Simulating the effects of climate change across the geographical distribution of two medicinal plants in the genus Nardostachys

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Biodiversity and Conservation

Introduction

According to the Chinese Pharmacopoeia, the medicinal plants of Radix et Rhizoma Nardostachyos include Nardostachys jatamansi and N. chinensis (Pharmacopeia Committee of P. R. China, 2010). These species are perennial, rhizomatous, in the family Valerianaceae (Airi et al., 2000). N. jatamansi is about 5–50 cm in height, with a thick and long woody stem. The dark gray main root is thick and long, densely covered with the leaf sheath fibers, with strong fragrance (Bhat & Malik, 2017; Zhang et al., 2016). The main difference between N. jatamansi and N. chinensis is that the obliquely stretched rhizome of the N. jatamansi, which with more dense leaf-based fibers to cover the stem, and the corolla tube is wider and shorter (Flora of China Editorial Committee, 2006). Also, N. jatamansi is mainly found growing between altitudes of 3,300–5,000 m, and it originated to the elevated ranges of the Himalayas in Nepal but also found in the high lands of Sikkim, Bhutan, and Punjab (Malik, Firdose & Bhat, 2018). In China, these species were primarily distributed in the eastern part of the Tibetan Plateau and its margins (Flora of China Editorial Committee, 2006). Although there are some differences in the morphology and distribution of these two species, they contain similar active ingredients and medical efficacy (An Editorial Committee of the Administration Bureau of Traditional Chinese Medicine, 2000). These rhizomes have been used in Chinese traditional medicine. Their medicinal properties include anti-epileptic, anticonvulsant, anti-depressant, anti-inflammatory, sedation, antiarrhythmic, antiparkinson, antibacterial, hypolipidemia, hepatoprotection, and nerve development (Ahmad et al., 2013). Recent research showed that the rhizome contains chemical components such as sesquiterpenes, flavonoids, polysaccharides, and lignans (Chatterjee et al., 2005). Because of the high content and special aroma of sesquiterpenes, these species have also been used for flavoring (Le et al., 2017).

Due to their wide application in medicine, food, cosmetics, and other industries, the market demand for the two species was increasing. However, due to the underdevelopment of the cultivation technology of Nardostachys, the industry mainly depended on wild resources. To meet the demands of the market, excessive wild collection has led to a sharp decrease in wild Nardostachys populations and serious habitat destruction. Measures need to be taken to protect the species and develop artificial planting technology for them.

The development of effective cultivation and protection of Nardostachys species is required to better meet the market demands and sustainably use the species. For long-term and effective development of cultivation of the Nardostachys species, it is essential to understand its suitable climate and geographic distribution in future.

Environmental factors have significant influences on the distribution of species. Global climate change is occurring at an unprecedented rate. And the global temperatures are expected to rise significantly in this century, even the greenhouse gas concentrations remain constant at the year 2000 levels (Rivaes et al., 2013). Representative concentration pathways (RCPs) were used in climate modeling and research to describe the four possible future climates in the fifth assessment report of the Intergovernmental Panel on Climate Change (IPCC, 2013). The four RCPs (RCP2.6, RCP4.5, RCP6, and RCP8.5) are named in the possible range of Radiative Forcing values in the year 2100 relative to pre-industrial values (+2.6, +4.5, +6.0, and +8.5 W/m2, respectively) (Ma & Sun, 2018).

Species distribution models could simulate the potential ecological niche of a species from various hypotheses about how environmental factors control the distribution of species and communities based on known occurrence points (Zhang et al., 2016). Therefore, the species distribution models could provide the basis for planting land selection and growing climatic conditions during the cultivation of the two plants. The main species distribution models for species distribution predictions include Bioclim, Climex, Domain, Garp, and Maxent maximum entropy modeling. Among these models, the Maxent model has a strong advantage in predicting species distribution and gained popularity, which is a presence-only modeling technique using a machine learning approach (Phillips, Anderson & Schapire, 2006). The Maxent model has successfully completed the prediction of the potential geographical distributions of multiple species for the past few years, including Fritillaria cirrhosa, Lilium nepalense, Phellodendron amurense Rupr, and Atractylodes lancea (Rana et al., 2017; Wan et al., 2014; Shoudong et al., 2017; Zhao et al., 2018).

