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基于MaxEnt模型的长白山泥炭藓生境预测

Habitat prediction of Sphagnum spp. in the Changbai Mountains based on MaxEnt model

  • 摘要: 泥炭沼泽是全球最重要的碳汇之一,对全球生态系统碳储存、水文调节、生态栖息地构建和调节气候变化发挥着重要作用。泥炭藓(Sphagnum spp.)作为湿地生态系统中关键的工程物种、泥炭沼泽的建群种,具有极高的生态学功能和环境指示价值。为了掌握长白山泥炭藓的时空分布格局和气候变化下适宜分布区的变化趋势,本研究基于14个环境因子数据和1 434个泥炭藓分布样点,利用最大熵模型(Maximum Entropy Model)模拟了基准期(1981—2010年)以及未来两个时间段(2041—2070年和2071—2100年)3个气候变化情景(SSP1-2.6、SSP3-7.0和SSP5-8.5)下泥炭藓的适宜生境分布区,并量化了关键环境因子的贡献度以及响应曲线特征。结果表明,MaxEnt模型的预测精度较好,3个时间段3种情景下模型AUC(受试者工作特征曲线下的面积)值均高于0.85;泥炭藓在基准期气候条件下适生区面积为5.28万km2,占长白山地区总面积的20.87%,海拔分布范围为200~1 900 m;在未来SSP1-2.6低排放情景下适宜生境的面积相对平稳,在中排放SSP3-7.0情景下呈下降趋势,而在高排放SSP5-8.5情景下呈先减少后增加趋势。影响泥炭藓分布的主要环境因子是地形因子(海拔和地形湿度指数)和气候因子(最暖月日均最高温、降水量季节性变异系数和最暖季月均降水量),海拔高度、土壤潜在含水量与温度共同奠定了泥炭藓适宜生境的基本格局;未来泥炭藓潜在适宜生境呈现出向高海拔迁移的趋势。本研究为泥炭藓及泥炭沼泽保护提供了科学依据。

     

    Abstract: Peatlands are among the most important carbon sinks on Earth and play vital roles in carbon sequestration, hydrological regulation, habitat maintenance, and climate change mitigation. Sphagnum spp. are key ecosystem engineers in wetland ecosystems and dominant peat-forming species in peatlands, with high ecological significance and strong environmental indicator value. To clarify the spatiotemporal distribution patterns of Sphagnum spp. in the Changbai Mountains and to reveal the trends in suitable habitat under future climate change, this study used 1 434 occurrence records and 14 environmental variables to simulate the suitable habitat distribution of Sphagnum spp. using the Maximum Entropy Model (MaxEnt). The simulations were conducted for the baseline period (1981—2010) and for two future periods (2041—2070 and 2071—2100 under three Shared Socioeconomic Pathway scenarios, namely SSP1-2.6, SSP3-7.0, and SSP5-8.5. In addition, the relative contributions of key environmental factors and the characteristics of their response curves were quantitatively analyzed. The results showed that the MaxEnt model performed well, with the Area Under the Receiver Operating Characteristic Curve (AUC) exceeding 0.85 for all simulations across the three periods and three scenarios, indicating good predictive accuracy. Under baseline climatic conditions, the suitable habitat area of Sphagnum spp. in the Changbai Mountains was estimated at 52 800 km2, accounting for 20.87% of the total area of the study region, with an elevational range of 200-1 900 m. Under future climate scenarios, the suitable habitat area for Sphagnum spp. showed different patterns of change. Specifically, under SSP1-2.6, the area remained relatively stable; under SSP3-7.0, it showed a declining trend; and under SSP5-8.5, it first decreased and then increased. The main environmental factors affecting the distribution of Sphagnum spp. were topographic factors, particularly elevation and topographic wetness index, as well as climatic factors, including the mean daily maximum temperature of the warmest month, precipitation seasonality, and mean monthly precipitation of the warmest quarter. These results indicate that elevation, potential soil water availability, and temperature together determine the basic spatial pattern of suitable habitat for Sphagnum spp. Future projections further suggest that the potential suitable habitat of Sphagnum spp. will shift toward higher elevations under climate change. This study improves the understanding of the distribution characteristics of Sphagnum spp. in the Changbai Mountains and reveals the potential effects of future climate change on their suitable habitat. The findings provide a scientific basis for the conservation of Sphagnum spp. and peatland ecosystems.

     

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