Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
2014
Ladd, Brenton | Peri, Pablo L. | Pepper, David (David A.) | Silva, Lucas C. R. | Sheil, Douglas | Bonser, Stephen P. | Laffan, Shawn W. | Amelung, Wulf | Ekblad, Alf | Eliasson, Peter | Bahamonde, Hector | Duarte‐Guardia, Sandra | Bird, Michael | Cornelissen, Hans
Leaf area index (LAI), a measure of canopy density, is a key variable for modelling and understanding primary productivity, and also water use and energy exchange in forest ecosystems. However, LAI varies considerably with phenology and disturbance patterns, so alternative approaches to quantifying stand‐level processes should be considered. The carbon isotope composition of soil organic matter (δ¹³CSOM) provides a time‐integrated, productivity‐weighted measure of physiological and stand‐level processes, reflecting biomass deposition from seasonal to decadal time scales. Our primary aim was to explore how well LAI correlates with δ¹³CSOM across biomes. Using a global data set spanning large environmental gradients in tropical, temperate and boreal forest and woodland, we assess the strength of the correlation between LAI and δ¹³CSOM; we also assess climatic variables derived from the WorldClim database. We found that LAI was strongly correlated with δ¹³CSOM, but was also correlated with Mean Temperature of the Wettest Quarter, Mean Precipitation of Warmest Quarter and Annual Solar Radiation across and within biomes. Synthesis. Our results demonstrate that δ¹³CSOM values can provide spatially explicit estimates of leaf area index (LAI) and could therefore serve as a surrogate for productivity and water use. While δ¹³CSOM has traditionally been used to reconstruct the relative abundance of C₃ versus C₄ species, the results of this study demonstrate that within stable C₃‐ or C₄‐dominated biomes, δ¹³CSOM can provide additional insights. The fact that LAI is strongly correlated to δ¹³CSOM may allow for a more nuanced interpretation of ecosystem properties of palaeoecosystems based on palaeosol ¹³C values.
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