| Literature DB >> 22558000 |
Francisco N Arroyo-López1, Verónica Romero-Gil, Joaquín Bautista-Gallego, Francisco Rodríguez-Gómez, Rufino Jiménez-Díaz, Pedro García-García, Amparo Querol, Antonio Garrido-Fernández.
Abstract
Yeasts play an important role in the food and beverage industry, especially in products such as bread, wine, and beer, among many others. However, their use as a starter in table olive processing has not yet been studied in detail. The candidate yeast strains should be able to dominate fermentation, together with lactic acid bacteria, but should also provide a number of beneficial advantages. Technologically, yeasts should resist low pH and high salt concentrations, produce desirable aromas, improve lactic acid bacteria growth, and inhibit spoilage microorganisms. Nowadays, they are being considered as probiotic agents because many species are able to resist the passage through the gastrointestinal tract and show favorable effects on the host. In this way, yeasts may improve the health of consumers by means of the degradation of non-assimilated compounds (such as phytate complexes), a decrease in cholesterol levels, the production of vitamins and antioxidants, the inhibition of pathogens, an adhesion to intestinal cell line Caco-2, and the maintenance of epithelial barrier integrity. Many yeast species, usually found in table olive processing (Wickerhamomyces anomalus, Saccharomyces cerevisiae, Pichia membranifaciens, and Kluyveromyces lactis, among others), have exhibited some of these properties. Thus, the selection of the most appropriate strains to be used as starters in this fermented vegetable, alone or in combination with lactic acid bacteria, is a promising research line to develop in the near future.Entities:
Keywords: probiotic microorganisms; table olives; technological characteristics; yeast starter
Year: 2012 PMID: 22558000 PMCID: PMC3927136 DOI: 10.3389/fmicb.2012.00161
Source DB: PubMed Journal: Front Microbiol ISSN: 1664-302X Impact factor: 5.640
Description of the .
| 0 | Cu-containing membrane | ||||
| Monooxygenase (CuMMO) | 6628 | ||||
| 0.1 | MOB_like | ||||
| 0.1.1 | TypeI | ||||
| 0.1.1.1 | TypeIa | ||||
| 0.1.1.1.1 | Mbacter | 552 | AJ414658 | Arctic wetland | |
| 0.1.1.1.2 | Mmicrobium_jap | 28 | AB253367 | Marine mud | |
| 0.1.1.1.3 | Mmicrobium_pel | 25 | U31652 | Upland soils | |
| 0.1.1.1.4 | Mmonas | 396 | U31653 | Lake sediments | |
| 0.1.1.1.5 | Msarcina | 517 | AF177326 | Landfill soil | |
| 0.1.1.1.6 | Msoma | 4 | DQ119047 | Lake sediment | |
| 0.1.1.1.7 | Mbacter_or_Mmonas | 2 | AY236078 | Movile cave | |
| 0.1.1.1.8 | Deep_sea_1 | 46 | AM283467 | Marine deep sea | |
| 0.1.1.1.9 | Deep_sea_3 | 191 | FJ858316 | Marine deep sea | |
| 0.1.1.1.10 | LP20 | 51 | AB064377 | Aquifer | |
| 0.1.1.1.11 | Landfill_cluster_2 | 4 | EU275117 | Landfill soil | |
| 0.1.1.1.12 | Lake_cluster_1 | 72 | EF623667 | Freshwater lakes | |
| 0.1.1.1.13 | RPC_2 | 148 | FN600101 | Rice field soil | |
| 0.1.1.1.14 | PS_80 | 8 | AF211872 | Marine | |
| 0.1.1.1.15 | Aquifer_cluster | 53 | AM410175 | Aquifer | |
| 0.1.1.2 | TypeIb | ||||
| 0.1.1.2.1 | Mcaldum | 98 | U89304 | Agricultural soil | |
| 0.1.1.2.2 | Mcoccus | 244 | L40804 | Aquatic environments | |
| 0.1.1.2.3 | Mthermus | 36 | AJ829010 | Hot spring | |
| 0.1.1.2.4 | JRC_4 | 27 | EU359002 | Rice field soil | |
| 0.1.1.2.5 | Deep_sea_4 | 26 | GU584280 | Marine deep sea | |
| 0.1.1.2.6 | Deep_sea_5 | 155 | EU417471 | Marine deep sea | |
| 0.1.1.2.7 | FWs | 100 | AF211878 | Freshwater lakes | |
| 0.1.1.2.8 | JRC_3 | 29 | AB222881 | Rice field soil | |
| 0.1.1.2.9 | Lake_cluster_2 | 74 | AF211879 | Freshwater lakes | |
| 0.1.1.2.10 | LWs | 83 | DQ067069 | Freshwater lakes | |
| 0.1.1.2.11 | OSC | 18 | AJ317928 | Organic soil | |
| 0.1.1.2.12 | RPC_1 | 67 | FN599957 | Rice field soil | |
| 0.1.1.2.13 | RPCs | 166 | FJ845814 | Rice field soil | |
| 0.1.1.3 | TypeIc | ||||
| 0.1.1.3.1 | Ncoccus | 83 | U96611 | Marine | |
| 0.1.1.3.2 | USCg | 185 | AJ579667 | Upland soils | |
