Hydrogeochemical investigation of geothermal springs in Erzurum, East Anatolia (Turkey)

2018 ◽  
Vol 77 (24) ◽  
Author(s):  
Mine Alacali
2021 ◽  
Vol 9 (7) ◽  
pp. 1473
Author(s):  
Ani Saghatelyan ◽  
Armine Margaryan ◽  
Hovik Panosyan ◽  
Nils-Kåre Birkeland

The microbial diversity of high-altitude geothermal springs has been recently assessed to explore their biotechnological potential. However, little is known regarding the microbiota of similar ecosystems located on the Armenian Highland. This review summarizes the known information on the microbiota of nine high-altitude mineralized geothermal springs (temperature range 25.8–70 °C and pH range 6.0–7.5) in Armenia and Nagorno-Karabakh. All these geothermal springs are at altitudes ranging from 960–2090 m above sea level and are located on the Alpide (Alpine–Himalayan) orogenic belt, a seismically active region. A mixed-cation mixed-anion composition, with total mineralization of 0.5 mg/L, has been identified for these thermal springs. The taxonomic diversity of hot spring microbiomes has been examined using culture-independent approaches, including denaturing gradient gel electrophoresis (DGGE), 16S rRNA gene library construction, 454 pyrosequencing, and Illumina HiSeq. The bacterial phyla Proteobacteria, Bacteroidetes, Cyanobacteria, and Firmicutes are the predominant life forms in the studied springs. Archaea mainly include the phyla Euryarchaeota, Crenarchaeota, and Thaumarchaeota, and comprise less than 1% of the prokaryotic community. Comparison of microbial diversity in springs from Karvachar with that described for other terrestrial hot springs revealed that Proteobacteria, Bacteroidetes, Actinobacteria, and Deinococcus–Thermus are the common bacterial groups in terrestrial hot springs. Contemporaneously, specific bacterial and archaeal taxa were observed in different springs. Evaluation of the carbon, sulfur, and nitrogen metabolism in these hot spring communities has revealed diversity in terms of metabolic activity. Temperature seems to be an important factor in shaping the microbial communities of these springs. Overall, the diversity and richness of the microbiota are negatively affected by increasing temperature. Other abiotic factors, including pH, mineralization, and geological history, also impact the structure and function of the microbial community. More than 130 bacterial and archaeal strains (Bacillus, Geobacillus, Parageobacillus, Anoxybacillus, Paenibacillus, Brevibacillus Aeribacillus, Ureibacillus, Thermoactinomyces, Sporosarcina, Thermus, Rhodobacter, Thiospirillum, Thiocapsa, Rhodopseudomonas, Methylocaldum, Desulfomicrobium, Desulfovibrio, Treponema, Arcobacter, Nitropspira, and Methanoculleus) have been reported, some of which may be representative of novel species (sharing 91–97% sequence identity with their closest matches in GenBank) and producers of thermozymes and biomolecules with potential biotechnological applications. Whole-genome shotgun sequencing of T. scotoductus K1, as well as of the potentially new Treponema sp. J25 and Anoxybacillus sp. K1, were performed. Most of the phyla identified by 16S rRNA were also identified using metagenomic approaches. Detailed characterization of thermophilic isolates indicate the potential of the studied springs as a source of biotechnologically valuable microbes and biomolecules.


Crustaceana ◽  
2014 ◽  
Vol 87 (3) ◽  
pp. 328-339 ◽  
Author(s):  
Hui Ming Li ◽  
Bo Ping Han ◽  
Fei Fei Guo ◽  
Henri J. Dumont

In 1964 and 1965, Shen & Tai described two species of calanoids, which they classified in the South American genus Argyrodiaptomus. We examined new material from the terra typica, South China, and show that both species belong in the Asian genus Sinodiaptomus. A biogeographic anomaly is thus corrected. Moreover, the two appear to be sister species and males are morphologically well separable. No intermediate morphotypes have so far been detected. S. cavernicolax (Shen & Tai, 1965), known only from the type locality, was claimed to be cavernicolous, but shows no stygobitic adaptations, and has eyes. It may have been pushed back into the cave environment by its congener S. ferus (Shen & Tai, 1964) with which it coexists in the same lake system. So far, four species of Sinodiaptomus have been found in China: the two mentioned above, i.e., S. cavernicolax only in Longyan Cave of Zhaoqing City, and S. ferus at about five locations, but its range is limited to a small part of Guangdong Province. All five other species of Sinodiaptomus, among which the other two that occur (also) in China, also occupy small to very small ranges, with the type species (S. chaffanjoni Richard, 1897) only living in North China, and S. indicus Kiefer, 1936 and S. mahanandiensis Reddy & Radhakrishna, 1980 confined to South India (Reddy & Radhakrishna, 1980). S. valkanovi Kiefer, 1938 from Japan is invasive (Ueda & Ohtsuka, 1998; Makino et al., 2010). S. sarsi Rylov, 1923, distributed in Japan, China, and most of Mongolia, is separated by a wide disjunction from a group of populations in Iran, the Caucasus, and East Anatolia. This western group of populations might be a separate species and deserves more study.


2007 ◽  
Vol 73 (20) ◽  
pp. 6669-6677 ◽  
Author(s):  
Eric S. Boyd ◽  
Robert A. Jackson ◽  
Gem Encarnacion ◽  
James A. Zahn ◽  
Trevor Beard ◽  
...  

ABSTRACT Elemental sulfur (S0) is associated with many geochemically diverse hot springs, yet little is known about the phylogeny, physiology, and ecology of the organisms involved in its cycling. Here we report the isolation, characterization, and ecology of two novel, S0-reducing Crenarchaea from an acid geothermal spring referred to as Dragon Spring. Isolate 18U65 grows optimally at 70 to 72°C and at pH 2.5 to 3.0, while isolate 18D70 grows optimally at 81°C and pH 3.0. Both isolates are chemoorganotrophs, dependent on complex peptide-containing carbon sources, S0, and anaerobic conditions for respiration-dependent growth. Glycerol dialkyl glycerol tetraethers (GDGTs) containing four to six cyclopentyl rings were present in the lipid fraction of isolates 18U65 and 18D70. Physiological characterization suggests that the isolates are adapted to the physicochemical conditions of Dragon Spring and can utilize the natural organic matter in the spring as a carbon and energy source. Quantitative PCR analysis of 16S rRNA genes associated with the S0 flocs recovered from several acid geothermal springs using isolate-specific primers indicates that these two populations together represent 17 to 37% of the floc-associated DNA. The physiological characteristics of isolates 18U65 and 18D70 are consistent with their potential widespread distribution and putative role in the cycling of sulfur in acid geothermal springs throughout the Yellowstone National Park geothermal complex. Based on phenotypic and genetic characterization, the designations Caldisphaera draconis sp. nov. and Acidilobus sulfurireducens sp. nov. are proposed for isolates 18U65 and 18D70, respectively.


2007 ◽  
Vol 25 (1-2) ◽  
pp. 58-63 ◽  
Author(s):  
Gülay Ecevit Genç ◽  
Ali Kandemir ◽  
İlker Genç

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