Abstract

Substrate–atmosphere interfaces in Antarctic geothermal environments are hot–cold regions that constitute thin habitable niches for microorganisms with possible counterparts in ancient Mars. Cerro Caliente hill in Deception Island (active volcano in the South Shetland Islands) is affected by ascending hydrothermal fluids that form a band of warm substrates buffered by low air temperatures. We investigated the influence of temperature on the community structure and metabolism of three microbial mats collected along the geothermal band of Cerro Caliente registering 88°C, 8°C, and 2°C at the time of collection. High-throughput sequencing of small subunit ribosomal ribonucleic acid (SSU rRNA) genes and Life Detector Chip (LDChip) microarray immunoassays revealed different bacterial, archaeal, and eukaryotic composition in the three mats. The mat at 88°C showed the less diverse microbial community and a higher proportion of thermophiles (e.g., Thermales). In contrast, microbial communities in the mats at 2°C and 8°C showed relatively higher diversity and higher proportion of psychrophiles (e.g., Flavobacteriales). Despite this overall association, similar microbial structures at the phylum level (particularly the presence of Cyanobacteria) and certain hot- and cold-tolerant microorganisms were identified in the three mats. Daily thermal oscillations recorded in the substrate over the year (4.5–76°C) may explain the coexistence of microbial fingerprints with different thermal tolerances. Stable isotope composition also revealed metabolic differences among the microbial mats. Carbon isotopic ratios suggested the Calvin–Benson–Bassham cycle as the major pathway for carbon dioxide fixation in the mats at 2°C and 8°C, and the reductive tricarboxylic acid cycle and/or the 3-hydroxypropionate bicycle for the mat at 88°C, indicating different metabolisms as a function of the prevailing temperature of each mat. The comprehensive biomarker profile on the three microbial mats from Cerro Caliente contributes to unravel the diversity, composition, and metabolism in geothermal polar sites and highlights the relevance of geothermal-cold environments to create habitable niches with interest in other planetary environments.

Highlights

  • Geothermal polar environments represent extreme habitats for microbial communities in which thermal adaptation is crucial for their survival and growth (Vogt et al, 1997; Dutta and Chaudhuri, 2010; Reed et al, 2013)

  • The three microbial mats located in the geothermal summit of Cerro Caliente showed differences in their bacterial, archaeal, and eukaryotic community structures below the phylum level

  • Microbial mats from Cerro Caliente were assessed with a multianalytical approach to characterize their composition and major metabolisms under variable thermal conditions

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Summary

Introduction

Geothermal polar environments represent extreme habitats for microbial communities in which thermal adaptation is crucial for their survival and growth (Vogt et al, 1997; Dutta and Chaudhuri, 2010; Reed et al, 2013). Antarctica harbors a combination of glaciers and geothermal activity from which originate ice-free terrains due to underground magma heat (Herbold et al, 2014). These geothermal sites in Antarctica result into hotspots of diversity and, during past glaciations, had a relevant role as long-term refugia with favorable microclimate conditions for microorganisms and plants (Fraser et al, 2014). Geothermal environments are hypothesized to be one of the scenarios wherein the origin of life took place on Earth by providing the hydration/dehydration cycle conditions. Departments of 1Molecular Evolution and 2Planetology and Habitability, Centro de Astrobiologıa (CSIC-INTA), Madrid, Spain.

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