Introduction

Cyanobacteria are geographically widespread autotrophs, inhabiting a wide range of environments, and constituting the main primary producers in many aquatic ecosystems (Whitton and Potts 2000). Due to the continuous uncovering of cryptic Cyanobacterial species, taxonomic identification of Cyanobacteria has become a challenge for phycologists. The first trials for the taxonomy of Cyanobacteria were done in the late nineteenth century. Rippka et al. (1979) recorded five orders of Cyanobacteria. Order I represented Chroococcales, which includes single-celled Cyanobacteria, multiply by binary fission and present solitary or in colonial shape. Order II, Pleurocapsales, constitutes coccoid Cyanobacteria, which are characterized by the formation of baeocytes. Order III, Oscillatoriales, includes filamentous Cyanobacteria formed only from vegetative cells. Order IV, Nostocales, composes of filamentous taxa capable of producing heterocytes and akinetes. Order V, Stigonematales, includes filamentous taxa which also form heterocytes and akinetes and are characterized by their ability to form true-branched trichomes (Castenholz et al. 2001). However, Rippka’s taxonomic scheme for Cyanobacteria, based on morphological traits, e.g., multicellularity, baeocyte formation, presence of akinetes, tapering, polarity, and branching patterns, has left overlapped phyletic groups, and consequently, does not always accurately represent evolutionary relationships.

As molecular identification tools become available, taxonomic updating for Cyanobacteria has been required (Komárek et al. 2014; Dvorak et al. 2015). With the introduction of the rRNA gene as a molecular taxonomy tool for the identification of Cyanobacteria, more than 92000 rRNA gene sequences have been deposited in DNA databases, http://ddbj.nig.ac.jp/arsa/search?lang=en&cond=quick_search&query=16S+Cyanobacteria&operator=AND, characterizing various taxonomic ranks of Cyanobacteria (Walter et al. 2017). Few studies have applied genetic markers to describe the taxonomy of uncultured Cyanobacteria in African lakes. Elsaied (2007) used 16S rRNA gene metabarcoding for recording 10 uncultured cyanobacterial phylotypes from Lake Manzala, Egypt. Uncultured Cyanobacteria-like 16S rRNA gene phylotypes have been recorded in desert lakes of Wadi An Natrun, Egypt (Mesbah et al. 2007). Dadheech et al. (2009) have used PCR-based denaturing gradient gel electrophoresis (DGGE) for 16S rRNA gene to identify uncultured Cyanobacteria in marine alkaline and freshwater lakes of Kenya. Arthrospira platensis NIOF17/003 has been isolated from El-Khadra saline-alkaline lake, Wadi El-Natrun, Egypt, characterized as a novel species, based on 16S rRNA gene barcoding, and screened for biodiesel metabolic production (Zaki et al. 2021).

However, the 16S rDNA has recently been shown to lack the power of characterizing lower taxonomic ranks, such as species and strains (Konstantinidis et al. 2006; Goris et al. 2007). The level of the 16S rRNA gene nucleotide identity that has been accepted to characterize prokaryotic species identification has been calculated as 98.65% (Kim et al. 2014). There have been records for differentiated populations of phenotypically different Cyanobacteria that had identical 16S rRNA gene sequences, though they varied considerably in metabolic features (Miller et al. 2006).

So, other potential molecular markers have been added for enhancing clarification of Cyanobacterial taxonomy. The gene cbbL, which encodes the large subunit of ribulose 1,5, bisphosphate carboxylase oxygenase, RuBisCO, the key enzyme of the Calvin cycle, has been considered as an efficient molecular marker for characterizing the functional phylogeny of Cyanobacteria (Dvorak et al. 2014). However, cbbL-based taxonomy has been used for the classification of more than 60 species of Cyanobacteria, http://ddbj.nig.ac.jp/arsa/search?lang=en&cond=quick_search&query=cbbl+Cyanobacteria&operator=AND. Hence, the combination of the 16S rRNA gene data with those of other molecular markers, collectively known as multilocus sequence analysis (MLSA), has become common in molecular studies to address the taxonomic gaps of the 16S rRNA gene, giving almost robust phylogenetic characterization (Wilmotte et al. 2017). A novel species, Dolichospermum hangangense has been taxonomically characterized by using MLSA of the 16S rRNA gene and cbbL (Choi et al. 2018).

