Manuscript accepted on : 02 November 2011
Published online on: 28-12-2011
Preliminary Study of Soil Algae of Protected Saja Mother Elegans, Mother Elegans, Saudi Arabia
Hend Alwathnani
Department of Botany and Microbiology, College of Science, King Saud University, Box 2455 Riyadh - 11 451 Saudi Arabia
Corresponding Author E-mail: wathnani@ksu.edu.sa
ABSTRACT: Saja Mother Elegans area in Riyadh city of Saudi Arabia received the first study regarding to soil algae identification. It is a protected area under the control of the Saudi wildlife Commission (SWC). Description of the samples sites and the distribution of each algae are given. A total of 21 species of algae were found in 10 sites from Saja Mother Elegans Um Al-Rimth 21 species of algae, 14 Cyanophyta, 5 Chlorophyta, one Euglenophyta and one Xanthophyta were isolated and identified. Most of the recorded algae were mainly related to Cyanophytes with the most common species such as Oscillatoria, Microcoleus, Nostoc. Species of algae in this study were identified only to the genus. Results from this study indicate that before meaningful comparisons between Saudi soil algae can be made, more studies must be conducted.
KEYWORDS: Economical- social factors; Development; Wood cultivation; Spruce; Spruce cultivator
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Introduction
Microbiotic crusts, also known as biological soil crusts, are major components of most desert ecosystems in the world. They occur on most soil types where sunlight can reach the soil surface. However it appears to be less developed in the hottest and driest deserts, but they are typical in that they are colonized by many filamentous species of cyanobacteria (Johansen et al., 2001; Flechtner et al., 1998). Soil algal crusts play an important role in the integration and stability of arid and semi-arid regions worldwide, this role represented in many aspects of the ecosystem sustainability, including the interactive components that rely on each other to keep soil vitality. One of the most important roles of these crusts is building up soil ecosystem to accomplish diversity and increment of many macrobiotic soil members. Algae, fungi, lichens and mosses are colonized together forming soil algal crusts, within which blue-green algae found abundantly (West, 1990; Belnap and Gardner 1993; Belnap, 1994). In general, the factors that determine algae species abundance are light, temperature, water availability, soil texture, and PH (Karnieli et al., 1999; Purcell et al., 2006). Biological soil crust including Cyanobacteria species serve several important roles in the desert, chiefly soil aggregation and protection, nitrogen fixation, and varied effects on vascular plant establishment (Nishaa et al., 2006; Prasanna et al., 2008). Their architecture could be preserved among regions aside from low infiltration capacity and soil erosion caused by pastoral nomadism; this mechanical factor in addition to the chemical and physical factors could maximize algal colonization in such hima areas, considering the rarity of sharp climatic changes (Tiwari et al., 2005). Although many studies of soil algae have been established from different soils around the world, very few papers based on taxonomic source, were published dealing with soil algal of the Saudi Arabia Soil. Arif studied saline soil of Al-Shiggah in Al-Qaseem in 1992 and he reported six species of blue-green algae and five green algae. Al-Fredan and Fathi in 2007 identified fifty two genera of algae of Al-Hasa region. New Algae species for the Saudi Arabian flora were recorded from South Western region of Saudi Arabia by Arif and El- Syed in 1997.
The present study represents the first attempt to identify algae species from a protected area Saja Mother Elegans of Riyadh City. For the fulfillments of the kingdom of Saudi Arabia government commendation to sustain terrestrial and marine wildlife, Saudi wildlife Commission (SWC) was established In 1986, by Royal Decree M/22 (Saudi wildlife Commission, 2011). SWC has been developing many projects for the purpose of confinement of specific areas all over the kingdom; so called protected area or hima. As its major goal is preservation, protection and development of wildlife to ensure an ecological balance in the Kingdom (Saudi wildlife Commission, 2011; Abuzinada, 2003), these areas conserve the integrity and stability of arid and semi-arid regions maintaining their characteristics, where microbiotic algal crusts are protected from destroying caused by soil erosion and lifelessness (Alwelaie, 1994; Abuzinada, 2003).
