[ { "key": "SAVNJFM6", "version": 4307, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/SAVNJFM6", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/SAVNJFM6", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Richards et al.", "parsedDate": "2025", "numChildren": 0 }, "data": { "key": "SAVNJFM6", "version": 4307, "itemType": "journalArticle", "title": "Map and Archival Evidence of the Historical Avulsion of the Brahmaputra River", "creators": [ { "creatorType": "author", "firstName": "Keith", "lastName": "Richards" }, { "creatorType": "author", "firstName": "Hugh", "lastName": "Brammer" }, { "creatorType": "author", "firstName": "Patricia", "lastName": "Saunders" } ], "abstractNote": "The Brahmaputra River is one of the world's largest rivers, entering the Bengal Basin from its extensive Himalayan catchment, flowing south through Bangladesh, and joining the Ganges to traverse a complex fan-delta and enter the Bay of Bengal. When Major James Rennell surveyed the river to establish the ‘Route Surveys’ for the East India Company between 1765 and 1777, it followed a different course, turning to the South-East into the Sylhet Basin, and joining the Meghna. Some time after this, it changed its course—it avulsed—and a re-survey was undertaken by Captain Richard Wilcox in 1828–1830 which first showed its present-day southerly route. However, there is uncertainty about when, why, and how this major adjustment occurred, and these questions can only be answered with recourse to archival materials. This paper accordingly pieces together information in the writings of travellers and East India Company officials in the region in the period between 1787 and 1854; evidence of boundary changes in 1806; archival material indicating that the East India Company was concerned enough about declining flow in the ‘Old’ Brahmaputra to consider engineering works by 1845; and contemporary evidence of the widespread impact of severe monsoon floods in 1787; to conclude that the avulsion probably took place rather earlier than often assumed. And intriguingly, it seems that although Rennell left India in 1777, in the first edition of his Memoir published after those floods had occurred (1788), he inserted a brief reference to the Brahmaputra changing its course.", "publicationTitle": "The Geographical Journal", "publisher": "", "place": "", "date": "2025", "volume": "n/a", "issue": "n/a", "section": "", "partNumber": "", "partTitle": "", "pages": "e70059", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1111/geoj.70059", "citationKey": "", "url": "https://onlinelibrary.wiley.com/doi/abs/10.1111/geoj.70059", "accessDate": "2025-12-14T10:49:26Z", "PMID": "", "PMCID": "", "ISSN": "1475-4959", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "© 2025 The Author(s). The Geographical Journal published by John Wiley & Sons Ltd on behalf of Royal Geographical Society (with the Institute of British Geographers).", "extra": "_eprint: https://rgs-ibg.onlinelibrary.wiley.com/doi/pdf/10.1111/geoj.70059", "tags": [ { "tag": "Brahmaputra River", "type": 1 }, { "tag": "East India Company", "type": 1 }, { "tag": "James Rennell", "type": 1 }, { "tag": "archival material", "type": 1 }, { "tag": "monsoon floods", "type": 1 }, { "tag": "river avulsion", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2025-12-14T10:49:26Z", "dateModified": "2025-12-14T10:50:03Z" } }, { "key": "RGYY6V5F", "version": 4301, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/RGYY6V5F", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/RGYY6V5F", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Ravanel", "parsedDate": "2025-07-01", "numChildren": 0 }, "data": { "key": "RGYY6V5F", "version": 4301, "itemType": "journalArticle", "title": "Les glacières, mémoire souterraine en péril", "creators": [ { "creatorType": "author", "firstName": "Ludovic", "lastName": "Ravanel" } ], "abstractNote": "Les glacières sont des cavités souterraines naturelles dans lesquelles de la glace formée il y a plusieurs siècles ou millénaires peut persister. Ces systèmes cryogéniques uniques se mettent en place dans des contextes géologiques, topographiques et climatiques spécifiques, qui favorisent l'accumulation et la conservation du froid hivernal tandis que la température moyenne annuelle de l’air en surface peut être positive. Contrairement aux glaciers, les masses de glace souterraines sont partiellement à l'abri des aléas climatiques immédiats, ce qui leur confère un rôle d’archives paléoenvironnementales. Fondé sur plus de 100 publications scientifiques, dont les 31 chapitres de l’ouvrage collectif de référence Ice Caves, cet article propose une synthèse des différentes dimensions de ces systèmes uniques : genèse, typologie morphodynamique, fonctionnement thermique, rôle d’archives paléoclimatiques et paléoenvironnementales, dimension patrimoniale, et menaces croissantes sur leur pérennité.", "publicationTitle": "Géomorphologie : relief, processus, environnement", "publisher": "", "place": "", "date": "2025/07/01", "volume": "31", "issue": "1", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.4000/14gyu", "citationKey": "", "url": "https://journals.openedition.org/geomorphologie/20066", "accessDate": "2025-08-13T07:42:06Z", "PMID": "", "PMCID": "", "ISSN": "1266-5304", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "journals.openedition.org", "callNumber": "", "rights": "All rights reserved", "extra": "Publisher: Groupe français de géomorphologie", "tags": [ { "tag": "archive paléoenvironnementale", "type": 1 }, { "tag": "glace souterraine", "type": 1 }, { "tag": "glacière", "type": 1 }, { "tag": "piège à froid", "type": 1 }, { "tag": "système cryogénique", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2025-08-13T07:42:06Z", "dateModified": "2025-08-13T07:42:06Z" } }, { "key": "FCRDZCJR", "version": 3853, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/FCRDZCJR", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/FCRDZCJR", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Becker et al.", "parsedDate": "2017-12-07", "numChildren": 0 }, "data": { "key": "FCRDZCJR", "version": 3853, "itemType": "journalArticle", "title": "A study of the Würm glaciation focused on the Valais region (Alps)", "creators": [ { "creatorType": "author", "firstName": "Patrick", "lastName": "Becker" }, { "creatorType": "author", "firstName": "Martin", "lastName": "Funk" }, { "creatorType": "author", "firstName": "Christian", "lastName": "Schlüchter" }, { "creatorType": "author", "firstName": "Kolumban", "lastName": "Hutter" } ], "abstractNote": "During the Last Glacial Maximum (LGM), the glaciation in the European Alps reached maximum ice extent. We already simulated the steady states of the Alpine ice coverage for several climate drivers in Becker et al. (2016) and heighten in this article such studies for the Swiss Valais region. To this end, we employ the Parallel Ice Sheet Model (PISM), which combines the shallow ice approximation (SIA) with basal sliding elements of the shallow shelf approximation (SSA), and subject this model to various external driving mechanisms. We further test the sensitivity of this kind of the ice coverage in the Valais region to a temporally constant climate and to monotonic ice sheet build-up from inception to steady state as well as to the Dye 3 temperature driving during the past 120 000 years. We also test differences in the precipitation patterns exerted to the northern and southern catchment areas of the Rhone and Toce rivers to possible transfluence changes in ice from the northern to the southern catchment areas and vice versa. Moreover, we study the effect of the ice deformability and estimate the removal up to 1000 m of sediment in the Rhone Valley and study the removal of rock hindering the flow through the valley cross section at the knee of Martigny. All these studies took place because of a discrepancy in the ice height prediction of the modelled ice sheet with its geomorphologically reconstructed counterpart with proxy data obtained by Bini et al. (2009) as well as a difference in ice height between the two of up to 800 m. Unfortunately, all the scenarios in the model do not sufficiently reduce this discrepancy in the height prediction and the geomorphological reconstruction. The model results have discovered an ice dynamical discrepancy with the land map in Bini et al. (2009).", "publicationTitle": "Geographica