Pub Date : 2025-12-12DOI: 10.1016/j.pedobi.2025.151109
Sékou F.M. Coulibaly , Juliette Chassain , Laure Vieublé-Gonod , Maxime Artru , Olivier De Carville , Swann Felin , Antoine Gardarin , Sophie Joimel
For several decades, techniques aimed at maximizing agricultural production have been developing rapidly. This has led to an intensification of cultural practices and concerns regarding the conservation of soil biodiversity and ecological functions and services it supports. A major challenge of agroecology is to define new methods for managing agroecosystems that enable a sustainable soil use and the preservation of its biodiversity. Sowing flower strips is often promoted in agri-environmental schemes, but their effect on soil biodiversity has yet been poorly considered. In this study, we followed the Collembola assemblages in response to the establishment of perennial wild flower strips within eight arable fields over four years (2018–2022). Collembola were sampled in the fields before the installation of the flower strips, in 2018 (y + 0), and in 2019 (y + 1), 2021 (y + 3) and 2022 (y + 4). Soil samples were taken within, at 5 m and at 30 m from the flower strips. Our results showed that there were no significant differences between the collembolan assemblages depending on the sampling distances from the flower strips. However, the age of the flower strips had an effect on Collembola assemblages, with y + 1 showing the lowest Collembola density and diversity. The differentiation between Collembola assemblages occurred three years after the flower strips sowing and was maintained for up to four years. Collembola appear to respond to environmental changes caused by flower strips sowing, since response traits such as sensory organs, pigmentation and sexual reproduction were the most dominant.
{"title":"Within-field flower strips effect on Collembola assemblages over time","authors":"Sékou F.M. Coulibaly , Juliette Chassain , Laure Vieublé-Gonod , Maxime Artru , Olivier De Carville , Swann Felin , Antoine Gardarin , Sophie Joimel","doi":"10.1016/j.pedobi.2025.151109","DOIUrl":"10.1016/j.pedobi.2025.151109","url":null,"abstract":"<div><div>For several decades, techniques aimed at maximizing agricultural production have been developing rapidly. This has led to an intensification of cultural practices and concerns regarding the conservation of soil biodiversity and ecological functions and services it supports. A major challenge of agroecology is to define new methods for managing agroecosystems that enable a sustainable soil use and the preservation of its biodiversity. Sowing flower strips is often promoted in agri-environmental schemes, but their effect on soil biodiversity has yet been poorly considered. In this study, we followed the Collembola assemblages in response to the establishment of perennial wild flower strips within eight arable fields over four years (2018–2022). Collembola were sampled in the fields before the installation of the flower strips, in 2018 (y + 0), and in 2019 (y + 1), 2021 (y + 3) and 2022 (y + 4). Soil samples were taken within, at 5 m and at 30 m from the flower strips. Our results showed that there were no significant differences between the collembolan assemblages depending on the sampling distances from the flower strips. However, the age of the flower strips had an effect on Collembola assemblages, with y + 1 showing the lowest Collembola density and diversity. The differentiation between Collembola assemblages occurred three years after the flower strips sowing and was maintained for up to four years. Collembola appear to respond to environmental changes caused by flower strips sowing, since response traits such as sensory organs, pigmentation and sexual reproduction were the most dominant.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"114 ","pages":"Article 151109"},"PeriodicalIF":2.2,"publicationDate":"2025-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145754153","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-12-01DOI: 10.1016/j.pedobi.2025.151099
Shijia Wang, Xia Peng, Jian Su, Lihua Tu
A clear understanding of microbial necromass carbon (MRC) accumulation mechanisms is essential for evaluating stable carbon budgets and informing effective strategies to enhance permanent carbon storage on a global forest scale. However, the complexity and heterogeneity inherent in forest systems have left the distribution of MRC at finer forest-type classification scales, and its driving factors still need to be solved. Thus, this study synthesized a dataset of 1220 data points from 88 peer-reviewed papers on global forests to investigate the distribution and mechanisms of MRC across diverse climate zones, forest types, elevation gradients, and soil depths. The analysis showed that temperate regions, with lower mean annual temperature and precipitation, had the highest MRC contents (21.88 g kg⁻¹), especially in mixed forests. MRC accumulation was further favored by low- to mid-elevations, Alfisols, and surface soil layers. Climate factors exerted both direct positive effects on MRC and indirect influences through microbial community structure and soil substrate properties. Overall, this global synthesis enhances our understanding of the environmental mechanisms governing MRC and its contribution to stable soil carbon storage in forests.
