| Literature DB >> 30151161 |
Yanbin Jiang1, Tiejun Wang2, Yupeng Wu1, Ronggui Hu1, Ke Huang3, Xiaoming Shao4.
Abstract
Epiphyllous liverworts form a special group of bryophytes that primarily grow on the leaves of understory vascular plants in tropical and subtropical evergreen broadleaf forests. Being sensitive to moisture and temperature changes, epiphyllous liverworts are often considered to be good indicators of climate change and forest degradation. However, they are a poorly collected and taxonomically complicated group, with an only partly identified distribution pattern. In this study, we built four models based on 24 environmental variables at four different spatial resolutions (i.e., 1 km, 5 km, 10 km, and 15 km) to predict the past distribution of epiphyllous liverworts in China, using Maxent model and 63 historical location records (i.e., presence-only data). Both area under the curve of the receiver operating characteristic (AUC) and true skill statistic (TSS) methods are used to assess the model performance. Results showed that the model with the predictors at a 15-km resolution achieved the highest predictive accuracy (AUC=0.946; TSS=0.880), although there was no statistically significant difference between the four models (p > 0.05). The most significant environmental variables included aridity, annual precipitation, precipitation of wettest month, precipitation of wettest quarter, and precipitation of warmest quarter, annual mean NDVI, and minimum NDVI. The predicted suitable areas for epiphyllous liverworts were mainly located in the south of Yangtze River and seldom exceed 35°N, which were consistent with the museum and herbarium records, as well as the historical records in scientific literatures. Our study further demonstrated the value of historical data to ecological and evolutionary studies.Entities:
Keywords: bryophytes; environmental variables; historical records; maxent; species distribution model
Year: 2018 PMID: 30151161 PMCID: PMC6106194 DOI: 10.1002/ece3.4274
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Figure 1Epiphyllous liverworts growing on leaves of various vascular plants. Photographs by Yanbin Jiang
Figure 2Study area and locations of the 63 occurrence records of epiphyllous liverworts in China used in the species distribution models
Environmental variables used for modeling the distribution of epiphyllous liverworts
| Data source | Category | Variables | Abbreviation | Units |
|---|---|---|---|---|
| WorldClim | Bioclimatic | Annual Mean Temperature | Bio1 | oC × 10 |
| Mean Diurnal Range (Mean of monthly (max temp ‐ min temp)) | Bio2 | oC × 10 | ||
| Isothermality (BIO2/BIO7) (* 100) | Bio3 | % | ||
| Temperature Seasonality (standard deviation *100) | Bio4 | oC × 10 | ||
| Max Temperature of Warmest Month | Bio5 | oC × 10 | ||
| Min Temperature of Coldest Month | Bio6 | oC × 10 | ||
| Temperature Annual Range (BIO5‐BIO6) | Bio7 | oC × 10 | ||
| Mean Temperature of Wettest Quarter | Bio8 | oC × 10 | ||
| Mean Temperature of Driest Quarter | Bio9 | oC × 10 | ||
| Mean Temperature of Warmest Quarter | Bio10 | oC × 10 | ||
| Mean Temperature of Coldest Quarter | Bio11 | oC × 10 | ||
| Annual Precipitation | Bio12 | mm | ||
| Precipitation of Wettest Month | Bio13 | mm | ||
| Precipitation of Driest Month | Bio14 | mm | ||
| Precipitation Seasonality (Coefficient of Variation) | Bio15 | % | ||
| Precipitation of Wettest Quarter | Bio16 | mm | ||
| Precipitation of Driest Quarter | Bio17 | mm | ||
| Precipitation of Warmest Quarter | Bio18 | mm | ||
| Precipitation of Coldest Quarter | Bio19 | mm | ||
| CGIAR‐CSI | Bioclimatic | Potential Evapotranspiration | PET | mm |
| Aridity index | AI | / | ||
| USGS GTOPO30 | Topographic | Altitude | Altitude | m |
| Aspect | Aspect | degree | ||
| Slope | Slope | degree | ||
| GIMMS | Vegetation | Annual minimum NDVI | NDVI_min | / |
| Annual mean NDVI | NDVI_mean | / | ||
| Annual maximum NDVI | NDVI_max | / | ||
| Standard deviation NDVI | NDVI_std | / |
Performance of models in predicting the distribution of epiphyllous liverworts at 1‐km, 5‐km, 10‐km, and 15‐km resolutions, showing threshold‐independent and threshold‐dependent model evaluation results by AUC and maximum TSS (TSSmax) in R (10,000 background points used as pseudo‐absence for AUC and TSSmax)
| Model | AUC | TSSmax | AICc |
|---|---|---|---|
| 1 km | 0.926 ± 0.062 | 0.760 ± 0.155 | 1840.243 ± 12.401 |
| 5 km | 0.936 ± 0.029 | 0.834 ± 0.075 | 1472.627 ± 4.320 |
| 10 km | 0.932 ± 0.039 | 0.740 ± 0201 | 1291.717 ± 4.682 |
| 15 km | 0.946 ± 0.027 | 0.880 ± 0.011 | 1173.088 ± 5.283 |
|
| 0.750 | 0.082 | 0.000 |
One‐way ANOVA was performed to assess the effect of spatial resolution on model performance.
