A newly isolated Haloalkaliphilic bacterium from middle-late Eocene halite formed in salt lakes in China
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10314088" target="_blank" >RIV/00216208:11310/15:10314088 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/15:00448076
Result on the web
<a href="http://dx.doi.org/10.1007/s13146-014-0227-0" target="_blank" >http://dx.doi.org/10.1007/s13146-014-0227-0</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s13146-014-0227-0" target="_blank" >10.1007/s13146-014-0227-0</a>
Alternative languages
Result language
angličtina
Original language name
A newly isolated Haloalkaliphilic bacterium from middle-late Eocene halite formed in salt lakes in China
Original language description
Ancient living halotolerant bacteria and ancient DNA have been reported from bedded marine halite, but seldom from lacustrine halite of the geological age. A halotolerant bacterium (Haloalkaliphilic bacterium, designated as 3-4) was isolated from primary halite with abundant fluid inclusions. Primary halite crystallized in lacustrine Yunying Depression located in the northeastern Jianghan Basin of central China. Yunying Depression is an inland salt paleolake residing in a faulted basin formed during late Cretaceous/early Tertiary. Brine inclusions from the same layer of the salt that housed Haloalkaliphilic bacterium 3-4 are the middle-late Eocene primary halite crystals and have homogenization temperatures between 5.8 and 43.3 A degrees C. The estimated age is between 33.9 and 48.6 Ma years old for these fluid inclusions, and this represents the long-term survivability of this microorganism Haloalkaliphilic bacterium 3-4. Sequence analysis of the partial fragment of 16S ribosomal DNA showed that the organism is similar to the lineage of Haloalkaliphilic bacterium and Oceanobacillus sp. The isolation of the microbe reinforces the long-term preservation possibility of life in extreme environment such as the fluid inclusions in halite.
Czech name
—
Czech description
—
Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
—
Result continuities
Project
<a href="/en/project/LK21303" target="_blank" >LK21303: Traces of catastroph that caused extinction of large mammals and climatic change 12900 years ago</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Carbonates and Evaporites
ISSN
0891-2556
e-ISSN
—
Volume of the periodical
30
Issue of the periodical within the volume
3
Country of publishing house
US - UNITED STATES
Number of pages
10
Pages from-to
321-330
UT code for WoS article
000360019200007
EID of the result in the Scopus database
2-s2.0-84939574426