明确微生物坏死体碳(MRC)积累机制对于评估稳定的碳预算和提供有效的策略以提高全球森林规模的永久碳储量至关重要。然而,森林系统固有的复杂性和异质性使得MRC的分布在更精细的森林类型分类尺度上,其驱动因素仍有待解决。因此,本研究综合了来自88篇全球森林同行评议论文的1220个数据点数据集,探讨了不同气候带、森林类型、高程梯度和土壤深度的MRC分布及其机制。分析表明,年平均气温和降水量较低的温带地区,尤其是混交林,其MRC含量最高(21.88 g kg⁻¹)。中低海拔、土层和表层更有利于MRC的积累。气候因子通过微生物群落结构和土壤基质特性对土壤MRC既有直接的正向影响,也有间接的影响。总的来说,这一全球综合增强了我们对控制MRC的环境机制及其对森林土壤碳稳定储存的贡献的理解。
{"title":"Global synthesis reveals that climate and soil substrate shape microbial necromass carbon in forest soils","authors":"Shijia Wang, Xia Peng, Jian Su, Lihua Tu","doi":"10.1016/j.pedobi.2025.151099","DOIUrl":"10.1016/j.pedobi.2025.151099","url":null,"abstract":"<div><div>A clear understanding of microbial necromass carbon (MRC) accumulation mechanisms is essential for evaluating stable carbon budgets and informing effective strategies to enhance permanent carbon storage on a global forest scale. However, the complexity and heterogeneity inherent in forest systems have left the distribution of MRC at finer forest-type classification scales, and its driving factors still need to be solved. Thus, this study synthesized a dataset of 1220 data points from 88 peer-reviewed papers on global forests to investigate the distribution and mechanisms of MRC across diverse climate zones, forest types, elevation gradients, and soil depths. The analysis showed that temperate regions, with lower mean annual temperature and precipitation, had the highest MRC contents (21.88 g kg⁻¹), especially in mixed forests. MRC accumulation was further favored by low- to mid-elevations, Alfisols, and surface soil layers. Climate factors exerted both direct positive effects on MRC and indirect influences through microbial community structure and soil substrate properties. Overall, this global synthesis enhances our understanding of the environmental mechanisms governing MRC and its contribution to stable soil carbon storage in forests.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151099"},"PeriodicalIF":2.2,"publicationDate":"2025-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145623735","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-12-01DOI: 10.1016/j.pedobi.2025.151091
Dave Coleman, Zoë Lindo
{"title":"Putting the “Ped” into Pedobiologia –– A call to a new generation of soil ecologists","authors":"Dave Coleman, Zoë Lindo","doi":"10.1016/j.pedobi.2025.151091","DOIUrl":"10.1016/j.pedobi.2025.151091","url":null,"abstract":"","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151091"},"PeriodicalIF":2.2,"publicationDate":"2025-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145736185","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-12-01DOI: 10.1016/j.pedobi.2025.151100
Yudai Kitagami , Naoki Makita
Roots serve as essential linkages between aboveground and belowground communities and play a key role in maintaining multiple ecosystem functions. Soil communities consist of plant roots and their associated mycorrhizal fungi, microorganisms such as bacteria and fungi, and fauna across a wide range of sizes and trophic groups, all interconnected within complex food webs. However, our understanding of how tree root systems mediate the composition and diversity of soil biota remains limited. This study aimed to determine the effects of the root systems of four coniferous tree species and the soil properties they mediate on soil bacterial, fungal, and nematode communities. We collected soil and root samples from monocultural coniferous stands; Pinus densiflora (Pine), Larix kaempferi (Larch), Chamaecyparis obtusa (Cypress), and Cryptomeria japonica (Cedar) in temperate forests of Japan. Bacterial and fungal communities were assessed using MiSeq high-throughput sequencing system, while nematodes were morphologically identified at the genus/family level and examined for both community structure and trophic composition. Our results showed that fungal and nematode abundances were significantly or marginally higher in pine soils, respectively. There were no significant differences in the abundance of bacteria among the four tree species. Fungal richness was significantly higher in cypress stands, while nematode richness was greater in cedar stands. Fungal richness was strongly influenced by root traits, whereas nematode richness was primarily explained by soil properties. There were no significant differences in the richness of bacteria among four tree species. Community structures of bacterial, fungal, and nematode varied significantly among the four tree species. Moreover, soil properties significantly influenced the community structures of all three-soil biota, whereas root-traits did not influence the community structures. These findings suggest that unique soil biological communities are shaped by the soil environment those root systems modify.