Helvetica", "publisher": "", "place": "", "date": "2017/12/07", "volume": "72", "issue": "4", "section": "", "partNumber": "", "partTitle": "", "pages": "421-442", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "https://doi.org/10.5194/gh-72-421-2017", "citationKey": "", "url": "https://www.geogr-helv.net/72/421/2017/", "accessDate": "2018-01-09T16:39:24Z", "PMID": "", "PMCID": "", "ISSN": "0016-7312", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "English", "libraryCatalog": "www.geogr-helv.net", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2018-01-09T16:39:24Z", "dateModified": "2018-01-09T16:39:24Z" } }, { "key": "66W4XK99", "version": 3715, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/66W4XK99", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/66W4XK99", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Favrod", "parsedDate": "2016-08-02", "numChildren": 0 }, "data": { "key": "66W4XK99", "version": 3715, "itemType": "newspaperArticle", "title": "Quand le fond du Léman explique un tsunami", "creators": [ { "creatorType": "author", "firstName": "Justin", "lastName": "Favrod" } ], "abstractNote": "C’est grâce aux limonologues que l’on a pu percer l’énigme du tsunami qui ravagea les rives du Léman et dont se sont faits les chroniqueurs Marius d’Avenches et Grégoire de Tours. Un gigantesque glissement de terrain qui charrie avec lui 250 millions de m3 de matière du haut lac vers le centre. Explication", "publicationTitle": "Le Temps", "publisher": "", "place": "Lausanne, Suisse", "date": "2016-08-02", "volume": "", "issue": "", "edition": "", "section": "", "pages": "", "ISSN": "", "DOI": "", "citationKey": "", "url": "https://www.letemps.ch/suisse/2016/08/02/fond-leman-explique-un-tsunami", "accessDate": "", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2016-08-04T09:00:45Z", "dateModified": "2016-08-04T09:01:34Z" } }, { "key": "PPDCKC8B", "version": 3708, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/PPDCKC8B", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/PPDCKC8B", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Baud and Reynard", "parsedDate": "2015-12-31", "numChildren": 0 }, "data": { "key": "PPDCKC8B", "version": 3708, "itemType": "journalArticle", "title": "Géohistoire d’une trajectoire paysagère dans la plaine du Rhône valaisan. Analyse du secteur entre Riddes et Martigny (1840-1965)", "creators": [ { "creatorType": "author", "firstName": "Dominique", "lastName": "Baud" }, { "creatorType": "author", "firstName": "Emmanuel", "lastName": "Reynard" }, { "creatorType": "contributor", "firstName": "Aziz", "lastName": "Ballouche" }, { "creatorType": "contributor", "firstName": "Karl Matthias", "lastName": "Wantzen" }, { "creatorType": "contributor", "firstName": "Isabelle", "lastName": "Longuet" }, { "creatorType": "contributor", "firstName": "Laura", "lastName": "Verdeli" } ], "abstractNote": "Le Rhône à l’amont du lac Léman, dans sa partie suisse, a vécu d’importants travaux d’aménagement (endiguement, rectification du cours) dès 1863. Cet aménagement a été à l’origine d’une transformation radicale du paysage fluvial, qui a vu progressivement les parcelles de cultures intensives (arboriculture, cultures maraîchères) remplacer progressivement les anciennes zones humides et les forêts alluviales. Cette transition paysagère a toutefois duré une centaine d’années et n’a été ni linéaire dans le temps ni homogène dans l’espace. L’approche géohistorique, qui exploite à la fois les sources iconographiques et cartographiques et les archives textuelles, permet non seulement de reconstituer de manière fine la trajectoire paysagère mais aussi d’analyser les raisons des transformations et les dynamiques sociales et politiques à l’origine des transformations paysagères.", "publicationTitle": "Norois. Environnement, aménagement, société", "publisher": "", "place": "", "date": "2015/12/31", "volume": "", "issue": "237", "section": "", "partNumber": "", "partTitle": "", "pages": "15-31", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://norois.revues.org/5761", "accessDate": "2016-07-19T12:33:18Z", "PMID": "", "PMCID": "", "ISSN": "0029-182X", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "norois.revues.org", "callNumber": "", "rights": "© Tous droits réservés", "extra": "", "tags": [ { "tag": "Rhône", "type": 1 }, { "tag": "aménagements", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "paysages fluviaux", "type": 1 }, { "tag": "transition paysagère", "type": 1 } ], "collections": [ "362FN9GJ", "WN9F88J4" ], "relations": {}, "dateAdded": "2016-07-19T12:33:18Z", "dateModified": "2016-07-19T12:33:18Z" } }, { "key": "4D8DA6EV", "version": 3662, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/4D8DA6EV", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/4D8DA6EV", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Häuselmann et al.", "parsedDate": "2015-10-15", "numChildren": 0 }, "data": { "key": "4D8DA6EV", "version": 3662, "itemType": "journalArticle", "title": "Snežna jama (Slovenia): Interdisciplinary dating of cave sediments and implication for landscape evolution", "creators": [ { "creatorType": "author", "firstName": "Philipp", "lastName": "Häuselmann" }, { "creatorType": "author", "firstName": "Andrej", "lastName": "Mihevc" }, { "creatorType": "author", "firstName": "Petr", "lastName": "Pruner" }, { "creatorType": "author", "firstName": "Ivan", "lastName": "Horáček" }, { "creatorType": "author", "firstName": "Stanislav", "lastName": "Čermák" }, { "creatorType": "author", "firstName": "Helena", "lastName": "Hercman" }, { "creatorType": "author", "firstName": "Diana", "lastName": "Sahy" }, { "creatorType": "author", "firstName": "Markus", "lastName": "Fiebig" }, { "creatorType": "author", "firstName": "Nadja Zupan", "lastName": "Hajna" }, { "creatorType": "author", "firstName": "Pavel", "lastName": "Bosák" } ], "abstractNote": "Caves are important markers of surface evolution, since they are, as a general rule, linked with ancient valley bottoms by their springs. However, caves can only be dated indirectly by means of the sediments they contain. If the sediment is older than common dating methods, one has to use multiple dating approaches in order to get meaningful results. U/Th dating, palaeomagnetic analysis of flowstone and sediment profiles, cosmogenic dating of quartz pebbles, and mammalian dating allowed a robust estimate of speleogenesis, sediment deposition, climatic change at the surface, and uplift history on the Periadriatic fault line during the Plio-Pleistocene. Our dates indicate that Snežna jama was formed in the (Upper) Miocene, received its sedimentary deposits during the Pliocene in a rather low-lying, hilly landscape, and became inactive due to uplift along the Periadriatic and Sava faults and climatic changes at the beginning of the Quaternary. Although it is only a single cave, the information contained within it makes it an important site of the Southern Alps.", "publicationTitle": "Geomorphology", "publisher": "", "place": "", "date": "octobre 15, 2015", "volume": "247", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "10-24", "series": "SPECIAL ISSUE KARST GEOMORPHOLOGY: FROM HYDROLOGICAL FUNCTIONING TO PALAEOENVIRONMENTAL RECONSTRUCTIONS. PART II", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Geomorphology", "DOI": "10.1016/j.geomorph.2014.12.034", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0169555X14006382", "accessDate": "2016-01-11T15:29:52Z", "PMID": "", "PMCID": "", "ISSN": "0169-555X", "archive": "", "archiveLocation": "", "shortTitle": "Snežna jama (Slovenia)", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Cave sediment dating", "type": 1 }, { "tag": "Dating methods", "type": 1 }, { "tag": "Periadriatic fault", "type": 1 }, { "tag": "Slovenia", "type": 1 }, { "tag": "Speleogenesis", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2016-01-11T15:29:52Z", "dateModified": "2016-01-11T15:29:52Z" } }, { "key": "7WQTSQ72", "version": 3655, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/7WQTSQ72", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/7WQTSQ72", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Beach et al.", "parsedDate": "2015-09-15", "numChildren": 0 }, "data": { "key": "7WQTSQ72", "version": 3655, "itemType": "journalArticle", "title": "Ancient Maya impacts on the Earth's surface: An Early Anthropocene analog?", "creators": [ { "creatorType": "author", "firstName": "Tim", "lastName": "Beach" }, { "creatorType": "author", "firstName": "Sheryl", "lastName": "Luzzadder-Beach" }, { "creatorType": "author", "firstName": "Duncan", "lastName": "Cook" }, { "creatorType": "author", "firstName": "Nicholas", "lastName": "Dunning" }, { "creatorType": "author", "firstName": "Douglas