Material and Methods
Site Description
Saja Mother Elegans northwest an area of 7190 square kilometers characterized by the average plant cover help to save the genetic origins of some mammals, birds and reptiles endemic and rare in there serve environments vary between low hills a few spikes, and the exposed gravel plains and valleys dominated by plants Alosmam and acacia trees, Acacia gerrardii , Artemisia monosperma, Citrullus colocynthis, Rhazya stricta, Maerua crassifolia, and Lycium shawii,.
The Kingdom of Saudi Arabia has a desert climate with fluctuation in temperature and humidity, as temperature increase at daytime and drop at night, while humidity fluctuates between coastal and central regions. Al Zawad 2008. Saja Mother Elegans protected area lies between the central and the eastern providence of Saudi Arabia. Central regions show relatively hot barren summer, cold rainy winter from the month of October to May. This area acquired several characteristics of the Najd plateau, where many landform units present including plateau, dune areas, shallow valleys, and open, undulating steppe desert (Sallam, 2002). The principle soil habitat consists of mixed sand and gravel plain. Upon analysis; soil sectors was found of low organic content, highly calcareous, very low Gypsum, and mostly non-saline to slight salinity medium (Sallam, 2002). Sectors for soil sampling was taken from areas that is suggested to maintain good microbiotic crust cover, where silt content and electrical conductivity is sufficient, maintaining the alkalinity of soil system, aside from soil exposed to heavy grazing in addition to soil erosion and increased aridity.
Field Method
Samples Collection
Soil samples were provided from the regions of the proposed study with approval of Saudi wildlife Commission (SWC) committee, Samples used in this study were all collected on 2010. Sample contained the most well developed microbiotic crusts. Site photographs, soil chemistry, and cover categories of vascular plants will be provided in this paper. 10 samples were taken from and around Saja Mother Elegans area, where each region was divided into 10 sectors within which sub-samples were taken. Sample were collected only once during December, 2010. Selection of these samples was based on areas with visible algae crusts as well as in undisturbed area.
Samples were collected using sterile scoops then transferred into small polyethylene bags. The soil samples were stored to the lab temperature. Duplicates of the samples were made for determination of soil physical and chemical parameters from the assigned sites. Each site was marked permanently by pounding an iron rod into the ground. Climatic data was compiled for the area from the historical data (1985 – 2008) collected between 35 East and 43 East longitudes and 25 North and 33 North latitudes, referring to meteorological units in Qasim and Hail cities.
Laboratory Methods
Isolation and Culture
Culture, isolation, and identification of algae were performed using dilution techniques with two series of cultures was sat up for each sample using two different media; Z-8 media and Chu’s10 media (Gerloff et al., 1950; Stein, 1979). Soil samples were crushed and mixed to produce homogenous samples. Subsamples (1.0 g) were dilution plated in triplicate on agar –solidified Z-8 medium (Carmichael 1986), as described in Flechtner et al., (1998), and were incubated at 20 °C under fluorescent light (200 μΕˉ¹ cmˉ¹) with a 16 h light / 8 h dark photoperiod until good growth was obtained (3-6 weeks). Regularly examined for visible algal growth after 2 weeks of incubation, then visible isolates was plated in triplicate on agar solidified media. All algae species were identified by direct microscopic examination. Algae were identified based on the morphological characteristics.
Soil Analysis
Soil analysis was conducted at the soil testing unit of Food and Agricultural Sciences college at King Saud University, including soil texture, soil organic matter, nitrate, ammonia, phosphorous, calcium, magnesium, sodium, potassium, sodium, electrical conductivity, and pH. Sub-samples within the 10 assigned sites were mixed to be representative for each protected area.
