Essentional oil ratio
The essential oil content and composition of the plant part to be used as a drug in medicinal and aromatic plants are the most important criteria that designate the quality of the product [28, 29]. Previous studies have revealed that genetic structure of the plant material used in production and ecological conditions of the region where the production is made had significant effects on essential oil ratios of aromatic plants [30–34].
Effects of altitude on essential oil ratios are provided in Table 2 and altitude differences were found to be significant (p < 0.001). Essential oil ratios of the samples varied between 4.67–6.50%, with the highest value (6.50%) from 766 m altitudes and the lowest value (4.67%) from 1079 m altitudes. Essential oil ratios decreased with increasing altitudes, but such a decrease was placed into the same statistical group, except for the altitudes of 800–900 m (5.43%) and 1079 m (4.67%). Altitude-dependent differences in essential oil ratios were mainly attributed to ecological factors that change with altitudes [35]. Essential oil ratios of medicinal and aromatic plants usually vary with the climate components such as temperature, precipitation, relative humidity, day light hours, light intensity, soil conditions and development period [31, 36, 37]. The highest essential oil ratio of 766 m altitudes could be attributed to greater air temperature and relative humidity than the other altitudes (Table 2).
Table 2
Descriptive statistics for essential oil ratios of Origanum majarona species
Altitude (m) | Essential oil ratio (%) |
766 | 6.50 ± 0.23a |
890 | 5.43 ± 0.46bc |
968 | 6.15 ± 0.46ab |
1079 | 4.67 ± 0.43c |
1180 | 5.85 ± 0.08ab |
1261 | 5.68 ± 0.28ab |
1387 | 5.73 ± 0.25ab |
p: 0.0004*** |
Difference in means indicated with different letter in the same column is significant (***p < 0.001) |
The factors that alter essential oil ratios of aromatic plants should be well-comprehended [34, 38], since pharmacopoeias specify the minimum essential oil ratios that aromatic plants must contain in order to be accepted as drugs and used as medicine and drugs containing essential oils below these ratios are not allowed to be used as medicine [39].
Essential Oil Components
Majority of the terpenes produced by plants are products of secondary metabolism and play an important role also in primary metabolism. These terpenoid structures, with their highly complex chemical structures, show great variation within and between the species and constitute the natural defense system of plants by damaging the other living things [40].
The GS-MS analysis revealed 69–126 terpenoid structures for essential oils of Origanum majorana samples collected from different altitudes. Terpenoid ratios varied between 0.01–79.84%. The differences in ratios of all components with altitude were found to be significant (p < 0.001). Analyses on Oregano, Thyme and Marjoram species revealed that mono and sesquiterpenes were the major components of essential oils of these species [41]. In this study, the ratio of oxygenated monoterpenes that form the essential oil and the terpenoid structure of Origanum majorana plants collected from different altitudes ranged between 65.69–84.62% and took the first place in total amount of essential oil. Oxygenated monoterpene ratios mathematically decreased with increasing altitudes, but there was no linear increase or decrease in oxygenated sesquiterpene ratios. Similar findings were also reported by [42]. Oxygenated monoterpenes were respectively followed by phenolic monoterpene (3.29–25.91%), sesquiterpene hydrocarbons (2.92–5.94%), oxygenated sesquiterpene (0.92–1.63%) and monoterpenes hydrocarbons (0.04–0.17%) (Table 3).
In studies on essential oil composition of Origanum majorana, major components of essential oils were reported as terpinene-4-ol and sabinene hydrate by [43] and as thymol and carvacrol by [14]. In this study, the major component was linalool (60.86–79.84%), an Oxygenated monoterpene. Linalool is an essential oil component used in soaps, cosmetics, perfumes, cleaning products, food preservatives, herbicides and insecticides. Linalool, which has strong antimicrobial and antioxidant properties, is the essential oil component of many medicinal and aromatic plants belonging to Lamiaceae, Lauraceae and Rutaceae families [44].
Both within the oxygenated monoterpene group components and among the other components that make up the essential oil, linalool ratios varied between 79.84% at 766 m altitudes and 60.86% at 1387 m altitudes. These values were the highest values among the total essential oil components. Linalool ratios decreased significantly (p < 0.001) with increasing altitudes. Similarly, greater linalool oxide (890 m: 1.28%) and trans-linalool oxide (890 m: 1.47%, 968 m: 1.30%, 1079 m: 1.31%) ratios were seen at lower altitudes. Linalool and linalool oxide ratios generally decrease with decreasing temperatures of high altitudes. Previous researchers emphasized that increase in phenolic components was positively affected by regional high temperatures [41, 45–47]. The cis-sabinene hydrate (0.82%) and terpinene-4-ol (0.55%) ratios were positively affected by increasing altitudes (p < 0.001) and the highest values of both were seen at 1387 m altitudes. The a-terpineol ratio of 0.55% at 766 m altitudes increased to 1.04% at 1079 m altitudes and borneol ratio of 0.32% at 766 m increased to 0.97% at 890 m altitudes and the difference was found to be significant (p < 0.001). The lowest 1,8-cineol ratio was determined as 0.08% at 766 m and the highest ratio as 0.33% at 968 m altitudes. Researchers have reported that differences in temperature, relative humidity, wind speed and light intensity as you go to higher altitudes above sea level will change the physiological reactions of the plant and thus will create variations in composition of secondary metabolites [25, 48, 49].
