| Literature DB >> 34917948 |
Yueyue Qiang1,2, Ruiru Si1, Suo Tan1,2, Hang Wei1, Biao Huang1, Miaohong Wu1,3, Mengzhu Shi1, Ling Fang1, Jianwei Fu1,2, Shaoxiao Zeng2.
Abstract
The objective of this study was to investigate the spatial variation of volatile organic compounds and antioxidant activity of turmeric essential oils (TEOs) harvested from four provinces of China. The major chemical components of these TEOs were analyzed using headspace solid-phase micro-extraction gas chromatography-mass spectrometry. More than forty volatile organic compounds in TEOs were identified, which accounted for 82.09-93.64% of the oil components. The relative abundances of the main volatile organic compounds in TEOs at the genus level were visualized by a heat map. The antioxidant activity of the TEOs of five different origins was characterized by the DPPH free radical scavenging activity, in which the antioxidant activity of the TEOs from Guangxi was superior to those of other sources. Furthermore, the IC50 values of the antioxidants TEOs collected from Guangxi, Sichuan, Yunnan, Changting, and Liancheng were 33.30, 42.5, 35.22, 63.27, and 39.96 mg/mL, respectively, which indicated the excellent free radical scavenging activity of those TEOs. Therefore, the TEOs might be considered as a natural antioxidant with potential applications in food and pharmaceutical industries.Entities:
Keywords: Antioxidant activity; Curcuma longa L; DPPH; HS-SPME-GC-MS; Turmeric essential oils (TEOs)
Year: 2021 PMID: 34917948 PMCID: PMC8646137 DOI: 10.1016/j.crfs.2021.11.002
Source DB: PubMed Journal: Curr Res Food Sci ISSN: 2665-9271
Geographic and climatic information on the collected turmeric for the study.
| Province | District | Locality | Longitude | Latitude | Accessions collected | Climate | Elevation |
|---|---|---|---|---|---|---|---|
| Guangxi | Baise | Napo | 105°84′ | 23°41′ | GX | subtropical monsoon climate | 1681 m |
| Yunnan | Wenshan | Maguan | 103°52′ | 22°42′ | YN | subtropical monsoon climate | 1447 m |
| Sichuan | Yibin | Yibin | 104°53′ | 28°69′ | SC | subtropical monsoon humid climate | 422 m |
| Fujian | Liancheng | Chixi | 116°32′ | 25°13′ | LC | subtropical monsoon climate | 375 m |
| Fujian | Changting | Tongfang | 116°57′ | 25°88′ | CT | subtropical monsoon climate | 658 m |
Fig. 1The total ion chromatograms (TICs) of TEOs collected from different origins.
The chemical compositions of TEOs of five different origins in China.
| Compounds | Formula | RT | RI | Relative Content% (mean ± SD) | |||||
|---|---|---|---|---|---|---|---|---|---|
| Guangxi | Yunnan | Sichuan | Liancheng | Changting | |||||
| 1 | β-Pinene | C10H16 | 8.22 | 976 | − | 0.45 ± 0.25a | 8.22 | 0.03 ± 0.01b | 0.06 ± 0.02b |
| 2 | Eucalyptol | C10H18O | 9.808 | 1032 | 0.05 ± 0.02b | 0.47 ± 0.23b | 0.24 ± 0.05b | 0.42 ± 0.07b | 3.25 ± 0.85a |
| 3 | Camphor | C10H16O | 13.245 | 1139 | 0.06 ± 0.01b | 0.64 ± 0.17a | 0.02 ± 0.01b | – | – |
| 4 | DL-Isoborneol | C10H18O | 13.753 | 1155 | 0.05 ± 0.01b | 0.37 ± 0.03a | 0.02 ± 0.01b | – | – |
| 5 | 2-Undecanone | C11H22O | 17.422 | 1279 | 0.09 ± 0.02b | 0.36 ± 0.12a | 0.08 ± 0.03b | 0.03 ± 0.01b | 0.03 ± 0.01b |
