Carbon stocks and soil sequestration rates of tropical riverine wetlands

Riverine wetlands are created and transformed by geomorphological processes that determine their vegetation composition, primary production and soil accretion, all of which are likely to influence C stocks. Here, we compared ecosystem C stocks (trees, soil and downed wood) and soil N stocks of different types of riverine wetlands (marsh, peat swamp forest and mangroves) whose distribution spans from an environment dominated by river forces to an estuarine environment dominated by coastal processes. We also estimated soil C sequestration rates of mangroves on the basis of soil C accumulation. We predicted that C stocks in mangroves and peat swamps would be larger than marshes, and that C, N stocks and C sequestration rates would be larger in the upper compared to the lower estuary. Mean C stocks in mangroves and peat swamps (784.5±73.5 and 722.2±63.6MgCha-¹, respectively) were higher than those of marshes (336.5±38.3MgCha-¹/. Soil C and N stocks of mangroves were highest in the upper estuary and decreased towards the lower estuary. C stock variability within mangroves was much lower in the upper estuary (range 744- 912MgCha-¹/ compared to the intermediate and lower estuary (range 537-1115MgCha-¹/ probably as a result of a highly dynamic coastline. Soil C sequestration values were 1.3±0.2MgCha-¹ yr-¹ and were similar across sites. Estimations of C stocks within large areas need to include spatial variability related to vegetation composition and geomorphological setting to accurately reflect variability within riverine wetlands.

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Main Authors: Adame, María Fernanda, Santini, N. S. autor/a, Tovilla Hernández, Cristian Doctor autor/a 3180, Vázquez Lule, Alma Delia autor/a, Castro, L. autor/a, Guevara, M. autor/a
Format: Texto biblioteca
Language:eng
Subjects:Reservorios de carbono, Captura de carbono, Humedales, Manglares, Artfrosur,
Online Access:http://www.biogeosciences.net/12/3805/2015/bg-12-3805-2015.pdf
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spelling KOHA-OAI-ECOSUR:73482024-03-12T12:44:23ZCarbon stocks and soil sequestration rates of tropical riverine wetlands Adame, María Fernanda Santini, N. S. autor/a Tovilla Hernández, Cristian Doctor autor/a 3180 Vázquez Lule, Alma Delia autor/a Castro, L. autor/a Guevara, M. autor/a textengRiverine wetlands are created and transformed by geomorphological processes that determine their vegetation composition, primary production and soil accretion, all of which are likely to influence C stocks. Here, we compared ecosystem C stocks (trees, soil and downed wood) and soil N stocks of different types of riverine wetlands (marsh, peat swamp forest and mangroves) whose distribution spans from an environment dominated by river forces to an estuarine environment dominated by coastal processes. We also estimated soil C sequestration rates of mangroves on the basis of soil C accumulation. We predicted that C stocks in mangroves and peat swamps would be larger than marshes, and that C, N stocks and C sequestration rates would be larger in the upper compared to the lower estuary. Mean C stocks in mangroves and peat swamps (784.5±73.5 and 722.2±63.6MgCha-¹, respectively) were higher than those of marshes (336.5±38.3MgCha-¹/. Soil C and N stocks of mangroves were highest in the upper estuary and decreased towards the lower estuary. C stock variability within mangroves was much lower in the upper estuary (range 744- 912MgCha-¹/ compared to the intermediate and lower estuary (range 537-1115MgCha-¹/ probably as a result of a highly dynamic coastline. Soil C sequestration values were 1.3±0.2MgCha-¹ yr-¹ and were similar across sites. Estimations of C stocks within large areas need to include spatial variability related to vegetation composition and geomorphological setting to accurately reflect variability within riverine wetlands.Riverine wetlands are created and transformed by geomorphological processes that determine their vegetation composition, primary production and soil accretion, all of which are likely to influence C stocks. Here, we compared ecosystem C stocks (trees, soil and downed wood) and soil N stocks of different types of riverine wetlands (marsh, peat swamp forest and mangroves) whose distribution spans from an environment dominated by river forces to an estuarine environment dominated by coastal processes. We also estimated soil C sequestration rates of mangroves on the basis of soil C accumulation. We predicted that C stocks in mangroves and peat swamps