Abstract:The Sahara Desert is characterized by extreme environmental conditions, which are a unique challenge for life. Cyanobacteria are key players in the colonization of bare soils and form assemblages with other microorganisms in the top millimetres, establishing biological soil crusts (biocrusts) that cover most soil surfaces in deserts, which have important roles in the functioning of drylands. However, knowledge of biocrusts from these extreme environments is limited. Therefore, to study cyanobacterial community… Show more
“…The 16S rRNA gene of cyanobacteria was amplified with the specific primer pairs CYA359F/CYA781Ra and CYA781Rb ( Nübel et al, 1997 ) in separate reactions. These specific cyanobacterial primers are widely used to identify cyanobacteria in different environments (e.g., Dorador et al, 2008 ; Azúa-Bustos et al, 2011 ; Mehda et al, 2021 ). Further information about the PCR conditions is available in the Supplementary Text 2 .…”
Hydrothermal systems and their deposits are primary targets in the search for fossil evidence of life beyond Earth. However, to learn how to decode fossil biomarker records in ancient hydrothermal deposits, we must first be able to interpret unambiguously modern biosignatures, their distribution patterns, and their association with physicochemical factors. Here, we investigated the molecular and isotopic profile of microbial biomarkers along a thermal gradient (from 29 to 72°C) in a hot spring (labeled Cacao) from El Tatio, a geyser field in the Chilean Andes with abundant opaline silica deposits resembling the nodular and digitate structures discovered on Mars. As a molecular forensic approach, we focused on the analysis of lipid compounds bearing recognized resistance to degradation and the potential to reconstruct the paleobiology of an environment on a broader temporal scale than other, more labile, biomolecules. By exploiting the lipid biomarkers’ potential to diagnose biological sources and carbon fixation pathways, we reconstructed the microbial community structure and its ecology along the Cacao hydrothermal transect. The taxonomic adscription of the lipid biomarkers was qualitatively corroborated with DNA sequencing analysis. The forensic capacity of the lipid biomarkers to identify biosources in fresh biofilms was validated down to the genus level for Roseiflexus, Chloroflexus, and Fischerella. We identified lipid biomarkers and DNA of several new cyanobacterial species in El Tatio and reported the first detection of Fischerella biomarkers at a temperature as high as 72°C. This, together with ecological peculiarities and the proportion of clades being characterized as unclassified, illustrates the ecological singularity of El Tatio and strengthens its astrobiological relevance. The Cacao hydrothermal ecosystem was defined by a succession of microbial communities and metabolic traits associated with a high- (72°C) to low-(29°C) temperature gradient that resembled the inferred metabolic sequence events from the 16S rRNA gene universal phylogenetic tree from thermophilic to anoxygenic photosynthetic species and oxygenic phototrophs. The locally calibrated DNA-validated lipidic profile in the Cacao biofilms provided a modern (molecular and isotopic) end member to facilitate the recognition of past biosources and metabolisms from altered biomarkers records in ancient silica deposits at El Tatio analogous to Martian opaline silica structures.
“…The 16S rRNA gene of cyanobacteria was amplified with the specific primer pairs CYA359F/CYA781Ra and CYA781Rb ( Nübel et al, 1997 ) in separate reactions. These specific cyanobacterial primers are widely used to identify cyanobacteria in different environments (e.g., Dorador et al, 2008 ; Azúa-Bustos et al, 2011 ; Mehda et al, 2021 ). Further information about the PCR conditions is available in the Supplementary Text 2 .…”
Hydrothermal systems and their deposits are primary targets in the search for fossil evidence of life beyond Earth. However, to learn how to decode fossil biomarker records in ancient hydrothermal deposits, we must first be able to interpret unambiguously modern biosignatures, their distribution patterns, and their association with physicochemical factors. Here, we investigated the molecular and isotopic profile of microbial biomarkers along a thermal gradient (from 29 to 72°C) in a hot spring (labeled Cacao) from El Tatio, a geyser field in the Chilean Andes with abundant opaline silica deposits resembling the nodular and digitate structures discovered on Mars. As a molecular forensic approach, we focused on the analysis of lipid compounds bearing recognized resistance to degradation and the potential to reconstruct the paleobiology of an environment on a broader temporal scale than other, more labile, biomolecules. By exploiting the lipid biomarkers’ potential to diagnose biological sources and carbon fixation pathways, we reconstructed the microbial community structure and its ecology along the Cacao hydrothermal transect. The taxonomic adscription of the lipid biomarkers was qualitatively corroborated with DNA sequencing analysis. The forensic capacity of the lipid biomarkers to identify biosources in fresh biofilms was validated down to the genus level for Roseiflexus, Chloroflexus, and Fischerella. We identified lipid biomarkers and DNA of several new cyanobacterial species in El Tatio and reported the first detection of Fischerella biomarkers at a temperature as high as 72°C. This, together with ecological peculiarities and the proportion of clades being characterized as unclassified, illustrates the ecological singularity of El Tatio and strengthens its astrobiological relevance. The Cacao hydrothermal ecosystem was defined by a succession of microbial communities and metabolic traits associated with a high- (72°C) to low-(29°C) temperature gradient that resembled the inferred metabolic sequence events from the 16S rRNA gene universal phylogenetic tree from thermophilic to anoxygenic photosynthetic species and oxygenic phototrophs. The locally calibrated DNA-validated lipidic profile in the Cacao biofilms provided a modern (molecular and isotopic) end member to facilitate the recognition of past biosources and metabolisms from altered biomarkers records in ancient silica deposits at El Tatio analogous to Martian opaline silica structures.
