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<dc:title xml:lang="fr">Impacts of global climate changes on continental environments : case study of the eocene-oligocene transition in the upper Rhine graben</dc:title>
<dcterms:alternative xml:lang="en">Impact des changements climatiques globaux sur les environnements continentaux : étude de cas de la transition eocène-oligocène dans le fossé Rhénan</dcterms:alternative>
<dc:subject xml:lang="fr">Transition Éocène-Oligocène</dc:subject>
<dc:subject xml:lang="fr">Dérèglement climatique</dc:subject>
<dc:subject xml:lang="fr">Fossé Rhénan</dc:subject>
<dc:subject xml:lang="fr">Paléoclimats</dc:subject>
<dc:subject xml:lang="fr">Paléoenvironnements</dc:subject>
<dc:subject xml:lang="fr">Sédimentologie</dc:subject>
<dc:subject xml:lang="fr">Cyclostratigraphie</dc:subject>
<dc:subject xml:lang="fr">Bassin de Mulhouse</dc:subject>
<dc:subject xml:lang="en">Eocene-oligocene transition</dc:subject>
<dc:subject xml:lang="en">Climate change</dc:subject>
<dc:subject xml:lang="en">Upper Rhine graben</dc:subject>
<dc:subject xml:lang="en">Paleoclimates</dc:subject>
<dc:subject xml:lang="en">Paleoenvironments</dc:subject>
<dc:subject xml:lang="en">Sedimentology</dc:subject>
<dc:subject xml:lang="en">Cyclostratigraphy</dc:subject>
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<tef:elementdEntree autoriteExterne="027568490" autoriteSource="Sudoc">Changements climatiques</tef:elementdEntree>
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<tef:elementdEntree autoriteExterne="027302407" autoriteSource="Sudoc">Paléoclimatologie</tef:elementdEntree>
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<dcterms:abstract xml:lang="fr">Comprendre l’impact des perturbations climatiques passées sur les environnements continentaux est crucial pour mieux anticiper le futur de notre Terre. Cette thèse contribue à l’effort collectif des études concernant la Transition Éocène-Oligocène (TEO) au prisme des environnements continentaux du Fossé Rhénan (FR). C’est une période de ~790 ka qui correspond à la transition de conditions « greenhouse » à « icehouse ». La chronostratigraphie du FR a été améliorée et les changements à travers la TEO documentés. Ces changements sont un refroidissement, une aridification, un contraste climatique saisonnier accru, et une plus grande sensibilité du climat aux variations orbitales. Dans le bassin de Mulhouse, la transition de pélites sans structures à des sédiments laminés et varves, ainsi que l’apparition de cycles sédimentaires forcés par les variations orbitales, sont les marqueurs de ces deux derniers changements. Des investigations géochimiques et palynologiques menées dans le bassin de Pechelbronn suggèrent l’occurrence d’une transgression marine proche de la base de la « Zone Fossilifère ».</dcterms:abstract>
<dcterms:abstract xml:lang="en">Understanding the impact of past climatic perturbations on continental environments is crucial to better assess and anticipate the future of our Earth. This thesis contributes to the collective effort of paleoclimate studies regarding the Eocene-Oligocene Transition (EOT) through the prism of the continental environments of the Upper Rhine Graben (URG). The EOT is a ~790 kyr period that corresponds to the transition from “greenhouse” to “incehouse” conditions. The chronostratigraphic framework of the URG has been improved and the changes across the EOT documented. These changes consist of cooling, aridification, increased seasonal climatic contrast, and a greater sensibility of the climate to orbital variations. In the Mulhouse basin, the transition from structureless mudstones to laminated sediments and varves at the base of the “Sel III”, along the onset of orbitally induced sedimentary cycles, are the markers of these last two changes. Geochemical and palynological investigations performed in the Pechelbronn basin suggest the occurrence of a marine transgression near the base of the “Zone Fossilifère”.</dcterms:abstract>
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