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Phytoplankton blooms provoke bacterioplankton blooms, from which bacterial biomass (necromass) is released via increased zooplankton grazing and viral lysis. While bacterial consumption of algal biomass during blooms is well-studied, little is known about the concurrent recycling of these substantial amounts of bacterial necromass. We demonstrate that bacterial biomass, such as bacterial alpha-glucan storage polysaccharides, generated from the consumption of algal organic matter, is reused and thus itself a major bacterial carbon source in vitro and during a diatom-dominated bloom. We highlight conserved enzymes and binding proteins of dominant bloom-responder clades that are presumably involved in the recycling of bacterial alpha-glucan by members of the bacterial community. We furthermore demonstrate that the corresponding protein machineries can be specifically induced by extracted alpha-glucan-rich bacterial polysaccharide extracts. This recycling of bacterial necromass likely constitutes a large-scale intra-population energy conservation mechanism that keeps substantial amounts of carbon in a dedicated part of the microbial loop.
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http://dx.doi.org/10.1038/s41467-024-48301-5 | DOI Listing |
BMC Plant Biol
September 2025
Key Laboratory of Grassland Resources of the Ministry of Education, College of Grassland Science, Inner Mongolia Agricultural University, Hohhot, 010011, China.
Background: Grazing, as one of the most important methods of utilizing natural grasslands, can significantly impact the accumulation and stabilization of soil organic carbon within grassland ecosystems. Soil microbial necromass carbon (MNC), including fungal necromass carbon (FNC) and bacterial necromass carbon (BNC), is an important source of soil organic carbon (SOC) and plays a critical role in the formation and stabilization of SOC. However, the effects of grazing intensity on soil MNC and its underlying drivers remain unclear.
View Article and Find Full Text PDFFront Microbiol
July 2025
Hebei Key Laboratory of Soil Ecology, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, China.
Substrate input and subsequent modification and turnover mediated by microbial systems determine the formation of soil organic carbon (C). However, the effects and mechanisms by which substrate stoichiometry (SS) adapts to microbial metabolic preferences and influences the dynamics of plant and microbial necromass C (PNC, MNC) remain unclear. Therefore, the variations and controlling factors of PNC and MNC in top- (0-20 cm) and subsoil (20-40 cm) across different SS conditions were investigated during the whole maize season.
View Article and Find Full Text PDFGlob Chang Biol
August 2025
Ministry of Education Key Lab of Environmental Remediation and Ecosystem Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou, China.
Soil organic carbon (C) is derived primarily from plant and microbial necromass; however, the global distribution and contribution of different necromass inputs to soil C storage remain unclear. We conducted a global meta-analysis encompassing 2410 observations from 249 microbial necromass studies and 786 observations from 72 plant residue studies. The results showed that the content of microbial-derived C (10.
View Article and Find Full Text PDFMol Ecol
August 2025
Department of Plant and Microbial Biology, University of Minnesota, St. Paul, Minnesota, USA.
Mycelial residues, also known as fungal necromass, represent a substantial fraction of soil organic matter (SOM) pools in terrestrial ecosystems worldwide. Although microbial decomposers are increasingly recognised as key drivers of fungal necromass carbon stock formation, the diversity and composition of their microbial predators-and the roles these predators play in mediating fungal necromass decomposition-have not been explored to date. To address this gap, we produced fungal necromass of varying biochemical quality from Hyaloscypha bicolor and decomposed it in forest topsoil in Minnesota, USA, to investigate how microbial decomposer (bacteria and fungi) and predator (protists and nematodes) communities differ between soil and necromass.
View Article and Find Full Text PDFEnviron Microbiome
July 2025
LART-IFEVA, Facultad de Agronomía/CONICET, Universidad de Buenos Aires, Buenos Aires, Argentina.
Background: Soil microbiomes are critical regulators of nutrient biogeochemical cycles, contributing significantly to ecosystem services that support plant productivity. In this study, we investigated the effects of agricultural rotations on soil microbial communities in Uruguayan grasslands, comparing cropland soils with native grasslands grazed by livestock. By employing advanced metagenomic techniques, we characterized the diversity and functional potential of the soil microbiome, with particular emphasis on its roles in carbon, nitrogen, and phosphorus cycling.
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