Energy sources for chemolithotrophs in an arsenic- and iron-rich shallow-sea hydrothermal system

Geobiology ◽  
2011 ◽  
Vol 9 (5) ◽  
pp. 436-445 ◽  
Author(s):  
N. H. AKERMAN ◽  
R. E. PRICE ◽  
T. PICHLER ◽  
J. P. AMEND
2016 ◽  
Vol 30 ◽  
pp. 93-95 ◽  
Author(s):  
Dan Lin ◽  
Kai Tang ◽  
Yu Han ◽  
Chenlan Li ◽  
Xiaofeng Chen

2013 ◽  
Vol 4 ◽  
Author(s):  
Roy E. Price ◽  
Ryan Lesniewski ◽  
Katja S. Nitzsche ◽  
Anke Meyerdierks ◽  
Chad Saltikov ◽  
...  

2020 ◽  
Vol 70 (12) ◽  
pp. 6251-6256 ◽  
Author(s):  
Qingfeng Zhang ◽  
Dan Lin ◽  
Jianing Ye ◽  
Ta-Hui Lin ◽  
Chenlan Li ◽  
...  

A novel Gram-stain-negative, non-flagellated, non-motile, rod-shaped (0.4–0.6×1.8–2.5 µm), aerobic bacterial strain, designated JLT21T, was isolated from seawater of a shallow-sea hydrothermal system. Growth occurred with 0–4.0 % (w/v) NaCl (optimum, 2.0 % NaCl), at 8–45 °C (optimum, 25 °C) and at pH 3.0–10.0 (optimum, pH 7.0). Analysis of 16S rRNA gene sequences revealed that strain JLT21T showed the highest 16S rRNA gene sequence similarity to Gaetbulibacter aquiaggeris KEM-8T (97.2 %), Gaetbulibacter marinus IMCC1914T (96.9 %) and Yeosuana aromativorans GW1-1T (96.9 %). Phylogenetic analysis based on 16S rRNA gene sequences revealed that strain JLT21T clustered with Y. aromativorans GW1-1T. The predominant respiratory quinone of strain JLT21T was menaquinone-6 (MK-6). Polar lipids were phosphatidylcholine, phosphatidylglycerol, phosphatidylethanolamine, three unidentified glycolipids and four unidentified lipids. The major fatty acids of strain JLT21T were iso-C15 : 0 (21.7 %), C16 : 1  ω6c/ω7c (11.5 %) and iso-C17 : 0 3-OH (10.9 %). The DNA G+C content of strain JLT21T was 32.6 %. On the basis of polyphasic analysis, strain JLT21T is considered to represent a novel species of the genus Yeosuana , for which the name Yeosuana marina sp. nov. is proposed. The type strain of Yeosuana marina is JLT21T (=CGMCC 1.15787T=JCM 31511T). The study helps us better understand the bacterial species in the shallow-sea hydrothermal system and their adaptations to the hydrothermal environment.


2017 ◽  
Vol 32 ◽  
pp. 19-21 ◽  
Author(s):  
Yu Han ◽  
Dan Lin ◽  
Liwei Yu ◽  
Xiaofeng Chen ◽  
Jia Sun ◽  
...  

2020 ◽  
Vol 19 (3) ◽  
pp. 253-259
Author(s):  
L. Ramírez-Vázquez ◽  
A. Negrón-Mendoza

AbstractLife originated on Earth possibly as a physicochemical process; thus, geological environments and their hypothetical characteristics on early Earth are essential for chemical evolution studies. Also, it is necessary to consider the energy sources that were available in the past and the components that could have contributed to promote chemical reactions. It has been proposed that the components could have been mineral surfaces. The aim of this work is to determine the possible role of mineral surfaces on chemical evolution, and to study of the stability of relevant molecules for metabolism, such as α-ketoglutaric acid (α-keto acid, Krebs cycle participant), using ionizing radiation and thermal energy as energy sources and mineral surfaces to promote chemical reactions. Preliminary results show α-ketoglutaric acid can be relatively stable at the simulated conditions of an impact-generated hydrothermal system; thus, those systems might have been plausible environments for chemical evolution on Earth.


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