Coronavirus Information for the UC San Diego Community

Our leaders are working closely with federal and state officials to ensure your ongoing safety at the university. Stay up to date with the latest developments. Learn more.

Recycling and metabolic flexibility dictate life in the lower oceanic crust

TitleRecycling and metabolic flexibility dictate life in the lower oceanic crust
Publication TypeJournal Article
Year of Publication2020
AuthorsLi J.T, Mara P., Schubotz F., Sylvan J.B, Burgaud G., Klein F., Beaudoin D., Wee S.Y, Dick H.JB, Lott S., Cox R., Meyer L.AE, Quemener M., Blackman D.K, Edgcomb V.P
Volume579
Pagination250-+
Date Published2020/03
Type of ArticleArticle
ISBN Number0028-0836
Accession NumberWOS:000519378900026
Keywordsbacteria; biomass; community; contamination; database; elemental organic-analysis; fluids; insights; mass-spectrometry; Science & Technology - Other Topics; sequence
Abstract

The lithified lower oceanic crust is one of Earth's last biological frontiers as it is difficult to access. It is challenging for microbiota that live in marine subsurface sediments or igneous basement to obtain sufficient carbon resources and energy to support growth(1-3) or to meet basal power requirements(4) during periods of resource scarcity. Here we show how limited and unpredictable sources of carbon and energy dictate survival strategies used by low-biomass microbial communities that live 10-750 m below the seafloor at Atlantis Bank, Indian Ocean, where Earth's lower crust is exposed at the seafloor. Assays of enzyme activities, lipid biomarkers, marker genes and microscopy indicate heterogeneously distributed and viable biomass with ultralow cell densities (fewer than 2,000 cells per cm(3)). Expression of genes involved in unexpected heterotrophic processes includes those with a role in the degradation of polyaromatic hydrocarbons, use of polyhydroxyalkanoates as carbon-storage molecules and recycling of amino acids to produce compounds that can participate in redox reactions and energy production. Our study provides insights into how microorganisms in the plutonic crust are able to survive within fractures or porous substrates by coupling sources of energy to organic and inorganic carbon resources that are probably delivered through the circulation of subseafloor fluids or seawater.

DOI10.1038/s41586-020-2075-5
Student Publication: 
No
sharknado