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Encroachment drives facilitation at alpine shrublines

Forest Ecosystems 2024年第1期11卷 62-72页

作者： Yafeng Wang eryuan liang J.Julio Camarero College of Ecology and Environment Nanjing Forestry UniversityNanjing210037China State Key Laboratory of Tibetan Plateau Earth System Environment and Resources(TPESER)Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing100101China Instituto Pirenaico de Ecología(IPE-CSIC) Zaragoza50080Spain

Ongoing encroachment is driving recent alpine shrubline dynamics globally,but the role of shrub-shrub interactions in shaping shrublines and their relationships with stem density changes remain poorly understood.Here,the size and age of shrubs from 26 Salix shrubline populations along a 900-km latitudinal gradient(30°-38°N)were measured and mapped across the eastern Tibetan Plateau.Point pattern analyses were used to quantify the spatial distribution patterns of juveniles and adults,and to assess spatial associations between them.Mean intensity of univariate and bivariate spatial patterns was related to biotic and abiotic variables.Bivariate mark correlation functions with a quantitative mark(shrub height,basal stem diameter,crown width)were also employed to investigate the spatial relationships between shrub traits of juveniles and adults.Structural equation models were used to explore the relationships among conspecific interactions,patterns,shrub traits and recruitment dynamics under climate change.Most shrublines showed clustered patterns,suggesting the existence of conspecific facilitation.Clustered patterns of juveniles and conspecific interactions(potentially facilitation)tended to intensify with increasing soil moisture stress.Summer warming before 2010 triggered positive effects on population interactions and spatial patterns via increased shrub recruitment.However,summer warming after2010 triggered negative effects on interactions through reduced shrub recruitment.Therefore,shrub recruitment shifts under rapid climate change could impact spatial patterns,alter conspecific interactions and modify the direction and degree of shrublines responses to climate.These changes would have profound implications for the stability of alpine woody ecosystems.

关键词： Alpine shrubline Positive interactions Facilitation Spatial clustering Point pattern analyses

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Linking leaf elemental traits to biomass across forest biomes in the Himalayas

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Science China Earth Sciences 2024年第5期67卷 1518-1528页

作者： Nita DYOLA eryuan liang Josep PEÑUELAS J.Julio CAMARERO Shalik Ram SIGDEL Sugam ARYAL Wentao LIN Xiang LIU Yongwen LIU Xingliang XU Sergio ROSSI State Key Laboratory of Tibetan Plateau Earth System Environment and Resources(TPESER)Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China University of Chinese Academy of Sciences Beijing 100049China Laboratoire sur lesécosystèmes terrestres boréaux Département des Sciences FondamentalesUniversitédu QuébecàChicoutimi555Boulevard de l′UniversitéChicoutimi(QC)G7H2B1Canada CSIC Global Ecology Unit CREAF-CSIC-UABBellaterraE-08193 CataloniaSpain CREAF Cerdanyola del VallèsE-08193 CataloniaSpain Instituto Pirenaico de Ecología(IPE-CSIC) Avenida Montañana 1005Zaragoza 50059Spain Friedrich-Alexander-Universität Erlangen-Nürnberg Institut für GeographieErlangen 91058Germany State Key Laboratory of Grassland Agro-Ecosystems College of EcologyLanzhou UniversityLanzhou 730000China Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of SciencesBeijing 100101China

