Soil respiration and rates of soil carbon turnover differ among six common European tree species

By L. Vesterdal, B. Elberling, J. Christiansen, I. Callesen, I. Schmidt. 2012

249 citations recorded by the source corpus.

Subfields: Ecology, Nature and Landscape Conservation, Soil Science

View Paper: https://www.semanticscholar.org/paper/04454772e67bc1bfba9b3c5139e97f86430e6ea3

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In Ecology

In Nature and Landscape Conservation

In Soil Science

Citations in the corpus

Tree Species Identity Shapes Earthworm Communities (2017, background): “This replicated common garden experiment has previously revealed tree species effects on C and N stocks in the forest floor and mineral soil [35], soil respiration and soil organic C turnover [36] and on N cycling and leaching and the water budget [37].”
Is Tree Species Diversity or Species Identity the More Important Driver of Soil Carbon Stocks, C/N Ratio, and pH? (2016, background): “Quercus robur proportion was not related to forest floor C stock which corresponds to its 377 intermediate status in terms of litter quality decomposition rates and earthworm abundance among the 378 studied species (Reich et al., 2005; Vesterdal et al., 2008; Vesterdal et al., 2012).”
Linking microbial communities, functional genes and nitrogen-cycling processes in forest floors under four tree species (2016, unknown): “Tree species also influence rates 96 of litter decomposition, nutrient release, C turnover and soil respiration through differences in 97 foliar N, Ca, Mg and lignin concentrations (Hobbie et al., 2006; Vesterdal et al., 2012, 98 2013).”
Biochemical pathways of amino acids in soil: Assessment by position-specific labeling and 13C-PLFA analysis (2013, unknown): “All rights reserved. vegetation and management (Van Miegroet and Jandl, 2007; Vesterdal et al., 2012).”
Root-induced changes in nutrient cycling in forests depend on exudation rates (2014, unknown): “A consequence of these dynamics is that ECM-dominated forests tend to cycle C and nutrients more conservatively than AM-dominated forests, and contribute to differential rates of soil C retention (Vesterdal et al., 2012; Averill et al., 2014) and N leaching losses (Midgley and Phillips, 2014).”
Digital mapping of soil organic matter for rubber plantation at regional scale: An application of random forest plus residuals kriging approach (2015, result): “Another inconsistence with other studies (Jobbagy and Jackson, 2000; Lorenz and Lal, 2010; Meier and Leuschner, 2010; Vesterdal et al., 2012; Wiesmeier et al., 2013) was that temperature was not the main factor influencing SOM variability in this study.”