Microbial assemblages in pressurized antarctic brine pockets (Tarn flat, northern Victoria land): A hotspot of biodiversity and activity

• Published in: Microorganisms
• Main Authors: Papale M., Lo Giudice A., Conte A., Rizzo C., Rappazzo A. C., Maimone G., Caruso G., La Ferla R., Azzaro M., Gugliandolo C., Paranhos R., Cabral A. S., Spica V. R., Guglielmin M.
• Other Authors: Papale, M., Lo Giudice, A., Conte, A., Rizzo, C., Rappazzo, A. C., Maimone, G., Caruso, G., La Ferla, R., Azzaro, M., Gugliandolo, C., Paranhos, R., Cabral, A. S., Spica, V. R., Guglielmin, M.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: Brine pocket; Hyperthermophile; Metabolic potential; Methanogen; Sulphur-reducing bacteria; Antarctic; Victoria Land; Ross Ice Shelf; Tarn Flat; Antarc*; Ice Shelf
• Online Access: https://hdl.handle.net/11383/2152831; https://doi.org/10.3390/microorganisms7090333

Two distinct pressurized hypersaline brine pockets (named TF4 and TF5), separated by a thin ice layer, were detected below an ice-sealed Antarctic lake. Prokaryotic (bacterial and archaeal) diversity, abundances (including virus-like particles) and metabolic profiles were investigated by an integrated approach, including traditional and new-generation methods. Although similar diversity indices were computed for both Bacteria and Archaea, distinct bacterial and archaeal assemblages were observed. Bacteroidetes and Gammaproteobacteria were more abundant in the shallowest brine pocket, TF4, and Deltaproteobacteria, mainly represented by versatile sulphate-reducing bacteria, dominated in the deepest, TF5. The detection of sulphate-reducing bacteria and methanogenic Archaea likely reflects the presence of a distinct synthrophic consortium in TF5. Surprisingly, members assigned to hyperthermophilic Crenarchaeota and Euryarchaeota were common to both brines, indicating that these cold habitats host the most thermally tolerant Archaea. The patterns of microbial communities were different, coherently with the observed microbiological diversity between TF4 and TF5 brines. Both the influence exerted by upward movement of saline brines from a sub-surface anoxic system and the possible occurrence of an ancient ice remnant from the Ross Ice Shelf were the likely main factors shaping the microbial communities.