Figure 3Maps showing the spatial distribution pattern of epiphyllous liverworts in China from four different model scenarios of 1 km, 5 km, 10 km, and 15 km resolutions
Threshold for determining epiphyllous liverwort presence and corresponding fractional predicted area identified as presence for each model
| Model | Logistic threshold | Fractional predicted area |
|
|---|---|---|---|
| 1 km | 0.210 | 0.081 | <0.001 |
| 5 km | 0.242 | 0.073 | <0.001 |
| 10 km | 0.206 | 0.080 | <0.001 |
| 15 km | 0.276 | 0.060 | <0.001 |
Thresholds were determined by rejecting the lowest 10% of possible predicted values.
Figure 4Importance of environmental variables to model the distribution of epiphyllous liverworts from different resolutions: (a) 1 km, (b) 5 km, (c) 10 km, and (d) 15 km. The graphs depict the training gains when a variable is used in isolation, when the variable is excluded, and when all variables are utilized. The gain is a measure of how better the Maxent probability distribution fits the distribution of occurrence data. A variable has useful information when the gain is high as it is used in isolation and has unique information when it reduces the gain most when it is excluded
Figure 5Response curves illustrating the relationship between presence probability of epiphyllous liverworts and environmental variables. These curves show how the response changes for a particular variable used in isolation. The response curves were derived from the 15‐km model in Maxent
| Province | Site name | Elevation (m) | Survey time | Sources |
|---|---|---|---|---|
| Anhui | Zhawan, Qimen | 200 | 1982 | Wu and Guo ( |
| Fujian | Wuyishan, Guadun | 450–1300 | 1955, 1979–82 | Chen and Wu ( |
| Jiufengshan | 400–900 | 1999 | Zhu, Wang, Zhu, and Sun ( | |
| Wanmulin | 350–450 | 1986 | Li ( | |
| Nanjing, Shuhaijinshan | 400 | 1963 | Zhu and So ( | |
| Longxishan, Jiangle | 1450 | 1991 | Herbarium, Institute of Botany, Chinese Academy of Sciences | |
| Guangdong | Dinghushan | 800 | 1989 | Zhu and Wang ( |
| Heishiding Nature Reserve | 350–600 | 1992 | Li ( | |
| Babaoshan | 550–1700 | 1989 | Zhu, Hu, and Guo ( | |
| Xinyi | 1932 | Chen and Wu, ( | ||
| Nankunshan, Zengcheng | 1932, 53 | Chen and Wu ( | ||
| Jiulongshan, Lianping | 650 | 1987 | Gao and Bi ( | |
| Guangxi | Huaping | 960 | 1981 | Hu, Jin, and Jin ( |
| Maoershan Nature Reserve | 550 | 1974 | Zhu and So ( | |
| Shiwandashan | 1989 | Herbarium, Institute of Botany, Chinese Academy of Sciences | ||
| Jiuwandashan | 1100 | 1993 | Wang and Jia ( | |
| Guizhou | Maolan | 420–800 | 1984 | Wu ( |
