{"id":2278,"date":"2021-07-30T18:25:38","date_gmt":"2021-07-30T18:25:38","guid":{"rendered":"http:\/\/www.sedimentologia.org.ar\/spa\/?p=2278"},"modified":"2021-07-30T18:59:47","modified_gmt":"2021-07-30T18:59:47","slug":"vii-ras-y-viii-cls-nueva-sesion-especial-se1","status":"publish","type":"post","link":"https:\/\/www.sedimentologia.org.ar\/spa\/vii-ras-y-viii-cls-nueva-sesion-especial-se1\/","title":{"rendered":"XVII RAS y VIII CLS: Nueva Sesi\u00f3n Especial SE1"},"content":{"rendered":"<p><span class=\"fontstyle0\" style=\"color: #785a46\"><strong> Sesi\u00f3n Especial SE1: ROL DE LA SEDIMENTOLOG\u00cdA EN LA INVESTIGACI\u00d3N DE CAMBIOS CLIM\u00c1TICOS Y RECONSTRUCCIONES <\/strong><strong>PALEOAMBIENTALES CUATERNARIAS<\/strong> <\/span><\/p>\n<p><span class=\"fontstyle2\" style=\"color: #785a46\">Coordinadores: Stella Moreiras (Argentina), Tania Villase\u00f1or (Chile) &amp; Fabiano Pupim (Brasil)<\/span><\/p>\n<p><span class=\"fontstyle3\">La sedimentolog\u00eda como rama esencial de la geolog\u00eda ha permitido avanzar en el conocimiento de los grandes cambios clim\u00e1ticos y ambientales que han acontecido tanto a nivel global como regional y local. El an\u00e1lisis de diferentes dep\u00f3sitos en los valles monta\u00f1osos, as\u00ed como los estudios en terrazas fluviales, niveles aluviales, lagos, paleosuelos, loess, dunas, turberas, humedales, fiordos y oc\u00e9anos han permitido vincular al registro sedimentario con diferentes eventos clim\u00e1ticos. Esta herramienta fundamental junto a diferentes cronolog\u00edas y proxies han acotado los periodos fr\u00edos y c\u00e1lidos, as\u00ed como los h\u00famedos y secos permitiendo la reconstrucci\u00f3n paleoambiental de diferentes zonas del planeta.<\/span><\/p>\n<p><span class=\"fontstyle3\">La actual crisis clim\u00e1tica y la creciente aceptaci\u00f3n del Antropoceno como una \u00e9poca de r\u00e1pidos cambios en la superficie de la Tierra destacan la importancia de la Sedimentolog\u00eda como una disciplina integradora que permite reconstruir y entender din\u00e1micas ambientales y su evoluci\u00f3n a diferentes escalas de tiempo y espacio bajo diferentes fuerzas, tanto end\u00f3genos como ex\u00f3genos. La comunidad que estudia el registro sedimentario es llamada a contribuir mediante proxies sedimentol\u00f3gicos a extender las series de tiempo del registro instrumental, as\u00ed como aportar a la comprensi\u00f3n de procesos superficiales pasados y modernos. En este contexto, la integraci\u00f3n de datos sedimentol\u00f3gicos con la informaci\u00f3n aportada por otras disciplinas intenta dimensionar la magnitud de diferentes peligros naturales.<\/span><\/p>\n<p><span class=\"fontstyle3\">Esta sesi\u00f3n especial busca reunir trabajos internacionales donde la sedimentolog\u00eda haya jugado un rol trascendente en identificar cambios clim\u00e1ticos en el Cuaternario, as\u00ed como reconstrucciones paleoambientales inferidas junto a estudios limnol\u00f3gicos, hidrol\u00f3gicos, palinol\u00f3gicos y cronoestratigr\u00e1ficos, entre otros. El objetivo principal es integrar a la comunidad cient\u00edfica dedicada a la reconstrucci\u00f3n de cambios ambientales a partir del registro sedimentario.<\/span><\/p>\n<p><strong><span class=\"fontstyle2\">Plazo para env\u00edo de res\u00famenes de 1 p\u00e1g.: 20 de agosto del 2021 <\/span><\/strong><span class=\"fontstyle3\">(adaptados a las normas publicadas en las circulares del evento).<\/span><\/p>\n<p><span class=\"fontstyle3\">Contacto: <\/span><span class=\"fontstyle3\">moreiras@mendoza-conicet.gob.ar<\/span><span class=\"fontstyle3\">, <\/span><span class=\"fontstyle3\">tania.villasenor@uoh.cl<\/span><span class=\"fontstyle3\">, <\/span><span class=\"fontstyle3\">f.pupim@unifesp.br<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span class=\"fontstyle0\" style=\"color: #785a00\"><strong>Special Session SE1: THE ROLE OF SEDIMENTOLOGY IN THE RESEARCH OF QUATERNARY CLIMATE CHANGE AND PALEOENVIRONMENT RECONSTRUCTIONS<\/strong> <\/span><\/p>\n<p><span class=\"fontstyle2\"><span style=\"color: #785a00\">CONVENERS: Stella Moreiras (Argentina), Tania Villase\u00f1or (Chile) &amp; Fabiano Pupim (Brasil)<\/span> <\/span><\/p>\n<p><span class=\"fontstyle3\">Sedimentology as an essential branch of geology has allowed us to advance in the knowledge of the major climatic and environmental changes occurred at a global, regional and local scale. The analysis of different deposits in mountain valleys, as well as studies of river terraces, alluvial levels, lakes, paleosoils, loess, dunes, peat bogs, wetlands, fjords and oceans have made possible to link the sedimentary record to different climatic events. This fundamental tool, together with different chronologies and proxies, has delimited cold and warm periods, and wet versus dry periods, allowing the\u00a0 palaeoenvironmental reconstruction in different regions of the planet.<\/span><\/p>\n<p><span class=\"fontstyle3\">The current climate crisis and the growing acceptance of the anthropocene as a period of rapid changes on Earth&#8217;s surface highlights the importance of sedimentology as an integrative discipline that allows the reconstruction and understanding of environmental dynamics and evolution at different time scales and space under different endogenous and exogenous forces. The sedimentology community is called upon to contribute through sedimentological proxies to extend the time series of the instrumental record, as well as to contribute to the understanding of past and modern surface processes. In this context, the integration of sedimentological data with information from other disciplines attempts to dimension the magnitude of different natural hazards.<\/span><\/p>\n<p><span class=\"fontstyle3\">This special session aims to gather international research in which sedimentology has played an important role in identifying climatic changes during the Quaternary, as well as inferred palaeoenvironmental reconstructions together with limnological, hydrological, palynological and chronostratigraphical studies, among others. The main objective is to integrate the scientific community dedicated to<br \/>\nthe reconstruction of environmental changes from the sedimentary record.<\/span><\/p>\n<p><strong><span class=\"fontstyle2\">Deadline for submission of 1-page abstracts: 20th August 2021 <\/span><\/strong><span class=\"fontstyle3\">(following the published author guide -4<\/span><span class=\"fontstyle3\">TH <\/span><span class=\"fontstyle3\">Circular-).<\/span><\/p>\n<p><span class=\"fontstyle3\">Contact<\/span><span class=\"fontstyle3\">: <\/span><span class=\"fontstyle3\">moreiras@mendoza-conicet.gob.ar, tania.villasenor@uoh.cl, f.pupim@unifesp.br<\/span><\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Sesi\u00f3n Especial SE1: ROL DE LA SEDIMENTOLOG\u00cdA EN LA INVESTIGACI\u00d3N DE CAMBIOS CLIM\u00c1TICOS Y RECONSTRUCCIONES PALEOAMBIENTALES CUATERNARIAS Coordinadores: Stella Moreiras (Argentina), Tania Villase\u00f1or (Chile) &amp; Fabiano Pupim (Brasil) La sedimentolog\u00eda como rama esencial de la geolog\u00eda ha permitido avanzar en el conocimiento de los grandes cambios clim\u00e1ticos y ambientales que han acontecido tanto a nivel [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":1948,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5,17],"tags":[],"class_list":["post-2278","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-noticias","category-xvii-ras"],"_links":{"self":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/posts\/2278","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/comments?post=2278"}],"version-history":[{"count":6,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/posts\/2278\/revisions"}],"predecessor-version":[{"id":2287,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/posts\/2278\/revisions\/2287"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/media\/1948"}],"wp:attachment":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/media?parent=2278"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/categories?post=2278"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/tags?post=2278"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}