Le Jeune, A.-H. | Search bioRxiv

bioRxiv2025

Non-living respiration: another breath in the soil?

The present study challenges the traditional view that respiration of organic carbon to CO2 is exclusively an intracellular process, revealing that organic compound respiration can occur spontaneously in an extracellular context in soils. Using 1H nuclear magnetic resonance spectroscopy to analyse the dynamics of the sterile soil exometabolomes alongside C-CO2 flux analyses and sterile soil fuel cells, we show that soil catalysts facilitate a diverse array of substrate-driven reactions, leading to the complete oxidation of organic compounds to CO2 with O2 consumption. Our results indicate that soil particles are capable of transferring electrons from substrates to the final acceptor, sustaining metabolic processes independently of living cells. Notably, some soil catalysts and induced respiration remain stable for over six years. Our results support the coexistence of cellular and non-cellular metabolic pathways in soil respiration.

ecology↗

bioRxiv2022

Variable impact of geochemical gradients on the functional potential of bacteria, archaea, and phages from the permanently stratified Lac Pavin

Permanently stratified lakes contain diverse microbial communities that vary with depth, and so serve as useful models for studying the relationships between microbial community structure and geochemistry. Recent work has shown that these lakes can also harbor numerous bacteria and archaea from novel lineages, including those from the Candidate Phyla Radiation (CPR). However, the extent to which geochemical stratification differentially impacts carbon metabolism and overall genetic potential in CPR bacteria compared to other organisms is not well defined. Here, we determine the distribution of microbial lineages along an oxygen gradient in Lac Pavin, a deep, stratified lake in central France, and examine the influence of this gradient on their metabolism. Genome-based analyses revealed an enrichment of distinct C1 and CO2 fixation pathways in the oxic lake interface and anoxic zone/sediments, suggesting that oxygen likely plays a role in structuring metabolic strategies in non-CPR bacteria and archaea. Notably, we find that oxidation of methane and its byproducts is largely spatially separated from methane production, which is mediated by diverse communities of sediment methanogens that vary on the centimeter scale. In contrast, we detected evidence for RuBisCO throughout the water column and sediments, including form II/III and form III-related enzymes encoded by CPR bacteria in the water column and DPANN archaea in the sediments. Overall, CPR bacteria and phages did not show strong signals of gene content differentiation by depth, despite the fact that distinct species groups populate different lake and sediment compartments. Thus, environmental gradients in Lac Pavin probably select for the capacities of CPR bacteria and phages to a lesser extent than other bacteria and archaea, possibly because selection on the former groups is indirect and depends on host characteristics.

microbiology↗