Soil Biology & Biochemistry

Papers
(The median citation count of Soil Biology & Biochemistry is 10. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-11-01 to 2025-11-01.)
ArticleCitations
Recoupling C and N cycles: a fertiliser template to synchronise N supply and limit C priming?631
Altered rainfall greatly affects enzyme activity but has limited effect on microbial biomass in Australian dryland soils292
Scaling up taxon-specific microbial traits to predict community-level microbial activity in agricultural systems227
Carbon acquisition ecological strategies to connect soil microbial biodiversity and carbon cycling224
Trophic interrelationships drive the biogeography of protistan community in agricultural ecosystems202
Land-use driven changes in elemental stoichiometry decouple the positive soil biodiversity-stability relationship191
Drying-rewetting of permanent pasture and agricultural soils induces a shift towards microbial use of more C-rich organic matter181
Responses of root architecture and the rhizosphere microbiome assembly of maize (Zea mays L.) to a soil texture gradient177
The soil microbial community and plant biomass differentially contribute to the retention and recycling of urinary-N in grasslands173
Limited effects of century-old biochar on taxonomic and functional diversities of collembolan communities across land-uses171
A microbial-explicit model with comprehensive nitrogen processes to quantify gaseous nitrogen production from agricultural soils165
Revisiting process-based simulations of soil nitrite dynamics: Tighter cycling between nitrite and nitrate than considered previously163
Biogeography of soil protistan consumer and parasite is contrasting and linked to microbial nutrient mineralization in forest soils at a wide-scale152
Microbial “hotspots” of organic matter decomposition in temperate peatlands are driven by local spatial heterogeneity in abiotic conditions and not by vegetation structure151
Disentangling the contribution of mycorrhizal fungi to soil organic carbon storage148
Strong rhizosphere priming effects on N dynamics in soils with higher soil N supply capacity: The ‘Matthew effect’ in plant-soil systems148
Nitrate-induced hydroxyl radical releases deep soil organic carbon by opening the ‘enzyme latch’ under micro-aerobic conditions148
Abundant and rare fungal taxa exhibit different patterns of phylogenetic niche conservatism and community assembly across a geographical and environmental gradient143
Microbial transformation mechanisms of particulate organic carbon to mineral-associated organic carbon at the chemical molecular level: Highlighting the effects of ambient temperature and soil moistur143
The influence of soil development on the depth distribution and structure of soil microbial communities139
Legacy effects of rhizodeposits on soil microbiomes: A perspective136
Stability of iron-carbon complexes determines carbon sequestration efficiency in iron-rich soils133
Nitrogen addition altered the plant-arbuscular mycorrhizal fungi network through reducing redundant interactions in an alpine meadow126
Crop productivity, resource allocation and nitrogen concentration as affected by soil decomposers, mixed cropping and crop genotype124
Tackling global biogeography and drivers of soil microbial dehalogenation traits and taxa: Insights from metagenomic profiling based on a curated dehalogenase database118
Fungal decomposition and transformation of molecular and colloidal fractions of dissolved organic matter extracted from boreal forest soil117
Earthworms in an enhanced weathering mesocosm experiment: Effects on soil carbon sequestration, base cation exchange and soil CO2 efflux115
Editorial Board115
Different responses of nitrous oxide emissions to liming and manure amendment of an acidic ultisol are controlled by autotrophic and heterotrophic nitrification113
Conversion of SIC to SOC enhances soil carbon sequestration and soil structural stability in alpine ecosystems of the Qinghai-Tibet Plateau109
Root exudation processes induce the utilization of microbial-derived components by rhizoplane microbiota under conservation agriculture108
Phosphorus addition ameliorates soil micro-food web simplification due to nitrogen enrichment but does not restore nematode community composition107
Contrasting effects of biological soil crusts on soil respiration in a typical steppe105
Shrub effects on the decomposition microenvironment and changes in litter quality have opposing effects on litter decomposition102
Earthworm ecotype diversity mitigates resource limitations of microbial community in arable soils99
Comparative analysis of diversity and environmental niches of soil bacterial, archaeal, fungal and protist communities reveal niche divergences along environmental gradients in the Alps96
