Potential distribution of Notopterygium incisum Ting ex H. T. Chang and its predicted responses to climate change based on a comprehensive habitat suitability model

Abstract

Notopterygium incisum Ting ex H. T. Chang is a rare and endangered traditional Chinese medicinal plant. In this research, we built a comprehensive habitat suitability (CHS) model to analyze the potential suitable habitat distribution of this species in the present and future in China. First, using nine different algorithms, we built an ensemble model to explore the possible impacts of climate change on the habitat distribution of this species. Then, based on this model, we built a CHS model to further identify the distribution characteristics of N. incisum‐suitable habitats in three time periods (current, 2050s, and 2070s) while considering the effects of soil and vegetation conditions. The results indicated that the current suitable habitat for N. incisum covers approximately 83.76 × 10³ km², and these locations were concentrated in the Tibet Autonomous Region, Gansu Province, Qinghai Province, and Sichuan Province. In the future, the areas of suitable habitat for N. incisum would significantly decrease and would be 69.53 × 10³ km² and 60.21 × 10³ km² in the 2050s and 2070s, respectively. However, the area of marginally suitable habitat would remain relatively stable. This study provides a more reliable and comprehensive method for modelling the current and future distributions of N. incisum, and it provides valuable insights for highlighting priority areas for medicinal plant conservation and resource utilization.

Built a comprehensive habitat suitability model (CHS) for Notopterygium incisum, which constructed separately for the climate, vegetation, and soil environment demands. Climate change will intensify the destruction and fragmentation of native habitats of N. incisum, which will lead to the disappearance of suitable habitat in these areas, increasing the risk of the extinction of this species.

1. INTRODUCTION

The growth, development, and reproduction of plants are limited by climatic and other environmental factors. Global warming is likely to result in changes in biological habitats, losses of regional species diversity, and increases in the risk of species extinction (Anderson, 2013; Marzloff et al., 2018; Pacifici et al., 2015; Urban, 2015). Topography affects the redistribution of moisture and heat in the natural environment; therefore, topography is an important driver of plant species distributions, especially for alpine plants, and in mountainous regions, macrotopographies are usually large enough to provide refuge for plant species under changing climates (Myan, Walker, & Paramor, 2013). The Qinghai–Tibet Plateau uplifted more than 3,000 m in the Quaternary period, which dramatically changed the topography and climate in this region and formed various climate types (Zhang, Fengquan, & Jianmin, 2000). Meanwhile, microtopography will hinder the ability of a species to shift poleward and upslope because it can cause a relatively stable and closed climate environment within a short distance (Patsiou, Conti, Zimmermann, Theodoridis, & Randin, 2015). Hence, microtopography created a biological refuge for many rare, relict, and endemic plants during the last glacial maximum (Elsen & Tingley, 2015; Yang, Zhou, Li, Song, & Chen, 2011). Global warming will inevitably affect the living environment and hydrothermal conditions of plants in the Qinghai–Tibet Plateau region, and the complex topography will exacerbate this impact (Li et al., 2013).