{"title":"Determinants of rhizosphere community structure: The role of root traits and soil properties in coniferous plantations","authors":"Yudai Kitagami , Naoki Makita","doi":"10.1016/j.pedobi.2025.151100","DOIUrl":"10.1016/j.pedobi.2025.151100","url":null,"abstract":"<div><div>Roots serve as essential linkages between aboveground and belowground communities and play a key role in maintaining multiple ecosystem functions. Soil communities consist of plant roots and their associated mycorrhizal fungi, microorganisms such as bacteria and fungi, and fauna across a wide range of sizes and trophic groups, all interconnected within complex food webs. However, our understanding of how tree root systems mediate the composition and diversity of soil biota remains limited. This study aimed to determine the effects of the root systems of four coniferous tree species and the soil properties they mediate on soil bacterial, fungal, and nematode communities. We collected soil and root samples from monocultural coniferous stands; <em>Pinus densiflora</em> (Pine), <em>Larix kaempferi</em> (Larch), <em>Chamaecyparis obtusa</em> (Cypress), and <em>Cryptomeria japonica</em> (Cedar) in temperate forests of Japan. Bacterial and fungal communities were assessed using MiSeq high-throughput sequencing system, while nematodes were morphologically identified at the genus/family level and examined for both community structure and trophic composition. Our results showed that fungal and nematode abundances were significantly or marginally higher in pine soils, respectively. There were no significant differences in the abundance of bacteria among the four tree species. Fungal richness was significantly higher in cypress stands, while nematode richness was greater in cedar stands. Fungal richness was strongly influenced by root traits, whereas nematode richness was primarily explained by soil properties. There were no significant differences in the richness of bacteria among four tree species. Community structures of bacterial, fungal, and nematode varied significantly among the four tree species. Moreover, soil properties significantly influenced the community structures of all three-soil biota, whereas root-traits did not influence the community structures. These findings suggest that unique soil biological communities are shaped by the soil environment those root systems modify.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151100"},"PeriodicalIF":2.2,"publicationDate":"2025-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145693892","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-12-01DOI: 10.1016/j.pedobi.2025.151101
Pengyi Hou , Cui Deng , Maokui Lyu , Yongmeng Jiang , Yuming Lu , Jinsheng Xie
Global warming may cause widespread soil carbon loss across multiple regions. Subtropical montane ecosystems store substantial soil organic carbon (SOC). However, the impacts of global warming on SOC pools with varying stability levels remain unclear. We simulated warming using an altitudinal translocation approach in Wuyishan Mountain, subtropical China. Specifically, soil columns were moved downslope from 1400 m (coniferous forest) to 1000 m (mixed forest), from 1000 m to 600 m (evergreen broadleaf forest), and from 600 m to 200 m (again, evergreen broadleaf forest). We investigated warming-induced changes in labile carbon, recalcitrant carbon, and total carbon pool in soils, along with the underlying mechanisms. Results showed temperature increases (1.45–2.11°C) following downward translocation of soil cores. Warming reduced labile carbon across all elevations but decreased recalcitrant carbon only at higher elevations, with no net change in total carbon stocks. Mantel tests revealed stronger linkages between temperature, enzyme, and microbial communities at higher elevations. Structural equation modeling revealed that warming-induced changes in labile carbon, mediated by edaphic factors, directly influenced recalcitrant carbon. This cascaded effect reflects the integrated biotic-abiotic interactions driven by environmental change. Our findings identify high-elevation montane forests as critical hotspots of soil carbon vulnerability under warming, where disproportionate losses in mineral-associated carbon occur via thermal disruption of Fe-organic complexes. Protecting these elevational refugia requires urgent prioritization in climate-smart strategies. Specific management should target iron redox cycling, fungal functional traits, and oxidative enzyme activities to stabilize mineral-associated organic carbon.
