SOIL, 2, 537–549, 2016 www.soil-journal.net/2/537/2016/ doi:10.5194/soil-2-537-2016 SOIL © Author(s) 2016. CC Attribution 3.0 License. Paleosols can promote root growth of recent vegetation – a case study from the sandy soil–sediment sequence Rakt, the Netherlands Martina I. Gocke1,2, Fabian Kessler1, Jan M. van Mourik3, Boris Jansen4, and Guido L. B. Wiesenberg1 1Department of Geography, University of Zurich, Winterthurerstr. 190, 8057 Zurich, Switzerland 2Institute of Crop Science and Resource Conservation, University of Bonn, Nussallee 13, 53115 Bonn, Germany 3IBED-Paleoecology, University of Amsterdam, P.O. Box 94240, Amsterdam 1090 GE, the Netherlands 4IBED-Earth Surface Science, University of Amsterdam, P.O. Box 94240, Amsterdam 1090 GE, the Netherlands Correspondence to: Martina I. Gocke (
[email protected]) Received: 3 November 2015 – Published in SOIL Discuss.: 14 December 2015 Accepted: 15 September 2016 – Published: 21 October 2016 Abstract. Soil studies commonly comprise the uppermost meter for tracing, e.g., soil development. However, the maximum rooting depth of various plants significantly exceeds this depth. We hypothesized that deeper parts of the soil, soil parent material and especially paleosols provide beneficial conditions in terms of, e.g., nutrient contents, thus supporting their utilization and exploitation by deep roots. We aimed to decipher the different phases of soil formation in Dutch drift sands and cover sands. The study site is located at Bedafse Bergen (south- eastern Netherlands) in a 200-year-old oak stand. A recent Podzol developed on drift sand covering a Plaggic Anthrosol that was piled up on a relict Podzol on Late Glacial eolian cover sand.