1881 - Microbiome structure of Karvachar (Nagorno-Karabakh) geothermal spring

Author(s):  
Hovik Panosyan
Keyword(s):  
Author(s):  
K. Yadav ◽  
A. Sircar ◽  
D. Jani ◽  
N. Bist ◽  
A. Nirantare ◽  
...  

Sedimentology ◽  
2017 ◽  
Vol 64 (4) ◽  
pp. 903-931 ◽  
Author(s):  
Benjamin Lopez ◽  
Gilbert Camoin ◽  
Mehmet Özkul ◽  
Rudy Swennen ◽  
Aurélien Virgone

Data in Brief ◽  
2020 ◽  
Vol 32 ◽  
pp. 106244
Author(s):  
Alexei S. Rozanov ◽  
Anton V. Korzhuk ◽  
Valeria N. Shlyakhtun ◽  
Aleksandra A. Shipova ◽  
Sergey E. Peltek

2018 ◽  
Vol 6 (11) ◽  
Author(s):  
Anna-Louise Reysenbach ◽  
John A. Donaho ◽  
John F. Kelley ◽  
Emily St. John ◽  
Christina Turner ◽  
...  

ABSTRACT A draft genome of a novel Dictyoglomus sp., NZ13-RE01, was obtained from a New Zealand hot spring enrichment culture. The 1,927,012-bp genome is similar in both size and G+C content to other Dictyoglomus spp. Like its relatives, Dictyoglomus sp. NZ13-RE01 encodes many genes involved in complex carbohydrate metabolism.


Genomics Data ◽  
2015 ◽  
Vol 5 ◽  
pp. 195-200 ◽  
Author(s):  
Sonu Bhatia ◽  
Navneet Batra ◽  
Ashish Pathak ◽  
Amit Joshi ◽  
Leila Souza ◽  
...  

2004 ◽  
Vol 70 (3) ◽  
pp. 1865-1868 ◽  
Author(s):  
Jessica Donahoe-Christiansen ◽  
Seth D'Imperio ◽  
Colin R. Jackson ◽  
William P. Inskeep ◽  
Timothy R. McDermott

ABSTRACT An arsenite-oxidizing Hydrogenobaculum strain was isolated from a geothermal spring in Yellowstone National Park, Wyo., that was previously shown to contain microbial populations engaged in arsenite oxidation. The isolate was sensitive to both arsenite and arsenate and behaved as an obligate chemolithoautotroph that used H2 as its sole energy source and had an optimum temperature of 55 to 60�C and an optimum pH of 3.0. The arsenite oxidation in this organism displayed saturation kinetics and was strongly inhibited by H2S.


2016 ◽  
Vol 15 (1) ◽  
pp. 1-11 ◽  
Author(s):  
Sujay Paul ◽  
Yolanda Cortez ◽  
Nadia Vera ◽  
Gretty Villena ◽  
Marcel Gutiérrez-Correa

2013 ◽  
Vol 295-298 ◽  
pp. 1948-1951
Author(s):  
Gui Fang Yang ◽  
Dong Li Wang ◽  
Na Li ◽  
Sheng Guang Zhuo

Beijing-Tianjin-Tangshan- Qinhuangdao area structurally lies in the fault-fold belt before Yanshan orogenic belt. The geothermal springs are divided into two types: the natural outcrop type and the hidden artificial type of heat reservoir, the former of which is controlled by piedmont faulted , extending EW; while the latter of which is controlled by regional structure and geothermal field. Geothermal spring water is low salinity and neutral even low alkaline water, whose chemical type is mainly SO4•HCO3- Na and SO4•Cl•HCO3- Na. As the water is rich in fluoride and multiple heavy metals, it pollutes drinking water, soil, crops in different degree during the development and utilization. H2S and CO2 in the geothermal water also does harm to the atmosphere more or less.


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