Response of soil microbial diversity and functionality to snow removal in a cool-temperate forest96
Nitrogen induced soil carbon gains are resistant to loss after the cessation of excess nitrogen inputs94
Straw return and low N addition modify the partitioning of dissimilatory nitrate reduction by increasing conversion to ammonium in paddy fields93
From rhizosphere to detritusphere – Soil structure formation driven by plant roots and the interactions with soil biota91
Soil nitrogen availability increases the abundance of nitrogen-fixing plants in subtropical forests91
Microbial starch degradation in arid soil: Community dynamics, environmental influences, and archaeological implications90
Time-dependent regulation of soil aggregates on fertilizer N retention and the influence of straw mulching89
Multi-amplicon nitrogen cycling gene standard: An innovative approach for quantifying N-transforming soil microbes in terrestrial ecosystems87
Distinct mechanisms drive plant-nitrifier interactions in topsoil and subsoil86
Expedited loss of soil biodiversity in blue carbon ecosystems caused by rising sea levels86
Soil oxidoreductase zymography: Visualizing spatial distributions of peroxidase and phenol oxidase activities at the root-soil interface85
Tree decline and mortality following pathogen invasion alters the diversity, composition and network structure of the soil microbiome85
Arbuscular mycorrhizal inoculation and plant response strongly shape bacterial and eukaryotic soil community trajectories85
Dual role of silt and clay in the formation and accrual of stabilized soil organic carbon84
Biochar addition regulates soil and earthworm gut microbiome and multifunctionality82
Cry for help from rhizosphere microbiomes and self-rescue strategies cooperatively alleviate drought stress in spring wheat82
Soil metabolomics - current challenges and future perspectives82
Long-term warming-induced trophic downgrading in the soil microbial food web82
Metabolic pathways of CO2 fixing microorganisms determined C-fixation rates in grassland soils along the precipitation gradient82
Hydrophilic and hydrophobic fractions of extracellular fungal phosphatases interact differently with clay mineral surfaces81
Drought-induced changes in rare microbial community promoted contribution of microbial necromass C to SOC in a subtropical forest81
Rice root Fe plaque increases paddy soil CH4 emissions via the promotion of electron transfer for syntrophic methanogenesis80
Corrigendum to “Spatial and temporal detection of root exudates with a paper-based microfluidic device” [Soil Biol. Biochem. 195 (2024), 109456]80
Mineral type and land-use intensity control composition and functions of microorganisms colonizing pristine minerals in grassland soils78
Historical forest disturbance reduces soil microbial efficiency across multiple carbon sources77
Editorial Board77
Thermodynamic control on the decomposition of organic matter across different electron acceptors76
Enhanced mite grazing leads to pattern shifts in soil N2O emissions after organic fertilizer application76
Sporadic P limitation constrains microbial growth and facilitates SOM accumulation in the stoichiometrically coupled, acclimating microbe–plant–soil model76
Contrasting responses of microbial diversity and community structure in decaying root bark and xylem to N addition in an alpine shrubland76
Impact of graphite nano amendments on soil enzyme activities, functional genes and microbiome composition in a soil-plant system74
Resolving dynamic mineral-organic interactions in the rhizosphere by combining in-situ microsensors with plant-soil reactive transport modeling74
No thermal adaptation in soil extracellular enzymes across a temperate grassland region74
The effects of climate warming and exogenous nitrogen input on soil N2O emissions from mangroves72
Soil textural control on moisture distribution at the microscale and its effect on added particulate organic matter mineralization72
Selective utilization of organic carbon molecules promotes arsenic methylation by increasing methyltransferase activity in arsM-harboring microbes of paddy soils71
Rapid transfer of C and N excreted by decomposer soil animals to plants and above-ground herbivores71
Long-term N-addition alters the community structure of functionally important N-cycling soil microorganisms across global grasslands70
Depth effects on bacterial community assembly processes in paddy soils70
The interplay between Azospirillum brasilense and the native bacterial communities in the soil and rhizosphere of maize (Zea mays L.)70
Biochar-influenced solubilization and mineralization mechanisms of phosphorus in saline-sodic soils70
Manure application effects on subsoils: Abundant taxa initiate the diversity reduction of rare bacteria and community functional alterations67
