Mycorrhizai associations with some plant species in a soil strip of different successional stages in Egypt

Abstract

In this study, soil and plant samples were collected from a strip of soil comprising four successional stages from the eastern desert plateau to the Nile Valley, Egypt. On one hand, some essential elements [i.e., potassium (K), calcium (Ca), magnesium (Mg), and sulfur (S)] and water contents decreased on transition from the desert soil to the Nile Valley. Soil nitrite content was the highest in Nile Valley soil and decreased toward desert soil. pH values of the soils did not strongly differ and were moderately alkaline. Root colonization with arbuscular‐mycorrhizae (AM) fungi of 33 plant species (11 cultivated and 22 wild) collected from the study area was highest in eastern desert plateau and decreased toward the Nile Valley. Mycorrhizai spore counts reflected the root colonization data. The decrease in mycorrhizai colonization was explained on the basis of difference in soil porosity, soil water contents, and toxicity of nitrite. Contents of K, Ca or Mg in some species were increased by increasing the colonization percentage of roots by AM fungi. Increasing the infection percentage of roots decreased or maintained the ratio of Na K+Ca+Mg (in meq) in the shoots of investigated plants. The contents of chlorophyll, soluble sugars, and protein significantly increased as a result of increasing colonization value. Also, mycorrhizal root colonization improved the water status of most plant species. These results suggest that increasing infection by AM fungi in the newly reclaimed soil may enable the plants to maintains its internal water status and mineral balance through decreasing the ratio of distressing ions to the nutrient ones.

Notes

Corresponding author (present address: Institute of Plant Nutrition, Südanalage 6, 35390 Giessen, Germany).