{"title":"Elevation-dependent vulnerability of soil carbon pools to warming in a subtropical forest: Insights from a translocation experiment","authors":"Pengyi Hou , Cui Deng , Maokui Lyu , Yongmeng Jiang , Yuming Lu , Jinsheng Xie","doi":"10.1016/j.pedobi.2025.151101","DOIUrl":"10.1016/j.pedobi.2025.151101","url":null,"abstract":"<div><div>Global warming may cause widespread soil carbon loss across multiple regions. Subtropical montane ecosystems store substantial soil organic carbon (SOC). However, the impacts of global warming on SOC pools with varying stability levels remain unclear. We simulated warming using an altitudinal translocation approach in Wuyishan Mountain, subtropical China. Specifically, soil columns were moved downslope from 1400 m (coniferous forest) to 1000 m (mixed forest), from 1000 m to 600 m (evergreen broadleaf forest), and from 600 m to 200 m (again, evergreen broadleaf forest). We investigated warming-induced changes in labile carbon, recalcitrant carbon, and total carbon pool in soils, along with the underlying mechanisms. Results showed temperature increases (1.45–2.11°C) following downward translocation of soil cores. Warming reduced labile carbon across all elevations but decreased recalcitrant carbon only at higher elevations, with no net change in total carbon stocks. Mantel tests revealed stronger linkages between temperature, enzyme, and microbial communities at higher elevations. Structural equation modeling revealed that warming-induced changes in labile carbon, mediated by edaphic factors, directly influenced recalcitrant carbon. This cascaded effect reflects the integrated biotic-abiotic interactions driven by environmental change. Our findings identify high-elevation montane forests as critical hotspots of soil carbon vulnerability under warming, where disproportionate losses in mineral-associated carbon occur via thermal disruption of Fe-organic complexes. Protecting these elevational refugia requires urgent prioritization in climate-smart strategies. Specific management should target iron redox cycling, fungal functional traits, and oxidative enzyme activities to stabilize mineral-associated organic carbon.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151101"},"PeriodicalIF":2.2,"publicationDate":"2025-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145693893","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-14DOI: 10.1016/j.pedobi.2025.151098
Hayden W. Bock, Suzanne M. Fleishman
Subsoils are often considered biologically inactive, yet the persistence of root channels in these habitats may significantly alter the distribution and diversity of soil organisms long after plant death. We investigated soil microarthropod communities in a former apple orchard in the northeastern United States approximately 13 years after tree removal, where we compared microarthropods in deep root channels (60–90 cm depth) with adjacent root-free bulk subsoil and surface soils. As anticipated, surface soils had the greatest abundance, richness, and diversity of soil microarthropods. Notably, however, deep root channels maintained distinctly richer and more diverse communities than surrounding bulk subsoil. Community analysis revealed that root channel fauna assemblages were compositionally distinct. The differences in beta diversity were due to a unique assemblage of species, rather than overlapping with the surface or bulk subsoil communities. These findings highlight root channels as long-lived microhabitats in deep soils, where detritosphere communities persist and provide resources and habitat to diverse soil organisms. By sustaining soil microarthropod diversity and providing refugia, root channels represent overlooked keystone structures in soil with potential for accelerating biological recovery and enhancing soil functionality in degraded or post-agricultural systems.
