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Biophys J, January 2002, p. 264-273, Vol. 82, No. 1


and
*Department of Biochemistry, Molecular Biology and Cell Biology,
Northwestern University, Evanston, Illinois 60208;
Department of Biochemistry, McMaster University,
Hamilton, Ontario L8N 3Z5, Canada; and
Institute of
Theoretical and Experimental Biophysics, Pushchino, Moscow Region,
142290, Russia
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ABSTRACT |
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The influence on the melting of calf thymus and plasmid
DNA of cationic lipids of the type used in gene therapy was studied by
ultraviolet spectrophotometry and differential scanning calorimetry. It
was found that various membrane-forming cationic lipids are able to
protect calf thymus DNA against denaturation at 100°C. After
interaction with cationic lipids, the differential scanning calorimetry
melting profile of both calf thymus and plasmid DNA revealed two major
components, one corresponding to a thermolabile complex with transition
temperature, Tm(labile), close to that of
free DNA and a second corresponding to a thermostable complex with a
transition temperature, Tm(stable), at 105 to 115°C. The parameter Tm(stable) did not
depend on the charge ratio, R(±). Instead, the amount
of thermostable DNA and the enthalpy ratio
H(stable)/
H(labile)
depended upon R(±) and conditions of complex formation.
In the case of O-ethyldioleoylphosphatidylcholine, the
cationic lipid that was the main subject of the investigation, the
maximal stabilization of DNA exceeded 90% between
R(±) = 1.5 and 3.0. Several other lipids gave at
least 75% protection in the range R(±) = 1.5 to
2.0. Centrifugal separation of the thermostable and thermolabile
fractions revealed that almost all the transfection activity was
present at the thermostable fraction. Electron microscopy of the
thermostable complex demonstrated the presence of multilamellar membranes with a periodicity 6.0 to 6.5 nm. This periodic multilamellar structure was retained at temperatures as high as 130°C. It is concluded that constraint of the DNA molecules between oppositely charged membrane surfaces in the multilamellar complex is responsible for DNA stabilization.
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INTRODUCTION |
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Complexes of DNA vectors with cationic lipids
(lipoplexes) are widely used for transfection of cultural cells and
have been successfully applied in modern gene therapy. Their physical
properties and structure have been increasingly studied since the
synthesis of the first effective cationic lipid transfection agent,
DOTMA, in 1987 (Felgner et al., 1987
). A number of investigators have found that the structure of lipoplexes and their transfection activity
varies considerably, depending, for example, on aspects of the
preparation protocol, such as the size of liposomes, positive to
negative charge ratio, and even the sequence of addition of DNA and
lipid (Chesnoy and Huang, 2000
; Lin et al., 2000
; Kennedy et al.,
2000
).
The first electron microscopy studies of DNA-cationic lipid complexes
revealed the presence of various tube-like structures of lipid, the
presence of which was initiated by interaction with DNA molecules
(Gustafsson et al., 1995
; Lasic et al., 1997
; Bhattacharya and Mandal,
1998
). Nonlamellar structures, coexisting with membrane vesicles, were
observed later by many authors (Sternberg et al., 1994
, 1998
; Zabner et
al., 1995
; Wheeler et al., 1996
; Xu et al., 1999
). Increasingly,
however, evidence has accumulated that indicates that multilamellar
structures consisting of many parallel lipid bilayers alternating with
monolayers of DNA helices predominate in a number of complexes of DNA
with cationic lipids (Gustafsson et al., 1995
; Lasic and Templeton,
1996
; Lasic et al., 1997
; Battersby et al., 1998
; MacDonald et al.,
1999
). Hexagonally ordered lipid tubes containing DNA molecules were
also observed in some cases (Ghirlando et al., 1992
; Tarahovsky et al.,
1996
; Mel'nikova et al., 1999
). The coexistence of multilamellar
structures with hexagonally ordered lipid tubes was confirmed by
small-angle x-ray scattering (Rädler et al., 1997
; Lasic et al.,
1997
; Koltover et al., 1998
). It is possible that a wide range of
different structures normally coexists in a given sample, and different
experimental approaches will be needed to reveal them. Furthermore, the
structure of complexes appears somewhat variable and can depend on
conditions of sample preparation and the proportion of positive and
negative charge. For example, multilamellar complexes predominated in
samples with excess of cationic lipid, whereas with excess negative
charged DNA, unilamellar coated vesicles were present (Huebner et al., 1999
).