would be larger than marshes, and that C, N stocks and C sequestration rates would be larger in the upper compared to the lower estuary. Mean C stocks in mangroves and peat swamps (784.5±73.5 and 722.2±63.6MgCha-¹, respectively) were higher than those of marshes (336.5±38.3MgCha-¹/. Soil C and N stocks of mangroves were highest in the upper estuary and decreased towards the lower estuary. C stock variability within mangroves was much lower in the upper estuary (range 744- 912MgCha-¹/ compared to the intermediate and lower estuary (range 537-1115MgCha-¹/ probably as a result of a highly dynamic coastline. Soil C sequestration values were 1.3±0.2MgCha-¹ yr-¹ and were similar across sites. Estimations of C stocks within large areas need to include spatial variability related to vegetation composition and geomorphological setting to accurately reflect variability within riverine wetlands.Adobe Acrobat profesional 6.0 o superiorReservorios de carbonoCaptura de carbonoHumedalesManglaresArtfrosurDisponible en líneaBiogeoscienceshttp://www.biogeosciences.net/12/3805/2015/bg-12-3805-2015.pdfAcceso en línea sin restricciones
institution ECOSUR
collection Koha
country México
countrycode MX
component Bibliográfico
access En linea
En linea
databasecode cat-ecosur
tag biblioteca
region America del Norte
libraryname Sistema de Información Bibliotecario de ECOSUR (SIBE)
language eng
topic Reservorios de carbono
Captura de carbono
Humedales
Manglares
Artfrosur
Reservorios de carbono
Captura de carbono
Humedales
Manglares
Artfrosur
spellingShingle Reservorios de carbono
Captura de carbono
Humedales
Manglares
Artfrosur
Reservorios de carbono
Captura de carbono
Humedales
Manglares
Artfrosur
Adame, María Fernanda
Santini, N. S. autor/a
Tovilla Hernández, Cristian Doctor autor/a 3180
Vázquez Lule, Alma Delia autor/a
Castro, L. autor/a
Guevara, M. autor/a
Carbon stocks and soil sequestration rates of tropical riverine wetlands
description Riverine wetlands are created and transformed by geomorphological processes that determine their vegetation composition, primary production and soil accretion, all of which are likely to influence C stocks. Here, we compared ecosystem C stocks (trees, soil and downed wood) and soil N stocks of different types of riverine wetlands (marsh, peat swamp forest and mangroves) whose distribution spans from an environment dominated by river forces to an estuarine environment dominated by coastal processes. We also estimated soil C sequestration rates of mangroves on the basis of soil C accumulation. We predicted that C stocks in mangroves and peat swamps would be larger than marshes, and that C, N stocks and C sequestration rates would be larger in the upper compared to the lower estuary. Mean C stocks in mangroves and peat swamps (784.5±73.5 and 722.2±63.6MgCha-¹, respectively) were higher than those of marshes (336.5±38.3MgCha-¹/. Soil C and N stocks of mangroves were highest in the upper estuary and decreased towards the lower estuary. C stock variability within mangroves was much lower in the upper estuary (range 744- 912MgCha-¹/ compared to the intermediate and lower estuary (range 537-1115MgCha-¹/ probably as a result of a highly dynamic coastline. Soil C sequestration values were 1.3±0.2MgCha-¹ yr-¹ and were similar across sites. Estimations of C stocks within large areas need to include spatial variability related to vegetation composition and geomorphological setting to accurately reflect variability within riverine wetlands.
format Texto
topic_facet Reservorios de carbono
Captura de carbono
Humedales
Manglares
Artfrosur
author Adame, María Fernanda
Santini, N. S. autor/a
Tovilla Hernández, Cristian Doctor autor/a 3180
Vázquez Lule, Alma Delia autor/a
Castro, L. autor/a
Guevara, M. autor/a
author_facet Adame, María Fernanda
Santini, N. S. autor/a
Tovilla Hernández, Cristian Doctor autor/a 3180
Vázquez Lule, Alma Delia autor/a
Castro, L. autor/a
Guevara, M. autor/a
author_sort Adame, María Fernanda
title Carbon stocks and soil sequestration rates of tropical riverine wetlands
title_short Carbon stocks and soil sequestration rates of tropical riverine wetlands
title_full Carbon stocks and soil sequestration rates of tropical riverine wetlands
title_fullStr Carbon stocks and soil sequestration rates of tropical riverine wetlands
title_full_unstemmed Carbon stocks and soil sequestration rates of tropical riverine wetlands
title_sort carbon stocks and soil sequestration rates of tropical riverine wetlands
url http://www.biogeosciences.net/12/3805/2015/bg-12-3805-2015.pdf
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