{"title":"Apple root channels continue to shape subsoil microarthropod communities more than a decade after orchard removal","authors":"Hayden W. Bock, Suzanne M. Fleishman","doi":"10.1016/j.pedobi.2025.151098","DOIUrl":"10.1016/j.pedobi.2025.151098","url":null,"abstract":"<div><div>Subsoils are often considered biologically inactive, yet the persistence of root channels in these habitats may significantly alter the distribution and diversity of soil organisms long after plant death. We investigated soil microarthropod communities in a former apple orchard in the northeastern United States approximately 13 years after tree removal, where we compared microarthropods in deep root channels (60–90 cm depth) with adjacent root-free bulk subsoil and surface soils. As anticipated, surface soils had the greatest abundance, richness, and diversity of soil microarthropods. Notably, however, deep root channels maintained distinctly richer and more diverse communities than surrounding bulk subsoil. Community analysis revealed that root channel fauna assemblages were compositionally distinct. The differences in beta diversity were due to a unique assemblage of species, rather than overlapping with the surface or bulk subsoil communities. These findings highlight root channels as long-lived microhabitats in deep soils, where detritosphere communities persist and provide resources and habitat to diverse soil organisms. By sustaining soil microarthropod diversity and providing refugia, root channels represent overlooked keystone structures in soil with potential for accelerating biological recovery and enhancing soil functionality in degraded or post-agricultural systems.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151098"},"PeriodicalIF":2.2,"publicationDate":"2025-11-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578723","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-12DOI: 10.1016/j.pedobi.2025.151096
Juliette Chassain , John S. Terblanche , Charlene Janion-Scheepers
Sugarcane cultivation covers large areas in southern Africa, where it provides local employment and a substantial part of farming incomes. Maintaining soil quality in these areas is essential to prevent environmental damage following long-term cultivation. Soil biodiversity constitutes a good proxy to monitor soil quality. However, soil organisms and their interactions remain poorly studied in southern Africa. Soil food web studies contribute to the understanding of these complex belowground interactions. This study is the first to investigate soil food webs in sugarcane cultivation areas in Africa. We sampled 10 sugarcane fields subjected to different cropping (conventional versus regenerative) and harvesting (burning versus green cane) practices, and an unmanaged site included as a reference. Stable isotope analyses were conducted on sugarcane leaves, roots and crop residues, soil, and on the most abundant arthropod taxa including Araneae (spiders), Blattodea (cockroaches), Collembola (springtails), Dermaptera (earwigs), Diplopoda (millipedes), Formicidae (ants; Pheidole and Tetramorium genera), Hemiptera (leafhoppers) and Oribatida (oribatid mites). Food webs and trophic niches of arthropod taxa were characterized by assessing C and N stable isotope ratios (δ13C and δ15N) and by computing isotopic metrics. Higher δ15N values were observed for Araneae, Formicidae and Dermaptera, intermediate values for Oribatida and Collembola followed by Diplopoda and Blattodea, and lower values for Hemiptera. Food chain length was significantly shorter in fields with regenerative than conventional practices, and longer with green harvest than with pre-harvest burning or in the unmanaged site. Isotopic uniqueness and evenness were lower in green-harvested than in burnt fields. Our results highlight the trophic functional diversity of decomposers (Blattodea, Diplopoda, Collembola) and soil predators (Araneae, Dermaptera, Formicidae) in sugarcane fields, and the effects of agricultural practices on these food webs. Overall, this study contributes to further our knowledge on the composition and factors influencing soil biodiversity that remains understudied in Africa.
