4.4 Article

Impacts of Mauritia flexuosa degradation on the carbon stocks of freshwater peatlands in the Pastaza-Maranon river basin of the Peruvian Amazon

Journal

Publisher

SPRINGER
DOI: 10.1007/s11027-018-9809-9

Keywords

Amazon basin; Forest degradation; River dynamics; Peat swamp forest; Soil carbon

Funding

  1. US Department of Agriculture, Forest Service (FS), Washington Office
  2. FS International Programs

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Tropical peat swamp forests (PSF) are characterized by high quantities of carbon (C) stored as organic soil deposits due to waterlogged conditions which slows down decomposition. Globally, Peru has one of the largest expanse of tropical peatlands, located primarily within the Pastaza-Maranon river basin in the Northwestern Peru. Peatland forests in Peru are dominated by a palm speciesMauritia flexuosa, and M. flexuosa-dominated forests cover similar to 80% of total peatland area and store similar to 2.3Pg C. However, hydrologic alterations, land cover change, and anthropogenic disturbances could lead to PSF's degradation and loss of valuable ecosystem services. Therefore, evaluation of degradation impacts on PSF's structure, biomass, and overall C stocks could provide an estimate of potential C losses into the atmosphere as greenhouse gases (GHG) emissions. This study was carried out in three regions within Pastaza-Maranon river basin to quantify PSF's floristic composition and degradation status and total ecosystem C stocks. There was a tremendous range in C stocks (Mg Cha(-1)) in various ecosystem poolsvegetation (45.6-122.5), down woody debris (2.1-23.1), litter (2.3-7.8), and soil (top 1m; 109-594). Mean ecosystem C stocks accounting for the top 1m soil were 400, 570, and 330Mg Cha(-1) in Itaya, Tigre, and Samiria river basins, respectively. Considering the entire soil depth, mean ecosystem C stocks were 670, 1160, and 330Mg Cha(-1) in Itaya, Tigre, and Samiria river basins, respectively. Floristic composition and calcium to Magnesium (Ca/Mg) ratio of soil profile offered evidence of a site undergoing vegetational succession and transitioning from minerotrophic to ombrotrophic system. Degradation ranged from low to high levels of disturbance with no significant difference between regions. Increased degradation tended to decrease vegetation and forest floor C stocks and was significantly correlated to reduced M. flexuosa biomass C stocks. Long-term studies are needed to understand the linkages between M. flexuosa harvest and palm swamp forest C stocks; however, river dynamics are important natural drivers influencing forest succession and transition in this landscape.

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