Estimations of total ecosystem carbon pools distribution and carbon biomass current annual increment of a moist tropical forest

2011 ◽  
Vol 261 (8) ◽  
pp. 1448-1459 ◽  
Author(s):  
Adrien N. Djomo ◽  
Alexander Knohl ◽  
Gode Gravenhorst
2011 ◽  
Vol 54 (3) ◽  
pp. 127-142 ◽  
Author(s):  
D Niu ◽  
SJ Hall ◽  
H Fu ◽  
J Kang ◽  
Y Qin ◽  
...  

2019 ◽  
Vol 5 (11) ◽  
pp. eaaw4418 ◽  
Author(s):  
Juan Carlos Quezada ◽  
Andres Etter ◽  
Jaboury Ghazoul ◽  
Alexandre Buttler ◽  
Thomas Guillaume

Alternatives to ecologically devastating deforestation land use change trajectories are needed to reduce the carbon footprint of oil palm (OP) plantations in the tropics. Although various land use change options have been proposed, so far, there are no empirical data on their long-term ecosystem carbon pools effects. Our results demonstrate that pasture-to-OP conversion in savanna regions does not change ecosystem carbon storage, after 56 years in Colombia. Compared to rainforest conversion, this alternative land use change reduces net ecosystem carbon losses by 99.7 ± 9.6%. Soil organic carbon (SOC) decreased until 36 years after conversion, due to a fast decomposition of pasture-derived carbon, counterbalancing the carbon gains in OP biomass. The recovery of topsoil carbon content, suggests that SOC stocks might partly recover during a third plantation cycle. Hence, greater OP sustainability can be achieved if its expansion is oriented toward pasture land.


1999 ◽  
Vol 26 (6) ◽  
pp. 1237-1248 ◽  
Author(s):  
D. T. Price ◽  
C. H. Peng ◽  
M. J. Apps ◽  
D. H. Halliwell

2014 ◽  
Vol 134 (2) ◽  
pp. 319-333 ◽  
Author(s):  
Ender Makineci ◽  
Emrah Ozdemir ◽  
Servet Caliskan ◽  
Ersel Yilmaz ◽  
Meric Kumbasli ◽  
...  

2011 ◽  
Vol 345 (1-2) ◽  
pp. 287-302 ◽  
Author(s):  
Andrea J. Britton ◽  
Rachel C. Helliwell ◽  
Allan Lilly ◽  
Lorna Dawson ◽  
Julia M. Fisher ◽  
...  

2016 ◽  
Vol 104 (4) ◽  
pp. 1020-1031 ◽  
Author(s):  
Erik S. Yando ◽  
Michael J. Osland ◽  
Jonathan M. Willis ◽  
Richard H. Day ◽  
Ken W. Krauss ◽  
...  

2020 ◽  
Vol 29 (1) ◽  
pp. e001
Author(s):  
Shatya Devi Quintero-Gradilla ◽  
Angelina Martínez-Yrizar ◽  
Felipe Gracía-Oliva ◽  
Ramón Cuevas-Guzmán ◽  
José Enrique Jardel-Peláez

Aim of the study: To analyze the recovery pattern of carbon pools in terms of size and the relative contribution of each pool to total ecosystem C along a fire chronosequence of tropical mixed pine-hardwood forest.Area of the study: Las Joyas Research Station (LJRS), core zone of Sierra de Manantlán Biosphere Reserve (SMBR) in the state of Jalisco, central western Mexico.Materials and methods: Carbon stored in aboveground plant biomass, standing dead trees, downed woody debris, forest floor, fine roots and mineral soil, was compared with a nested analysis of variance (ANOVA) in post-fire stands of eight-year-old, 28- and 60-year-old stands of mixed Pinus douglasiana-hardwood forest.Main results: The total ecosystem carbon in eight-year-old stands was 50% lower than that of 60-year-old stands. Carbon content in the biomass and mineral soil increased with stand age. The carbon in the biomass recovered to the undisturbed forest in the 28 years of succession. The main C storage in the eight-year-old stands were the mineral soil (64%) and downed woody debris (18%), while in the 28- and 60-year-old stands, live tree biomass and mineral soil were the two largest components of the total C pool (43% and 46%, respectively).Research highlights: We found a significant effect of high-severity fire events on ecosystem C storage and a shift in carbon distribution. The relatively fast recovery of C in ecosystem biomass suggests that mixed Pinus douglasiana hardwood forest possess functional traits that confer resilience to severe fire events.Key words: chronosequence; carbon dynamics; mineral soil; Pinus douglasiana; fire effects.Abbreviations used: LJRS, Las Joyas Research Station; DBH, diameter at breast height; DL, duff layer; LL, litter layer; DWD, downed woody debris; ANOVA, analysis of variance; CO2, carbon dioxide; SMBR, Sierra de Manantlán Biosphere Reserve; C, carbon. AGV, above ground vegetation.


Sign in / Sign up

Export Citation Format

Share Document