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THE MESSINIAN SALINITY CRISIS GEOSITES IN THE LANDSCAPE OF THE MIDDLE TANARO VALLEY

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THE MESSINIAN SALINITY CRISIS GEOSITES IN THE

LANDSCAPE OF THE MIDDLE TANARO VALLEY

Enrico Giordano*(1) , Marcello Natalicchio(1), Luca Ghiraldi(2), Francesca Lozar(1),

Francesco Dela Pierre(1) and Marco Giardino(1)

(1)University of Torino, Earth Sciences Department, via Valperga Caluso, 35 – 10125 Torino, Italy (2)Natural Sciences Museum, via Giolitti, 36 – 10123 Torino, Italy

E-mail: * [email protected]

Keywords: Tanaro river, landscape, geosite, geotourism, Messinian salinity crisis

This study analyzes the relationship between geoheritage and landscape in the SW sector of the Piemonte region (NW Italy), along the Tanaro riverside. From the geological point of view the area is part of the Piedmont Basin, a wedge-top basin filled with a thick succession of marine sediments deposited from the Eocene to Holocene. In particular we focused on four geosites dealing with the Messinian salinity crisis, a dramatic palaeoenvironmental, palaeobiological and palaeoclimatic event that occurred in the Mediterranean area around 6 Ma ago. From the geomorphologic point of view, the study area is located in the SE part of the Cuneo plain, at the foot of the Langhe hills, where heterogeneous forms, mainly related to the Tanaro river piracy, are observed.

The aims of this study are: 1) to analyze the link between geosites and recent landscape modification, 2) to reconstruct the landscape evolution (past and future) and, through geotourism, 3) to promote geological knowledge in an area with great potential for tourism.

Two maps have been produced to disseminate the geodiversity (the geological -landscape map) and to promote geotourism (the geotouristic map).

The geological - landscape map allows us to deal with different topics based on geological and geomorphologic issues thanks to illustrations of the main features of the Messinian deposits, their depositional environments and the exposed landforms. The area has been divided into some morphologic sectors on the basis of their characteristic landforms and evolution. In each of these sectors geosites have been identified to clarify the comprehension of these topics at the widest public: the geosites will help to reconstruct the stages of the MSC and understand the implication of fast environmental changes on the living beings.

The geotouristic map describes the geological and geomorphologic features with a simpler and shorter language than the previous one. Trails, viewpoints and museums will be reported on the map to facilitate the comprehension of the landscape and to create a link between the scientific issues and human activities (i.e. use of gypsum in the building industry). Moreover the geomorphologic analysis of the present landscape allowed to decipher its recent evolution and to evaluate the risks connected with the tourist fruition, thus improving the potential use of anthropogenic landforms for geo-environmental education. Here the MSC is dealt with through the stages of scientific discoveries that led to the formulation of the current theories.

In conclusion, the produced maps may help both to improve people knowledge and awareness on environmental modification and past climate variability and to address the crucial question whether they could happen again in the future.

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