Research Keyword: soil carbon

Necromass of Diverse Root-Associated Fungi Suppresses Decomposition of Native Soil Carbon via Impacts of Their Traits

When fungi die in soil, their dead remains (necromass) affect how quickly the rest of the soil carbon breaks down. This study found that fungi with dark pigments and certain chemical compositions can actually slow down the decomposition of native soil carbon, helping more carbon stay stored in the soil longer. The researchers identified specific fungal traits like melanin content and growth rates that determine whether fungal remains promote or suppress carbon loss from soil.

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Contrasting stability of fungal and bacterial communities during long-term decomposition of fungal necromass in Arctic tundra

Scientists studied how dead fungal material breaks down in Arctic soil over three years. They found that melanized fungi, especially Pseudogymnoascus, are key decomposers that help break down tough fungal material containing melanin. While bacterial diversity increased over time, the fungal community remained relatively stable. Even after three years, about 20% of the fungal material remained undecomposed, suggesting it can help store carbon in Arctic soils.

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Warming and Reduced Rainfall Alter Fungal Necromass Decomposition Rates and Associated Microbial Community Composition and Functioning at a Temperate–Boreal Forest Ecotone

When soil gets warmer and drier due to climate change, dead fungal biomass breaks down faster at first but slower overall compared to normal conditions. The microorganisms that decompose this fungal material change their composition and abilities depending on how long the decomposition has been happening. This study shows that climate change affects soil carbon cycling in complex ways that depend on timing and environmental conditions.

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