Models are useful tools for simulating the impact of future climate change on plant species distribution, especially in this study, which considered a large spatiotemporal scale. In recent years, species distribution models (SDMs) have been popular tools for assessing the spatial–temporal variations in species distributions under different climate scenarios (Anderson, 2013; Mcquillan & Rice, 2015; Zhang et al., 2014). In the past two decades, advancements in statistical methods have promoted the development of SDMs, and numerous statistical methods and software programs have been developed to describe the niche characteristics of species and predict species distribution patterns. The popular algorithms are as follows: surface range envelope (SRE, i.e., BIOCLIM) (Booth, Nix, Busby, & Hutchinson, 2014), flexible discriminant analysis (FDA) (Basile et al., 2016), generalized linear model (GLM) (Lopatin, Dolos, Hernández, Galleguillos, & Fassnacht, 2016), generalized additive model (GAM) (Muñoz‐Mas, Papadaki, Martinez‐Capel, Zogaris, & Ntoanidis, 2016), multiple adaptive regression splines (MARS) (Friedman, 1991), generalized boosting model (GBM) (Moisen et al., 2006), classification tree analysis (CTA) (Thuiller & Lavorel, 2010), artificial neural network (ANN) (Segurado & Araujo, 2004), random forest (RF) (Mi, Huettmann, Guo, Han, & Wen, 2017), and maximum entropy (MaxEnt) (Phillips, Anderson, & Schapire, 2006). However, differential niche requirements of species shape the geographic distribution of species within an environment. Hence, the following factors should be considered when selecting an appropriate SDM algorithm for species distribution research on specific spatiotemporal scales, that is, species niche characteristics, especially those related to specific traits of species; environmental characteristics, especially the limiting factors in species' habitats; and data quality, including data availability and the spatial and temporal resolution of data (Bell & Schlaepfer, 2016; Guisan, Thuiller, & Zimmermann, 2017; Li & Wang, 2013). Simultaneously, for the same species with the same input data, different response curves and variable weights can be adopted according to the corresponding statistical properties of different algorithms, which will lead to different simulation results (Guo, Li, Zhao, & Wei, 2018) and will notably increase the uncertainties in the predicted species distribution. Therefore, the ensemble model (EM) strategy is proposed to solve this problem. This strategy applies several SDM methods within a consensus modelling framework and reduces the predictive uncertainty of individual models by combining the results from multiple models (Araújo & New, 2007; Guisan et al., 2017). Previous studies have indicated that EMs can substantially improve model accuracy and applicability (Grenouillet, Buisson, Casajus, & Lek, 2011).

Notopterygium incisum Ting ex H. T. Chang, also known as the “Emissary of Qiang Nationality” and “messenger of King Hu,” is a Chinese herbal medicine associated with many beautiful and moving folk stories, and it is also an endangered traditional Tibetan medicinal plant (Committee of Flora of China, 1986). According to field investigations and the literature, N. incisum is mainly distributed in Shaanxi Province, Sichuan Province, Qinghai Province, and the Tibet Autonomous Region (Committee of Flora of China, 1986). Modern science has confirmed that N. incisum can be used to relieve inflammation, cure arrhythmia and myocardial ischemia, promote cerebral circulation, remove thrombosis and bacteria, and carry out other pharmacological actions (Committee of National Pharmacopoeia, 2015; Li, Zhang, Wang, & Lei, 2003). Due to the increasing demands in the domestic and international medical markets and increasingly intense human activities, N. incisum is becoming increasingly threatened, primarily due to habitat disturbance and destruction (Liu, 2006; Sun et al., 2015; Zhou et al., 2003). In addition, this plant has been included on the Red List of endangered species in China since 2005. Thus, information on the potential geographic distribution and its response to climate change is vital to the protection and resource utilization of N. incisum.

Existing studies on N. incisum mainly focus on the identification of medicinal components, pharmacological analyses, cultivation, industrialization, and resource investigations (Gao & Fang, 2007; Li, Zhou, & Zhou, 2011; Li et al., 2003; Peng, Dong, Zhu, & Yan, 2006), while the emphasis of our research is on the distribution of N. incisum. This research analyzed the potential habitat distribution characteristics of N. incisum under future climate change scenarios, exploring the relationship between the spatial and temporal distribution of N. incisum and related geographic environmental factors. Additionally, this research will help with the introduction and cultivation of a good agricultural practice (GAP) and germplasm resource repositories under different environmental change conditions.

2. MATERIALS AND METHODS

2.1. Occurrence data

In this research, the occurrence data for this species were from a variety of sources, including published scientific literature, field survey reports (Jiang et al., 2006; Liu, 2006; Sun et al., 2015), and online plant databases, such as the Global Biodiversity Information Facility (GBIF, 2019) and Chinese Virtual Herbarium (CVH, 2019). To improve the geographic accuracy and perform scientific modelling, we selected only data with precise longitude and latitude information and removed duplicate coordinates and incomplete information. Finally, we obtained 99 occurrence data points to build the model (Figure 1, Table S1).

Figure 1.

