scholarly journals Cyanobacterial Diversity in Microbial Mats from the Hypersaline Lagoon System of Araruama, Brazil: An In-depth Polyphasic Study

2017 ◽  
Vol 8 ◽  
Author(s):  
Vitor M. C. Ramos ◽  
Raquel Castelo-Branco ◽  
Pedro N. Leão ◽  
Joana Martins ◽  
Sinda Carvalhal-Gomes ◽  
...  
2021 ◽  
Vol 8 ◽  
Author(s):  
Juline Marta Walter ◽  
Louisi Souza de Oliveira ◽  
Diogo Antonio Tschoeke ◽  
Pedro Milet Meirelles ◽  
Maria Helena Campos Baeta Neves ◽  
...  

The hypersaline lagoon system of Araruama (HLSA) is one of the largest in the world and one of the most important sources of evaporative salt in Brazil. The biogeochemical characteristics of this lagoon system led it to be considered a Precambrian relic. The HLSA also harbors extensive microbial mats, but the taxonomic and metabolic attributes of these mats are poorly understood. Our high-throughput metagenomics analyses demonstrated that the HLSA microbial mats are dominated by Proteobacteria, Cyanobacteria, and Bacteroidetes. Among Proteobacteria, Deltaproteobacteria comprises approximately 40% of the total population and it includes sulfate-reducing bacteria such as Desulfobacterales, Desulfuromonadales, and Desulfovibrionales. Differing in composition and function of their reaction centers, other phylogenetic diverse anoxygenic phototrophic bacteria were detected in the HLSA microbial mats metagenomes. The presence of photolithoautotrophs, sulfate reducers, sulfide oxidizers, and aerobic heterotrophs suggests the existence of numerous cooperative niches that are coupled and regulated by microbial interactions. We suggest that the HLSA microbial mats hold microorganisms and the necessary machinery (genomic repertoire to sustain metabolic pathways) to promote favorable conditions (i.e., create an alkaline pH microenvironment) for microbially mediated calcium carbonate precipitation process. Metagenome-assembled genomes (Ca. Thiohalocapsa araruaensis HLSAbin6 sp. nov. and Ca. Araruabacter turfae HLSAbin9 gen. nov. sp. nov.) obtained support the relevance of Sulfur metabolism and they are enriched with genes involved in the osmoadaptive networks, hinting at possible strategies to withstand osmotic stress. Metabolically versatile bacteria populations, able to use multiple nutrient sources and osmolytes, seem to be a relevant attribute to survive under such stressful conditions.


2008 ◽  
Vol 65 (3) ◽  
pp. 449-462 ◽  
Author(s):  
Raeid M.M. Abed ◽  
Katharina Kohls ◽  
Raphaela Schoon ◽  
Ann-Kathrin Scherf ◽  
Marion Schacht ◽  
...  

2020 ◽  
Vol 90 (8) ◽  
pp. 887-905
Author(s):  
Carolina N. Keim ◽  
Hélisson Nascimento dos Santos ◽  
Carolina Souza Santiago ◽  
Simone Pennafirme ◽  
Reiner Neumann ◽  
...  

ABSTRACT Stromatolites are domes, columns, or nearly flat crusts of laminated sedimentary rocks, usually consisting of Ca-Mg carbonates. Stromatolites result from lithification of microbial mats, which are benthic microbial ecosystems where microorganisms arrange themselves in layers according to their physiology. Despite a century of research, the hypothesis of stromatolite genesis by lithification of microbial mats remains controversial, and a convincing explanation for how stromatolites arise from microbial mats is still lacking. In this work, we analyze in detail a stromatolite from Lagoa Vermelha, a coastal hypersaline lagoon in Rio de Janeiro State, Brazil. The stromatolite presents a laminated core and thrombolitic regions at the periphery. Both thrombolitic and laminated facies consist of fine-grained authigenic minerals with minor contributions of bioclasts and quartz grains. X-ray diffraction shows aragonite, high-magnesium calcite (HMC) containing about 17% MgCO3, a very-high-Mg calcite (VHMC) containing 29–46% MgCO3, and small amounts of quartz and pyrite. Scanning electron microscopy of polished samples coupled to energy-dispersive X-ray analysis (EDS) showed that each lamina was composed of 1–4 distinct mineral phases embedded within each other, indicating sequential steps of precipitation of Ca-Mg carbonates under distinct biogeochemical conditions. The coexistence of different phases in a single lamina suggests that several processes contribute to mineral deposition as the incipient stromatolite laminae are left behind by microorganisms from the lower layers of the microbial mat when they grow and/or move upwards.


Ophelia ◽  
2004 ◽  
Vol 58 (3) ◽  
pp. 151-156 ◽  
Author(s):  
Elia Diestra ◽  
Antonio Solé ◽  
Isabel Esteve

2019 ◽  
Vol 31 ◽  
pp. 100769 ◽  
Author(s):  
S. Pennafirme ◽  
D.C. Pereira ◽  
L.G.M. Pedrosa ◽  
A.S. Machado ◽  
G.O.A. Silva ◽  
...  

Geology ◽  
2004 ◽  
Vol 32 (8) ◽  
pp. 701 ◽  
Author(s):  
Naila F. Moreira ◽  
Lynn M. Walter ◽  
Crisogono Vasconcelos ◽  
Judith A. McKenzie ◽  
Patti J. McCall

2017 ◽  
Vol 284 (1857) ◽  
pp. 20170833 ◽  
Author(s):  
Anne D. Jungblut ◽  
Ian Hawes

Evidence of climate-driven environmental change is increasing in Antarctica, and with it comes concern that this will propagate to impacts on biological communities. Recognition and prediction of change needs to incorporate the extent and timescales over which communities vary under extant conditions. However, few observations of Antarctic microbial communities, which dominate inland habitats, allow this. We therefore carried out the first molecular comparison of Cyanobacteria in historic herbarium microbial mats from freshwater ecosystems on Ross Island and the McMurdo Ice Shelf, collected by Captain R.F. Scott's ‘Discovery’ Expedition (1902–1903), with modern samples from those areas. Using 16S rRNA gene surveys, we found that modern and historic cyanobacteria assemblages showed some variation in community structure but were dominated by the same genotypes. Modern communities had a higher richness, including genotypes not found in historic samples, but they had the highest similarity to other cyanobacteria sequences from Antarctica. The results imply slow cyanobacterial 16S rRNA gene genotype turnover and considerable community stability within Antarctic microbial mats. We suggest that this relates to Antarctic freshwater 'organisms requiring a capacity to withstand diverse stresses, and that this could also provide a degree of resistance and resilience to future climatic-driven environmental change in Antarctica.


Fottea ◽  
2011 ◽  
Vol 11 (1) ◽  
pp. 215-224 ◽  
Author(s):  
Raeid M. M. Abed ◽  
Sergey Dobrestov ◽  
Samiha Al-Kharusi ◽  
Angela Schramm ◽  
Barry Jupp ◽  
...  

Sedimentology ◽  
2016 ◽  
Vol 63 (4) ◽  
pp. 972-1016 ◽  
Author(s):  
Anthony Bouton ◽  
Emmanuelle Vennin ◽  
Aurélie Pace ◽  
Raphaël Bourillot ◽  
Christophe Dupraz ◽  
...  

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