与蚯蚓生物量模式匹配的世界湿润林地生态系统的实用分类

IF 4.8 2区 农林科学 Q1 SOIL SCIENCE
Jiro Tsukamoto
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引用次数: 0

摘要

在气候变化的世界中,迫切需要预测全球碳动态的变化。蚯蚓是最强大的生态系统工程师,在调节土壤过程中起着主导作用,包括碳固存和分解。描述蚯蚓生物量的区域和全球格局对预测全球碳动态变化至关重要。最近对土壤大型动物指标(生物量、丰度和多样性)的荟萃分析试图通过使用不同生态系统分类的不同模型来确定蚯蚓生物量的全球格局。观测到的或预测的模式是不一致的,因此不利于其实际使用应用,例如全球碳模型和可持续森林管理规划。生态系统分类的标准化有望减少这些不一致性。本研究旨在提供湿润林地生态系统的最佳分类,该分类将比以前的分类更符合蚯蚓生物量的模式。为此,将已发表的湿润林地生态系统蚯蚓生物量数据重新合成为一个默认的类别系统,考虑树木功能群分类和蚯蚓生态学,以及常规的气候和森林类型分类。根据蚯蚓生物量在类别间变化的显著性来评价默认分类的总体有效性,然后进行改进,以便更好地反映成对类别之间差异的显著性/不显著性。形成了寒带/冷温带针叶林/山毛榉/栎树和白杨落叶、暖温带落叶阔叶和常绿阔叶、热带未受干扰和人工林/受干扰次生林3个气候× 2植被类型。在各气候类型中,前者植被类型蚯蚓生物量显著低于后者。这种分类揭示了在全球温度梯度上,凋落物类型(顽固性与不稳定性)与蚯蚓生物量之间的关系是反转的;也就是说,在寒带/冷温带森林中,较高的生物量与不稳定凋落物有关,而在暖温带森林中,较高的生物量与顽固凋落物有关。对这种逆转的一种可能解释是,不稳定凋落物通过与低温地区微生物的协同作用促进蚯蚓生长,但通过与高温地区微生物的竞争阻碍蚯蚓生长。提出了世界湿润林地生态系统中蚯蚓生物量的双重模式,即顽固性产凋落物林系列和不稳定产凋落物林系列,为全球碳模型和可持续森林管理规划提供了新的基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Pragmatic categorization of moist woodland ecosystems of the world matching the pattern of earthworm biomass
Predicting changes in global carbon dynamics is urgently required in a climatically changing world. Earthworms, the most powerful ecosystem engineers, play a dominant role in the regulation of soil processes, including carbon sequestration and decomposition. Delineating the regional and global patterns of earthworm biomass is vital to predicting changes in global carbon dynamics. Recent meta-analyses of soil macrofaunal metrics (biomass, abundance, and diversity) attempted to determine the global patterns of earthworm biomass by applying different models using different ecosystem categorizations. The observed or predicted patterns were inconsistent, and therefore inconvenient in regard to their practical use application, such as global carbon modelling and sustainable forest management planning. The standardization of ecosystem categorization is expected to lessen these inconsistencies. This study has aimed to provide an optimal categorization of moist woodland ecosystems that would better match the patterns of earthworm biomass than previous categorizations. To this end, published data on earthworm biomass in moist woodland ecosystems were resynthesized into a default category system, considering tree functional group classification and earthworm ecology as well as conventional climate and forest type classifications. The overall effectiveness of the default categorization was evaluated based on the significance of the variations in earthworm biomass among the categories and then improved in order to better reflect the significance/insignificance of the differences between paired categories. This resulted in the following three climate × two vegetation categories: boreal/cool temperate conifer/beech/oak and mull forming deciduous, warm temperate deciduous broadleaf and evergreen broadleaf, and tropical undisturbed and tree plantation/disturbed secondary. The former vegetation category within each climate category exhibited significantly lower earthworm biomass than the latter. This categorization revealed a reversal in the relationship between litter type (recalcitrant versus labile) and earthworm biomass along the global temperature gradient; that is, higher biomass was found to be associated with labile litter in boreal/cool temperate forests, versus higher biomass with recalcitrant litter in warm temperate forests. A possible explanation for this reversal is that labile litter promotes earthworms through synergistic interactions with microbes in the regions at lower temperatures, but impedes them through competitions with microbes in the regions at higher temperatures. A dual pattern of earthworm biomass in moist woodland ecosystems of the world consisting of recalcitrant litter producing forest series and labile litter-producing forest series was proposed as a novel basis for global carbon modelling and also sustainable forest management planning.
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来源期刊
Applied Soil Ecology
Applied Soil Ecology 农林科学-土壤科学
CiteScore
9.70
自引率
4.20%
发文量
363
审稿时长
5.3 months
期刊介绍: Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.
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