Results
Physical and Chemical Analysis of Soil
Physico-chemical characteristics of the selected 10 sites around Saja Mother Elegans are presented in Table 1. On average, soil samples showed sandy texture (91.3%), with neutral to alkaline pH (7.5), and relatively high electrical conductivity. Moreover, chemical analysis revealed that the selected soils had Calcium-Sodium cationic, and Sulfate-Chloride anionic structure. With significant organic matters, low phosphorus, but high Iron, Potassium and nitrogen content. On the other hand, elevation in cationic, anionic structure, and accordingly high electrical conductivity was noticed within area 7 and 8.
Table 1a: Soil physical and chemical properties of Saja Mother Elegans sites.
SP % | pH | EC | Cations (meq/l) | Anions(meq/l) | Partical size % | Texture class | CaCO3
% |
|||||||||
Ca2+ | Mg2+ | Na+ | K+ | HCO3– | CO3= | Cl– | SO4= | Sand | Silt | Clay | ||||||
1 R | 24.0 | 7.2 | 2.9 | 31.5 | 4.5 | 5.5 | 0.8 | 1.3 | 0.0 | 2.3 | 26.3 | 92.7 | 2.0 | 5.3 | sand | 1.6 |
2 R | 22.6 | 7.3 | 20 | 77.5 | 16.5 | 131.9 | 2.2 | 5.0 | 0.0 | 220.0 | 28.0 | 89.7 | 3.0 | 7.3 | sand | 1.4 |
3 R | 20.0 | 7.8 | 2.47 | 8.3 | 2.3 | 11.0 | 1.3 | 2.3 | 0.0 | 13.3 | 4.6 | 92.7 | 2.0 | 5.3 | sand | 1.4 |
4 R | 22.0 | 7.8 | 1.05 | 7.5 | 1.0 | 4.9 | 0.6 | 3.8 | 0.0 | 3.8 | 3.8 | 89.7 | 2.0 | 8.3 | sand | 1.4 |
5 R | 21.6 | 7.7 | 2.45 | 22.0 | 6.0 | 5.3 | 0.8 | 4.0 | 0.0 | 4.5 | 4.1 | 90.7 | 4.0 | 5.3 | sand | 3.9 |
6 R | 20.3 | 7.5 | 4.27 | 29.0 | 3.0 | 19.8 | 1.7 | 5.0 | 0.0 | 21.0 | 23.7 | 92.7 | 2.0 | 5.3 | sand | 1.1 |
7 R | 18.6 | 7.0 | 94.8 | 280.0 | 65.0 | 1072.0 | 6.6 | 1.3 | 0.0 | 1412.0 | 13.1 | 91.7 | 2.0 | 6.3 | sand | 0.8 |
8 R | 21.6 | 7.6 | 67.3 | 160.0 | 49.0 | 625.0 | 4.4 | 4.0 | 0.0 | 800.0 | 15.6 | 92.7 | 2.0 | 5.3 | sand | 0.6 |
9 R | 24.0 | 7.6 | 11.6 | 30.0 | 3.0 | 66.0 | 1.7 | 3.0 | 0.0 | 110.0 | 8.5 | 92.7 | 2.0 | 5.3 | sand | 1.2 |
10 R | 23.0 | 7.4 | 1.3 | 4.0 | 1.0 | 6.2 | 0.5 | 3.0 | 0.0 | 5.0 | 2.5 | 87.7 | 5.0 | 7.3 | loamy sand | 2.4 |
Table 1b: Soil physical and chemical properties of Saja Mother Elegans sites.