Lake Nasser is one of the largest worldwide artificial freshwater reservoirs, (Imam et al. 2020). According to current speed, turbidity, nutrient availability, and suspended solids, the lake has been divided into three sections: riverine, transition zone, and lacustrine section, where the first two sections are eutrophic, while the third section is mesotrophic. Cyanobacteria have been recorded as the abundant group in the transition and lacustrine sections (Salem 2011; Abdel-Gawad and Abdel-Aal 2018). Cyanobacterial genera, such as Anabaena, Aphanizomenon, Chroococcus, Lyngbya, Merismopedia, Microcystis, Nostoc, Oscillatoria, Phormidium, and Spirulina, have been microscopically observed at Lake Nasser. Synechococcus- and Oscillatoria-like 16S rRNA gene phylotypes have been recorded in the guts of Nile tilapia, Oreochromis niloticus, along Lake Nasser (Elsaied et al. 2019).

Lake Qarun has been considered a saline eutrophic lake, located as a depression in the western desert of Egypt. It is an inland closed lake that receives about 450 million m3/year of agricultural runoff from drains, El-Bats, and El Wadi (Redwan and Elhaddad 2017). Salinity in Lake Qarun varies between 14.24 and 39.8 g/l (Abd El-Aal et al. 2020). The main phytoplankton fractions in Lake Qarun have been found to belong to diatoms, dinoflagellates, and Cyanobacteria (Abd El-Karim 2012; Zaher and Ibrahim 2018). Cyanobacterial fraction constituted about 26.8% of the total phytoplankton cell concentration in Lake Qarun (Flefil and Mahmoud 2021). The microscopic survey has observed Cyanobacterial genera Anabaena, Chroococcus, Gomphosphaeria, Merismopedia, Microcystis, Oscillatoria, and Phormidium at the lake (Fathi and Flower 2005).

Cyanobacteria produce various types of natural products, considering this phylum as one of the main aquatic bioresources for several biotechnological applications (Singh et al. 2018). Cyanobacteria are important sources of carbohydrates, proteins, lipids, natural pigments, and novel bioactive compounds, such as oscillapeptin A, hapalindole A, alkaloids, lipopeptides, fatty acids, anabaenopeptin E, sester-terpenes, lyngbic acid, glycolipids, macrolactones, glycosidic macrolides, and tetrasaccharides (Nagarajan et al. 2012; Rai and Rajashekhar 2015; Demay et al. 2019). Some studies have shown the relationship between trophic status and the metabolic potential of Cyanobacteria in freshwater lakes (Shen et al. 2019).

The studies on cyanobacterial diversity in Egyptian lakes have been limited to conventional taxonomic methods, based on morphology, and some traditional biochemical analyses. The current study explored and characterized some novel freshwater and saline cyanobacterial species from Egyptian lakes, based on morphology and two molecular tools, 16S rRNA gene coupling with cbbL barcoding. The biochemical composition of the isolates was determined to assess their biotechnological potential.

Materials and methods

Sampling

Sampling sites from Lake Nasser and Lake Qarun are shown in Fig. 1. Water samples, each of 500 mL, were collected in sterilized bottles and maintained at low-temperature conditions (2–8 °C) for culture and isolation procedures. Ten milliliter of water samples was inoculated into 250-mL Erlenmeyer flasks, which contained 100 mL of BG11 medium (Allen 1968). The pH of the culture medium was adjusted to 7.1. For saline cultures, NaCl (10 g/L) was added to prepare marine BG11 medium. All inoculated flasks were incubated at 25 °C with a 16:8 light–dark cycle of 37 µmol. m−2 s−1 photon flux density until reaching stationary phase (3–4 weeks).

Fig. 1
figure 1

Map shows the isolate sampling sites in Egyptian lakes, Lake Qarun, and Lake Nasser

Isolation and identification of Cyanobacteria

Cyanobacteria were isolated and purified through serial dilutions, optical microscopic examination, picking with Pasteur micropipette, spreading on an agar plate, and frequent sub-culturing for obtaining the pure isolates (Guillard 2005; Andersen and Kawachi 2005).