| 6 | 2-Tridecanol | C13H28O | 17.715 | 1289 | 0.01 ± 0.01b | 0.23 ± 0.13a | – | 0.02 ± 0.01b | 0.02 ± 0.01b |
| 7 | β-Elemene | C15H24 | 20.096 | 1375 | 0.34 ± 0.05b | 1.38 ± 0.62a | 0.25 ± 0.05b | 0.54 ± 0.08b | 0.47 ± 0.09b |
| 8 | 7-epi-Sesquithujene | C15H24 | 20.413 | 1387 | 0.97 ± 0.08ab | 1.04 ± 0.28a | 0.72 ± 0.18b | 0.69 ± 0.05b | 0.69 ± 0.09b |
| 9 | C15H24 | 21.218 | 1414 | 0.45 ± 0.02b | 1.01 ± 0.50a | 0.61 ± 0.07ab | 0.25 ± 0.02b | 0.24 ± 0.02b | |
| 10 | β-Sesquiphellandrene | C15H24 | 21.397 | 1419 | 0.50 ± 0.03a | 0.46 ± 0.15a | 0.55 ± 0.06a | 0.31 ± 0.02b | 0.27 ± 0.02b |
| 11 | ( | C15H24 | 21.683 | 1428 | 1.70 ± 0.15a | 1.42 ± 0.31a | 1.37 ± 0.18a | 1.68 ± 0.02a | 1.50 ± 0.19a |
| 12 | α-Humulene | C15H24 | 21.813 | 1432 | 0.34 ± 0.03a | 0.57 ± 0.36a | 0.59 ± 0.04a | – | – |
| 13 | C15H22 | 22.465 | 1452 | 22.80 ± 0.98a | 14.50 ± 1.83bc | 11.40 ± 1.98d | 15.45 ± 1.91b | 12.01 ± 0.79cd | |
| 14 | β-Eudesmene | C15H24 | 22.678 | 1458 | – | 1.12 ± 0.44 | – | – | – |
| 15 | α-Zingiberene | C15H24 | 22.794 | 1462 | 12.33 ± 0.59c | 14.07 ± 5.58c | 15.57 ± 0.60bc | 20.94 ± 1.96ab | 24.41 ± 3.96a |
| 16 | β-Bisabolene | C15H24 | 23.109 | 1472 | 8.77 ± 0.24a | 8.50 ± 1.39a | 5.18 ± 0.55c | 8.35 ± 0.59ab | 7.07 ± 0.46b |
| 17 | δ-Cadinene | C15H24 | 23.372 | 1480 | 0.32 ± 0.07a | – | – | 0.08 ± 0.03b | 0.06 ± 0.03b |
| 18 | β-Cedrene | C15H24 | 23.537 | 1484 | 25.37 ± 0.43a | 17.04 ± 0.56b | 15.75 ± 1.23b | 25.89 ± 1.02a | 24.37 ± 1.22a |
| 19 | C15H26O | 24.202 | 1504 | 0.42 ± 0.01b | 0.47 ± 0.05a | – | 0.18 ± 0.01c | 0.14 ± 0.02c | |
| 20 | Humulene epoxide II | C15H24O | 24.214 | 1504 | – | – | 0.37 ± 0.02 | – | – |
| 21 | Germacrene B | C15H24 | 24.372 | 1508 | 0.14 ± 0.02c | 0.49 ± 0.03b | 0.63 ± 0.05a | 0.61 ± 0.02a | 0.50 ± 0.05b |
| 22 | 3,3,5,5-Tetramethylcyclopentene | C9H16 | 24.515 | 1511 | 0.08 ± 0.01bc | 0.07 ± 0.01c | 0.13 ± 0.01a | 0.09 ± 0.01b | 0.07 ± 0.01c |
| 23 | C15H22O | 24.742 | 1517 | 0.48 ± 0.07b | – | 0.75 ± 0.09a | 0.14 ± 0.04c | 0.09 ± 0.03c | |
| 24 | Caryophyllene oxide | C15H24O | 24.917 | 1521 | 0.25 ± 0.01b | 0.34 ± 0.08a | 0.22 ± 0.01b | 0.04 ± 0.01c | 0.02 ± 0.01c |
| 25 | Cryptomeridiol | C15H28O2 | 25.2 | 1527 | – | 0.17 ± 0.06 | – | – | – |
| 26 | Epicurzerenone | C15H18O2 | 25.295 | 1530 | 0.88 ± 0.08 | 2.08 ± 0.30 | – | – | – |
| 27 | Zingiberenol | C15H26O | 25.622 | 1537 | 0.92 ± 0.05a | 0.66 ± 0.27b | 0.45 ± 0.05bc | 0.39 ± 0.04c | 0.31 ± 0.12c |
| 28 | C15H22O | 25.772 | 1541 | 0.33 ± 0.04a | – | – | 0.23 ± 0.02b | 0.18 ± 0.07b | |
| 29 | α-Acorenol | C15H26O | 26.09 | 1548 | – | 0.31 ± 0.06a | – | 0.15 ± 0.02b | 0.12 ± 0.03b |
| 30 | β-Ylangene | C15H24 | 26.086 | 1548 | 0.30 ± 0.02 | – | – | – | – |
| 31 | ( | C15H22O | 26.35 | 1554 | 0.14 ± 0.02b | – | 0.58 ± 0.04a | 0.10 ± 0.03b | 0.09 ± 0.03b |
| 32 | C15H20O | 26.737 | 1563 | 7.94 ± 0.57ab | 5.47 ± 1.43c | 9.90 ± 1.22a | 6.15 ± 0.56bc | 5.52 ± 1.72c | |
| 33 | Turmerone | C15H22O | 26.853 | 1566 | 3.03 ± 0.37c | 3.12 ± 0.62c | 13.31 ± 1.70a | 5.87 ± 0.82b | 5.87 ± 0.57b |
| 34 | ( | C15H22O | 27.113 | 1572 | – | 0.22 ± 0.14 | – | – | – |