{"title":"Soil food webs in sugarcane fields: Sweet dreams for soil organisms in subtropical Africa","authors":"Juliette Chassain , John S. Terblanche , Charlene Janion-Scheepers","doi":"10.1016/j.pedobi.2025.151096","DOIUrl":"10.1016/j.pedobi.2025.151096","url":null,"abstract":"<div><div>Sugarcane cultivation covers large areas in southern Africa, where it provides local employment and a substantial part of farming incomes. Maintaining soil quality in these areas is essential to prevent environmental damage following long-term cultivation. Soil biodiversity constitutes a good proxy to monitor soil quality. However, soil organisms and their interactions remain poorly studied in southern Africa. Soil food web studies contribute to the understanding of these complex belowground interactions. This study is the first to investigate soil food webs in sugarcane cultivation areas in Africa. We sampled 10 sugarcane fields subjected to different cropping (conventional <em>versus</em> regenerative) and harvesting (burning <em>versus</em> green cane) practices, and an unmanaged site included as a reference. Stable isotope analyses were conducted on sugarcane leaves, roots and crop residues, soil, and on the most abundant arthropod taxa including Araneae (spiders), Blattodea (cockroaches), Collembola (springtails), Dermaptera (earwigs), Diplopoda (millipedes), Formicidae (ants; <em>Pheidole</em> and <em>Tetramorium</em> genera), Hemiptera (leafhoppers) and Oribatida (oribatid mites). Food webs and trophic niches of arthropod taxa were characterized by assessing C and N stable isotope ratios (δ<sup>13</sup>C and δ<sup>15</sup>N) and by computing isotopic metrics. Higher δ<sup>15</sup>N values were observed for Araneae, Formicidae and Dermaptera, intermediate values for Oribatida and Collembola followed by Diplopoda and Blattodea, and lower values for Hemiptera. Food chain length was significantly shorter in fields with regenerative than conventional practices, and longer with green harvest than with pre-harvest burning or in the unmanaged site. Isotopic uniqueness and evenness were lower in green-harvested than in burnt fields. Our results highlight the trophic functional diversity of decomposers (Blattodea, Diplopoda, Collembola) and soil predators (Araneae, Dermaptera, Formicidae) in sugarcane fields, and the effects of agricultural practices on these food webs. Overall, this study contributes to further our knowledge on the composition and factors influencing soil biodiversity that remains understudied in Africa.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151096"},"PeriodicalIF":2.2,"publicationDate":"2025-11-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578721","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-10DOI: 10.1016/j.pedobi.2025.151095
Dennis Castillo-Figueroa , Camilo Castillo-Avila , Miguel Angel Jaramillo
Centipedes are among the top predators regulating soil food webs in terrestrial ecosystems. Yet, they remain one of the least studied groups of soil fauna, particularly regarding their ecology and natural history. This gap is especially pronounced in upper Andean tropical forests (UATF), where few surveys have been conducted despite extensive habitat transformation. In this study, we investigated changes in centipede communities along a successional gradient in UATF and identified the ecological factors associated with changes in their abundance. We collected 168 soil samples across four UATF sites along a successional gradient in Colombia, covering all climatic seasons in 2022. Differences in species composition between sites were analyzed using ANOSIM, NMDS, and SIMPER. We also measured forest structure (litter depth, slope, canopy openness, leaf area index), microclimatic conditions (temperature, moisture), and prey availability (abundance, richness) to examine their relationships with centipede abundance through simple and multiple regressions. A total of 291 individuals from eight species were recorded, with each forest site showing a distinct community. Centipede abundance followed a hump-shaped pattern along succession, with one species indicative of secondary forests and another characteristic of mature forests. Temperature fluctuation and prey availability were the main factors associated with total centipede abundance. However, the two centipede orders responded differently: Scolopendromorpha were primarily associated with maximum temperature, while Geophilomorpha were linked to a combination of prey availability, temperature fluctuation, and slope. Our findings provide novel insights into centipede ecology in tropical montane forests, highlighting the role of environmental gradients in shaping predator communities.
