By Abraham Weinstein, Department of Agronomy & Natural Resources, The Volcani Center, Bet Dagan.
Casuarinas are widespread in Israel along roadsides and used as windbreaks, and in parks, small wood lots and forest plantations.
Casuarinas planted in Israel were found to be mixtures of C. cunninghamiana and C. glauca, and subsequent indiscriminate gathering of seeds, caused by lack of differentiation between the two species within plots, resulted in a continuation of mixed plots. Since C. cunninghamiana and C. glauca flower at about the same time the possibility of hybridization and back-crossing was recognized.
There was considerable interest in testing additional species under a wide range of ecological conditions, in order to fully utilize the potential of casuarinas for afforestation and reforestation. Therefore, it was necessary to study a large number of old plots and to establish new ones, in order to study the adaptability of the various species for afforestation purposes. Introduction and forest plots were studied in areas from Even Izhak in the north to Nir Izhak in the western Negev, and it was established that 17 species of casuarinas are grown in Israel. Most of these trees are Casuarina cunninghamiana, C. glauca, C. cristata and Allocasuarina leumannii.
C. cunninghamiana, C. glauca and their hybrids grow well in Israel on the red loamy sand and brown rendsina soils in the Mediterranean region, where mean annual rainfall is 400-650 mm.
C. glauca can thrive in drier regions which receive 200-300 mm mean annual rainfall, especially in depressions on sandy loam, loess, and loessial light brown soils.
C. cristata grows well in the center and south (western and northern Negev) of Israel, in conditions of 220-250 mm mean annual rainfall on loessial light brown clay loam, and on steep slopes with brown lithosol.
Allocasuarina luehmannii grows well in the center and south of the country, on both plains and hills, in conditions of 200-600 mm mean annual rainfall, on brown rendzina, on brown lithosols, on moderate slopes covered with loessial serozem and where loessial light brown clay loam grades intoloessial serozem.