Cust. No | Available nutrients (mg/kg) | O.M % | ||||||
N | P | K | Fe | Mn | Zn | Cu | ||
1 R | 9.8 | 0.8 | 85.7 | 10.1 | 1.2 | 0.34 | 0.6 | 1.85 |
2 R | 42.0 | 1.3 | 177.0 | 10.4 | 1.4 | 0.26 | 0.6 | 1.57 |
3 R | 21.0 | 2.1 | 167.4 | 10.1 | 1.4 | 0.29 | 0.6 | 1.54 |
4 R | 129.5 | 1.9 | 135.7 | 13.4 | 2.4 | 0.34 | 0.6 | 1.63 |
5 R | 10.7 | 3.6 | 107.4 | 10.0 | 2.7 | 0.40 | 0.8 | 1.25 |
6 R | 39.2 | 3.7 | 167.4 | 11.0 | 4.0 | 0.40 | 0.6 | 1.06 |
7 R | 53.2 | 1.0 | 119.1 | 10.4 | 3.2 | 0.66 | 0.6 | 1.05 |
8 R | 144.2 | 1.8 | 63.6 | 11.2 | 4.2 | 0.35 | 0.6 | 0.85 |
9 R | 113.4 | 2.7 | 96.3 | 10.6 | 1.6 | 0.32 | 0.6 | 0.91 |
10 R | 183.4 | 2.3 | 92.7 | 12.2 | 1.7 | 0.36 | 0.6 | 0.81 |
Figure 1: Saja Mother Elegans protected area suited at the center of Saudi Arabia. |
Identification of Algae Isolates
Visible algal growth was observed after three weeks of incubation, total of 21 algal genera was isolated and identified from the investigated soils (Table 2), belonging to 4 algal divisions which predominated with Cyanophyta (14 genera) followed by Chlorophyta (5 genera), in addition to one genera from each of Euglenophyta and Xanthophyta. Modified Chu’s.10 media had shown productivity toward all divisions, while Z8 media was suitable media only for Cyanophyta and Chlorophyta.
Table 2: List of algae species identified by the use of tow algae media (Z8 an Chu’s no. 10) in the selected sites of Saja Mother Elegans protected area in the present study.
Division | Genus | R1 | R2 | R3 | R4 | R5 | R6 | R7 | R8 | R9 | R10 | ||||||||||
Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | Z8 | Chu 10 | ||
Cyanophyta | Anabaena | + | + | + | + | + | + | + | + | + | |||||||||||
Calothrix | + | ||||||||||||||||||||
Chroococcus | + | + | + | + | + | + | + | + | |||||||||||||
Gleothece | + | + | |||||||||||||||||||
Leptolyngbya
|
+ | ||||||||||||||||||||
Microcoleus | + | + | + | + | + | + | + | + | + | + | + | + | |||||||||
Lyngbya | + | ||||||||||||||||||||
Nodularia | + | + | + | + | |||||||||||||||||
Nostoc | + | + | + | + | + | + | + | + | + | + | + | + | + | ||||||||
Oscillatoria | + | ||||||||||||||||||||
Phormedium | + | + | + | + | + | + | + | + | + | + | + | + | + | + | |||||||
Schixothrix | + | + | |||||||||||||||||||
Scytonema | + | ||||||||||||||||||||
Tolypothrix | + | + | + | ||||||||||||||||||
Euglenophyta | Euglena | + | |||||||||||||||||||
Xanthophyta | Tribonema | + | |||||||||||||||||||
Chlorophyta | Chlaymydomonas | + | + | ||||||||||||||||||
Chlorella | + | + | + | + | |||||||||||||||||
Cosmarium | + | ||||||||||||||||||||
Dunaliella | + | + | + | ||||||||||||||||||
Pandorina | + |
The most common soil algal genera present along different media and through all over the studied region were the ones that belong to Cyanobacteria (Anabaena, Microcoleus, Chroococcus, Nostoc and Phormedium), followed by (Calothrix, Gleothece, Leptolyngbya, Lyngbya, Nodularia, Oscillatoria, Schixothrix, Scytonema and Tolypothrix). In addition to genera identified among other divisions: Chlorophyta (Chlaymydomonas, Chlorella, Cosmarium, Dunaliella and Pandorina), Euglena and Tribonema that belong to Euglenophyta and Xanthophyta respectively.