J.", "lastName": "Kennett" }, { "creatorType": "author", "firstName": "Samantha", "lastName": "Krause" }, { "creatorType": "author", "firstName": "Richard", "lastName": "Terry" }, { "creatorType": "author", "firstName": "Debora", "lastName": "Trein" }, { "creatorType": "author", "firstName": "Fred", "lastName": "Valdez" } ], "abstractNote": "The measure of the “Mayacene,” a microcosm of the Early Anthropocene that occurred from c. 3000 to 1000 BP, comes from multiple Late Quaternary paleoenvironmental records. We synthesized the evidence for Maya impacts on climate, vegetation, hydrology and the lithosphere, from studies of soils, lakes, floodplains, wetlands and other ecosystems. Maya civilization had likely altered local to regional ecosystems and hydrology by the Preclassic Period (3000-1700 BP), but these impacts waned by 1000 BP. They altered ecosystems with vast urban and rural infrastructure that included thousands of reservoirs, wetland fields and canals, terraces, field ridges, and temples. Although there is abundant evidence that indicates the Maya altered their forests, even at the large urban complex of Tikal as much as 40% of the forest remained intact through the Classic period. Existing forests are still influenced by ancient Maya forest gardening, particularly by the large expanses of ancient stone structures, terraces, and wetland fields that form their substrates. A few studies suggest deforestation and other land uses probably also warmed and dried regional climate by the Classic Period (1700-1100 BP). A much larger body of research documents the Maya impacts on hydrology, in the form of dams, reservoirs, canals, eroded soils and urban design for runoff. Another metric of the “Mayacene” are paleosols, which contain chemical evidence for human occupation, revealed by high phosphorus concentrations and carbon isotope ratios of C4 species like maize in the C3–dominated tropical forest ecosystem. Paleosol sequences exhibit “Maya Clays,” a facies that reflects a glut of rapidly eroded sediments that overlie pre-Maya paleosols. This stratigraphy is conspicuous in many dated soil profiles and marks the large-scale Maya transformation of the landscape in the Preclassic and Classic periods. Some of these also have increased phosphorous and carbon isotope evidence of C4 species. We synthesize and provide new evidence of Maya-period soil strata that show elevated carbon isotope ratios (δ13C), indicating the presence of C4 species in typical agricultural sites. This is often the case in ancient Maya wetland systems, which also have abundant evidence for the presence of several other economic plant species. The “Mayacene” of c. 3000 to 1000 BP was thus a patchwork of cities, villages, roads, urban heat islands, intensive and extensive farmsteads, forests and orchards. Today, forests and wetlands cover much of the Maya area but like so many places, these are now under the onslaught of the deforestation, draining, and plowing of the present Anthropocene.", "publicationTitle": "Quaternary Science Reviews", "publisher": "", "place": "", "date": "septembre 15, 2015", "volume": "124", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "1-30", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Quaternary Science Reviews", "DOI": "10.1016/j.quascirev.2015.05.028", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0277379115300056", "accessDate": "2015-12-09T14:51:23Z", "PMID": "", "PMCID": "", "ISSN": "0277-3791", "archive": "", "archiveLocation": "", "shortTitle": "Ancient Maya impacts on the Earth's surface", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Aggradation", "type": 1 }, { "tag": "Carbon isotopes", "type": 1 }, { "tag": "Early Anthropocene", "type": 1 }, { "tag": "Maya Lowlands", "type": 1 }, { "tag": "Mayacene", "type": 1 }, { "tag": "Paleoecology", "type": 1 }, { "tag": "Paleosols", "type": 1 }, { "tag": "Phosphorus", "type": 1 }, { "tag": "geoarchaeology", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2015-12-09T14:51:23Z", "dateModified": "2015-12-09T14:51:23Z" } }, { "key": "GQRDXRUQ", "version": 3615, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/GQRDXRUQ", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/GQRDXRUQ", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Mardhiah et al.", "parsedDate": "2015", "numChildren": 0 }, "data": { "key": "GQRDXRUQ", "version": 3615, "itemType": "journalArticle", "title": "Reconstructing the development of sampled sites on fluvial island surfaces of the Tagliamento River, Italy, from historical sources", "creators": [ { "creatorType": "author", "firstName": "Ulfah", "lastName": "Mardhiah" }, { "creatorType": "author", "firstName": "Matthias C", "lastName": "Rillig" }, { "creatorType": "author", "firstName": "Angela", "lastName": "Gurnell" } ], "abstractNote": "In parallel with research on surface sediment characteristics of evolving island features (patches) along an island-braided reach of the Tagliamento River, Italy, the present research reconstructed the development of the sampled sites using historical information coupled with field measurements. Since any field sediment sampling programme inevitably focuses on small areas (of the order of a few metres), the historical sources were assessed bearing in mind their spatial resolution and geographical accuracy in relation to the size of the sampled sites, and the information they could provide regarding the historical evolution of those sites. The analysis combined four sources of information: (i) river stage records revealed flood events that had the potential to reset bar surfaces and float in wood and seeds to initiate vegetation colonization; (ii) oblique ground photographs identified areas of the river's active corridor where riparian vegetation colonization appeared to have been initiated by specific flood events; (iii) dendrochronology was used to estimate the age of sampled sites; (iv) field-measured geographical locations of the sampled sites were combined with historical vertical areal imagery to further establish sampling site age and changes in vegetation cover from 1944 to 2012. A chronosequence of sampled sites (0, 2, 8, 12, 40 years) was established. Vegetation colonization and island development showed a statistically significant development trajectory among sites of each age across the 40 year period following formative floods in 1965–1966, 2000, 2004 and a flow pulse in 2010. The trajectory progressed through pioneer and building island stages until vegetated areas became part of established islands. Evidence from the younger sites indicates that the pioneer island phase lasts up to eight years. Evidence from the oldest site indicates a building island phase lasting a maximum of 30 years, but probably a lot less. Copyright © 2014 John Wiley & Sons, Ltd.", "publicationTitle": "Earth Surface Processes and Landforms", "publisher": "", "place": "", "date": "avril 1, 2015", "volume": "40", "issue": "5", "section": "", "partNumber": "", "partTitle": "", "pages": "629-641", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Earth Surf. Process. Landforms", "DOI": "10.1002/esp.3658", "citationKey": "", "url": "http://onlinelibrary.wiley.com/doi/10.1002/esp.3658/abstract", "accessDate": "2015-05-18T12:06:05Z", "PMID": "", "PMCID": "", "ISSN": "1096-9837", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "Copyright © 2014 John Wiley & Sons, Ltd.", "extra": "", "tags": [ { "tag": "Braided river", "type": 1 }, { "tag": "Fluvial processes", "type": 1 }, { "tag": "historical analysis", "type": 1 }, { "tag": "island development", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2015-05-18T12:06:05Z", "dateModified": "2015-05-18T12:06:05Z" } }, { "key": "TXUW6I55", "version": 3598, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/TXUW6I55", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/TXUW6I55", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Guerrin", "parsedDate": "2015", "numChildren": 0 }, "data": { "key": "TXUW6I55", "version": 3598, "itemType": "journalArticle", "title": "A floodplain restoration project on the River Rhône (France): analyzing challenges to its implementation", "creators": [ { "creatorType": "author", "firstName": "Joana", "lastName": "Guerrin" } ], "abstractNote": "", "publicationTitle": "Regional Environmental