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1. Population Genomics of Aspergillus sojae is Shaped by the Food Environment

   https://doi.org/10.1093/gbe/evaf067  

   Acevedo, Kimberly L; Eaton, Elizabeth; Leite, Julia; Zhao, Shu; Chacon-Vargas, Katherine; McCarthy, Colin M; Choi, Dasol; O’Donnell, Samuel; Gluck-Thaler, Emile; Yu, Jae-Hyuk; et al (April 2025, Genome Biology and Evolution)

   Zufall, Rebecca (Ed.)

   Abstract Traditional fermented foods often contain specialized microorganisms adapted to their unique environments. For example, the filamentous mold Aspergillus oryzae, used in saké fermentation, has evolved to thrive in starch-rich conditions compared to its wild ancestor, Aspergillus flavus. Similarly, Aspergillus sojae, used in soybean-based fermentations like miso and shochu, is hypothesized to have been domesticated from Aspergillus parasiticus. Here, we examined the effects of long-term A. sojae use in soybean fermentation on population structure, genome variation, and phenotypic traits. We analyzed 17 A. sojae and 24 A. parasiticus genomes (23 of which were sequenced for this study), alongside phenotypic traits of 9 isolates. Aspergillus sojae formed a distinct, low-diversity population, suggesting a recent clonal expansion. Interestingly, a population of A. parasiticus was more closely related to A. sojae than other A. parasiticus populations. Genome comparisons revealed loss-of-function mutations in A. sojae, notably in biosynthetic gene clusters encoding secondary metabolites, including the aflatoxin cluster. Interestingly though, A. sojae harbored a partial duplication of a siderophore biosynthetic cluster. Phenotypic assays showed A. sojae lacked aflatoxin production, while it was variable in A. parasiticus isolates. Additionally, certain A. sojae strains exhibited larger colony diameters under miso-like salt conditions. These findings support the hypothesis that A. parasiticus is the progenitor of A. sojae and that domestication significantly reduced genetic diversity. Future research should explore how wild and food-associated strains influence sensory attributes and microbial community dynamics in fermented soy products. 

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2. Hydrolysis of lignocellulose by anaerobic fungi produces free sugars and organic acids for two‐stage fine chemical production with Kluyveromyces marxianus

   https://doi.org/10.1002/btpr.3172  

   Hillman, Ethan_T; Li, Mengwan; Hooker, Casey_A; Englaender, Jacob_A; Wheeldon, Ian; Solomon, Kevin_V (May 2021, Biotechnology Progress)

   Abstract Development of the bioeconomy is driven by our ability to access the energy‐rich carbon trapped in recalcitrant plant materials. Current strategies to release this carbon rely on expensive enzyme cocktails and physicochemical pretreatment, producing inhibitory compounds that hinder subsequent microbial bioproduction. Anaerobic fungi are an appealing solution as they hydrolyze crude, untreated biomass at ambient conditions into sugars that can be converted into value‐added products by partner organisms. However, some carbon is lost to anaerobic fungal fermentation products. To improve efficiency and recapture this lost carbon, we built a two‐stage bioprocessing system pairing the anaerobic fungusPiromyces indianaewith the yeastKluyveromyces marxianus, which grows on a wide range of sugars and fermentation products. In doing so we produce fine and commodity chemicals directly from untreated lignocellulose.P.indianaeefficiently hydrolyzed substrates such as corn stover and poplar to generate sugars, fermentation acids, and ethanol, whichK.marxianusconsumed while producing 2.4 g/L ethyl acetate. An engineered strain ofK.marxianuswas also able to produce 550 mg/L 2‐phenylethanol and 150 mg/L isoamyl alcohol fromP.indianaehydrolyzed lignocellulosic biomass. Despite the use of crude untreated plant material, production yields were comparable to optimized rich yeast media due to the use of all available carbon including organic acids, which formed up to 97% of free carbon in the fungal hydrolysate. This work demonstrates that anaerobic fungal pretreatment of lignocellulose can sustain the production of fine chemicals at high efficiency by partnering organisms with broad substrate versatility. 

