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Net landscape carbon balance of a tropical savanna: Relative importance of fire and aquatic export in offsetting terrestrial production.

Authors :
Duvert C
Hutley LB
Beringer J
Bird MI
Birkel C
Maher DT
Northwood M
Rudge M
Setterfield SA
Wynn JG
Source :
Global change biology [Glob Chang Biol] 2020 Oct; Vol. 26 (10), pp. 5899-5913. Date of Electronic Publication: 2020 Aug 13.
Publication Year :
2020

Abstract

The magnitude of the terrestrial carbon (C) sink may be overestimated globally due to the difficulty of accounting for all C losses across heterogeneous landscapes. More complete assessments of net landscape C balances (NLCB) are needed that integrate both emissions by fire and transfer to aquatic systems, two key loss pathways of terrestrial C. These pathways can be particularly significant in the wet-dry tropics, where fire plays a fundamental part in ecosystems and where intense rainfall and seasonal flooding can result in considerable aquatic C export (ΣF <subscript>aq</subscript> ). Here, we determined the NLCB of a lowland catchment (~140 km <superscript>2</superscript> ) in tropical Australia over 2 years by evaluating net terrestrial productivity (NEP), fire-related C emissions and ΣF <subscript>aq</subscript> (comprising both downstream transport and gaseous evasion) for the two main landscape components, that is, savanna woodland and seasonal wetlands. We found that the catchment was a large C sink (NLCB 334 Mg C km <superscript>-2</superscript>  year <superscript>-1</superscript> ), and that savanna and wetland areas contributed 84% and 16% to this sink, respectively. Annually, fire emissions (-56 Mg C km <superscript>-2</superscript>  year <superscript>-1</superscript> ) and ΣF <subscript>aq</subscript> (-28 Mg C km <superscript>-2</superscript>  year <superscript>-1</superscript> ) reduced NEP by 13% and 7%, respectively. Savanna burning shifted the catchment to a net C source for several months during the dry season, while ΣF <subscript>aq</subscript> significantly offset NEP during the wet season, with a disproportionate contribution by single major monsoonal events-up to 39% of annual ΣF <subscript>aq</subscript> was exported in one event. We hypothesize that wetter and hotter conditions in the wet-dry tropics in the future will increase ΣF <subscript>aq</subscript> and fire emissions, potentially further reducing the current C sink in the region. More long-term studies are needed to upscale this first NLCB estimate to less productive, yet hydrologically dynamic regions of the wet-dry tropics where our result indicating a significant C sink may not hold.<br /> (© 2020 John Wiley & Sons Ltd.)

Details

Language :
English
ISSN :
1365-2486
Volume :
26
Issue :
10
Database :
MEDLINE
Journal :
Global change biology
Publication Type :
Academic Journal
Accession number :
32686242
Full Text :
https://doi.org/10.1111/gcb.15287