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 2021-06-01 to 2025-06-01.)
ArticleCitations
Revisiting process-based simulations of soil nitrite dynamics: Tighter cycling between nitrite and nitrate than considered previously493
The soil microbial community and plant biomass differentially contribute to the retention and recycling of urinary-N in grasslands234
Protists modulate fungal community assembly in paddy soils across climatic zones at the continental scale187
Limited effects of century-old biochar on taxonomic and functional diversities of collembolan communities across land-uses184
A microbial-explicit model with comprehensive nitrogen processes to quantify gaseous nitrogen production from agricultural soils178
Wildland fire ash enhances short-term CO2 flux from soil in a Southern African savannah168
Microbial “hotspots” of organic matter decomposition in temperate peatlands are driven by local spatial heterogeneity in abiotic conditions and not by vegetation structure154
Impact of common sample pre-treatments on key soil microbial properties144
Nitrate-induced hydroxyl radical releases deep soil organic carbon by opening the ‘enzyme latch’ under micro-aerobic conditions141
Strong rhizosphere priming effects on N dynamics in soils with higher soil N supply capacity: The ‘Matthew effect’ in plant-soil systems141
Altered rainfall greatly affects enzyme activity but has limited effect on microbial biomass in Australian dryland soils140
Scaling up taxon-specific microbial traits to predict community-level microbial activity in agricultural systems134
The influence of soil development on the depth distribution and structure of soil microbial communities133
Drying-rewetting of permanent pasture and agricultural soils induces a shift towards microbial use of more C-rich organic matter132
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 moistur124
Responses of root architecture and the rhizosphere microbiome assembly of maize (Zea mays L.) to a soil texture gradient123
Legacy effects of rhizodeposits on soil microbiomes: A perspective123
Trophic interrelationships drive the biogeography of protistan community in agricultural ecosystems121
Biogeography of soil protistan consumer and parasite is contrasting and linked to microbial nutrient mineralization in forest soils at a wide-scale118
Carbon acquisition ecological strategies to connect soil microbial biodiversity and carbon cycling115
Abundant and rare fungal taxa exhibit different patterns of phylogenetic niche conservatism and community assembly across a geographical and environmental gradient115
Stability of iron-carbon complexes determines carbon sequestration efficiency in iron-rich soils114
Editorial Board113
Distinct mechanisms drive plant-nitrifier interactions in topsoil and subsoil111
Tackling global biogeography and drivers of soil microbial dehalogenation traits and taxa: Insights from metagenomic profiling based on a curated dehalogenase database111
Nitrogen induced soil carbon gains are resistant to loss after the cessation of excess nitrogen inputs104
Multi-amplicon nitrogen cycling gene standard: An innovative approach for quantifying N-transforming soil microbes in terrestrial ecosystems101
Response of soil microbial diversity and functionality to snow removal in a cool-temperate forest97
VNIR and MIR spectroscopy of PLFA-derived soil microbial properties and associated soil physicochemical characteristics in an experimental plant diversity gradient96
Soil oxidoreductase zymography: Visualizing spatial distributions of peroxidase and phenol oxidase activities at the root-soil interface96
Expedited loss of soil biodiversity in blue carbon ecosystems caused by rising sea levels93
Shrub effects on the decomposition microenvironment and changes in litter quality have opposing effects on litter decomposition92
Conversion of SIC to SOC enhances soil carbon sequestration and soil structural stability in alpine ecosystems of the Qinghai-Tibet Plateau91
Arbuscular mycorrhizal inoculation and plant response strongly shape bacterial and eukaryotic soil community trajectories90
Biochar addition regulates soil and earthworm gut microbiome and multifunctionality87
Crop productivity, resource allocation and nitrogen concentration as affected by soil decomposers, mixed cropping and crop genotype86
Fungal decomposition and transformation of molecular and colloidal fractions of dissolved organic matter extracted from boreal forest soil85
Long-term warming-induced trophic downgrading in the soil microbial food web85
