Micropropagation of Capparis decidua through In Vitro Shoot Proliferation on Nodal Explants of Mature Tree and Seedling Explants
In vitro clonal propagation of Capparis decidua was achieved using nodal explants from mature trees, and cotyledonary node, cotyledon and hypocotyl explants taken from the seedlings. Explants cultured on MS medium supplemented with BAP showed differentiation of multiple shoots and shoot buds in 4–5 weeks in the primary cultures. The medium with BAP (5 mg/l) was the best for shoot bud proliferation from the nodal as well as seedling explant. Shoot multiplication was best on cotyledonary node. In the nodal explants shoot multiplication was best on medium supplemented with 5 mg/l BAP and after second subculturing further multiplication of shoot buds was highest on the medium containing 3 mg/l BAP. Shoots were separated from mother cultures in each subculturing for rooting. Rooting was best achieved using 1 mg/l IBA in the medium. Rooted plantlets were transferred td earthen pots with garden soil and peat moss mixture.
Totipotency of coleoptile tissue in indica rice (Oryza sativa L. cv. ch 1039)
Embryogenic and non-embryogenic calluses were induced from 3,4,5 and 7d old coleoptile segments of indica rice (Oryza sativa L. cv. CH 1039). Compact, globular, yellow and creamy embryogenic and white friable non-embryogenic callus arose from the cut end and entire length of the coleoptile segments. Murashige and Skoog's (MS) medium supplemented with 2.5mg/1 2,4-D was used as callus induction medium. Plant regeneration from coleoptile segments occurred with the transfer of embryogenic callus to MS basal medium supplemented with 2.0mg/1 BAP and 0.5mg/1 NAA in combination. Average number of regenerated plants from one coleoptile ranged from9.1 to 14.0.Four day old coleoptiles showed the highest frequency of plant regeneration.
AN INTRODUCTION T O THE SOILS OF THE SOUTH-EASTERN PORTION OF THE AUSTRALIAN ARID ZONE
Summary 
 
Seven soil regions, each of which is dominated by soils belonging to one or two great soil groups, are defined and mapped. The outstanding feature is the presence of a variety of soils with widely differing characteristics. The soils are deeper, have more profile differentiation and are finer-extured than those in most-arid regions and are frequently overlain by currently-forming deposits of wind-transported materials. Because the vegetative cover is better developed and there are only small areas of rocky hills and bare rock pediments, water erosion and deposition are not as prominent as in other arid areas.