Soil Biology & Biochemistry

Papers
(The TQCC of Soil Biology & Biochemistry is 25. 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 2020-09-01 to 2024-09-01.)
ArticleCitations
Plant- or microbial-derived? A review on the molecular composition of stabilized soil organic matter474
The microplastisphere: Biodegradable microplastics addition alters soil microbial community structure and function331
Microbial necromass as the source of soil organic carbon in global ecosystems316
Microplastics in the agroecosystem: Are they an emerging threat to the plant-soil system?234
How microbes can, and cannot, be used to assess soil health229
Effects of microplastics on plant growth and arbuscular mycorrhizal fungal communities in a soil spiked with ZnO nanoparticles179
The physical structure of soil: Determinant and consequence of trophic interactions174
Soil extracellular enzyme stoichiometry reflects the shift from P- to N-limitation of microorganisms with grassland restoration140
Network analysis and subsequent culturing reveal keystone taxa involved in microbial litter decomposition dynamics140
Soil microbial diversity and composition: Links to soil texture and associated properties138
Changes in soil bacterial and fungal community composition and functional groups during the succession of boreal forests132
Soil microbial network complexity predicts ecosystem function along elevation gradients on the Tibetan Plateau129
Effects of nitrogen and phosphorus addition on microbial community composition and element cycling in a grassland soil129
Deliberate introduction of invisible invaders: A critical appraisal of the impact of microbial inoculants on soil microbial communities128
Negative effects of multiple global change factors on soil microbial diversity122
Microbial necromass on the rise: The growing focus on its role in soil organic matter development112
Soil aggregate size-dependent relationships between microbial functional diversity and multifunctionality112
Global patterns and associated drivers of priming effect in response to nutrient addition106
Organic amendments drive shifts in microbial community structure and keystone taxa which increase C mineralization across aggregate size classes106
Organic fertilization promotes crop productivity through changes in soil aggregation102
Long-term excess nitrogen fertilizer increases sensitivity of soil microbial community to seasonal change revealed by ecological network and metagenome analyses100
Tradeoffs among microbial life history strategies influence the fate of microbial residues in subtropical forest soils99
Glomalin – Truths, myths, and the future of this elusive soil glycoprotein95
Biochar stability and impact on soil organic carbon mineralization depend on biochar processing, aging and soil clay content95
Stoichiometric imbalance and microbial community regulate microbial elements use efficiencies under nitrogen addition93
Application of biofertilizer containing Bacillus subtilis reduced the nitrogen loss in agricultural soil92
Priming mechanisms providing plants and microbes access to mineral-associated organic matter92
Sticky dead microbes: Rapid abiotic retention of microbial necromass in soil90
From diversity to complexity: Microbial networks in soils90
How soil biota regulate C cycling and soil C pools in diversified crop rotations90
Microbial communities in crop phyllosphere and root endosphere are more resistant than soil microbiota to fertilization90
Global biogeography of fungal and bacterial biomass carbon in topsoil88
Assembly of abundant and rare bacterial and fungal sub-communities in different soil aggregate sizes in an apple orchard treated with cover crop and fertilizer87
Adaptive pathways of soil microorganisms to stoichiometric imbalances regulate microbial respiration following afforestation in the Loess Plateau, China87
Increasing contribution of microbial residues to soil organic carbon in grassland restoration chronosequence87
Fertilization changes soil microbiome functioning, especially phagotrophic protists86
Changes in assembly processes of soil microbial communities during secondary succession in two subtropical forests86
Long-term high-P fertilizer input decreased the total bacterial diversity but not phoD-harboring bacteria in wheat rhizosphere soil with available-P deficiency86
An evaluation of carbon indicators of soil health in long-term agricultural experiments86
Fungi determine increased soil organic carbon more than bacteria through their necromass inputs in conservation tillage croplands85
Deep-C storage: Biological, chemical and physical strategies to enhance carbon stocks in agricultural subsoils84
Metagenomics and stable isotope probing reveal the complementary contribution of fungal and bacterial communities in the recycling of dead biomass in forest soil84