Radix et Rhizoma Nardostachyos is an endangered and valuable Chinese herbal medicine that needs to be protected and developed. Moreover, its two medical plants with similar medical effects, and more importantly, the two species are on the verge of extinction. For better utilization and development of Radix et Rhizoma Nardostachyos, climate change was used as a screening factor to select one species that is more suitable for artificial cultivation. The subject of this paper is to discover the effects of climate change on the two species by the Maxent model, and provide a basis for their artificial cultivation.

Materials and methods

The complete analysis workflow was summarized in Fig. 1.

The processing method in the flowchart.

Figure 1: The processing method in the flowchart.

The study mainly included three processes of data preparation, Maxent simulation, and comprehensive evaluation.

Basic geographic data

A total of 1:400,000 vector map of China’s administrative divisions was downloaded from the national basic geographic information system as the base map for the analysis.

Study area

N. jatamansi and N. chinensis were mainly distributed in subalpine to alpine areas, where the elevation is more than 3,000 m. The Qinghai–Tibetan Plateau is the main distribution area, ranging from 25° to 40°N, 74° to 104°E. The Qinghai–Tibetan Plateau is the world’s highest plateau, with an altitude of between 3,000 and 5,000 m and an average elevation of over 3,500 m. The climate of the Qinghai–Tibetan Plateau is monsoonal. The annual average temperature in most parts of the region is below 8 °C, and the annual precipitation is 400–900 mm/year.

Data collection

Occurrence records of N. jatamansi and N. chinensis were mainly obtained through online databases and consulting literature. The online database includes the Chinese Virtual Herbarium (http://www.cvh.ac.cn/), Specimen Resources Sharing Platform for Education (http://mnh.scu.edu.cn/), and Global Biodiversity Information Facility (https://www.gbif.org/). The literature used was open-source and available worldwide. In the absence of specific geographical coordinate records, Google Earth 7.0 was utilized to find the approximate latitude and longitude according to the described geographical location. After duplicate and invalid records were removed, the sampling points of N. jatamansi and N. chinensis were 183 and 60, respectively. We obtained sampling points from the specimen database and literature, and all the specimens collected in the specimen database are wild. In accordance with the requirements of the Maxent software, the distribution records of N. jatamansi and N. chinensis were organized into .csv format files including the species name and distribution point longitude and latitude, with the east and north latitudes positive and the west and south latitudes negative.

Environmental variables

Climate variables are crucial in simulating the distribution of species. This article mainly analyzed the impact of climate change on the distribution of N. jatamansi and N. chinensis. Refer to other literature, 19 bioclimatic variables with 2.5-min resolution of the current conditions and future conditions (2050s and 2070s) were downloaded from the WorldClim-Global Climate Data (http://worldclim.org/) (Suwannatrai et al., 2017). The 2.5-min resolution could meet the simulation requirements based on the published article (Bai, Wei & Li, 2018; Qu, Wang & Zhang, 2018). These variables are derived from monthly temperature (maximum and minimum) and rainfall data, which express seasonality, annual trends and extreme conditions (Mendoza-Gonzalez et al., 2013). The 19 bioclimatic variables with strong biological significance explained the adaptation of species with extreme environmental factors. Here, two greenhouse gas concentration scenarios, RCP 2.6 (the minimum greenhouse gas emission scenario) and RCP 8.5 (the maximum greenhouse gas emission scenario) were selected under the CCSM4 (The Community Climate System Model version 4.0) model in this work. Referring to the research of Ma & Sun (2018), RCP2.6 and RCP8.5 are the most common emissions scenarios. The CCSM4 climate model, which was developed by the National Center for Atmospheric Research of the United States, has been thoroughly evaluated in China. It has recently been verified that the CCSM4 model can better simulate the climate characteristics of East Asia (Tian & Jiang, 2013).

Distribution modeling

The Maxent model was a widely used and effective model for species distribution modeling because it produced believable results. It is based on the freely available Maxent software V3.3.3k (https://github.com/mrmaxent/Maxent/blob/master/ArchivedReleases/3.3.3k/maxent.jar). Maxent was used to predict the current and future potential distributions of N. jatamansi and N. chinensis based on the occurrence records and climate data. The logical output (results are expressed in terms of probability) was selected to assess the likelihood of the presence of a species in each grid cell. A total of 25% of the occurrence records were chosen as the test set, and the remaining parameters were the default settings (Yi et al., 2016). Jackknifing in the environment parameter settings was checked to measure the percentage contribution of each environmental variable and to evaluate the importance of environmental factors in affecting the geographical distribution of species.

