生物多样性 ›› 2022, Vol. 30 ›› Issue (6): 21503. DOI: 10.17520/biods.2021503
所属专题: 青藏高原生物多样性与生态安全; 物种形成与系统进化
王健铭1,3, 曲梦君1, 王寅1, 冯益明2, 吴波2, 卢琦2, 何念鹏3, 李景文1,*()
收稿日期:
2021-12-07
接受日期:
2022-02-11
出版日期:
2022-06-20
发布日期:
2022-04-20
通讯作者:
李景文
作者简介:
* E-mail: lijingwenhy@bjfu.edu.cn基金资助:
Jianming Wang1,3, Mengjun Qu1, Yin Wang1, Yiming Feng2, Bo Wu2, Qi Lu2, Nianpeng He3, Jingwen Li1,*()
Received:
2021-12-07
Accepted:
2022-02-11
Online:
2022-06-20
Published:
2022-04-20
Contact:
Jingwen Li
摘要:
戈壁荒漠广泛分布于全球干旱和极旱区域, 是我国陆地生态系统的重要组成部分。由于自然环境恶劣和交通条件限制, 目前有关戈壁植物群落物种、功能和系统发育等多维度β多样性形成机制的系统研究还很缺乏, 严重制约着对戈壁植物多样性维持机制的认知。本文以青藏高原北部61个典型戈壁生境植物群落为研究对象, 通过构建系统发育树和测量8个关键功能性状, 获取戈壁生境的物种、功能和系统发育β多样性, 比较3个维度β多样性格局与零模型的差异, 同时量化环境距离和地理距离对其的相对影响, 以探讨戈壁植物多样性的形成机制。结果显示: (1)戈壁植物的物种、功能和系统发育β多样性均表现出显著的距离衰减效应; (2)戈壁植物的物种、功能和系统发育β多样性均表现为非随机的格局; (3)由于功能性状趋同进化, 植物功能和系统发育β多样性变化趋势并不一致; (4)环境差异对植物3个维度β多样性均有着比空间距离更为重要的影响, 且土壤含水量、地表砾石盖度等局域生境因素的影响比气候更为强烈。以上结果表明, 戈壁植物的β多样性可能主要由局域生境过滤作用控制, 且不同维度的β多样性分布格局并不一致。
王健铭, 曲梦君, 王寅, 冯益明, 吴波, 卢琦, 何念鹏, 李景文 (2022) 青藏高原北部戈壁植物群落物种、功能与系统发育β多样性分布格局及其影响因素. 生物多样性, 30, 21503. DOI: 10.17520/biods.2021503.
Jianming Wang, Mengjun Qu, Yin Wang, Yiming Feng, Bo Wu, Qi Lu, Nianpeng He, Jingwen Li (2022) The drivers of plant taxonomic, functional, and phylogenetic β-diversity in the gobi desert of northern Qinghai-Tibet Plateau. Biodiversity Science, 30, 21503. DOI: 10.17520/biods.2021503.
图1 青藏高原北部戈壁荒漠区植被调查样点分布图。戈壁荒漠分布区底图数据来源于冯益明和卢琦(2017)。
Fig. 1 Distribution of survey sites in gobi deserts of northern Qinghai-Tibet Plateau. The gobi deserts map dataset was provided by Feng and Lu (2017).