Microbial resistance in rhizosphere hotspots under biodegradable and conventional microplastic amendment: Community and functional sensitivity66
Microbial necromass as the source of soil organic carbon in global ecosystems66
Testing the environmental controls of microbial nitrogen-mining induced by semi-continuous labile carbon additions in the subarctic66
Nitrogen availability and mineral particles contributed fungal necromass to the newly formed stable carbon pool in the alpine areas of Southwest China65
Arbuscular mycorrhizal fungi have a greater role than root hairs of maize for priming the rhizosphere microbial community and enhancing rhizosphere organic P mineralization65
Pathways of biogenically excreted organic matter into soil aggregates65
Shedding light on the functional role of the Ignavibacteria in Italian rice field soil: A meta-genomic/transcriptomic analysis64
Spatial and temporal detection of root exudates with a paper-based microfluidic device64
Kinetics of arsenic and antimony reduction and oxidation in peatlands treating mining-affected waters: Effects of microbes, temperature, and carbon substrate62
Alternate wetting-drying had no preferences for rice P uptake but increased microbial P allocation to phospholipids: Evidence from dual 32P and 33P labeling62
A global meta-analysis reveals the positive effect of invasive alien plants on soil heterotrophic respiration62
Soil legacies of a primary invader strongly drive secondary invasions for species that are phylogenetically distant62
Tillage and pesticide seed treatments have distinct effects on soil microbial diversity and function61
Role of different size classes of organisms in cropped soils: What do litterbag experiments tell us? A meta-analysis61
Reductive dissolution of iron phosphate modifies rice root morphology in phosphorus-deficient paddy soils61
Spatial access and resource limitations control carbon mineralization in soils61
Effects of warming on bacterial growth rates in a peat soil under ambient and elevated CO260
Drought shifts soil nematodes to smaller size across biological scales60
Soil carbon mineralization and microbial community dynamics in response to pyrogenic organic matter addition60
The newly proposed threshold for enzymatic stoichiometry: A reliable solution?59
Soil clay minerals: An overlooked mediator of gross N transformations in Regosolic soils of subtropical montane landscapes58
Carbon flow from roots to rhizobacterial networks: Grafting effects58
Whole soil warming promotes surface soil carbon loss but deep soil carbon gain, depending on land management practices in temperate climate57
Coupling energy balance and carbon flux during cellulose degradation in arable soils57
Abundant and rare bacteria possess different diversity and function in crop monoculture and rotation systems across regional farmland57
Energy and matter dynamics in an estuarine soil are more sensitive to warming than salinization57
Mixing with coniferous tree species alleviates rhizosphere soil phosphorus limitation of broad-leaved trees in subtropical plantations56
Eukaryotes in soil aggregates across conservation managements: Major roles of protists, fungi and taxa linkages in soil structuring and C stock56
Disentangling carbon stabilization in a Calcisol subsoil amended with iron oxyhydroxides: A dual-13C isotope approach55
Identification of the rhizosphere microbes that actively consume plant-derived carbon54
Root exudation and rhizosphere microbial assembly are influenced by novel plant trait diversity in carrot genotypes53
Field application of pure polyethylene microplastic has no significant short-term effect on soil biological quality and function53
Plant root exudates and rhizosphere bacterial communities shift with neighbor context53
Corrigendum to “Plant phenology modulates and undersown cover crops mitigate N2O emissions” [Soil Biol. Biochem. 198 (2024) 109548]52
Nitrifier controls on soil NO and N2O emissions in three chaparral ecosystems under contrasting atmospheric N inputs52
Organic cropping systems alter metabolic potential and carbon, nitrogen and phosphorus cycling capacity of soil microbial communities52
Editorial Board52
Evaluation of the relation between soil biomass of arbuscular mycorrhizal fungi and glomalin-related soil protein in conservation agriculture51
Unravelling the facilitation-competition continuum among ectomycorrhizal and saprotrophic fungi51
Root exudate stoichiometry is a key driver of soil N cycling: implications for forest responses to global change51
How does organic amendment affect soil microbial nitrate immobilization rate?51
Dose-response patterns of anaerobic oxidation of methane to nitrogen addition in Chinese paddy fields51
Editorial Board51
