4.3 Article

At the origins of Pompeii: the plant landscape of the Sarno River floodplain from the first millennium bc to the ad 79 eruption

期刊

VEGETATION HISTORY AND ARCHAEOBOTANY
卷 31, 期 2, 页码 171-186

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SPRINGER
DOI: 10.1007/s00334-021-00847-w

关键词

Pompeii; (pre-)Roman age; Pollen; Brassicaceae; Vesuvius

资金

  1. Universita degli Studi di Napoli Federico II within the CRUI-CARE Agreement
  2. University of Padua

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This study reconstructs the environmental evolution and plant landscape of the Sarno floodplain surrounding the ancient city of Pompeii from 900 to 750 cal bc and ad 79, revealing a thin forest cover and a mosaic of vegetation types. Human activities, such as pasturelands, cultivated fields, and the introduction of cabbage cultivation, have been present since pre-Roman times. The study also shows the influence of Mediterranean coastal shrubland, hygrophilous riverine forest, and mesophilous plain forest on the local environment until the catastrophic eruption in ad 79.
The ad 79 eruption of the Vesuvius severely affected the floodplain surrounding the ancient city of Pompeii, i.e. the Sarno River floodplain. The landscape was covered with volcaniclastic materials that destroyed the ecosystem but, at the same time, preserved the traces of former environmental conditions. This study provides-for the first time-a pollen sequence reconstructing the environmental evolution and the plant landscape of the Sarno floodplain between 900 and 750 cal bc and ad 79, i.e. before and during the foundation of the city, and during its life phases. Previous geomorphological studies revealed that the portion of the Sarno floodplain under the Pompeii hill was a freshwater backswamp with patchy inundated and dry areas. Palynology depicts a thin forest cover since the Early Iron Age, suggesting an open environment with a mosaic of vegetation types. The local presence of Mediterranean coastal shrubland, hygrophilous riverine forest and mesophilous plain forest is combined with the regional contribution of mountain vegetation through the sequence. Oscillations between inundated and wet ground characterized the studied area until the ad 79 eruption. Such a natural environment shows anthropogenic traits since pre-Roman times: pasturelands, cultivated fields and olive groves, which probably occupied drier soils. The most important change in the land use system was the introduction of cabbage cultivation in the fourth century bc and its intensification from the second century bc, when Roman influence grew. The presence of tree crops and of ornamental trees reveals the opulence of the Imperial age until the catastrophic eruption.

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