Plants require a number of essential elements in different proportions for ensuring their growth and development.The elemental concentrations in leaves reflect the functions and adaptations of plants under specific environmental conditions.However,less is known about how the spectrum of leaf elements associated with resource acquisition,photosynthesis and growth regulates forest biomass along broad elevational gradients.We examined the influence of leaf element distribution and diversity on forest biomass by analyzing ten elements(C,N,P,K,Ca,Mg,Zn,Fe,Cu,and Mn)in tree communities situated every 100 meters along an extensive elevation gradient,ranging from the tropical forest(80 meters above sea level)to the alpine treeline(4200 meters above sea level)in the Kangchenjunga Landscape in eastern Nepal Himalayas.We calculated communityweighted averages(reflecting dominant traits governing biomass,i.e.,mass-ratio effect)and functional divergence(reflecting increased trait variety,i.e.,complementarity effect)for leaf elements in a total of 1,859 trees representing 116 species.An increasing mass-ratio effect and decreasing complementarity in leaf elements enhance forest biomass accumulation.A combination of elements together with elevation explains biomass(52.2%of the variance)better than individual elemental trait diversity(0.05%to 21%of the variance).Elevation modulates trait diversity among plant species in biomass accumulation.Complementarity promotes biomass at lower elevations,but reduces biomass at higher elevations,demonstrating an interaction between elevation and complementarity.The interaction between elevation and mass-ratio effect produces heterogeneous effects on biomass along the elevation gradient.Our research indicates that biomass accumulation can be disproportionately affected by elevation due to interactions among trait diversities across vegetation zones.While higher trait variation enhances the adaptation of species to environmental changes,it reduces biomass accumulation,especially at higher elevat

关键词： Ecosystem function Elevational gradient Functional diversity Functional traits Leaf elements Niche complementarity

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互利作用促进了高山树线幼苗的存活

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Journal of Plant Ecology 2024年第3期17卷 115-127页

作者： Wensheng Chen Jiangrong Li Jesús Julio Camarero Huihui Ding Fangwei Fu Yueyao Li Xiangyu Zheng Xiaoxia Li Wei Shen Shalik Ram Sigdel Steven W.Leavitt eryuan liang Institute of Tibet Plateau Ecology Tibet Agricultural&Animal Husbandry UniversityNyingchi 860000China Key Laboratory of Forest Ecology in Tibet Plateau(Tibet Agricultural&Animal Husbandry University) Ministry of EducationNyingchi 860000China National Forest Ecosystem Observation&Research Station of Nyingchi Tibet Nyingchi 860000China Key Laboratory of Alpine Vegetation Ecological Security in Tibet Nyingchi 860000China Zhejiang Zhoushan Archipelago Observation and Research Station Zhejiang Tiantong Forest Ecosystem National Observation and Research Stationand Shanghai Key Lab for Urban Ecological Processes and Eco-RestorationSchool of Ecological and Environmental SciencesEast China Normal UniversityShanghai 200241China State Key Laboratory of Tibetan Plateau Earth System Resources and Environment(TPESRE)Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China Instituto Pirenaico de Ecología(IPE-CSIC) Zaragoza 50059Spain Anhui Province Key Lab of Farmland Ecological Conservation and Pollution Prevention Key Laboratory of JiangHuai Arable Land Resources Protection and Eco-restorationMinistry of Natural ResourcesCollege of Resources and EnvironmentAnhui Agricultural UniversityHefei 230036China Laboratory of Tree-Ring Research University of ArizonaTucsonAZ 85721USA

高山树线被视为记录气候变化对树木和森林影响的生态监测器。迄今为止,大多数树线研究都集中在气候变化如何驱动树线动态的变化。然而,关于生物相互作用如何调节树线变化,特别是在树木更新这一树线动态的瓶颈方面,人们知之甚少。本研究... 详细信息

高山树线被视为记录气候变化对树木和森林影响的生态监测器。迄今为止,大多数树线研究都集中在气候变化如何驱动树线动态的变化。然而,关于生物相互作用如何调节树线变化,特别是在树木更新这一树线动态的瓶颈方面,人们知之甚少。本研究假设种间和种内促进作用决定了高山树线树苗的定居和存活。为了验证这一假设,我们在青藏高原东南部的色季拉山高山树线交错区(海拔4300–4500 m)的3个生长生境(林冠内、林冠外和草地)中共计移植了630株不同年龄(4–6年、7–9年和10–15年)的急尖长苞冷杉(Abies georgei var.smithii)幼苗,连续3年监测了移植后幼苗的微气候、高度生长、死亡率和叶片功能性状。结果发现,叶片功能性状的变化是由微气候驱动的。移植后,叶片可溶性糖和淀粉浓度以及C:P比增加,而叶面积减小。幼苗的资源利用逐渐转向更保守的策略,其背后机制主要受到了生理性状(非结构性碳水化合物和植物养分)的介导。同时,由结构方程模型发现太阳辐射、温度和水分条件在植物相互作用下,通过介导叶片形态性状的变化最终影响了幼苗的死亡率和年生长。上述研究结果表明,植物间的互利作用通过改变太阳辐射和叶片功能性状,最终在决定幼苗生长和存活上起到至关重要的作用,同时也为理解全球气候变化背景下高山树线动态变化的驱动机制提供了新的见解。