{"title":"Unveiling the hidden soil predators of the Andes: Contrasting centipede responses to ecological factors along a successional gradient in tropical montane forests","authors":"Dennis Castillo-Figueroa , Camilo Castillo-Avila , Miguel Angel Jaramillo","doi":"10.1016/j.pedobi.2025.151095","DOIUrl":"10.1016/j.pedobi.2025.151095","url":null,"abstract":"<div><div>Centipedes are among the top predators regulating soil food webs in terrestrial ecosystems. Yet, they remain one of the least studied groups of soil fauna, particularly regarding their ecology and natural history. This gap is especially pronounced in upper Andean tropical forests (UATF), where few surveys have been conducted despite extensive habitat transformation. In this study, we investigated changes in centipede communities along a successional gradient in UATF and identified the ecological factors associated with changes in their abundance. We collected 168 soil samples across four UATF sites along a successional gradient in Colombia, covering all climatic seasons in 2022. Differences in species composition between sites were analyzed using ANOSIM, NMDS, and SIMPER. We also measured forest structure (litter depth, slope, canopy openness, leaf area index), microclimatic conditions (temperature, moisture), and prey availability (abundance, richness) to examine their relationships with centipede abundance through simple and multiple regressions. A total of 291 individuals from eight species were recorded, with each forest site showing a distinct community. Centipede abundance followed a hump-shaped pattern along succession, with one species indicative of secondary forests and another characteristic of mature forests. Temperature fluctuation and prey availability were the main factors associated with total centipede abundance. However, the two centipede orders responded differently: Scolopendromorpha were primarily associated with maximum temperature, while Geophilomorpha were linked to a combination of prey availability, temperature fluctuation, and slope. Our findings provide novel insights into centipede ecology in tropical montane forests, highlighting the role of environmental gradients in shaping predator communities.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151095"},"PeriodicalIF":2.2,"publicationDate":"2025-11-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578722","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-10-16DOI: 10.1016/j.pedobi.2025.151094
Yanbo An , Xiaotong Ji , Jiahui Zhang , Qifeng Wu , Wenhao Jin , Jiajia Xing , Hua Qin
Trichoderma guizhouense is recognized as an effective antagonistic fungus against Ralstonia solanacearum, the causative agent of tomato bacterial wilt. However, how T. guizhouense-enriched organic fertilizer affects the survival of R. solanacearum and bacterial community in tomato rhizosphere soil is still poorly understood. To address this, a pot experiment was conducted to assess changes in the abundance of the fliC gene (a marker for R. solanacearum) and to investigate shifts in the rhizosphere bacterial community after T. guizhouense-enriched organic fertilizer application using quantitative PCR and high-throughput sequencing, respectively. The results showed that T. guizhouense-enriched organic fertilizer application significantly reduced the abundance of fliC gene in tomato rhizosphere soil after 15 days of R. solanacearum inoculation, and notably decreased the disease index of tomato wilt after 13 days of R. solanacearum inoculation (P < 0.05). Compared to common organic fertilizer application alone, T. guizhouense-enriched organic fertilizer application significantly increased the Shannon index of soil bacterial community and enhanced the relative abundance of beneficial bacterial genera, including Caulobacter, Chitinophaga and Bacillus. Both T. guizhouense-enriched organic fertilizer application and R. solanacearum inoculation significantly altered soil bacterial community composition. Moreover, the bacterial co-occurrence network exhibited greater complexity and cohesiveness in the T. guizhouense-enriched organic fertilizer application treatment, which could contribute to maintaining the stability of rhizospheric bacterial community of R. solanacearum-infected tomato. The findings suggested that T. guizhouense-enriched organic fertilizer would significantly suppress bacterial wilt and changed the bacterial community structure of the soil.
{"title":"Trichoderma guizhouense enhances tomato (Solanum lycopersicum) Ralstonia wilt suppression by organic fertilizer, focusing on rhizosphere soil bacterial community","authors":"Yanbo An , Xiaotong Ji , Jiahui Zhang , Qifeng Wu , Wenhao Jin , Jiajia Xing , Hua Qin","doi":"10.1016/j.pedobi.2025.151094","DOIUrl":"10.1016/j.pedobi.2025.151094","url":null,"abstract":"<div><div><em>Trichoderma guizhouense</em> is recognized as an effective antagonistic fungus against <em>Ralstonia solanacearum</em>, the causative agent of tomato bacterial wilt<em>.</em> However, how <em>T. guizhouense</em>-enriched organic fertilizer affects the survival of <em>R. solanacearum</em> and bacterial community in tomato rhizosphere soil is still poorly understood. To address this, a pot experiment was conducted to assess changes in the abundance of the <em>fliC</em> gene (a marker for <em>R. solanacearum</em>) and to investigate shifts in the rhizosphere bacterial community after <em>T. guizhouense-</em>enriched organic fertilizer application using quantitative PCR and high-throughput sequencing, respectively. The results showed that <em>T. guizhouense-</em>enriched organic fertilizer application significantly reduced the abundance of <em>fliC</em> gene in tomato rhizosphere soil after 15 days of <em>R. solanacearum</em> inoculation, and notably decreased the disease index of tomato wilt after 13 days of <em>R. solanacearum</em> inoculation (<em>P</em> < 0.05). Compared to common organic