Volcanos are charismatic conduits of Earth's deep carbon, and contribute to gas emissions during eruption episodes and diffuse degassing. Diffuse degassing is a key feature of volcanoes, yet its relationship to volcanic activity is unclear. Epiard et al. show diffuse degassing represents up to 10% of the total CO₂ volcanic output, and find evidence for a shift in the patterns of degassing in the lead-up to eruptions. In a related contribution, Viveiros et al. highlight the pathways that CO₂ takes to reach the surface, and show diffuse degassing is concentrated along volcanic-tectonic structures rather than in the vicinity of the youngest volcanic edifices.

Carbonates have been proposed as the principal oxidized carbon-bearing phases in the Earth's interior. Boulard et al. investigated the behavior of MnCO₃ at high temperature and pressure and report a phase transition from MnCO₃ into MnCO₃-II without an accompanying change in the manganese oxidation state until temperatures reached 1,400 K leading to the formation of manganese oxides and reduced carbon.

C-O-H volatiles are important throughout the lithosphere and are commonly found confined in pores, grain boundaries, and fractures. Gautam et al. present a systematic review of the use of nuclear magnetic resonance (NMR), neutron scattering (NS), and molecular dynamics (MD) simulations to show how application of these three techniques has shed light on the complex behavior of water, CO₂, and C-O-H volatiles.

In situ sequestration of CO₂ in mantle peridotites has been proposed as a method to alleviate the amount of anthropogenic CO₂ in the atmosphere. Lacinska et al. indicate a rate of carbonation of ~2% in half a year, using natural ophiolites, suggesting that serpentinite might be a good host rock for CO₂ sequestration.

Microbial communities in deep subsurface environments comprise a significant portion of Earth's biomass, but the microbial activity in these habitats is largely unknown. Hoarfrost et al. present a new fluorescent method to measure extracellular enzymatic activities. The method improves recovery of the labeled substrate from sediment subsamples resulting in greater reliability of quantifying microbially catalyzed hydrolytic activities in sediments.

Yucel et al. show sediment sulfide accumulation is moderated by microbial oxidation at the sediment surface and FeS precipitation in deeper sediment layers, Microorganisms rely on electron flow to drive metabolism and biogeochemical cycles. Taran uses cyclic voltammetry to show that quinone, a microbially produced electron shuttle, interacts and exchanges electrons with pyrite thereby creating a cycle. Using mesocosm incubations, Rajala and Bomberg show rapid microbial response to methane and methanol amendments from two isolated groundwater fractures at 180 m and 500 m depths of the Outokumpu Deep Drill hole (Finland). Purkamo et al. used acetate to stimulate microbial community diversity and show treatments dominated by clostridial hydrogenotrophic thiosulfate reducers in fluids obtained from the same Outokumpu Deep Drill hole. Nixon et al. show guar gum stimulates biogenic sulfide production by sulfate-reducing microorganisms at elevated pressure. Their results have implications for the potential role in microbially induced corrosion during hydraulic fracturing operations.

Serpentinization is of particular interest for deep carbon science, as alteration of ultramafic rocks produce abundant reductants (H₂ and CH₄) that fuel life and sequester significant quantities of carbon. In a groundbreaking interdisciplinary study, Twing et al. show the Coast Range Ophiolite Microbial Observatory serpentinites are low in microbial diversity and dominated by members of the Betaproteobacteria and Clostridia, involved in hydrogen metabolism, carbon monoxide oxidation, carbon fixation, and acetogenesis. Crespo-Medina et al. report the Santa Elena Ophiolite communities are dominated by hydrogen, methane, and methanol oxidizers of the bacterial genera Hydrogenophaga, Methylobacterium, and Methylibium as well as methanogenic Archaea.

Changes in the carbon cycle through deep time have astrobiological implications. Brandano et al. show the importance of understanding the role of the slow carbon cycle through deep time using extant data of seagrass productivity along the Mediterranean Sea and integrating GPlate models. Azua-Bustos et al. present a compelling case for the study of the physiological and molecular mechanisms utilized by heterotrophic microorganisms to detect, mobilize, incorporate, and use carbon under extremely harsh conditions in the Atacama Desert in Chile with astrobiological significance.

Building a large community of interdisciplinary scientists focused on studying the different aspects of deep carbon science requires also creating a supporting infrastructure to foster community growth and facilitate information exchange. Ma et al. describe how the DCO has leveraged state of the art information technologies to establish a knowledge network, which promotes collaboration, reproducibility, accreditation, and stimulates new ideas across deep carbon related studies.

DG, BB, AC, and CS have all equally contributed to this editorial.