Morphology

The morphological features, including cell dimension, cell shape, presence or absence of calyptra, heterocysts, akinetes, and sheath characters, were described for each isolate, using an inverted microscope, Zeiss Axiovert 25, Carl Zeiss. Species characterizations were carried out based on classical algae keys (Kützing 1845; Gomont 1892; Meffert 1988; Castenholz 1989; Komárek and Anagnostidis 2005), concerning algae database (Guiry and Guiry 2021) http://www.algaebase.org/).

Molecular characterization

Genomic DNA was extracted from 2 mL of each Cyanobacterial pure isolate culture, using the DNeasy Power Water kit (Qiagen, catalog no.14900–50-NF), with modifications of Elsaied et al. (2002). The culture sample was centrifuged, and the cell pellets were washed several times with TE buffer, 10 mmol/L Tris, 1 mmol/L EDTA, pH 8. The algal cells were lysed with glass beads and lysis buffer in the extraction kit. The purified DNA was run on 0.9% agarose gel, stained with ethidium bromide, and visualized by Gel Doc™ XR + imager (Bio-Rad, UK, Catalog number 1708195). The extracted DNA was kept at − 20 °C for further molecular analyses.

PCR for amplification of the 16S rRNA gene was performed using primers, EuBac-27F, 5′-agagtttgatcctggctcag-3′, and EuBac-1492R, 5′-ggttaccttgttacgactt-3′ (Lane 1991), producing amplicon with size ~ 1500 bp. The primers IAB-595F, 5′-gayttmactaargatgayga-3′, and IAB-1385R, 5′-tcgaacttgatttctttcca-3′ (Elsaied and Naganuma 2001), were used to amplify 800 bp of the RuBisCO large subunit-encoding gene, cbbL. PCR was performed in 50 μL volume of reaction mixture, 5 μL MgCl2 (2.5 mM), 5 μL dNTPs (2.5 mmol), 5 μL EX taq buffer (Mg2+ free) 10 × , 2 μL of each primer (10 pmol), 0.3 μL Takara EX-Taq™ Polymerase 250 U, and 2 μL DNA template (25 ng). PCR was carried out by a ProFlex™ thermal cycler (Life Technology, USA). The PCR program for amplification of the 16S rRNA gene included an initial denaturation step at 95 °C for 3 min, followed by 30 cycles, each one consisting of 50 s at 95 °C, 50 s at 55 °C, and 1 min at 72 °C, with a final extension step at 72 °C for 12 min. For amplification of the gene cbbL, thermal cycling was initiated with denaturation at 95 °C for 1 min, followed by 30 cycles of denaturation at 95 °C for 50 s, annealing at 49 °C for 1 min, and extension at 72 °C for 2 min, followed by final extension step at 72 °C for 12 min. The PCR products were purified using a QIAquick® PCR purification kit (Catalog no. 28104, Qiagen, Germany) and sequenced using a Sanger ABI 3730xl capillary DNA analyzer (Applied Biosystems, Foster City, CA, USA).

Phylogenetic analysis

Sequences were submitted to the BLASTN homology search tool, for screening their similarities with those deposited in the DNA database. The nucleotide sequences of the gene cbbL were translated into deduced amino acids, using the Transeq tool, https://www.ebi.ac.uk/Tools/st/, and submitted to the BLASTP homology search tool. Phylogenetic trees, based on partial nucleotide sequences, for the 16S rRNA gene, and deduced amino acid sequences, for cbbL, were constructed through two analyses. First, recorded sequences were aligned with those from related members of Cyanobacteria deposited at databases, using Clustal Omega, http://www.ebi.ac.uk/Tools/msa/clustalo/. Second, consensus trees were drawn through MEGA11 software (Tamura et al. 2021), using compatibility of phylogeny algorithms, maximum likelihood, neighbor-joining, and maximum parsimony, with the bootstrap confidence level, 1000 replicates. The 16S rRNA gene sequences of current isolates were deposited in the gene bank under accession numbers from MZ504747 to MZ504752, while cbbL sequences were recorded under accession numbers from MZ702731 to MZ702736.

Phytochemical screening

Total carbohydrate

Total carbohydrate content was determined using the phenol–sulfuric acid method with modification of Quero-Jiménez et al. (2019). The absorbance of the extract was measured at 490 nm, and the total carbohydrate content was calculated from a linear regression equation obtained from the glucose standard curve.

