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It could be argued that in warmer, wetter climes, an increase in resource availability enabled both taxa to co-exist.
In detail, this trend appears to have been highly irregular, with alternating stratigraphical intervals containing indicators of drier and wetter conditions.
In conclusion, the species strongly favours wetter forests.
Higher values of this ratio are associated with drier times, and lower values with wetter times.
It helps to explain why adoption of new varieties is often faster in the wetter areas.
A baseflow regression model predicts that drought mitigation attributed to increased forestation is typically concentrated in the wetter southern watersheds.
Only a wetter-thanaverage period could enable the system to recover.
Patterns of litterfall suggest that the driest site may be slightly more productive than wetter forests.
This relationship appeared in the wetter, southern part of the country.
This created a patch of wet sand with a wetter centre and drier periphery, of about 70 cm x 30 cm (see fig. 2b).
One might expect the topsoil to be drier and the subsoil to be wetter in gaps compared to the understorey.
With the lush food available in the wetter weather the dry matter declined to 17-19%.
Most of the stuff we use is from the warmer, wetter half of the planet where plants grow best.
Any wetter month would therefore have failed to trigger flowering and fruiting.
But, it is difficult to imagine a wetter world in which little of the substantial increase in precipitation falls on forests and agricultural lands.
