Global pattern in terrestrial leaf litter decomposition: The effects of climate, litter chemistry, life form, growth form and mycorrhizal association

IF 5.6 1区 农林科学 Q1 AGRONOMY Agricultural and Forest Meteorology Pub Date : 2024-12-14 DOI:10.1016/j.agrformet.2024.110368
Xiaoxiang Zhao , Qiuxiang Tian , Anders Michelsen , Boshen Ren , Zhiyang Feng , Long Chen , Qinghu Jiang , Rudong Zhao , Feng Liu
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Abstract

Leaf litter decomposition plays an important role in nutrient and carbon cycling in terrestrial ecosystems. However, at a global scale, the effects of climate, initial litter chemistry, and different plant functional types on litter decomposition are not fully understood. Additionally, it remains unclear whether the effects of litter chemistry on leaf litter decomposition are consistent with responses observed at local scales. Here, 1585 observations of leaf litter decomposition encompassing 861 species from 298 field studies were synthesized to investigate the effects of climate, litter initial chemistry, and various plant groups on decomposition rates. The results demonstrate that at a global scale, leaf litter decomposition rates increased with mean annual temperature (MAT), mean annual precipitation (MAP), initial litter concentrations of nitrogen (N), phosphorus (P), and magnesium (Mg), but decreased with initial lignin concentrations. Moreover, except for initial leaf litter Mg concentrations, the influence of initial leaf litter chemistry characteristics on decomposition rates were consistent at global and local scales. In woody plants, leaf litters from deciduous, broadleaf, and arbuscular mycorrhizal (AM) species exhibited faster decomposition rates than from evergreen, coniferous, and ectomycorrhizal (ECM) species leaf litters, respectively. In herbaceous plants, the leaf litter of forbs had faster decomposition rates than graminoid and leguminous plants. For all plants, leaf litter decomposition is primarily controlled by MAP and MAT globally, while for woody and herbaceous plants, leaf litter decomposition is primarily controlled by initial leaf N and P concentrations, respectively. These results indicated that various functional groups of plants play a crucial role in understanding the decomposition of leaf litter. Moreover, when investigating the effect of leaf litter initial chemistry on its decomposition, it is almost unnecessary to consider effects at different scales.
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陆生凋落叶分解的全球格局:气候、凋落叶化学、生命形式、生长形式和菌根关联的影响
落叶分解在陆地生态系统的养分和碳循环中发挥着重要作用。然而,在全球范围内,气候、初始落叶化学和不同植物功能类型对落叶分解的影响尚未完全明了。此外,目前还不清楚落叶化学对落叶分解的影响是否与在局部尺度上观察到的反应一致。本文综合了298项野外研究中对861个物种的1585次枯落叶分解观测,研究了气候、枯落叶初始化学性质和不同植物群对枯落叶分解率的影响。结果表明,在全球范围内,枯落叶分解率随年平均气温(MAT)、年平均降水量(MAP)、枯落叶初始氮(N)、磷(P)和镁(Mg)浓度的增加而增加,但随初始木质素浓度的增加而减少。此外,除初始落叶层镁浓度外,在全球和地方尺度上,初始落叶层化学特征对分解率的影响是一致的。在木本植物中,落叶、阔叶和丛枝菌根(AM)物种叶屑的分解速率分别快于常绿、针叶和外生菌根(ECM)物种叶屑的分解速率。在草本植物中,牧草的落叶分解速度快于禾本科植物和豆科植物。对所有植物而言,叶屑的分解主要受全球 MAP 和 MAT 的控制,而对木本植物和草本植物而言,叶屑的分解分别主要受初始叶片 N 和 P 浓度的控制。这些结果表明,植物的不同功能群对了解落叶的分解起着至关重要的作用。此外,在研究落叶初始化学成分对落叶分解的影响时,几乎没有必要考虑不同尺度的影响。
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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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