Role of plant growth-promoting rhizobacteria in boosting the phytoremediation of stressed soils: Opportunities, challenges, and prospects DOI

Poonam Bhanse,

Manish Kumar, Lal Singh

et al.

Chemosphere, Journal Year: 2022, Volume and Issue: 303, P. 134954 - 134954

Published: May 17, 2022

Language: Английский

The concept and future prospects of soil health DOI
Johannes Lehmann, Déborah Bossio, Ingrid Kögel‐Knabner

et al.

Nature Reviews Earth & Environment, Journal Year: 2020, Volume and Issue: 1(10), P. 544 - 553

Published: Aug. 25, 2020

Language: Английский

Citations

1000

Life and death in the soil microbiome: how ecological processes influence biogeochemistry DOI
Noah W. Sokol, Eric Slessarev, Gianna L. Marschmann

et al.

Nature Reviews Microbiology, Journal Year: 2022, Volume and Issue: 20(7), P. 415 - 430

Published: Feb. 28, 2022

Language: Английский

Citations

672

Dynamic interactions at the mineral–organic matter interface DOI
Markus Kleber, Ian C. Bourg, Elizabeth K. Coward

et al.

Nature Reviews Earth & Environment, Journal Year: 2021, Volume and Issue: 2(6), P. 402 - 421

Published: May 11, 2021

Language: Английский

Citations

657

Particulate organic matter as a functional soil component for persistent soil organic carbon DOI Creative Commons
Kristina Witzgall, Alix Vidal,

David Schubert

et al.

Nature Communications, Journal Year: 2021, Volume and Issue: 12(1)

Published: July 5, 2021

Abstract The largest terrestrial organic carbon pool, in soils, is regulated by an intricate connection between plant inputs, microbial activity, and the soil matrix. This manifested how microorganisms, key players transforming plant-derived into carbon, are controlled physical arrangement of inorganic particles. Here we conduct incubation isotopically labelled litter to study effects structure on fate litter-derived matter. While activity fungal growth enhanced coarser-textured soil, show that occlusion matter aggregates formation organo-mineral associations occur concurrently fresh surfaces regardless structure. These two mechanisms—the most prominent processes contributing persistence matter—occur directly at plant–soil interfaces, where constitute a nucleus build-up persistence. We extend notion litter, i.e., particulate matter, from solely easily available labile substrate, functional component which determined.

Language: Английский

Citations

453

Microplastic effects on carbon cycling processes in soils DOI Creative Commons
Matthias C. Rillig, Eva F. Leifheit, Johannes Lehmann

et al.

PLoS Biology, Journal Year: 2021, Volume and Issue: 19(3), P. e3001130 - e3001130

Published: March 30, 2021

Microplastics (MPs), plastic particles <5 mm, are found in environments, including terrestrial ecosystems, planetwide. Most research so far has focused on ecotoxicology, examining effects performance of soil biota controlled settings. As pivots to a more ecosystem and global change perspective, questions about soil-borne biogeochemical cycles become important. MPs can affect the carbon cycle numerous ways, for example, by being themselves influencing microbial processes, plant growth, or litter decomposition. Great uncertainty surrounds nano-sized particles, an expected by-product further fragmentation MPs. A major concerted effort is required understand pervasive functioning soils ecosystems; importantly, such needs capture immense diversity these terms chemistry, aging, size, shape.

Language: Английский

Citations

390

Microbial carbon use efficiency promotes global soil carbon storage DOI Creative Commons
Feng Tao, Yuanyuan Huang, Bruce A. Hungate

et al.

Nature, Journal Year: 2023, Volume and Issue: 618(7967), P. 981 - 985

Published: May 24, 2023

Abstract Soils store more carbon than other terrestrial ecosystems 1,2 . How soil organic (SOC) forms and persists remains uncertain 1,3 , which makes it challenging to understand how will respond climatic change 3,4 It has been suggested that microorganisms play an important role in SOC formation, preservation loss 5–7 Although affect the accumulation of matter through many pathways 4,6,8–11 microbial use efficiency (CUE) is integrative metric can capture balance these processes 12,13 CUE potential act as a predictor variation storage, persistence unresolved 7,14,15 Here we examine relationship between SOC, interactions with climate, vegetation edaphic properties, using combination global-scale datasets, microbial-process explicit model, data assimilation, deep learning meta-analysis. We find at least four times evaluated factors, such input, decomposition or vertical transport, determining storage its spatial across globe. In addition, shows positive correlation content. Our findings point major determinant global storage. Understanding underlying their environmental dependence may help prediction feedback changing climate.

