Littérature scientifique sur le sujet « Archéologie sédimentaire »
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Articles de revues sur le sujet "Archéologie sédimentaire"
Piau, Théophile, François Bétard, Fabienne Dugast, Gilles Arnaud-Fassetta et Vincent Viel. « Dynamique géomorphologique holocène et occupation humaine dans le bassin-versant de l’Eure (Bassin de Paris, France) : potentiels d’une approche géoarchéologique multiscalaire et diachronique ». Archimède. Archéologie et histoire ancienne 7 (9 juin 2020) : 188–204. http://dx.doi.org/10.47245/archimede.0007.act.07.
Texte intégralBorderie, Quentin, Barbora Wouters, Rowena Banerjea, Cristiano Nicosia, Grégory Schutz, Franck Gama, Stéphane Augry et Pierre Wech. « Il était une fois des sociétés qui stockaient du carbone en ville : processus de formation et implications sociétales des terres noires urbaines de l’Europe médiévale (Ve−XIe s.). » BSGF - Earth Sciences Bulletin 192 (2021) : 23. http://dx.doi.org/10.1051/bsgf/2021016.
Texte intégralMoulin, Bernard, et Pierre-Jérome Rey. « Les séquences pédo-sédimentaires du col du Petit-Saint-Bernard dans leur contexte archéologique, première approche ». Collection EDYTEM. Cahiers de géographie 6, no 1 (2008) : 191–206. http://dx.doi.org/10.3406/edyte.2008.1040.
Texte intégralBraillard, L. « Remplissages quaternaires et paléohydrologie des vallées sèches d’Ajoie (Jura tabulaire, Suisse) ». Geographica Helvetica 64, no 3 (30 septembre 2009) : 148–56. http://dx.doi.org/10.5194/gh-64-148-2009.
Texte intégralBeaumont, Léa, Chloé Garcia, Pierre Antoine, Nicole Limondin-Lozouet, Boris Brasseur et Julie Dabkowski. « Les tufs calcaires holocènes de la moyenne vallée de la Somme (Nord de la France) : répartition spatiale, chronostratigraphie et implications paléogéographiques ». Varia 29, no 4 (2023). http://dx.doi.org/10.4000/11rh0.
Texte intégralMoulin, Bernard, Marylise Onfray et Ludovic Mevel. « Occupations et réoccupations d’un abri-sous-roche à la fin du Paléolithique récent. Dynamique sédimentaire et microstratigraphie de la séquence archéologique de l’abri des Douattes (Musièges, Haute-Savoie) ». Palethnologie, no 11 (1 juillet 2023). http://dx.doi.org/10.4000/palethnologie.10136.
Texte intégralThèses sur le sujet "Archéologie sédimentaire"
Morin, Denis. « Les systèmes d'exploitation du minerai de fer sédimentaire en Franche-Comté (XVIé-XIXé siècles) : Archéologie, Typologie et Dynamique des systèmes ». Besançon, 1993. http://www.theses.fr/1993BESA1022.
Texte intégralAssi-Kaudjhis, Chimène. « Dynamique des écosystèmes et biodiversité des montagnes du Cameroun au cours des derniers 20 000 ans : Analyse palynologique d'une série sédimentaire du lac Bambili ». Versailles-St Quentin en Yvelines, 2011. http://www.theses.fr/2011VERS0011.
Texte intégralFor many years, interpretations of palynological analysis suggested the opposite climatic conditions between large and small elevations of Atlantic Central Africa. The objective of this work was to document the history of mountain forests of central Africa Atlantic, from the analysis of 14 m of sediment collected near the crater lake Bambili, Cameroon (05 ° 56'11 ''N, 10 ° 14'31''E, 2273m alt. ). This series though dated, has provided unique data covering the last 20 thousand years. Microflora well diversified, shows several changes. Forest cover is extremely low during the glacial period, the vegetation is dominated by herbaceous plants and characterized by the presence of taxa of savannas and steppes: Aerva-type, Boscia-type Capparidaceae undiff. , Commiphora, Crudia-type, Lannea-type. . . That demonstrate the importance of aeolian long distance. As far as global warming at post-glacial, forest recolonization’s observed. It starts at 18,400 cal BP with the appearance of Anthospermum. From 11 500 cal BP, Schefflera opens a new phase of forest expansion, which led to the establishment of the optimum forest dated between 10,000 and 8400 cal BP, interrupted around 8200 cal BP. Subsequently, an instability develops gradually forest leading to the brutal destruction of the forest at 3300 cal BP. This degradation associated with human action, has depleted environment despite the short forest stages that take place between 2500 and 1300 cal BP and beyond than 960 cal BP
Bochaton, Sidonie. « Les chanoines réguliers en Savoie du Nord : Restitution des abbayes d'Abondance et de Sixt (XIIe-XVIIe siècle) ». Electronic Thesis or Diss., Lyon, 2021. http://www.theses.fr/2021LYSE2076.