It is known that cationic substances influence the physical properties
of DNA. For example, the DNA melting process displays considerable
sensitivity to the presence of mono- and especially polyvalent cations.
A large number of metal cations, including the naturally abundant
K+, Na+,
Ca2+, and Mg2+, can
significantly influence the thermodynamic parameters of the DNA melting
process (Dove and Davidson, 1962
; Eichhorn and Shin, 1968
; Gruenwedel,
1974
; Duguid et al., 1993
, 1995
). These effects may be assumed to be
due to differential interactions of the metal ions, i.e., in general,
any ligand that interacts more strongly with double-stranded than with
single-stranded DNA will influence the thermodynamic parameters of
helix-coil transition and hence also the DNA melting process by
shifting the equilibrium toward stabilization of the helix form
(Bloomfield et al., 2000
). Thus, low and moderate concentrations of
metal cations stabilize DNA and increase the temperature of melting.
There are limits to such effects, however, because high concentrations
of alkaline earths and the transition metal ions cause rupture of
hydrogen bounds, base unstacking, and ultimately decrease of thermal
stability of DNA.
The thermal stability of DNA, its base pairing, as well as the
electrostatic interactions of DNA with some ligands are also sensitive
to the aqueous environment. The extent of hydration of DNA influences
interactions of cations with the DNA phosphate groups and the strength
of base pairing. Some uncharged molecules, polyethylene glycol for
example, can alter water activity and, as consequence, significantly
affect the temperature and free energy of DNA melting (Spink and
Chaires, 1999
). The hydration shell of DNA consists of a specifically
ordered array of ~15 to 20 water molecules per base pair (Rentzeperis
et al., 1993
; Chalikian et al., 1999
). DNA melting is accompanied by
release of four water molecules per base pair and 0.3 to 0.5 Na+ ions per phosphate charge, depending on the
salt concentration (Spink and Chaires, 1999
).
Here we describe thermal stabilization of DNA molecules by cationic amphiphiles. We observed that thermal stabilization of DNA by membrane-forming cationic lipids depends on the charge ratio in a way that it is substantially different from that of the case of water-soluble cationic substances like metal cations. This indicates a fundamental difference in interaction with DNA of cationic water-soluble compounds and cationic membrane surfaces formed by lipid. It is assumed that the structural characteristics of DNA-lipid complexes are important for understanding their physical properties.
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MATERIALS AND METHODS |
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Materials
Tetradecyltrimethylammonium bromide (TTMA),
dimethylaminoethanecarbamoyl cholesterol (DC-Chol), and
highly-polymerized calf thymus DNA were purchased from Sigma (St.
Louis, MO). Dioleoyltrimethylammoniumpropane (DOTAP),
dioleoylphosphatidylcholine (DOPC), and
dioleoylphosphatidylethanolamine (DOPE) were from Avanti Polar Lipids
(Alabaster, AL). Ethyldioleoylphosphatidylcholine (EDOPC) was either
from Avanti as the chloride salt or synthesized as previously described
as the trifluoromethysulfonate salt (Rosenzweig et al., 2000
). Plasmid
pCMVSport
-gal (7853 bp) was purchased from Bayou Biolabs (Harahan,
LA) in quantities sufficient for physical characterization.