The area under the receiver operating curve, called AUC, was used to evaluate the accuracy of the prediction results (Zhang et al., 2016). AUC values range from zero to one, and the larger the AUC value, the farther away from the random distribution. High AUC values indicate the better prediction of the model. AUC values generally range from 0.5 to 0.7 when accuracy is low; moderate accuracy is generally 0.7∼0.9; a high degree of accuracy is typically greater than 0.9 (Wakie et al., 2014).

Results

Occurrences of N. jatamansi and N. chinensis

Figure 2 showed the original occurrences of N. jatamansi and N. chinensis were mainly distributed in Sichuan Province, parts of Yunnan, Gansu, and Qinghai Provinces, and the Tibetan Autonomous Region. The main areas in which N. jatamansi was distributed were the Tibetan Autonomous Region, Sichuan Province, Yunnan Province, and a small part of Qinghai and Gansu Provinces. In addition, N. jatamansi was also distributed in other countries including India and Nepal. Hence, the distribution of N. jatamansi is more extensive than that of N. chinensis.

The original occurrence records.

Figure 2: The original occurrence records.

Red dots represented georeferenced locations of 60 occurrences of N. chinensis (A), and black dots represented georeferenced locations of 183 occurrences of N. chinensis in Qinghai–Tibetan Plateau (B).

Predicting the distribution under current conditions

Figures 3A and 3F showed the predicted area of distribution for N. jatamansi and N. chinensis by the Maxent model under the current climate conditions. The simulation output results from the Maxent software are between zero and one. According to a previously published article by Wang et al. (2014), the results were divided into four levels: 0–0.05, 0.05–0.25, 0.25–0.5, and 0.5–1. Elith et al. (2011) considered that the average probability of species being present in suitable areas was 0.5. For the two species in this study, the area with probabilities above 0.5 was the main natural distribution area. Thus, the probabilities above 0.5 was defined as suitable habitats, and probabilities less than 0.5 were unsuitable based on the study of Wang et al. (2018).

Present (A and F), and future (B–E and G–J) potential spatial distribution of N. jatamansi and N. chinensis.

Figure 3: Present (A and F), and future (B–E and G–J) potential spatial distribution of N. jatamansi and N. chinensis.

Future predictions (2050s and 2070s) were based on two representative concentration pathways under CCSM4 climate model.

As showed in Figs. 3A and 3F, suitable areas under current conditions of N. jatamansi were mainly distributed in the Qinghai–Tibetan Plateau in China, including western parts of Sichuan Province, northern Yunnan Province, the eastern part of the Tibetan Autonomous Region, and a small part of southern Qinghai and Gansu Provinces. In addition, it has a small suitable area in India, Bhutan, and Nepal. Among these distributions, the suitable areas of Sichuan, Tibet, and Yunnan are extensive and concentrated in the high mountain plateau region, which was roughly in line with the records of the distribution of N. jatamansi.

Suitable areas of N. chinensis were mainly distributed at the junction of the Tibetan Autonomous Region and Sichuan and Qinghai Provinces in China. Sichuan Province has the most suitable habitats. This was consistent with the collection records from Sichuan, indicating that N. chinensis was primarily distributed in the province, and no suitable habitats were indicated in other countries. According to the prediction, the area in which N. jatamansi is distributed was significantly larger than the distribution of N. chinensis under current conditions.

The effects of climate change on the geographical distribution of N. jatamansi and N. chinenis

Figures 3B3E and 3G3J showed the potential geographical distributions of N. jatamansi and N. chinenis predicted by the Maxent model under the CCSM4 of the 2050s and 2070s. There was an overall upward trend in the area of suitable habitats for N. jatamansi and N. chinensis (Fig. 4).

The area of suitable habitats of N. jatamansi and N. chinensis for present and future conditions predicted by Maxent based on CCSM4 climate model.

Figure 4: The area of suitable habitats of N. jatamansi and N. chinensis for present and future conditions predicted by Maxent based on CCSM4 climate model.

There was an overall upward trend in the area of suitable habitats for N. jatamansi and N. chinensis.

By 2050, suitable areas (RCP2.6 and RCP8.5) of N. jatamansi increased. Relative to the current situation, both ranges increased in RCP2.6 and RCP8.5 with a greater growth rate under RCP8.5. The scope of suitable areas in Qinghai and Tibet increased obviously and exhibited a trend of northward expansion. Suitable areas of N. chinensis under RCP2.6 and RCP8.5 emissions scenarios also increased compared to the current situation. The scope of suitable areas in western Sichuan Province and Tibet increased obviously and also exhibited a trend of northward expansion.

