The Garigliano alluvial-coastal plain, at the Latium-Campania border (Italy), witnessed a long-lasting history of human-environment interactions, as demonstrated by the rich archaeological knowledge. With the aim of reconstructing the evolution of the landscape and its interaction with human activity during the last millennia, new pollen results from the coastal sector of the Garigliano Plain were compared with the available pollen data from other nearby sites. The use of pollen data from both the coastal and marine environment allowed integrating the local vegetation dynamics within a wider regional context spanning the last 8000 years. The new pollen data presented in this study derive from the analysis of a core, drilled in the coastal sector, which intercepted the lagoon-marshy environments that occurred in the plain as a response to the Holocene transgression and subsequent coastal progradation. Three radiocarbon ages indicate that the chronology of the analyzed core interval ranges from c. 7200 to c. 2000 cal yr BP. The whole data indicate that a dense forest cover characterized the landscape all along the Prehistoric period, when a few signs of human activity are recorded in the spectra, such as cereal crops, pasture activity and fires. The main environmental changes, forced by natural processes (coastal progradation) but probably enhanced by reclamation works, started from the Graeco-Roman period and led to the reduction of swampy areas that favoured the colonisation of the outer plain.

丰富的考古学知识证明，在拉图-坎帕尼亚边境（意大利）的加里格里亚诺冲积海岸沿岸见证了人类与环境互动的悠久历史。为了重建过去一千年的景观演变及其与人类活动的相互作用，我们将加里利亚诺平原沿海地区的新花粉结果与附近其他站点的现有花粉数据进行了比较。利用来自沿海和海洋环境的花粉数据，可以在过去8000年的更广泛区域范围内整合当地植被动态。这项研究中提供的新花粉数据来自对沿海地区钻探的岩心的分析，它截断了平原上发生的泻湖沼泽环境，这是对全新世海侵和随后沿海退化的反应。三个放射性碳年龄表明，所分析的岩心间隔的年代顺序为c。7200至c BP 2000 cal yr。整个数据表明，史前时期，当光谱中记录了一些人类活动的迹象时，例如谷物作物，牧场活动和火灾，茂密的森林覆盖物是整个景观的特征。主要的环境变化是自然过程（沿海退化）的推动，但可能是开垦工程加剧的变化，始于希腊罗马时期，导致减少了有利于外平原殖民化的沼泽地区。三个放射性碳年龄表明，所分析的岩心间隔的年代顺序为c。7200至c BP 2000 cal yr。整个数据表明，史前时期，当光谱中记录了一些人类活动的迹象时，例如谷物作物，牧场活动和火灾，茂密的森林覆盖物是整个景观的特征。主要的环境变化是自然过程（沿海退化）的推动，但可能是开垦工程加剧的变化，始于希腊罗马时期，导致减少了有利于外平原殖民化的沼泽地区。三个放射性碳年龄表明，所分析的岩心间隔的年代顺序为c。7200至c BP 2000 cal yr。整个数据表明，史前时期，当光谱中记录了一些人类活动的迹象时，例如谷物作物，牧场活动和火灾，茂密的森林覆盖物是整个景观的特征。主要的环境变化是自然过程（沿海退化）的推动，但可能是开垦工程加剧的变化，始于希腊罗马时期，导致减少了有利于外平原殖民化的沼泽地区。当在光谱中记录到一些人类活动的迹象时，例如谷物作物，牧场活动和火灾。主要的环境变化是自然过程（沿海退化）的推动，但可能是开垦工程加剧的变化，始于希腊罗马时期，导致减少了有利于外平原殖民化的沼泽地区。当在光谱中记录到一些人类活动的迹象时，例如谷物作物，牧场活动和火灾。主要的环境变化是自然过程（沿海退化）的推动，但可能是开垦工程加剧的变化，始于希腊罗马时期，导致减少了有利于外平原殖民化的沼泽地区。