Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/135837
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Type: Journal article
Title: A vegetation carbon isoscape for Australia built by combining continental-scale field surveys with remote sensing
Author: Munroe, S.E.M.
Guerin, G.R.
McInerney, F.A.
Martín-Forés, I.
Welti, N.
Farrell, M.
Atkins, R.
Sparrow, B.
Citation: Landscape Ecology, 2022; 37(8):1987-2006
Publisher: Springer
Issue Date: 2022
ISSN: 0921-2973
1572-9761
Statement of
Responsibility: 
Samantha E. M. Munroe, Greg R. Guerin, Francesca A. McInerney, Irene Martín, Forés, Nina Welti, Mark Farrell, Rachel Atkins, Ben Sparrow
Abstract: Context: Maps of C3 and C4 plant abundance and stable carbon isotope values (δ13C) across terrestrial landscapes are valuable tools in ecology to investigate species distribution and carbon exchange. Australia has a predominance of C4- plants, thus monitoring change in C3: C4 cover and δ13C is essential to national management priorities. Objectives: We applied a novel combination of field surveys and remote sensing data to create maps of C3 and C4 abundance in Australia, and a vegetation δ13C isoscape for the continent. Methods: We used vegetation and land-use rasters to categorize grid-cells (1 ha) into woody ( C3), native herbaceous, and herbaceous cropland ( C3 and C4) cover. Field surveys and environmental factors were regressed to predict native C4 herbaceous cover. These layers were combined and a δ13C mixing model was used to calculate site-averaged δ13C values. Results: Seasonal rainfall, maximum summer temperature, and soil pH were the best predictors of C4 herbaceous cover. Comparisons between predicted and observed values at field sites indicated our approach reliably predicted generalised C3: C4 abundance. Southern Australia, which has cooler temperatures and winter rainfall, was dominated by C3 vegetation and low δ13C values. C4- dominated areas included northern savannahs and grasslands. Conclusions: Our isoscape approach is distinct because it incorporates remote sensing products that calculate cover beneath the canopy, the influence of local factors, and extensive validation, all of which are critical to accurate predictions. Our models can be used to predict C3: C4 abundance under climate change, which is expected to substantially alter current C3: C4 abundance patterns.
Keywords: Photosynthesis; C4; C3; Isoscape; Carbon
Description: Published online: 5 July 2022
Rights: © The Author(s) 2022. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http:// creativecommons.org/ licenses/ by/4.0/.
DOI: 10.1007/s10980-022-01476-y
Grant ID: http://purl.org/au-research/grants/arc/FT110100100793
Published version: http://dx.doi.org/10.1007/s10980-022-01476-y
Appears in Collections:Ecology, Evolution and Landscape Science publications

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