Study area and geographic locations of Notopterygium incisum population distributions

2.2. Pseudo‐absence data

In practice, most SDM models require species absence data; however, true absence data are usually not available, so we use pseudo‐absence data as a substitute (Zhang et al., 2016). The numbers and qualities of pseudo‐absence data affect the accuracy of the SDMs (Zhang et al., 2016). In this research, using the “Sample by Buffered Local Adaptive Convex‐Hull” tool in the SDMtoolbox 2.0 (Brown, Bennett, & French, 2017), we generated pseudo‐absence data (Barbet‐Massin, Jiguet, Albert, & Thuiller, 2012) within 200 km buffers around the occurrence points. We selected three random subsets of the background to generate three groups of pseudo‐absence data, and each group included 500 points (Figure 2).

Figure 2.

Modelling process in a flow diagram

2.3. Environmental variables

In this study, we chose four categories of environmental datasets with a total of 24 environmental variables to characterize the environmental demands of N. incisum (Table 1). Among these environmental variables, all climate variables, including 19 bioclimatic variables under three time periods, were downloaded from the WorldClim dataset (WORLDCLIM, 2019), with a resolution of 30″ (approximately 1 km²) (Fick & Hijmans, 2017). The future time periods were set to the 2050s (average for 2041–2060) and 2070s (average for 2061–2080), and we used bioclimatic variables under four IPCC–CMIP5 representative concentration pathways (RCPs), namely, RCP2.6, RCP4.5, RCP6, and RCP8.5, which are labelled after the possible range of radiative forcing values in the year 2100 (2.6, 4.5, 6.0, and 8.5 W/m², respectively) (IPCC, 2013) to depict future temperature and rainfall. We used bioclimatic variables from three GCMs (BCC–CSM1–1, MIROC5, and CCSM4) for model building.

Table 1.

Environmental element index used for predicting the potential geographic distribution of Notopterygium incisum

Environmental index	Code	Name	Selection
Climate variables	Bio1	Annual mean air temperature	√
	Bio2	Mean diurnal temperature range
	Bio3	Isothermality
	Bio4	Temperature seasonality	√
	Bio5	Max temperature of warmest month
	Bio6	Min temperature of coldest month
	Bio7	Temperature annual range
	Bio8	Mean temperature of wettest quarter
	Bio9	Mean temperature of driest quarter
	Bio10	Mean temperature of warmest quarter	√
	Bio11	Mean temperature of coldest quarter	√
	Bio12	Annual precipitation	√
	Bio13	Precipitation of wettest month
	Bio14	Precipitation of driest month
	Bio15	Precipitation seasonality	√
	Bio16	Precipitation of wettest quarter
	Bio17	Precipitation of driest quarter
	Bio18	Precipitation of warmest quarter
	Bio19	Precipitation of coldest quarter	√
Topographic variables	ASL	Elevation above sea level
	SLOP	Slope	√
	ASPE	Aspect	√
Soil variable	ST	Soil type variables	√
Vegetation variable	VT	Vegetation type variables.	√

√ means the variables were selected to build the model, for a total of 11 variables.

The topographic variables, including elevation, slope, and aspect, have the same resolution as the bioclimatic variables. The elevation variable was also acquired from the WorldClim dataset, and the slope and aspect variables were generated by the ArcGIS spatial analysis function based on the elevation variable.

In this research, the 1:1 million soil database of China was used for the soil type variables, and the 1:1 million China vegetation data were used for the vegetation type variables. Both of these data types were acquired from the National Tibetan Plateau Data Centre (Li, Nan, et al., 2011; NTPDC, 2019; Ran, Li, Lu, & Li, 2012) and had the same resolution as the other environmental variables. Because changes in vegetation and soil types lag behind climate change (Wu et al., 2015), we used the same soil type and vegetation type data in the future climate change scenarios.

2.4. Methods

The “biomod2” package is an object‐oriented, expandable, and reproducible R platform for forecasting species distributions (R Project, 2018; Thuiller, Lafourcade, Engler, & Miguel, 2009). The “biomod2” package supports 10 model algorithms (i.e., ANN, CTA, FDA, GAM, GBM, GLM, MaxEnt, MARS, RF, and SRE), and in this study, we separately used all 10 model algorithms to build the corresponding SDM. The accuracy of each model algorithm was evaluated by the area under the receiver operating characteristics (ROC) curve (AUC) and true skill statistic (TSS) (Thuiller et al., 2009). Then, we selected the algorithm that met the precision requirements to construct an EM to simulate the migration trend of N. incisum. Finally, we used biotic variables (vegetation and soil) to further refine the EM results.

