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Implications of fires on carbon budgets in Andean cloud montane forest: The importance of peat soils and tree resprouting
Authors:RM Román-Cuesta  N SalinasH Asbjornsen  I OliverasV Huaman  Y GutiérrezL Puelles  J KalaD Yabar  M RojasR Astete  DY JordánM Silman  R MosandlM Weber  B StimmS Günter  T KnokeY Malhi
Institution:a Institute of Silviculture, Technische Universität München, Am Hochanger 13, 85354 Weihenstephan, Freising, Munich, Germany
b Oxford University Centre for the Environment, Dyson Perrins Building, South Parks Road, OX13QY Oxford, United Kingdom
c Department of Natural Resource Ecology and Management, 339 Science II, Ames, IA 50011-3221, Iowa, USA
d Universidad San Antonio Abad del Cusco, Av. de la Cultura, Nro. 733, Apartado Postal No. 921 Cusco, Peru
e The Wake Forest University, Office: 134, Winston Hall, 1834 Wake Forest Road, Winston-Salem, NC 27106, USA
f Institute of Forest Management, Technische Universität München, Center of Life and Food Sciences Weihenstephan, Hans-Carl-von-Carlowitz-Platz 2, 85354 Freising, Germany
Abstract:Fire in tropical montane cloud forests (TMCFs) is not as rare as once believed. Andean TMCFs sit immediately below highly flammable, high-altitude grasslands (Puna/Páramo) that suffer from recurrent anthropogenic fire. This treeline is a zone of climatic tension where substantial future warming is likely to force upward tree migrations, while increased fire presence and fire impacts are likely to force it downwards. TMCFs contain large carbon stocks in their peat soils and their loss through fire is a currently unaccounted for regional source of CO2. This study, conducted in the southern Peruvian Andes (>2800 m), documents differences in live tree biomass, fine root biomass, fallen and standing dead wood, and soil organic carbon in 4 paired-sample plots (burned versus control) following the severe ground fires that occurred during the 2005 Andean drought. Peat soils contributed the most to biomass burning emissions, with lower values corresponding to an 89% mean stock difference compared to the controls (mean ± SE) (54.1 ± 22.3 vs. 5.8 ± 5.3 MgC ha−1). Contrastingly, carbon stocks from live standing trees differed by a non-significant 37% lower value in the burned plots compared to the controls, largely compensated by vigorous resprouting (45.5 ± 17.4 vs. 69.2 ± 13.4 MgC ha−1). Both standing dead trees and fallen dead wood were significantly higher in the burned plots with a three-fold difference from the controls: dead Trees 45.2 ± 9.4 vs. 16.4 ± 4.4 MgC ha−1, and ca. a 2 fold difference for the fallen dead wood: 11.2 ± 5 vs. 6.7 ± 3.2 MgC ha−1 for the burned plots versus their controls. A preliminary estimate of the regional contribution of biomass burning emissions from Andean TMCFs for the period 2000-2008, resulted in mean carbon emission rates of 1.3 TgC yr−1 (max-min: 1.8-0.8 TgC yr−1). This value is in the same order of magnitude than South American annual fire emissions (300 TgC yr−1) suggesting the need for further research on Andean forest fires. On-going projects on the region are working on the promotion of landowner participation in TMCFs conservation through REDD+ mechanism. The heart of the proposed initiative is reforestation of degraded lands with green fire breaks enriched with economically valuable Andean plant species. The cultivation of these species may contribute to reduce deforestation pressure on the Amazonian cloud forest by providing an alternative income to local communities, at the same time that they prevent the spread of fire into Manu National Park and adjacent community-held forests, protecting forest and reducing CO2 emissions.
Keywords:Biomass burning emissions  Resprouting  Montane cloud forests  Andes  Peat soil  REDD+
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