Earthworm ecotype diversity mitigates resource limitations of microbial community in arable soils85
Time-dependent regulation of soil aggregates on fertilizer N retention and the influence of straw mulching83
Earthworms in an enhanced weathering mesocosm experiment: Effects on soil carbon sequestration, base cation exchange and soil CO2 efflux83
Phosphorus addition ameliorates soil micro-food web simplification due to nitrogen enrichment but does not restore nematode community composition82
Root exudation processes induce the utilization of microbial-derived components by rhizoplane microbiota under conservation agriculture81
Soil macrofauna: Study problems and perspectives79
Aggregate fractions shaped molecular composition change of soil organic matter in a rice paddy under elevated CO2 and air warming79
Straw return and low N addition modify the partitioning of dissimilatory nitrate reduction by increasing conversion to ammonium in paddy fields79
Nitrogen addition altered the plant-arbuscular mycorrhizal fungi network through reducing redundant interactions in an alpine meadow79
Soil metabolomics - current challenges and future perspectives78
Different responses of nitrous oxide emissions to liming and manure amendment of an acidic ultisol are controlled by autotrophic and heterotrophic nitrification78
Tree decline and mortality following pathogen invasion alters the diversity, composition and network structure of the soil microbiome78
Drought-induced changes in rare microbial community promoted contribution of microbial necromass C to SOC in a subtropical forest77
Comparative analysis of diversity and environmental niches of soil bacterial, archaeal, fungal and protist communities reveal niche divergences along environmental gradients in the Alps77
Dual role of silt and clay in the formation and accrual of stabilized soil organic carbon76
Contrasting effects of biological soil crusts on soil respiration in a typical steppe76
Metabolic pathways of CO2 fixing microorganisms determined C-fixation rates in grassland soils along the precipitation gradient75
From rhizosphere to detritusphere – Soil structure formation driven by plant roots and the interactions with soil biota74
Corrigendum to “Spatial and temporal detection of root exudates with a paper-based microfluidic device” [Soil Biol. Biochem. 195 (2024), 109456]74
Rapid transfer of C and N excreted by decomposer soil animals to plants and above-ground herbivores73
Hydrophilic and hydrophobic fractions of extracellular fungal phosphatases interact differently with clay mineral surfaces72
Sporadic P limitation constrains microbial growth and facilitates SOM accumulation in the stoichiometrically coupled, acclimating microbe–plant–soil model72
Enhanced mite grazing leads to pattern shifts in soil N2O emissions after organic fertilizer application71
Root-o-Mat: A novel tool for 2D image processing of root-soil interactions and its application in soil zymography71
Thermodynamic control on the decomposition of organic matter across different electron acceptors71
Editorial Board70
Historical forest disturbance reduces soil microbial efficiency across multiple carbon sources69
No thermal adaptation in soil extracellular enzymes across a temperate grassland region69
Contrasting responses of microbial diversity and community structure in decaying root bark and xylem to N addition in an alpine shrubland68
The effects of climate warming and exogenous nitrogen input on soil N2O emissions from mangroves68
Spatial and temporal detection of root exudates with a paper-based microfluidic device67
Testing the environmental controls of microbial nitrogen-mining induced by semi-continuous labile carbon additions in the subarctic67
Nitrogen availability and mineral particles contributed fungal necromass to the newly formed stable carbon pool in the alpine areas of Southwest China67
Addition of base cations increases microbial carbon use efficiency and biomass in acidic soils67
Rice root Fe plaque increases paddy soil CH4 emissions via the promotion of electron transfer for syntrophic methanogenesis66
The interplay between Azospirillum brasilense and the native bacterial communities in the soil and rhizosphere of maize (Zea mays L.)65
Continuous application of conservation tillage affects in situ N2O emissions and nitrogen cycling gene abundances following nitrogen fertilization65
Manure application effects on subsoils: Abundant taxa initiate the diversity reduction of rare bacteria and community functional alterations65
