机构地区:[1]内蒙古大学生态与环境学院,内蒙古呼和浩特010021 [2]内蒙古大学环境地质研究所,内蒙古呼和浩特010021 [3]北京师范大学环境演变与自然灾害教育部重点实验室地表过程与资源生态国家重点实验室,北京100875
出 处:《干旱区地理》2019年第5期1011-1022,共12页Arid Land Geography
基 金:国家自然科学基金(41562009,41962011,41330748);内蒙古自治区草原英才项目(CYYC7004)
摘 要:过去植被覆盖度重建在长尺度气候模拟和陆地生态环境演变机制研究等方面具有重要意义。基于现代过程的孢粉—植被覆盖度转换函数研究,可为利用孢粉地层数据重建过去植被覆盖度变化提供一条新的途径。以内蒙古高原等地39个湖泊和7个水库中心的表层沉积物孢粉组合与归一化植被指数(NDVI)为研究对象,利用加权平均偏最小二乘法(WA-PLS)、局部加权加权平均法(LWWA)和最佳类比法(MAT)分别建立了孢粉—NDVI转换函数;通过留一交叉检验法、自助法和空间自相关性等检验,筛选出最优模型并应用于古地层孢粉数据,实现定量重建过去植被覆盖度变化。结果表明:MAT和WA-PLS模型均受到空间自相关性的显著影响,而LWWA模型则是建立孢粉—NDVI转换函数的最优模型。与已有类似转换函数表现能力的对比表明,本研究建立的转换函数具有较强的可靠性和应用潜力。基于本研究转换函数重建的内蒙古辉腾锡勒(HTL)区域全新世植被覆盖变化与孢粉重建的植被变化具有很好的一致性,进一步印证了本研究转换函数的较强潜力,均表现出对降水变化的响应更为显著。Vegetation cover was an important factor in palaeo-climate simulation.The study of pollen-vegetation cover transfer function based on modern processes provides a way to reconstruct the past vegetation cover change by using pollen stratum data.The Inner Mongolia Plateau and its adjacent area,which is located at the marginal monsoon area of northern China and has a large climatic and vegetal gradient,provides us an ideal area to study the pollen-vegetation cover transfer functions.In this paper,we investigated pollen assemblages of lake central surface sediment from 46 lakes and reservoirs,and developed transfer functions between lake surface sediment pollen assemblage and Normalized Difference Vegetation Index(NDVI) using three different methods which include weighted average partial least squares(WA-PLS),local weighted average method(LWWA) and modern analogue technique(MAT).We used leave-one-out cross-validation,bootstrapping and autocorrelation test to evaluate the performance of those three pollen-NDVI transfer functions and select the most reliable to reconstruct the Holocene vegetation cover history of Huitengxile Plateau of central Inner Mongolia.As results,the redundancy analysis(RDA) was conducted on the pollen data and environmental data according to the linear data type of the pollen data,as indicated by the gradient length(i.e.,2.047) of the detrended correspondence analysis(DCA).The RDA plot displays that the NDVI points to the positive of the first axis where forest and forest steppe sites clustered,and has smaller angles with the Pinus and Betula and larger angles with the desert pollen type such as Nitraria,Ephedra and Tamaricaeae,which suggested that the NDVI index was closely related to the spatial distribution of pollen and thus the pollen-NDVI transfer functions could be reliably developed.The leave-one-out cross-validation and the bootstrapping test showed that the LWWA_Inv(R^2jack=0.57,R^2boot=0.57) and WA-PLS-3(R^2jack=0.56,R^2boot=0.54) models have better performance than the MAT(R^2jack=0.5
关 键 词:内蒙古高原 湖泊表层沉积物 孢粉组合 植被覆盖 归一化植被指数 转换函数
分 类 号:P532[天文地球—古生物学与地层学]
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