功能性状 Functional trait | Blomberg’s K | P |
---|---|---|
叶片氮含量 Leaf nitrogen concentrations (LNC) | 0.10 | 0.29 |
叶片磷含量 Leaf phosphorus concentrations (LPC) | 0.10 | 0.32 |
叶面积 Leaf area (LA) | 0.43 | 0.03 |
比叶面积 Specific leaf area (SLA) | 0.08 | 0.52 |
细根氮含量 Fine root nitrogen concentrations (RNC) | 0.17 | 0.09 |
细根磷含量 Fine root phosphorus concentrations (RPC) | 0.07 | 0.66 |
根长 Root length (RL) | 0.41 | 0.02 |
比根长 Specific root length (SRL) | 0.19 | 0.10 |
表1 8个功能性状的系统发育信号
Table 1 Phylogenetic signal for eight functional traits
功能性状 Functional trait | Blomberg’s K | P |
---|---|---|
叶片氮含量 Leaf nitrogen concentrations (LNC) | 0.10 | 0.29 |
叶片磷含量 Leaf phosphorus concentrations (LPC) | 0.10 | 0.32 |
叶面积 Leaf area (LA) | 0.43 | 0.03 |
比叶面积 Specific leaf area (SLA) | 0.08 | 0.52 |
细根氮含量 Fine root nitrogen concentrations (RNC) | 0.17 | 0.09 |
细根磷含量 Fine root phosphorus concentrations (RPC) | 0.07 | 0.66 |
根长 Root length (RL) | 0.41 | 0.02 |
比根长 Specific root length (SRL) | 0.19 | 0.10 |
图2 青藏高原北部戈壁植物群落物种、功能(平均最近邻体性状距离)和系统发育(平均最近邻体系统发育距离) β多样性观测值(a-c)及其标准效应(d-e)随地理距离的变化趋势
Fig. 2 Variation in plant taxonomic, functional (mean nearest neighbor trait distance), and phylogenetic (mean nearest neighbor phylogenetic distance) β-diversity observed values (a-c) and their standardized effect sizes (d-e) along geographic distance in the gobi deserts of northern Qinghai-Tibet Plateau
环境差异 Environmental difference | 物种β多样性 Taxonomic β-diversity | 功能β多样性 Functional β-diversity | 系统发育β多样性 Phylogenetic β-diversity | |||
---|---|---|---|---|---|---|
观测值 OV | 标准效应 SES | 观测值 OV | 标准效应 SES | 观测值 OV | 标准效应 SES | |
太阳辐射强度 Solar radiation | 0.140** | 0.167** | 0.102 | 0.104 | 0.021 | -0.0002 |
年均温 Annual mean temperature | 0.144** | 0.117** | 0.146* | 0.105 | -0.004 | -0.091 |
温度季节性 Temperature seasonality | 0.112* | 0.065 | 0.117 | 0.039 | 0.091 | 0.026 |
年降水量 Annual precipitation | 0.012 | 0.02 | -0.056 | -0.118 | -0.081 | -0.116 |
降水季节性 Precipitation seasonality | 0.055 | 0.105 | -0.071 | -0.098 | -0.02 | 0.003 |
地表砾石盖度 Gravel coverage | 0.268*** | 0.204*** | 0.372*** | 0.226*** | 0.35*** | 0.191*** |
土壤含水量 Soil moisture content | 0.295*** | 0.270*** | 0.431*** | 0.335*** | 0.27*** | 0.116 |
土壤氮含量 Soil total nitrogen content | 0.017 | 0.089 | -0.021 | 0.031 | 0.014 | 0.071 |
土壤有机碳含量 Soil organic carbon content | 0.104 | 0.123* | 0.199** | 0.175** | 0.013 | -0.056 |
土壤pH值 Soil pH | 0.323*** | 0.328*** | 0.353*** | 0.216** | 0.325*** | 0.183* |
表2 青藏高原北部戈壁植物群落物种、功能(平均最近邻体性状距离)和系统发育(平均最近邻体系统发育距离) β多样性观测值及其标准效应与不同环境因素差异间的相关性
Table 2 Mantel tests for the relationships of plant taxonomic, functional (mean nearest neighbor trait distance), and phylogenetic (mean nearest neighbor phylogenetic distance) β-diversity observed values (OV) and their standard effect size (SES) of with different environmental factors in the gobi deserts of northern Qinghai-Tibet Plateau
环境差异 Environmental difference | 物种β多样性 Taxonomic β-diversity | 功能β多样性 Functional β-diversity | 系统发育β多样性 Phylogenetic β-diversity | |||