Language: Английский

Citations

358

Soil organic matter formation, persistence, and functioning: A synthesis of current understanding to inform its conservation and regeneration DOI
Maurizio Cotrufo, Jocelyn M. Lavallee

Advances in agronomy, Journal Year: 2022, Volume and Issue: unknown, P. 1 - 66

Published: Jan. 1, 2022

Language: Английский

Citations

353

Biochar in agriculture – A systematic review of 26 global meta‐analyses DOI Creative Commons
Hans‐Peter Schmidt, Claudia Kammann, Nikolas Hagemann

et al.

GCB Bioenergy, Journal Year: 2021, Volume and Issue: 13(11), P. 1708 - 1730

Published: Sept. 1, 2021

Abstract Biochar is obtained by pyrolyzing biomass and is, definition, applied in a way that avoids its rapid oxidation to CO 2 . Its use agriculture includes animal feeding, manure treatment (e.g. as additive for bedding, composting, storage or anaerobic digestion), fertilizer component direct soil application. Because the feedstock carbon photosynthetically fixed from atmosphere, producing applying biochar essentially dioxide removal (CDR) technology, which has high‐technology readiness level. However, swift implementation of pyrogenic capture (PyCCS), needs deliver co‐benefits, example, improving crop yields ecosystem services and/or climate change resilience ameliorating key properties. Agronomic research rapidly evolving field moving less than 100 publications 2010 more 15,000 end 2020. Here, we summarize 26 rigorously selected meta‐analyses published since 2016 investigated multitude properties agronomic performance parameters impacted application, effects on yield, root biomass, water efficiency, microbial activity, organic greenhouse gas emissions. All show compelling evidence overall beneficial effect all parameters. One remaining challenges standardization basic analysis, still lacking many studies. Incomplete characterization increases uncertainty because adverse individual studies included might be related low‐quality biochars, would not qualify certification subsequent high content contaminants, salinity, incomplete pyrolysis, etc.). In summary, our systematic review suggests potential combine CDR with significant environmental co‐benefits.

Language: Английский

Citations

290

Contrasting pathways of carbon sequestration in paddy and upland soils DOI
Xiangbi Chen,

Yajun Hu,

Yinhang Xia

et al.

Global Change Biology, Journal Year: 2021, Volume and Issue: 27(11), P. 2478 - 2490

Published: March 13, 2021

Paddy soils make up the largest anthropogenic wetlands on earth, and are characterized by a prominent potential for organic carbon (C) sequestration. By quantifying plant- microbial-derived C in across four climate zones, we identified that accrual is achieved via contrasting pathways paddy upland soils. Paddies 39%-127% more efficient soil (SOC) sequestration than their adjacent counterparts, with greater differences warmer cooler climates. Upland replenished C, whereas enriched proportion of plant-derived because retarded microbial decomposition under anaerobic conditions induced flooding paddies. Under both land-use types, maximal contribution plant residues to SOC at intermediate mean annual temperature (15-20°C), neutral (pH~7.3), low clay/sand ratio. contrast, high (~24°C), pH (~5), large ratio favorable strengthening necromass. The necromass waterlogged paddies climates likely due fast anabolism from bacteria, fungi unlikely be involved as they aerobic. In scenario conversion upland, total 504 Tg may lost CO

Language: Английский

Citations

239

A critical review of mineral–microbe interaction and co-evolution: mechanisms and applications DOI Creative Commons
Hailiang Dong, Liuqin Huang, Linduo Zhao

et al.

National Science Review, Journal Year: 2022, Volume and Issue: 9(10)

Published: July 4, 2022

Mineral–microbe interactions play important roles in environmental change, biogeochemical cycling of elements and formation ore deposits. Minerals provide both beneficial (physical chemical protection, nutrients, energy) detrimental (toxic substances oxidative pressure) effects to microbes, resulting mineral-specific microbial colonization. Microbes impact dissolution, transformation precipitation minerals through their activity, either genetically controlled or metabolism-induced biomineralization. Through these interactions, microbes co-evolve Earth history. typically occur at microscopic scale but the effect is often manifested global scale. Despite advances achieved decades research, major questions remain. Four areas are identified for future research: integrating mineral ecology, establishing biosignatures, linking laboratory mechanistic investigation field observation, manipulating mineral–microbe benefit humankind.

Language: Английский

Citations

227