Abstract
Defoliation of the mid crown of Douglas-fir trees on Vancouver Island followed the hot, dry summer of 1967. Reddening of foliage in a similar mid crown position occurred on other trees in the spring of 1968. The position of these effects could not be attributed to localized fungus infections, insects, or microclimatic influences. A differential response to moisture stress by affected tissues is thought to have caused the unusual patterns. Other effects are also described.
Publisher
Canadian Science Publishing
Cited by
6 articles.
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