Total protein

The total protein content was determined using the Folin–Ciocalteau reagent (Lowry et al. 1951). The extract absorbance was measured at 660 nm, and the sample’s protein content was calculated from a linear regression equation obtained from the bovine serum albumin standard curve.

Total lipid

The total lipid content was determined by the gravimetric method (Folch et al. 1957), in which 0.5 g of the dry weighted sample was extracted with a solvent mixture of methanol-chloroform (1:2 v/v), and the filtrate was collected in a pre-weighed flask and evaporated, and weight of dry material was determined. The difference between the initial weight and final weight gave the total lipid content.

Chlorophyll-a determination

Chlorophyll-A was determined according to Lorenzen (1967). About 4 mL of Cyanobacterial culture was centrifuged, and the pellets were homogenized, followed by chlorophyll-a extraction with 90% aqueous acetone. Chlorophyll-a absorbance was measured at 750 nm and 665 nm, before and after acidification with two drops of 1 mol/L HCl for correction against phaeopigments. The chlorophyll-a was calculated using the following equation.

$$\mathrm{Chl-a}\ \mathrm{(\mu g/L)}=26.7\mathrm{[(A665^b-A750^b)-(A665^a-A750^a)]}\ \mathrm{v/VI}$$
$$\mathrm{Chl-a}\;{(\mathrm {mg/g}\;\mathrm D\mathrm W)}=\text{Chl-a}\ \mathrm{(\mu g/L)}-1000 \times\mathrm{Y}$$
  • A665b -A750b = Absorbance at 665 and 750 before acidification.

  • A665a-A750a = Absorbance at 665 and 750 of the acidified extract.

  • v = volume of the extract (mL).

  • V = volume of the filtrate (L).

  • I = light path of the cuvette (cm).

  • Y = Dry weight yield in grams

Phycobiliprotein content measurements

Phycobiliproteins were extracted through centrifugation of 250 mL of stationary phase growing culture, at 4000 rpm for 10 min, and the supernatant was decanted. The cell pellets were suspended in 10 mL of 0.1 M phosphate buffer pH 7.0, homogenized, and extracted by sequential freezing and thawing cycles until the pellets turned greenish. The homogenate was centrifuged at 4000 rpm for 10 min, and the phycobiliproteins-containing supernatant was collected into a clean tube. The phycobiliproteins were measured with a spectrophotometer, under absorbance at 280 nm, and 562 nm for phycoerythrin; 615 nm for phycocyanin; and 652 nm for allophycocyanin, followed by quantifications using equations of Bennett and Bogorad (1973).

  • Phycocyanin concentration: 

    $$\mathrm{(PC) mg/mL = [A615-0.474 (A652)]/5.34}$$
  • Allophycocyanin concentration: 

    $$\mathrm{(APC) mg/mL} = [\mathrm{A}652-0.208 (\mathrm{A}615)]/5.09$$
  • Phycoerythrin concentration:

    $$\mathrm{(PE) mg/mL} = [\mathrm{A}562-2.41\mathrm{(PC)}-0.849 \mathrm{(APC)}]/9.62$$

All phycobiliproteins were normalized to mg/g DW by dividing their content in liters by the corresponding dry weight yield in grams.

Determination of carotenoids

Carotenoids were determined based on the methodology of Zavřel et al. (2015). One gram of dry weight biomass was extracted with absolute methanol and kept protected from light at 4 °C for 20 min, and the carotenoid-containing supernatant was measured under absorbance wavelengths of 470 nm, 665 nm, and 720 nm. The carotenoids were calculated through the following equations:

\(\mathrm{Chl a}\ \mathrm{(\mu g/L)}=12.9447\ \mathrm{(A665-A750)}\) (Ritchie 2006)

\(\mathrm{Carotenoids}\ [\mu \mathrm{g}/\mathrm{mL}]=[1000\ (A470-A720)-2.86\)\((\mathrm{Chl}\ \mathrm{a})]/211\) (Wellburn 1994)

Ash-free dry weight (AFDW) content

Ash-free dry weight content was determined according to AOAC (2000) protocol. About 0.5 g of the dry weight sample was incinerated in a furnace at 500–550 °C until the white ash was formed (about 5 h), and the dry weight of the ash was estimated.