2.4.1. Input data processing

In this research, the processing of input data included the removal of collinearity between environmental variables and the generation of pseudosampling points. First, principal component analysis (PCA) (Supplementary materials 1) and Pearson correlations were used to select a subset of environmental variables (Guisan et al., 2017; Guo, Li, Zhao, & Nawaz, 2019). Finally, we selected seven bioclimatic variables and two topographic variables (i.e., annual mean air temperature, bio1; temperature seasonality, bio4; mean temperature of the warmest quarter, bio10; mean temperature of the coldest quarter, bio11; annual precipitation, bio12; precipitation seasonality, bio15; precipitation of the coldest quarter, bio19; slope; and aspect) (Table 1). Second, three sets of pseudosampling points were randomly generated, and there were 500 pseudosampling points in each group. We obtained three sets of model inputs using the three sets of pseudosampling points and the N. incisum occurrence data.

2.4.2. Single modelling technique

We separately input the three sets of data into the model. For each modelling process, the sampling data of the N. incisum points involved in the modelling were divided into two parts. Seventy percent of the sampling data were used as a training set, and the remaining data were used as testing data. In addition, we set an equal weight for the total presence of sampling points and pseudosampling points. We used TSS and AUC to evaluate the model, and Equation (1) for TSS is as follows:

$$\text{TSS}=\text{Sensitivity}+\text{Specificity}-1$$ (1)

$$\text{Sensitivity}=a/(a+c)$$ (2)

$$\text{Specificity}=d/(b+d)$$ (3)

where a refers to the number of true positives, b refers to the number of false positives, c refers to the number of false negatives, and d refers to the number of true negatives. TSS values > 0.6 are considered good (Allouche, Tsoar, & Kadmon, 2006; Jones, Acker, & Halpern, 2010). The AUC indicates the area under the ROC curve, and the ROC plots display the relationship between sensitivity (Equation (2)) and 1—specificity (Equation (3)) over a range of threshold values (0–100). For AUC, which does not require selection of a habitat suitability threshold, values > 0.9 are considered good, and values from 0.7 to 0.9 are considered moderate (Allouche et al., 2006; Jones et al., 2010).

In addition, for each modelling algorithm, we repeated this modelling process 10 times with a bootstrapping sampling strategy; thus, in total, we built 300 single models (three sets of sampling data × 10 single modelling techniques × 10 repeats).

2.4.3. Ensemble model

Here, we used an EM to reduce the uncertainty caused by different modelling algorithms and sample datasets (Ran et al., 2012; Zhao, Wei, Guo, & Gu, 2016). First, we excluded the SRE because the average TSS value of this method was <0.5. Second, and we used the TSS values to determine the weight of the other 270 single model results. Equation (4) is as follows:

$$w_j=\frac{r_j}{\sum _{j=1}^h{r}_j}$$ (4)

where w_j refers to the weight of the results of model j, r_j refers to the TSS of model j, and h (h = 270) refers to the number of model results.

Then, we constructed the EM using Equation (5):

$${\mathit{\text{BT}}}_{\mathit{i}}=\sum _{\mathit{j}=\mathit{1}}^{\mathit{n}}{\mathit{w}}_{\mathit{j}}\times {\mathit{x}}_{\mathit{ij}}$$ (5)

where BT_i refers to the potential habitat suitability index of the evaluation unit (grid) i, w_j refers to the weight of the results of model j, and x_ij refers to the value of evaluation unit i in the results of model j. The comprehensive evaluation index for the potentially suitable habitat distribution of N. incisum is BT_i (range [0,1]). When the value of BT_i is close to 1, the geographic space of the grid unit is considered suitable for the growth of N. incisum.