Change", "publisher": "", "place": "", "date": "3/2015", "volume": "15", "issue": "3", "section": "", "partNumber": "", "partTitle": "", "pages": "559-568", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1007/s10113-014-0650-8", "citationKey": "", "url": "http://link.springer.com/10.1007/s10113-014-0650-8", "accessDate": "2015-02-17T14:34:16Z", "PMID": "", "PMCID": "", "ISSN": "1436-3798, 1436-378X", "archive": "", "archiveLocation": "", "shortTitle": "A floodplain restoration project on the River Rhône (France)", "language": "en", "libraryCatalog": "CrossRef", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2015-02-17T14:34:16Z", "dateModified": "2015-02-17T14:34:16Z" } }, { "key": "RWCNZF5V", "version": 3585, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/RWCNZF5V", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/RWCNZF5V", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Stockhecke et al.", "parsedDate": "2014", "numChildren": 0 }, "data": { "key": "RWCNZF5V", "version": 3585, "itemType": "journalArticle", "title": "Chronostratigraphy of the 600,000 year old continental record of Lake Van (Turkey)", "creators": [ { "creatorType": "author", "firstName": "Mona", "lastName": "Stockhecke" }, { "creatorType": "author", "firstName": "Ola", "lastName": "Kwiecien" }, { "creatorType": "author", "firstName": "Luigi", "lastName": "Vigliotti" }, { "creatorType": "author", "firstName": "Flavio S.", "lastName": "Anselmetti" }, { "creatorType": "author", "firstName": "Jürg", "lastName": "Beer" }, { "creatorType": "author", "firstName": "M. Namik", "lastName": "Çağatay" }, { "creatorType": "author", "firstName": "James E.T.", "lastName": "Channell" }, { "creatorType": "author", "firstName": "Rolf", "lastName": "Kipfer" }, { "creatorType": "author", "firstName": "Johannes", "lastName": "Lachner" }, { "creatorType": "author", "firstName": "Thomas", "lastName": "Litt" }, { "creatorType": "author", "firstName": "Nadine", "lastName": "Pickarski" }, { "creatorType": "author", "firstName": "Michael", "lastName": "Sturm" } ], "abstractNote": "", "publicationTitle": "Quaternary Science Reviews", "publisher": "", "place": "", "date": "11/2014", "volume": "104", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "8-17", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1016/j.quascirev.2014.04.008", "citationKey": "", "url": "http://linkinghub.elsevier.com/retrieve/pii/S0277379114001243", "accessDate": "2014-12-11T09:22:30Z", "PMID": "", "PMCID": "", "ISSN": "02773791", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "CrossRef", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-11T09:22:30Z", "dateModified": "2014-12-11T09:22:30Z" } }, { "key": "PSIKKSBW", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/PSIKKSBW", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/PSIKKSBW", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Valette et al.", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "PSIKKSBW", "version": 3584, "itemType": "journalArticle", "title": "Construction géohistorique du « sauvage » de la Garonne toulousaine : quelle part de naturalité dans les paysages fluviaux ? (3ème partie)", "creators": [ { "creatorType": "author", "firstName": "Philippe", "lastName": "Valette" }, { "creatorType": "author", "firstName": "Jean-Michel", "lastName": "Carozza" }, { "creatorType": "author", "firstName": "Denis", "lastName": "Salles" }, { "creatorType": "author", "firstName": "Mélodie", "lastName": "David" }, { "creatorType": "author", "firstName": "Guillaume", "lastName": "Simonet" } ], "abstractNote": "La Garonne toulousaine (entre Toulouse et la confluence du Tarn) est composée de nombreuses annexes fluviales : bras-morts, zones humides et ripisylves. Ici, différents dispositifs de protection labellisent une dimension « sauvage » pour le fleuve, favorisant son maintien et sa conservation sans réellement s'interroger sur leur état d’origine. Face à ce constat, comment considérer la part de naturalité des paysages fluviaux de la Garonne toulousaine aujourd’hui ? Au dire des gestionnaires, la Garonne possède une image forte de fleuve « sauvage » alors que l’héritage géohistorique montre plutôt une Garonne impactée par les activités humaines. Ce travail interroge le sens du décalage entre cette réalité géohistorique et l’image véhiculée par les représentations contemporaines du fleuve.", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10629", "accessDate": "2014-12-09T13:19:34Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "Construction géohistorique du « sauvage » de la Garonne toulousaine", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [ { "tag": "Garonne", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "impacts anthropiques", "type": 1 }, { "tag": "naturalité", "type": 1 }, { "tag": "préservation", "type": 1 }, { "tag": "restauration", "type": 1 }, { "tag": "sauvage", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:19:34Z", "dateModified": "2014-12-09T13:19:34Z" } }, { "key": "P86CDS5M", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/P86CDS5M", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/P86CDS5M", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Valette et al.", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "P86CDS5M", "version": 3584, "itemType": "journalArticle", "title": "Construction géohistorique du « sauvage » de la Garonne toulousaine : quelle part de naturalité dans les paysages fluviaux ? (1ère partie)", "creators": [ { "creatorType": "author", "firstName": "Philippe", "lastName": "Valette" }, { "creatorType": "author", "firstName": "Jean-Michel", "lastName": "Carozza" }, { "creatorType": "author", "firstName": "Denis", "lastName": "Salles" }, { "creatorType": "author", "firstName": "Mélodie", "lastName": "David" }, { "creatorType": "author", "firstName": "Guillaume", "lastName": "Simonet" } ], "abstractNote": "La Garonne toulousaine (entre Toulouse et la confluence du Tarn) est composée de nombreuses annexes fluviales : bras-morts, zones humides et ripisylves. Ici, différents dispositifs de protection labellisent une dimension « sauvage » pour le fleuve, favorisant son maintien et sa conservation sans réellement s'interroger sur leur état d’origine. Face à ce constat, comment considérer la part de naturalité des paysages fluviaux de la Garonne toulousaine aujourd’hui ? Au dire des gestionnaires, la Garonne possède une image forte de fleuve « sauvage » alors que l’héritage géohistorique montre plutôt une Garonne impactée par les activités humaines. Ce travail interroge le sens du décalage entre cette réalité géohistorique et l’image véhiculée par les représentations contemporaines du fleuve.", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10578", "accessDate": "2014-12-09T13:19:34Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "Construction géohistorique du « sauvage » de la Garonne toulousaine", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [ { "tag": "Garonne", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "impacts anthropiques", "type": 1 }, { "tag": "naturalité", "type": 1 }, { "tag": "préservation", "type": 1 }, { "tag": "restauration", "type": 1 }, { "tag": "sauvage", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:19:34Z", "dateModified": "2014-12-09T13:19:34Z" } }, { "key": "CIG28WTS", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/CIG28WTS", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/CIG28WTS", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Ballut and Michelin", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "CIG28WTS", "version": 3584, "itemType": "journalArticle", "title": "Des zones humides pas si sauvages que cela : apport des données historiques et paléo-environnementales à la réflexion sur la gestion des paysages de la chaîne des Puys (France)", "creators": [ { "creatorType": "author", "firstName": "Christèle", "lastName": "Ballut" }, { "creatorType": "author", "firstName": "Yves", "lastName": "Michelin" } ], "abstractNote": "La chaine des Puys compte un grand nombre de zones humides issues de l’activité volcanique (maars ou lacs de barrage volcanique) dont l’aspect actuel fait passer beaucoup d’entre elles pour « sauvages » auprès des visiteurs car elles ne sont plus entretenues. Pourtant, elles traduisent, par le paysage qu’elles offrent, aussi bien l’histoire géomorphologique que l’histoire des sociétés car elles sont le produit d’une longue évolution. À l’heure où le Conseil général du Puy-de-Dôme présente un dossier de candidature