Javascript must be enabled to continue!
Linking microbial genomes with their potential to degrade terrestrial organic matter in the Amazon River
View through CrossRef
Abstract
Rivers connect the carbon cycle in land with that in aquatic ecosystems by transporting and transforming terrestrial organic matter (TeOM). The Amazon River receives huge loads of TeOM from the surrounding rainforest, promoting a substantial microbial heterotrophic activity and consequently, CO2 outgassing. In the Amazon River, microbes degrade up to 55% of the lignin present in the TeOM. Yet, the main microbial genomes involved in TeOM degradation were not known. Here, we characterize 51 population genomes (PGs) representing some of the most abundant microbes in the Amazon River deriving from 106 metagenomes. The 51 reconstructed PGs are among the most abundant microbes in the Amazon River, and 53% of them are not able to degrade TeOM. Among the PGs capable of degrading TeOM, 20% were exclusively cellulolytic, while the others could also oxidize lignin. The transport and consumption of lignin oxidation byproducts seemed to be decoupled from the oxidation process, being apparently performed by different groups of microorganisms. Altogether, based on our findings, we suggest a new priming effect model that explains the quick turnover of TeOM as a product of the microbial consumption of lignin-derived aromatic compounds produced by lignin oxidation, reducing the inhibition of cellulose degradation and ensuring structural carbon and energy for cell growth. By connecting the genomic features of abundant microbes in the Amazon River with the degradation of recalcitrant TeOM, we contribute to increase our understanding of the rapid consumption of recalcitrant compounds in this ecosystem.
Springer Science and Business Media LLC
Title: Linking microbial genomes with their potential to degrade terrestrial organic matter in the Amazon River
Description:
Abstract
Rivers connect the carbon cycle in land with that in aquatic ecosystems by transporting and transforming terrestrial organic matter (TeOM).
The Amazon River receives huge loads of TeOM from the surrounding rainforest, promoting a substantial microbial heterotrophic activity and consequently, CO2 outgassing.
In the Amazon River, microbes degrade up to 55% of the lignin present in the TeOM.
Yet, the main microbial genomes involved in TeOM degradation were not known.
Here, we characterize 51 population genomes (PGs) representing some of the most abundant microbes in the Amazon River deriving from 106 metagenomes.
The 51 reconstructed PGs are among the most abundant microbes in the Amazon River, and 53% of them are not able to degrade TeOM.
Among the PGs capable of degrading TeOM, 20% were exclusively cellulolytic, while the others could also oxidize lignin.
The transport and consumption of lignin oxidation byproducts seemed to be decoupled from the oxidation process, being apparently performed by different groups of microorganisms.
Altogether, based on our findings, we suggest a new priming effect model that explains the quick turnover of TeOM as a product of the microbial consumption of lignin-derived aromatic compounds produced by lignin oxidation, reducing the inhibition of cellulose degradation and ensuring structural carbon and energy for cell growth.
By connecting the genomic features of abundant microbes in the Amazon River with the degradation of recalcitrant TeOM, we contribute to increase our understanding of the rapid consumption of recalcitrant compounds in this ecosystem.
Related Results
Degradation of terrestrial organic matter by aquatic microbial genomes in the Amazon River
Degradation of terrestrial organic matter by aquatic microbial genomes in the Amazon River
Abstract
Rivers connect the carbon cycle in land with that in aquatic ecosystems by transporting and transforming terrestrial organic matter (TeOM). The Amazon River receiv...
Flodfund - Bronzealderdeponeringer fra Gudenåen
Flodfund - Bronzealderdeponeringer fra Gudenåen
River findsBronze Age metalwork from the river GudenåBronze Age metalwork (primarily swords and other weapons) found in European rivers has aroused interest for many years, but lit...
Structure and Fractal Characteristics of Organic Matter Pores in Wufeng–Lower Longmaxi Formations in Southern Sichuan Basin, China
Structure and Fractal Characteristics of Organic Matter Pores in Wufeng–Lower Longmaxi Formations in Southern Sichuan Basin, China
Organic matter pores constitute a significant storage space in shale gas reservoirs, contributing to approximately 50% of the total porosity. This study employed a comprehensive ap...
Uncovering the gene machinery of the Amazon River microbiome to degrade rainforest organic matter
Uncovering the gene machinery of the Amazon River microbiome to degrade rainforest organic matter
Abstract
Background: The Amazon River is one of the largest in the world and receives huge amounts of terrestrial organic matter (TeOM) from the surrounding rainforest. Des...
Capacity of Arctic fjord sediments to degrade carbohydrates from permafrost active layer
Capacity of Arctic fjord sediments to degrade carbohydrates from permafrost active layer
ABSTRACT
The degradation of organic matter (OM) by microorganisms in thawing permafrost produces greenhouse gases. Terre...
GEOMORPHIC BOUNDARIES WITHIN RIVER NETWORKS
GEOMORPHIC BOUNDARIES WITHIN RIVER NETWORKS
Author contributions: MWS and MCT contributed equally to all aspects of
this research and manuscript preparation. Key Points 1. The physical
character of different functional proce...
Changes in soil organic matter quality during long-term bare fallow do not affect microaggregate stability
Changes in soil organic matter quality during long-term bare fallow do not affect microaggregate stability
Organic substances of diverse origins are known to promote the formation of microaggregates in soils. However, their contribution to the resistance of microaggregates against mecha...
Using radiocarbon to identify the impact of climate and mineralogy on soil organic matter turnover
Using radiocarbon to identify the impact of climate and mineralogy on soil organic matter turnover
Soils are the largest carbon (C) reservoir in terrestrial ecosystems. There are still numerous uncertainties concerning the fate of soil organic carbon and its feedback on climate ...

