Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes

Ladd, Brenton, Peri, Pablo L., Pepper, 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, and Bird, Michael (2014) Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes. Journal of Ecology, 102 (6). pp. 1606-1611.

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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 (δ^13C(SOM)) 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 δ^13C(SOM) 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 δ^13C(SOM); we also assess climatic variables derived from the WorldClim database. We found that LAI was strongly correlated with δ^13C(SOM), 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 δ^13C(SOM) values can provide spatially explicit estimates of leaf area index (LAI) and could therefore serve as a surrogate for productivity and water use. While δ^13C(SOM) 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, δ^13C(SOM) can provide additional insights. The fact that LAI is strongly correlated to δ^13C(SOM) may allow for a more nuanced interpretation of ecosystem properties of palaeoecosystems based on palaeosol 13C values.

Item ID: 38018
Item Type: Article (Research - C1)
ISSN: 1365-2745
Keywords: climate, isoscapes, leaf area index, paleoecosystems, plant–soil (below-ground) interactions, productivity, stable isotopes, water stress, δ^13C, δ^13C(SOM)
Funders: City of Onkaparinga, University of New South Wales (UNSW), University of Bonn, Swedish University of Agricultural Sciences
Date Deposited: 31 Mar 2015 00:10
FoR Codes: 04 EARTH SCIENCES > 0402 Geochemistry > 040203 Isotope Geochemistry @ 50%
05 ENVIRONMENTAL SCIENCES > 0501 Ecological Applications > 050104 Landscape Ecology @ 50%
SEO Codes: 97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%
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