Dead fungal cells, known as necromass, are increasingly recognised as significant contributors to long-term soil carbon pools, yet the genes involved in necromass decomposition are poorly understood. In particular, how microorganisms degrade necromass with differing initial cell wall chemical compositions using carbohydrate-active enzymes (CAZymes) has not been well studied. Based on the frequent occurrence and high abundance of the fungal genus Trichoderma on decaying fungal necromass in situ, we grew Trichoderma reesei RUT-C30 on low and high melanin necromass of Hyaloscypha bicolor (Ascomycota) in liquid cultures and assessed T. reesei gene expression relative to each other and relative to glucose. Transcriptome data revealed that T. reesei up-regulated many genes (over 100; necromass versus glucose substrate) coding for CAZymes, including enzymes that would target individual layers of an Ascomycota fungal cell wall. We also observed differential expression of protease- and laccase-encoding genes on high versus low melanin necromass, highlighting a subset of genes (fewer than 15) possibly linked to the deconstruction of melanin, a cell wall constituent that limits necromass decay rates in nature. Collectively, these results advance our understanding of the genomic traits underpinning the rates and fates of carbon turnover in an understudied pool of Earth's belowground carbon, fungal necromass.
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http://dx.doi.org/10.1111/1462-2920.70006 | DOI Listing |
Sci Total Environ
January 2025
Institute of Ecology and Ministry of Education Key Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China. Electronic address:
Soil organic carbon (SOC) plays a critical role in mitigating climate change. Conceptualizing SOC into particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) helps us more accurately predict the responses of organic carbon, with varying chemical composition, molecular size, and degree of association with soil minerals, to environmental changes. To assess the controlling factors of particulate organic carbon (POC) and mineral-associated organic carbon (MAOC), plant and soil samples were collected from 54 temperate grassland sites in Northern China, and the impacts of climate, plants, soil properties and microorganisms on POC and MAOC contents were analyzed.
View Article and Find Full Text PDFEnviron Microbiol
December 2024
Department of Plant and Microbial Biology, College of Biological Sciences, University of Minnesota, Twin Cities, Minnesota, USA.
Environ Res
January 2025
Environment Research Institute, Shandong University, Qingdao 266237, China. Electronic address:
Inland wetlands might be an important "carbon sink", and the chronosequence development of newly formed inland wetlands offers a natural and suitable opportunity for studying the dynamic effect of plant and microbial necromass carbon (PlantC and MNC) on the soil organic carbon (SOC) stabilization. The space-for-time chronosequence approach was used and plots were established in the three ages of newly formed inland wetlands (2, 5, and 16 years). Soil samples were collected in the surface (0-10 cm) and subsurface soil (20-30 cm).
View Article and Find Full Text PDFJ Environ Manage
December 2024
Key Laboratory of Land Resources Evaluation and Monitoring in Southwest, Ministry of Education, Sichuan Normal University, Jingan Road 5, 610068, Chengdu, China; Institute of Landscape Ecology, University of Münster, Heisenbergstr. 2, Münster, 48149, Germany. Electronic address:
Mineral-associated organic matter (MAOM) constitutes a significant portion of carbon (C) pools in wetlands, determining their role as C sinks or sources. Nevertheless, detailed knowledge of the response of MAOM formation pathways to wetland restoration is lacking. Here, we collected 0-20 cm soil samples from two typical wetlands (meadow and peat wetlands) subjected to both grazing and restoration treatments (through micro dam construction) in the Zoige area.
View Article and Find Full Text PDFEnviron Sci Technol
December 2024
Key Laboratory of Agro-Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China.
Microbial carbon (C) use efficiency (CUE) drives soil C formation, while physical-chemical protection stabilizes subsequent microbial necromass, both shaped by soil aggregates and minerals. Soils inherit many properties from the parent material, yet the influence of lithology and associated soil geochemistry on microbial CUE and necromass stabilization remains unknow. Here, we quantified microbial CUE in well-aggregated bulk soils and crushed aggregates, as well as microbial necromass in bulk soils and the mineral-associated organic matter fraction, originating from carbonate-containing (karst) and carbonate-free (clastic rock, nonkarst) parent materials along a broad climatic gradient.
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