2.4.4. Comprehensive habitat suitability model

In its natural habitats, N. incisum is not the dominant species and is usually an associated species that grows in alpine shrublands, alpine meadows, and woodlands (Mcquillan & Rice, 2015). Hence, the vegetation types are the important limiting factors, reflecting the limitations of the species' migration ability, and here, according to the literature, we conducted binary conversion of the vegetation type data. A suitability value of 1 was defined as a suitable vegetation type for N. incisum, namely, alpine forest land, shrubland, and alpine meadows, while all other vegetation types received a value of 0. Because there are no clearly defined soil types that are suitable for the growth of N. incisum, we used the soil type variables and occurrence data of N. incisum to create a MaxEnt model to assess the soil suitability requirements. The model settings were as follows: 75% of the occurrence data were used as a training set, and the remaining data were used as testing data. Ten replications were performed, and the AUC was used to evaluate model performance.

Then, based on the EM and considering the effect of soil and vegetation conditions, we built a CHS model to further identify the distribution characteristics of N. incisum‐suitable habitats, and the index of CHS for N. incisum was defined using the following equation (Equation (6)):

$${\mathit{\text{CHS}}}_i={\text{BT}}_i\cap S_i\cap V_i$$ (6)

where CHS_i refers to the comprehensive habitat suitability index for N. incisum in evaluation unit i, BT_i refers to the value of the EM result in evaluation unit i, S_i refers to the result of soil suitability in evaluation unit i, and V_i refers to the habitat suitability value for vegetation. Here, we classified the whole result into three classes based on the BT_i, S_i, and V_i values: unsuitable habitats, BT_i or S_i values below 0.3 (i.e., BT_i < 0.3 or S_i < 0.3); marginally suitable habitats, with a V_i value of 1, BT_i and S_i values ≥ 0.3, but at last one of them below 0.5 (i.e., (0.3 ≤ BT_i < 0.5 and S_i ≥ 0.3) or (0.3 ≤ S_i < 0.5 and BT_i ≥ 0.3)); and suitable habitats, BT_i and S_i values ≥ 0.5 (i.e., BT_i ≥ 0.5 and S_i ≥ 0.5).

Finally, we used the CHS model to simulate the potential changes in the suitable habitat distribution for N. incisum in the future (Figure 2). Based on bioclimatic variable data from the three GCMs of two future periods (2050s and 2070s), we used the EM to explore the possible impacts of climate change on the habitat distribution of this species. The future EM results for N. incisum under each IPCC–CMIP5 RCP and for both periods were obtained by averaging the results. We used the average result of the four IPCC–CMIP5 RCP scenarios as the final EM result. Then, combined with the same result of soil suitability, we obtained the future potential suitable habitat distribution with the CHS model. At last, we mapped all habitat suitability values of N. incisum for three periods (current, 2050s, and 2070s) and calculated the areas in Figures 3, 4, 5.

Figure 3.

Potential habitat distribution of Notopterygium incisum predicted by the ensemble model at present

Figure 4.

Potential spatial distribution of Notopterygium incisum based on the ensemble model in the 2050s

Figure 5.

Potential spatial distribution of Notopterygium incisum based on the ensemble model in the 2070s

3. RESULTS

3.1. Model performance

The statistical accuracy results for the 10 models showed that RF was the best model, and the TSS and AUC values were 0.929 and 0.984, respectively. This model was followed by FDA and GBM, and the TSS values for these two models were above 0.90. The accuracy of the SRE was lowest, and the TSS and AUC values were 0.50 and 0.75, respectively (Figure 6). In addition, in the nine models involved in the EM, the average TSS value of each single model was >0.74, and the average AUC value of each single model was >0.91 (Figure 6). Therefore, the EM provided satisfactory results, and the TSS and AUC values were 0.80 and 0.96, respectively. The AUC value of the MaxEnt model for the soil environment requirements was 0.87, which means that the model results were scientific and reasonable.

Figure 6.

Boxplots of the predictive performance of the different techniques used for SDMs. (a) TSS and (b) AUC

3.2. Distribution of suitable habitats in the current climate environment

In this study, different statistical algorithms led to different simulation results, but the spatial distribution patterns of N. incisum were consistent. In addition, all model results showed that the suitable distribution area for N. incisum was concentrated in the transitional zone from the first step to the second step in the “ladder topography” of western China, including the edge of the Qinghai–Tibet Plateau and the western Sichuan Plateau.

