Department of Molecular Evolution, Centro de Astrobiología (CSIC-INTA), Madrid, Spain.
Department of Planetology and Habitability, Centro de Astrobiología (CSIC-INTA), Madrid, Spain.
Astrobiology. 2019 Dec;19(12):1490-1504. doi: 10.1089/ast.2018.2004. Epub 2019 Jul 24.
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 (, ). In contrast, microbial communities in the mats at 2°C and 8°C showed relatively higher diversity and higher proportion of psychrophiles (, ). Despite this overall association, similar microbial structures at the phylum level (particularly the presence of ) 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.
南极地热环境中的基岩-大气界面是热-冷区域,为微生物提供了狭小的栖息地,这些微生物可能与古代火星上的微生物有对应关系。欺骗岛(南设得兰群岛上的活火山)的卡尔旺特山(Cerro Caliente)受到上升热液的影响,形成了一条温暖基岩带,周围的空气温度较低。我们调查了温度对从卡尔旺特山地热带采集的三个微生物垫的群落结构和代谢的影响,这三个微生物垫的温度分别为 88°C、8°C 和 2°C。对小亚基核糖体核糖核酸(SSU rRNA)基因和生命探测芯片(LDChip)微阵列免疫测定的高通量测序显示,三个垫子中的细菌、古菌和真核生物组成不同。88°C 处的垫子显示出微生物群落的多样性较低,嗜热菌的比例较高(,)。相比之下,2°C 和 8°C 垫子中的微生物群落具有相对较高的多样性和较高的嗜冷菌比例(,)。尽管存在这种总体关联,但在三个垫子中仍然可以识别出在门水平上相似的微生物结构(特别是存在)和某些耐热和耐寒微生物。一年中在基岩中记录的每日热振荡(4.5-76°C)可以解释不同热容忍度的微生物指纹的共存。稳定同位素组成也揭示了微生物垫之间的代谢差异。碳同位素比值表明,2°C 和 8°C 垫子中的二氧化碳固定主要途径是卡尔文-本森-巴斯汉姆循环,而 88°C 垫子中的主要途径是还原三羧酸循环和/或 3-羟基丙酸循环,这表明不同的代谢方式与每个垫子的主要温度有关。卡尔旺特山三个微生物垫的综合生物标志物谱有助于揭示地热极区的多样性、组成和代谢,并强调了地热-冷环境在创造宜居小生境方面的重要性,这在其他行星环境中也具有重要意义。