Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, China.
AMAP, Univ Montpellier, CIRAD, CNRS, INRAE, IRD, Montpellier, 34000, France.
BMC Res Notes. 2023 Nov 8;16(1):321. doi: 10.1186/s13104-023-06601-x.
Soil fauna plays a crucial role in contributing to litter breakdown, accelerating the decomposition rate and enhancing the biogeochemical cycle in terrestrial ecosystems. Comprehending the specific fauna role of functional species in litter decomposition is challenging due to their vast numbers and diversity. Climate and litter quality are widely acknowledged as dominant drives of litter decomposition across large spatial scales. However, the pattern of climate and litter quality modulates the effect of soil fauna on litter decomposition remains largely unexplored. To address this gap, we conducted an extensive analysis using data from 81 studies to investigate how climate and litter traits affects soil fauna in the decomposition.
The paper describes fauna body size, climate zones (tropical, subtropical and temperate), ecosystem types (forest, grassland, wetland and farmland), soil types (sand, loam and clay), decomposed duration (< 180, 180-360, > 360 days), litter initial traits, average annual temperature and precipitation. The litter traits encompass various parameters such as concentrations of carbon, nitrogen, phosphorus, potassium, lignin, cellulose, total phenol, condensed tannin, hydrolysable tannin and other nutrient traits. These comprehensive datasets provide valuable insights into the role of soil fauna on the decomposition at global scale. Furthermore, the data will give researchers keys to assess how climate, litter quality and soil fauna interact to determine decomposition rates.
土壤动物在促进凋落物分解、加速分解速率和增强陆地生态系统生物地球化学循环方面发挥着至关重要的作用。由于其数量庞大且多样,理解功能物种在凋落物分解中特定的动物区系作用具有挑战性。气候和凋落物质量被广泛认为是影响大空间尺度上凋落物分解的主要驱动因素。然而,气候和凋落物质量模式调节土壤动物对凋落物分解的影响在很大程度上仍未得到探索。为了解决这一差距,我们利用来自 81 项研究的数据进行了广泛的分析,以调查气候和凋落物特征如何影响分解中的土壤动物。
本文描述了动物体型、气候带(热带、亚热带和温带)、生态系统类型(森林、草原、湿地和农田)、土壤类型(沙、壤土和粘土)、分解持续时间(<180、180-360、>360 天)、凋落物初始特征、年平均温度和降水。凋落物特征包括碳、氮、磷、钾、木质素、纤维素、总酚、缩合单宁、水解单宁和其他养分特征的浓度等各种参数。这些综合数据集提供了对全球范围内土壤动物在分解中的作用的宝贵见解。此外,这些数据将为研究人员提供评估气候、凋落物质量和土壤动物如何相互作用以确定分解速率的关键。