
The current study aimed to analyze bacterial communities' diversity and abundance in three different deserted areas (Merzouga, Mhamid Elghizlane, and Erg lihoud) located in Moroccan Sahara, as well as to investigate osmotolerant microorganisms producing hydrolytic enzymes. The isolates were taxonomically affiliated using 16S rRNA gene sequencing. Four different hydrolase activities (amylase, lipase, cellulase, and protease) and osmotic stress tolerance were evaluated. The phylogenetic analysis of 364 screened isolates belonged to three phyla (Firmicutes 73%, Proteobacteria 26% and Actinobacteria 1%) and 18 different genera, from Bacillus, Ornithinibacillus, Paenibacillus, Geobacillus, Pseudomonas, Acinetobacter, Agrobacterium, Arthrobacter, Paenarthrobacter, Enterobacter, Staphylococcus, Erwinia, Herbasprillum, Ocuria, Massilia, Planomicrobium, Hodococcus, and Stenotrophomonas. The results detected a high proportion of osmotolerant and enzymes producing bacteria, many isolates can tolerate up to 55 °C (40%, 28%, and 30% in Merzouga, Mhamid Elghizlane, and Erg lihoudi, respectively). Meanwhile, the salinity tolerance reached 12% in some isolates with different proportions in each site, 29% in Merzouga, 24% in Mhamid Elghizlane, and 9% in Erg lihoudi. Furthermore, the enzymatic tests showed the presence of an amylolytic, lipolytic, cellulolytic, proteolytic activities in 20%, 31%, 63% and 72% of total strains, respectively.
As a result, the present study is thus a preliminary yet critical step towards identifying the best bacterial candidates for further biotechnological applications.
Citation: Amina Manni, Abdelkarim Filali-Maltouf. Diversity and bioprospecting for industrial hydrolytic enzymes of microbial communities isolated from deserted areas of south-east Morocco[J]. AIMS Microbiology, 2022, 8(1): 5-25. doi: 10.3934/microbiol.2022002
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The current study aimed to analyze bacterial communities' diversity and abundance in three different deserted areas (Merzouga, Mhamid Elghizlane, and Erg lihoud) located in Moroccan Sahara, as well as to investigate osmotolerant microorganisms producing hydrolytic enzymes. The isolates were taxonomically affiliated using 16S rRNA gene sequencing. Four different hydrolase activities (amylase, lipase, cellulase, and protease) and osmotic stress tolerance were evaluated. The phylogenetic analysis of 364 screened isolates belonged to three phyla (Firmicutes 73%, Proteobacteria 26% and Actinobacteria 1%) and 18 different genera, from Bacillus, Ornithinibacillus, Paenibacillus, Geobacillus, Pseudomonas, Acinetobacter, Agrobacterium, Arthrobacter, Paenarthrobacter, Enterobacter, Staphylococcus, Erwinia, Herbasprillum, Ocuria, Massilia, Planomicrobium, Hodococcus, and Stenotrophomonas. The results detected a high proportion of osmotolerant and enzymes producing bacteria, many isolates can tolerate up to 55 °C (40%, 28%, and 30% in Merzouga, Mhamid Elghizlane, and Erg lihoudi, respectively). Meanwhile, the salinity tolerance reached 12% in some isolates with different proportions in each site, 29% in Merzouga, 24% in Mhamid Elghizlane, and 9% in Erg lihoudi. Furthermore, the enzymatic tests showed the presence of an amylolytic, lipolytic, cellulolytic, proteolytic activities in 20%, 31%, 63% and 72% of total strains, respectively.
As a result, the present study is thus a preliminary yet critical step towards identifying the best bacterial candidates for further biotechnological applications.
Sweeping surface is the surface swept out by the movement of a plane curve (the profile curve or generatrix) whilst the plane is moved through space in such away that the movement of the plane is always in the direction of the normal to the plane. Sweeping is a very substantial, strongly, and spread method in geometric modelling. The fundamental idea is to select various geometrical object (generators), which is then swept over a spine curve (trajectory) in the space. The result of such evolution, depend on movement through space and intrinsic shape deformation, is a sweep object. The sweep object type is given by the choice of the generator and the trajectory. Additional specifics on the sweeping surfaces can be found in [1,2,3,4]. In recent years, the ownerships of sweeping surfaces and their offset surfaces have been examined in Euclidean and non-Euclidean spaces (see e.g., [5,6,7,8,9]). There are several different names for the sweeping surface in previous written works, namely, tubular surface, pipe surface, string, and canal surface [10,11]. However, to the best of the authors knowledge, we can not find any literature on the study for regarding curves lying in surfaces as the original objects and considering the singularities and convexity of sweeping surfaces generated by these curves. Serve such a need and as the extension of the study[7], the current study focuses our attention on the geometrical properties of sweeping surfaces whose center curves in surfaces in Euclidean 3-space E3.
In this work, in analogous with the well known Bishop and Frenet-Serret frames, we define a new version of Darboux frame using a common tangent vector field to a surface along a curve and call this frame the rotation minimizing Darboux frame (RMDF). By using this frame, we give the parametric representation for a sweeping surface. We also show that the parametric curves on this surface are curvature lines. Then, we study the local singularities and convexity of a sweeping surface. Consequently, the necessary and sufficient condition for the sweeping surface to be a developable ruled surface is derived. In addition, some examples of application are introduced and explained in detail.
The ambient space is the Euclidean 3-space E3, and for our work we have used [10,11] as general references. Let
R(s,u)=(x1(s,u),x2(s,u),x3(s,u)), (s,u)∈D⊆R2, |
represent a regular surface M. The R′s tangent vectors are
Rs(s,u)=∂R∂s, Ru(s,u)=∂R∂u. |
The unit normal vector to the surface M is
u(s,u)=Rs×Ru‖Rs×Ru‖, |
where × denotes the cross product in E3. The metric (first fundamental form) I is defined by
I(s,u)=g11ds2+2g12dsdu+g22du2, |
where g11=<Rs,Rs>, g12=<Rs,Ru>, g22=<Ru,Ru>. We define the second fundamental form II of M by
II(s,u)=h11ds2+2h12dsdu+h22du2, |
where h11=<Rss,u>, h12=<Rsu,u>, h22=<Ruu,u>. The Gaussian K(s,u) and mean H(s,u) curvature are defined by
K(s,u)=h11h22−h212g11g22−g212 and H(s,u)=g11h22+g22h11−2g12h222(g11g22−g212). |
Let γ:I⊆R→M is a unit speed curve on M. Since γ(s) is a space curve, there exists the Serret-Frenet frame {t(s), n(s), b(s)}. The derivative formulas for Serret-Frenet frame are given by
(t′n′b′)=(0κ0−κ0τ0−τ0)(tnb), (′=dds), |
where κ(s) is the curvature and τ(s) is the torsion of γ(s). Due to γ(s) on the surface M, we have the moving Darboux frame {γ(s);e1,e2,e3}; t=e1(s), e3=e3(s) is the surface unit normal restricted to γ, and e2=e3×e1 be the unit tangent to the surface M. The the relationships between these frames is expressed as:
(e1e2e3)=(1000cosφsinφ0−sinφcosφ)(tnb);φ=φ(s). | (2.1) |
Then we have the following Frenet-Serret type formulae:
(e′1e′2e′3)=(0κgκn−κg0τg−κn−τg0)(e1e2e3)=˜ω(s)×(e1e2e3), | (2.2) |
where ˜ω(s)=τge1−κne2+κge3 is referred to as the Darboux vector. Here,
{κn(s)=κsinφ=<γ′′,e3>,κg(s)=κcosφ=det(γ′,γ′′,e3),τg(s)=τ−φ′=det(γ′,e3,e′3). | (2.3) |
We call κg(s) a geodesic curvature, κn(s) a normal curvature, and τg(s) a geodesic torsion of γ(s), respectively. In terms of these quantities, the geodesics, curvatures lines, and asymptotic lines on a smooth surface may be characterized, as loci along which κg=0, τg=0, and κn=0, respectively.
