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

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...

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Autores principales: Ladd, Brenton, Peri, Pablo Luis, Pepper, David A., Silva, Lucas C.R., Sheil, Douglas, Bonser, Stephen P., Laffan, Shawn W., Amelung, Wulf, Ekblad, Alf, Eliasson, Peter, Bahamonde, Héctor Alejandro, Duarte Guardia, Sandra, Bird, Michael I.
Formato: Artículo
Lenguaje:Inglés
Publicado: Wiley 2019
Materias:
Acceso en línea:https://besjournals.onlinelibrary.wiley.com/doi/10.1111/1365-2745.12309
http://hdl.handle.net/20.500.12123/4745
https://doi.org/10.1111/1365-2745.12309
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author Ladd, Brenton
Peri, Pablo Luis
Pepper, David A.
Silva, Lucas C.R.
Sheil, Douglas
Bonser, Stephen P.
Laffan, Shawn W.
Amelung, Wulf
Ekblad, Alf
Eliasson, Peter
Bahamonde, Héctor Alejandro
Duarte Guardia, Sandra
Bird, Michael I.
author_browse Amelung, Wulf
Bahamonde, Héctor Alejandro
Bird, Michael I.
Bonser, Stephen P.
Duarte Guardia, Sandra
Ekblad, Alf
Eliasson, Peter
Ladd, Brenton
Laffan, Shawn W.
Pepper, David A.
Peri, Pablo Luis
Sheil, Douglas
Silva, Lucas C.R.
author_facet Ladd, Brenton
Peri, Pablo Luis
Pepper, David A.
Silva, Lucas C.R.
Sheil, Douglas
Bonser, Stephen P.
Laffan, Shawn W.
Amelung, Wulf
Ekblad, Alf
Eliasson, Peter
Bahamonde, Héctor Alejandro
Duarte Guardia, Sandra
Bird, Michael I.
author_sort Ladd, Brenton
collection INTA Digital
description 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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spelling INTA47452019-06-05T18:12:44Z Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes Ladd, Brenton Peri, Pablo Luis Pepper, David A. Silva, Lucas C.R. Sheil, Douglas Bonser, Stephen P. Laffan, Shawn W. Amelung, Wulf Ekblad, Alf Eliasson, Peter Bahamonde, Héctor Alejandro Duarte Guardia, Sandra Bird, Michael I. Materia Orgánica del Suelo Carbono Isótopos Índice de Superficie Foliar Plantas Leñosas Soil Organic Matter Carbon Isotopes Leaf Area Index Woody Plants 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. EEA Santa Cruz Fil: Ladd, Brenton. Universidad Científica del Sur. Escuela de Agroforestería; Peru. University of New South Wales. School of Biological. Earth and Environmental Sciences, Evolution and Ecology Research Centre; Australia Fil: Peri, Pablo Luis. Universidad Nacional de la Patagonia Austral; Argentina. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Santa Cruz; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Pepper, David A. University of New South Wales. School of Biological, Earth and Environmental Sciences; Australia. Fil: Silva, Lucas C.R. University of California. Department of Land, Air and Water Resources; Estados Unidos Fil: Sheil, Douglas. Southern Cross University. School of Environmental Science and Management; Australia. Center for International Forestry Research; Indonesia. Norwegian University of Life Sciences. Department of Ecology and Natural Resource Management; Noruega Fil: Bonser, Stephen P. University of New South Wales. School of Biological, Earth and Environmental Sciences. Evolution and Ecology Research Centre; Australia Fil: Laffan, Shawn W. University of New South Wales. School of Biological, Earth and Environmental Sciences; Australia Fil: Amelung, Wulf. University of Bonn. Soil Science and Soil Ecology. Institute of Crop Science and Resource Conservation (INRES); Alemania Fil: Ekblad, Alf. Örebro University. School of Science and Technology; Suecia Fil: Eliasson, Peter. Örebro University. School of Science and Technology; Suecia. Lund University. Department of Physical Geography and Ecosystem Science; Suecia Fil: Bahamonde, Héctor Alejandro. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Santa Cruz; Argentina. Universidad Nacional de la Patagonia Austral; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Duarte Guardia, Sandra. Universidad Científica del Sur. Facultad de Ciencias Ambientales; Perú Fil: Bird, Michael I. Swedish University of Agricultural Sciences. Department of Ecology; Suecia. James Cook University. College of Science, Technology and Engineering and Centre for Tropical Environmental and Sustainability Science; Australia 2019-03-26T15:35:27Z 2019-03-26T15:35:27Z 2014-11 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion https://besjournals.onlinelibrary.wiley.com/doi/10.1111/1365-2745.12309 http://hdl.handle.net/20.500.12123/4745 0022-0477 1365-2745 https://doi.org/10.1111/1365-2745.12309 eng info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf Wiley Journal of Ecology 102 (6) : 1606-1611 (November 2014)
spellingShingle Materia Orgánica del Suelo
Carbono
Isótopos
Índice de Superficie Foliar
Plantas Leñosas
Soil Organic Matter
Carbon
Isotopes
Leaf Area Index
Woody Plants
Ladd, Brenton
Peri, Pablo Luis
Pepper, David A.
Silva, Lucas C.R.
Sheil, Douglas
Bonser, Stephen P.
Laffan, Shawn W.
Amelung, Wulf
Ekblad, Alf
Eliasson, Peter
Bahamonde, Héctor Alejandro
Duarte Guardia, Sandra
Bird, Michael I.
Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
title Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
title_full Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
title_fullStr Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
title_full_unstemmed Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
title_short Carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
title_sort carbon isotopic signatures of soil organic matter correlate with leaf area index across woody biomes
topic Materia Orgánica del Suelo
Carbono
Isótopos
Índice de Superficie Foliar
Plantas Leñosas
Soil Organic Matter
Carbon
Isotopes
Leaf Area Index
Woody Plants
url https://besjournals.onlinelibrary.wiley.com/doi/10.1111/1365-2745.12309
http://hdl.handle.net/20.500.12123/4745
https://doi.org/10.1111/1365-2745.12309
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