Texte intégralFounded in the Savoyard "deserts" in the first half of the 12th century, the Abondance congregation had five abbeys in its heyday, spread between Savoy and the Jura, before disappearing at the beginning of the 17th century due to the reform of the mother abbey. Abondance and its first daughter in Sixt are the only abbeys of the congregation to remain in the former diocese of Geneva and are today major sites of Savoyard heritage. While Abondance has benefited from the curiosity of a few archaeologists and architects since 1860, Sixt remained ignored until the year 2000, due to the destruction of parts of the conventual buildings and the development of a hotel within them. A transdisciplinary approach, calling on archaeology, history, art history and the study of textual and iconographic sources, has made it possible to retrace the architectural evolution of the two sites over time, from the 12th to the 19th century. Confronted with the main issues of the canonical movement, such as communal life, pastoral ministry, assistance and charity, or the presence of women in the Augustinian communities, the study of the buildings reveals the choices and the evolution of the life of the brothers of Abondance, from the Gregorian reform to François de Sales, who put an end to this part of Savoyard religious history in 1604. More broadly, this thesis has made it possible to better understand Augustinian architecture in Northern Savoy, a historical region where the Regular Canons were numerous and spread over the territory, but also to refute certain legends and hypotheses generally accepted, such as the identity of Blessed Ponce "de Faucigny"
Ouchaou, Rachid. « Evolution morphosédimentaire de la plaine maritime flamande depuis l'Antiquité : apport des prospections géoradar à la géoarchéologie ». Electronic Thesis or Diss., Université de Lille (2022-....), 2023. http://www.theses.fr/2023ULILR081.
Texte intégralGround-penetrating radar (GPR) is a non-destructive geophysical prospecting tool used to image the finest discontinuities of the underground where the soil is not too conductive. GPR equipment was acquired in 2020 by the Oceanology and Geosciences Laboratory (LOG), which gave rise to bachelor's and master's internships supervised as part of this thesis, as well as academic and industrial collaborations. The first part of the results presented in this memoir is a summary of the surveys carried out on a variety of targets to test the method. GPR gives excellent results on wind-blown sands, and makes it possible to reconstruct the evolution of the coastal dunes affected by climate change. Examples of very-high resolution architectures are provided on the Slack and Pilat dunes. The combined use of different GPR antennas allows describing the mechanisms of sand erosion and deposition, from the scale of seasonal events to that of dune construction on a millennial scale. The backshore area is also explored. The Flemish coastal plain contains sandbodies of kilometer extension, partly buried under the silt of the polders, and which are strategic both for water resources and for the diversity of natural environments. One of the best known is the Ghyvelde fossil dune, an area managed by the Coastal Conservatory. The GPR profiles carried out on the Ghyvelde dune make it possible to image a few meters below the dune a sandy unit of marine or estuarine origin. The polders themselves constitute a target, against all expectations given the clayey and conductive component of these lands. By previously stripping the topsoil, the GPR signal penetrates sufficiently (4m) to image the last channels that drained the plain before it dried up. Finally, two examples show the potential of GPR in geological studies of deeper sedimentary or rocky layers. In the Brussels sands of the Leuven region (Belgium), a penetration depth of more than 30 meters was obtained with a low frequency antenna, making it possible to reconstruct the geometry of tidal sand bar cropping in a sand pit and thereby to guide the sand mining. In the faluns of Anjou, on the heritage and tourist geosite of Perrières, the profiles obtained show the possibility of perfectly imaging the architecture of the rock layers exposed in the subterraneous quarries. Profiles realized on the roads show the feasability of potential extensive mapping by installing the tool on a vehicle. The results obtained on these targets opened up possibilities for developing other areas of research in applied geosciences, particularly with regard to georesources, geoheritage, geohazards and geoenvironment. The memoir presents these different aspects through an article manuscript submitted for publication in a co-edited book produced for decision makers. The second part of the thesis results presented in this memoir is focused on the work done in collaboration with INRAP (the National Institute of