Now, we introduce a new rotation minimizing frame using a common tangent vector field to a surface along a curve and call this frame the rotation minimizing Darboux frame.
Definition 3.1. A moving orthogonal frame {ξ1, ξ3, ξ3}, along a space curve r(s), is called rotation minimizing frame (RMF) with respect to a certain reference direction if its angular velocity ω has no component along that direction.
Although the Darboux frame is not RMF with respect to ei(i=1, 2, 3), one can easily derive such a RMF from it. New plane vectors (ξ1, ζ2) are specified through a rotation of (e2, e3) according to
(ζζ1ζ2)=(1000cosϑsinϑ0−sinϑcosϑ)(e1e2e3), | (3.1) |
with a certain angle ϑ(s). Here, we will call the set {ζ, ζ1, ζ2}} as rotation minimizing Darboux frame (RMDF). Therefore, we have the alternative frame equations:
(ζ′ζ′1ζ′2)=(0κ1κ2−κ100−κ200)(ζζ1ζ2)=ω×(ζζ1ζ2), | (3.2) |
where ω(s)=−κ2ζ1+κ1ζ2 is the Darboux vector. One can show that:
{κ1(s)=κgcosϑ+κnsinϑ,κ2(s)=κgsinϑ−κncosϑ,√κ21+κ22=√κ2g+κ2n=κ(s),ϑ(s)=−∫s0τgds+ϑ0,ϑ0=ϑ(0). | (3.3) |
From Eqs (2.2) and (3.2) we observe that the relative velocity is
˜ω(s)−ω(s)=τge1. |
This shows that, the Darboux frame involves an additional rotation about the tangent, whose speed equals the geodesic torsion τg(s). This examination explains the integral formula of Eq (3.3) for computing the RMDF by rectifying the unwanted rotation of the Darboux frame. Hence, the Darboux frame is conformable with the RMDF for curvature lines, that is, τg=0. This is in analogous with Klok's result[1].
Proposition 3.1. Under the above notations we state the following:
(1) If γ(s) is a geodesic curve on M, then the curvatures κ1(s), and κ2(s) satisfy the following:
tan−1(κ1κ2)=−ϑ(s),withϑ(s)=−∫s0τgds+ϑ0,ϑ0=ϑ(0). |
(2) If γ(s) is an asymptotic curve on M, then the curvatures κ1(s), and κ2(s) satisfy the following:
cot−1(κ1κ2)=ϑ(s), withϑ(s)=−∫s0τgds+ϑ0,ϑ0=ϑ(0). |
In this subsection, we give the parametric representations of sweeping surface through the spine curve γ(s) on the surface M in the following: The sweeping surface associated to γ(s), is the envelope of the family of unit spheres, with the center on the curve γ(s)∈M.
Remark 3.1. Clearly, if γ(s) is a straight line, thus the sweeping surface is just a circular cylinder, having γ(s) as symmetry axis. If, on the other hand, γ(s) is a circle, then the corresponding sweeping surface is a torus.
Now, it is easy to see that the connect between the spheres from the family and the sweeping surface is a great circle of the unit sphere, lying in the subspace Sp{ζ1(s),ζ2(s)}, of the spine curve γ(s). Let us indicate by q the position vector attaching the point from the curve γ(s) with the point from the sweeping surface. Then, clearly, we have
Υ:q=γ(s)+r, | (3.4) |
where the unit vector r itself lies in the same subspace Sp{ζ1(s),ζ2(s)}. Let us indicate by the angle u between the vectors r and ζ1. Then, as one can see immediately, we have
r(u)=cos(u)ζ1(s)+sin(u)ζ2(s), | (3.5) |
which is the characteristic circles of sweeping surface. Combining Eqs (3.4) and (3.5), we see that we obtained a representation of the sweeping surface,
Υ:q(s,u)=γ(s)+cosuζ1(s)+sinuζ2(s), | (3.6) |
This representation of Υ excludes sweeping surfaces with stationary vector ζ, because its geometrical properties that is not very important and very easy to be studied.
The q′s tangent vectors are
{qu(s,u)=−sinuζ1+cosuζ2,qs(s,u)=(1−κ1cosu−κ2sinu)ζ. | (3.7) |
Then,
u(s,u)=qs×qu‖qs×qu‖=cosuζ1+sinuζ2, | (3.8) |
which shows that surface normal is included in the subspace Sp{ζ1(s),ζ2(s)}, since it is orthogonal to ζ. The coefficients of the first fundamental form g11, g12 and g22 are
{g11=<qs,qs>=(1−κ1cosu−κ2sinu)2,g12=<qs,qu>=0, g22=<qu,qu>=1. | (3.9) |
For the second fundamental form, we have
{qss=−(κ′1cosu+κ′2sinu)ζ+(1−κ1cosu−κ2sinu)(κ1ζ1+κ2ζ2),qsu=(κ1sinu+κ2cosu)ζ,quu=−cosuζ1−sinuζ2. |
Hence, the elements of the second fundamental form h11, h12, and h22 are
{h11=<qss,u>=−(1−κ1cosu−κ2sinu)(κ1sinu+κ2cosu),h12=<qsu,u>=0,h22=<quu,u>=−1. |
Then, the u-and s curves are curvature lines, that is, g12 and h12 vanish identically (g12=h12=0). Thus, the Gaussian and mean curvature are calculated as
K(s,u)=−κ1cosu+κ2sinu1−(κ1cosu+κ2sinu), |
and
H(s,u)=1−2(κ1cosu+κ2sinu)2−2(κ1cosu+κ2sinu). |
Corollary 3.1. The sweeping surface defined by Eq (3.6) has a constant Gaussian curvature iff
κ1cosu+κ2sinu=cc−1 |
for some real constant c.