The ‘soil health’ metaphor: Illuminating or illusory?84
Management practices differently affect particulate and mineral-associated organic matter and their precursors in arable soils84
Biogeographic patterns of microbial co-occurrence ecological networks in six American forests83
Soil properties rather than climate and ecosystem type control the vertical variations of soil organic carbon, microbial carbon, and microbial quotient82
Cautionary notes on the use of co-occurrence networks in soil ecology80
Responses of soil nitrogen and phosphorus cycling to drying and rewetting cycles: A meta-analysis80
Globally nitrogen addition alters soil microbial community structure, but has minor effects on soil microbial diversity and richness79
Strong priming of soil organic matter induced by frequent input of labile carbon78
The role of plant input physical-chemical properties, and microbial and soil chemical diversity on the formation of particulate and mineral-associated organic matter78
Heterotrophic nitrification – An eternal mystery in the nitrogen cycle75
Pathways of biogenically excreted organic matter into soil aggregates74
Aridity and NPP constrain contribution of microbial necromass to soil organic carbon in the Qinghai-Tibet alpine grasslands74
The life of soils: Integrating the who and how of multifunctionality74
Metagenomics reveals taxon-specific responses of the nitrogen-cycling microbial community to long-term nitrogen fertilization73
Nematode-based indices in soil ecology: Application, utility, and future directions72
Soil texture affects the coupling of litter decomposition and soil organic matter formation72
Predicting measures of soil health using the microbiome and supervised machine learning71
Patterns and determinants of soil microbial residues from tropical to boreal forests71
A global meta-analysis on freeze-thaw effects on soil carbon and phosphorus cycling70
Impact of nitrogen addition on plant-soil-enzyme C–N–P stoichiometry and microbial nutrient limitation69
Deterministic selection dominates microbial community assembly in termite mounds68
NosZ clade II rather than clade I determine in situ N2O emissions with different fertilizer types under simulated climate change and its legacy68
Dissolved organic matter characteristics in soils of tropical legume and non-legume tree plantations68
Century long fertilization reduces stochasticity controlling grassland microbial community succession68
Root functional traits are key determinants of the rhizosphere effect on soil organic matter decomposition across 14 temperate hardwood species68
Niche differentiation of clade A comammox Nitrospira and canonical ammonia oxidizers in selected forest soils67
Stoichiometric regulation of priming effects and soil carbon balance by microbial life strategies66
Root exudates shift how N mineralization and N fixation contribute to the plant-available N supply in low fertility soils65
Deciphering the relative importance of soil and plant traits on the development of rhizosphere microbial communities65
Rhizosphere microbial communities explain positive effects of diverse crop rotations on maize and soybean performance64
Initial soil formation by biocrusts: Nitrogen demand and clay protection control microbial necromass accrual and recycling64
Mycorrhizal fungi and phosphatase involvement in rhizosphere phosphorus transformations improves plant nutrition during subtropical forest succession64
Can moisture affect temperature dependences of microbial growth and respiration?63
Microplastics effects on soil biota are dependent on their properties: A meta-analysis63
Global effects on soil respiration and its temperature sensitivity depend on nitrogen addition rate63
Plant carbon inputs through shoot, root, and mycorrhizal pathways affect soil organic carbon turnover differently63
Plant root exudates and rhizosphere bacterial communities shift with neighbor context63
Where and why do particulate organic matter (POM) and mineral-associated organic matter (MAOM) differ among diverse soils?63
Plant residue chemical quality modulates the soil microbial response related to decomposition and soil organic carbon and nitrogen stabilization in a rainfed Mediterranean agroecosystem62
Visualizing the transfer of organic matter from decaying plant residues to soil mineral surfaces controlled by microorganisms62
Organic matter stabilization in aggregates and density fractions in paddy soil depending on long-term fertilization: Tracing of pathways by 13C natural abundance62
Rare fungus, Mortierella capitata, promotes crop growth by stimulating primary metabolisms related genes and reshaping rhizosphere bacterial community62
Comparing root exudate collection techniques: An improved hybrid method62