Based on the prediction results of the EM, we mapped the distribution of suitable habitats for N. incisum in China (Figure 3). The results showed that suitable habitats for N. incisum were mainly distributed in the region along the Qilian Mountains, northwest of the Qinling‐Daba mountain area in Gansu Province, eastern margin of the Tibetan Plateau and a great portion of the western Sichuan Plateau. The marginally suitable habitats were distributed in some areas of Gansu Province, east of Qinghai Province, southeast of Tibet Autonomous Region, west and north of Sichuan Province, part of southwest Shaanxi Province, part of Chongqing municipality, Shennongjia Forestry District of Hubei Province, Shanxi Province, Xinjiang Uygur Autonomous Region, Guizhou, and Yunnan Province, which had a sporadic distribution. In addition, the habitats of N. incisum were fragmented with large local patches of suitable habitat that were not spatially contiguous. We also calculated the areas of suitable habitats and marginally suitable habitats for N. incisum, and the results showed that the suitable habitats had an area of approximately 83.76 × 10³ km², and the marginally suitable habitats had an area of approximately 102.72 × 10³ km² (Table 2). In summary, the proportions of N. incisum‐suitable habitats were small and narrow, and the distribution region was mainly around the eastern Qinghai–Tibet Plateau.

Table 2.

Areas and percentages of habitat suitability distributions for Notopterygium incisum in different provinces and autonomous regions under the current environment

Region	Percentage of area (%)			Area (103 km2)
	Suitable habitat	Marginally suitable habitat	Unsuitable habitat	Suitable habitat	Marginally suitable habitat	Unsuitable habitat
Gansu	4.20	4.31	91.49	19.06	19.55	415.09
Qinghai	1.93	1.82	96.25	13.86	13.07	691.34
Tibet	1.01	2.23	96.76	11.69	25.82	1,120.17
Sichuan	8.02	7.85	84.13	38.71	37.89	406.12
Shaanxi	0.12	0.90	98.98	0.25	1.89	207.54
Other area				0.19	4.5

3.3. Suitable habitat distributions under climate change

Currently, the suitable habitat for N. incisum is approximately 0.78% of the land area in China. According to the forecasted results of the EM, the area of suitable habitats of N. incisum showed a decreasing trend. The area percentages were 0.65% in the 2050s (average of four RCPs results) and 0.60% in the 2070s (average of four RCPs results). From the present to 2070, the areas of suitable habitat for N. incisum in western Sichuan Province and northeastern Tibet Autonomous Region will be significantly reduced. In Chongqing municipality and Hubei Province, the areas of suitable habitat increased, but the distributions became more fragmented. In addition, many of the suitable habitats turned into marginally suitable habitats (Figures 4 and 5). The area of suitable habitats decreased gradually with habitat fragmentation in all RCPs scenarios in the future. The marginally suitable habitats decreased in area. Marginally suitable habitats showed an increasing trend by the 2050s but showed a decreasing trend by the 2070s. In general, the suitable habitats for N. incisum are currently limited in area, and as the effects of climate change become more serious, a large part of the suitable habitat will turn into marginally suitable habitat or unsuitable habitat. Only a few unsuitable habitat areas advanced to marginally suitable habitats or suitable habitats, and the areas of marginally suitable habitats only occasionally became suitable habitats. In brief, N. incisum habitats are declining. Hence, saving the habitat resources for N. incisum and restoring its habitat are urgent tasks.

4. DISCUSSION

4.1. Model rationality

Currently, several studies have been devoted to identifying the current distribution range of N. incisum (Shang et al., 2015; Sun et al., 2015), but there are many shortcomings in these studies, and one of them is the use of a simple algorithm, which can delimit only the general distribution scope and cannot provide many landscape details (Sun et al., 2015). Other studies have focused on only the local distribution of this species (Shang et al., 2015). In contrast to previous studies, we used an EM based on nine different models with different mathematical algorithms to simulate the potential distribution of N. incisum throughout China. This model strategy avoids the selection of a single best model, thus eliminating (or at least limiting) model selection bias and, even more importantly, reducing the uncertainty of the modelling results caused by different modelling algorithms (Guisan et al., 2017; Guo et al., 2019); additionally, this strategy can provide significant landscape details and show the true distribution characteristics.

