, Joswiak ME, Devkota LP, Tayal S, Jilani R, Fayziev R (2012). Third pole environment (TPE). Environmental Development, 3, 52-64. DOI URL
[40]	Zhang JQ, Qie JZ, Zhang Y(2020). Investigation of the distribution of traumatic resin ducts in Picea crassifolia. Mountain Research, 38, 710-716.
	[ 张建奇, 郄佳志, 张永(2020). 青海云杉创伤树脂道分布调查. 山地学报, 38, 710-716.]
[41]	Zhang L, Li GJ, Dong GQ, Wang M, Di DW, Kronzucker HJ, Shi WM (2019). Characterization and comparison of nitrate fluxes in Tamarix ramosissima and cotton roots under simulated drought conditions. Tree Physiology, 39, 628-640. DOI PMID
[42]	Zhang QB, Fang OY (2020). Tree rings circle an abrupt shift in climate. Science, 370, 1037-1038. DOI URL
[43]	Zhu JF, Liu JT, Lu ZH, Li JS, Sun JK (2018). Water-use strategies of coexisting shrub species in the Yellow River Delta, China. Canadian Journal of Forest Research, 48, 1099-1107. DOI URL

黄河上游甘蒙柽柳生长对极端旱涝的响应

Growth responses of Tamarix austromongolica to extreme drought and flood in the upper Yellow River basin

全文

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

图/表 6

参考文献 43

相关文章 15

编辑推荐

Metrics

本文评价

[1]	陈以恒玉素甫江·如素力阿卜杜热合曼·吾斯曼. 2001-2020年天山新疆段草地植被覆盖度时空变化及驱动因素分析[J]. 植物生态学报, 2024, 48(5): 561-576.
[2]	白皓然侯盟刘艳杰. 少花蒺藜草入侵与干旱对羊草草原生产力的影响机制[J]. 植物生态学报, 2024, 48(5): 577-589.
[3]	张计深, 史新杰, 刘宇诺, 吴阳, 彭守璋. 气候变化下中国潜在自然植被生态系统碳储量动态[J]. 植物生态学报, 2024, 48(4): 428-444.
[4]	臧妙涵, 王传宽, 梁逸娴, 刘逸潇, 上官虹玉, 全先奎. 基于纬度移栽的落叶松叶、枝、根生态化学计量特征对气候变暖的响应[J]. 植物生态学报, 2024, 48(4): 469-482.
[5]	梁逸娴, 王传宽, 臧妙涵, 上官虹玉, 刘逸潇, 全先奎. 落叶松径向生长和生物量分配对气候变暖的响应[J]. 植物生态学报, 2024, 48(4): 459-468.
[6]	吴茹茹, 刘美珍, 谷仙, 常馨月, 郭立月, 蒋高明, 祁如意. 气候变化对巨柏适宜生境分布的潜在影响和预测[J]. 植物生态学报, 2024, 48(4): 445-458.
[7]	杨宇萌, 来全, 刘心怡. 气候变化和人类活动对内蒙古植被总初级生产力的定量影响[J]. 植物生态学报, 2024, 48(3): 306-316.
[8]	张启, 程雪寒, 王树芝. 北京西山老龄树记载的森林干扰历史[J]. 植物生态学报, 2024, 48(3): 341-348.
[9]	韩路, 冯宇, 李沅楷, 王雨晴, 王海珍. 地下水埋深对灰胡杨叶片与土壤养分生态化学计量特征及其内稳态的影响[J]. 植物生态学报, 2024, 48(1): 92-102.
[10]	吴瀚, 白洁, 李均力, 古丽•加帕尔, 包安明. 新疆地区植被覆盖度时空变化及其影响因素分析[J]. 植物生态学报, 2024, 48(1): 41-55.
[11]	马常钦, 黄海龙, 彭政淋, 吴纯泽, 韦庆钰, 贾红涛, 卫星. 水曲柳雌雄株复叶类型及光合功能对不同生境的响应[J]. 植物生态学报, 2023, 47(9): 1287-1297.
[12]	韩聪, 母艳梅, 查天山, 秦树高, 刘鹏, 田赟, 贾昕. 2012-2016年宁夏盐池毛乌素沙地黑沙蒿灌丛生态系统通量观测数据集[J]. 植物生态学报, 2023, 47(9): 1322-1332.
[13]	施梦娇, 李斌, 伊力塔, 刘美华. 美洲黑杨幼苗生长和生理生态指标对干旱-复水响应的性别差异[J]. 植物生态学报, 2023, 47(8): 1159-1170.
[14]	王晓悦, 许艺馨, 李春环, 余海龙, 黄菊莹. 长期降水量变化下荒漠草原植物生物量、多样性的变化及其影响因素[J]. 植物生态学报, 2023, 47(4): 479-490.
[15]	任培鑫, 李鹏, 彭长辉, 周晓路, 杨铭霞. 洞庭湖流域植被光合物候的时空变化及其对气候变化的响应[J]. 植物生态学报, 2023, 47(3): 319-330.