RNA fingerprinting analysis of Oenococcus oeni strains under wine conditions

2012 ◽  
Vol 31 (2) ◽  
pp. 238-245 ◽  
Author(s):  
Ana Paula Marques ◽  
Maria Vitória San Romão ◽  
Rogério Tenreiro
1997 ◽  
Vol 14 (2) ◽  
pp. 119-123 ◽  
Author(s):  
Hideki Sakai ◽  
Shigeru Nakashima ◽  
Kei Nakatani ◽  
Shin-ichi Yoshimura ◽  
Yasuaki Nishimura ◽  
...  

1991 ◽  
Vol 142 (1) ◽  
pp. 57-65 ◽  
Author(s):  
J.A.M. Brandful ◽  
N. Takeda ◽  
T. Yoshii ◽  
K. Miyamura ◽  
J.A.A. Mingle ◽  
...  

2003 ◽  
Author(s):  
Charles Thomas Parker ◽  
Dorothea Taylor ◽  
George M Garrity
Keyword(s):  

2003 ◽  
Author(s):  
Charles Thomas Parker ◽  
Dorothea Taylor ◽  
George M Garrity
Keyword(s):  

Author(s):  
S., R. Muthasyabiha

Geochemical analysis is necessary to enable the optimization of hydrocarbon exploration. In this research, it is used to determine the oil characteristics and the type of source rock candidates that produces hydrocarbon in the “KITKAT” Field and also to understand the quality, quantity and maturity of proven source rocks. The evaluation of source rock was obtained from Rock-Eval Pyrolysis (REP) to determine the hydrocarbon type and analysis of the value of Total Organic Carbon (TOC) was performed to know the quantity of its organic content. Analysis of Tmax value and Vitrinite Reflectance (Ro) was also performed to know the maturity level of the source rock samples. Then the oil characteristics such as the depositional environment of source rock candidate and where the oil sample develops were obtained from pattern matching and fingerprinting analysis of Biomarker data GC/GCMS. Moreover, these data are used to know the correlation of oil to source rock. The result of source rock evaluation shows that the Talangakar Formation (TAF) has all these parameters as a source rock. Organic material from Upper Talangakar Formation (UTAF) comes from kerogen type II/III that is capable of producing oil and gas (Espitalie, 1985) and Lower Talangakar Formation (LTAF) comes from kerogen type III that is capable of producing gas. All intervals of TAF have a quantity value from very good–excellent considerable from the amount of TOC > 1% (Peters and Cassa, 1994). Source rock maturity level (Ro > 0.6) in UTAF is mature–late mature and LTAF is late mature–over mature (Peters and Cassa, 1994). Source rock from UTAF has deposited in the transition environment, and source rock from LTAF has deposited in the terrestrial environment. The correlation of oil to source rock shows that oil sample is positively correlated with the UTAF.


Foods ◽  
2021 ◽  
Vol 10 (7) ◽  
pp. 1540
Author(s):  
Aitor Balmaseda ◽  
Laura Aniballi ◽  
Nicolas Rozès ◽  
Albert Bordons ◽  
Cristina Reguant

Oenococcus oeni is the main agent of malolactic fermentation in wine. This fermentation takes place after alcoholic fermentation, in a low nutrient medium where ethanol and other inhibitor compounds are present. In addition, some yeast-derived compounds such as mannoproteins can be stimulatory for O. oeni. The mannoprotein concentration in wine depends on the fermenting yeasts, and non-Saccharomyces in particular can increase it. As a result of the hydrolytic activity of O. oeni, these macromolecules can be degraded, and the released mannose can be taken up and used as an energy source by the bacterium. Here we look at mannoprotein consumption and the expression of four O. oeni genes related to mannose uptake (manA, manB, ptsI, and ptsH) in a wine-like medium supplemented with mannoproteins and in natural wines fermented with different yeasts. We observe a general gene upregulation in response to wine-like conditions and different consumption patterns in the studied media. O. oeni was able to consume mannoproteins in all the wines. This consumption was notably higher in natural wines, especially in T. delbrueckii and S. cerevisiae 3D wines, which presented the highest mannoprotein levels. Regardless of the general upregulation, it seems that mannoprotein degradation is more closely related to the fermenting medium.


2020 ◽  
Vol 307 ◽  
pp. 125556 ◽  
Author(s):  
Beatriz Quintanilla-Casas ◽  
Sofia Bertin ◽  
Kerstin Leik ◽  
Julen Bustamante ◽  
Francesc Guardiola ◽  
...  

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