Figure 2: The principle soil habitat of the described areas consists of mixed sand and gravel plain. |
Discussion
Algal colonization within soil biological crusts sustain ecosystem integrity for various soil communities, especially in arid and semi-arid regions being deficient in nitrogen fixing bacteria as reported by many studies (Loftis and Kurtz, 1980), our physio-chemical parameters of the selected region had shown little silt with sandy calcified texture; alkaline pH; relatively high electric conductively and nitrogen contents, with decline in organic matter and other nutrients as phosphorous, these soil characteristics is in agreement to that reported for Najd plateau (Sallam, 2002). Diverse forms of green and blue green algae was reported in our study, confirming the fact that these species characterize arid and semiarid regions (Hahn and Kusserow, 1998; Chun-Xiang et al., 2002; Nayak et al., 2004), where aggregation and colonization happened mainly within saline to alkaline conditions with good salt content. In accordance to climatic conditions and sampling time, at this time of the year, the region exhibit significant humidity with drop in temperature (5 – 26 ºC), interestingly this has been positively correlated with algal diversity.
High nitrogen content was observed in the studied soils confirming the believes of the effective role of cyanobacteria in nitrogen fixation, thus, sustaining many macrobiotic soil members (Hahn and Kusserow, 1998; Singh et al., 2008).
Four algal divisions were reported in the subjected soils. Among the detected genera, Species of Cyanobacteria were the most abundant and dominant within the selected sectors, the result mostly agree with the study of Al-Fredan and Fathi in 2007 .Therefore, no correlation was assessed between Cyanobacterial distribution and physyco-chemical parameters within the selected 10 sites, although, some sites exhibited high electrical conductivity and salt contents, this finding support the suggestion of Cynobacterial adaptation in fluctuated desert conditions, to tolerate extremely dry and at the same time, saline habitat (Wierzchos et al., 2006).
Studying algal species emanating all over Saudi Arabia; coastal regions, peninsulas, oasis, lakes, rain-fed pools and rice fields, have been screened for algal distribution, sufficient data was presented by studying aquatic ecosystems in several areas: rain-fed pool at Al-Kharj (Al-Homaidan and Arif, 1997), Asir (Mohammed and Al-Shehri, 2008), gizan coastal region ( Basahy, 1993) , Jedda (Al-Amoudi et al., 2009), Al-Hasa oases (Fathi and Al-Kahtani, 2009). Phycological analysis in these studies have been shown a notable diversity of algal groups including; Chlorophyta, Cyanophyta and Euglenophyta (Fathi and Al-Kahtani, 2009). most of the recorded algae were mainly related to cyanophytes within the regarded regions such as Oscillatoria, Chroococcus, Microcoleus, Pseudanabaena, Nostoc, Aphanothece, and Pannus spp. (Al-Homaidan and Arif, 1997; Mohammed and Al-Shehri, 2008). Although These results was obtained within aquatic habitats in Saudi Arabia, there is some concordance with that recorded in our study. Taking in consideration the ecological discrepancy of both environments, we can conclude that seasonality could retain some characteristics of aquatic habitats that affect algal groups development in semi-arid areas (Ostergaard et al., 1985; Romo and Miracle, 1993; Dokulil and Teubner, 2000).
Furthermore, algal composition found in our study have been shown the same pattern of that in world deserts (Wierzchos et al., 2006; Bhatnagar et al., 2005; Jafari et al., 2004; Rios et al., 2004; Pichel et al., 2001). It was revealed that spp. of Anabaena, Chroococcus, Nostoc and Phormedium are the most widely distributed algae in the sampling sites, in addition (Calothrix, Gleothece, Leptolyngbya, Lyngbya, Nodularia, Oscillatoria, Schixothrix, Scytonema and Tolypothrix). Chlorophyta, Euglenophyta and Xanthophyta was observed to less extent, periodical sampling should be obtained from the studied area within different seasons, in order to characterize patterns of algae colonization, and rule out overlapping factors affecting genus diversity.
Acknowledgment
The study was supported by the Deanship of Scientific Research Center, King Saud University; I also thank the College of Science Research Center, King Saud University, Saudi Arabia, for support.