DNA preparation
Highly polymerized calf thymus DNA was hydrated overnight in milli-Q water and treated in a 250-W laboratory ultrasound bath for 5 h at 40°C in a sealed glass vial filled with argon. Electrophoresis in 1% agarose of DNA treated in this way revealed the presence of predominantly 6000- to 7000-bp fragments. The DNA fragments were diluted 2 times with 10 mM sodium cacodylate, pH 7.0, or double concentrated Dulbecco phosphate-buffered saline (DPBS), pH 7.2, which contained 1 mM Ca2+, 4 mM K+, 5 mM Mg2+, and 150 mM Na+.
Preparation of liposomes and DNA-lipid complexes
The appropriate volume of a chloroform solution of lipid was transferred to a glass vial and the bulk of the solvent removed under an argon stream. Subsequently the lipid was placed under high vacuum for ~2 h. The dried film was then hydrated in either 5 mM cacodylate, pH 7.0, or DPBS, pH 7.2 and vortexed for a few minutes to yield an apparently homogenous white suspension with a final lipid concentration of 10 mM. Sonicated liposomes were prepared from vortexed liposomes by immersing glass vials containing a few milliliters of sample in an 80-kHz ultrasound bath (Laboratory Supplies Co., Hicksville, NY) for a few minutes. The suspension was saturated with argon before sonication. Stock dispersions of liposomes were added to DNA fragments or plasmid DNA under conditions of continuous magnetic stirring. Sometimes the complexation was accompanied by the formation of a heavy precipitate, in which case, the precipitated complexes were homogenized by 10 to 100 passes through a syringe until a homogenous suspension was formed.
Differential scanning microcalorimetry
Solutions of DNA or dispersions of DNA-lipid complexes were prepared as described above. Complexes prepared from sonicated calf thymus DNA (1 mg/ml) or plasmid DNA (0.5 mg/ml) and a corresponding amount of lipid were analyzed with a VP-DSC Micro Calorimeter (MicroCal Inc, Northampton, MA) at a scan rate of 10°C/h. Additional details on preparation of individual samples are provided below in the Results section. Computer analysis of the differential scanning calorimetry (DSC) data was performed using Origin Scientific plotting software, version 5. Data were analyzed after subtraction of the baseline obtained by scanning with the corresponding buffers in both sample and reference cell. Repeated scans revealed good reproducibility in both the transition maxima and their thermodynamic parameters.
Ultraviolet absorption measurements
The concentration of DNA was determined from ultraviolet (UV)
absorption at 260 nm using the relationship 1.0 absorbance units (A) = 50 µg/ml DNA. For determination of DNA denaturation in DNA-lipid complexes, the appropriate amount of lipid suspension was added to 2 ml
of stock solution containing 50 µM DNA in 5 mM sodium cacodylate, pH
7.0. Glass tubes containing the complexes were immersed in boiling
water for 10 min, cooled to room temperature, and then 1 M sodium
dodecyl sulfate (SDS) was added to a final concentration of 25 mM. The
percentage of native DNA (DNA%nat) was calculated according to:
DNA%nat = 100%(DNAden
DNAs)/(DNAden + DNAnat), in which
DNAden, DNAnat, and DNAs are absorption of denatured, native, and
sample DNA at 260 nm, respectively, in the presence of 25 mM SDS.
Separation and assay of DNA-lipid complexes
Complexes were separated into two fractions by centrifugation in an Eppendorf centrifuge (15,000 rpm at 4°C for 30 min). After removal of the supernatant, the sediment was vigorously suspended in the initial volume of buffer. The amount of DNA in both sediment and supernatant was estimated spectrophotometrically at 260 nm in the presence of 25 mM SDS to diminish light scattering. To assay for lipid content, 1% (lissamine Rhodamine B sulfonyl)-DOPE was added to the liposomes and its concentration determined by measuring absorbance at 560 nm.