Drought accentuates the role of mycorrhiza in phosphorus uptake61
Organic matter chemistry and bacterial community structure regulate decomposition processes in post-fire forest soils61
Different contribution of species sorting and exogenous species immigration from manure to soil fungal diversity and community assemblage under long-term fertilization60
Fungal denitrification revisited – Recent advancements and future opportunities60
Temperatures beyond the community optimum promote the dominance of heat-adapted, fast growing and stress resistant bacteria in alpine soils60
Continuous application of conservation tillage affects in situ N2O emissions and nitrogen cycling gene abundances following nitrogen fertilization60
Biochar with large specific surface area recruits N2O-reducing microbes and mitigate N2O emission59
Effects of disturbance to moss biocrusts on soil nutrients, enzyme activities, and microbial communities in degraded karst landscapes in southwest China58
Field application of pure polyethylene microplastic has no significant short-term effect on soil biological quality and function58
Functional compensation dominates the assembly of plant rhizospheric bacterial community58
Direct and indirect influences of long-term fertilization on microbial carbon and nitrogen cycles in an alpine grassland57
Crop production correlates with soil multitrophic communities at the large spatial scale57
Straw chemistry links the assembly of bacterial communities to decomposition in paddy soils56
Oxygen availability determines key regulators in soil organic carbon mineralisation in paddy soils55
Identification of microbial strategies for labile substrate utilization at phylogenetic classification using a microcosm approach55
Priming, stabilization and temperature sensitivity of native SOC is controlled by microbial responses and physicochemical properties of biochar55
Improved global-scale predictions of soil carbon stocks with Millennial Version 255
Plant and microbial pathways driving plant diversity effects on soil carbon accumulation in subtropical forest54
Sensitivity of soil carbon dynamics to nitrogen and phosphorus enrichment in an alpine meadow54
Does the ratio of β-1,4-glucosidase to β-1,4-N-acetylglucosaminidase indicate the relative resource allocation of soil microbes to C and N acquisition?54
Precipitation balances deterministic and stochastic processes of bacterial community assembly in grassland soils53
Biochar induces mineralization of soil recalcitrant components by activation of biochar responsive bacteria groups53
Differential accumulation of microbial necromass and plant lignin in synthetic versus organic fertilizer-amended soil52
Rhizosphere hotspots: Root hairs and warming control microbial efficiency, carbon utilization and energy production52
Rice rhizodeposition promotes the build-up of organic carbon in soil via fungal necromass52
Distribution of phosphorus cycling genes across land uses and microbial taxonomic groups based on metagenome and genome mining52
Modulation of the soil microbiome by long-term Ca-based soil amendments boosts soil organic carbon and physicochemical quality in a tropical no-till crop rotation system51
Nitrogen addition increases microbial necromass in croplands and bacterial necromass in forests: A global meta-analysis51
Different stochastic processes regulate bacterial and fungal community assembly in estuarine wetland soils51
Coarse mineral-associated organic matter is a pivotal fraction for SOM formation and is sensitive to the quality of organic inputs51
Long-term diverse rotation alters nitrogen cycling bacterial groups and nitrous oxide emissions after nitrogen fertilization50
Impacts of forest thinning on soil microbial community structure and extracellular enzyme activities: A global meta-analysis50
Soil acidification modifies soil depth-microbiome relationships in a no-till wheat cropping system50
Quantification of the global impact of agricultural practices on soil nematodes: A meta-analysis50
Rhizosphere microbiome assembly involves seed-borne bacteria in compensatory phosphate solubilization50
Depth effects on bacterial community assembly processes in paddy soils50
Primings of soil organic matter and denitrification mediate the effects of moisture on nitrous oxide production49
A critical perspective on interpreting amplicon sequencing data in soil ecological research49
Revisiting the quantitative contribution of microbial necromass to soil carbon pool: Stoichiometric control by microbes and soil49
Organic phosphorus availability shapes the diversity of phoD-harboring bacteria in agricultural soil49
Nitrogen addition stimulates priming effect in a subtropical forest soil49
Effects of elevated pH and phosphorus fertilizer on soil C, N and P enzyme stoichiometry in an acidic mixed mesophytic deciduous forest48