By 2070, the area of suitable habitats for N. jatamansi under the RCP2.6 emission scenario will continue to grow. However, the range of suitable areas under the RCP8.5 emission scenario was significantly reduced and was significantly lower than the current level. The results showed that the climate-suitable area decreased in the 2070s under the RCP8.5 climate scenario compared to the current period.

Suitable areas of N. chinensis under RCP2.6 also continued to increase, relative to the 2050s and the present. Suitable areas of N. chinensis under RCP8.5 still increased compared to the present. However, suitable areas of N. chinensis under RCP8.5 decreased from the 2050s.

Contribution of environmental variables

A total of 19 bioclimatic variables from the BIOCLIM climate dataset were used as the background environmental data, such as temperature and rainfall. These variables are comprehensive conclusions and quantitative descriptions of the climatic environment in the regions containing the targeted species. The potential distributions of N. jatamansi and N. chinensis were simulated by the Maxent model, which automatically predicted the contribution percentage of each variable to the forecasted results. Table 1 listed selected bioclimatic variables and their percent contribution in the Maxent model for N. jatamansi and N. chinensis in their current distribution range. Among them, precipitation of the driest period (Bio14) was the largest contributing factor when modeling the distributions of N. jatamansi and N. chinensis.

Table 1:
Bioclimatic variables used for model construction and their percentage contribution in predicting the current distribution of N. jatamansi and N. chinensis using MaxEnt.
Abbreviation Description Percent contribution
N. jatamansi N. chinensis
Bio1 Annual mean temperature (°C) 0.8 1.5
Bio2 Mean diurnal range (mean of monthly (max temp–min temp)) (°C) 0.1 0
Bio3 Isothermally (Bio2/Bio7) (×100) 15.4 7.7
Bio4 Temperature seasonality (standard deviation × 100) (C of V) 0.1 0
Bio5 Max temperature of warmest month (°C) 5.2 8.1
Bio6 Min temperature of coldest month (°C) 0.5 3.4
Bio7 Temperature annual range (Bio5–Bio6) (°C) 0.3 0.3
Bio8 Mean temperature of wettest quarter (°C) 9.6 9.6
Bio9 Mean temperature of driest quarter (°C) 0.3 0
Bio10 Mean temperature of warmest quarter (°C) 5.3 2.7
Bio11 Mean temperature of coldest quarter (°C) 0.2 0
Bio12 Annual precipitation (mm) 0.2 0.1
Bio13 Precipitation of wettest month (mm) 13 15.2
Bio14 Precipitation of driest month (mm) 36 36
Bio15 Precipitation seasonality (C of V) 0.6 0.1
Bio16 Precipitation of wettest quarter (mm) 0.1 2.5
Bio17 Precipitation of driest quarter (mm) 8.6 0.2
Bio18 Precipitation of warmest quarter (mm) 0.5 0.1
Bio19 Precipitation of coldest quarter (mm) 3.4 12.6
DOI: 10.7717/peerj.6730/table-1

The jackknife test also showed that precipitation of the coldest quarter (Bio19), precipitation of the driest quarter (Bio17), and precipitation of the driest period (Bio14) were the main variables in the simulation of N. chinensis (Fig. 5). However, isothermality (Bio3), precipitation seasonality (Bio15), and precipitation of the driest period (Bio14) were the main factors affecting the modeled distribution of N. jatamansi (Fig. 5).

The Jackknife test for evaluating the relative importance of environmental variables for N. chinensis (A) and N. jatamansi (B).

Figure 5: The Jackknife test for evaluating the relative importance of environmental variables for N. chinensis (A) and N. jatamansi (B).

The blue, aqua, and red bars represent the results of the model created with each individual, all remaining variables, and all the variables, respectively.

Figure 6 showed the response curves for single climate variables in the Maxent forecast of N. jatamansi and N. chinensis. Response curves indicated the correlation between the environmental variables used for prediction and the probability of the presence of N. jatamansi and N. chinensis. In Fig. 6, Bio14 response curves peak in the distribution predictions of N. jatamansi and N. chinensis. The distribution probability of N. jatamansi and N. chinensis increased with the increase of variable value. After exceeding this peak, the distribution probability decreased with the increase of the value for environmental factors, indicating that N. jatamansi and N. chinensis have some adaptability to these variables. When the probability is greater than 0.5, the corresponding ecological factor value is more suitable for the growth of the plant.