关键词：青藏高原移栽实验叶片功能性状太阳辐射

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火山喷发对陆地植被与碳循环影响的研究进展

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科学通报 2024年第2期69卷 160-168页

作者：张原梁尔源汪涛朴世龙中国科学院青藏高原研究所高寒生态重点实验室北京100101 Laboratory for Sciences of Climate and Environment Institute Pierre-Simon LaplaceFrench Alternative Energies and Atomic Energy Commission/French National Centre for Scientific Research/Versailles-St-Quentin UniversityGif sur Yvette 91191France 中国科学院青藏高原地球科学卓越创新中心北京100101 北京大学城市与环境学院北京100871

1991年,Pinatubo火山喷发导致全球大气二氧化碳浓度上升态势出现停滞,这一现象揭示了地球内部系统可以通过火山活动对地表生物地球化学循环产生重大影响.近些年,火山喷发对陆地生态系统的影响及其驱动机制引起科学界的广泛讨论.本文系... 详细信息

1991年,Pinatubo火山喷发导致全球大气二氧化碳浓度上升态势出现停滞,这一现象揭示了地球内部系统可以通过火山活动对地表生物地球化学循环产生重大影响.近些年,火山喷发对陆地生态系统的影响及其驱动机制引起科学界的广泛讨论.本文系统梳理了火山喷发对陆地生态系统影响的研究,总结了火山活动的辐射效应和气候效应对树木生长和陆地碳循环产生影响的机制.大型火山喷发形成的平流层气溶胶一方面引起散射辐射增加促进光合作用,另一方面,还引起总辐射减弱抑制光合作用,由于散射辐射的影响相比更强,总体上火山辐射效应有利于陆地碳汇的增加.火山的气候效应体现在全球尺度的降温和区域降水的改变.降温作用在低纬地区促进植被的光合作用,在高纬地区抑制光合作用,同时在全球尺度减弱生态系统的呼吸作用,总体上也有利于增加碳汇.对火山造成降水变化影响的评估目前还存在较大不确定性.在对这些机制总结的基础上,本文评述了当前的认识盲点和研究难点,以期为未来进一步推进火山喷发影响的研究、完善地球内外系统联动机制的认识提供参考.

关键词：火山爆发陆地生态系统火山冷却效应散射辐射碳循环

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Warming-induced phenological mismatch between trees and shrubs explains high-elevation forest expansion

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National Science Review 2023年第10期10卷 62-71页

作者： Xiaoxia Li eryuan liang J.Julio Camarero Sergio Rossi Jingtian Zhang Haifeng Zhu Yongshuo H.Fu Jian Sun Tao Wang Shilong Piao Josep Pe?uelas State Key Laboratory of Tibetan Plateau Earth System Environment and Resources (TPESER)Institute of Tibetan Plateau ResearchChinese Academy of Sciences Laboratoire sur les écosystèmes terrestres boréaux Département des Sciences FondamentalesUniversité du Québec à Chicoutimi Instituto Pirenaico de Ecología (IPE-CSIC) College of Water Sciences Beijing Normal University CREAF Cerdanyola del Valles CSIC Global Ecology Unit CREAF-CSIC-UAB

