Plants, Fire and Landscape at the Prehistoric Pile-Dwelling Village of Palù di Livenza (PaluON1), UNESCO Site in the Italian Alps
Jessica Zappa,
Nicola Degasperi,
Michele Bassetti,
Assunta Florenzano,
Paola Torri,
Gabriel Servera-Vives,
Anna Maria Mercuri,
Roberto Micheli
Affiliations
Jessica Zappa
Laboratorio di Palinologia e Paleobotanica, Dipartimento Scienze Vita, Università degli Studi di Modena e Reggio Emilia, Via Campi 287, 41125 Modena, Italy
Nicola Degasperi
Cora Società Archeologica S.r.l., Via Salisburgo 16, I-38121 Trento, Italy
Michele Bassetti
Cora Società Archeologica S.r.l., Via Salisburgo 16, I-38121 Trento, Italy
Assunta Florenzano
Laboratorio di Palinologia e Paleobotanica, Dipartimento Scienze Vita, Università degli Studi di Modena e Reggio Emilia, Via Campi 287, 41125 Modena, Italy
Paola Torri
Laboratorio di Palinologia e Paleobotanica, Dipartimento Scienze Vita, Università degli Studi di Modena e Reggio Emilia, Via Campi 287, 41125 Modena, Italy
Gabriel Servera-Vives
Laboratorio di Palinologia e Paleobotanica, Dipartimento Scienze Vita, Università degli Studi di Modena e Reggio Emilia, Via Campi 287, 41125 Modena, Italy
Anna Maria Mercuri
Laboratorio di Palinologia e Paleobotanica, Dipartimento Scienze Vita, Università degli Studi di Modena e Reggio Emilia, Via Campi 287, 41125 Modena, Italy
Roberto Micheli
Soprintendenza Archeologia, Belle Arti e Paesaggio del Friuli Venezia Giulia, Piazza della Libertà 7, I-34135 Trieste, Italy
This paper presents palynological data obtained from a trench excavated at the Neolithic pile-dwelling archaeological site of Palù di Livenza (northeastern Italy). The site is in a wetland located in a tectonic basin at the foot of the Cansiglio plateau, crossed by the Livenza river. Environmental conditions have made this wetland a suitable area for settlements since prehistoric times. Thanks to the peaty sediments that characterise the area, archaeological materials and botanical remains have been exceptionally well preserved. Their study has shed light on a Neolithic pile-dwelling settlement that developed in various phases between c. 6350 and 5600 cal BP (c. 4400 and 3650 BC), and has also allowed for a detailed environmental reconstruction of the surrounding environment. A vertical sequence of 20 samples was analysed to study pollen, non-pollen palynomorphs and microcharcoals. An age-depth model was performed based on three radiocarbon dates. The palynological analysis provided insight into the response of vegetation to environmental changes caused by both climatic fluctuations and human pressure. In this sense, it was possible to highlight differences in vegetation cover, some fires, the use of woody resources, the spread of cereal fields, as well as the presence of other cultivated plants and plant processing by the people within the village.