The response curves of precipitation of driest month under the current period for N. chinensis (A) and N. jatamansi (B).

Figure 6: The response curves of precipitation of driest month under the current period for N. chinensis (A) and N. jatamansi (B).

Response curves indicated the correlation between the environmental variables used for prediction and the probability of the presence of N. jatamansi and N. chinensis.

The prediction showed that the best ranges for these indicators were precipitation of the driest month, one to five mm for N. chinensis and 0–10 mm for N. jatamansi. The optimum range of precipitation of the driest month is very narrow, indicating that N. jatamansi and N. chinensis were sensitive to precipitation.

Discussion

With global warming, upon changes in temperature, precipitation, and CO2 concentration, and the changes in certain climatic resources changed the dynamics and balance of different species, thereby affecting their productivity (Rivaes et al., 2014). When the distributions of climate resources adapting to N. jatamansi and N. chinensis change, the geographical distributions also undergo corresponding changes. The temperature increases strongly under RCP8.5 and may exceed the suitable temperature for plant growth (Lv & Zhou, 2018). Thus, the climate-suitable area decreased in the 2070s under the RCP8.5 climate scenario compared to the current period.

This indicated that more areas will be suitable for the distribution of N. jatamansi, which would have greater potential for expansion in China in the future under a low-emission scenario, contrary to high-emission scenarios. In addition, suitable areas in Qinghai and Tibet decreased obviously and exhibited a trend of northward expansion. Nevertheless, suitable sites in the high altitude area of Tibet markedly increased. And previous studies have shown that with global warming, some species will migrate to high latitude or high elevation (Zhang et al., 2018). The variation of the suitable area of N. jatamansi was consistent with this result.

Ma & Sun (2018) had predicted the distribution of Stipa purpurea across the Tibetan Plateau via the Maxent model. The habitat suitability of S. purpurea in RCP2.6 and RCP8.5 revealed that the habitat suitability for the species increased from the 1990s to 2050s, then decreased from the 2050s to 2070s. Their results indicated the trend of the suitable habitat area was consistent with our prediction. However, they also considered the impact of topographic variables in the study, which was our shortcoming.

According to the above results, the suitable habitat N. jatamansi varies greatly under different climate scenarios and was more affected by climate change. However, the potential distributions of N. chinensis showed a growing trend in different climate scenarios compared to its current situation and was less affected by climate change. Therefore, in order to avoid the impact of climate change on the artificial cultivation of the genus Nardostachys, and achieve stable development, we could choose N. chinensis as the main cultivated species.

Studying the interaction between species and the environment is an essential aspect of species cultivation. The relationship between the probability of species presence and dominant environmental variables was analyzed in this paper. The percent contribution of bioclimatic variables, the jackknife test and the response curves were created by the MaxEnt software.

According to the results of above forecase, we can conclude that precipitation of the driest period is the most important environmental factor affecting the growth of N. chinensis and N. jatamansi. The research has shown that while comparing the distribution of the two contrasting hill slopes (east and west), the density of N. jatamansi has increased significantly with altitude was revealed on a west-facing slope. And the north and west-facing slopes in the alpine zone of this region are broadly considered as the shady areas with low light and high moisture (Airi et al., 2000). The advantage of high water and nutrient supply for rhizome and root production has also been reported elsewhere for related valerian species (Bernath, 1997). These results indicated that the precipitation plays a dominant role in simulating the effects of climate change on N. jatamansi and N. chinensis compared to temperature and other environmental variables.

The analysis for the response curves showed that the probability of species presence changed as a result of the dominant environmental variables. The results indicated that N. jatamansi and N. chinensis were sensitive to precipitation. Thus, this showed that research on water management should be strengthened for future cultivation practices.

Conclusion

The results of this Maxent simulation of climate change impacts on the distribution of two Nardostachys species and prediction of their potential distributions under current and future climate conditions are reliable. Considering the effects of climate change, N. chinensis is more suitable for cultivation. In addition, precipitation of the driest period is an important factor in the impact of climate change on N. jatamansi and N. chinensis. It is of great significance to study the impact of climate change on the genus Nardostachys to predict their potential distribution in the future for the protection, sustainable use, and value assessment of these biological resources. It is essential to conduct future studies on the effect of watering of N. chinensis for developing effective techniques to cultivate N. chinensis. The study will provide references for the cultivation planning and resource utilization of N. jatamansi and N. chinensis.

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