\(\mathrm{AFDW}=\mathrm{total}\ \mathrm{dry}\ \mathrm{weight-ash}\ \mathrm{weight}\) 

Statistical analysis

Statistical analysis was carried out with XLSTAT 2019.1 software. All the results were calculated as mean ± standard deviation. One-way ANOVA was applied to test for significant differences at p < 0.05.

Results

Characterization of the isolates

Six Cyanobacterial isolates, four from Lake Nasser and two from Lake Qarun, were recovered (Fig. 2). The freshwater isolate SN1, from Lake Nasser, (Fig. 2a), has a colonial form, with 4–16 up to 64 cells, per colony, arranging perpendicular in longitudinal and transverse rows, forming quadrangular colonies, which enclosed by a distinct, hyaline, and homogeneous mucilage. Cells are spherical or hemispherical, with 2.5–4.0 µm diameters and 2.0–3.0 µm in length, having bright blue-green and homogenous content.

Fig. 2
figure 2

Photomicrographs show morphology of Cyanobacterial isolates. a Isolate SN1, b isolate SN2, c isolate SN3, d isolate SN4, e isolate Q1, f Isolate Q2

The freshwater isolate SN2, from Lake Nasser (Fig. 2b), has trichomes, which form a brown mass on BG11 medium, straight not tapering toward the apex. The apical cell is rounded and slightly capitated with a thick outer membrane. Cells have 15 µm in width and 1.3–3.0 µm in length and granulated and distinctly constricted at the cross wall. The isolate has vegetative reproduction, which is carried out by the disintegration of trichomes into small fragments through the formation of necridic cells.

The Lake Nasser isolate SN3 (Fig. 2c) has a thin thallus, filament solitary, free-floating (planktonic), with slow motility by gliding with oscillation. Filaments are unsheathed, not constricted at the cross wall, and not attenuated at the apex. Trichome has a pale blue-green color and consists of narrow cylindrical, elongated cells, with 1.0–1.5 µm in width and 5.0–6.0 µm in length. The isolate contains obvious gas vesicles and polar aerotopes. Apical cells are cylindrical without calyptra.

Isolate SN4, Lake Nasser (Fig. 2d), has morphological characteristics similar to isolate SN3, but its growth differs slightly, as the trichrome is tangled, forming mats at the bottom of the culture vessels, and the cells contain less obvious gas vesicles.

Isolate Q1, Lake Qarun (Fig. 2e), has a filamentous form, solitary and tangled into clusters to form mats, being attached to the substrate. Trichomes are motile with thin, firm, and colorless sheaths, opening at the apex. Filaments are cylindrical, not constricted at the cross walls, not attenuated at the apex with rounded apical cells, and the end cells are without thickened walls or calyptras. Trichomes have a bright blue-green color and compose of cells with an average width of 2 µm, length of 8–10 µm, and have prominent granules.

Isolate Q2, Lake Qarun (Fig. 2f), has filamentous form. Filaments are thin, straight, or slightly bent, pale to bright blue-green, solitary or entangled, and attenuate at one or both ends. Trichomes are not or are slightly constricted at cell walls. The isolate moves by gliding or pendulum. The filament composes of cylindrical isodiametric cells with 2.5–2.8 µm in width and 2.0–3.0 µm in length. Apical cells are long conical with rounded, slightly hooked, or bent apex and do not capitate. The isolate reproduces by disintegration into small parts, without the formation of necridic cells.

