A newly isolated Haloalkaliphilic bacterium from middle-late Eocene halite formed in salt lakes in China
Identifikátory výsledku
Kód výsledku v 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>
Nalezeny alternativní kódy
RIV/67985831:_____/15:00448076
Výsledek na webu
<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>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
A newly isolated Haloalkaliphilic bacterium from middle-late Eocene halite formed in salt lakes in China
Popis výsledku v původním jazyce
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.
Název v anglickém jazyce
A newly isolated Haloalkaliphilic bacterium from middle-late Eocene halite formed in salt lakes in China
Popis výsledku anglicky
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.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
—
Návaznosti výsledku
Projekt
<a href="/cs/project/LK21303" target="_blank" >LK21303: Stopy katastrofy, která způsobila úhyn velkých savců a klimatické změny před 12 900 lety</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Carbonates and Evaporites
ISSN
0891-2556
e-ISSN
—
Svazek periodika
30
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
10
Strana od-do
321-330
Kód UT WoS článku
000360019200007
EID výsledku v databázi Scopus
2-s2.0-84939574426