| Literature DB >> 35541466 |
Dan Zhang1, Yun-Ling Gao2, Sheng Jiang3, Yiwen Chen2, Yi Zhang4, Zheng Pan1.
Abstract
Lamiophlomis rotata (L. rotata) is a Tibetan medicinal herb used for centuries that contains iridoid glycosides (IGs), which are pharmacologically active ingredients and can be used for quality control. The IG profiles of the underground and aerial parts of the plant were determined by UPLC-TOF-MS to evaluate the similarity and variability of the different herbal parts listed in the Chinese Pharmacopoeia. Twenty-six IGs were detected in the total ion current (TIC) profile of L. rotata, and twenty-two of these were identified by comparing the retention times and mass spectra of the compounds to those of authentic standards. Among these compounds, five IGs with the same molecular formula (C17H26O11) were identified for the first time by mass spectrometry based on their different hydroxyl group-substituted positions. The aerial part has a similar chemical profile to that of the roots. The difference between the two parts was determined by multivariate statistical analysis of the UPLC-TOF-MS data of 24 specimens. Sesamoside was explored as the most characteristic marker to distinguish the two parts of L. rotata. To further estimate the distinction between the two parts, the content of total IGs and the antioxidant capacity were investigated in samples from different locations. The aerial parts showed a high content of total IGs and high antioxidant capacity, although not higher than those of the roots. The results also suggest the dosage should be increased when the aerial parts are used as crude medicinal materials instead of the underground parts. This journal is © The Royal Society of Chemistry.Entities:
Year: 2018 PMID: 35541466 PMCID: PMC9077588 DOI: 10.1039/c7ra10143k
Source DB: PubMed Journal: RSC Adv ISSN: 2046-2069 Impact factor: 4.036
Fig. 1Chemical structures of major components identified from L. rotata. The compound numbers represent the same meanings as in Table 2.
Populations of Lamiophlomis rotata from four provinces used in this paper
| Location | Longitude (E) | Latitude (N) | Altitude (m) | No. of samples |
|---|---|---|---|---|
| Gansu | 104.7733–101.9308 | 33.9361–33.7805 | 3789–3500 | 3 |
| Qinghai | 101.7353–96.6487 | 34.5261–31.1594 | 4178–3519 | 3 |
| Sichuan | 100.5236–98.7732 | 31.6583–31.4244 | 4323–3865 | 3 |
| Tibet | 94.2936–90.5775 | 32.0844–30.0183 | 4803–4235 | 3 |
Fig. 2TIC chromatography (positive) of the aerial and root parts of L. rotata. Meanings as in Table 1.
The identification iridoid glycosides of L. rotata by UPLC-Q/TOF-MSa
| Peak no. | RT (min) | Compound | Formula | Calculated (Da) | Selected ion | Precursor ion (Da) | Mass accuracy (ppm) | Root part | Aerial part |
|---|---|---|---|---|---|---|---|---|---|
| 1 | 3.765 | 7- | C17H26O13 | 438.1373 | [M + Na]+ | 461.1275 | 0.4 | ✓ | ✓ |
| 2 | 4.056 | Schismoside | C17H26O12 | 422.1424 | [M + Na]+ | 445.1308 | −3.6 | — | ✓ |
| 3 | 4.969 | 5-Deoxypulchelloside I | C17H26O11 | 406.1475 | [M + Na]+ | 429.1360 | −3.5 | ✓ | ✓ |
| 4 | 5.428 | Phlorigidoside C. | C17H24O11 | 404.1319 | [M + Na]+ | 427.1221 | 0.5 | ✓ | ✓ |
| 5 | 5.665 | Loganic acid | C16H24O10 | 376.1370 | [M + Na]+ | 399.1263 | −1.8 | ✓ | ✓ |
| 6 | 6.057 | Unknown | C17H24O11 | 404.1319 | [M + Na]+ | 427.1209 | −2.3 | — | ✓ |
| 7 | 7.092 | Lamalbide | C17H26O12 | 422.1424 | [M + Na]+ | 445.1325 | 0.2 | ✓ | ✓ |
| 8 | 8.599 | Penstemoside | C17H26O11 | 406.1475 | [M + Na]+ | 429.1402 | 6.3 | ✓ | ✓ |
| 9 | 8.802 | Sesamoside | C17H24O12 | 420.1268 | [M + Na]+ | 443.1158 | −2.3 | ✓ | ✓ |
| 10 | 10.093 | Unknown | C16H24O12 | 408.1267 | [M + Na]+ | 431.1163 | −0.9 | ✓ | ✓ |
| 11 | 10.127 | 8- | C18H26O12 | 434.1424 | [M + Na]+ | 457.1318 | −1.3 | ✓ | ✓ |
| 12 | 10.668 | Shanzhiside methyl ester | C17H26O11 | 406.1475 | [M + Na]+ | 429.1360 | −3.5 | ✓ | ✓ |
| 13 | 10.972 | 10-Methylixoside | C17H22O11 | 402.1162 | [M + Na]+ | 425.1046 | −3.8 | ✓ | ✓ |
| 14 | 11.398 | 6- | C19H28O12 | 448.1581 | [M + Na]+ | 471.1484 | 0.6 | ✓ | ✓ |
| 15 | 11.736 | Unknown | C17H22O11 | 402.1162 | [M + Na]+ | 425.1046 | −3.8 | — | ✓ |
| 16 | 11.803 | Phloyoside II | C17H25ClO12 | 456.1034 | [M + Na]+ | 479.0951 | 3.5 | ✓ | ✓ |
| 17 | 11.972 | 5-Desoxylamiide | C17H26O11 | 406.1475 | [M + Na]+ | 429.1360 | −3.5 | — | ✓ |
| 18 | 12.840 | Chlorotuberroside | C17H25ClO11 | 440.1085 | [M + Na]+ | 463.1010 | 5.4 | ✓ | ✓ |
| 19 | 13.466 | 7,8-Dehydropenstemo side | C17H24O11 | 404.1319 | [M + Na]+ | 427.1221 | 0.5 | ✓ | ✓ |
| 20 | 13.737 | 7,8-Dehydropenstemonoside | C17H20O10 | 388.1369 | [M + Na]+ | 411.1280 | 2.7 | ✓ | ✓ |
| 21 | 13.906 | Zaluzioside | C17H24O11 | 404.1319 | [M + Na]+ | 427.1221 | 0.5 | ✓ | ✓ |
| 22 | 14.703 | Deoxypulchelloside I | C17H26O11 | 406.1475 | [M + Na]+ | 429.1360 | −3.5 | ✓ | ✓ |
| 23 | 15.332 | Loganin | C17H26O10 | 390.1526 | [M + Na]+ | 413.1412 | −3.4 | ✓ | ✓ |
| 24 | 17.231 | 8- | C19H28O12 | 448.1581 | [M + Na]+ | 471.1484 | 0.6 | ✓ | ✓ |
| 25 | 17.772 | Unknown | C16H24O12 | 408.1267 | [M + Na]+ | 431.1171 | 0.9 | ✓ | ✓ |
| 26 | 18.231 | 7- | C17H26O10 | 390.1526 | [M + Na]+ | 413.1417 | −2.2 | ✓ | ✓ |
✓ have been detected, — not have been detected.