en vue d’un classement au patrimoine mondial de l’UNESCO, cet article montre que reconstruire finement l’histoire de tels milieux peut aider les gestionnaires à penser leur politique de gestion non plus sous un angle conservatoire et strictement de protection mais dans une continuité avec la dynamique historique afin de mieux répondre à la fois aux exigences de l’UNESCO de préserver le site et aux demandes sociales locales de pouvoir maintenir voire développer leurs activités. De ce fait, le double caractère naturel et culturel de ces entités en fait un bon modèle pour intégrer dans le plan de gestion imposé par l’UNESCO des modalités qui concilient la Valeur universelle exceptionnelle (VUE) du site fondée sur des critères esthétiques et géologiques et la valeur écologique et culturelle qui découle de la succession d’aménagements et d’abandons qui les ont affectées.", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10586", "accessDate": "2014-12-09T13:19:34Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "Des zones humides pas si sauvages que cela", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [ { "tag": "chaîne des Puys", "type": 1 }, { "tag": "gestion adaptative", "type": 1 }, { "tag": "histoire des paysages", "type": 1 }, { "tag": "patrimoine mondial de l’UNESCO", "type": 1 }, { "tag": "zones humides", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:19:34Z", "dateModified": "2014-12-09T13:19:34Z" } }, { "key": "BQJ3BPFU", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/BQJ3BPFU", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/BQJ3BPFU", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Valette et al.", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "BQJ3BPFU", "version": 3584, "itemType": "journalArticle", "title": "Construction géohistorique du « sauvage » de la Garonne toulousaine : quelle part de naturalité dans les paysages fluviaux ? (2ème partie)", "creators": [ { "creatorType": "author", "firstName": "Philippe", "lastName": "Valette" }, { "creatorType": "author", "firstName": "Jean-Michel", "lastName": "Carozza" }, { "creatorType": "author", "firstName": "Denis", "lastName": "Salles" }, { "creatorType": "author", "firstName": "Mélodie", "lastName": "David" }, { "creatorType": "author", "firstName": "Guillaume", "lastName": "Simonet" } ], "abstractNote": "La Garonne toulousaine (entre Toulouse et la confluence du Tarn) est composée de nombreuses annexes fluviales : bras-morts, zones humides et ripisylves. Ici, différents dispositifs de protection labellisent une dimension « sauvage » pour le fleuve, favorisant son maintien et sa conservation sans réellement s'interroger sur leur état d’origine. Face à ce constat, comment considérer la part de naturalité des paysages fluviaux de la Garonne toulousaine aujourd’hui ? Au dire des gestionnaires, la Garonne possède une image forte de fleuve « sauvage » alors que l’héritage géohistorique montre plutôt une Garonne impactée par les activités humaines. Ce travail interroge le sens du décalage entre cette réalité géohistorique et l’image véhiculée par les représentations contemporaines du fleuve.", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10628", "accessDate": "2014-12-09T13:19:34Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "Construction géohistorique du « sauvage » de la Garonne toulousaine", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [ { "tag": "Garonne", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "impacts anthropiques", "type": 1 }, { "tag": "naturalité", "type": 1 }, { "tag": "préservation", "type": 1 }, { "tag": "restauration", "type": 1 }, { "tag": "sauvage", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:19:34Z", "dateModified": "2014-12-09T13:19:34Z" } }, { "key": "TETPUCNS", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/TETPUCNS", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/TETPUCNS", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Gramond", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "TETPUCNS", "version": 3584, "itemType": "journalArticle", "title": "Géohistoire environnementale : contours sémantiques et conceptuels. Discussions sur les héritages et patrimoines reconnus aux zones humides fluviales", "creators": [ { "creatorType": "author", "firstName": "Delphine", "lastName": "Gramond" } ], "abstractNote": "Les stratégies récentes de gestion des zones humides, visant à l’entretien voire à la reconquête de ces milieux, mettent l’accent sur les fonctions écosystémiques traduites en termes de services rendus d’une part, en soulignant de plus en plus fortement d’autre part les valeurs, notamment patrimoniales, que l’on peut leur reconnaître. Cette approche à coloration utilitariste pose la question des potentialités des milieux et nécessite de facto de retracer leur « trajectoires » entre dynamiques biophysiques et logiques anthropiques à temporalités et spatialités complexes et intriquées. Cet article propose une réflexion sur l’utilisation et l’efficacité des concepts et méthodes de la géohistoire pour identifier et valoriser la/les mémoire(s) des zones humides, ici en contexte fluvial.", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10585", "accessDate": "2014-12-09T13:19:34Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "Géohistoire environnementale", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [ { "tag": "approche sémantique", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "héritage", "type": 1 }, { "tag": "patrimoine", "type": 1 }, { "tag": "zones humides", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:19:34Z", "dateModified": "2014-12-09T13:19:34Z" } }, { "key": "KF827XVC", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/KF827XVC", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/KF827XVC", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Franchomme et al.", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "KF827XVC", "version": 3584, "itemType": "journalArticle", "title": "De l’approche géohistorique à l’élaboration de nouveaux outils de sensibilisation et de prévention du risque inondation", "creators": [ { "creatorType": "author", "firstName": "Magalie", "lastName": "Franchomme" }, { "creatorType": "author", "firstName": "Sylvie", "lastName": "Servain-Courant" }, { "creatorType": "author", "firstName": "Bertrand", "lastName": "Sajaloli" } ], "abstractNote": "Les risques et les milieux fluviaux, tant qu’objets de recherche, nous amènent à nous pencher sur les relations entre l’homme et son territoire au fil du temps. La dimension temporelle, longtemps négligée, a réémergé dans le traitement des questions environnementales à la fin des années 1980 (Beck et Delort (dir.), 1993), grâce notamment au concept de développement durable qui a permis l’apparition de nouvelles pratiques en matière de politiques d’aménagement du territoire. Celles-ci s’intére...", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10560", "accessDate": "2014-12-09T13:17:40Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [], "collections": [ "HBKPMAG2", "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:17:40Z", "dateModified": "2014-12-09T13:17:40Z" } }, { "key": "D9U5II9Q", "version": 3584, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/D9U5II9Q", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/D9U5II9Q", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Watteaux and Chouquer", "parsedDate": "2014-12-05", "numChildren": 0 }, "data": { "key": "D9U5II9Q", "version": 3584, "itemType": "journalArticle", "title": "L’inflation disciplinaire et conceptuelle dans les sciences paléoenvironnementales", "creators": [ { "creatorType": "author", "firstName": "Magali", "lastName": "Watteaux" }, { "creatorType": "author", "firstName": "Gérard", "lastName": "Chouquer" } ], "abstractNote": "À l’issue d’un travail historiographique et épistémologique sur les disciplines au carrefour de l’histoire, de l’archéologie, de la géographie et des sciences naturalistes, les auteurs ont proposé, dans un essai récemment paru, un inventaire raisonné de 152 intitulés scandant et diversifiant le domaine de recherche géohistorique. Ici, ils abordent plus spécifiquement la situation des sciences du paléoenvironnement où l’on observe également une profusion des appellations. Ce faisant, ils donnent une lecture critique du concept d’environnement, omniprésent dans les recherches. Enfin, ils soutiennent la thèse selon laquelle cette inflation disciplinaire témoigne de l’émergence d’un vaste