干旱
生态系统
环境科学
生态学
非生物成分
固碳
土壤碳
气候变化
碳循环
农林复合经营
全球变化
森林生态学
全球变暖
碳纤维
生物多样性
小气候
促进
多样性指数
总有机碳
物种多样性
干旱指数
树(集合论)
植物多样性
土壤有机质
木本植物
自然(考古学)
作者
Haoru Yan,X H Liu,Bernhard Schmid,Yi Li,Kristina J. Anderson‐Teixeira,Sabine Both,Norman A. Bourg,David F. R. P. Burslem,Chengjin Chu,Keith Clay,Hu Du,Nathaly R. Guerrero‐Ramírez,Hua Huang,Daniel J. Johnson,Guangze Jin,Luxiang Lin,Feng Liu,Yankun Liu,William J. McShea,Xiangcheng Mi
摘要
Soil organic carbon (SOC) plays an essential role in carbon sequestration and climate change mitigation in forest ecosystems. While experimental studies have shown that plant diversity usually increases SOC, it remains unclear whether this positive relationship holds in natural ecosystems across varying climatic conditions. Using a global dataset of 15 large and long-term monitored natural forest sites spanning a wide latitudinal range, we assess the relationship between tree diversity and SOC within and across sites in temperate, subtropical, and tropical regions. We found an overall positive relationship between tree taxonomic diversity and SOC. The relationships between tree taxonomic or functional diversity and SOC became stronger under colder and more arid conditions. Additionally, tree functional composition was linked to SOC only within a subset of sites in more arid climates. These findings suggest that warmer and more humid conditions increase decomposition, offsetting diversity-driven carbon inputs, while colder and more arid conditions enhance SOC through low decomposition and increased inputs through abiotic facilitation and biotic interactions in high-diversity communities. Our findings indicate that conserving plant diversity is critical for enhancing carbon sequestration and mitigating the effects of climatic conditions, particularly in cold climates and regions facing an increase in arid conditions.
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