Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 12, issue 12
Biogeosciences, 12, 3805–3818, 2015
https://doi.org/10.5194/bg-12-3805-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 12, 3805–3818, 2015
https://doi.org/10.5194/bg-12-3805-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 23 Jun 2015

Research article | 23 Jun 2015

Carbon stocks and soil sequestration rates of tropical riverine wetlands

M. F. Adame1, N. S. Santini2, C. Tovilla3, A. Vázquez-Lule4, L. Castro5, and M. Guevara6 M. F. Adame et al.
  • 1Australian Rivers Institute, Griffith University, Nathan, 4111, QLD, Australia
  • 2Coastal Plant Laboratory, The School of Biological Sciences, The University of Queensland, St Lucia, 4072, QLD, Australia
  • 3Colegio de la Frontera Sur, Tuxtla Gutiérrez, Chiapas, Mexico
  • 4Comisión Nacional para el Conocimiento y Uso de la Biodiversidad (CONABIO), Mexico City, Mexico
  • 5Comisión Nacional de Áreas Naturales Protegidas, Chiapas, Mexico
  • 6Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USA

Abstract. 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 ± 63.6 MgC ha−1, respectively) were higher than those of marshes (336.5 ± 38.3 MgC ha−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 744–912 MgC ha−1) compared to the intermediate and lower estuary (range 537–1115 MgC ha−1) probably as a result of a highly dynamic coastline. Soil C sequestration values were 1.3 ± 0.2 MgC ha−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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Riverine wetlands of the south Pacific coast of Mexico had large ecosystem C stocks (784.5 MgC ha-1 for mangroves, 722.2 MgC ha-1 for peat swamps, and 336.5 MgC ha-1 for marshes). Long-term soil C sequestration values in mangroves were 1.3 ± 0.2 MgC ha-1yr-1. C stocks, and soil nitrogen stocks were in general larger for mangroves in the upper than in the lower estuary.
Riverine wetlands of the south Pacific coast of Mexico had large ecosystem C stocks (784.5 MgC...
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