Leaf-litter decomposition was examined from November 2008 to October 2009 using litter bags in a secondary mangrove forest along the Trat River, eastern Thailand. The study site exhibited three distinct vegetation zones (dominated by
Avicennia,
Rhizophora, and
Xylocarpus spp.) moving inland from the river edge. The decomposition rates (K), indicated by a negative exponential curve, were numerically ranked with the highest,
Avicennia (0.023), at the river edge and decreasing as heading inland through the
Rhizophora (0.020) zone to the lowest decomposition rate at the most inland
Xylocarpus zone (0.014). They were similar to previously reported values for mangrove forests. The amount of residual leaf litter in the Avicennia and Rhizophora zones decreased rapidly during the first 112 days of the trial, whereas that in the
Xylocarpus zone decreased more slowly. Over the remainder of the trial period (total of 362 days), residual leaf litter slowly declined. At the end of the trial, the weight of leaf litter lost was highest in the
Avicennia zone, followed by the
Xylocarpus and
Rhizophora zones. Correspondingly, the C/N ratio of the residual leaf litter decreased rapidly over the first 54 days of exposure time in all three zones, and then stabilized to a slow change after 112 days of exposure onwards. Differences in the amount of leaf litter lost were discussed in terms of causative physical factors such as inundation period and soil temperature. The soil temperature at a depth of 10 cm below the surface was highest in the
Avicennia zone and decreased with increasing distance from the river edge. The relative elevation of the forest floor in the
Avicennia zone at the river edge resulted in the longest period of inundation, which, along with high soil temperature, promoted the decomposition of leaf litter. Additionally, we mentioned the contribution of CO
2 released from litter decomposition through soil respiration of the mangrove forest.
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