Long-term farmyard manure application affects soil organic phosphorus cycling: A combined metagenomic and 33P/14C labelling study48
Application of manure from cattle administered antibiotics has sustained multi-year impacts on soil resistome and microbial community structure48
Decreased rhizodeposition, but increased microbial carbon stabilization with soil depth down to 3.6 m47
Fungal extracellular polymeric substance matrices – Highly specialized microenvironments that allow fungi to control soil organic matter decomposition reactions47
Ecoenzymatic stoichiometry can reflect microbial resource limitation, substrate quality, or both in forest soils47
Labile carbon facilitated phosphorus solubilization as regulated by bacterial and fungal communities in Zea mays47
The contribution of ammonia-oxidizing archaea and bacteria to gross nitrification under different substrate availability47
Earthworms accelerate the biogeochemical cycling of potentially toxic elements: Results of a meta-analysis47
Microbial solubilization of silicon and phosphorus from bedrock in relation to abundance of phosphorus-solubilizing bacteria in temperate forest soils46
Linkages between the temperature sensitivity of soil respiration and microbial life strategy are dependent on sampling season46
Co-symbiosis of arbuscular mycorrhizal fungi (AMF) and diazotrophs promote biological nitrogen fixation in mangrove ecosystems46
Mineralization of organic carbon and formation of microbial biomass in soil: Effects of clay content and composition and the mechanisms involved46
Meta-analysis of the impact of freeze–thaw cycles on soil microbial diversity and C and N dynamics45
Resistant soil carbon is more vulnerable to priming effect than active soil carbon45
Turnover of gram-negative bacterial biomass-derived carbon through the microbial food web of an agricultural soil45
Rhizosphere effects of woody plants on soil biogeochemical processes: A meta-analysis45
Stable isotopes reveal that fungal residues contribute more to mineral-associated organic matter pools than plant residues45
Abiotic and biotic regulation on carbon mineralization and stabilization in paddy soils along iron oxide gradients45
Active metabolic pathways of anaerobic methane oxidation in paddy soils45
Arbuscular mycorrhizal fungi and goethite promote carbon sequestration via hyphal-aggregate mineral interactions45
Interacting effects of land use type, microbes and plant traits on soil aggregate stability45
Potential of crop-livestock integration to enhance carbon sequestration and agroecosystem functioning in semi-arid croplands45
Soil microbiome drives the recovery of ecosystem functions after fire45
Nitrogen addition alters composition, diversity, and functioning of microbial communities in mangrove soils: An incubation experiment45
Resistance of microbial community and its functional sensitivity in the rhizosphere hotspots to drought45
Global meta-analysis of terrestrial nitrous oxide emissions and associated functional genes under nitrogen addition44
The importance of rare versus abundant phoD-harboring subcommunities in driving soil alkaline phosphatase activity and available P content in Chinese steppe ecosystems44
Distinct factors drive the diversity and composition of protistan consumers and phototrophs in natural soil ecosystems44
Soil macrofauna: Study problems and perspectives43
Iron-bound organic carbon is conserved in the rhizosphere soil of freshwater wetlands43
Priming effects induced by degradable microplastics in agricultural soils43
Sulfate addition and rising temperature promote arsenic methylation and the formation of methylated thioarsenates in paddy soils43
Dynamic changes in bacterial community structure are associated with distinct priming effect patterns43
Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter43
Dominant plants affect litter decomposition mainly through modifications of the soil microbial community43
Antibiotic resistance gene abundance and bacterial community structure in soils altered by Ammonium and Nitrate Concentrations42
Plant-derived lipids play a crucial role in forest soil carbon accumulation42
Soil enzyme stoichiometry is tightly linked to microbial community composition in successional ecosystems after glacier retreat42
Nutrient (C, N and P) enrichment induces significant changes in the soil metabolite profile and microbial carbon partitioning42
Protists modulate fungal community assembly in paddy soils across climatic zones at the continental scale42
Drought accelerated recalcitrant carbon loss by changing soil aggregation and microbial communities in a subtropical forest41
Microbial substrate stoichiometry governs nutrient effects on nitrogen cycling in grassland soils41
