In: Plant and Soil, 2015, vol. 394, no. 1-2, p. 127-137
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In: Tree Physiology, 2018, vol. 38, no. 5, p. 706-720
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In: Boreas, 2020, p. bor.12480
Several palaeoclimatic archives have documented the pronounced climatic and environmental change associated with the Lateglacial–Holocene transition in the European Alps. However, the geomorphic response to this major environmental transition has only been punctually investigated. In this study, we propose a detailed reconstruction of post‐Last Glacial Maximum palaeoenvironmental...
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In: Climate of the Past, 2020, vol. 16, no. 3, p. 1061–1074
Differences between paleoclimatic reconstructions are caused by two factors: the method and the input data. While many studies compare methods, we will focus in this study on the consequences of the input data choice in a state-of-the-art Kalman- filter paleoclimate data assimilation approach. We evaluate reconstruction quality in the 20th century based on three collections of tree-ring...
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In: Tectonophysics, 2019, vol. 768, p. 228179
This work focuses particularly on the geomorphological evidence for the tectonic controls on the development of the present-day fluvial landscapes in the westernmost part of Switzerland. The tectonic deformation was evaluated on the basis of a combined analysis of several classical geomorphic indices (hypsometric curves and integrals, transverse topographic symmetry index, and channel's...
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In: Biogeochemistry, 2013, vol. 115, no. 1-3, p. 251-266
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In: Swiss Journal of Geosciences, 2010, vol. 103, no. 2, p. 283-292
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, no. 3, p. 409-428
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In: Plant and Soil, 2010, vol. 334, no. 1-2, p. 175-187
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In: Plant Ecology, 2012, vol. 213, no. 1, p. 35-46
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