Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil

Abstract Microbial decomposition drives the transformation of plant-derived substrates into microbial products that form stable soil organic matter (SOM). Recent theories have posited that decomposition depends on an interaction between SOM chemistry with microbial diversity and resulting function (...

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Autores principales: Nanette C. Raczka, Juan Piñeiro, Malak M. Tfaily, Rosalie K. Chu, Mary S. Lipton, Ljiljana Pasa-Tolic, Ember Morrissey, Edward Brzostek
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/3b54716e1a65496a9f21c0fc69bde5b1
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spelling oai:doaj.org-article:3b54716e1a65496a9f21c0fc69bde5b12021-12-02T17:37:40ZInteractions between microbial diversity and substrate chemistry determine the fate of carbon in soil10.1038/s41598-021-97942-92045-2322https://doaj.org/article/3b54716e1a65496a9f21c0fc69bde5b12021-09-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-97942-9https://doaj.org/toc/2045-2322Abstract Microbial decomposition drives the transformation of plant-derived substrates into microbial products that form stable soil organic matter (SOM). Recent theories have posited that decomposition depends on an interaction between SOM chemistry with microbial diversity and resulting function (e.g., enzymatic capabilities, growth rates). Here, we explicitly test these theories by coupling quantitative stable isotope probing and metabolomics to track the fate of 13C enriched substrates that vary in chemical composition as they are assimilated by microbes and transformed into new metabolic products in soil. We found that differences in forest nutrient economies (e.g., nutrient cycling, microbial competition) led to arbuscular mycorrhizal (AM) soils harboring greater diversity of fungi and bacteria than ectomycorrhizal (ECM) soils. When incubated with 13C enriched substrates, substrate type drove shifts in which species were active decomposers and the abundance of metabolic products that were reduced or saturated in the highly diverse AM soils. The decomposition pathways were more static in the less diverse, ECM soil. Importantly, the majority of these shifts were driven by taxa only present in the AM soil suggesting a strong link between microbial identity and their ability to decompose and assimilate substrates. Collectively, these results highlight an important interaction between ecosystem-level processes and microbial diversity; whereby the identity and function of active decomposers impacts the composition of decomposition products that can form stable SOM.Nanette C. RaczkaJuan PiñeiroMalak M. TfailyRosalie K. ChuMary S. LiptonLjiljana Pasa-TolicEmber MorrisseyEdward BrzostekNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-10 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Nanette C. Raczka
Juan Piñeiro
Malak M. Tfaily
Rosalie K. Chu
Mary S. Lipton
Ljiljana Pasa-Tolic
Ember Morrissey
Edward Brzostek
Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
description Abstract Microbial decomposition drives the transformation of plant-derived substrates into microbial products that form stable soil organic matter (SOM). Recent theories have posited that decomposition depends on an interaction between SOM chemistry with microbial diversity and resulting function (e.g., enzymatic capabilities, growth rates). Here, we explicitly test these theories by coupling quantitative stable isotope probing and metabolomics to track the fate of 13C enriched substrates that vary in chemical composition as they are assimilated by microbes and transformed into new metabolic products in soil. We found that differences in forest nutrient economies (e.g., nutrient cycling, microbial competition) led to arbuscular mycorrhizal (AM) soils harboring greater diversity of fungi and bacteria than ectomycorrhizal (ECM) soils. When incubated with 13C enriched substrates, substrate type drove shifts in which species were active decomposers and the abundance of metabolic products that were reduced or saturated in the highly diverse AM soils. The decomposition pathways were more static in the less diverse, ECM soil. Importantly, the majority of these shifts were driven by taxa only present in the AM soil suggesting a strong link between microbial identity and their ability to decompose and assimilate substrates. Collectively, these results highlight an important interaction between ecosystem-level processes and microbial diversity; whereby the identity and function of active decomposers impacts the composition of decomposition products that can form stable SOM.
format article
author Nanette C. Raczka
Juan Piñeiro
Malak M. Tfaily
Rosalie K. Chu
Mary S. Lipton
Ljiljana Pasa-Tolic
Ember Morrissey
Edward Brzostek
author_facet Nanette C. Raczka
Juan Piñeiro
Malak M. Tfaily
Rosalie K. Chu
Mary S. Lipton
Ljiljana Pasa-Tolic
Ember Morrissey
Edward Brzostek
author_sort Nanette C. Raczka
title Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
title_short Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
title_full Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
title_fullStr Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
title_full_unstemmed Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
title_sort interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/3b54716e1a65496a9f21c0fc69bde5b1
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