---|---|---|---|---|---|---|
观测值 OV | 标准效应 SES | 观测值 OV | 标准效应 SES | 观测值 OV | 标准效应 SES | |
太阳辐射强度 Solar radiation | 0.140** | 0.167** | 0.102 | 0.104 | 0.021 | -0.0002 |
年均温 Annual mean temperature | 0.144** | 0.117** | 0.146* | 0.105 | -0.004 | -0.091 |
温度季节性 Temperature seasonality | 0.112* | 0.065 | 0.117 | 0.039 | 0.091 | 0.026 |
年降水量 Annual precipitation | 0.012 | 0.02 | -0.056 | -0.118 | -0.081 | -0.116 |
降水季节性 Precipitation seasonality | 0.055 | 0.105 | -0.071 | -0.098 | -0.02 | 0.003 |
地表砾石盖度 Gravel coverage | 0.268*** | 0.204*** | 0.372*** | 0.226*** | 0.35*** | 0.191*** |
土壤含水量 Soil moisture content | 0.295*** | 0.270*** | 0.431*** | 0.335*** | 0.27*** | 0.116 |
土壤氮含量 Soil total nitrogen content | 0.017 | 0.089 | -0.021 | 0.031 | 0.014 | 0.071 |
土壤有机碳含量 Soil organic carbon content | 0.104 | 0.123* | 0.199** | 0.175** | 0.013 | -0.056 |
土壤pH值 Soil pH | 0.323*** | 0.328*** | 0.353*** | 0.216** | 0.325*** | 0.183* |
图3 青藏高原北部戈壁植物群落物种、功能(平均最近邻体性状距离)和系统发育(平均最近邻体系统发育距离) β多样性(a-c)及其标准效应(d-e)与地表砾石盖度差异的关系
Fig. 3 The relationships of plant taxonomic, functional (mean nearest neighbor trait distance), and phylogenetic (mean nearest neighbor phylogenetic distance) β-diversity observed value (a-c) and their standardized effect size (d-e) with gravel coverage divergence in the gobi deserts of northern Qinghai-Tibet Plateau
图4 青藏高原北部戈壁植物群落物种(a)、功能和系统发育β多样性(b-c)标准效应与零值的比较。(b)平均最近邻体性状距离和平均最近邻体系统发育距离; (c)平均成对性状距离和平均成对系统发育距离。*** P < 0.001。
Fig. 4 Comparison of the standardized effect size for plant taxonomic (a), functional, and phylogenetic β-diversity (b-c) with zero value across the gobi deserts of northern Qinghai-Tibet Plateau. (b) Mean nearest neighbor trait distance and mean nearest neighbor phylogenetic distance; (c) Mean pairwise trait distance and mean pairwise phylogenetic distance. *** P < 0.001.
图5 单个功能性状β多样性标准效应与零值的比较。(a)平均最近邻体性状距离; (b)平均成对性状距离。NS, P > 0.05; ***, P < 0.001。
Fig. 5 Comparison of the standardized effect size for single functional trait β-diversity with zero value across the gobi deserts of northern Qinghai-Tibet Plateau. (a) Mean nearest neighbor trait distance; (b) Mean pairwise trait distance. LNC, Leaf nitrogen concentrations; LPC, Leaf phosphorus concentrations; SLA, Specific leaf area; LA, Leaf area; RNC, Fine root nitrogen concentrations; RPC, Fine root phosphorus concentrations; SRL, Specific root length; RL, Root length. NS, P > 0.05; ***, P < 0.001.
图6 青藏高原北部戈壁区环境差异与地理距离对植物群落物种、功能(平均最近邻体性状距离)和系统发育(平均最近邻体系统发育距离) β多样性观测值(a)及其标准效应(b)的解释
Fig. 6 The relative contribution of environmental and geographic distance in driving the vraiation in plant taxonomic, functional (mean nearest neighbor trait distance), and phylogenetic (mean nearest neighbor phylogenetic distance) β-diversity observed values (a) and their standardized effect sizes (b) across the gobi deserts of northern Qinghai-Tibet Plateau
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