Long-term N-addition alters the community structure of functionally important N-cycling soil microorganisms across global grasslands65
Impact of graphite nano amendments on soil enzyme activities, functional genes and microbiome composition in a soil-plant system65
Arbuscular mycorrhizal fungi have a greater role than root hairs of maize for priming the rhizosphere microbial community and enhancing rhizosphere organic P mineralization64
Mineral type and land-use intensity control composition and functions of microorganisms colonizing pristine minerals in grassland soils64
Microbial resistance in rhizosphere hotspots under biodegradable and conventional microplastic amendment: Community and functional sensitivity63
Selective utilization of organic carbon molecules promotes arsenic methylation by increasing methyltransferase activity in arsM-harboring microbes of paddy soils63
Soil textural control on moisture distribution at the microscale and its effect on added particulate organic matter mineralization63
Climate change drivers alter root controls over litter decomposition in a semi-arid grassland63
Depth effects on bacterial community assembly processes in paddy soils62
Shedding light on the functional role of the Ignavibacteria in Italian rice field soil: A meta-genomic/transcriptomic analysis62
Microbial necromass as the source of soil organic carbon in global ecosystems62
Use and abuse of potential rates in soil microbiology61
Resolving dynamic mineral-organic interactions in the rhizosphere by combining in-situ microsensors with plant-soil reactive transport modeling61
Organic cropping systems alter metabolic potential and carbon, nitrogen and phosphorus cycling capacity of soil microbial communities60
Root-induced fungal growth triggers macroaggregation in forest subsoils60
Energy and matter dynamics in an estuarine soil are more sensitive to warming than salinization60
Pathways of biogenically excreted organic matter into soil aggregates60
Soil carbon mineralization and microbial community dynamics in response to pyrogenic organic matter addition59
Soil clay minerals: An overlooked mediator of gross N transformations in Regosolic soils of subtropical montane landscapes59
Coupling energy balance and carbon flux during cellulose degradation in arable soils58
Carbon flow from roots to rhizobacterial networks: Grafting effects58
Effects of warming on bacterial growth rates in a peat soil under ambient and elevated CO257
A global meta-analysis on freeze-thaw effects on soil carbon and phosphorus cycling57
Disentangling carbon stabilization in a Calcisol subsoil amended with iron oxyhydroxides: A dual-13C isotope approach56
A global meta-analysis reveals the positive effect of invasive alien plants on soil heterotrophic respiration56
Mixing with coniferous tree species alleviates rhizosphere soil phosphorus limitation of broad-leaved trees in subtropical plantations55
Identification of the rhizosphere microbes that actively consume plant-derived carbon55
Spatial access and resource limitations control carbon mineralization in soils54
Role of different size classes of organisms in cropped soils: What do litterbag experiments tell us? A meta-analysis54
Altered microbial CAZyme families indicated dead biomass decomposition following afforestation53
Eukaryotes in soil aggregates across conservation managements: Major roles of protists, fungi and taxa linkages in soil structuring and C stock53
Drought shifts soil nematodes to smaller size across biological scales53
Root exudation and rhizosphere microbial assembly are influenced by novel plant trait diversity in carrot genotypes53
Kinetics of arsenic and antimony reduction and oxidation in peatlands treating mining-affected waters: Effects of microbes, temperature, and carbon substrate53
Plant root exudates and rhizosphere bacterial communities shift with neighbor context52
Reductive dissolution of iron phosphate modifies rice root morphology in phosphorus-deficient paddy soils52
Tillage and pesticide seed treatments have distinct effects on soil microbial diversity and function52
Field application of pure polyethylene microplastic has no significant short-term effect on soil biological quality and function52
Alternate wetting-drying had no preferences for rice P uptake but increased microbial P allocation to phospholipids: Evidence from dual 32P and 33P labeling52
Abundant and rare bacteria possess different diversity and function in crop monoculture and rotation systems across regional farmland52
Editorial Board51
Primary carbon sources and self-induced metabolic landscapes shape community structure in soil bacterial hotspots50
