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European Journal of Scientific Research - EuroJournals

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Germination Studies in Selected Native Desert Plants <strong>of</strong> Kuwait 340<br />

and Phragmites australis, soaking <strong>of</strong> seeds in GA3 solution for 24 hrs increased the<br />

germination from germination by 64 and 86%, respectively. While hot water treatment<br />

improved the germination in Asteragalus sieberri seeds, KNO3 was more effective than<br />

heat treatment in increasing the germination <strong>of</strong> Citrullus colocynthis seeds.<br />

Key words: Revegetation, propagation, biodiversity conservation, gibberellic acid,<br />

stratification, seed dormancy<br />

1. Introduction<br />

Extreme aridity <strong>of</strong> the climate, over grazing, Gulf war activities and other human activities have led to<br />

a significant loss <strong>of</strong> native vegetation cover, increased mobility <strong>of</strong> sand particles and the frequent<br />

occurrences <strong>of</strong> dust storms in the Kuwaiti desert. Encroachment <strong>of</strong> agricultural lands, roads and other<br />

infrastructure by wind blown sand has also become a serious problem in Kuwait (Abdulwahid, 1979;<br />

Abolkhaire, 1981). Because the majority <strong>of</strong> native plants in Kuwait are annuals, uncertainties <strong>of</strong><br />

climate have a major influence on their germination, establishment, flowering and seed production.<br />

The lack <strong>of</strong> sufficient native seed stocks has been the main bottleneck in all restoration programs in the<br />

region including Kuwait (Peacock et al. 2003). Under normal conditions, seeds get buried in soil and<br />

remain dormant for several years until sufficient amount <strong>of</strong> rainfall percolate into the soil to initiate<br />

germination and new growth.<br />

In nature, germination <strong>of</strong> fresh seeds in desert species is usually prevented by adverse climatic<br />

conditions (drought and extreme temperatures). Hard seed coats and presence <strong>of</strong> high levels <strong>of</strong> growth<br />

inhibitors also allow them to remain dormant during unfavorable growing conditions. Dormancy is<br />

normally broken when seeds after they have absorbed sufficient moisture are exposed to mild<br />

temperatures. The availability <strong>of</strong> sufficient moisture in the soil is also necessary to leach out growth<br />

inhibitors present in the seed completely, a precondition to be fulfilled for successful germination<br />

(Bryant, 1985).<br />

Efficient propagation and establishment techniques that are crucial for both conservation <strong>of</strong><br />

native species and large-scale revegetation programs are currently not available. In view <strong>of</strong> these facts,<br />

studies were conducted to determine the effects <strong>of</strong> seed treatments on germination in five main native<br />

desert species (Cyperus conglomeratus, Citrullus colocynthis, Moltkiopsis ciliata, Astragalus sieberri<br />

and Phragmits australis).<br />

2. Materials and Methods<br />

2.1. Climate and Soil <strong>of</strong> Kuwait<br />

Geographically, Kuwait occupies approximately 17,800 km 2 <strong>of</strong> the northwestern part <strong>of</strong> the Arabian<br />

Gulf, between 28º30’ and 30º05’N, and 46º33’ and 48º30’E It is bounded on the South by Saudi<br />

Arabia, on the North and west by Iraq, and on the East by the Arabian Gulf.(Annual Statistical<br />

Abstract, 1998). Kuwait’s climate is characterized by harsh summers and mild winters. Temperature<br />

extremes are high, with means during the warmest and coolest months ranging between 46.2ºC and<br />

6.9ºC (Annual Statistical Abstract, 1998). Winter brings occasional frost. Rainfall is minimal, not<br />

exceeding 115 mmyr -1 , but evaporation is very high, averaging 14.1 mm.d -1 . The relative humidity is<br />

low, and strong, dry and hot, northwesterly winds prevail during summer, particularly in June and July.<br />

Kuwait’s soils are sandy in texture, alkaline, high in calcareous materials (CaCO3) and low in organic<br />

matter and plant nutrients. Underground water resources are limited and brackish in nature with total<br />

dissolved solids (TDS) concentrations ranging from 3.0 to 10.0 g.L -1 .

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