| Literature DB >> 36177121 |
Xingtong Wu1, Minqiu Wang1, Xinyu Li1, Yadan Yan1, Minjun Dai1,2, Wanyu Xie1, Xiaofen Zhou1, Donglin Zhang2, Yafeng Wen1.
Abstract
Climate change affects the species spatio-temporal distribution deeply. However, how climate affects the spatio-temporal distribution pattern of related species on the large scale remains largely unclear. Here, we selected two closely related species in Taxus genus Taxus chinensis and Taxus mairei to explore their distribution pattern. Four environmental variables were employed to simulate the distribution patterns using the optimized Maxent model. The results showed that the highly suitable area of T. chinensis and T. mairei in current period was 1.616 × 105 km2 and 3.093 × 105 km2, respectively. The distribution area of T. chinensis was smaller than that of T. mairei in different periods. Comparison of different periods shown that the distribution area of the two species was almost in stasis from LIG to the future periods. Temperature and precipitation were the main climate factors that determined the potential distribution of the two species. The centroids of T. chinensis and T. mairei were in Sichuan and Hunan provinces in current period, respectively. In the future, the centroid migration direction of the two species would shift towards northeast. Our results revealed that the average elevation distribution of T. chinensis was higher than that of T. mairei. This study sheds new insights into the habitat preference and limiting environment factors of the two related species and provides a valuable reference for the conservation of these two threatened species.Entities:
Keywords: Climate change; Elevational differences; Geographic distribution; Species distribution modeling; Taxus chinensis; Taxus mairei
Year: 2022 PMID: 36177121 PMCID: PMC9475124 DOI: 10.1002/ece3.9302
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 3.167
FIGURE 1Organism photograph of the two species. (a) Taxus chinensis from Zhen'an, Shaanxi. Leaves linear, straight to distally falcate, usually (0.8‐) 1.5–2.2 cm × 2–3.2 mm. (b) Taxus mairei in Qiyang, Hunan. Leaves linear, usually falcate and 1.5–3.5 cm × 2–4 mm.
Contribution rate and importance of environmental variables for Taxus chinensis and Taxus mairei
| Type | Variables | Taxus chinensis | Variables | Taxus mairei | ||
|---|---|---|---|---|---|---|
| Percent of Contribution (%) | Permutation importance (%) | Percent of Contribution (%) | Permutation importance (%) | |||
| Climate | bio2 | 28.4 | 5.7 | bio4 | 2.0 | 13.4 |
| bio5 | 10.8 | 0.2 | bio5 | 0.5 | 4.3 | |
| bio7 | 9.7 | 2.4 | bio8 | 3.1 | 3.2 | |
| bio11 | 39.4 | 58.4 | bio11 | 24.1 | 16.5 | |
| bio13 | 0.2 | 1.8 | bio15 | 9.2 | 14.2 | |
| bio15 | 0.1 | 0.1 | bio18 | 34.7 | 16.9 | |
| Topographical | Elevation | 5.4 | 17.0 | Elevation | 14.2 | 8.0 |
| Aspect | 0.1 | 0.1 | Aspect | 0.6 | 1.7 | |
| Slope | 0.6 | 0 | Slope | 3.8 | 3.4 | |
| Soil | Nutrient availability | 2.3 | 12.0 | Nutrient availability | 0 | 0 |
| Rooting conditions | 0.4 | 0.5 | Rooting conditions | 0.3 | 15.6 | |
| Oxygen availability to roots | 0.8 | 0.8 | Oxygen availability to roots | 0 | 0 | |
| Topsoil Base Saturation | 0.5 | 0.3 | Topsoil Base Saturation | 6.4 | 0.9 | |
| Available water storage capacity | 0.1 | 0 | Available water storage capacity | 0.3 | 0.9 | |
| Human influence | Human influence index | 1.3 | 0.8 | Human influence index | 0.8 | 0.8 |
Note: bio2: Mean Diurnal Range; bio4: Temperature Seasonality; bio5: Max Temperature of Warmest Month; bio7: Temperature Annual Range; bio8: Mean Temperature of Wettest Quarter; bio11: Mean Temperature of Coldest Quarter; bio13: Precipitation of Wettest Month; bio15: Precipitation Seasonality; bio18: Precipitation of Warmest Quarter.