Alterations in substrate stoichiometry control the responses of soil diazotrophs to nutrient enrichment51
Dynamic stability of mineral-associated organic matter: enhanced stability and turnover through organic fertilization in a temperate agricultural topsoil50
Priming effect on soil carbon decomposition by root exudate surrogates: A meta-analysis50
Microbial community assembly and its influencing factors of secondary forests in Qinling Mountains50
Dynamic changes in bacterial community structure are associated with distinct priming effect patterns49
Litter diversity accelerates labile carbon but slows recalcitrant carbon decomposition49
Soil P availability and mycorrhizal type determine root exudation in sub-tropical forests49
Phosphorus limitation regulates the responses of microbial carbon metabolism to long-term combined additions of nitrogen and phosphorus in a cropland49
Transferring concepts from plant to microbial ecology: A framework proposal to identify relevant bacterial functional traits48
Soil nematode community profiling using reference-free mito-metagenomics48
Mineral-bound lipid formation in soils and sediments: the importance of microbial pathways48
Simplified estimates of soil nematode body mass using maximum diameter: Insights from large-scale grasslands across China48
Rewetting alongside biochar and sulphate addition mitigates greenhouse gas emissions and retain carbon in degraded upland peatlands48
Primary carbon sources and self-induced metabolic landscapes shape community structure in soil bacterial hotspots48
Fiddler crab bioturbation stimulates methane emissions in mangroves: Insights into microbial mechanisms47
Do chromogenic assays of soil enzyme activities need buffers? More disadvantages than advantages of modified universal buffer in the para-nitrophenyl-based assay of phosphomonoesterase and β-glucosida47
Regulation of soil nitrogen cycling by shrubs in grasslands47
Molecular weight of dissolved organic matter determines its interactions with microbes and its assembly processes in soils46
Tillage homogenizes soil bacterial communities in microaggregate fractions by facilitating dispersal46
Disproportional oxidation rates of ammonia and nitrite deciphers the heterogeneity of fertilizer-induced N2O emissions in agricultural soils46
Divergent responses of soil glomalin and microbial necromass to precipitation reduction: New perspectives from soil aggregates and multi-trophic networks46
Modeling ecosystem-scale carbon dynamics in soil: The microbial dimension46
Forest restoration increases energy flow through the fungal channel and decreases energy flow through the herbivorous channel in soil micro-food webs46
Spatiotemporal variation in soil methane uptake in a cool-temperate immature deciduous forest46
Factors predictive of the biogeographic distribution of comammox Nitrospira in terrestrial ecosystems45
Editorial Board44
The soil microbial methylome: A tool to explore the role of epigenetic memory in driving soil abiotic legacy effects44
Interplanting leguminous shrubs boosts the trophic interactions of soil micro-food web in a karst grassland44
Editorial Board44
Editorial Board44
Earthworm influence on soil aggregate distribution and protected carbon at managed forest sites in Vermont, USA44
Deciphering factors controlling decay and nitrogen accumulation in coarse wood debris of five tree species using 15N labeled wood disks43
Precipitation balances deterministic and stochastic processes of bacterial community assembly in grassland soils43
Differential accumulation patterns of microbial necromass induced by maize root vs. shoot residue addition in agricultural Alfisols43
The only constant is change: Endogenous circadian rhythms of soil microbial activities43
Aeolian dust deposition as a driver of cyanobacterial community structure in biological soil crusts43
Plant organ rather than cover crop species determines residue incorporation into SOC pools42
Microplastics exert minor influence on bacterial community succession during the aging of earthworm (Lumbricus terrestris) casts42
Preceding crop legacy modulates the early growth of winter wheat by influencing root growth dynamics, rhizosphere processes, and microbial interactions42
N-induced soil acidification triggers metal stimulation of soil methane oxidation in a temperate steppe ecosystem42
Carbon cycle in the microbial ecosystems of biological soil crusts42
Acidic amelioration of soil amendments improves soil health by impacting rhizosphere microbial assemblies42
High stochasticity in rare bacterial community assembly in rice-wheat rotation soils at a regional scale42
Restructuring of soil food webs reduces carbon storage potential in boreal peatlands42
When microclimates meet soil microbes: Temperature controls soil microbial diversity along an elevational gradient in subtropical forests42