Research in Preventive Archaeology) on the Flemish coastal plain. It justifies the title of the dissertation, and is the subject of a manuscript submitted for publication in an international peer-reviewed journal (The Depositional Record). This concerns the evolution since the Middle Age of the eastern bank of the paleo-Denna, a banch of the paleo-delta of the Aa river that had its mouth between Gravelines and Dunkirk. About 30km of GPR profiles acquired as part of the archaeological diagnosis prior to the extension of the Grand Maritime Port of Dunkirk were used to map the last estuarine channels and their evolution during land reclamation. They show progressive shift of the front dikes towards the west which resulted in replacement of the channel system by a continuous layer sandier than the underlying estuarine sediments. This ultimate deposit forms the substrate of the modern agricultural soil of the coastal plain
Sechi-Sapowicz, Serafina. « Les Archives sédimentaires témoins des phases d'érosion : approche géo-archéologique appliquée au bassin versant de la Basse Vallée de la Seine (Normandie, France) et au Campidano Septentrional (Sardaigne, Italie) ». Rouen, 2012. http://www.theses.fr/2012ROUES045.
Texte intégralThe study of sedimentary archives of all geomorphological compartments of the Lower Seine Valley watershed (Normandy), as well as sites of piedmont in the Septentrional Campidano (Central Western Sardinia), enabled us to identify several erosion and sedimentation phases. These phases mark important changes resulting from the direct or indirect impact of several factors or from their combinations Thus erosion markers reveal morphogenetic "crises" controlled by the internal lithologic properties of the studied system, as well as by the climatic and anthropogenic signals. In our study areas, the first erosional phases we have encountered (from the late Pleistocene to the early Holocene) correspond to the major climatic and eustatic changes identified on a global scale. The main impact of the climatic factor continues at least until the beginning of the Neolithic era. From the middle final Neolithic to the Protohistory era, Man became a more active player in causing soil imbalance (i. E: deforestation, switch from a mono-specific agriculture to a professionalized agriculture). From the end of the Iron Age to the Roman period, Man became an aggravating factor (i. E: high deforestation, intensive land use). Later, from the Middle-Ages to the Contemporary era, Man became the triggering factor (i. E: the land becomes a mosaic of cropped agricultural areas with a shift towards agriculture with heavy animal tractation) that has a direct impact on the major erosional phases. Once it passed a certain threshold of imbalance accelerated by human activities that made the soil more susceptible to the weather hazards, the resilience of the environment stops and follows to climate fluctuations however minor
Borderie, Quentin. « L'espace urbain entre Antiquité et Moyen Age : analyse géoarchéologique des terres noires : études de cas ». Paris 1, 2011. http://www.theses.fr/2011PA010689.
Texte intégralKerdivel, Gwenolé. « Occupation de l'espace et gestion des ressources à l'interface entre massifs primaires et bassins secondaires et tertiaires : l'exemple du Massif armoricain et de ses marges au Néolitihique ». Rennes 1, 2009. https://tel.archives-ouvertes.fr/tel-00482886.
Texte intégralThis work approaches the question of the occupation of the space and the management of the resources between Armorican Massif and Paris or Aquitain Basin. It postulates that the characteristics of these two geologic entities were relevant as regards human settlement, which changed a lot during the Neolithic period. To achieve this study, I used methodological and statistical tools as for geography studies. After discussing the archaeological research, listing, observing and analysing the settlements, period after period, I will enhance the role of the cultural factors. Then, the relation of these settlements according to several physical criteria (topographical, hydrographical, geological, pedological) will be discussed, in particular to show various ways to manage resources unevenly distributed. As the study covers a huge territory (more than 62 000 km²), we can demonstrate that now the spatial distribution of the sample of available data (4201 settlements), although for a long time considered as only dependent on a state of the research, is also significant henceforth of a reality in prehistoric past. A proposition of model of populating for the whole Neolithic in the interface Armorican Massif / Paris or Aquitain Basin, is formulated. This one shows the acquisition of new strategies of subsistence, which would have become a reality by a progressive adaptation to environments more and more varied from the Early Neolithic to the Final Neolithic