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Reconstruction du paysage végétal dans les Apennins septentrionaux, au Monte Cimone et à Corne Alle Scole (Italie) durant l'holocène tardif : approche multi proxy / Ricostruzione del paesaggio vegetale dell'Appennino settentrionale al Monte Cimone e al Corno Alle Scale (italia) durante il tardo olocene : approccio multriproxyBenatti, Alessandra 07 November 2018 (has links)
La recherche de doctorat ici présentée porte sur l’histoire et sur l’évolution du paysage végétal montagnard nord-apenninique et de son lien avec les activités anthropiques qui l’ont façonné au fil du temps. Notre idée de thèse est née grâce au projet international AGRESPE (réseAu Gestion de Ressources Environnementales passéeS et Patrimonialisation paysagèrE), dirigé par Marie Bal du laboratoire de Géographie GEOLAB UMR/CNRS 6042 de l’Université de Limoges. Le travail de thèse a été mené en cotutelle avec l’Université de Modena et Reggio Emilia (Italie).Le paysage végétal des Apennins du Nord a fait l'objet de nombreuses recherches scientifiques sur le paléo-environnement, représentées surtout par des études polliniques (ex. Cruise 1990a, 1990b ; Lowe, 1992 ; Watson, 1996 ; Vescovi et al, 2010a, 2010a, 2010b ; Branch, 2013), mais il présente encore des lacunes sur les recherches paléoenvironnementales et paléoécologiques de haute résolution spatiale. À cause de facteurs liés aux conditions physiques de la montagne et aux intérêts des chercheurs, la recherche archéologique (notamment celle pastorale) n’est pas très développée par rapport aux études de la plaine (Fontana, 1997 ; Cardarelli et Malnati, 2006 ; Ferrari et al., 2006). Ce manque d'études sur les relations entre les sociétés et leur environnement dans les Apennins nous a donc encouragés à en découvrir davantage. Au sein de ce secteur montagnard nous avons choisi deux montagnes clés : le Monte Cimone et le Corno alle Scale. Faisant partie de deux parc régionaux, ces zones d’étude sont caractérisées par des hêtraies qui, jusqu’au milieu du XXe siècle, ont été gérées en taillis pour la production de bois de chauffage et de charbon. La limite altitudinale de la forêt est plus basse que celle écologique potentielle. Au Monte Cimone elle est localisée à 1700 m, tandis que dans la zone du Corno alle Scale elle est située à environ 1600 m. Au-dessus de la limite forestière il y a des bruyères à myrtille et des prairies qui, à l’instar du passé, sont aujourd’hui destinées au pâturage. / This PhD thesis concerns the reconstruction and the development of the Late Holocene plant landscape of two mountain areas of the Northern Apennines: the area of Monte Cimone and the area of Monte Corno alle Scale, located in the two regional parks. Previous research in the two study areas consists of quite numerous pollen analyses at regional scale while studies at local-scale, such as archaeoanthracology and pedoanthracology, are scarce.We have therefore decided to study these two mountain areas through pedoanthracology that is the taxonomic identification of wood charcoals contained in soils. Moreover, archaeoanthracology was applied to charcoal platforms and consists in the analysis of charcoals contained in the platforms which were used until the mid-20th century to produce charcoal. In the methodology used in this thesis are also included field surveys with the aim of locate and geolocalize ancient pastoral structures, witnesses of pastoral activities at high elevations.The main objectives of this research were: - to reconstruct the plant landscape; - to understand how human activities (e.g. pastoralism and forest exploitation) have transformed the landscape; to study the fire history; - to identify the variations of tree and timberline in the past.In the Monte Cimone area, nine pedoanthracological trenches were cut between 1650 m and 2078 m of elevation, and about 4000 charcoals were analyzed; moreover, 10 pastoral structures were found and georeferenced. In the Corno alle Scale area, eight pedoanthracological trenches were cut between 1600 m and 1860 m of elevation, and more than 2000 charcoals were analyzed; no pastoral structure were identified here. In each study area, four charcoal platforms were sampled with a total of 1200 charcoals analysed. Overall, 33 C14datings were performed on charcoals. Almost all C14 dates of soil charcoal are concentrated in the Late Holocene and only two are from the Early Holocene. The anthracomass of the low elevation sampling points (e.g. 962.8 mg/kg) is higher than the anthracomass of the high elevation sampling points (e.g. 1.6 mg/kg). The charcoals are evidence of the past presence of Ericaceae, Fabaceae, Juniperus sp., Abies alba, Quercus sp./Castanea sp., Prunus sp., Betula sp., Taxus baccata, Fagus sylvatica, Fraxinus sp. And Acer sp.The main results of this research show a plant landscape during the last 3000 years that is very similar to the current one with little variations in the tree and timberline. Charcoal platforms analysis has shown a beech charcoal production during the centuries between the 15th and mid-20th centuries. Estimation of the wood size used suggest a well-run exploitation of the timber resource. The two main activity in high mountain, pastoralism and charcoal production, seem to have played an important role in the shaping the current plant landscape.
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Charcoal Kiln Detection from LiDAR-derived Digital Elevation Models Combining Morphometric Classification and Image Processing TechniquesZutautas, Vaidutis January 2017 (has links)
This paper describes a unique method for the semi-automatic detection of historic charcoal production sites in LiDAR-derived digital elevation models. Intensified iron production in the early 17th century has remarkably influenced ways of how the land in Sweden was managed. Today, the abundance of charcoal kilns embedded in the landscape survives as cultural heritage monuments that testify about the scale forest management for charcoal production has contributed to the uprising iron manufacturing industry. An arbitrary selected study area (54 km2) south west of Gävle city served as an ideal testing ground, which is known to consist of already registered as well as unsurveyed charcoal kiln sites. The proposed approach encompasses combined morphometric classification methods being subjected to analytical image processing, where an image that represents refined terrain morphology was segmented and further followed by Hough Circle transfer function applied in seeking to detect circular shapes that represent charcoal kilns. Sites that have been identified manually and using the proposed method were only verified within an additionally established smaller validation area (6 km2). The resulting outcome accuracy was measured by calculating harmonic mean of precision and recall (F1-Score). Along with indication of previously undiscovered site locations, the proposed method showed relatively high score in recognising already registered sites after post-processing filtering. In spite of required continual fine-tuning, the described method can considerably facilitate mapping and overall management of cultural resources.
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