Corollary 3.2. The sweeping surface defined by Eq (3.6) has a constant mean curvature iff
κ1cosu+κ2sinu=2c−1c−1 |
for some real constant c.
Corollary 3.3. The sweeping surface defined by Eq (3.6) is a (K(s,u),H(s,u))-Weingarten surface.
Corollary 3.4. The sweeping surface defined by Eq (3.6) is a (K(s,u),H(s,u))-linear Weingarten surface iff
κ1cosu+κ2sinu=c+c12(c1+c2−c) |
where c, c1 and c2 are not all zero real numbers.
On the other hand, the isoparametric curve
π(u):β(u):=q(u,s0)=γ(s0)+cosuζ1(s0)+sinuζ2(s0), | (3.10) |
is a planar unit speed curvature line. Equation (3.10) define a set of one-parameter set of planes in E3. The unit tangent vector to β(u) is
tβ(u)=−sinuζ1(s0)+cosuζ2(s0), |
and thus the unit principal normal vector of β(u) is given by
nβ=ζ(s0)×tβ(u)=cosuζ1+sinuζ2=u(s0,u). |
Thus, the surface normal u(s0,u) is parallel to the principal normal nβ, that is, the curve β(u) is a geodesic planar curvature line, and cannot be asymptotic curve.
Surfaces whose parametric curves are curvature lines have several implementations in geometric design[1,2,3,4]. In the situation of sweeping surfaces, one has to figure the offset surfaces qf(s,u)=q(s,u)+f u(s,u) of a given surface q(s,u) at a certain distance f. In consequence of this equation, the offsetting process for sweeping surface can be reduced to the offsetting of planar profile curve, which is considerably easier to deal with. Hence, we can state the following proposition:
Proposition 3.2. Consider a sweeping surface Υ defined by Eq (3.6). Let xf(u) be the planar offset of the profile r(u) at constant distance f. Then the offset surface qf(s,u) is still a sweeping surface, generated by the spine curve γ(s) and profile curve rf(u).
Singularities and convexity are useful for grasping the ownerships of sweeping surfaces and are investigated in the following:
The sweeping surface Υ has singular points iff the first derivatives are linearly dependent, that is,
qu×qs=(1−κ1cosu−κ2sinu)u=0. | (3.11) |
Since u is a nonzero unit vector, then 1−κ1cosu−κ2sinu=0, that is,
sinu=−κ2±κ1√|κ22+κ21−1|κ22+κ21, | (3.12) |
and
cosu=−κ1±κ2√|κ22+κ21−1|κ22+κ21. | (3.13) |
Hence, there are two singular points on every generating circle. Connecting these two sets of singular points gives two curves that contain all the singular points of a sweeping surface. From Eqs (3.6) and (3.12) it follows that the expression of the two curves is
Γ(s)=γ(s)+−κ1±κ2√|κ22+κ21−1|κ22+κ21ζ1+−κ2±κ1√|κ22+κ21−1|κ22+κ21ζ2. | (3.14) |
From the above analysis it can easily be seen that:
Corollary 3.5. The sweeping surface Υ represented by Eq (3.6), has no singular points if the condition
1−κ1(−κ1±κ2√|κ22+κ21−1|κ22+κ21)−κ2(−κ2±κ1√|κ22+κ21−1|κ22+κ21)≠0, |
is satisfied.
In Computer Aided Geometric Design, conditions that guarantee the convexity of a surface are required in various applications (such as manufacturing of sculptured surfaces, or layered manufacturing). In the case of the sweeping surface Υ, however, the convexity can be controlled with the help of the differential geometric properties. Therefore, we discuss the Gaussian curvature K(s,u)=χ1χ2; χi(s,u) (i=1,2) are the principal curvatures, as follows:
Since g12=h12=0, the value of one principal curvature is
χ1(s0,u):=‖drdu×d2rdu2‖‖drdu‖−3=1. | (3.15) |
The other principal curvature is easy to get
χ2(s,u)=K(s,u)χ1(s0,u)=−κ1cosu+κ2sinu1−(κ1cosu+κ2sinu). | (3.16) |
On the other hand, the curvature for the s-curves (u-constant) can be obtained as:
χ(s,u0)=‖qs×qss‖‖qs‖3=κ1−κ1cosu−κ2sinθ. | (3.17) |
In view of Meusnier's theorem, the expression of χ2(s,u) in Eq (3.16) is
χ2(s,u)=χ(s,u0)cosψ. | (3.18) |
Here ψ=cos−1<n,u>. Thus, the the Gaussian curvature K(s,u) can be obtained as:
K(s,u)=χ(s,u)cosψ. | (3.19) |
We now concentrate on the curves on Υ that are created by parabolic points, that is, points with vanishing Gaussian curvature. These curves separate elliptic (K>0, locally convex) and hyperbolic (K<0, hence non-convex) parts of the surface. From Eq (3.18), it follows that
K(s,u)=0⇔χ(s,u)cosψ=0. |
It can be seen that there are two main cases that cause parabolic points:
Case 3.1. When χ(s,u)=0, that is κ=0. Thus, a planar point of the spine curve γ generates a parabolic curve u = const. on Υ. In other words, the spine curve γ is degenerate to a straight line. Therefore, an inflection or flat point of the spine curve gives a parabolic curve u = const.
Case 3.2. When ψ=π2(<n,u>=0), that is, the osculating plane of γ at each point coincides with the tangent plane to the surface Υ at that point. Then, the spine curve γ is not only a curvature line but also an asymptotic curve on Υ.
In fact we have the following:
Corollary 3.6. Consider a sweeping surface represented by Eq (3.6) with spine and profile curves have non-vanishing curvatures anywhere. If the spine curve γ is a curvature line and also asymptotic curve, then Υ has parabolic points.
This part exmaine in what conditions the sweeping surfaces are developable surfaces. Therefore, we analyze the case that the profile curve r(u) degenerates into a line. Then, we have the following developable surface
S:P(s,u)=γ(s)+uζ2(s),u∈R. | (3.20) |
We also have that
S⊥:P⊥(s,u)=γ(s)+uζ1(s),u∈R | (3.21) |
It is easy to show P(s,0)=α(s) (resp. P⊥(s,0)=α(s)), 0≤s≤L, that is, the surface S (resp. S⊥) interpolate the curve γ(s). Furthermore, since
Ps×Pu:=−(1−uκ2)ζ1(s), | (3.22) |
then S⊥ is the normal developable surface of S along γ(s). Hence, the curve γ(s) is a curvature line on S (resp. S⊥).
Theorem 3.1. Let Υ be the sweeping surface expressed by Eq (3.6). Then we have the following:
(1) the developable surfaces S and S⊥ intersect along γ(s) at a right angle,
(2) the curve γ(s) is a curvature line on S and S⊥.
