Articles | Volume 13, issue 5
Biogeosciences, 13, 1537–1552, 2016
https://doi.org/10.5194/bg-13-1537-2016
Biogeosciences, 13, 1537–1552, 2016
https://doi.org/10.5194/bg-13-1537-2016

Research article 11 Mar 2016

Research article | 11 Mar 2016

Time since death and decay rate constants of Norway spruce and European larch deadwood in subalpine forests determined using dendrochronology and radiocarbon dating

Marta Petrillo1,2, Paolo Cherubini2, Giulia Fravolini4, Marco Marchetti4, Judith Ascher-Jenull5,6, Michael Schärer1, Hans-Arno Synal3, Daniela Bertoldi7, Federica Camin7, Roberto Larcher7, and Markus Egli1 Marta Petrillo et al.
  • 1Department of Geography, University of Zurich, 8057 Zurich, Switzerland
  • 2WSL Swiss Federal Institute for Forest, Snow and Landscape Research, 8903 Birmensdorf, Switzerland
  • 3Laboratory of Ion Beam Physics, ETH Zurich, 8093 Zurich, Switzerland
  • 4Department of Bioscience and Territory, University of Molise, 86090 Pesche, Italy
  • 5Department of Agrifood and Environmental Science, University of Florence, 50144 Florence, Italy
  • 6Institute of Microbiology, University of Innsbruck, 6020 Innsbruck, Austria
  • 7Fondazione Edmund Mach, 38010 San Michele all'Adige, Italy

Abstract. Due to the large size (e.g. sections of tree trunks) and highly heterogeneous spatial distribution of deadwood, the timescales involved in the coarse woody debris (CWD) decay of Picea abies (L.) Karst. and Larix decidua Mill. in Alpine forests are largely unknown. We investigated the CWD decay dynamics in an Alpine valley in Italy using the chronosequence approach and the five-decay class system that is based on a macromorphological assessment. For the decay classes 1–3, most of the dendrochronological samples were cross-dated to assess the time that had elapsed since tree death, but for decay classes 4 and 5 (poorly preserved tree rings) radiocarbon dating was used. In addition, density, cellulose, and lignin data were measured for the dated CWD. The decay rate constants for spruce and larch were estimated on the basis of the density loss using a single negative exponential model, a regression approach, and the stage-based matrix model. In the decay classes 1–3, the ages of the CWD were similar and varied between 1 and 54 years for spruce and 3 and 40 years for larch, with no significant differences between the classes; classes 1–3 are therefore not indicative of deadwood age. This seems to be due to a time lag between the death of a standing tree and its contact with the soil. We found distinct tree-species-specific differences in decay classes 4 and 5, with larch CWD reaching an average age of 210 years in class 5 and spruce only 77 years. The mean CWD rate constants were estimated to be in the range 0.018 to 0.022 y−1 for spruce and to about 0.012 y−1 for larch. Snapshot sampling (chronosequences) may overestimate the age and mean residence time of CWD. No sampling bias was, however, detectable using the stage-based matrix model. Cellulose and lignin time trends could be derived on the basis of the ages of the CWD. The half-lives for cellulose were 21 years for spruce and 50 years for larch. The half-life of lignin is considerably higher and may be more than 100 years in larch CWD. Consequently, the decay of Picea abies and Larix decidua is very low. Several uncertainties, however, remain: 14C dating of CWD from decay classes 4 and 5 and having a pre-bomb age is often difficult (large age range due to methodological constraints) and fall rates of both European larch and Norway spruce are missing.

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The timescales involved in the decay of coarse woody debris (CWD) and related chemical components of spruce and larch in Alpine forests are largely unknown. Dendrochronology and 14C dating were used to assess time and rates. Distinct differences between tree species occur only at an advanced stage of decay. Larch CWD reaches an age of 210 years and spruce 77 years. Using this approach, the half-lives of cellulose (21 yr for spruce and 50 yr for larch) and lignin (> 100 yr) could be determined.
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