0000000000417584

AUTHOR

Charlotte Prud'homme

0000-0002-1417-033x

showing 2 related works from this author

Millennial-scale terrestrial ecosystem responses to Upper Pleistocene climatic changes: 4D-reconstruction of the Schwalbenberg Loess-Palaeosol-Sequen…

2021

Abstract Loess-Palaeosol-Sequences (LPS) in the Central European region provide outstanding terrestrial polygenetic and multiphase archives responding to past climate and environments over various spatial and temporal scales. As yet, however, the geomorphological and pedogenic processes involved in LPS formation, and their interplay with changes in ecological conditions, impede robust correlation with other palaeoenvironmental archives. The Schwalbenberg LPS, which drape a hillslope in the Middle Rhine Valley in western Central Europe, provide unique high-resolution records highly suitable for investigating the processes involved in their formation and the relationship to climatic influence…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere010504 meteorology & atmospheric sciencesPleistocene04 agricultural and veterinary sciencesEcological succession15. Life on land01 natural sciencesPaleosolPedogenesis13. Climate actionLoess040103 agronomy & agriculture0401 agriculture forestry and fisheriesTerrestrial ecosystemPhysical geographyTransectTemporal scales[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes
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Improved discrimination of subglacial and periglacial erosion using10Be concentration measurements in subglacial and supraglacial sediment load of th…

2015

Deciphering the complex interplays between climate, uplift and erosion is not straightforward and estimating present-day erosion rates can provide useful insights. Glaciers are thought to be powerful erosional agents, but most published ‘glacial’ erosion rates combine periglacial, subglacial and proglacial erosion processes. Within a glaciated catchment, sediments found in subglacial streams originate either from glacial erosion of substratum or from the rock walls above the glacier that contribute to the supraglacial load. Terrestrial cosmogenic nuclides (TCN) are produced by interactions between cosmic ray particles and element targets at the surface of the Earth, but their concentration …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesBedrockGeography Planning and DevelopmentSedimentGlacier15. Life on land010502 geochemistry & geophysics01 natural sciencesSubglacial stream13. Climate actionEarth and Planetary Sciences (miscellaneous)Subglacial eruptionErosionGlacial periodCosmogenic nuclideGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesEarth Surface Processes and Landforms
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