Theorem 3.2. (Existence and uniqueness). Under the above notations there exists a unique developable surface represented by Eq (3.19).
Proof. For the existence, we have the developable represented by Eq (3.19). Furthermore, since S is a ruled surface, we may write that
{S:P(s,u)=γ(s)+uζ(s),u∈R,η(s)=η1(s)ζ1+η2(s)ζ2+η3(s)ζ,‖η(s)‖2=η21+η22+η23=1, η′(s)≠0. | (3.23) |
It can be immediately seen that S is developable iff
det(γ′,η,η′)=0⇔η1η′2−η2η′1+η3(η1κ2−η2κ1)=0. | (3.24) |
On the other hand, in view of Eq (3.21), we have
(Ps×Pu)(s,u)=−ψ(s,u)ζ1, | (3.25) |
where θ=θ(s,u) is a differentiable function. Furthermore, the normal vector Ps×Pv at the point (s,0) is
(Ps×Pu)(s,0)=−η2ζ1+η1ζ2. | (3.26) |
Thus, from Eqs (3.24), and (3.25), one finds that:
η1=0, and η2=θ(s,0), | (3.27) |
which follows from Eq (3.23) that η2η3κ1=0, which leads to η2η3=0, with κ1≠0. If (s,0) is a regular point (i.e., θ(s,0)≠0), then η2(s)≠0, and η3=0. Therefore, we obtain η(s)=ζ2. This means that uniqueness holds.
As an application (such as flank milling or cylindrical milling), during the movement of the RMDF along γ, let a cylindrical cutter be rigidly linked to this frame. Then the equation of a set of cylindrical cutters, which is defined by the movement of cylindrical cutter along γ(s), can be gotten as follows:
Sf:¯P(s,u)=P(s,u)+ρζ1(s), | (3.28) |
where ρ denotes cylindrical cutter radius. This surface is a developable surface offset of the surface P(s,u). The equation of Sf, can therefore be written as:
Sf:¯P(s,u)=γ(s)+uζ2(s)+ρζ1(s). | (3.29) |
The normal vector of cylindrical cutter can be represented as
uf(s,0)=¯PsׯPu‖¯PsׯPu‖=ζ1(s). | (3.30) |
Also, from Eq (3.27), we have
S:P(s,u)=¯P(s,u)−ρζ1(s). | (3.31) |
The derivative of Eq (3.30) with respect to s can be derived as follows
¯Ps(s,u)=Ps(s,u)−(ρω)×ζ1. | (3.32) |
Equation (3.22) shows that the vector ¯Ps(s,u) is orthogonal to the normal vector ζ1. And, the vector ζ1 is orthogonal to the tool axis vector ζ(s). Subsequently, the envelope surface of the cylindrical cutter and the developable surface P(s,u) have the common normal vector and the distance between the two surfaces is cylindrical cutter radius ρ. Hence, we can draw a conclusion as follows:
Proposition 3.3. Consider a developable surface S defined by Eq (3.19). Let Sf be the envelope surface of cylindrical cutter at distance ρ. Then the two surfaces S and Sf are offset developable surfaces.
As it is will known, there are three types of developable surfaces, the given curve can be distributed into three kinds correspondingly[12,13,14,15]. In what follows, we will discuss the relationship between the given curve γ(s)∈M and its isoparametric developable surface. The first case is when,
ζ2×ζ′2=0⇔κ2ζ1=0. | (3.33) |
In this situation, S is referred to as a cylindrical surface. Since ζ1 is a nonzero unit vector, then Υ is a cylindrical surface iff
κ2=0⇔κgcosϑ−κnsinϑ=0⇔ϑ=tan−1(κgκn),κn≠0. | (3.34) |
Similarly, we can also have ζ2×ζ′2≠0. In this situation, S is referred to as a non-cylindrical surface. Therefore, the first derivative of the directrix is
γ′(s)=c′(s)+σ(s)ζ′2(s)+σ′(s)ζ2(s), | (3.35) |
where c′ is the first derivative of the striction curve, σ(s) is a smooth function. By an immediate calculation, we can show that
det(c′,ζ2,ζ′2)=<c′,ζ×ζ′2>=0. | (3.36) |
Then the next two situations hold:
The first situation is when the first derivative of the striction curve is c′=0. Geometrically this position implies that the striction curve degenerates to a point, and S becomes a cone; the striction point of a cone is generally referred to as the vertex. By using Eqs (3.2) and (3.34) we have that S is a cone iff there exists a fixed point c and a function σ(s) such that σκ2=−1, σ′=0, which imply that
σ(s)=const.=1κ2⇔κgcosϑ−κnsinϑ=κg0cosϑ0−κn0sinϑ0. | (3.37) |
The second situation is when c′≠0, that is,
σ(s)=const.≠1κ2⇔κgcosϑ−κnsinϑ≠κg0cosϑ0−κn0sinϑ0. | (3.38) |
From Eq (3.35), we have <c′,ζ2×ζ′2>=0, that is, c′∈Sp{ζ2, ζ′2}. The condition for c to be striction curve is therefore equivalent to c′ and ζ′2 are perpendicular to each other. Therefore, we may conclude that the ruling is parallel to the first derivative of the striction curve, which is also the tangent of the striction curve. This ruled surface is referred too as a tangent ruled surface. So, the surface S is a tangent surface iff there exists a curve c(s) so that σ(s)=const.≠1κ2.
In this subsection, as an application of our main results, we give the following examples.
Example 1. Let M be a hyperboloid of one sheet defined by
M:R(s,u)=(coss−u√2coss,sins+u√2sins,u√2). |
It is easy to see that γ(s)=(coss,sins,0) lies on M. Then, we have the Darboux frame as follows:
e1(s)=(−sins,coss,0),e2(s)=(0,0,1),e3(s)=(coss,sins,0). |
The normal curvature, the geodesic curvature, and the geodesic torsion of γ(s) on M, respectively, are
κn=−1, and κg=τg=0. |
Then ϑ(s)=ϑ0 is a constant, moreover,
ζ1(s)=(sinϑ0coss,sinϑ0sins,cosϑ0),ζ2(s)=(cosϑ0coss,cosϑ0sins,−sinϑ0),κ1(s)=−sinϑ0, and κ2(s)=cosϑ0. |
1) If we take ϑ0=π2(κ2(s)=0), then we immediately obtain a sweeping surface given by
Υ:q(s,u)=((1+cosu)coss,(1+cosu)sins,−sinu). |
The graphs of the surfaces M, Υ, and M∪Υ are shown in Figure 1; 0≤u,s≤2π. Obviously, κ2(s)=0 satisfies Eq (3.33), and the developable surface
S:P(s,u)=(coss,sins,−u)+u(0,0,−1)=(coss,sins,−u) |
is a cylinder with γ(s) as a curvature line; 0≤s≤2π, and −1≤u≤1 (Figure 2).
