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Effects of experimental stem burial on radial growth and wood anatomy of pedunculate oak
Institution:2. Climatic Change and Climate Impacts (C3i), Institute for Environmental Sciences, University of Geneva, 7 route de Drize, CH-1227 Carouge-Geneva, Switzerland;3. Section of Earth and Environmental Sciences, University of Geneva, rue des Maraîchers 13, CH-1205 Geneva, Switzerland;1. Department of Geoinformatics (www.geoinformatics.upol.cz), Faculty of Science, Palacký University, 17. listopadu 50, CZ-771 46 Olomouc, Czech Republic;2. Faculty of Regional Development and International Studies, Mendel University, t?ída Generála Píky 7, CZ-613 00 Brno, Czech Republic;3. Centre for Environment and Land Assessment – Ekotoxa, Otická 37, CZ-746 01 Opava, Czech Republic;4. Faculty of Philosophy and Science, Silesian University at Opava, Masarykova 37, CZ-746 01 Opava, Czech Republic;5. Regional Centre of Advanced Technologies and Materials, Faculty of Science, Palacký University, ?lechtitel? 27, CZ-78371 Olomouc, Czech Republic;6. Global Change Research Institute, The Czech Academy of Sciences, v.v.i., Bělidla 986/4a, CZ-603 00 Brno, Czech Republic;7. Forest Management Institute Brandýs nad Labem, Náb?e?ní 1326, CZ-250 01 Brandýs nad Labem, Czech Republic
Abstract:In dendrogeomorphology, abrupt changes in wood anatomy are frequently used to date the exact year of burial and exposure events. However, few studies have addressed the precision and underlying mechanisms of these changes. In a field experiment, performed in a drift-sand area in the Netherlands, we buried the stems of mature pedunculate oak trees (Quercus robur L.) up to a height of 50 cm and analysed the responses in ring width and earlywood-vessel characteristics, while monitoring the course of temperature above and below the soil surface.After 3 years of stem burial, we found no significant differences in ring width and earlywood-vessel characteristics between control and buried trees both above and below the burial level. Burial however strongly reduced temperature amplitude and the occurrence of sub-zero temperatures around the buried stems. All buried trees formed epitropic roots that grew upward into the new sediment layer, but no adventitious roots were formed on the buried stems. Irrespective of the burial treatments, we found that the mean ring width was largest at the original stem base and lowest at breast height. In contrast, vessel sizes were significantly larger at breast height compared with the stem base. Differences in vessel density barely differed between years and heights.In our field experiment on mature pedunculate oak trees, the burial of stems by 50 cm of drift sand did not induce any local growth suppression or detectable changes in wood anatomy. As wood-anatomical changes in response to burial have previously been reported for trees that had formed adventitious roots, we stress the role of adventitious-root formation as a possible trigger behind the local changes in wood anatomy, reflecting a functional change of a buried stem towards a root. Based on our field experiment, it seems unlikely that years of shallow or moderate burial events (≤50 cm) can be reconstructed using the wood structure of buried stems. As epitropic roots develop quickly after burial, dating such roots may potentially yield better estimates of burial events. Further research on the relation between adventitious root and changes in stem anatomy is needed to ascertain the precision of dating sand-burial events using tree rings.
Keywords:Dendrogeomorphology  Drift sand  Growth response  Wood anatomy
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