Editorial Board50
Soil nematode community profiling using reference-free mito-metagenomics50
Corrigendum to “Plant phenology modulates and undersown cover crops mitigate N2O emissions” [Soil Biol. Biochem. 198 (2024) 109548]49
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-glucosida49
Forest restoration increases energy flow through the fungal channel and decreases energy flow through the herbivorous channel in soil micro-food webs49
Molecular weight of dissolved organic matter determines its interactions with microbes and its assembly processes in soils48
Soil P availability and mycorrhizal type determine root exudation in sub-tropical forests48
Transferring concepts from plant to microbial ecology: A framework proposal to identify relevant bacterial functional traits48
Priming effect varies with root order: A case of Cunninghamia lanceolata48
Regulation of soil nitrogen cycling by shrubs in grasslands48
Simplified estimates of soil nematode body mass using maximum diameter: Insights from large-scale grasslands across China48
How does organic amendment affect soil microbial nitrate immobilization rate?47
Root exudate stoichiometry is a key driver of soil N cycling: implications for forest responses to global change47
Nitrifier controls on soil NO and N2O emissions in three chaparral ecosystems under contrasting atmospheric N inputs46
Modeling ecosystem-scale carbon dynamics in soil: The microbial dimension46
Litter diversity accelerates labile carbon but slows recalcitrant carbon decomposition46
Dominant plants affect litter decomposition mainly through modifications of the soil microbial community46
Alterations in substrate stoichiometry control the responses of soil diazotrophs to nutrient enrichment45
Priming effect on soil carbon decomposition by root exudate surrogates: A meta-analysis45
Phosphorus limitation regulates the responses of microbial carbon metabolism to long-term combined additions of nitrogen and phosphorus in a cropland45
Microbial community assembly and its influencing factors of secondary forests in Qinling Mountains45
Factors predictive of the biogeographic distribution of comammox Nitrospira in terrestrial ecosystems45
Disproportional oxidation rates of ammonia and nitrite deciphers the heterogeneity of fertilizer-induced N2O emissions in agricultural soils44
Fiddler crab bioturbation stimulates methane emissions in mangroves: Insights into microbial mechanisms44
Tillage homogenizes soil bacterial communities in microaggregate fractions by facilitating dispersal44
Evaluation of the relation between soil biomass of arbuscular mycorrhizal fungi and glomalin-related soil protein in conservation agriculture44
Dynamic changes in bacterial community structure are associated with distinct priming effect patterns44
Priming mechanisms providing plants and microbes access to mineral-associated organic matter43
Rice rhizodeposition promotes the build-up of organic carbon in soil via fungal necromass43
Soil microbial response to silicate fertilization reduces bioavailable arsenic in contaminated paddies43
Divergent responses of soil glomalin and microbial necromass to precipitation reduction: New perspectives from soil aggregates and multi-trophic networks42
Spatiotemporal variation in soil methane uptake in a cool-temperate immature deciduous forest42
Dynamic stability of mineral-associated organic matter: enhanced stability and turnover through organic fertilization in a temperate agricultural topsoil42
Editorial Board42
The soil microbial methylome: A tool to explore the role of epigenetic memory in driving soil abiotic legacy effects41
Corrigendum to “A meta-analysis of global cropland soil carbon change from cover cropping” [Soil Biol. Biochem. 143 (2020) 107735]41
Editorial Board41
Corrigendum to “Biological nitrogen fixation in peatlands: Comparison between acetylene reduction assay and 15N2 assimilation methods” [Soil Biology and Biochemistry 131 (2019) 157–165]41
Earthworm influence on soil aggregate distribution and protected carbon at managed forest sites in Vermont, USA41
Editorial Board41
Structure and function of bacterial metaproteomes across biomes40
Time-lapse approach to correct deficiencies of 2D soil zymography40
Linking Rock-Eval parameters to soil heterotrophic respiration and microbial residues in a black soil40
Plant organ rather than cover crop species determines residue incorporation into SOC pools40
Topographic differences in nitrogen cycling mediate nitrogen retention in a subtropical, N-saturated forest catchment39