Electron microscopy and image analyses
For thin section electron microscopy, complexes of DNA were prepared with cationic lipids containing the unsaturated oleic acid. Complexes were prepared according to the procedure described above. Samples with a 1-mg/ml DNA concentration and a corresponding concentration of lipid in 5 mM cacodylate or DPBS buffers were fixed with 1% osmium tetroxide overnight. Fixation at temperatures above 100°C was performed in screw cap vials heated to the desired temperature in a dry block heater. After 10 to 15 min incubation at the necessary temperature, the osmium tetroxide solution was injected by syringe through a rubber septum. After fixation, the sample was sedimented by centrifugation at 5000 to 8000 rev/min in an Eppendorf centrifuge, postfixed overnight with 1% tannic acid in the buffers mentioned above, dehydrated in series of alcohol and propylene oxide, and embedded in Epon resin according to standard procedures. Thin sections of ~50-nm thickness were cut on a MT6000-XL microtome (RMC, Inc., Tucson, AZ) and observed with a JEM-100CX (JEOL, Peabody, MA) electron microscope. The micrographs (magnification = 250,000) were digitized, and fast Fourier transforms of the selected regions were performed with Scion Image (Scion Corporation Imaging Software, Frederick, MD) for Windows 98.
Transfection assay
The transfection procedure has been described elsewhere
(MacDonald et al., 1999
). In brief, lipid at 1 mg/ml was quickly added to pCMVSport-
-gal plasmid at 0.1 mg/ml to give a 1:1 weight ratio (corresponding to a 3% positive charge excess). Both compounds were in
the DPBS buffer. In some experiments, complexes were separated by
centrifugation as described above. Transfection using both whole
complex and its fractions (supernatant and sediment) was performed on
BHK cells. Cells were grown in 96-well plates, and complex containing 3 µg of DNA was added to each well.
-Galactosidase was assayed after
20 to 24 h using a microtiter plate assay described elsewhere
(Rakhmanova and MacDonald, 1998
).
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RESULTS |
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UV spectrophotometry of DNA-lipid complexes after boiling
When calf thymus DNA was held at 100°C for 10 min and then cooled to room temperature, an increase in absorption at 260 nm was observed. As is well known, this is the hyperchromic effect due to denaturation-induced unstacking of base pairs. In contrast to the significant hyperchromicity of free DNA, changes in UV absorption were much smaller when samples of DNA were treated with various cationic lipids before heating, i.e., the presence of the lipids greatly reduced the extent of DNA denaturation at 100°C. The effect was observed only in the samples treated with SDS after cooling the sample to room temperature; if SDS was added before or during heating, no protection of the DNA against thermal denaturation was observed and its denaturation was close to 100%.
The extent of protection depended strongly on the charge ratio of DNA-lipid mixtures, R(±). As shown in Fig. 1, for most cationic lipids and lipid mixtures (containing the neutral lipids DOPC or DOPE) used in our experiments, the protection was above 75% in the range of R(±) = 1.5 to 2.0. In the absence of a cationic component, DOPC had no protective activity. The effect of the cationic detergent TTMA alone was considerable smaller than that of the cationic lipids, EDOPC or DOTAP, however, mixtures of TTMA with the bilayer-forming neutral lipids DOPC or DOPE expressed a protective activity similar to that of the other cationic lipids.
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It should be noted that above R(±) = 2.5 to 3.0 we observed such a dramatic increase of UV absorption, evidently due to extensive aggregation, which led to high levels of light scattering, that reliable data could only be obtained in the range shown in Fig. 1.