Molecular identifications based on the 16S rRNA gene and cbbL sequencing

Isolate SN1 had 16S rRNA gene nucleotide identity percentage of 95.5% with that of Merismopedia glauca (acc. no. AJ781044), showing monophyletic and paraphyletic lineages with M. glauca isolates (Fig. 3a) (Rajaniemi-Wacklin et al. 2006). The deduced amino acid sequence of the cbbL of isolate SN1 had an average identity percentage of 96% with those of Synechocystis sp. (P54205), and Crocosphaera subtropica (B1WXH3), forming a phylogenetic cluster (Fig. 3b). The 16S rRNA gene nucleotide sequence and cbbL deduced amino acid sequence of isolate SN2 showed identities 97.8% and 99.6%, respectively, with those of belonging to Oscillatoria sancta, representing similar phylogenetic profiles (Fig. 3a, b). The 16S rRNA gene sequences of isolates SN3 and SN4 formed a clade within the cluster of Limnothrix sp. (Fig. 3a), showing nucleotide identities, 97.6% and 97.4%, respectively, with those of previously recorded Limnothrix planctonica isolates (Zhu et al. 2012). On the other hand, the isolate SN3 represented a unique monophyletic lineage, based on cbbL phylogeny (Fig. 3b). The cbbL of isolate SN4 formed a monophyletic clade with Limnothrix planktonica KLL-C001, with 92.4% amino acid identity (Fig. 3b). Isolate Q1 had 16S rRNA gene nucleotide identity 97.8%, with that of Persinema komarekii, where both clustered together in a monophyletic clade (Fig. 3a). The cbbL sequence of isolate Q1 was clustered with that of Phormidium pseudopriestley (WP_207087136), showing 81.3% amino acid identity (Fig. 3b). The 16S rRNA gene sequence of isolate Q2 was localized in the cluster of Jacksonvillea apiculate, representing 96.9% nucleotide identity with those of Jacksonvillea apiculate clones (Fig. 3a). The cbbL of the isolate Q2 formed a monophyletic clade with Lyngbya majuscule (Fig. 3b), and both showed 92.5% amino acid identity.

Fig. 3
figure 3

Phylogenetic trees are based on partial 16S rRNA gene nucleotide sequences (a) and cbbL deduced amino acid sequences (b). Consensus trees were constructed by compatibility of maximum likelihood, neighbor-joining, and maximum-parsimony algorithms. Bootstrap values were calculated from 1000 replicates, and only values more than 50 were specified at the nodes

Phytochemical constituents

The phytochemical constituents varied from one isolate to another and were significantly different at p value < 0.05 (Table 1). The total carbohydrate content varied from 187.0 ± 2.8 to 274 ± 14.5 mg/g DW in isolates SN1 and Q2, respectively. The total protein values ranged from 147.2 ± 7.8 to 364.7 ± 6.4 mg/g DW in isolates SN1 and SN4, respectively (Table 1). The total lipid content fluctuated between 35.5 ± 1.2 mg/g DW in isolate Q2 to 67.6 ± 0.2 mg/g DW in isolate SN4.

Table 1 Biochemical constituents of Cyanobacterial isolates

Total phycobiliproteins (TPBPs) ranged between 82.2 ± 20 and 250 ± 18 mg/g DW for isolates SN4 and SN2, respectively (Table 2). The isolate Q1 had the highest content, 114 ± 20.7 mg/g DW, of phycocyanin (PC), while the isolate SN2 harbored the largest amount of allophycocyanin (APC), 71.0 ± 4.8 mg/g DW, and phycoerythrin (PE) (98 ± 6.7 mg/g DW) (Table 2). The isolate SN4 had a minimal amount of PC (60.9 ± 13.4 mg/g DW), while the isolate SN1 had a minimal amount of APC (17.3 ± 4.6 mg/g DW). The lowest PE content, 1.2 ± 0.1 mg/g DW, was recorded in isolate SN3 (Table 2).

Table 2 Pigment contents of Cyanobacterial isolates, normalized to mg/g DW

The current isolates had carotenoid contents with different concentrations, from 0.044 ± 0.01 to 0.261 ± 0.01 mg/g DW for isolates SN2 and SN4, respectively (Table 2). The Chlorophyll-a content varied from 3.3 ± 0.5 mg/g DW in isolate SN2 to 10.0 ± 0.6 mg/g DW in SN4 (Table 2). The ash-free dry weight amount fluctuated between 824.8 ± 3.2 and 891.8 ± 2.8 mg/g DW in isolates Q1 and Q2, respectively (Table 1).