champ de recherche : celui de la redécouverte du rapport à l’écoumène et de la complexité des héritages qui le composent.", "publicationTitle": "Développement durable et territoires. Économie, géographie, politique, droit, sociologie", "publisher": "", "place": "", "date": "2014/12/05", "volume": "", "issue": "vol. 5, n°3", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://developpementdurable.revues.org/10648", "accessDate": "2014-12-09T13:17:21Z", "PMID": "", "PMCID": "", "ISSN": "1772-9971", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "developpementdurable.revues.org", "callNumber": "", "rights": "© Développement durable et territoires", "extra": "", "tags": [ { "tag": "Nature", "type": 1 }, { "tag": "archéogéographie", "type": 1 }, { "tag": "disciplines", "type": 1 }, { "tag": "environnement", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "historiographie", "type": 1 }, { "tag": "sciences paléoenvironnementales", "type": 1 }, { "tag": "épistémologie", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-12-09T13:17:21Z", "dateModified": "2014-12-09T13:17:21Z" } }, { "key": "ZPP8FAXV", "version": 3512, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/ZPP8FAXV", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/ZPP8FAXV", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Viveen et al.", "numChildren": 0 }, "data": { "key": "ZPP8FAXV", "version": 3512, "itemType": "journalArticle", "title": "Paleofloods and ancient fishing weirs in NW Iberian rivers", "creators": [ { "creatorType": "author", "firstName": "Willem", "lastName": "Viveen" }, { "creatorType": "author", "firstName": "Jorge", "lastName": "Sanjurjo-Sanchez" }, { "creatorType": "author", "firstName": "Ana", "lastName": "Goy-Diz" }, { "creatorType": "author", "firstName": "Antonie", "lastName": "Veldkamp" }, { "creatorType": "author", "firstName": "Jeroen M.", "lastName": "Schoorl" } ], "abstractNote": "A 15-m-thick, fluvial sedimentary record of the NW Iberian lower Miño River was studied. Grain-size analyses were performed and twelve samples were dated using optically stimulated luminescence dating techniques, documenting a 1300-yr-old reconstructed fluvial record that does not match with known climate fluctuations in the area, but is linked instead to the construction of a series of ancient fishing weirs (pesqueiras). The sedimentation phases are in agreement with known episodes of increased population density, which suggests active use of the pesqueiras. A number of sedimentation hiatuses in the fluvial record point towards damage to the pesqueiras during large-scale flooding in the Miño River basin, and a sudden drop in population probably due to the arrival of the plague in the 13th century AD. The oldest sedimentation phases started just after 700 AD, and we infer that the first pesqueiras were constructed around this time. This timing coincides with the transition of the NW Iberian landscape towards a more intensively used agricultural landscape, as evidenced from other geo-archeological investigations. The results demonstrate that the pesqueiras are several hundreds of years older than known from historical records, but not so old as to date back to the Roman occupation.", "publicationTitle": "Quaternary Research", "publisher": "", "place": "", "date": "", "volume": "", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Quaternary Research", "DOI": "10.1016/j.yqres.2014.04.011", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0033589414000507", "accessDate": "2014-05-28T10:12:15Z", "PMID": "", "PMCID": "", "ISSN": "0033-5894", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Fish trap", "type": 1 }, { "tag": "Minho", "type": 1 }, { "tag": "Miño River", "type": 1 }, { "tag": "OSL dating", "type": 1 }, { "tag": "geoarcheology", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-05-28T10:12:15Z", "dateModified": "2014-05-28T10:12:15Z" } }, { "key": "WW9TWKJT", "version": 3504, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/WW9TWKJT", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/WW9TWKJT", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Forget", "parsedDate": "2015-12-15", "numChildren": 0 }, "data": { "key": "WW9TWKJT", "version": 3504, "itemType": "journalArticle", "title": "Le rôle des sources historiques dans la compréhension des dynamiques fluviales d’un grand fleuve de plaine. Le cas du Paraná argentin", "creators": [ { "creatorType": "author", "firstName": "Marie", "lastName": "Forget" } ], "abstractNote": "Le Paraná argentin, cinquième plus grand fleuve du monde par son débit et la taille de son bassin-versant, est aujourd’hui peu connu. Cela peut s’expliquer par le caractère récent de sa découverte et par l’histoire de son exploitation incomplète. Les relevés physiques qui y sont faits sont souvent lacunaires et couvrent une période de temps insuffisante pour comprendre les changements dans sa morphologie à l’échelle de son bassin-versant et sur le temps long. Nous avons été amenés à nous interroger sur les données capables de nous aider à retracer la dynamique fluviale de ce grand fleuve de plaine. Situé dans le Nouveau Monde, l’appropriation de ce territoire est récente et il reste encore des stigmates de sa colonisation. Le tracé du fleuve a changé et il est alors légitime de se demander si les cartes, dans leur diachronie, permettent d’identifier ce changement. Nos recherches en archives nous ont permis de rassembler 43 cartes illustrant une période multiséculaire du XVe s. jusqu’à 1904. Les échelles d’analyse sont également variées : de l’échelle régionale (1/100 000) jusqu’à l’échelle continentale (1/18 500 000). La méthode utilisée est celle de la comparaison carte à carte dans laquelle les bancs de sable et la forme en plan du fleuve sont considérés comme des marqueurs de la dynamique fluviale. Les premières cartes (XVe s.) nous montrent un tracé en tresses sur le haut Paraná et un cours du Paraguay libre de tout dépôt. La dynamique actuelle indique un fonctionnement inverse. En partant des résultats obtenus, ce travail recherche les facteurs explicatifs liés aux phénomènes territoriaux et climatiques. Les mécanismes de défrichement dans les territoires des Misiones et leur abandon progressif après l’expulsion des Jésuites permettent de poser l’hypothèse d’un basculement dans l’origine de la charge sédimentaire.", "publicationTitle": "Géomorphologie : relief, processus, environnement", "publisher": "", "place": "", "date": "2015/12/15", "volume": "", "issue": "4/2013", "section": "", "partNumber": "", "partTitle": "", "pages": "445-462", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://geomorphologie.revues.org/10399", "accessDate": "2014-05-08T08:28:57Z", "PMID": "", "PMCID": "", "ISSN": "1266-5304", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "geomorphologie.revues.org", "callNumber": "", "rights": "© Groupe français de géomorphologie", "extra": "", "tags": [ { "tag": "Paraná", "type": 1 }, { "tag": "cartes anciennes", "type": 1 }, { "tag": "charge sédimentaire", "type": 1 }, { "tag": "géohistoire", "type": 1 }, { "tag": "géomorphologie", "type": 1 }, { "tag": "système fluvial", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-05-08T08:28:57Z", "dateModified": "2014-05-08T08:28:57Z" } }, { "key": "HCMUU38I", "version": 3476, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/HCMUU38I", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/HCMUU38I", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Scapozza and Oppizzi", "parsedDate": "2013-11-10", "numChildren": 0 }, "data": { "key": "HCMUU38I", "version": 3476, "itemType": "journalArticle", "title": "Évolution morpho-sédimentaire et paléo-environnementale de la plaine fluvio-deltaïque du Ticino pendant l’Holocène récent (Canton du Tessin, Suisse)", "creators": [ { "creatorType": "author", "firstName": "Cristian", "lastName": "Scapozza" }, { "creatorType": "author", "firstName": "Paolo", "lastName": "Oppizzi" } ], "abstractNote": "L’évolution pendant l’Holocène récent du delta du Ticino dans le Lac Majeur a été étudiée à l’aide de plusieurs sondages réalisés dans les Bolle di Magadino, de l’analyse de documents historiques et de la comparaison avec la stratigraphie pollinique déterminée dans deux petits lacs du Sud des Alpes suisses. Ces données ont permis de déterminer les principales étapes de la progradation du delta du Ticino de l’Époque romaine à aujourd’hui ainsi que l’évolution du style fluvial et de la dynamique morphosédimentaire du Ticino dans le Piano