@Article{GurdakARHCDFSMSM:2014:BaAbIn,
author = "Gurdak, Daniel J. and Arag{\~a}o, Luiz Eduardo Oliveira e Cruz de
and Rozas-D{\'a}vila, Angela and Huasco, Walter H. and Cabrera,
Karina G. and Doughty, Chris E. and Farfan-Rios, William and
Silva-Espejo, Javier E. and Metcalfe, Daniel B. and Silman, Miles
R. and Malhi, Yadvinder",
affiliation = "{Oxford University} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Universidad Nacional de San Antonio Abad del Cusco}
and {Universidad Nacional de San Antonio Abad del Cusco} and {Wake
Forest University} and {Oxford University} and {Wake Forest
University} and {Universidad Nacional de San Antonio Abad del
Cusco} and {Oxford University} and {Wake Forest University} and
{Oxford University}",
title = "Assessing above-ground woody debris dynamics along a gradient of
elevation in Amazonian cloud forests in Peru: balancing
above-ground inputs and respiration outputs",
journal = "Plant Ecology \& Diversity",
year = "2014",
volume = "7",
number = "1-2",
pages = "143--160",
keywords = "Amazon Basin, Andes, carbon balance, cloud forest, montane forest,
necromass, respiration, temperature sensitivity, tropical forest,
turnover.",
abstract = "Background: Dead biomass, including woody debris (WD), is an
important component of the carbon cycle in tropical forests. Aims:
This study analyses WD (>2 cm) and other above-ground fluxes in
mature tropical forest plots along an elevational gradient
(2103025 m above sea level) in southern Peru. Methods: This work
was based on inventories of fine and coarse WD (FWD and CWD,
respectively), above-ground biomass, and field-based and
experimental respiration measurements. Results: Total WD stocks
ranged from 6.26 Mg C ha\−1 at 3025 m to 11.48 Mg C
ha\−1 at 2720 m. WD respiration was significantly
correlated with moisture content (P < 0.001; R 2 = 0.25),
temperature (P < 0.001; R 2 = 0.12) and wood density (P < 0.001; R
2 = 0.16). Controlled experiments showed that both water content
and temperature increased respiration rates of individual WD
samples. The full breadth of the temperature sensitivity
coefficient, or Q 10, estimates, ranging from 1.142.13, was low
compared to other studies. In addition, temperature sensitivity of
WD respiration was greater for higher elevations. Conclusions:
Carbon stocks, mortality and turnover of above-ground biomass
varied widely and were not significantly related with elevation or
slope. This study demonstrates that some forests may be a carbon
source due to legacies of disturbance and increasing temperatures,
which may cause additional, short-term carbon efflux from WD.
Predictions of tropical forest carbon cycles under future climate
should incorporate WD dynamics and related feedback.",
doi = "10.1080/17550874.2013.818073",
url = "http://dx.doi.org/10.1080/17550874.2013.818073",
issn = "1755-0874",
label = "self-archiving-INPE-MCTI-GOV-BR",
language = "en",
targetfile = "
gurdak_et_al._2013_assessing_above-ground_woody_debris_dynamics_along_a_gradient_of_elevation_in_amazonian_cloud_forests_in_peru_balancing_above-ground_inputs_and_respiration_outputs.pdf",
urlaccessdate = "27 abr. 2024"
}