DSC assay of boiled DNA-lipid complexes
Because of the light scattering limitation of absorbance methods for determining DNA denaturation, we used DSC to further characterize the protection of DNA by the cationic lipid, EDOPC, i.e., the compound that exhibited the largest effect according to Fig. 1. In the presence of EDOPC and SDS, control samples of calf thymus DNA melted in the temperature range of 60 to 85°C with a maximum at 71°C (Fig. 2 A). The shape of the curve shown is typical for calf thymus DNA, although the position of the maximum depends on the amount and type of electrolyte present. As shown in Fig. 2 A', when the sample was first heated to 100°C and then scanned in the calorimeter, no heat absorption was revealed because denaturation of calf thymus DNA is effectively irreversible on the time scale of these experiments. In contrast to the results of Fig. 2, A and A', when membrane-forming lipid EDOPC was added to DNA before first heating at 100°C, its protective effect was readily apparent in the significant heat absorption that was revealed in the subsequent heating scan (Fig. 2, B-D). Thus, the DNA from the complex that had been heated to 100°C was clearly native because it could be subsequently denatured after being released from the lipid by SDS treatment. It may be seen that the extent of DNA protection depended upon the charge ratio R(±) (Fig. 3), and a 1.5-fold excess of positive lipid over negative DNA charge of was required for maximal protection. It may also be observed in Fig. 2 E that a distinct fraction of native DNA was present even after heating up to 110°C, although the melting profile of DNA was distorted and the principal transitions occurred at somewhat elevated temperatures. In general, the DSC experiments confirm the results of the UV measurements described above. The protective effect depended on R(±) in a similar manner for both experiments (compare Figs. 1 and 3).
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DSC assay of naive DNA-lipid complexes
Although the experiments described above indicated that DNA in complexes with cationic lipid denatures at a much higher temperature than does a control solution of free DNA, they did not reveal the actual value of that denaturation temperature. To characterize the DNA melting profile after complexation with cationic lipid, DSC scans were carried to a considerably higher temperature than 100°C. Such scans are presented in Fig. 4 for both calf thymus and plasmid DNA in complexes with EDOPC. These samples were examined at two different ionic strengths. In addition, two different sizes (vortexed and sonicated) of liposomes were used to form the complex with DNA. The quantitative data from these scans is given in Table 1. Both types of DNA revealed the presence of two fractions with very different melting temperatures. One fraction had a denaturation temperature, Tm(labile), close to that of the control sample; it is termed the thermolabile component. The other fraction, with a denaturation temperature in the range above 100°C, Tm(stable), is termed the thermostable component. The shape of melting curve and the position of maxima of both thermostable and thermolabile components, but especially the latter, depended up the nature of DNA and the electrolyte composition of solution, as may be seen in the three panels of Fig. 4. Calf thymus exhibited its typical denaturation profile of a broad major peak with three high-temperature shoulders. It also exhibited the expected shift to a higher temperature at a higher ionic strength; for example, the melting curve of calf thymus DNA in 5 mM cacodylate had a maximum at ~65°C, whereas in high ionic strength DPBS buffer, the maxima moved up to ~85°C (Fig. 4, (1) A and (2) A; Table 1). Most of the DNA in the lipid complex was thermostable and denatured with maxima in the range 103 to 107°C (Fig. 4, (1) B and (2) B). The thermostable melting profiles were narrower that those of thermolabile DNA and lacked the shoulders, although a small, separate peak, centered at 115°C, is visible at high ionic strength.
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When the complex was formed from sonicated lipid, more thermostable DNA
was present than when it was formed from vortexed lipid (compare Fig.
4, (1) B and C, see also enthalpies
H(labile),
H(stable) and enthalpy ratio
H(stable)/
H(labile);
Table 1), and when the ratio of sonicated lipid to DNA was increased
from R(±) = 1:1 to R(±) = 1.7:1, the
amount of thermostable DNA was increased by almost two times (compare
Fig. 4, (1) B and D and (2)
B and D; see Table 1). Upon rescanning, both the
control DNA and the complexed DNA were seen to be completely denatured (see absence of endotherm in Fig. 4, (2) A' and
B'). Calf thymus DNA by itself is too complex to
significantly renature on the time scale of our experiments.
Apparently, interactions with the lipid are unable to prevent the loss
of alignment of the single strands, and the DNA remains denatured after
heating to a high temperature even in the lipid complex.