The only constant is change: Endogenous circadian rhythms of soil microbial activities39
Interplanting leguminous shrubs boosts the trophic interactions of soil micro-food web in a karst grassland39
Restructuring of soil food webs reduces carbon storage potential in boreal peatlands38
Distinct seasonal and annual variability of prokaryotes, fungi and protists in cropland soil under different tillage systems and soil texture38
Elevated CO2 and nitrogen interactively affect the rhizosphere priming effect of Cunninghamia lanceolata38
Degradation dynamics and microbial processes in yak dung on the Tibetan Plateau37
N-induced soil acidification triggers metal stimulation of soil methane oxidation in a temperate steppe ecosystem37
Aeolian dust deposition as a driver of cyanobacterial community structure in biological soil crusts37
Microplastics exert minor influence on bacterial community succession during the aging of earthworm (Lumbricus terrestris) casts37
Nematode community diversity and function across an alpine landscape undergoing plant colonization of previously unvegetated soils37
Differential accumulation patterns of microbial necromass induced by maize root vs. shoot residue addition in agricultural Alfisols37
Deciphering factors controlling decay and nitrogen accumulation in coarse wood debris of five tree species using 15N labeled wood disks37
Nitrogen addition increases the glucose-induced priming effect of the particulate but not the mineral-associated organic carbon fraction36
Carbon cycle in the microbial ecosystems of biological soil crusts36
Co-localised phosphorus mobilization processes in the rhizosphere of field-grown maize jointly contribute to plant nutrition36
Plant mixture effects on carbon-degrading enzymes promote soil organic carbon accumulation36
When microclimates meet soil microbes: Temperature controls soil microbial diversity along an elevational gradient in subtropical forests36
Acidic amelioration of soil amendments improves soil health by impacting rhizosphere microbial assemblies36
Editorial Board36
High stochasticity in rare bacterial community assembly in rice-wheat rotation soils at a regional scale36
Editorial Board36
Precipitation balances deterministic and stochastic processes of bacterial community assembly in grassland soils36
Preceding crop legacy modulates the early growth of winter wheat by influencing root growth dynamics, rhizosphere processes, and microbial interactions36
Visualizing the transfer of organic matter from decaying plant residues to soil mineral surfaces controlled by microorganisms36
Obituary : Clive Arthur Tudor Edwards - 16 June 1925–20 July 202135
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 warming35
Nitrogen-15 natural abundance is robust to quantify nitrogen transfer from clover to grass in temporary grassland35
Editorial Board35
Editorial Board35
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 rhizosphere35
Editorial Board35
Wood decomposition in poorly-drained forested wetland soils: How important are termites?35
Seed treatment with plant-defense elicitors decreases the abundance of ammonia oxidizers associated with winter wheat roots35
No effect of long-term soil warming on diffusive soil inorganic and organic nitrogen fluxes in a temperate forest soil35
Aridity thresholds of microbiome-soil function relationship along a climatic aridity gradient in alpine ecosystem34
Long-term N inputs shape microbial communities more strongly than current-year inputs in soils under 10-year continuous corn cropping34
The effects of tree-mycorrhizal type on soil organic matter properties from neighborhood to watershed scales34
Decoupled responses of leaf and root decomposition to nutrient deposition in a subtropical plantation34
Specific utilization of biopolymers of plant and fungal origin reveals the existence of substrate-specific guilds for bacteria in temperate forest soils34
Seasonal changes in soil biofilm microbial communities34
Deepened snow in combination with summer warming increases growing season nitrous oxide emissions in dry tundra, but not in wet tundra34
Adult body mass influences multi-element stoichiometry in ground beetles34
The role of the soil microbiome in the colonisation of glacier forefields by Antarctic pearlwort (Colobanthus quitensis) under current and future climate change scenarios34
Biocrusts drive soil respiration across seasons and depths in a cold-winter desert33
Linkages between the temperature sensitivity of soil respiration and microbial life strategy are dependent on sampling season33