References
- Abuzinada AH. (2003). The role of protected areas in conserving biological diversity in the kingdom of Saudi Arabia. Journal of Arid Environments. 54: 39–45.
- Al-Fredan, M.A. and A. A. Fathi. (2007). Preliminary survey of edaphic algae in Al-Hasa region, Saudi Arabia. Pakistan Journal of Biological Science 10 (18): 3210-3214.
- Al-Amoudi OA, Mutawie HH, Patel AV, Blunden G. (2009). Chemical composition and antioxidant activities of Jeddah corniche algae, Saudi Arabia. Saudi Journal of Biological Sciences. 16: 23-29.
- Al-Homaidan AA , Arif IA. (1998). Ecology and bloom-forming algae of a semi-permanent rain-fed pool at Al-Kharj, Saudi Arabia. Journal of Arid Environments. 38: 15-25.
- Al-Kahtani MA, Youssef AM, Fathi AA. (2007). Ecological studies on Al-Khadoud spring, Al-Hassa, Saudi Arabia. Pakistan Journal of Biological Sciences. 10(22):4063-8.
- Al Zawad FM. Impacts of Climate Change on Water Resources in Saudi Arabia. Presidency of Meteorology and Environment. The 3rd International Conference on Water Resources and Arid Environments. (2008) and the 1st Arab Water Forum.
- Alwelaie AN (1994). Protected areas in Saudi Arabia: Sustainable use of natural resources. GeoJournal. 34: 4:383-392.
- Arif I. A., Algae from the saline soils of Al-Shiggah in Al-Qaseem, Saudi Arabia
- Journal of arid environmentS 1992, vol. 22, no4, pp. 333-338 (14 ref.)
- Arif I. A., and A.M.A. El-Syed (1997). Edaphic properties and soil Cyanobacteria of South Western Saudi Arabia.Qatar Univ. Sci. J. 17 (2):281-291.
- Basahy AY (1994). Water chemistry of hot springs in Gizan area of Saudi Arabia. J. King Saud Univ.: Sci. 6(1):23-29.
- Belnap J (1994). Potential role of cryptobiotic soil crust in semiarid rangelands. In: Monsen, S.B., and S.G. Kitchen, eds. Proceedings_Ecology and Management of Annual Rangelands. General Technical Report INT-GTR-313. USDA Forest Service, Intermountain Research Station, Ogden, UT. Pages 179-185.
- Belnap J, Gardner JS (1993). Soil microstructure of the Colorado Plateau: the role of the cyanobacterium Microcoleus vaginatus. Great Basin Naturalist. 53: 40-47.
- Bhatnagar A, Bhatnagar. M. (2005). Microbial diversity in desert ecosystems. Current Sci. 89: 91-100.
- Carmichael, W.W. (1986). Isolation, culture, and toxicity testing of toxic freshwater Cyanobacteria (blue-green algae). Pages 1249–1262 in V. Shilov, editor, Fundamental research in homogenous catalysis. Volume 3. Gordon & Breach, New York, NY.
- Chun-Xiang HU, Yong-Ding IU, Delu Z, Zebo H, Paulsen BS. (2002). Cementing mechanism of algal crusts from desert area. Chinese Science Bulletin, 47(16): Pp 1361.
- Dokulil M, Teubner K. (2000). Cyanobacterial dominance in lakes. Hydrobiologia. 438:1–12.
- Flechtner, V.R., J.R. Johansen, and W.H. Clark (1998). Algal composition of
- microbiotic crusts from the central desert of Baja California, Mexico. Great Basin Naturalist 58:295–311.
- Gerloff GC, Fizgerald GP, skoog F (1950): The isolation, purification and culture of blue-green algae. Amer. J. Bot. 37:216-218.
- Hahn A, Kusserow H, (1998). Spatial and temporal distribution of algae in soil crusts in the Sahel of W Africa: Preliminary results. Willdenowia, 28: 227-238. 1998.