| 35 | ( | C15H22O | 27.46 | 1580 | 0.75 ± 0.10b | 1.84 ± 0.32a | 1.39 ± 0.24a | 1.79 ± 0.10a | 1.62 ± 0.39a |
| 36 | Curlone | C15H22O | 27.588 | 1583 | 2.60 ± 0.26b | 1.69 ± 0.42b | 6.02 ± 0.80a | 2.64 ± 0.25b | 2.56 ± 0.81b |
| 37 | Curdione | C15H24O2 | 27.889 | 1591 | 0.22 ± 0.06 | 0.90 ± 0.25 | – | – | – |
| 38 | Curcumenol | C15H22O2 | 28.116 | 1596 | 0.05 ± 0.02a | 0.26 ± 0.12a | – | 0.05 ± 0.02a | 0.17 ± 0.27a |
| 39 | Bisabolone | C15H24O | 28.48 | 1604 | 0.39 ± 0.04a | 0.21 ± 0.08a | 0.24 ± 0.06a | 0.39 ± 0.02a | 0.46 ± 0.33a |
| 40 | ( | C15H22O | 29.078 | 1616 | 0.25 ± 0.04b | 0.15 ± 0.05c | 0.41 ± 0.05a | 0.16 ± 0.02c | 0.14 ± 0.05c |
| Total identified (%) | 93.34 ± 0.45 | 82.09 ± 1.78 | 86.74 ± 0.58 | 93.64 ± 0.62 | 92.28 ± 1.55 | ||||
| Sesquiterpene hydrocarbons | 74.33 ± 2.08 | 61.61 ± 2.45 | 52.62 ± 4.74 | 74.78 ± 0.87 | 71.57 ± 5.55 | ||||
| Oxygenated sesquiterpenes | 18.67 ± 1.64 | 17.89 ± 3.36 | 33.62 ± 4.19 | 18.28 ± 1.00 | 17.28 ± 4.27 | ||||
| Monoterpene hydrocarbons | – | 0.45 ± 0.25 | – | 0.03 ± 0.01 | 0.06 ± 0.02 | ||||
| Oxygenated Monoterpenes | 0.16 ± 0.04 | 1.48 ± 0.09 | 0.28 ± 0.09 | 0.42 ± 0.07 | 3.25 ± 0.85 | ||||
Relative content (%) is given as means ± SDs (n = 3); The different labelled letters (a, b, c, d) in a row indicted the values are significantly different among the TEOs of different origins (P < 0.05) by Duncan's Multiple Range Test.
RT is the abbreviation for retention time.
Retention indices (RI) represents the retention index obtained using the C10–C25 n-alkane series as the reference in the Rxi-5Sil MS column.
- represents that the component was not retrieved in the corresponding sample.
Fig. 2HCA dendrogram associated with the heat map of the components of TEOs from Yunnan(YN), Sichuan(SC), Guangxi(GX), Changting(CT) and Liangcheng(LC).
Fig. 3Principal component analysis (PCA) score plot of the components in the TEOs of five different origins GX, YN, SC, LC, and CT. (A) The PCA score plot of the first two principal components (PC1 and PC2); (B) The PCA score plot of the first and third principal components (PC1 and PC3). GX, YN, SC, LC, and CT represented the TEOs from Guangxi, Yunnan, Sichuan, Liancheng, and Changting.
Fig. 4The extended error bar plot identified the differences of volatile organic compounds in the TEOs among the mean proportions of bacterial taxa. The differences between groups were determined using a Welsh’s t-test, while the Benjamini–Hochberg procedure was used to control the false discovery rate due to multiple tests. The corresponding p values were shown on the right sides. (A) CT (green) versus GX (red); (B) CT (green) versus SC (black); (C) CT (green) versus YN (purple pink); (D) LC (blue) versus CT (green); (E) LC (blue) versus GX (red); (F) LC (blue) versus SC (black); (G)LC (blue) versus YN (purple pink). The confidence intervals were provided to allow for the critical assessment of the biological relevance of the test results. (For interpretation of the references to color in this figure legend, the reader is referred to the Web version of this article.)
Fig. 5The DPPH-radical-scavenging activity (%) of the TEOs of Guangxi, Yunnan, Sichuan, Liancheng, and Changting.