Environmental variables that can effectively and reliably describe the suitable habitat characteristics of the target species are the basic element in successful species distribution research. Bioclimatic variables are one of the most widely used environmental variables in SDM research. These variables describe climatic characteristics such as the average, extreme and seasonal, or annual changes in climate factors that have ecological significance (Fick & Hijmans, 2017; Title & Bemmels, 2018; Vega, Pertierra, & Olalla‐Tárraga, 2017). Here, based on PCA, the redundancy of bioclimatic variables was further reduced. Then, we selected a subset of bioclimatic variables for the model based on the characteristics of species habitats. These processes guarantee the accuracy of the model.

In nature, N. incisum is not a constructive or dominant species; thus, at the regional scale, the vegetation and soil conditions dictate the distribution of the species, even in a favorable climate. Thus, during the modelling process, the soil and vegetation types were used as overlying variables to further test the prediction results, and including these variables made the prediction results more realistic.

4.2. Habitat area estimates for Notopterygium incisum

According to previous studies, the optimal potential habitats for N. incisum in some parts of Sichuan Province, Tibet Autonomous Region, Qinghai Province, and Gansu Province have areas >1.42 × 10⁵ km² (Sun et al., 2009). The most suitable habitat is in Sichuan Province, and more than 60% of the most suitable area for N. incisum is located in western Sichuan, such as in Aba and Ganzi prefectures (Sun et al., 2009, 2015). The EM results showed that the suitable habitats for N. incisum were mainly distributed in Sichuan Province, Gansu Province, Qinghai Province, Tibet Autonomous Region, and Shaanxi Province (Figure 3). In addition, the current suitable habitat area for N. incisum in mainland China covers 83.76 × 10³ km², and the suitable habitats are mainly distributed in Sichuan Province, with an area of approximately 38.71 × 10³ km², which is approximately 8.02% of the total area of Sichuan Province (Table 2). Our model result is consistent with that of previous studies in terms of the spatial range (Sun et al., 2009, 2015) but provides more details about the distribution of N. incisum habitats. The model results indicated that by the 2070s, the areas of suitable habitats will have persistently decreased (Figures 3, 4, 5). Moreover, the suitable habitats for N. incisum are narrowly distributed, and in the centralized distribution area, most suitable habitats will remain roughly unchanged in the future. This result suggests that the suitable habitats and marginally suitable habitats should be selected as resource conservation areas for the sustainable utilization of wild N. incisum resources. At the same time, suitable habitats should be taken into consideration when selecting and constructing the GAP base of N. incisum.

Our model results show that under global warming scenarios, the suitable habitat for N. incisum will continue to decrease with no obvious northward movement due to the dramatic topographic changes in the Qinghai–Tibet Plateau. At present, the N. incisum habitats are small and show noncontinuous, patchy, and mosaic distribution forms. Our model results show that climate change will intensify the destruction and fragmentation of native N. incisum habitats, which will lead to the disappearance of suitable habitat in these areas, increasing the risk of the extinction of this species.

4.3. The dominant environmental index response to suitability

Previous studies have shown that cold tolerance, growth‐season temperatures, and available water supply are the main environmental indexes that influence the distribution of alpine vegetation (Woodwand, 1987). In this study, according to the model results, the major variables that affected the distribution of N. incisum habitats were annual mean air temperature, temperature seasonality, mean temperature of warmest quarter, mean temperature of coldest quarter, annual precipitation, and precipitation seasonality. To further clarify the suitable ranges of environmental factors and the critical values, we drew the response curves for each variable mentioned above (Figure 7) and defined the suitable ranges of the variables (logistic probability of presence > 0.3). The results showed that the suitable ranges were −2.5 to 16.9°C for annual mean air temperature, 6.0–8.6°C for temperature seasonality, 6.8 –16.3°C for mean temperature of warmest quarter, −12.8 to 7.7°C for mean temperature of coldest quarter, 419–1181 mm for annual precipitation, and 71.4–98.5 mm for precipitation seasonality. The habitat characteristics of N. incisum, such as cold humid climates, were summarized through these environmental indexes. The results were more detailed than those of previous studies (Shang et al., 2015; Sun et al., 2015).