- Jafari M, Tavili A, Zargham N, Heshmati GA, Zare Chahouki MA, Shirzadian S, Azarnivand H, Zehtabian GR, Sohrabi M (2004). Comparing Some Properties of Crusted and Uncrusted Soils in Alagol Region of Iran. Pak. J. Nutr. 3: 273-277.
- Johansen, J.R., and L.E. Shubert (2001). Algae in soils. Nova Hedwigia 123:297–306.
- Karnieli A, Kidron GJ, Glaesser C, Ben-Dor E (1999). Spectral Characteristics of Cyanobacteria Soil Crust in Semiarid Environments. Remote Sensing of Environment. 69: 1: 67-75.
- Loftis SG, Kurtz EB (1980). Field studies of inorganic nitrogen added to semiarid soils by rainfall and blue-green algae. Soil Sci. 129: 150-155.
- Mohamed ZA, Al-Shehri AM (2008). Cyanobacteria of surface and ground waters in Asir region with new records to Kingdom of Saudi Arabia. JKAU: Sci. 20(2):113-129.
- Nayak S, Prasanna R, Dominic TK, Singh PK (2004). Effect of BGA-Azolla biofertilizers on nitrogen fixation and chlorophyll accumulation at different depths in soil cores. Biology and Fertility of Soils. 40: 67-72.
- Nishaa R, Kaushik A, Kaushika CP (2007). Effect of indigenous cyanobacterial application on structural stability and productivity of an organically poor semi-arid soil. Geoderma. 138:1-2: 49-56.
- Ostergaard HS, Hvelplund EK, Rasmussen D (1985). Assessment of optimum nitrogen fertilizer requirement on the basis of soil analysis and weather conditions prior to the growing season. In: Neeteson JJ; Dilz K, ed. Assessment of nitrogen fertilizer requirement. Institute for Soil Fertility, Haren, 25-36.
- Pichel FG, Cortez AL, Nubel U (2001). Phylogenetic and morphological diversity of cyanobacteria in soil desert crusts from the Colorado plateau. Appl. and Environ. Microbiol. 67: 1902-1910.
- Prasanna R, Jaiswal P, Kaushik BD (2008). Cyanobacteria as potential options for environmental sustainability – promises and challenges. Indian J. Microbiol. 48:89–94.
- Purcell D, Sompong U, Yim LC, Barraclough TG, Peerapornpisal Y, Pointing SB (2006). The effects of temperature, pH and sulphide on the community structure of hyperthermophilic streamers in hot springs of northern Thailand. FEMS Microbiol. Ecol. 60: 456–466.
- Rios A, Ascaso C, Wierzchos J, Valiente EF, Quesada A (2004). Microstructural characterization of cyanobacterial mats from the McMurdo Ice Shelf, Antarctica. Appl. and Environ. Microbiol. 70: 569- 580.
- Romo S, Miracle MR (1993). Long-term periodicity of Planktothrix agardhii, Pseudoanabaena galeata and Geitlerinema sp. in a shallow hypertrophic lagoon, the Albufera of Valencia (Spain) Arch. Hydrobiol. 126: 469–486.
- Sallam ASh (2002). Evaluation of Some Soils in Najd Plateau (Central Region, Saudi Arabia). J. Saudi Soc. Agric. Sci. 1: 2 pp: 21-40.
- Singh PK, Kishore S, Prakash J, Singh SK, Shukla M (2008). Cyanophycean algae inhabiting sodic soil exhibit diverse morphology: And adaptation to high exchangeable sodium. Ecoprint, 15: 15-21.
- Stein JR (1979). Handbook of phycological methods, culture methods and growth measurements. Cambridge University Press. pp 11-15.
- West NE (1990). Structure and function of soil microphytic crusts in wildland ecosystems of arid and semi-arid regions. Advances in Ecological Research. 20: 179-223.
- Wierzchos J, Ascaso C, McKay CP (2006). Endolithic cyanobacteria in halite rocks from the hyperarid core of the Atacama Desert. Astrobiol. 6: 1-8.
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