Loss of microbial diversity does not decrease γ-HCH degradation but increases methanogenesis in flooded paddy soil41
Effect of a tree mixture and water availability on soil nutrients and extracellular enzyme activities along the soil profile in an experimental forest41
Top-down effects of protists are greater than bottom-up effects of fertilisers on the formation of bacterial communities in a paddy field soil41
Soil bacterial community functions and distribution after mining disturbance41
Estimating microbial carbon use efficiency in soil: Isotope-based and enzyme-based methods measure fundamentally different aspects of microbial resource use40
The role of land management and elevation in shaping soil microbial communities: Insights from the Central European Alps39
Grassland degradation-induced declines in soil fungal complexity reduce fungal community stability and ecosystem multifunctionality39
Microbial carbon use efficiency and priming of soil organic matter mineralization by glucose additions in boreal forest soils with different C:N ratios39
Chronic nitrogen addition differentially affects gross nitrogen transformations in alpine and temperate grassland soils39
Microbial community succession in soil is mainly driven by carbon and nitrogen contents rather than phosphorus and sulphur contents39
Nitrogen-induced acidification plays a vital role driving ecosystem functions: Insights from a 6-year nitrogen enrichment experiment in a Tibetan alpine meadow39
Carbon nanotubes accelerate acetoclastic methanogenesis: From pure cultures to anaerobic soils39
Rates of dark CO2 fixation are driven by microbial biomass in a temperate forest soil39
Maize root exudate composition alters rhizosphere bacterial community to control hotspots of hydrolase activity in response to nitrogen supply39
Trade-offs in greenhouse gas emissions across a liming-induced gradient of soil pH: Role of microbial structure and functioning39
Succession of the composition and co-occurrence networks of rhizosphere microbiota is linked to Cd/Zn hyperaccumulation39
Plants with an ammonium preference affect soil N transformations to optimize their N acquisition38
Iron-bound carbon increases along a freshwater−oligohaline gradient in a subtropical tidal wetland38
Carbon pathways in aggregates and density fractions in Mollisols under water and straw management: Evidence from 13C natural abundance38
Invasive plant-derived dissolved organic matter alters microbial communities and carbon cycling in soils38
Biochar alters nitrogen and phosphorus dynamics in a western rangeland ecosystem38
Sources and priming of soil N2O and CO2 production: Nitrogen and simulated exudate additions38
Microbial resistance in rhizosphere hotspots under biodegradable and conventional microplastic amendment: Community and functional sensitivity38
Long-term organic fertilization promotes the resilience of soil multifunctionality driven by bacterial communities38
Soil aggregate-mediated microbial responses to long-term warming38
Root and mycorrhizal strategies for nutrient acquisition in forests under nitrogen deposition: A meta-analysis38
Impact of grassland afforestation with contrasting tree species on soil phosphorus fractions and alkaline phosphatase gene communities38
Soil microbiome signatures are associated with pesticide residues in arable landscapes37
Mycorrhizal association of common European tree species shapes biomass and metabolic activity of bacterial and fungal communities in soil37
Evidence for involvement of keystone fungal taxa in organic phosphorus mineralization in subtropical soil and the impact of labile carbon37
Drought-induced and seasonal variation in carbon use efficiency is associated with fungi:bacteria ratio and enzyme production in a grassland ecosystem37
Abundance of saprotrophic fungi determines decomposition rates of leaf litter from arbuscular mycorrhizal and ectomycorrhizal trees in a subtropical forest37
Temperature and soil management effects on carbon fluxes and priming effect intensity37
Plant pathological condition is associated with fungal community succession triggered by root exudates in the plant-soil system37
Predicting the influence of fertilization regimes on potential N fixation through their effect on free-living diazotrophic community structure in double rice cropping systems37
Root-induced fungal growth triggers macroaggregation in forest subsoils36
Metagenomic reconstruction of nitrogen and carbon cycling pathways in forest soil: Influence of different hardwood tree species36
Soil carbon dynamics during drying vs. rewetting: Importance of antecedent moisture conditions36
Energy flux across multitrophic levels drives ecosystem multifunctionality: Evidence from nematode food webs36
Decomposing cover crops modify root-associated microbiome composition and disease tolerance of cash crop seedlings36