Despite the importance of species interaction in modulating the range shifts of plants,little is known about the responses of coexisting life forms to a warmer climate.Here,we combine long-term monitoring of cambial phenology in sympatric trees and shrubs at two treelines of the Tibetan Plateau,with a meta-analysis of ring-width series from 344 shrubs and 575 trees paired across 11 alpine treelines in the Northern Hemisphere.Under a spring warming of +1℃,xylem resumption advances by 2-4 days in trees,but delays by 3-8 days in shrubs.The divergent phenological response to warming was due to shrubs being3.2 times more sensitive than trees to chilling accumulation.Warmer winters increased the thermal requirement for cambial reactivation in shrubs,leading to a delayed response to warmer springs.Our meta-analysis confirmed such a mechanism across continental scales.The warming-induced phenological mismatch may give a competitive advantage to trees over shrubs,which would provide a new explanation for increasing alpine treeline shifts under the context of climate change.

关键词： chilling climate warming forcing treeline shift xylogenesis

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Critical minimum temperature limits xylogenesis and maintains treelines on the southeastern Tibetan Plateau

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Science Bulletin 2017年第11期62卷 804-812页

作者： Xiaoxia Li eryuan liang Jozica Gricar Sergio Rossi Katarina Cufar Aaron M. Ellison Key Laboratory of Alpine Ecology and Biodiversity Key Laboratory of Tibetan Environment Changes and Land Surface Processes Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100101 China CAS Center for Excellence in Tibetan Plateau Earth Sciences Beijing 100101 China Sloven ian Forestry Institute Department of Yield and Silviculture Vecna pot 2 S1-1000 Ljubljana Slovenia University of Quebec in Chicoutimi Departement des Sciences Fondamentales 555 Boulevard de l'Universite Chicoutimi (QC) G7H2B1 Canada Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems Guangdong Provincial Key Laboratory of Applied Botany South China Botanical Garden Chinese Academy of Sciences Guangzhou 510650 China University of Ljubljana Biotechnical Faculty Department of Wood Science and Technology Jamnikarjeva 101 S1-1000 Ljubljana Slovenia Harvard Forest Harvard University 324 North Main St. Petersham MA 01366 USA

Physiological and ecological mechanisms that define treelines are still debated.It has been suggested that the absence of trees above the treeline is caused by low temperatures that limit growth.Thus,we hypothesized that there is a critical minimum temperature(CTmin) preventing xylogenesis at treeline.We tested this hypothesis by examining weekly xylogenesis across three and four growing seasons in two natural Smith fir(Abies georgei var.smithii) treeline sites on the southeastern Tibetan Plateau.Despite differences in the timing of cell differentiation among years,minimum air temperature was the dominant climatic variable associated with xylem growth;the critical minimum temperature(CTmin) for the onset and end of xylogenesis occurred at 0.7 ± 0.4 °C.A process-based modelling chronology of tree-ring formation using this CTminwas consistent with actual tree-ring data.This extremely low CTminpermits Smith fir growing at treeline to complete annual xylem production and maturation and provides both support and a mechanism for treeline formation.

关键词：西藏高原临界温度东南部温度范围生态机制生长季节树轮年代学木质部

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Strong link between large tropical volcanic eruptions and severe droughts prior to monsoon in the central Himalayas revealed by tree-ring records

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Science Bulletin 2019年第14期64卷 1018-1023页

作者： eryuan liang Binod Dawadi Neil Pederson Shilong Piao Haifeng Zhu Shalik Ram Sigdel Deliang Chen Key Laboratory of Alpine Ecology Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100101 China Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences Beijing 100101 China Central Department of Hydrology and Meteorology Tribhuvan University Kathmandu Nepal Harvard Forest Harvard University Petersham MA 01366 USA College of Urban and Environmental Sciences Peking University Beijing 100871 China Key Laboratory of Tibetan Environment Changes and Land Surface Processes Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100101 China Regional Climate Group Department of Earth Sciences University of Gothenburg Gothenburg 40530 Sweden