di Magadino. En particulier, grâce à une analyse des taux de sédimentation, il a été possible de mettre en évidence une intensification de l’activité hydrosédimentaire entre l’Epoque romaine et l’Antiquité tardive/Haut Moyen Âge, suivie par une période moins active pendant le Moyen Âge Central et le Bas Moyen Âge, caractérisée par un style fluvial à méandres. Le passage du Bas Moyen Âge à l’Époque Moderne a été caractérisé par l’inondation catastrophique de 1515, nommée « Buzza di Biasca », qui, en s’additionnant à l’évolution climatique naturelle, a engendré une métamorphose fluviale du Ticino, évoluant vers un style fluvial tressé qui s’est maintenu jusqu’à sa correction dans la deuxième moitié du XIXe siècle.", "publicationTitle": "Géomorphologie : relief, processus, environnement", "publisher": "", "place": "", "date": "2013/11/10", "volume": "", "issue": "3/2013", "section": "", "partNumber": "", "partTitle": "", "pages": "265-286", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "http://geomorphologie.revues.org/10289", "accessDate": "2014-02-14T11:06:01Z", "PMID": "", "PMCID": "", "ISSN": "1266-5304", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "geomorphologie.revues.org", "callNumber": "", "rights": "© Groupe français de géomorphologie", "extra": "", "tags": [ { "tag": "Bolle di Magadino", "type": 1 }, { "tag": "Suisse", "type": 1 }, { "tag": "Ticino", "type": 1 }, { "tag": "métamorphose fluviale", "type": 1 }, { "tag": "plaine alluviale", "type": 1 }, { "tag": "progradation du delta", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2014-02-14T11:06:01Z", "dateModified": "2014-02-14T11:06:01Z" } }, { "key": "6VD5REHI", "version": 3460, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/6VD5REHI", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/6VD5REHI", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Sternai et al.", "parsedDate": "2013", "numChildren": 0 }, "data": { "key": "6VD5REHI", "version": 3460, "itemType": "journalArticle", "title": "Spatial and temporal variations of glacial erosion in the Rhône valley (Swiss Alps): Insights from numerical modeling", "creators": [ { "creatorType": "author", "firstName": "Pietro", "lastName": "Sternai" }, { "creatorType": "author", "firstName": "Frédéric", "lastName": "Herman" }, { "creatorType": "author", "firstName": "Pierre G.", "lastName": "Valla" }, { "creatorType": "author", "firstName": "Jean-Daniel", "lastName": "Champagnac" } ], "abstractNote": "", "publicationTitle": "Earth and Planetary Science Letters", "publisher": "", "place": "", "date": "4/2013", "volume": "368", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "119-131", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1016/j.epsl.2013.02.039", "citationKey": "", "url": "http://hal-sde.archives-ouvertes.fr/insu-00853433", "accessDate": "2013-12-18T14:52:44Z", "PMID": "", "PMCID": "", "ISSN": "0012821X", "archive": "", "archiveLocation": "", "shortTitle": "Spatial and temporal variations of glacial erosion in the Rhône valley (Swiss Alps)", "language": "", "libraryCatalog": "CrossRef", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2013-12-18T14:52:44Z", "dateModified": "2013-12-18T14:52:44Z" } }, { "key": "M42WW37J", "version": 3451, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/M42WW37J", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/M42WW37J", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Słowik", "parsedDate": "2013", "numChildren": 0 }, "data": { "key": "M42WW37J", "version": 3451, "itemType": "journalArticle", "title": "Holocene evolution of meander bends in lowland river valley formed in complex geological conditions (the Obra River, Poland)", "creators": [ { "creatorType": "author", "firstName": "Marcin", "lastName": "Słowik" } ], "abstractNote": "Ground-penetrating radar surveys, coring and the analyses of satellite and aerial images have been carried out to study differences in the evolution of meander bends formed in various geological conditions. The research was conducted in the lower course of the Obra River (western Poland) characterized by a complex geology: particular sections of the valley were formed in glacial, stagnant water and fluvioglacial deposits. The research was conducted in four detailed study sites representing different formation conditions for the meander bends. Four types of meanders were distinguished: laterally migrating bends characterized by frequent changes of migration direction accompanied by river bed avulsions and cutoffs; bends with traces of continuous migration limited by stagnant water basin deposits; confined meanders in a narrow valley formed in glacial till characterized by the occurrence of mid-channel islands; and meanders with traces of complex changes of the river bed migration influenced by anthropogenic intervention followed by intensive overbank deposition. Moreover, traces of an early development of the Obra valley and remains of multi-channel pattern were discovered. The results also show that despite being formed in different geological conditions, a similar number of the meander migration phases were recorded in the floodplain architecture during the last 7000 years at each of the sites. It is also found that the development of the studied meanders was slow compared with cases of actively migrating meandering rivers.", "publicationTitle": "Geografiska Annaler: Series A, Physical Geography", "publisher": "", "place": "", "date": "2013", "volume": "", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "n/a–n/a", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1111/geoa.12029", "citationKey": "", "url": "http://onlinelibrary.wiley.com/doi/10.1111/geoa.12029/abstract", "accessDate": "2013-12-02T16:08:04Z", "PMID": "", "PMCID": "", "ISSN": "1468-0459", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "© 2013 Swedish Society for Anthropology and Geography", "extra": "", "tags": [ { "tag": "Holocene", "type": 1 }, { "tag": "ground-penetrating radar", "type": 1 }, { "tag": "meander bends", "type": 1 }, { "tag": "river bed migration", "type": 1 }, { "tag": "river channel changes", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2013-12-02T16:08:04Z", "dateModified": "2013-12-02T16:08:04Z" } }, { "key": "X64DQZ63", "version": 3448, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/X64DQZ63", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/X64DQZ63", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Förster et al.", "parsedDate": "2013-10-29", "numChildren": 0 }, "data": { "key": "X64DQZ63", "version": 3448, "itemType": "journalArticle", "title": "Towards mutual understanding within interdisciplinary palaeoenvironmental research: An exemplary analysis of the term landscape", "creators": [ { "creatorType": "author", "firstName": "Frank", "lastName": "Förster" }, { "creatorType": "author", "firstName": "Ralph", "lastName": "Großmann" }, { "creatorType": "author", "firstName": "Martin", "lastName": "Hinz" }, { "creatorType": "author", "firstName": "Karina", "lastName": "Iwe" }, { "creatorType": "author", "firstName": "Hanno", "lastName": "Kinkel" }, { "creatorType": "author", "firstName": "Annegret", "lastName": "Larsen" }, { "creatorType": "author", "firstName": "Uta", "lastName": "Lungershausen" }, { "creatorType": "author", "firstName": "Chiara", "lastName": "Matarese" }, { "creatorType": "author", "firstName": "Philipp", "lastName": "Meurer" }, { "creatorType": "author", "firstName": "Oliver", "lastName": "Nelle" }, { "creatorType": "author", "firstName": "Vincent", "lastName": "Robin" }, { "creatorType": "author", "firstName": "Michael", "lastName": "Teichmann" } ], "abstractNote": "Abstract\nThe term landscape is a crucial term for a diversity of scientific disciplines researching the Quaternary, each of which maintains different concepts and definitions. With increasing interdisciplinary research cooperation between disparate disciplines, a basis for communication has to be established. The aim of this paper is a) to survey an assortment of concepts and understandings of landscape within diverse disciplinary contexts and b) to explore the possibilities and usefulness of a common concept in an interdisciplinary palaeo-environmental research field, shared by scholars from the humanities and natural sciences alike. This comprises the disciplines art history, prehistoric archaeology, classical archaeology, ecology, geography, geology, and history. As a result, it can be stated that landscape is a cultural term: Landscapes are