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3. Climate-driven succession in marine microbiome biodiversity and biogeochemical function

   https://doi.org/10.1038/s41467-025-59382-1  

   Larkin, Alyse_A; Brock, Melissa_L; Fagan, Adam_J; Moreno, Allison_R; Gerace, Skylar_D; Lees, Lauren_E; Suarez, Stacy_A; Eloe-Fadrosh, Emiley_A; Martiny, Adam_C (April 2025, Nature Communications)

   Abstract Seasonal and El Niño-Southern Oscillation (ENSO) warming result in similar ocean changes as predicted with climate change. Climate-driven environmental cycles have strong impacts on microbiome diversity, but impacts on microbiome function are poorly understood. Here we quantify changes in microbial genomic diversity and functioning over 11 years covering seasonal and ENSO cycles at a coastal site in the southern California Current. We observe seasonal oscillations between large-genome lineages during cold, nutrient rich conditions in winter and spring versus small-genome lineages, includingProchlorococcusandPelagibacter, in summer and fall. Parallel interannual changes separate communities depending on ENSO condition. Biodiversity shifts translate into clear oscillations in microbiome functional potential. Ocean warming induced an ecosystem with less iron but more macronutrient stress genes, depressed organic carbon degradation potential and biomass, and elevated carbon-to-nutrient biomass ratios. The consistent microbial response observed across time-scales points towards large climate-driven changes in marine ecosystems and biogeochemical cycles. 

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4. Enhanced plant leaf P and unchanged soil P stocks after a quarter century of warming in the arctic tundra

   https://doi.org/10.1002/ecs2.3838  

   McLaren, Jennie R.; Buckeridge, Kate M. (November 2021, Ecosphere)

   Abstract Phosphorus (P) limits or co‐limits plant and microbial life in multiple ecosystems, including the arctic tundra. Although current global carbon (C) models focus on the coupling between soil nitrogen (N) and C, ecosystem P response to climate warming may also influence the global C cycle. Permafrost soils may see enhanced or reduced P availability under climate warming through multiple mechanisms including changing litter inputs through plant community change, changing plant–microbial dynamics, altered rates of mineralization of soil organic P through increased microbial activity, and newly exposed mineral‐bound P via deeper thaw. We investigated the effect of long‐term warming on plant leaf, multiple soil and microbial C, N, and P pools, and microbial extracellular enzyme activities, in Alaskan tundra plots underlain by permafrost. Here, we show that 25 yr of experimental summer warming increases community‐level plant leaf P through changing community composition to favour relatively P‐rich plant species. However, despite associated increases in P‐rich litter inputs, we found only a few responses in the belowground pools of P available for plant and microbial uptake, including a weak positive response for citric acid–extractable PO₄in the surface soil, a decrease in microbial biomass P, and no change in soil P (or C or N) stocks. This weak, neutral, or negative belowground P response to warming despite enhanced litter P inputs is consistent with a growing number of studies in the arctic tundra that find no long‐term response of soil C and N stocks to warming. 

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5. Substrate availability and not thermal acclimation controls microbial temperature sensitivity response to long‐term warming

   https://doi.org/10.1111/gcb.16544  

   Domeignoz‐Horta, Luiz A.; Pold, Grace; Erb, Hailey; Sebag, David; Verrecchia, Eric; Northen, Trent; Louie, Katherine; Eloe‐Fadrosh, Emiley; Pennacchio, Christa; Knorr, Melissa A.; et al (March 2023, Global Change Biology)

   Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stocks under climate change are highly sensitive to shifts in the mechanisms assumed to control the microbial physiological response to warming. Two mechanisms have been suggested to explain the long-­ term warming impact on microbial physiology: microbial thermal acclimation and changes in the quantity and quality of substrates available for microbial metabolism. Yet studies disentangling these two mechanisms are lacking. To resolve the drivers of changes in microbial physiology in response to long-­ term warming, we sampled soils from 13-­ and 28-­ year-­ old soil warming experiments in different seasons. We performed short-­ term laboratory incubations across a range of temperatures to measure the relationships between temperature sensitivity of physiology (growth, respiration, carbon use efficiency, and extracellular enzyme activity) and the chemical composition of soil organic matter. We observed apparent thermal acclimation of microbial respiration, but only in summer, when warming had exacerbated the seasonally-­ induced, already small dissolved organic matter pools. Irrespective of warming, greater quantity and quality of soil carbon increased the extracellular enzymatic pool and its temperature sensitivity. We propose that fresh litter input into the system seasonally cancels apparent thermal acclimation of C-­ cycling processes to decadal warming. Our findings reveal that long-term warming has indirectly affected microbial physiology via reduced C availability in this system, implying that earth system models including these negative feedbacks may be best suited to describe long-­ term warming effects on these soils. 

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