Large tropical volcanic eruptions can cause short-term global cooling. However, little is known whether large tropical volcanic eruptions, like the one in Tambora/Indonesia in 1815, cause regional hydroclimatic anomalies. Using a tree-ring network of precisely dated Himalayan birch in the central Himalayas, we reconstructed variations in the regional pre-monsoon precipitation back to 1650 CE. A superposed epoch analysis indicates that the pre-monsoon regional droughts are associated with large tropical volcanic eruptions, appearing to have a strong influence on hydroclimatic conditions in the central Himalayas. In fact, the most severe drought since 1650 CE occurred after the Tambora eruption. These results suggest that dry conditions prior to monsoon in the central Himalayas were associated with explosive tropical volcanism. Prolonged La Ni?a events also correspond with persistent pre-monsoon droughts in the central Himalayas. Our results provide evidence that large tropical volcanic eruptions most likely induced severe droughts prior to monsoon in the central Himalayas.

关键词： Tree ring Drought Tropical volcanic eruptions Central Himalayas

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Toward a sustainable grassland ecosystem worldwide

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The Innovation 2022年第4期3卷 15-16页

作者： Jian Sun Yi Wang Shilong Piao Miao Liu Guodong Han Junran Li eryuan liang Tien Ming Lee Guohua Liu Andreas Wilkes Shiliang Liu Wenwu Zhao Huakun Zhou Mesenbet Yibeltal Mulatu Liyew Berihun Dawn Browning Ayele Almaw Fenta Atsushi Tsunekawa Joel Brown Walter Willms Mitsuru Tsubo State Key Laboratory of Earth System Resources and Environment of Tibetan Plateau Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China School of Life Sciences and School of Ecology State Key Lab of Biological ControlSun Yat-sen UniversityGuangzhou 510275China Sino-French Institute for Earth System Science College of Urban and Environmental SciencesPeking UniversityBeijing 100871China College of Grassland Science and Technology China Agricultural UniversityBeijing 100193China Key Laboratory of Grassland Resources of the Ministry of Education College of GrasslandResources and EnvironmentInner Mongolia Agricultural UniversityHohhot 010011China Department of Geosciences The University of TulsaTulsaOK 74137USA State Key Laboratory of Urban and Regional Ecology Research Center for Eco-Environmental SciencesChinese Academy of SciencesBeijing 100085China Values for Development Ltd Bury St.Edmunds IP333EQUK School of Environment Beijing Normal UniversityBeijing 100875China Faculty of Geographical Science Beijing Normal UniversityBeijing 100875China Key Laboratory of Restoration Ecology for Cold Regions in Qinghai Northwest Institute of Plateau BiologyChinese Academy of SciencesXining 810008China Faculty of Civil and Water Resource Engineering Bahir Dar Institute of TechnologyBahir Dar UniversityBahir DarEthiopia Arid Land Research Center Tottori UniversityTottori 6800001Japan USDA–ARS Jornada Experimental Range Las CrucesNM 88003USA USDA NRCS Jornada Experimental RangeNew Mexico State UniversityMSC 3JERPO Box 30003Las CrucesNMUSA Agriculture and Agri-Food Canada Lethbridge Research Centre54031st Avenue SouthLethbridgeABCanada

Globally,grasslands,covering about 40%of the Earth’s land area,are vital for supporting important ecosystem functions,services,and livelihoods of millions of humans.Currently,grassland degradation is a major threat to the maintenance of ecological services,1 food security,and sustainable development,and directly hinders the global efforts with meeting goals and targets such as the The UN Decade on Ecosystem Restoration and Sustainable Development Goals(SDGs).Remote sensing approaches have the advantages of spanning large geographical areas withmultiple spatial,spectral,and temporal resolutions.In global scale,remote sensing methods used normalized difference vegetation index to determine net primary productivity(NPP),which still is the effectivemethod to indicate grassland conditions.To master the general situation of grassland,we analyzed the global spatial-temporal variation of NPP from 2001 to 2019 at the pixel level across the globe.As presented in Figure 1A,the NPP values of global grasslands showed an obvious variation trend,which indicated a considerable distribution pattern of spatial heterogeneity.The decreasing and increasing trend in grassland NPP covered approximately 25.3%and 74.5%of the total grassland area,respectively.