2) In the case of ϑ0=π4(κ2(s)=const.), we obtain a sweeping surface given by
Υ:q(s,u)=((1+sinu+cosu)coss,(1+sinu+cosu)sins,(cosu−sinu)). |
The graphs of the surfaces M, Υ, and M∪Υ are shown in Figure 3; 0≤u,s≤2π. Also, the developable surface
S:P(s,u)=(coss,sins,−u)+u(0,0,−1)=(coss,sins,−u) |
is a cone with γ(s) as a curvature line; 0≤s≤2π, and −5≤u≤2 (Figure 4).
Example 2. Consider the tubular surface parameterized by
M:R(s,u)=(coss√2+√2sinu,sins√2+√2cosu,s√2), |
where 0≤u,s≤2√2π. It is clear that γ(s)=(coss√2,sins√2,s√2) lies on M. By a similar procedure as in Example 1, we have
e1(s)=1√2(−sins√2,coss√2,1√2),e2(s)=1√2(−coss√2+1√2sins√2,−sins√2−1√2coss√2,1√2),e3(s)=1√2(coss√2+1√2sins√2,sins√2−1√2coss√2,1√2),κn=κg=1√2, and τg=12. |
Then ϑ(s)=−s2+ϑ0. If we choose ϑ0=0, for example, we have
ζ1(s)=(1√2[cos(s√2−s2)+sin(s√2−s2)](cos(s2)−sin(s2))sin(s√2)−1√2(cos(s2)+sin(s2))cos(s√2)1√2(cos(s2)+sin(s2))),ζ2(s)=(1√2[cos(s√2−s2)−sin(s√2−s2)](cos(s2)+sin(s2))sin(s√2)−1√2(cos(s2)−sin(s2))cos(s√2)−1√2(cos(s2)−sin(s2))),κ1(s)=12√2(sins2+coss2), and κ2(s)=12√2(sins2−coss2). |
Therefore, the sweeping surface is
Υ:q(s,u)=(coss√2+1√2[cos(s√2−s2+u)+sin(s√2−s2+u)]sins√2+[(cos(s2−u)−sin(s2+u))sin(s√2)−1√2(cos(s2−u)+sin(s2+u))cos(s√2)]s√2−1√2(cos(s2−u)+sin(s2−u))). |
The graphs of the surfaces M, Υ, and M∪Υ are shown in Figure 5; 0≤u,s≤2√2π. In view of κ2(s)≠κ2(s0) and Eq (3.37), the developable surface
S:P(s,u)=(coss√2+u√2[cos(s√2−s2)+sin(s2−s√2)]sins√2+u[(coss2+sins2)sins√2−1√2(coss2−sins2)coss√2]s√2−u√2(coss2−sins2)) |
is a tangent surface with γ(s) as a curvature line; 0≤s≤2√2π, and −1≤u≤1 (Figure 6).
This paper introduce and study sweeping surface with a new RMDF associated with a curve on the surface. The paper further investigated the problem of requiring the sweeping surface is a developable surface. There are several opportunities for further work. An analogue of the problem addressed in this paper may be consider for surfaces in Minkowski 3-space. We will study this problem in the future.
All of the data are available within the paper. The authors have no conflicts of interest.
[1] | Cherlet M, Hutchinson C, Reynolds J, et al. (2018) World atlas of desertification. Luxembourg: Publication office of the european union. https://data.europa.eu/doi/10.2760/9205 |
[2] |
Zhou L (2016) Desert amplification in a warming climate. Sci Rep 6: 1-13. https://doi.org/10.1038/srep31065 ![]() |
[3] |
Huang J, Yu H, Guan X, et al. (2015) Accelerated dryland expansion under climate change. Nat Clim Chang 6: 166-171. https://doi.org/10.1038/nclimate2837 ![]() |
[4] |
Tong H (2020) Iron mineralogy in the Chinese seserts and mongolian gobi: Impact for the biogeochemical cycle. Int J Earth Sci Geophys 6: 034. https://doi.org/10.35840/2631-5033/1834 ![]() |
[5] |
Eberwein JR, Homyak PM, Carey CJ, et al. (2020) Large nitrogen oxide emission pulses from desert soils and associated microbiomes. Biogeochemistry 149: 239-250. https://doi.org/10.1007/s10533-020-00672-9 ![]() |
[6] |
Peel MC, Finlayson BL, McMahon TA (2007) Updated world map of the Köppen-Geigerclimate classification. Hydrol Earth Syst Sci 11: 1633-1644. https://doi.org/10.5194/hessd-4-439-2007 ![]() |
[7] |
Makhalanyane TP, Valverde A, Gunnigle E, et al. (2015) Microbial ecology of hot desert edaphic systems. FEMS Microbiol Rev 39: 203-221. https://doi.org/10.1093/femsre/fuu011 ![]() |
[8] | Singh P, Jain K, Desai C, et al. (2019) Microbial community dynamics of extremophiles/extreme environment. Microb Divers Genomic Era 323–332. https://doi.org/10.1016/B978-0-12-814849-5.00018-6 |
[9] |
Maestre FT, Delgado-Baquerizo M, Jeffries TC, et al. (2015) Increasing aridity reduces soil microbial diversity and abundance in global drylands. Proc Natl Acad Sci USA 112: 15684-15689. https://doi.org/10.1016/B978-0-12-814849-5.00018-6 ![]() |
[10] | Abrevaya XC, Anderson R, Arney G, et al. (2016) The astrobiology primer v2.0. AStro 16: 561-653. https://doi.org/10.1089/ast.2015.1460 |
[11] |
Hallsworth JE, Mancinelli RL, Conley CA, et al. (2021) Astrobiology of life on Earth. Environ Microbiol 23: 3335-3344. https://doi.org/10.1111/1462-2920.15499 ![]() |
[12] |
Gmach MR, Cherubin MR, Kaiser K, et al. (2018) Processes that influence dissolved organic matter in the soil: a review. Sci Agric 77: e20180164. https://doi.org/10.1590/1678-992X-2018-0164 ![]() |
[13] |
Delgado-Baquerizo M, Maestre FT, Gallardo A, et al. (2013) Aridity modulates N Availability in arid and semiarid mediterranean grasslands. PLoS One 8: e598. https://doi.org/10.1371/journal.pone.0059807 ![]() |
[14] | Abdel-Aziz SM (2014) Universal journal of pharmacy. Univers J Pharm 02: 78-83. https://doi.org/10.1155/2014/524930 |
[15] |
Leung PM, Bay SK, Meier D V, et al. (2020) Energetic basis of microbial growth and persistence in desert ecosystems. mSystems 5: 1-14. https://doi.org/10.1128/mSystems.00495-19 ![]() |
[16] |
Molina-menor E, Gimeno-valero H, Pascual J, et al. (2021) High culturable bacterial diversity from a European desert : The Tabernas desert. Front Microbiol 11: 1-15. https://doi.org/10.3389/fmicb.2020.583120 ![]() |
[17] |
Zhang W, Bahadur A, Sajjad W, et al. (2021) Bacterial diversity and community composition distribution in Cold-Desert habitats of qinghai–tibet Plateau, China. Microorganisms 9: 262. https://doi.org/10.3390/microorganisms9020262 ![]() |
[18] | Wu MH, Zhang GS, Chen T, et al. (2017) Advance in lithophilous microorganisms. J Microbiol 37: 64-73. https://doi.org/10.3969/j.issn.1005-7021.2017.04.011 |