Figure 7.

The dominant environmental index response curve. Annual mean temperature (bio1), temperature seasonality (bio4), mean temperature of warmest quarter (bio10), mean temperature of coldest quarter (bio11), annual precipitation (bio12), and precipitation seasonality (bio15)

Climate change will influence N. incisum physiology through several interrelated processes, which will lead to changes in N. incisum distributions. As a perennial herb, freezing winter temperatures (i.e., bio11) at middle to high latitudes will harm the underground rhizome of N. incisum, which will be a main limiting factor affecting the N. incisum distribution; however, this situation may change in some areas with a warming climate. In addition, climate change will contribute to the increase in accumulated temperatures and lengthen the duration of plant growth (Zhang, Li, Ding, & Zheng, 2017). As a medicinal plant, the root and rhizome have been used in traditional Chinese medicine; hence, with increasing accumulated temperatures, the production of medicinal material will increase. Furthermore, in high and cold regions, increasing temperatures will lengthen the duration of soil moisture necessary for plant growth and reduce frost damage. However, if temperatures exceed their physiological optimum range, the growth and reproduction of N. incisum will be affected, and suitable habitats will gradually disappear.

Similarly, changes in precipitation patterns can influence the N. incisum distribution. Global warming will lead to an increase in precipitation in western China, especially the Qinghai–Tibet Plateau; hence, the water supply available for plants will increase. Nevertheless, prior work has suggested a relatively low impact of precipitation on the distribution of N. incisum; rather, the impact of temperature change will be the strongest (Shang et al., 2015; Sun et al., 2015). Indeed, in this study, nearly all 10 single models showed that among the nine environmental variables, all four temperature variables had key impacts on the distribution of N. incisum, and for the EM, the contribution rates of the temperature variables were higher than those of the precipitation variables, which indicated that the N. incisum distributions were less sensitive to precipitation variation than temperature variation.

5. CONCLUSIONS

Numerous studies have indicated that species will shift their geographic distributions poleward and upslope due to the dramatic topographic changes in the Qinghai–Tibet Plateau; this shift will be complex and heterogeneous. Here, we conducted an analysis of the endangered medicinal plant N. incisum, which is mainly distributed in the eastern margin of the Qinghai–Tibet Plateau, and we built a CHS model to simulate the distribution of N. incisum‐suitable habitats in three time periods (current, 2050s, and 2070s). The results showed that under climate change, the suitable habitats for N. incisum would significantly decrease with no obvious northward movement, and the increase in temperature would intensify the destruction and fragmentation of native habitats.

This study was a successful attempt to model the distribution of a medicinal plant with CHS and provided new information for modelling medicinal plant distributions in an area with complicated topography and a variable climate. We also tried to provide valuable insights to highlight the priority areas for medicinal plant conservation and resource utilization.

CONFLICT OF INTEREST

The authors have no competing interests to declare.

AUTHOR CONTRIBUTIONS

ZFZ, YLG, HYW, and WG conceived and designed the study. ZFZ and YLG collected the samples and established the model. ZFZ, QR, JL, and QZZ analyzed the data. ZFZ, YLG, HYW, and WG wrote the paper. All authors read and approved the final product.

Supporting information

 

 

Zhao Z, Guo Y, Wei H, et al. Potential distribution of Notopterygium incisum Ting ex H. T. Chang and its predicted responses to climate change based on a comprehensive habitat suitability model. Ecol Evol. 2020;10:3004–3016. 10.1002/ece3.6117

DATA AVAILABILITY STATEMENT

All environmental variables used in the manuscript are already publicly accessible, and we have provided the download address in the manuscript; relevant sampling site information can be found in Table S1 in the online version.