Modern pollen precipitation studies were carried out on a regional scale in the territory of the classical city of Sagalassos (Southwest Turkey). 57 moss cushions and 7 soil samples from different vegetation types were analysed palynologically. The resulting pollen spectra were grouped into 14 vegetation groups, which were examined using discriminant analysis and principal components analysis. These numerical procedures are applied to display the structure in the data set in a comprehensive way. Some of the modern spectra groups seem to be well-defined, whereas others are difficult to distinguish from each other. After the relationships between the modern pollen spectra had been analysed, the fossil data from a core from the marsh of Gravgaz were added to the data set so that any similarities between fossil and modern spectra could be seen. A joint principal components analysis of the modern and fossil pollen spectra revealed that the pollen spectra from the earliest (ca. 2600-2500 BP; Cal. 830-590 BC till 790-520 BC) and the latest (starting at ca. 1300 BP; Cal. 660-780 AD) pollen assemblage zones have modern counterparts. On the other hand, the pollen spectra from the pollen assemblage zone dominated by Artemisia (ca. 2500-2300 BP; Cal. 790-520 BC till 410-210 BC) and from the pollen assemblage zone that indicated the practice of arboriculture (ca. 2300-1300 BP; Cal. 410-210 BC till 660-780 AD) have no close modern analogues, although individual tabulated pollen percentages revealed some similarities with some modern spectra groups.

中文翻译：

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Sagalassos（土耳其西南部）领土的现代花粉研究及其在解释全新世晚期花粉图时的应用

现代花粉降水研究是在古典城市萨加拉索斯（土耳其西南部）的区域范围内进行的。对来自不同植被类型的 57 个苔藓垫和 7 个土壤样品进行孢粉学分析。所得花粉光谱分为 14 个植被组，使用判别分析和主成分分析对其进行检查。这些数值程序用于以全面的方式显示数据集中的结构。一些现代光谱组似乎是明确定义的，而其他的则很难相互区分。在分析了现代花粉光谱之间的关系后，将来自 Gravgaz 沼泽岩心的化石数据添加到数据集中，以便可以看到化石和现代花粉光谱之间的任何相似之处。现代和化石花粉光谱的联合主成分分析表明，花粉光谱从最早（约 2600-2500 BP；Cal. 830-590 BC 到 790-520 BC）和最晚（从约 1300 BP 开始） ; Cal. 660-780 AD) 花粉组合区有现代对应物。另一方面，来自以蒿属为主的花粉组合区（约公元前 2500-2300 年；公元前 790-520 年至公元前 410-210 年）和来自表明树木栽培实践的花粉组合区的花粉光谱（约. . 2300-1300 BP; Cal. 410-210 BC 到 660-780 AD) 没有近代的类似物，尽管单独的表格花粉百分比显示与一些现代光谱组有一些相似之处。830-590 BC 到 790-520 BC）和最新的（从大约 1300 BP 开始；Cal. 660-780 AD）花粉组合区有现代对应物。另一方面，来自以蒿属为主的花粉组合区（约公元前 2500-2300 年；公元前 790-520 年至公元前 410-210 年）和来自表明树木栽培实践的花粉组合区的花粉光谱（约. . 2300-1300 BP; Cal. 410-210 BC 到 660-780 AD) 没有近代的类似物，尽管单独的表格花粉百分比显示与一些现代光谱组有一些相似之处。830-590 BC 到 790-520 BC）和最新的（从大约 1300 BP 开始；Cal. 660-780 AD）花粉组合区有现代对应物。另一方面，来自以蒿属为主的花粉组合区（约公元前 2500-2300 年；公元前 790-520 年至公元前 410-210 年）和来自表明树木栽培实践的花粉组合区的花粉光谱（约. . 2300-1300 BP; Cal. 410-210 BC 到 660-780 AD) 没有近代的类似物，尽管单独的表格花粉百分比显示与一些现代光谱组有一些相似之处。