[19] |
Aislabie JM, Lau A, Dsouza M, et al. (2013) Bacterial composition of soils of the lake Wellman area, Darwin Mountains, Antarctica. Extremophiles 17: 775-786. https://doi.org/10.1007/s00792-013-0560-6 ![]() |
[20] | Kour D, Rana KL, Kaur T, et al. (2020) Extremophiles for hydrolytic enzymes productions: Biodiversity and potential biotechnological applications. Bioprocessing for biomolecules production . UK: Wiley & Sons 321-372. https://doi.org/10.1002/9781119434436.ch16 |
[21] |
Yadav AN, Sachan SG, Verma P, et al. (2015) Prospecting cold deserts of north western himalayas for microbial diversity and plant growth promoting attributes. J Biosci Bioeng 119: 683-693. https://doi.org/10.1016/j.jbiosc.2014.11.006 ![]() |
[22] |
Merino N, Aronson HS, Bojanova DP, et al. (2019) Living at the extremes: Extremophiles and the limits of life in a planetary context. Front Microbiol 10: 780. https://doi.org/10.31223/OSF.IO/8EAY6 ![]() |
[23] |
Orellana R, Macaya C, Bravo G, et al. (2018) Living at the frontiers of life: Extremophiles in Chile and their potential for bioremediation. Front Microbiol 9: 1-25. https://doi.org/10.3389/fmicb.2018.02309 ![]() |
[24] |
Chen GQ, Jiang XR (2018) Next generation industrial biotechnology based on extremophilic bacteria. Curr Opin Biotechnol 50: 94-100. https://doi.org/10.1016/j.copbio.2017.11.016 ![]() |
[25] | Allied market researchEnzymes market size & industry forecast by 2027, 2021 (2021). Available from: https://www.alliedmarketresearch.com/enzymes-market |
[26] | BCC ResearchGlobal enzymes market in industrial applications, 2021 (2021). Available from: https://www.bccresearch.com/market-research/biotechnology/global-markets-for-enzymes-in-industrial-applications.html |
[27] |
Li S, Yang X, Yang S, et al. (2012) Technology prospecting on enzymes: Application, marketing and engineering. Comput Struct Biotechnol J 2: e201209017. https://doi.org/10.5936/csbj.201209017 ![]() |
[28] |
Rigoldi F, Donini S, Redaelli A, et al. (2018) Review: Engineering of thermostable enzymes for industrial applications. APL Bioeng 2: 1-17. https://doi.org/10.1063/1.4997367 ![]() |
[29] |
Kuske RC, Barns MS, Busch DJ (1997) Diverse uncultivated bacterial groups from soils of the arid southwestern United States that are present in many geographic regions. Appl Environ Microbiol 63: 3614-3621. https://doi.org/10.1128/aem.63.9.3614-3621.1997 ![]() |
[30] | Funk CC, Peterson PJ, Landsfeld MF, et al. (2014) A Quasi-Global precipitation time series for drought monitoring. US Geol Surv Data Ser 832: 4. https://doi.org/10.3133/ds832 |
[31] |
Kumar S, Stecher G, Li M, et al. (2018) MEGA X: Molecular evolutionary genetics analysis across computing platforms. Mol Biol Evol 35: 1547-1549. https://doi.org/10.1093/molbev/msy096 ![]() |
[32] |
Amoozegar MA, Malekzadeh F, Malik KA (2003) Production of amylase by newly isolated moderate halophile, Halobacillus sp. strain MA-2. J Microbiol Methods 52: 353-359. https://doi.org/10.1016/S0167-7012(02)00191-4 ![]() |
[33] |
Kembhavi AA, Kulkarni A, Pant A (1993) Salt-tolerant and thermostable alkaline protease from Bacillus subtilis NCIM No. 64. Appl Biochem Biotechnol 38: 83-92. https://doi.org/10.1007/BF02916414 ![]() |
[34] |
Jette JF, Ziomek E (1994) Determination of lipase activity by a rhodamine-triglyceride-agarose assay. Anal Biochem 219: 256-260. https://doi.org/10.1006/abio.1994.1265 ![]() |
[35] |
Teather RM, Wood PJ (1982) Use of Congo red-polysaccharide interactions in enumeration and characterization of cellulolytic bacteria from the bovine rumen. Appl Environ Microbiol 43: 777-780. https://doi.org/10.1128/aem.43.4.777-780.1982 ![]() |
[36] |
Osman JR, Fernandes G, Regeard C, et al. (2017) Examination of the bacterial biodiversity of coastal eroded surface soils from the Padza de Dapani (Mayotte Island). Geomicrobiol J 35: 355-365. https://doi.org/10.1080/01490451.2017.1368740 ![]() |
[37] |
Crits-Christoph A, Robinson CK, Barnum T, et al. (2013) Colonization patterns of soil microbial communities in the Atacama desert. Microbiome 1: 1-13. https://doi.org/10.1186/2049-2618-1-28 ![]() |
[38] |
Ronca S, Ramond JB, Jones BE, et al. (2015) Namib desert dune/interdune transects exhibit habitat-specific edaphic bacterial communities. Front Microbiol 6: 1-12. https://doi.org/10.3389/fmicb.2015.00845 ![]() |
[39] |
Rao S, Chan Y, Bugler-Lacap DC, et al. (2016) Microbial diversity in soil, sand dune and rock substrates of the Thar Monsoon Desert, India. Indian J Microbiol 56: 35-45. https://doi.org/10.1007/s12088-015-0549-1 ![]() |
[40] |
Liu S, Wang T, Lu Q, et al. (2021) Bioprospecting of soil-derived actinobacteria along the Alar-Hotan desert highway in the Taklamakan desert. Front Microbiol 12: 604999. https://doi.org/10.3389/fmicb.2021.604999 ![]() |
[41] | Heulin T, De Luca G, Barakat M, et al. (2017) Bacterial adaptation to hot and dry deserts. Adaption of microbial life to environmental extremes : 69-85. https://doi.org/10.1007/978-3-319-48327-6_4 |
[42] |
Suzuki H (2018) Peculiarities and biotechnological potential of environmental adaptation by Geobacillus species. Appl Microbiol Biotechnol 102: 10425-10437. https://doi.org/10.1007/s00253-018-9422-6 ![]() |
[43] |
Hernández-González IL, Moreno-Hagelsieb G, Olmedo-Álvarez G (2018) Environmentally-driven gene content convergence and the Bacillus phylogeny. BMC Evol Biol 18: 1-15. https://doi.org/10.1186/s12862-018-1261-7 ![]() |
[44] |