| Fanjingshan | 1500–2000 | 1983 | Zhu and So ( | |
| Kuankuoshui | 1600 | 1983 | Zhu and So ( | |
| Xiaoqikong | 600 | 1998 | Zhu and So ( | |
| Hainan | Bawangling Nature Reserve | 600–1100 | 1989 | Zhu and So ( |
| Jianfengling Nature Reserve | 320–1200 | 1941, 62, 84 | Wu and Lin, ( | |
| Diaoluoshan | 400–1050 | 1974, 77, 84 | Zhu and So ( | |
| Wuzhishan | 650–1200 | 1977 | Zhu and So ( | |
| Hongkong | Taimoshan | 600–900 | 1995–97 | Zhu and So ( |
| Taipokau | 1996–98 | Zhu and So ( | ||
| Wukaotang | 50 | 1995–96 | Zhu and So ( | |
| Hunan | Jinbianxi, Zhangjiajie | 460 | 1992 | Zhu and So ( |
| Mangshan, Yizhang | 1974 | Zhu and So ( | ||
| Jiangxi | Jinggangshan | 650–950 | 1984 | Li and Wu ( |
| Wuyishan Nature Reserve | 960 | 1993–94 | Ji and Liu ( | |
| Guanshan Nature Reserve | 300–900 | 1995, 96 | Ji, Zheng, Xie, Wu and Qiang ( | |
| Sanqingshan | 660 | 1987 | Ji, Liu, Zhang, Chen, and Luo ( | |
| JiulingMufushan, Xiushui | 350–400 | 1994, 95 | Ji and Liu ( | |
| JiulingMufushan, Wuning | 300 | 1994, 95 | Ji and Liu ( | |
| Jiulianshan | 450–700 | 1992, 95 | Ji, Xie, Liu, Zhang, and Chen ( | |
| Sichuan | Ermeishan | 900–1500 | 1979, 80 | Zhu and So ( |
| Erlangshan | 160–1800 | 1974 | Zhu and So ( | |
| Jinfoshan | 2100 | 1984 | Zhu and So ( | |
| Moxi | 1980 | Zhu and So ( | ||
| Tiangtang | 900–1200 | 1984 | Zhu and So ( | |
| Taiwan | Zhibenzhushan | 1932 | Chen and Wu ( | |
| Taipinghsan | 1932 | Chen and Wu ( | ||
| Alishan | 1932 | Zhu and So ( | ||
| Yuanyanghu, Xinzhu | 1670 | 1998 | Zhu and So ( | |
| Xizang | Medog | 780–2450 | 1960, 82, 83 | Chen and Wu ( |
| Yunnan | Daweishan Nature Reserve | 1300–1960 | 1974, 88 | Zhu and So ( |
| Tongbiguan, Longchuan | 1100 | 1974 | Zhu and So ( | |
| Huanglianshan | 1973 | Zhu and So ( | ||
| Gongshan, Dulongjiang | 1240–2800 | 1982 | Zhu and So ( | |
| Mengyang | 850–1200 | 1936 | Chen and Wu ( | |
| Menglun Botanical garden | 850–1100 | 1957, 74, 82 | Zhu and So ( | |
| Yiwu | 750–1900 | 1936 | Chen and Wu ( | |
| Mengla | 1000 | 1936, 64, 95 | Chen and Wu ( | |
| Menghai | 1300 | 1936 | Chen and Wu ( | |
| Mengzhe | 1900 | 1936 | Chen and Wu ( | |
| Zhejiang | Wuyanling | 600–1140 | 1987 | Zhu and Hu ( |
| Baishanzu Nature Reserve | 600–1200 | 1990 | Zhu, Zhang, and Mao ( | |
| Jiulongshan | 400–1600 | 1981 | Liu ( | |
| Fengyangshan | 350–1580 | 1992–1993 | Zhu, Ye, and Cai ( | |
| Gutianshan | 360 | 1993 | Zhu and So ( |
| Method | 1 km | 5 km | 10 km | 15 km |
|---|---|---|---|---|
| LPT | 0.062 | 0.097 | 0.092 | 0.122 |
| T10 | 0.210 | 0.242 | 0.206 | 0.276 |
| Max Se+Sp | 0.173 | 0.225 | 0.125 | 0.195 |