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Pristine groundwater is a highly stable environment with microbes adapted to dark, oligotrophic conditions. Input events like heavy rainfalls can introduce excess particulate organic matter including surface-derived microbes into the groundwater, hereby creating a disturbance to the groundwater micr...
ORGANISM(S): Escherichia coli 
2022-05-31 | PXD031173 | Pride
Necromass Interactions 16S Metagenome
Studying the effect of necromass addition to groundwater samples using stable isotope probing
Fungal necromass in soil is one of the major carbon stocks. A wide range of fungi are associated with necromass decomposition in soil, however, wood rot fungi have not be tested to determine how they might be utilizing carbon and nitrogen embedded in the fungal necromass. Given their saprotrophic ca...
ORGANISM(S): Trametes versicolor Gloeophyllum trabeum 
2026-06-02 | GSE326267 | GEO
Bacteria are major drivers of organic matter decomposition and play crucial roles in global nutrient cycling. Although the degradation of dead fungal biomass (necromass) is increasingly recognized as an important contributor to soil carbon (C) and nitrogen (N) cycling, the genes and metabolic pathwa...
ORGANISM(S): Serratia marcescens Cellvibrio japonicus Chitinophaga pinensis 
2024-05-29 | GSE268149 | GEO
Fungal necromass in soil represents the stable carbon pools. While fungi are known to decompose fungal necromass, how fungi decomopose melanin, remains poorly understood. Recently, Trichoderma species was found to be one of the most commonly associated fungi in soil, we have used a relevant fungal s...
ORGANISM(S): Trichoderma reesei 
2024-05-01 | GSE263516 | GEO
Transcriptomic evidence that lignolytic fungi deconstruct fungal necromass and plant litter via similar pathways
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