Peix A, Ramírez-Bahena MH, Velázquez E (2018) The current status on the taxonomy of Pseudomonas revisited: An update. Infect Genet Evol 57: 106-116. https://doi.org/10.1016/j.meegid.2017.10.026 ![]() |
[45] |
Hadjithomas M, Chen IMA, Chu K, et al. (2017) IMG-ABC: New features for bacterial secondary metabolism analysis and targeted biosynthetic gene cluster discovery in thousands of microbial genomes. Nucleic Acids Res 45: D560-D565. https://doi.org/10.1093/nar/gkw1103 ![]() |
[46] |
Belov AA, Cheptsov VS, Vorobyova EA (2018) Soil bacterial communities of sahara and gibson deserts: Physiological and taxonomical characteristics. AIMS Microbiol 4: 685-710. https://doi.org/10.3934/microbiol.2018.4.685 ![]() |
[47] |
Alotaibi MO, Sonbol HS, Alwakeel SS, et al. (2020) Microbial diversity of some sabkha and desert sites in Saudi Arabia. Saudi J Biol Sci 27: 2778-2789. https://doi.org/10.1016/j.sjbs.2020.06.038 ![]() |
[48] |
Yadav AN, Yadav N, Sachan SG, et al. (2019) Biodiversity of psychrotrophic microbes and their biotechnological applications. J Appl Biol Biotechnol 7: 99-108. https://doi.org/10.7324/JABB.2019.70415 ![]() |
[49] |
Mukhia S, Khatri A, Acharya V, et al. (2021) Genomics comparative genomics and molecular adaptational analysis of arthrobacter from Sikkim Himalaya provided insights into its survivability under multiple high-altitude stress. Genomics 113: 151-158. https://doi.org/10.1016/j.ygeno.2020.12.001 ![]() |
[50] |
Zhang B, Kong W, Nan W, et al. (2016) Bacterial diversity and community along the succession of biological soil crusts in the Gurbantunggut desert, northern China. J Basic Microbiol 56: 670-679. https://doi.org/10.1002/jobm.201500751 ![]() |
[51] |
Gommeaux M, Barakat M, Montagnac G, et al. (2010) Mineral and bacterial diversities of desert sand grains from south-east Morocco. Geomicrobiol J 27: 76-92. https://doi.org/10.1080/01490450903393066 ![]() |
[52] |
Bhatt HB, Gohel SD, Singh SP (2018) Phylogeny, novel bacterial lineage and enzymatic potential of haloalkaliphilic bacteria from the saline coastal desert of little rann of Kutch, Gujarat, India. 3 Biotech 8: 1-12. https://doi.org/10.1007/s13205-017-1075-0 ![]() |
[53] | Kashi FJ, Owlia P, Amoozegar MA, et al. (2014) Diversity of cultivable microorganisms in the eastern part of Urmia salt lake, Iran. J Microbiol Biotechnol Food Sci 4: 36-43. https://doi.org/10.15414/jmbfs.2014.4.1.36-43 |
[54] |
Osman JR, Wang Y, Jaubert C, et al. (2021) The bacterial communities of surface soils from desert sites in the eastern Utah (USA) portion of the Colorado Plateau. Microbiol Res 244: 126664. https://doi.org/10.1016/j.micres.2020.126664 ![]() |
[55] |
An S, Couteau C, Luo F, et al. (2013) Bacterial diversity of surface sand samples from the Gobi and Taklamaken deserts. Microbiol Ecol 66: 850-860. https://doi.org/10.1007/s00248-013-0276-2 ![]() |
[56] |
Aabed K, Almutairi A, Al-shwuair A, et al. (2021) Diversity and distribution of thermophiles and thermo- tolerant bacteria in the soil samples obtained from different regions in Saudi Arabia. Biosci Biotechnol Res ASIA 18: 163-172. https://doi.org/10.13005/bbra/2904 ![]() |
[57] |
Hanna AL, Youssef HH, Amer WM, et al. (2013) Diversity of bacteria nesting the plant cover of north Sinai deserts, Egypt. J Adv Res 4: 13-26. https://doi.org/10.1016/j.jare.2011.11.003 ![]() |
[58] |
Rittner M, Vermeesch P, Carter A, et al. (2016) The provenance of Taklamakan desert sand. Earth Planet Sci Lett 437: 127-137. https://doi.org/10.1016/j.epsl.2015.12.036 ![]() |
[59] |
Perfumo A, Marchant R (2010) Global transport of thermophilic bacteria in atmospheric dust. Environ Microbiol Rep 2: 333-339. https://doi.org/10.1111/j.1758-2229.2010.00143.x ![]() |
[60] |
Weil T, De Filippo C, Albanese D, et al. (2017) Legal immigrants: Invasion of alien microbial communities during winter occurring desert dust storms. Microbiome 5: 1-11. https://doi.org/10.1186/s40168-017-0249-7 ![]() |
[61] |
Sakrouhi I, Belfquih M, Sbabou L, et al. (2016) Recovery of symbiotic nitrogen fixing acacia rhizobia from Merzouga desert sand dunes in south east Morocco-Identification of a probable new species of ensifer adapted to stressed environments. Syst Appl Microbiol 39: 122-131. https://doi.org/10.1016/j.syapm.2016.01.001 ![]() |
[62] |
Buckley E, Lee KC, Higgins CM, et al. (2019) Whole-Genome sequences of one arthrobacter strain and three pseudarthrobacter strains isolated from the Namib desert. Microbiol Resour Announc 8: e00885-19. https://doi.org/10.1128/MRA.00885-19 ![]() |
[63] |
Röttig A, Hauschild P, Madkour MH, et al. (2020) Corrigendum to “Analysis and optimization of triacylglycerol synthesis in novel oleaginous Rhodococcus and Streptomyces strains isolated from desert soil” (Journal of Biotechnology (2016) 225 (48–56), (S016816561630147X), (10.1016/j.jbiotec.2016.03.040)). J Biotechnol 310: 114. https://doi.org/10.1016/j.jbiotec.2020.01.011 ![]() |
[64] |
Sun Y, Shi Y, Wang H, et al. (2018) Diversity of bacteria and the characteristics of actinobacteria community structure in Badain Jaran desert and Tengger desert of China. Front Microbiol 9: 1-14. https://doi.org/10.3389/fmicb.2018.01068 ![]() |
[65] |
Qin S, Li WJ, Klenk HP, et al. (2019) Editorial: Actinobacteria in special and extreme habitats: Diversity, function roles and environmental adaptations, second edition. Front Microbiol 10: 944. https://doi.org/10.3389/fmicb.2019.00944 ![]() |
[66] |