fertilizer application alone, <em>T. guizhouense-</em>enriched organic fertilizer application significantly increased the Shannon index of soil bacterial community and enhanced the relative abundance of beneficial bacterial genera, including <em>Caulobacter, Chitinophaga</em> and <em>Bacillus</em>. Both <em>T. guizhouense-</em>enriched organic fertilizer application and <em>R. solanacearum</em> inoculation significantly altered soil bacterial community composition. Moreover, the bacterial co-occurrence network exhibited greater complexity and cohesiveness in the <em>T. guizhouense-</em>enriched organic fertilizer application treatment, which could contribute to maintaining the stability of rhizospheric bacterial community of <em>R. solanacearum</em>-infected tomato. The findings suggested that <em>T. guizhouense</em>-enriched organic fertilizer would significantly suppress bacterial wilt and changed the bacterial community structure of the soil.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151094"},"PeriodicalIF":2.2,"publicationDate":"2025-10-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145325599","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-10-14DOI: 10.1016/j.pedobi.2025.151093
Angela Lafuente , Louis J. Lamit , Rodney A. Chimner , John Hribljan , Nathan Basiliko , Juan C. Benavides , Erik A. Lilleskov
The balance between methane producing and methane consuming microorganisms is partially responsible for the magnitude and direction of soil-atmosphere methane fluxes. Therefore, understanding the effects of vegetation and land use on relative abundance, community structure and vertical distribution of methane cycling microorganisms should help us interpret patterns of net emissions of methane. Mountain peatlands in the tropics are abundant and are important in global carbon cycling, but little is known about the communities of methane-cycling microorganisms in these ecosystems. We sampled peat from eight Andean peatlands in Peru, Ecuador and Colombia and described the dominant vegetation, grazing intensity and other site characteristics at each site. We characterised the microbial community of each peat sample at different depths and identified the methane cycling microorganisms. We observed a higher proportion of methanogens and methanogen:methanotroph in the shallow peat of grazed sites than ungrazed sites. At ungrazed sites we found relatively high methanotroph abundance relative to methanogens, even at the deepest sampling depths, suggesting plant aerenchymal oxygen transport structures communities at depth. We found changes in the methane cycling microbial communities among sites and with depth, e.g., in the superficial peat the hydrogenotrophic methanogens were more abundant but at depth there was more metabolic diversity. Our study provides new insights into the community structure of methane cycling microorganism of the tropical mountain peatlands, and raises interesting questions regarding the drivers of methanotroph abundance deeper in peat.
{"title":"Variability in depth-mediated shifts in methanogen and methanotroph communities across tropical Andean mountain peatlands","authors":"Angela Lafuente , Louis J. Lamit , Rodney A. Chimner , John Hribljan , Nathan Basiliko , Juan C. Benavides , Erik A. Lilleskov","doi":"10.1016/j.pedobi.2025.151093","DOIUrl":"10.1016/j.pedobi.2025.151093","url":null,"abstract":"<div><div>The balance between methane producing and methane consuming microorganisms is partially responsible for the magnitude and direction of soil-atmosphere methane fluxes. Therefore, understanding the effects of vegetation and land use on relative abundance, community structure and vertical distribution of methane cycling microorganisms should help us interpret patterns of net emissions of methane. Mountain peatlands in the tropics are abundant and are important in global carbon cycling, but little is known about the communities of methane-cycling microorganisms in these ecosystems. We sampled peat from eight Andean peatlands in Peru, Ecuador and Colombia and described the dominant vegetation, grazing intensity and other site characteristics at each site. We characterised the microbial community of each peat sample at different depths and identified the methane cycling microorganisms. We observed a higher proportion of methanogens and methanogen:methanotroph in the shallow peat of grazed sites than ungrazed sites. At ungrazed sites we found relatively high methanotroph abundance relative to methanogens, even at the deepest sampling depths, suggesting plant aerenchymal oxygen transport structures communities at depth. We found changes in the methane cycling microbial communities among sites and with depth, e.g., in the superficial peat the hydrogenotrophic methanogens were more abundant but at depth there was more metabolic diversity. Our study provides new insights into the community structure of methane cycling microorganism of the tropical mountain peatlands, and raises interesting questions regarding the drivers of methanotroph abundance deeper in peat.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"113 ","pages":"Article 151093"},"PeriodicalIF":2.2,"publicationDate":"2025-10-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145363962","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}