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The production and turnover of extramatrical mycelium of ectomycorrhizal fungi in forest soils: role in carbon cycling

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TLDR
There is increasing evidence that residues of EM fungi play a major role in the formation of stable N and C in SOM, which highlights the need to include mycorrhizal effects in models of global soil C stores.
Abstract
There is growing evidence of the importance of extramatrical mycelium (EMM) of mycorrhizal fungi in carbon (C) cycling in ecosystems. However, our understanding has until recently been mainly based on laboratory experiments, and knowledge of such basic parameters as variations in mycelial production, standing biomass and turnover as well as the regulatory mechanisms behind such variations in forest soils is limited. Presently, the production of EMM by ectomycorrhizal (EM) fungi has been estimated at similar to 140 different forest sites to be up to several hundreds of kg per ha per year, but the published data are biased towards Picea abies in Scandinavia. Little is known about the standing biomass and turnover of EMM in other systems, and its influence on the C stored or lost from soils. Here, focussing on ectomycorrhizas, we discuss the factors that regulate the production and turnover of EMM and its role in soil C dynamics, identifying important gaps in this knowledge. C availability seems to be the key factor determining EMM production and possibly its standing biomass in forests but direct effects of mineral nutrient availability on the EMM can be important. There is great uncertainty about the rate of turnover of EMM. There is increasing evidence that residues of EM fungi play a major role in the formation of stable N and C in SOM, which highlights the need to include mycorrhizal effects in models of global soil C stores.

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Quantitative assessment of microbial necromass contribution to soil organic matter.

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The impact of climate change and anthropogenic activities on alpine grassland over the Qinghai-Tibet Plateau

TL;DR: In this article, the authors used process-based terrestrial ecosystem model to stimulate the potential climate-driven alpine grassland net primary production (NPP), and Carnegie-Ames-Stanford Approach based on remote sensing to stimulate actual grassland NPP influenced by both of climate change and anthropogenic activities over the Qinghai-Tibet plateau (QTP) from 1982 to 2011.
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Carbon sequestration is related to mycorrhizal fungal community shifts during long-term succession in boreal forests.

TL;DR: It is postulate that, by affecting turnover and decomposition of fungal tissues, mycorrhizal fungal identity and growth form are critical determinants of C and N sequestration in boreal forests.
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Forest microbiome: diversity, complexity and dynamics

TL;DR: The understanding of these processes can be only achieved by the exploration of the complex 'ecosystem microbiome' and its functioning using focused, integrative microbiological and ecological research performed across multiple habitats.
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Forest Soil Bacteria: Diversity, Involvement in Ecosystem Processes, and Response to Global Change

TL;DR: Bacteria contribute to a range of essential soil processes involved in the cycling of carbon, nitrogen, and phosphorus, and mediate multiple critical steps in the nitrogen cycle, including N fixation.
References
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Journal ArticleDOI

On Optimal Use of a Patchy Environment

TL;DR: A graphical method is discussed which allows a specification of the optimal diet of a predator in terms of the net amount of energy gained from a capture of prey as compared to the energy expended in searching for the prey.
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Mycorrhizal fungal diversity determines plant biodiversity, ecosystem variability and productivity

TL;DR: It is shown that below-ground diversity of arbuscular mycorrhizal fungi (AMF) is a major factor contributing to the maintenance of plant biodiversity and to ecosystem functioning, and that microbial interactions can drive ecosystem functions such as plant biodiversity, productivity and variability.
Journal ArticleDOI

Review of mechanisms and quantification of priming effects.

TL;DR: In this paper, the authors reveal possible causes and processes leading to priming actions using the references on agricultural ecosystems and model experiments, and summarize in Tables for positive and negative real and apparent priming effects induced after the addition of different organic and mineral substances to the soil.
Journal ArticleDOI

Controls on the dynamics of dissolved organic matter in soils: a review.

TL;DR: In this article, the authors summarize the recent literature about controls on dissolved organic matter (DOM) concentrations and fluxes in so-called "soil degraded organic matter" (SOCOM).
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