Microbial life in marine sediment contributes substantially to global biomass and is a crucial component of the Earth system. Subseafloor sediment includes both aerobic and anaerobic microbial ecosystems, which persist on very low fluxes of bioavailable energy over geologic time. However, the taxonomic diversity of the marine sedimentary microbial biome and the spatial distribution of that diversity have been poorly constrained on a global scale. We investigated 299 globally distributed sediment core samples from 40 different sites at depths of 0.1 to 678 m below the seafloor. We obtained ∼47 million 16S ribosomal RNA (rRNA) gene sequences using consistent clean subsampling and experimental procedures, which enabled accurate and unbiased comparison of all samples. Statistical analysis reveals significant correlations between taxonomic composition, sedimentary organic carbon concentration, and presence or absence of dissolved oxygen. Extrapolation with two fitted species–area relationship models indicates taxonomic richness in marine sediment to be 7.85 × 103 to 6.10 × 105 and 3.28 × 104 to 2.46 × 106 amplicon sequence variants for Archaea and Bacteria, respectively. This richness is comparable to the richness in topsoil and the richness in seawater, indicating that Bacteria are more diverse than Archaea in Earth’s global biosphere.

Bacterial endospores are dominant members of the marine deep biosphere.

Antifreeze proteins are structurally diverse polypeptides that have thermal hysteresis activity and have been discovered in many cold-adapted organisms. Of these, fungal antifreeze protein has been purified and partially characterized only in a species of psychrophilic basidiomycete, Typhula ishikariensis. Here we report a new fungal antifreeze protein from another psychrophile, Antarctomyces psychrotrophicus. We examined its biochemical properties and thermal hysteresis activity, and compared them with those of the T. ishikariensis antifreeze protein. The antifreeze protein from A. psychrotrophicus was purified and identified as an extracellular protein of approximately 28 kDa, which halved in size following digestion with glycosidase. The A. psychrotrophicus antifreeze protein generated bipyramidal ice crystals and exhibited thermal hysteresis activity (for example thermal hysteresis = 0.42 degrees C for a 0.48 mM solution) similar to that of fish antifreeze proteins, while a unique rugged pattern was created on the facets of the ice bipyramid. The thermal hysteresis activity of the A. psychrotrophicus antifreeze protein was maximized under alkaline conditions, while that of the T. ishikariensis antifreeze protein was greatest under acidic conditions. The T. ishikariensis antifreeze protein exhibited a bursting ice growth normal to the c-axis of the ice crystal and high thermal hysteresis activity (approximately 2 degrees C), as in the case of insect hyperactive antifreeze proteins. From these results, we speculate that the A. psychrotrophicus antifreeze protein is very different from the T. ishikariensis antifreeze protein, and that these two psychrophiles have evolved from different genes.

No abstract