关键词： grassland Figure hinder

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Spatiotemporal variability in tree ring's δ^(13)C of Picea crassifolia in the Qilian Mountains:climatic significance and responses to rising CO_2

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Research in Cold and Arid Regions 2011年第2期3卷 93-102页

作者： XiaoHong Liu WenLing An eryuan liang WenZhi Wang XueMei Shao Lei Huang DaHe Qin State Key Laboratory of Cryospheric Sciences CoM and Arid Regions Environmental and Engineering Research Institute Lanzhou Gansu 730000 China Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100085 China Institute of Geographical Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 China National Climate Centre China Meteorological Administration Beijing 100081 China

Abstract：The carbon isotopic composition （δ13C） of tree rings was used to assess changes in intrinsic water-use efficiency （Wi） to increasing atmospheric CO2 and climate change during the period of 1891–2003. Five Qinghai spruce （Picea crassifolia） stands were selected in the Qilian Mountains, growing along a precipitation gradient. All five δ13C were correlated to each other, but two sites （DDS and CLS）, which are far from the main body of the mountains, show relative weak connections to other sites. Although trees at all sites had improved their Wi in response to increasing atmospheric CO2 concentration, spruce growing in the regions far away from the main body of the mountains were less sensitive to improved Wi than those of other sites. Based on the correlation between carbon isotope discrimination （Δ） and Palmer Drought Severity Index （PDSI）, the drought history covering the period of 1891–2003 was reconstructed in the study region. The two most severe drought epochs of the late 1920s and the last decade were caused by reduced precipitation and climate warming, respectively. Our results will be useful in assessing any further spatial climate-related bioclimatic information.

关键词： Tree-ring δ13C intrinsic water-use efficiency drought history Picea crassifolia Qilian Motmtains

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Tree-ring based PDSI reconstruction since AD 1842 in the Ortindag Sand Land,east Inner Mongolia

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Chinese Science Bulletin 2007年第19期52卷 2715-2721页

作者： liang eryuan SHAO XueMei LIU HongYan ECKSTEIN Dieter Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100085 China Institute of Geographic Science and Natural Resource Research Chinese Academy of Sciences Beijing 100101 China College of Environmental Science Peking University Beijing 100871 China Department of Wood Science University of Hamburg Hamburg D-21031 Germany

epartment of Wood Science, University of Hamburg, Hamburg D-21031, GermanyBased on three Chinese pine (Pinus tabulaeformis Carr.) and one Meyer spruce (Picea meyeri Rehd. et Wils.) ring-width chronologies, a 163-year drought history was reconstructed in the eastern Ortindag Sand Land. All tree-ring chronologies show large inter-annual variations and strong common signals and fairly consistent variation between different chronologies, indicating that they are excellent proxy of regional climate. A regional chronology (RC) was established by averaging the four standard chronologies and further employed for the analysis and climatic reconstruction. The analysis revealed that tree growth is primarily limited by low precipitation in February-March and June-July and high temperature in May-July. In addition, RC has high correlations with the monthly Palmer drought severity index (PDSI) prior to and during the growing season because the PDSI considers the accumulation of the droughts. Response function analysis revealed that RC only exhibits significant correlations with the PDSI in June and July (close to the 95% significance level in May). Because May―July is a critical period for tree growth, the average May-July PDSI (PDSI5-7) was reconstructed back to 1842 using RC in the Ortindag Sand Land. The reconstruction can explain 52% of the PDSI variance and the equation was rather stable over time. It agrees well with the variation of the average dryness/wetness indices in North China,and captures the decline process of the East Asian summer monsoon since the mid-1960s. It is worth noting that the Ortindag Sand Land has experienced the most severe drought in the recent 40 years based on the 163-year drought reconstruction. Like summer precipitation in North China the reconstructed PDSI5-7 also displays a 20-year oscillation.

关键词：干旱沙地环境地质

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