The melting profile of plasmid DNA (Fig. 4 (3) A) was very
different from that of the more complex chromosomal DNAs, and
individual melting domains (Volker et al., 1999
) were clearly resolved.
Heating and then rescanning the DNA revealed considerable renaturation of this DNA, for the scan (Fig. 4 (3) A') shows heat
absorption in the same range as native plasmid, although the annealing
was imperfect, because the profile lost its characteristic features. In
any case, the general consequence of plasmid DNA complexation with
EDOPC was similar to that for calf thymus DNA, namely a shift of the
transition to above 100°C (Fig. 4 (3) B; Table 1). In this
case, several maxima were seen, principally at 107 and 114°C. In all
experiments with calf thymus and plasmid DNA, the high-temperature melting fraction was observed only when EDOPC was present. In all
samples, the thermostable fraction melted in the temperature range 100 to 120°C, usually with more than one peak. With plasmid, as with
thymus DNA, sonicated lipid afforded more thermal protection than did
vortexed lipid. When the plasmid complex was first heated to 120°C,
and then rescanned, a thermolabile fraction was again seen (Fig. 4
(3) C'). This behavior was consistent with the partial renaturability of this DNA on the time scale of these experiments, although the profile was even more distorted than that of the free
plasmid that had previously been heated to 120°C (Fig. 4 (3)
A').
In the case of calf thymus DNA, the total enthalpy (
H)
of all fractions of DNA-lipid complex was somewhat smaller than the enthalpy of the free DNA. This is illustrated in Table 1, where all

Hs of the B and C scans of Fig. 4, (1) and
(2), were somewhat smaller than corresponding

Hs of the corresponding A scans. In contrast,

H of lipid complexes with plasmid DNA were larger than

H of free plasmid DNA (compare scans Fig. 4 (3)
A-C; Table 1). A difference is not unexpected,
however, because the environment of neutralized DNA in the complex is
much different than that of DNA free in solution, i.e., the charge is
neutralized by a surface and it is relatively dehydrated
(Choosakoonkriang et al., 2001
). It should be noted, however, that
others have described problems during sample transfer of other
DNA-cationic lipid complexes; because such complexes can be adhesive,
quantitative transfers are difficult, which can lead to uncertainties
in calorimetric measurements (Zantl et al., 1999
).
Separation and analysis of thermostable and thermolabile complexes
Complexation of DNA with cationic lipids was accompanied by
formation of aggregates, which was especially pronounced in the samples
with an excess of cationic lipid and R(±)
1. The
aggregates were easily sedimented by centrifugation and hence could be
easily collected for further investigation. Analysis, in particular by DSC, revealed that the pellet contained essentially the entire fraction
of thermostable DNA, whereas the transparent supernatant contained the
major portion of the thermolabile fraction (Fig. 5). It may be seen that the thermostable
fraction contained more than one peak (Fig. 5; see also Fig. 4). It is
possible that this material is not homogenous and contains a mixture of
different complexes of DNA with lipid, but if so, they did not readily
separate by centrifugation. More than 95% of lipid and ~80% of DNA
was present in the sediment, whereas in the supernatant the
concentration of DNA was much larger than that of lipid (Fig.
6). Transfection assays revealed that
almost all of the DNA delivery activity was present in the sediment and
that in the supernatant was very low. The transfection activity per
unit weight of DNA was 31 times larger for the pellet than for the
supernatant.
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Thin section electron microscopy of DNA-lipid complexes fixed with osmium tetroxide revealed the presence of multilamellar membrane structures in the pellet, as shown in Fig. 7. The periodic lamellar structures were very stable and were retained even at 130°C, i.e., above the presumptive denaturation temperature of the thermostable DNA. Fourier analysis of the images revealed that the repeat distance between lamellae, both at room temperature and at 130°C, was 6.0 to 6.5 nm. This indicates that, in the whole range of temperatures used in our experiments, the multilamellar structure was present and is thus a likely candidate for the basic structure of thermostable DNA.