Discussion

The current study targeted the characterization of Cyanobacterial isolates, which were recovered from topological and physicochemical distinct lakes. The isolate characterization tools included morphology, molecular, and biochemical features. We demonstrated the phylogenetic positions of the current isolates based on two types of marker genes, the 16S rRNA gene, which represents the structural phylogeny marker, and cbbL, a representative marker of functional phylogeny for Cyanobacteria. The morphology of the isolate SN1 was similar to that of Merismopedia glauca (Ehrenberg) Kützing 1845, a feature supported by the rRNA gene phylogeny profile. Although the family Merismopediaceae harbors about six known genera, only the cbbL sequence of the genus Synechocystis has been recorded (Kaneko et al. 1996). However, the current cbbL sequence was the first record for an isolate belonging to the genus Merismopedia, generating cbbL data for this genus in lakes. However, the genus Merismopedia has been recorded, through a microscopic survey, as a major component of Cyanobacterial blooms in Lake Nasser (Goher et al. 2021).

Both morphology and molecular tools confirmed that the isolate SN2 belonged to the genus Oscillatoria, representing a new strain of species O. sancta (Gomont 1892). The genus Oscillatoria has been reported to be widely spread in the transition and lacustrine zones of Lake Nasser (Salem 2011). O. sancta has been found to be frequent in freshwater aquatic bodies that have pH value within the alkaline range and even in the presence of low nutrient content, an optimizing condition for lacustrine zones of Lake Nasser (Halder 2017; Zaher et al. 2021).

Both the morphological criteria and 16S rRNA gene homology confirmed that the isolates SN3 and SN4 belonged to the genus Limnothrix (Meffert 1988), but the cbbL phylogeny localized SN3 isolate as a unique phylogenetic lineage. The deviation in cbbL phylogenetic position of the isolate SN3 may be due to lacking knowledge about the diversity of cbbL for the genus Limnothrix. In terms of growth, isolate SN3 formed planktonic growth through the culture vessels, while isolate SN4 formed mat settled at the walls and bottom of the culture flask. In addition, both isolates, SN3 and SN4, showed differences in the phytochemical contents, suggesting differentiated isolates. A polyphasic study on Limnothrix planktonica strains, isolated from shallow eutrophic lakes in China, has suggested that Limnothrix species are polyphyletic and their taxonomy requires further examination (Zhu et al. 2012). Limnothrix planktonica has been reported to be the most abundant Cyanobacterial species in eutrophic European lakes (Noges et al. 2008). These observations may suggest that the current Limnothrix-like isolates are bioindicators of eutrophication in Lake Nasser.

The phylogenies of some isolates based on cbbL differed from those based on the 16S rRNA gene. The phylogenetic profile derived from cbbL sequences sometimes shows a relationship between distant taxonomic species, which are classified based on rRNA gene phylogeny (Iniguez et al. 2020). This disagreement between the 16S rRNA gene and cbbL phylogenies may refer to the concept of the possibility of horizontal gene transfer of cbbL in the evolution of Cyanobacteria (Delwiche and Palmer 1996; Badger et al. 2002; Iniguez et al. 2020). This rampant horizontal cbbL transfer, in addition to lacking knowledge of cbbL sequence for some Cyanobacterial genera, may explain the variation in the phylogenetic position of isolates, Q1 and Q2, in both current trees. The isolate Q1 had morphological features and rRNA gene homology similar to that of Persinema komarekii, a species, which commonly occurs in the highly radiated aquatic area (Heidari et al. 2018). However, some areas of Lake Qarun are characterized by the existence of radioactive 40 K due to excessive discharge of K-containing fertilizers, from agricultural drains into the lake (Imam 2005; Darwish et al. 2013; Amin 2015). These environmental conditions may favor the occurrence of Persinema-like isolate Q1. Both of morphology and rRNA gene homology of isolate Q2 showed similarity with Jacksonvillea apiculata, a species that belongs to Desertifilaceae (Hasler et al. 2017). Both Persinema komarekii and Jacksonvillea apiculata have limited studies and have no cbbL sequences deposited in the DNA database. However, the taxonomic observation of isolates Q1 and Q2 may support the concept that functional cbbL phylogeny shows conservation among distant Cyanobacterial taxa (Liu et al. 2017). The cbbL phylogenetic radiation within Cyanobacteria may be due to a response to environmental stresses (Jaffe et al. 2018).

