Rhizosphere microbiome engineering with PGPR to combat soil-mediated climate change. [PDF]
Longhinos NB +10 more
europepmc +1 more source
Reduced legacy precipitation decreases microbial community growth efficiency and alters soil organic carbon in a California grassland. [PDF]
Hernandez LK +12 more
europepmc +1 more source
The impact of fertilization on the health of paddy soil: pathways and prospects for fertility regulation based on microbial communities. [PDF]
Xu H +9 more
europepmc +1 more source
Development of a high-throughput growth assay for bacteria or yeasts using an agar-based insoluble carbon source immobilization method. [PDF]
Liang J +5 more
europepmc +1 more source
Continental-scale drivers of soil microbial extracellular polymeric substances. [PDF]
Shi K +7 more
europepmc +1 more source
Degradation and Regeneration of Soil Structure in Intensified Paddy Fields: Plant-Soil Interactions, Ecological Effects, and Restoration Pathways. [PDF]
Fang M, Shen J, Liu G, Zhang C, Tang Z.
europepmc +1 more source
Editorial: Microbial solutions for restoring depleted soils. [PDF]
Mehnaz S, Shahid I, Walia A, Mumtaz MZ.
europepmc +1 more source
Microbial necromass as the source of soil organic carbon in global ecosystems
Abstract Despite the recognized importance of the contribution of microbial necromass to soil organic carbon (SOC) sequestration, at a global scale, there has been no quantification for cropland, grassland, and forest ecosystems. To address this knowledge gap, the contents of fungal and bacterial necromass were estimated based on glucosamine and ...
Wang Baorong, Chao Liang, Yakov Kuzyakov
exaly +4 more sources
Deconstructing the microbial necromass continuum to inform soil carbon sequestration
Abstract Microbial necromass is a large, dynamic and persistent component of soil organic carbon, the dominant terrestrial carbon pool. Quantification of necromass carbon stocks and its susceptibility to global change is becoming standard practice in soil carbon research.
Courtney A. Creamer +2 more
exaly +3 more sources
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