“…Los estudios centrados en abordar la problemática global de la degradación de los suelos se han enfrentado a que hoy en día muchos aspectos continúan desconocidos en lo que se ref iere al estudio y aprovechamiento de las comunidades microbianas de la biocostra, su diversidad aún resulta desconocida o se encuentra mal caracterizada, por lo que la identif icación y el seguimiento de las funciones que desempeñan los organismos que habitan la biocostra son los primeros pasos a considerarse (Mehda et al, 2021). En este sentido, el conocimiento del microbioma de las biocostras, sobre todo de aquellas de regiones geográf icas poco exploradas con condiciones ambientales extremas contribuye a la caracterización integral para la elaboración de propuestas que impacten en la restauración de los suelos degradados por procesos naturales y humanos (Giraldo-Silva, Nelson, Barger y Garcia, 2019).…”
Section: Metagenómicaunclassified
“…Algunas de las funciones reportadas de estos microorganismos en las biocostras destacan sus estrategias de supervivencia a condiciones de desecación y radiación UV a través de la producción de enzimas y diversas moléculas implicadas en el mantenimiento y reparación celular, las cuales han sido reportadas gracias al desarrollo de las tecnologías ómicas (Wase et al, 2014;Shang et al, 2019). De igual forma, se realizó un estudio en el desierto del Sahara en el que se logró el aislamiento e identif icación morfológica y metagenómica de miembros que han sido encontrados en biocostras de diferentes localidades geográf icas (Microcoleus steenstrupii, Microcoleus vaginatus, Scytonema hyalinum, Tolypothrix distorta, Calothrix sp., entre otros); sin embargo, además de la identif icación, se realizó una evaluación de la resistencia al calor extremo y a la desecación, encontrando que la mayoría de las especies resisten temperaturas elevadas, y que además especies como S. hyalinum, M. steenstrupii, Pseudophormidium sp., N. commune y Nodosilinea muestran una resiliencia después de una etapa de rehidratación, lo que los convierte en candidatos potenciales para su evaluación in vivo como una alternativa de inoculación para evitar la degradación de los suelos (Mehda et al, 2021).…”
Las tecnologías “ómicas” son herramientas novedosas que facilitan el estudio de las comunidades microbianas de distintos ecosistemas, particularmente de la costra biológica del suelo, también llamada biocostra. Entre estas tecnologías se encuentran la genómica, transcriptómica, proteómica, metabolómica y metagenómica, que son utilizadas para analizar la diversidad y las funciones que llevan a cabo los microorganismos a través del estudio de sus biomoléculas y vías metabólicas. Entre los microorganismos que habitan la biocostra destacan las cianobacterias, las cuales son un grupo de bacterias fototróficas encargadas de realizar procesos importantes en el suelo, tal como la fijación de nitrógeno atmosférico, carbono orgánico, síntesis de clorofila y ficobilinas, así como la producción de exopolisacáridos para mejorar la estabilidad y fertilidad del suelo. Por lo tanto, el objetivo de la presente revisión es el de explorar la diversidad y la función que desempeñan estas comunidades microbianas en la biocostra, particularmente las cianobacterias, destacando los estudios realizados mediante el uso de las tecnologías ómicas. El conocimiento generado en los últimos años a través de las tecnologías ómicas ha demostrado la limitada cobertura que presentan las técnicas moleculares tradicionales, resultando en una subestimación de la diversidad real de las comunidades microbianas. Además, se ha mejorado la comprensión de los procesos ecológicos desarrollados por los microorganismos en beneficio de la biocostra, así como las capacidades funcionales individuales y colectivas, las cuales servirán como línea base para proponer estrategias importantes que solucionen la problemática de la degradación de los suelos.
“…On the other hand, many cyanobacteria species form heterocysts, the cells that carry out atmospheric nitrogen fixation, especially during nitrogen deprivation [33]. This uniquely differentiated cell results in the dispersion of cyanobacterial genera in various ecosystems; for example, Anabaena and Trichodesmium inhabit open oceans, thermal springs and freshwaters [34,35], whereas Leptolynbya grows in geothermal springs, hot deserts, and surface crusts of semideserts [36,37].…”
Section: Physiological Adaptationmentioning
confidence: 99%
“…Noteworthy, most filamentous cyanobacteria produce extracellular sheath as a method of adaptation, especially to water level fluctuation and high solute concentration, by providing a microenvironment for trichomes. For example, Microcoleus, Trichocoleus, Oscillatoria and some Schizothrix covered by thick sheath grow in saline soil crusts, semidesert regions, soil crusts of desert and polar environments [35,55,56]. However, some mat-forming Schizothrix and Oscillatoria enveloped by firm and thin sheaths inhabit diverse aquatic environments, freshwater, marine environments, thermal springs and polar water bodies [55].…”
Cyanobacteria are the most abundant oxygenic photosynthetic organisms inhabiting various ecosystems on earth. As with all other photosynthetic organisms, cyanobacteria release oxygen as a byproduct during photosynthesis. In fact, some cyanobacterial species are involved in the global nitrogen cycles by fixing atmospheric nitrogen. Environmental factors influence the dynamic, physiological characteristics, and metabolic profiles of cyanobacteria, which results in their great adaptation ability to survive in diverse ecosystems. The evolution of these primitive bacteria resulted from the unique settings of photosynthetic machineries and the production of bioactive compounds. Specifically, bioactive compounds play roles as regulators to provide protection against extrinsic factors and act as intracellular signaling molecules to promote colonization. In addition to the roles of bioactive metabolites as indole alkaloids, terpenoids, mycosporine-like amino acids, non-ribosomal peptides, polyketides, ribosomal peptides, phenolic acid, flavonoids, vitamins, and antimetabolites for cyanobacterial survival in numerous habitats, which is the focus of this review, the bioactivities of these compounds for the treatment of various diseases are also discussed.
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