Soil respiration across a disturbance gradient in sclerophyllous ecosystems in Central Chile

Indexado

WoS: WOS:000336641900009

Scopus: SCOPUS_ID:84901786733

SciELO: S0718-16202014000100009

Año

2014

Tipo

artículo de investigación

0
Citas Totales
0
Autores Afiliación Chile
0
Instituciones Chile
0
% Participación Internacional
0
Autores Afiliación Extranjera
0
Instituciones Extranjeras

Abstract

Sclerophyllous shrubs and forests are predominant in semiarid Central Chile and have a long history of degradation by fire, cultivation, firewood extraction and grazing. The aim of this study was to compare the amount and environmental drivers of soil respiration across a disturbance gradient in sclerophyllous ecosystems in the National Reserve Robleria del Cobre de Loncha in Central Chile. In a north-facing toe slope, four disturbance conditions were identified: slightly (D1) and moderately disturbed (D2) sclerophyllous forest, (D3) strongly disturbed thorn scrub and (D4) most disturbed A. caven savanna. Twelve 25x25-m plots (625 m(2)) were distributed equally across D1, D2, D3 and D4. Soil respiration (R-s), soil temperature (T-s), volumetric water content (theta(v)) and exchangeable nitrogen (N-s) were measured at six dates in each plot between August 2009 and May 2010. Additionally, T-s and theta(v), were continuously recorded from July 2010 to August 2012 (30-minute intervals) in one plot per disturbance condition (i.e., 4 out of 12 plots). The values of R-s increased linearly with theta(v) with similar slopes but different intercepts, which increased as the disturbance receded. Once soil water content was taken into account, R-s increased with T-s with the same slope but with a disturbance-dependent intercept. Additionally, the response of R-s to T-s was more pronounced as theta(v), increased. The values of N-s were uncorrelated with R-s. The annual values of R-s were 4.4-fold greater in D1 (1,735 g C m(-2)yr(-1)) compared with D4 (392 g C m(-2) yr(-1)). Disturbance presumably decreased R-s by reducing the litter layer, soil organic matter, root biomass and soil water content, particularly in the hot-dry season. Under a predicted climate change scenario of a 40% decrease in rainfall and 4 degrees C increase in air temperature by the year 2100, we found that annual R-s would be reduced on average by 28% compared with the current climate, with that reduction being more pronounced under more disturbed conditions, suggesting that less disturbed conditions would be more resistant to climate change, thus further justifying the restoration of these damaged ecosystems.

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Disciplinas de Investigación

WOS
Agriculture, Multidisciplinary
Scopus
Agricultural And Biological Sciences (All)
SciELO
Agricultural Sciences
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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

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Citas No-identificadas: 25.0 %

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Citas Identificadas: 75.0 %
Citas No-identificadas: 25.0 %

Financiamiento

Fuente
FONDECYT
CONICYT
Comisión Nacional de Investigación Científica y Tecnológica
Directorate For Geosciences; ICER
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Agradecimientos

Agradecimiento
During this work, the senior author was supported by the Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) through the project FONDECYT N degrees 1090259: "Disturbance mediated water and nutrient stresses regulate carbon assimilation and allocation in sclerophyllous forests in Central Chile: A process-based approach". Soil physical variables were provided by FONDECYT N degrees 1090283 "Quality and fluxes of soil organic carbon as affected by anthropogenic perturbations of sclerophyllous vegetation of Central Chile". We thank Mr. Jorge Vega B. (Universidad de Chile), Mrs. Cristina Saez N. (Universidad de Chile), Mr. Roberto Cerda R. (Forest Service CONAF) and Mr. Eric Campos (Universidad de Chile) for their kind advice and valuable technical skills. The experiments and measurements performed for this paper comply with the current laws of Chile.
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