Thymol content within total essential oil was measured as 0.32% at 766 m, 0.44% at 890 m, 0.49% at 968 m, 0.45% at 1079 m and 0.99% at 1261 m altitudes. These values were statistically placed into the same group. Thymol ratio was 6.28% at 1180 m altitudes and 4.41% thymol was detected at 1387 m, which is the highest altitude and the the first place statistically.
Table 3
Chemical composition of Origanum majorana essential oil
Components | f | 700–800 | 800–900 | 900–1000 | 1000–1100 | 1100–1200 | 1200–1300 | 1300–1400 |
Monoterpenes hydrocarbons | | 0.06 | 0.04 | 0.08 | 0.07 | 0.11 | 0.13 | 0.17 |
α- terpinene | 0.0001*** | 0.06 ± 0.006de | 0.04 ± 0.0e | 0.08 ± 0.0cd | 0.07 ± 0.01de | 0.11 ± 0.01bc | 0.13 ± 0.03b | 0.17 ± 0.02a |
Oxygenated monoterpen | | 83.13 | 82.93 | 84.62 | 84.11 | 71.43 | 75.90 | 65.69 |
Linalool | 0.0001*** | 79.84 ± 1.10a | 77.75 ± 3.03ab | 79.68 ± 2.11ab | 79.20 ± 0.63ab | 67.62 ± 0.13cd | 71.53 ± 4.21bc | 60.86 ± 5.23d |
α- terpineol | 0.0001*** | 0.55 ± 0.02d | 0.63 ± 0.05cd | 0.76 ± 0.05bc | 0.88 ± 0.13ab | 1.04 ± 0.00a | 0.90 ± 0.02ab | 0.86 ± 0.09ab |
Borneol | 0.0001*** | 0.32 ± 0.02e | 0.97 ± 0.04a | 0.83 ± 0.04abc | 0.87 ± 0.04ab | 0.65 ± 0.01d | 0.77 ± 0.01bcd | 0.69 ± 0.15cd |
Cis-sabinene hydrate | 0.0002*** | 0.27 ± 0.01b | 0.28 ± 0.02b | 0.30 ± 0.03b | 0.44 ± 0.07b | 0.39 ± 0.0b | 0.43 ± 0.03b | 0.82 ± 0.26a |
Terpinen 4-ol | 0.0001*** | 0.22 ± 0.01d | 0.24 ± 0.03d | 0.34 ± 0.04bc | 0.28 ± 0.02cd | 0.42 ± 0.00b | 0.43 ± 0.02b | 0.55 ± 0.07a |
1,8-cineole | 0.0010*** | 0.08 ± 0.0d | 0.31 ± 0.0ab | 0.33 ± 0.0a | 0.14 ± 0.0bcd | 0.13 ± 0.0cd | 0.25 ± 0.0a'd | 0.28 ± 0.0abc |
Linalool oxide | 0.0007*** | 0.75 ± 0.02bc | 1.28 ± 0.05a | 1.08 ± 0.04ab | 0.99 ± 0.07abc | 0.63 ± 0.16c | 0.74 ± 0.23bc | 0.82 ± 0.07bc |
Trans- linalool oxide | 0.0001*** | 1.10 ± 0.03ab | 1.47 ± 0.01a | 1.30 ± 0.01a | 1.31 ± 0.31a | 0.55 ± 0.01c | 0.85 ± 0.26bc | 0.81 ± 0.09bc |
Phenolic monoterpen | | 3.29 | 4.99 | 5.76 | 3.70 | 19.93 | 14.89 | 25.91 |
Thymol | 0.0001*** | 0.32 ± 0.02c | 0.44 ± 0.11c | 0.49 ± 0.17c | 0.45 ± 0.09c | 6.28 ± 0.03a | 0.99 ± 0.53c | 4.41 ± 1.15b |
Carvacrol | 0.0001*** | 2.97 ± 0.13c | 4.55 ± 1.90c | 5.27 ± 1.54c | 3.25 ± 0.79c | 13.65 ± 0.05b | 13.90 ± 3.95b | 21.50 ± 5.25a |
Sesquiterpene hydrocarbons | | 4.82 | 5.94 | 4.44 | 4.89 | 4.78 | 4.01 | 2.92 |
Caryophyllene | 0.0001*** | 2.76 ± 0.06a | 2.78 ± 0.10a | 2.41 ± 0.0ab | 2.42 ± 0.23ab | 2.29 ± 0.01b | 1.61 ± 0.03c | 1.80 ± 0.25c |
α-humulene | 0.0006*** | 0.15 ± 0.01bc | 0.21 ± 0.02a | 0.15 ± 0.01bc | 0.16 ± 0.02abc | 0.13 ± 0.00bc | 0.16 ± 0.04ab | 0.11 ± 0.02c |
Germacrene-D | 0.0001*** | 0.18 ± 0.01bc | 0.31 ± 0.02a | 0.20 ± 0.01bc | 0.32 ± 0.01a | 0.22 ± 0.01b | 0.29 ± 0.04a | 0.17 ± 0.0c |
Bicyclogermacrene | 0.0001*** | 1.73 ± 0.04c | 2.64 ± 0.17a | 1.68 ± 0.05c | 1.99 ± 0.17bc | 2.14 ± 0.01b | 1.95 ± 0.26bc | 0.84 ± 0.02d |
Oxygenated sesquiterpene | | 1.11 | 1.27 | 1.32 | 1.63 | 0.92 | 1.20 | 1.18 |
Caryophyllene oxide | 0.0001*** | 0.26 ± 0.02b | 0.33 ± 0.03ab | 0.31 ± 0.03ab | 0.35 ± 0.01a | 0.15 ± 0.01c | 0.18 ± 0.040c | 0.30 ± 0.04ab |
Sapthulenol | 0.0067*** | 0.85 ± 0.22b | 0.94 ± 0.15ab | 1.01 ± 0.14ab | 1.28 ± 0.08a | 0.77 ± 0.02b | 1.02 ± 0.12ab | 0.88 ± 0.09b |
Others | | 7.59 | 4.83 | 3.78 | 5.60 | 2.83 | 3.87 | 4.13 |
Total (%) | | 100 | 100 | 100 | 100 | 100 | 100 | 100 |
In the same row, the difference between the component ratios without a common letter is significant (***p < 0.001)
