Soil indicators of plant diversity for global ecoregions: Implications for management practices

被引:12
作者
Wan, Ji-Zhong [1 ,2 ]
Li, Qiang-Feng [2 ]
Li, Ning [2 ]
Si, Jian-Hua [2 ]
Zhang, Zhi-Xiang [3 ]
Wang, Chun-Jing [1 ,2 ]
Li, Xi-Lai [2 ]
Li, Zong-Ren [2 ]
机构
[1] Qinghai Univ, State Key Lab Plateau Ecol & Agr, Xining 810016, Qinghai, Peoples R China
[2] Qinghai Univ, Coll Agr & Anim Husb, Xining 810016, Qinghai, Peoples R China
[3] Beijing Forestry Univ, Sch Nat Conservat, Beijing 100083, Peoples R China
基金
对外科技合作项目(国际科技项目);
关键词
Conservation management; Ecoregional plant richness; Soil variable; Vulnerability assessment; Worldwide; ANTHROPOGENIC CLIMATE-CHANGE; ENVIRONMENTAL HETEROGENEITY; SPECIES-DIVERSITY; FUNCTIONAL DIVERSITY; ECOSYSTEM PROCESSES; ORGANIC-CARBON; SPATIAL SCALES; COMMUNITIES; VULNERABILITY; DETERMINANTS;
D O I
10.1016/j.gecco.2018.e00404
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Environmental indicators have been developed widely to promote biodiversity conservation, ecological restoration, and nature resource management from local to global scales. Ecoregions are effective tools for global conservation of plant diversity, and soil conditions can affect the plant diversity within ecoregions. Hence, soil indicators of plant diversity have substantial potential as tools for effectively understanding global ecoregions. Here, we used plant diversity data from 361 ecoregions and seven soil variables in a regression analysis to explore the relationships between soil and ecoregional plant diversity (EPD). We found that soil means and heterogeneity were significantly related to EPD. EPD decreased curvilinearly as both mean cation exchange capacity and mean soil pH increased, while mean soil organic carbon stock was negatively related to EPD (P < 0.05). EPD increased curvilinearly with mean soil texture clay fraction and mean soil texture silt fraction (P < 0.05). Heterogeneity of bulk density, cation exchange capacity, and soil pH had positive relationships with EPD (P<0.05). EPD had a negative, unimodal response to soil organic carbon stock heterogeneity, with an opposite trend in heterogeneity of soil texture clay fraction (P< 0.05). Furthermore, such relationships may depend on the vulnerability of ecoregions of interest. Specially, means of soil texture clay fraction and heterogeneity of bulk density were useful indicators of EPD for relatively stable or intact and vulnerable ecoregions (P <0.05), and mean cation exchange capacity and heterogeneity of soil organic carbon stock were useful indicators of EPD in critical or endangered ecoregions (P < 0.05). Hence, monitoring soil conditions should be conducted for plant diversity at broad scales, and conservation efforts should focus on soil diversity, with a particular emphasis on relatively stable or intact ecoregions worldwide. (C) 2018 The Authors. Published by Elsevier B.V.
引用
收藏
页数:9
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