The carbohydrate contents of isolates SN4, Q1, and Q2 (Table 1) were higher than those recorded in members of the closest genera Synechococcus (148 mg/g DW), Oscillatoria (186 mg/g DW), and Lyngbya (173 mg/g DW), besides the species, Arthrospira platensis (146.7 mg/g DW), Anabaena sp. (114.6 mg/g DW), Merismopedia tenussima (109.3 mg/g DW), and Spirulina platenesis (50.7 mg/g DW) (Patel et al. 2017; Cheng et al. 2019; Issa et al. 2020; Ennaji et al. 2021), suggesting suitable sources for carbohydrate-dependent industry, such as bioethanol production. On the other hand, the protein contents of the isolates, SN4, Q1, and Q2 (Table 1), were higher than those have been recorded in Anabaena sp. (118.5 mg/g DW), Merismopedia tenussima (72.3 mg/g DW), Spirulina platenesis (160.7 mg/g DW) (Issa et al. 2020), and Nostoc sp. (109.8–280.2 mg/g DW), and other seven Cyanobacterial species, Oscillatoria foreaui, O. calcuttensis, O. acuminate, Gloeocapsa livida, Lyngbya limnetica, Calothrix fusca, and Scytonema bohneri, which have protein contents fluctuated between 16 and 70 mg/g DW (Rajeshwari and Rajashekhar 2011). The protein contents obtained from the current isolates were similar to those recorded from Nostoc sp. (109.8–280.2 mg/g DW) and Cylindrospermum sp. (141.1–366.9 mg/g DW) (Borah et al. 2016). So, the current study isolates could be used as a protein source or as food additives in the food industry.

The lipid contents of current isolates were consistent with those previously recorded in Cyanobacterial species Spirulina platensis, Oscillatoria acuta, Calothrix sp., Lyngbya sp. Leptolyngbya sp., Synechococcus sp., Nostoc muscorum, Oscillatoria marina, Anabaena sp. Cyanobium sp., Limnothrix sp., Nostoc sp., and Merismopedia tenuissima that had lipid content fluctuated between 25 and 66 mg/g DW (Sahu et al. 2013; Oliveira et al. 2018; Issa et al. 2020). However, further studies should be carried out for optimizing the growth parameters to increase the lipid content of these isolates to be more attractive for commercial production (Vargas et al. 1998).

Phycobiliproteins (PBPs), phycocyanin, allophycocyanin, and phycoerythrin are light-harvesting colored proteins produced by Cyanobacteria, as photosynthetic accessory pigments and have biotechnological potentials. The phycobiliprotein compositions in current Cyanobacterial isolates showed variations. Isolate Q1 was attractable for its highest phycocyanin content and can be used as an alternative for Arthrospira platensis (Basheva et al. 2018) since isolate Q1 was recovered from heavily polluted marine water. Isolate SN2 can be added to Oscillatoria members for mass production of phycoerythrin (Rai and Rajashekhar 2015). In their study of phycobiliproteins production by 18 Cyanobacterial strains, Hemlata and Fatma (2009) recorded the highest amount of phycobiliproteins, 91 mg/g DW, in Anabaena NCCU-9. However, this amount was lower than those recorded in current isolates. Chlorophyll-a along with phycobiliproteins is the main photosynthetic pigment in Cyanobacteria (Munir et al. 2013). The chlorophyll-a and carotenoid contents of isolate SN4 were higher than those recorded for Synechococcus elongates, S. aeruginosus, and Phormidium fragile (Jeevanantham et al. 2019). Generally, isolates SN2 and Q1 could be sources for pigment production.

Conclusion

The study aimed to characterize Cyanobacterial isolates from different desert lakes and to assess their biochemical composition with a view toward biotechnology applications. The study recorded new six Cyanobacterial isolates, from Egyptian lakes. Isolates were characterized based on morphology, genetic signatures, and biochemical composition. The isolates SN1, SN2, SN3, SN4, Q1, and Q2 belonged to the genera, Merismopedia, Oscillatoria, Limnothrix, Persinema, and Jacksonvillea, respectively, according to phylogenetic analyses of the 16S rRNA gene. In addition, the study presented the first cbbL sequence for the genera Merismopedia, Persinema, and Jacksonvillea, represented by the isolates SN1, Q1, and Q2. On the other hand, isolates, SN4 and Q2 had the highest protein and carbohydrate contents, respectively, while isolate SN2 showed contents rich with pigments, and may therefore have biotechnological potential.