FIGURE 2Changing tendency of elevation and bio11 under different climate periods
FIGURE 3Potential distribution of the Taxus chinensis and Taxus mairei under different climate periods
Changes in the distribution area of Taxus chinensis and Taxus mairei in different periods and different scenarios
| Species | Periods | Suitable area (×105 km2) (%) | Highly suitable area (×105 km2) (%) | Contraction (×105 km2) | Stable (×105 km2) | Expansion (×105 km2) | Percentage loss(%) | Percentage gain (%) |
|---|---|---|---|---|---|---|---|---|
|
| RCP4.5_2070 | 6.952 (−0.90) | 1.703 (2.16) | 0.244 | 1.517 | 0.280 | 14.32 | 16.44 |
| RCP4.5_2050 | 7.015 (−1.52) | 1.668 (3.22) | 0.165 | 1.539 | 0.221 | 9.89 | 13.24 | |
| Current | 7.123 (−7.21) | 1.616 (−5.99) | 0.299 | 1.507 | 0.197 | 18.50 | 12.19 | |
| Holocene | 7.677 (13.00) | 1.719 (8.80) | 0.128 | 1.544 | 0.261 | 7.45 | 15.18 | |
| LGM | 6.792 (−7.89) | 1.580 (−10.89) | 0.341 | 1.547 | 0.125 | 20.94 | 7.91 | |
| LIG | 7.374 | 1.773 | ||||||
|
| RCP4.5_2070 | 14.392 (−0.06) | 2.969 (0.75) | 0.352 | 2.831 | 0.373 | 11.86 | 12.56 |
| RCP4.5_2050 | 14.401 (−3.17) | 2.947 (−4.72) | 0.472 | 2.864 | 0.320 | 16.02 | 10.86 | |
| Current | 14.873 (3.83) | 3.093 (−0.55) | 0.490 | 2.878 | 0.459 | 15.84 | 14.84 | |
| Holocene | 14.325 (2.50) | 3.110 (7.13) | 0.36 | 2.777 | 0.590 | 11.58 | 18.97 | |
| LGM | 13.976 (0.89) | 2.903 (4.69) | 0.199 | 2.795 | 0.342 | 6.86 | 11.78 | |
| LIG | 13.854 | 2.773 |
Note: Future: RCP4.5_2070 and RCP4.5_2050 under CCSM; Holocene: Holocene; LGM: Last Glacial Maximum; LIG: Last Inter Glacial. Changing of the distribution area were based on the previous periods. Suitable area, 0.1 ≤ p < 1; Highly suitable area, 0.5 ≤ p < 1.0.
FIGURE 4Changes in distribution area of the Taxus chinensis and Taxus mairei between two adjacent periods
FIGURE 5Centroid migration routes under different climate periods for Taxus chinensis and Taxus mairei
Coordinates and the distance of the centroids
| Periods | Taxus chinensis | Taxus mairei | ||||
|---|---|---|---|---|---|---|
| Longitude (E) | Latitude (N) | Migration distance (km) | Longitude (E) | Latitude (N) | Migration distance (km) | |
| RCP4.5_2070 | 105.978 | 30.433 | 18.26 | 112.955 | 27.792 | 10.67 |
| RCP4.5_2050 | 105.986 | 30.268 | 8.86 | 112.89 | 27.715 | 29.44 |
| Current | 105.894 | 30.271 | 33.35 | 112.586 | 27.697 | 8.33 |
| Holocene | 105.899 | 30.573 | 26.72 | 112.532 | 27.639 | 80.27 |
| LGM | 105.914 | 30.331 | 33.52 | 113.304 | 27.905 | 13.00 |
| LIG | 105.576 | 30.401 | 113.312 | 27.790 | ||
Note: Future: RCP4.5_2070 and RCP4.5_2050 under CCSM; LGM: Last Glacial Maximum; LIG: Last Inter Glacial. Migration of the distance were based on the previous periods.