Van Elsas JD, Chiurazzi M, Mallon CA, et al. (2012) Microbial diversity determines the invasion of soil by a bacterial pathogen. Proc Natl Acad Sci USA 109: 1159-1164. https://doi.org/10.1073/pnas.1109326109 ![]() |
[67] |
Azua-Bustos A, Urrejola C, Vicuña R (2012) Life at the dry edge: Microorganisms of the Atacama desert. FEBS Lett 586: 2939-2945. https://doi.org/10.1016/j.febslet.2012.07.025 ![]() |
[68] |
Amin A, Ahmed I, Khalid N, et al. (2020) Insights on comparative bacterial diversity between different arid zones of Cholistan desert, Pakistan. 3 Biotech 10: 224. https://doi.org/10.1007/s13205-020-02204-6 ![]() |
[69] |
Janssen PH (2006) Identifying the dominant soil bacterial taxa in libraries of 16S rRNA and 16S rRNA genes. Appl Environ Microbiol 72: 1719-1728. https://doi.org/10.1128/AEM.72.3.1719-1728.2006 ![]() |
[70] |
Pasternak Z, Al-Ashhab A, Gatica J, et al. (2013) Spatial and temporal biogeography of soil microbial communities in arid and semiarid regions. PLoS One 8. https://doi.org/10.1371/journal.pone.0069705 ![]() |
[71] |
Mohammadipanah F, Wink J (2016) Actinobacteria from arid and desert habitats: Diversity and biological activity. Front Microbiol 6: 1-10. https://doi.org/10.3389/fmicb.2015.01541 ![]() |
[72] |
Hu Q, Chu X, Xiao M, et al. (2016) Arthrobacter deserti sp. nov., isolated from a desert soil sample. Int J Syst Evol Microbiol 66: 2035-2040. https://doi.org/10.1099/ijsem.0.000986 ![]() |
[73] | Greenstein JLPH Developing cell surface-display of enzymes in thermophilic Geobacillus (2020). Available from: https://repository.lib.ncsu.edu/bitstream/handle/1840.20/37441/etd.pdf?sequence=1&isAllowed=y |
[74] |
Zhang DC, Liu HC, Xin YH, et al. (2009) Planomicrobium glaciei sp. nov., a psychrotolerant bacterium isolated from a glacier. Int J Syst Evol Microbiol 59: 1387-1390. https://doi.org/10.1099/ijs.0.002592-0 ![]() |
[75] | LI Jian-hui, LU Pan-pan ZY Northern horticulture, studies on physiological characteristics and identification of a Planomicrobium, 2010 (2010). Available from: https://en.cnki.com.cn/Article_en/CJFDTotal-BFYY201017065.htm |
[76] |
Belov AA, Cheptsov VS, Vorobyova EA, et al. (2019) Stress-tolerance and taxonomy of culturable bacterial communities isolated from a central mojave desert soil sample. Geosciences 9: 166. https://doi.org/10.3390/geosciences9040166 ![]() |
[77] |
Raddadi N, Giacomucci L, Marasco R, et al. (2018) Bacterial polyextremotolerant bioemulsifiers from arid soils improve water retention capacity and humidity uptake in sandy soil. Microb Cell Fact 17: 1-12. https://doi.org/10.1186/s12934-018-0934-7 ![]() |
[78] |
Saker R, Meklat A, Bouras N, et al. (2015) Diversity and antagonistic properties of culturable halophilic actinobacteria in soils of two arid regions of septentrional Sahara: M'zab and Zibans. Ann Microbiol 65: 2241-2253. https://doi.org/10.1007/s13213-015-1065-6 ![]() |
[79] | Alzubaidy HS (2020) Induction of salt tolerance by Enterobacter sp. SA187 in the model organism arabidopsis thaliana. KAUST Res Repos . https://doi.org/10.25781/KAUST-Z710H |
[80] |
Kambourova M (2018) Thermostable enzymes and polysaccharides produced by thermophilic bacteria isolated from Bulgarian hot springs. Eng Life Sci 18: 758-767. https://doi.org/10.1002/elsc.201800022 ![]() |
[81] | Shahid Raza, Ayesha Ameen (2017) Halophiles and their important enzymes used for biotechnology application. LGU J Lifes Sci 1. Available from: https://ojs.lgu.edu.pk/index.php/lgujls/article/download/670/613 |
[82] |
Ding D, Chen G, Wang B, et al. (2013) Culturable actinomycetes from desert ecosystem in northeast of Qinghai-Tibet Plateau. Ann Microbiol 63: 259-266. https://doi.org/10.1007/s13213-012-0469-9 ![]() |
[83] |
Charlesworth J, P. Burns B (2016) Extremophilic adaptations and biotechnological applications in diverse environments. AIMS Microbiol 2: 251-261. https://doi.org/10.3934/microbiol.2016.3.251 ![]() |
[84] |
Selim SA (2012) Novel thermostable and alkalitolerant amylase production by Geobacillus stearothermophilus HP 3. Nat Prod Res 26: 1626-1630. https://doi.org/10.1080/14786419.2011.583923 ![]() |
[85] |
Berekaa MM, Zaghloul TI, Abdel-Fattah YR, et al. (2009) Production of a novel glycerol-inducible lipase from thermophilic Geobacillus stearothermophilus strain-5. World J Microbiol Biotechnol 25: 287-294. https://doi.org/10.1007/s11274-008-9891-3 ![]() |
[86] |
Verma S, Kumar R, Kumar P, et al. (2020) Cloning, characterization, and structural modeling of an extremophilic bacterial lipase isolated from saline habitats of the Thar desert. Appl Biochem Biotechnol 192: 557-572. https://doi.org/10.1007/s12010-020-03329-3 ![]() |
[87] |
Dhyani A, Gururani R, Selim SA, et al. (2017) Production of industrially important enzymes by thermobacilli isolated from hot springs of INDIA. Res Biotechnol 8: 19-28. https://doi.org/10.25081/rib.2017.v8.3594 ![]() |
[88] | Abbasi MH, Mehmood R, Khawar MB, et al. (2020) Alkalophilic protease producing bacteria and some biotechnological potentials. RADS J Biol Res Appl Sci 11: 135-142. https://doi.org/10.37962/jbas.v11i2.280 |
[89] | Ward RD, Stajich JE, Johansen JR, et al. (2021) Metagenome sequencing to explore phylogenomics of terrestrial cyanobacteria. Microbiol Resour Announc 10. https://doi.org/10.1128/MRA.00258-21 |
[90] |
Wang Y, Osman JR, DuBow MS (2020) Bacterial communities on the surface of the mineral sandy soil from the desert of maine (USA). Curr Microbiol 77: 1429-1437. https://doi.org/10.1007/s00284-020-01946-z ![]() |
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