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The canopy is very open causing exposed conditions within the forest, and dead wood above the forest floor is usually very dry.
They found no difference in the amount of dead wood by decomposition class among life zones.
To estimate the annual dead wood net accumulation, all quadrats and transects were resampled again 1 y later.
Dead wood in the form of snags and dead-wood patches a ccounted for approximately 40% of all foraging observations.
Decomposition state (solid, partially decomposed, fully decomposed) was noted for each piece of fallen dead wood.
Dead wood is an important component of forest ecosystems.
The amount of total dead wood was 3- to 14-fold greater in burned forests compared with unburned forests.
The decomposition rates of dead wood can not be understood without information about the saprotrophic organisms involved.
After three years, the two sole survivors were seedlings which had established on dead wood.
The molluscan infauna of dead wood was also included, but no sieving for soil infauna was attempted.
This may provide a basis for understanding the possible slower turnover rates of dead wood in wetter life zones.
The turnover rate of dead wood was lowest in the moist forest life zone where climatic conditions seemed to be most favourable for decomposition.
Also, lianas may entangle many pieces of dead wood in the canopy and delay their fall to the ground.
These are mainly generalist parasitoids which use their very long ovipositors to attack hosts living deep in dead wood.
The moisture content of the dead wood in the moist and especially the wet forest could be too high for many wood-rotting fungal species to survive.
