4.6 Article

The presence of peat and variation in tree species composition are under different hydrological controls in Amazonian wetland forests

Journal

HYDROLOGICAL PROCESSES
Volume 36, Issue 9, Pages -

Publisher

WILEY
DOI: 10.1002/hyp.14690

Keywords

Amazon basin; climate change; ecohydrology; electrical conductivity; Pastaza-Maranon Foreland Basin; peatland

Funding

  1. Gordon and Betty Moore Foundation [5349]
  2. Natural Environment Research Council [NE/R000751/1]

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This study investigates the ecohydrological controls of the peat-forming wetland forests in northern Peruvian Amazonia, by measuring water table depth, pH, and electrical conductivity. The results show that flood levels and pH are related to tree species composition, while the presence of peat is linked to maximum water table depth.
The peat-forming wetland forests of Amazonia are characterized by high below-carbon stocks and supply fruit, fibres and timber to local communities. Predicting the future of these ecosystem services requires understanding how hydrological conditions are related to tree species composition and the presence, or absence, of peat. Here, we use continuous measurements of water table depth over 2.5 years and manual measurements of pore-water pH and electrical conductivity to understand the ecohydrological controls of these variables across the large peatland complex in northern Peruvian Amazonia. Measurements were taken in permanent forest plots in four palm swamps, four seasonally flooded forests and four peatland pole forests. All trees >= 10 cm diameter were also measured and identified in the plots to assess floristic composition. Peat occurs in eight of these twelve sites; three seasonally flooded forests and one palm swamp are not associated with peat. Variation in tree species composition among forest types was linked to high flood levels (maximum flooding height) and pH: seasonally flooded forests experience high flood levels (up to 3.66 m from the ground surface) and have high pH values (6-7), palm swamps have intermediate flood levels (up to 1.34 m) and peatland pole forests experience shallow flooding (up to 0.28 m) and have low pH (4). In contrast, the presence of peat was linked to variation in maximum water table depth (i.e. the depth to which the water table drops below the ground surface). Surface peat is found in all forest types where maximum water table depth does not fall >0.55 m below the ground surface at any time. Peat formation and variation in tree species composition therefore have different ecohydrological controls. Predicted increases in the frequency and strength of flooding events may alter patterns of tree species composition, whereas increases in drought severity and declines in minimum river levels may pose a greater risk to the belowground carbon stores of these peatland ecosystems.

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