Iron oxidation coupled with nitrate reduction affects the acetate-assimilating microbial community structure elucidated by stable isotope probing in flooded paddy soil33
Shifts in C-degradation genes and microbial metabolic activity with vegetation types affected the surface soil organic carbon pool33
Distinct N-cycling microbial communities contribute to microtopographic variation in soil N2O emissions from denitrification33
Land use intensification homogenizes soil protist communities and alters their diversity across Europe33
Aligning theoretical and empirical representations of soil carbon-to-nitrogen stoichiometry with process-based terrestrial biogeochemistry models33
Disentangling the abiotic and biotic components of AMF suppressive soils33
Nitrogen deposition stimulates decomposition via changes in the structure and function of litter food webs33
Tracing sources and turnover of soil organic matter in a long-term irrigated dry forest using a novel hydrogen isotope approach32
The influence of forest-to-cropland conversion on temperature sensitivity of soil microbial respiration across tropical to temperate zones32
Time-varying associations between absorptive fine roots and leaf litter decomposition across 23 plant species32
Interactive dynamics between rhizosphere bacterial and viral communities facilitate soybean fitness to cadmium stress revealed by time-series metagenomics32
Polar soils exhibit distinct patterns in microbial diversity and dominant phylotypes32
Phosphorus fertiliser source determines the allocation of root-derived organic carbon to soil organic matter fractions32
Plants with nitrate preference can regulate nitrification to meet their nitrate demand32
Biocrusts regulate the effect of rainfall pulses on soil respiration at different temporal scales on the Loess Plateau32
Lithologic control of microbial-derived carbon in forest soils32
Bacterial community response to environmental change varies with depth in the surface soil32
Obituary: Philip Charles Brookes: 26th March 1951–28th September 202332
Root exudates from drought-affected plants increase soil respiration across a range of grassland species32
Soil aggregate isolation method affects interpretation of protistan community31
Recording earthworm diversity on the tropical island of Martinique using DNA barcoding unveiled endemic species in bromeliad plants31
Soil microbial communities are driven by the declining availability of cations and phosphorus during ecosystem retrogression31
Strong conditionality in plant-fungal community assembly after soil inoculation in post-agricultural grasslands31
Opposite priming responses to labile carbon versus oxygen pulses in anoxic peat31
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 soils31
Revising the dynamic energy budget theory with a new reserve mobilization rule and three example applications to bacterial growth31
Year-round activity of microbial communities in cold-climate peatlands treating mining-affected waters31
Arbuscular mycorrhizal fungal communities of pristine rainforests and adjacent sugarcane fields recruit from different species pools31
Editorial Board30
Increase in iron-bound organic carbon content under simulated sea-level rise: A “marsh organ” field experiment30
Use of metabolomics to quantify changes in soil microbial function in response to fertiliser nitrogen supply and extreme drought30
Responses of soil rare and abundant microorganisms to recurring biotic disturbances30
Respiration and carbon use efficiency characteristics of soluble protein-derived carbon by soil microorganisms: A case study at afforested sites30
Plant community composition and traits modulate the impacts of drought intensity on soil microbial community composition and function30
Sorption strength determines alanine mineralization in volcanic soils30
Different stochastic processes regulate bacterial and fungal community assembly in estuarine wetland soils30
Mapping of suitable habitats for earthworms in China30
Arbuscular mycorrhizal trees cause a higher carbon to nitrogen ratio of soil organic matter decomposition via rhizosphere priming than ectomycorrhizal trees30
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-resolut30
Phosphorus addition decreases soil fungal richness and alters fungal guilds in two tropical forests30
UV-B stress reshapes root-associated microbial communities and networks, driven by host plant resistance29
Life at the extreme: Plant-driven hotspots of soil nutrient cycling in the hyper-arid core of the Atacama Desert29
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