Fig. 3(A) MS2 spectra and (B) the fragmentation pathways of five compounds. (a) 5-Deoxypulchelloside I; (b) penstemoside; (c) shanzhiside methyl ester; (d) 5-desoxylamiide; (e) deoxypulchelloside I.
Fig. 4(a) PCA/Score plot of the aerial and root parts of L. rotata. (b) OPLS-DA/S-plot of the aerial and root parts of L. rotata. a: (tR 8.80 min, m/z 443.1158).
Fig. 5Selected ion intensity trend plots. a/sesamoside: (tR 8.80 min, m/z 443.1158) ▲: aerial parts; ●:roots.
Contents of the total IGS and antioxidant activity in 24 samples of L. rotataa
| Sample | Total IGS (mg g−1) | Antioxidant activity | Sample | Total IGS (mg g−1) | Antioxidant activity | ||
|---|---|---|---|---|---|---|---|
| DPPH (IC50 mg ml−1) | Reducing power (IC50 mg ml−1) | DPPH (IC50 mg ml−1) | Reducing power (IC50 mg ml−1) | ||||
| Tibet 01A | 20.03 ± 0.01 | 0.61 ± 0.01 | 33.34 ± 1.02 | Tibet 01R | 35.67 ± 0.10 | 0.58 ± 0.11 | 6.19 ± 0.54 |
| Tibet 02A | 19.78 ± 0.04 | 1.10 ± 0.14 | 8.26 ± 0.25 | Tibet 02R | 38.71 ± 0.02 | 0.31 ± 0.04 | 6.23 ± 0.35 |
| Tibet 03A | 20.09 ± 0.07 | 0.69 ± 0.07 | 5.23 ± 0.55 | Tibet 03R | 39.47 ± 0.07 | 0.55 ± 0.01 | 6.08 ± 0.61 |
| Sichuan 01A | 21.23 ± 0.03 | 1.29 ± 0.13 | 29.81 ± 1.33 | Sichuan 01R | 40.99 ± 0.15 | 0.37 ± 0.01 | 6.40 ± 0.59 |
| Sichuan 02A | 21.99 ± 0.05 | 1.30 ± 0.19 | 31.26 ± 1.39 | Sichuan 02R | 43.27 ± 0.07 | 0.37 ± 0.04 | 6.11 ± 0.58 |
| Sichuan 03A | 24.27 ± 0.10 | 1.32 ± 0.07 | 29.81 ± 0.92 | Sichuan 03R | 44.03 ± 0.01 | 0.21 ± 0.03 | 4.46 ± 0.42 |
| Qinghai 01A | 27.31 ± 0.01 | 0.55 ± 0.06 | 5.82 ± 0.48 | Qinghai 01R | 44.03 ± 0.11 | 0.06 ± 0.01 | 5.47 ± 0.33 |
| Qinghai 02A | 28.83 ± 0.01 | 0.73 ± 0.02 | 6.36 ± 0.41 | Qinghai 02R | 45.56 ± 0.03 | 0.28 ± 0.01 | 5.56 ± 0.51 |
| Qinghai 03A | 31.87 ± 0.01 | 0.40 ± 0.05 | 5.80 ± 0.39 | Qinghai 03R | 53.16 ± 0.01 | 0.25 ± 0.02 | 5.83 ± 0.41 |
| Gansu 01A | 32.63 ± 0.04 | 0.47 ± 0.07 | 5.67 ± 0.44 | Gansu 01R | 53.92 ± 0.03 | 0.28 ± 0.04 | 4.78 ± 0.23 |
| Gansu 02A | 32.63 ± 0.04 | 0.80 ± 0.14 | 5.93 ± 0.37 | Gansu 02R | 53.92 ± 0.08 | 0.24 ± 0.02 | 3.88 ± 0.11 |
| Gansu 03A | 33.39 ± 0.04 | 0.48 ± 0.05 | 6.20 ± 0.52 | Gansu 03R | 58.48 ± 0.02 | 0.26 ± 0.01 | 5.91 ± 0.47 |
| BHT | 0.01 ± 0.001 | 0.10 ± 0.01 | |||||
A – the aerial parts of L. rotata, R – the root of L. rotata, each value represents the mean of three determinations (n = 3) and three independent experiments ± standard deviation.