Elevated CO2 and nitrogen interactively affect the rhizosphere priming effect of Cunninghamia lanceolata41
Distinct seasonal and annual variability of prokaryotes, fungi and protists in cropland soil under different tillage systems and soil texture41
Linking Rock-Eval parameters to soil heterotrophic respiration and microbial residues in a black soil41
Plant mixture effects on carbon-degrading enzymes promote soil organic carbon accumulation41
Back to the roots: Characterizing root exudates of dominant tundra plants to improve the understanding of plant-soil interactions in a changing arctic40
The influence of forest-to-cropland conversion on temperature sensitivity of soil microbial respiration across tropical to temperate zones40
Editorial Board40
Editorial Board40
Controlling matric potential in microfluidics to examine microbial dynamics in unsaturated porous media40
Signal molecules and enzymes produced by Rhizobium leguminosarum sv. trifolii strains originating from the subpolar and temperate climate zones as elements of adaptation to low temperature stress40
Nitrogen addition increases the glucose-induced priming effect of the particulate but not the mineral-associated organic carbon fraction40
Co-localised phosphorus mobilization processes in the rhizosphere of field-grown maize jointly contribute to plant nutrition40
Degradation dynamics and microbial processes in yak dung on the Tibetan Plateau40
Wood decomposition in poorly-drained forested wetland soils: How important are termites?40
Obituary : Clive Arthur Tudor Edwards - 16 June 1925–20 July 202139
Editorial Board39
Adult body mass influences multi-element stoichiometry in ground beetles39
The role of the soil microbiome in the colonisation of glacier forefields by Antarctic pearlwort (Colobanthus quitensis) under current and future climate change scenarios39
Deepened snow in combination with summer warming increases growing season nitrous oxide emissions in dry tundra, but not in wet tundra39
Editorial Board39
Editorial Board39
D genome acquisition and breeding have had a significant impact on interaction of wheat with ACC deaminase producers in soil or ACC deaminase potential activity in the rhizosphere39
Seed treatment with plant-defense elicitors decreases the abundance of ammonia oxidizers associated with winter wheat roots39
Seasonal changes in soil biofilm microbial communities39
Bacterial community response to environmental change varies with depth in the surface soil38
Aridity thresholds of microbiome-soil function relationship along a climatic aridity gradient in alpine ecosystem38
Linkages between the temperature sensitivity of soil respiration and microbial life strategy are dependent on sampling season38
Nitrogen deposition stimulates decomposition via changes in the structure and function of litter food webs38
Polar soils exhibit distinct patterns in microbial diversity and dominant phylotypes38
Decoupled responses of leaf and root decomposition to nutrient deposition in a subtropical plantation38
Specific utilization of biopolymers of plant and fungal origin reveals the existence of substrate-specific guilds for bacteria in temperate forest soils37
Tracing sources and turnover of soil organic matter in a long-term irrigated dry forest using a novel hydrogen isotope approach37
Biocrusts drive soil respiration across seasons and depths in a cold-winter desert37
Shifts in C-degradation genes and microbial metabolic activity with vegetation types affected the surface soil organic carbon pool37
Lithologic control of microbial-derived carbon in forest soils37
Contributions of microbial necromass and plant lignin to soil organic carbon stock in a paddy field under simulated conditions of long-term elevated CO2 and warming36
Land use intensification homogenizes soil protist communities and alters their diversity across Europe36
Nitrogen-15 natural abundance is robust to quantify nitrogen transfer from clover to grass in temporary grassland36
Global climate changes decoupled soil nitrogen mineralization and immobilization36
Distinct N-cycling microbial communities contribute to microtopographic variation in soil N2O emissions from denitrification36
Phosphorus fertiliser source determines the allocation of root-derived organic carbon to soil organic matter fractions36
Aligning theoretical and empirical representations of soil carbon-to-nitrogen stoichiometry with process-based terrestrial biogeochemistry models35
Obituary: Philip Charles Brookes: 26th March 1951–28th September 202335
Editorial Board35
Year-round activity of microbial communities in cold-climate peatlands treating mining-affected waters35
Iron oxidation coupled with nitrate reduction affects the acetate-assimilating microbial community structure elucidated by stable isotope probing in flooded paddy soil35
