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生态学杂志 ›› 2026, Vol. 45 ›› Issue (6): 1920-1932.doi: 10.13292/j.1000-4890.202606.015

• 研究报告 • 上一篇    下一篇

未来气候变化情景下攀枝花苏铁潜在适生区预测及保护建议

冯源1,2,3,代光辉1,2*,覃阳平4   

  1. 1云南省林业和草原科学院, 昆明 650201; 2云南省高黎贡山生物多样性重点实验室, 昆明 650201; 3高黎贡山森林生态系统云南省野外科学观测研究站, 昆明 650201; 4国家林业和草原局西南调查规划院, 昆明 650031)

  • 出版日期:2026-06-10 发布日期:2026-12-01

Predicting potential suitable habitats and conservation strategies for Cycas panzhihuaensis under future climate change scenarios.

FENG Yuan1,2.3, DAI Guanghui1,2*, QIN Yangping4   

  1. (1Yunnan Academy of Forestry and Grassland, Kunming 650201, China; 2Yunnan Key Laboratory of Biodiversity of Gaoligong Mountain, Kunming 650201, China; 3Gaoligong Mountain Forest Ecosystem Observation and Research Station of Yunnan Province, Kunming 650201, China; 4Southwest Survey and Planning Institute, National Forestry and Grassland Administration, Kunming 650031, China).

  • Online:2026-06-10 Published:2026-12-01

摘要: 气候会对物种地理分布产生显著影响,探究气候变化背景下攀枝花苏铁(Cycas panzhihuaensis)潜在适生区的时空格局变化,将有助于开展种群保护工作。本研究基于攀枝花苏铁的现有分布点,运用最大熵(MaxEnt)模型,探究环境变量对其地理分布的影响,并预测当代以及未来不同时段(2050s、2070s、2090s)、不同气候变化情景(SSP245、SSP585)下攀枝花苏铁潜在适生区时空变化特征及质心移动趋势。结果表明:(1)MaxEnt模型对于攀枝花苏铁的预测表现较好(AUC值0.980),表明其可用于进一步预测;(2)影响攀枝花苏铁分布的主导环境因子有温度季节性变化标准差、最干季降水量、最热月最高温度和土壤有机碳储量;(3)当代攀枝花苏铁潜在分布的总适生区面积为316.58×104 hm2,其中高适生区面积为33.87×104 hm2,主要沿金沙江大弯曲及其支流的干热河谷地带呈现较为连续的枝状分布特征;(4)未来气候变化情景下攀枝花苏铁总适生区面积将扩大,SSP245、SSP585情景下最大值分别达481.98×104和589.16×104 hm2,较当代扩张52.25%和86.10%,分布质心分别向北迁移124.53和111.80 km;高适生区面积持续萎缩,SSP245、SSP585情景的最低值较当代分别减少45.87%和88.34%。研究结果显示,尽管总适生区面积有所扩大,但高适生区面积持续缩减,表明气候变化将对攀枝花苏铁的生存构成严重威胁。研究结果可为攀枝花苏铁的就地保护提供科学依据,同时也可为其迁地保护位点、引种种植地点的选择提供参考。


关键词: 气候变化, 攀枝花苏铁, 物种分布模型, 地理分布, 空间格局

Abstract: Climate exerts a significant impact on the geographical distribution of species. Investigating the potential distribution of Cycas panzhihuaensis under the context of climate change is beneficial for conservation. Based on the current distribution points of C. panzhihuaensis, we used the Maximum Entropy (MaxEnt) model to examine the influence of environmental variables on its geographical distribution. The spatiotemporal changes and centroid shift trends in the potential distributions of C. panzhihuaensis were predicted under various climate scenarios (SSP245, SSP585) for both the current and future periods (2050s, 2070s, 2090s). The results showed that: (1) The MaxEnt model performed well in predicting the distributions of C. panzhihuaensis (with an AUC of 0.980), indicating its suitability for further predictive applications. (2) The temperature seasonality, precipitation in the driest quarter, maximum temperature of the warmest month, and organic carbon stock were the main factors influencing the distribution of C. panzhihuaensis. (3) The total suitable habitat for the current distribution of C. panzhihuaensis was 316.58×104 hm2, with a highly suitable habitat of 33.87×104 hm2. Its distribution appeared relatively continuous, forming a branch-like pattern along the dry, hot river valley regions of the Jinsha River’s great bend and its tributaries. (4) Under future climate change scenarios, the suitable habitat for C. panzhihuaensis will expand. Under the SSP245 and SSP585 scenarios, the maximum total suitable habitat will reach 481.98×104 and 589.16×104 hm2, respectively, representing increases of 52.25% and 86.10%. The centroid of the suitable habitat will shift northward by 124.53 and 111.80 km, respectively. The minimum values of highly suitable habitat reduced by 45.87% and 88.34%, respectively. The results indicate that while the overall suitable habitat increases, a significant decrease in the highly suitable habitat can pose serious challenges to the viability of C. panzhihuaensis. Our results can provide a scientific basis for the in situ conservation of C. panzhihuaensis, and provide a reference for the selection of sites for ex situ conservation, introduction, and cultivation.


Key words: climate change, Cycas panzhihuaensis, species distribution modelling, geographical distribution, spatial pattern