High levels of carvacrol are encountered in Origanum, Thymbra, Cordiothymus, Satureja and Lippia species. Increasing carvacrol ratios were seen with increasing altitudes and the greatest value (21.50%) was seen at 1387 m altitudes. The increase in both thymol and carvacrol ratio with increasing altitude may be due to the prolongation of the growth period and the emergence of sufficient vegetation period for the conversion of intermediate components to these two components [41]. At high altitudes, plants are exposed to higher light intensity and lower average temperature. Therefore, plants at high altitudes have developed a protection mechanism against climate-induced damages. Plants adapted to high altitudes perform photosynthesis more effectively at low temperatures [50–52]. Previous studies indicated that carvacrol ratios increased with increasing altitudes [53] and carvacrol ratios increased under stress conditions arising from environmental conditions [54].
The a-terpinene represents monoterpenes hydrocarbons and the least encountered in monoterpene structures of Origanum majarona essential oil. The greatest value (0.17%) was seen at 1387 m altitudes. Previous researchers also reported that climate and environmental factors affected the essential oil composition [20, 55, 56].
Caryophyllene is also a constituent of sesquiterpene hydrocarbon structure. Caryophyllene ratio was determined as 2.76% at 766 m and 2.78% at 890 m altitudes and they were placed into the same statistical group. Caryophyllene ratios decreased with increasing altitudes and decreased to 1.61% at 1261 m and 1.80% at 1387 m altitudes. The a-humulene (0.21%) and bicyclogermacrene (2.64%) ratios had the highest values at altitude of 890 m altitudes. At the highest altitudes (1387 m), a-humulene ratio decreased to 0.11% and bicyclogermacrene to 0.84%. Like the other sesquiterpene hydrocarbons, the lowest germacrene-D ratio (0.17) was seen at 1387 m altitudes and germacrene-D ratios at 890 m (0.31%), 1079 m (0.32%) and 1261 m (0.29%) altitudes were placed into the same highest group. In some specific studies, it was indicated that chemical metabolic profiles of plants belonging to Lamiaceae family with pharmacological properties, were affected by abiotic and biotic factors such as ecological conditions, soil profile, weeds, diseases and pests, harvest periods, geographical region and especially altitude [20, 21, 57].
Caryophyllene oxide is a compound of oxygenated sesquiterpene group. The greatest caryophyllene oxide ratio (0.35%) was seen at 1079 m altitudes, while the lowest values were obtained seen at 1180 m (0.15%) and 1261 m (0.18%) altitudes. Spathulenol ratios varied between 0.85–1.28% and differences were found to be significant (p > 0.001). It was determined that caryophyllene oxide and spathulenol ratios of the samples collected from both low and high altitudes did not exhibit a linear increase or decrease.
Climate parameters vary with the altitudes. Altitude has significant effects on yield levels, essential oil ratios and compositions [58, 59, 60]. Temperature, precipitation, relative humidity, day light hours, light intensity and day and night temperature differences change with altitude [31]. Altitude-dependent changes in oxygenated sesquiterpene ratios such as caryophyllene oxide and spathulenol can be explained by prevailing ecological factors of altitudes.