a cultural construct, and any landscape is the result of contemporary vision which is culturally influenced by the current context. Thus, landscapes are always shaped through today's construction of landscapes, independent from the discipline, and equally if in or for modern, or prehistoric times, and equally, if with or without humans.", "publicationTitle": "Quaternary International", "publisher": "", "place": "", "date": "octobre 29, 2013", "volume": "312", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "4-11", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Quaternary International", "DOI": "10.1016/j.quaint.2013.07.045", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S1040618213004448", "accessDate": "2013-11-18T13:46:02Z", "PMID": "", "PMCID": "", "ISSN": "1040-6182", "archive": "", "archiveLocation": "", "shortTitle": "Towards mutual understanding within interdisciplinary palaeoenvironmental research", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "362FN9GJ", "WN9F88J4" ], "relations": {}, "dateAdded": "2013-11-18T13:46:02Z", "dateModified": "2013-11-18T13:46:02Z" } }, { "key": "HJA7BP8G", "version": 3434, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/HJA7BP8G", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/HJA7BP8G", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Denis et al.", "parsedDate": "2013-07-01", "numChildren": 0 }, "data": { "key": "HJA7BP8G", "version": 3434, "itemType": "journalArticle", "title": "Reconstitution de la dynamique d’une rivière ardennaise (La Lienne) depuis le Tardiglaciaire grâce à l’analyse géomorphologique et chronostratigraphique d’une tourbière de fond de vallée", "creators": [ { "creatorType": "author", "firstName": "Anne-Cécile", "lastName": "Denis" }, { "creatorType": "author", "firstName": "Cécile", "lastName": "Wastiaux" }, { "creatorType": "author", "firstName": "François", "lastName": "Petit" }, { "creatorType": "author", "firstName": "Louis", "lastName": "Leclercq" }, { "creatorType": "author", "firstName": "Étienne", "lastName": "Juvigné" }, { "creatorType": "author", "firstName": "Jean Van", "lastName": "Campenhout" }, { "creatorType": "author", "firstName": "Geoffrey", "lastName": "Houbrechts" } ], "abstractNote": "La dynamique géomorphologique (incision, mobilité latérale, taux de sédimentation) d’une rivière ardennaise (la Lienne) a été étudiée au niveau d’un secteur de tourbière de fond de vallée. Ce type de site présente un intérêt majeur car la morphologie des dépôts fluviatiles anciens est préservée en dessous des dépôts tourbeux et l’utilisation des pollens conservés dans la tourbe permet de dater les différentes phases d’évolution de la rivière. La présence de pollens du Dryas récent par-dessus une nappe de cailloutis perchée 1,4 m au-dessus du lit actuel ainsi que de dépôts tourbeux datés du Préboréal au niveau du lit actuel indiquent qu’une phase d’incision s’est produite à la transition Dryas récent-Préboréal. Le téphra du Laacher See a été retrouvé à l’état remanié au contact de la nappe de cailloutis perchée, ce qui confirme qu’elle a été mise en place au Dryas récent, en contexte périglaciaire. La Lienne présentait vraisemblablement des chenaux multiples au Préboréal, puis l’abandon d’un des chenaux, elle s’est déplacée latéralement, ce qui a permis à la tourbière de s’étendre jusqu’à occuper plus des deux tiers du fond de vallée dès l’Atlantique. L’utilisation des scories sidérurgiques comme marqueur stratigraphique montre une faible mobilité latérale de la Lienne ainsi qu’un faible taux d’aggradation de la plaine alluviale au cours des derniers siècles.", "publicationTitle": "Géomorphologie : relief, processus, environnement", "publisher": "", "place": "", "date": "2013/07/01", "volume": "", "issue": "2/2013", "section": "", "partNumber": "", "partTitle": "", "pages": "133-152", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.4000/geomorphologie.10187", "citationKey": "", "url": "http://geomorphologie.revues.org/10187", "accessDate": "2013-10-07T13:09:40Z", "PMID": "", "PMCID": "", "ISSN": "1266-5304", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "fr", "libraryCatalog": "geomorphologie.revues.org", "callNumber": "", "rights": "© Groupe français de géomorphologie", "extra": "", "tags": [ { "tag": "Ardenne", "type": 1 }, { "tag": "Holocène", "type": 1 }, { "tag": "Téphra", "type": 1 }, { "tag": "plaine alluviale", "type": 1 }, { "tag": "pollens", "type": 1 }, { "tag": "rivière à charge caillouteuse", "type": 1 }, { "tag": "scories", "type": 1 }, { "tag": "systèmes fluviaux", "type": 1 }, { "tag": "tourbière", "type": 1 } ], "collections": [ "WN9F88J4" ], "relations": {}, "dateAdded": "2013-10-07T13:09:40Z", "dateModified": "2013-10-07T13:09:40Z" } }, { "key": "PMHT79PC", "version": 3432, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/PMHT79PC", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/PMHT79PC", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Thiry et al.", "parsedDate": "2013-09-01", "numChildren": 0 }, "data": { "key": "PMHT79PC", "version": 3432, "itemType": "journalArticle", "title": "Periglacial morphogenesis in the Paris basin: insight from geophysical survey and consequences for the fate of soil pollution", "creators": [ { "creatorType": "author", "firstName": "Médard", "lastName": "Thiry" }, { "creatorType": "author", "firstName": "Folkert", "lastName": "van Oort" }, { "creatorType": "author", "firstName": "Julien", "lastName": "Thiesson" }, { "creatorType": "author", "firstName": "Brigitte", "lastName": "Van Vliet-Lanoe" } ], "abstractNote": "Abstract\nGeophysical survey by Automatic Resistivity Profiling (ARP©) system of the Pierrelaye–Bessancourt area revealed remarkable conductive polygon patterns of 20- to 30-m diameter detected between 0.5- and 1.7-m depth. Trenches dug down to the limestone substrate allowed detailing of the pedological and lithological units that compose such polygonal features. The patterns are formed by greenish glauconite and carbonated sand hollows where clay-rich pedological horizons bend downward, forming narrow tongs extending up to 2- to 3-m depth. Such structures were interpreted as a buried polygonal ice-wedge network (thermokarst depressions). Geometrical relationships between the lithological units and consecutive erosional surfaces allowed the identification of successive landscape events and a landscape chronology. The sequence started during the Saalian glaciation with (1) the development of patterned grounds by thermokarstic cryoturbation; (2) the consecutive deflation/erosion during post-permafrost aridity; (3) the loess and eolian sand deposits; (4) the weathering of the former deposits with development of pedogenic horizons during the Eemian interglacial; (5) the recurrent cryoturbation and thermal cracking leading to infolding of the pedogenic horizons during the Pleniglacial optimum (Weichselian); and finally (5) the erosion that levelled the periglacial microreliefs, most probably during the last glacial stage (Weichselian), leading to the modern landscape. In this agricultural area, urban waste water has been spread for more than 100 years by flooding irrigation for food crop production and has led to high levels of metal pollution in the surface horizons of the soils. The polygonal cryogenic structures have major impacts on soil hydrology and dispersion/distribution of heavy metals toward the geological substrate. Such structures are essential to consider when conceiving proposals for future soil management of this polluted area.", "publicationTitle": "Geomorphology", "publisher": "", "place": "", "date": "septembre 1, 2013", "volume": "197", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "34-44", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Geomorphology", "DOI": "10.1016/j.geomorph.2013.04.027", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0169555X13002432", "accessDate": "2013-10-07T11:56:40Z", "PMID": "", "PMCID": "", "ISSN": "0169-555X", "archive": "", "archiveLocation": "", "shortTitle": "Periglacial morphogenesis in the Paris basin", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Cryoturbation", "type": 1 }, { "tag": "Electrical mapping", "type": 1 }, { "tag": "Geophysical method", "type": 1 }, { "tag": "Periglacial", "type": 1 }, { "tag": "pollution", "type": 1 }, { "tag": "soils", "type": 1 } ], "collections": [ "NTF93FJ4", "UN94AR8C", "WN9F88J4" ], "relations": {}, "dateAdded": "2013-10-07T11:56:40Z", "dateModified": "2013-10-07T11:56:40Z" } } ]