Arbuscular mycorrhizal fungal communities of pristine rainforests and adjacent sugarcane fields recruit from different species pools35
Linking microbial-mediated methane production in wetlands to invasive plants35
The size-variation of microplastics alters plant nitrogen uptake by regulating soil gross nitrogen transformation rates35
Sorption strength determines alanine mineralization in volcanic soils35
Physical characterisation of chia mucilage polymeric gel and its implications on rhizosphere science - Integrating imaging, MRI, and modelling to gain insights into plant and microbial amended soils35
Recording earthworm diversity on the tropical island of Martinique using DNA barcoding unveiled endemic species in bromeliad plants34
Opposite priming responses to labile carbon versus oxygen pulses in anoxic peat34
Strong conditionality in plant-fungal community assembly after soil inoculation in post-agricultural grasslands34
The role of earthworms in the transformation of labile plant litter into mineral-associated organic matter34
Root exudates from drought-affected plants increase soil respiration across a range of grassland species34
Respiration and carbon use efficiency characteristics of soluble protein-derived carbon by soil microorganisms: A case study at afforested sites34
Revising the dynamic energy budget theory with a new reserve mobilization rule and three example applications to bacterial growth34
Are enzymes transported in soils by water fluxes?33
Interactive dynamics between rhizosphere bacterial and viral communities facilitate soybean fitness to cadmium stress revealed by time-series metagenomics33
Insight into the role of competition in niche differentiation between ammonia-oxidizing archaea and bacteria in ammonium-rich alkaline soil: A network-based study33
A rapid and sensitive assay to quantify amino sugars, neutral sugars and uronic acid necromass biomarkers using pre-column derivatization, ultra-high-performance liquid chromatography and high-resolut33
Increase in iron-bound organic carbon content under simulated sea-level rise: A “marsh organ” field experiment33
Mapping of suitable habitats for earthworms in China33
Influences of arsenate and/or phosphate adsorption to ferrihydrite on iron-reducing and arsenic-reducing microbial communities in paddy soil revealed by rRNA-13C-acetate probing33
Turnover of fungal glucosamine and bacterial muramic acid in comparison with soil organic carbon in two arable soils with distinct fungal communities33
Time-varying associations between absorptive fine roots and leaf litter decomposition across 23 plant species33
Biocrusts regulate the effect of rainfall pulses on soil respiration at different temporal scales on the Loess Plateau33
Plant community composition and traits modulate the impacts of drought intensity on soil microbial community composition and function33
Phosphorus-transforming microbes enhance phosphatase catalytic efficiency to alleviate phosphorus limitation under nitrogen and phosphorus additions in subtropical forest soil33
Different stochastic processes regulate bacterial and fungal community assembly in estuarine wetland soils32
Rigorous, empirical, and quantitative: a proposed pipeline for soil health assessments32
Soil microbial communities are driven by the declining availability of cations and phosphorus during ecosystem retrogression32
Responses of soil rare and abundant microorganisms to recurring biotic disturbances32
Plants with nitrate preference can regulate nitrification to meet their nitrate demand32
Phosphorus addition decreases soil fungal richness and alters fungal guilds in two tropical forests32
Combining multiple baiting cycles with digital droplet PCR optimizes description of the distribution of entomopathogenic nematodes in French maize fields31
LC-MS analysis of D2O-labelled soil suggests a large fraction of membrane lipid exists within slow growing microbes31
Litter decomposition rate response to multiple global change factors: A meta-analysis31
Arbuscular mycorrhiza fungi colonisation stimulates uptake of inorganic nitrogen and sulphur but reduces utilisation of organic forms in tomato31
Tracing service crops' net carbon and nitrogen rhizodeposition into soil organic matter fractions using dual isotopic brush-labeling31
Prolonged drought causes negative plant-soil feedbacks in grassland species under field conditions31
A full-length SSU rRNA-based workflow for high-resolution monitoring of nematode communities reveals direct and indirect responses to plant-based manipulations31
Microbial carbon use and associated changes in microbial community structure in high-Arctic tundra soils under elevated temperature31
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