| 0.1.1.3.3 | JR2 | 68 | AY654695 | Upland soils | |
| 0.1.1.3.4 | JR3 | 65 | AY654702 | Upland soils | |
| 0.1.2 | TypeII | ||||
| 0.1.2.1 | TypeIIa | ||||
| 0.1.2.1.1 | Msinus | 70 | AJ459007 | Various | |
| 0.1.2.1.2 | Mcystis | 1085 | AJ431386 | Various | |
| 0.1.2.1.3 | Msinus_Mcystis | 79 | AJ431388 | Various | |
| 0.1.2.2 | TypeIIb | ||||
| 0.1.2.2.1 | Mcapsa | 27 | AJ278727 | Sphagnum bog | |
| 0.1.2.2.2 | MO3 | 23 | AF283229 | Landfill soil | |
| 0.1.2.2.3 | pmoA2 | 45 | AJ431387 | Various | |
| 0.1.2.2.4 | USCa | 888 | AF148521 | Upland soils | |
| 0.1.2 | pXMO_like | ||||
| 0.1.2.1 | TUSC_like | ||||
| 0.1.2.1.1 | Verr_1 | 3 | EU223859 | Geothermal soil | |
| 0.1.2.1.2 | Verr_2 | 3 | EU223862 | Geothermal soil | |
| 0.1.2.1.3 | Verr_3 | 3 | EU223855 | Geothermal soil | |
| 0.1.2.1.4 | TUSC | 101 | AJ868282 | Various | |
| 0.1.2.1.5 | NC10 | Cand. Methylomirabilis oxyfera | 33 | JX262154 | Freshwater sediment |
| 0.1.2.2 | RA21_like | ||||
| 0.1.2.2.1 | RA21 | 157 | AF148522 | Rice field soil | |
| 0.1.2.2.2 | M84_P22 | 9 | AJ299963 | Rice field soil | |
| 0.1.2.2.3 | gp23 | 1 | AF264137 | Upland soils | |
| 0.1.2.2.4 | Alkane_1 | Methylococcaceae ET-SHO | 2 | AB453961 | Marine |
| 0.1.2.2.5 | Alkane_2 | Methylococcaceae ET-HIRO | 2 | AB453962 | Marine |
| 0.1.2.2.6 | MR1 | 7 | AF200729 | Upland soils | |
| 0.1.2.3 | M84_P105_like | ||||
| 0.1.2.3.1 | M84_P105 | 34 | EU722433 | Various | |
| 0.1.2.4 | Crenothrix_like | ||||
| 0.1.2.4.1 | Crenothrix | Crenothrix polyspora (enrichment) | 69 | DQ295904 | Freshwater |
| 0.1.2.4.2 | Crenothrix_rel | 160 | AJ868245 | Various | |
| 0.2 | AOB_like | 206 | AF042171 | Various |
Figure 1Overview of the basic procedure for classifying . The manuscript section where a procedure is described is indicated and detailed instructions are available in the supplementary materials.
Figure 2Comparison of classifications of paddy soil . The datasets were generated from three different soils (young Chinese, old Chinese, and Italian) and with two different PCR primer combinations (A189f/A682r, A189f/mb661r) as indicated. The number of sequences assigned to each taxon is plotted. Only pmoA taxa detected in at least one dataset are shown.
Figure 3Examples of MEGAN visualizations of assignments for the . The tree shows the summary of taxa identified and their abundances (A); the circles at the nodes are proportional to the number of reads assigned to that taxon. Individual assignments can be inspected by right-clicking on a node and selecting “inspect,” as shown for the JRC-3 clade (B). Summary alignments can also be visualized, as shown for USCα (C); in this case it quickly shows that the best alignment to USCα have approximately 40 conserved mismatches, suggesting it is a novel pmoA cluster most closely related to USCα.
Figure 4Analysis of selected Type II . The sequences chosen for analysis are color-coded in the partial MEGAN tree (A). The USCα and Methylocapsa-assigned sequences were selected since the alignments showed conserved mismatches to the reference database (as shown for USCα sequences in Figure 3C). The sequences were imported into an ARB pmoA database, quality filtered by removing sequences with frameshifts, translated to amino acid sequences and added to the PmoA tree by parsimony and then reanalyzed by neighbor-joining. The positions of the sequences analyzed in ARB are shown (B). The new clades were named HY-1, HY-2 (Deng et al., 2013) and HY-4 (this study).
Figure 5MEGAN comparison view of . The pmoA datasets were obtained from triplicate samples from hummock (HYa) and hollow (HYb) sites. PCRs were performed with two primer combinations (A189f/A682r or A189f/mb661r), as indicated. The option to subsample datasets (3309 sequences) was chosen for the comparison. Assignments to internal nodes are not shown. MEGAN only shows taxa detected in at least one sample. The height of the bars was scaled to the number of reads assigned in each dataset and color-coded as indicated in the legend. The labeling at the top of the columns was added.