Ammonia-oxidizing bacteria and fungal denitrifier diversity are associated with N2O production in tropical soils36
Canonical ammonia oxidizers, rather than comammox Nitrospira, dominated autotrophic nitrification during the mineralization of organic substances in two paddy soils36
Loss of microbial diversity weakens specific soil functions, but increases soil ecosystem stability36
Aridity decreases soil protistan network complexity and stability36
Synthesis of methods used to assess soil protease activity35
Microbial functional genes driving the positive priming effect in forest soils along an elevation gradient35
Modeling ecosystem-scale carbon dynamics in soil: The microbial dimension35
Maize genotype-specific exudation strategies: An adaptive mechanism to increase microbial activity in the rhizosphere35
Species pool and local ecological assembly processes shape the β-diversity of diazotrophs in grassland soils35
Niche specialization of comammox Nitrospira clade A in terrestrial ecosystems35
Disentangling the impact of contrasting agricultural management practices on soil microbial communities – Importance of rare bacterial community members34
Active phoD-harboring bacteria are enriched by long-term organic fertilization34
Soil and temperature effects on nitrification and denitrification modified N2O mitigation by 3,4-dimethylpyrazole phosphate34
You must choose, but choose wisely: Model-based approaches for microbial community analysis34
Gross nitrogen transformations in tropical pasture soils as affected by Urochloa genotypes differing in biological nitrification inhibition (BNI) capacity34
The unexplored role of preferential flow in soil carbon dynamics34
Carbon cycle in the microbial ecosystems of biological soil crusts34
The chemodiversity of paddy soil dissolved organic matter is shaped and homogenized by bacterial communities that are orchestrated by geographic distance and fertilizations34
Soil aggregate development and associated microbial metabolic limitations alter grassland carbon storage following livestock removal34
Metabolic pathways of CO2 fixing microorganisms determined C-fixation rates in grassland soils along the precipitation gradient34
A soil microbial model to analyze decoupled microbial growth and respiration during soil drying and rewetting34
The nitrogen gap in soil health concepts and fertility measurements34
Microbial carbon use efficiency, biomass residence time and temperature sensitivity across ecosystems and soil depths34
Soil carbon balance by priming differs with single versus repeated addition of glucose and soil fertility level34
Co-occurring increased phosphatase activity and labile P depletion in the rhizosphere of Lupinus angustifolius assessed with a novel, combined 2D-imaging approach34
Soil aggregate modulates microbial ecological adaptations and community assemblies in agricultural soils34
Niche differentiation of bacteria and fungi in carbon and nitrogen cycling of different habitats in a temperate coniferous forest: A metaproteomic approach34
Effect of rice (Oryza sativa L.) genotype on yield: Evidence from recruiting spatially consistent rhizosphere microbiome33
Biochar amendment increases bacterial diversity and vegetation cover in trace element-polluted soils: A long-term field experiment33
Physical mechanisms for soil moisture effects on microbial carbon-use efficiency in a sandy loam soil in the western United States33
A meta-analysis of phosphatase activity in agricultural settings in response to phosphorus deficiency33
Long-term regional evidence of the effects of livestock grazing on soil microbial community structure and functions in surface and deep soil layers33
Differential accumulation patterns of microbial necromass induced by maize root vs. shoot residue addition in agricultural Alfisols33
Form of nitrogen input dominates N effects on root growth and soil aggregation: A meta-analysis33
Disentangling the effects of nitrogen availability and soil acidification on microbial taxa and soil carbon dynamics in natural grasslands33
Soil organic carbon becomes newer under warming at a permafrost site on the Tibetan Plateau33
Long-term increase in rainfall decreases soil organic phosphorus decomposition in tropical forests33
Acidic amelioration of soil amendments improves soil health by impacting rhizosphere microbial assemblies33
Electron shuttle potential of biochar promotes dissimilatory nitrate reduction to ammonium in paddy soil33
Bacterial community structure and putative nitrogen-cycling functional traits along a charosphere gradient under waterlogged conditions33
Plant litter traits control microbial decomposition and drive soil carbon stabilization32
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