0000000000417593

AUTHOR

Mathias Vinnepand

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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Combining inorganic and organic carbon stable isotope signatures in the Schwalbenberg Loess-Palaeosol-Sequence near Remagen (Middle Rhine valley, Ger…

2020

Western Central European Loess-Palaeosol-Sequences (LPS) provide valuable terrestrial records of palaeoenvironmental conditions, which formed in response to variability in the North Atlantic climate systems. Over the last full glacial cycle (∼130 ka), climate oscillations within these systems are best documented in deep sea- and ice cores; the responses of terrestrial systems are not yet fully understood. A better understanding of metabolism governing input and output variables of organic- and inorganic C pools is, however, crucial for investigating landscape-atmospheric feedback processes and in particularly, for understanding the formation of calcareous LPS as environmental archives. Here…

550 Earth sciencesSchwalbenberg LPSGeneral Earth and Planetary Sciencesstable isotopeslcsh:Qenvironmental changeOIS 3Loess-Palaeosol-Sequenceslcsh:Science550 Geowissenschaften
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