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DISCUSSION |
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Two kinds of experiments demonstrated the existence of DNA
stable to heating above 100°C in complexes with cationic lipids. The
first set of experiments revealed that several common cationic lipid
transfection agents protected DNA against denaturation and also
provided evidence for the presence of native DNA after exposure to
100°C. The DNA-lipid complexes were treated with the anionic detergent SDS to release DNA from its complex with cationic lipids (Bhattacharya and Mandal, 1998
) and to eliminate light-scattering interference during UV spectrophotometry. It was found that if SDS was
added before or during the thermal treatment, the cationic lipids did
not protect DNA against denaturation. As shown in Fig. 1, native DNA
was found only in the samples treated with SDS after cooling to room
temperature; i.e., the protective effect required that the lipid be in
its normal self-associated array. UV spectrophotometry revealed that
the thermal protection of DNA in the interval 1.5 < R(±) < 2.0 exceeded 75%, and for some lipids, like
EDOPC and the TTMA-DOPE mixture, it was above 90%. High protection was
exhibited both by the potent DNA delivery agents EDOPC, DOTAP, and
DC-Chol/DOPE, as well as by the weak transfection agents DC-Chol/DOPC,
TTMA/DOPE, and TTMA/DOPC. All these lipids or lipid mixtures exist in
the bilayer structure. The cationic micellar detergent, TTMA, exhibited considerably lower protective activity than the lamellar phase lipids,
although this class of cationic detergents can electrostatically interact with DNA and finally form a hydrophobic complex (Spink and
Chaires, 1999
; Wang et al., 2000
). It thus seems clear that the bilayer
structure of lipids is important for DNA protection. It is equally
clear that interaction of DNA molecules with the cationic charge of the
membrane surfaces is also necessary for stabilization of DNA
against thermal denaturation, for the bilayer-forming, neutral DOPC did
not exhibit detectable protective activity.
To confirm and extend the UV absorbance measurements, DSC was applied to DNA complexes formed with the cationic lipid EDOPC, which exhibited the largest protective effect. Using an experimental protocol similar to that of the spectrophotometric experiments, we observed a similar protective effect (Figs. 2 and 3) and moreover, were able to extend the determination to a higher R(±). Indeed, with this technique we found that the protective effect of EDOPC was close to 100% at R(±) = 1.5 to 3.0 and some native DNA was even detectable even after heating to 110°C. Although EDOPC has very good transfection activity, in general, the protective effect of cationic lipids did not correlate with their transfection activity.
The presence of native DNA after boiling could be explained either by a reversibility of DNA denaturation or by an increase of the DNA melting temperature to above 100°C. A second set of experiments, using DSC, was performed to distinguish between the two possibilities. DSC analyses of DNA-EDOPC complexes over a wide range of temperatures (Fig. 4; Table 1) directly demonstrated the appearance of two fractions of DNA: a thermolabile DNA with a melting profile and melting temperature, Tm(labile), quite similar to that of the control DNA solution, and a thermostable DNA with a greatly increased melting temperature, Tm(stable). Cationic lipids stabilized both DNAs that were examined, namely, calf thymus (Fig. 4, (1) and (2)) and bacterial plasmid DNA (Fig. 4 (3)); however, the denaturation of plasmid DNA, unlike that of calf thymus DNA, was substantially reversible.
On the basis of the parameter
H2/
H(labile)
(Table 1), it is apparent that the procedure for complex formation and
the size of liposomes are both important for DNA stabilization. Small
ultrasound treated liposomes were consistently more effective in the
stabilization of DNA than large vortexed liposomes (Fig. 4; Table 1).
The difference could be related to different extent of aggregation of
liposomes observed after addition of lipid to DNA. Large liposomes
aggregated more intensively and produced larger aggregates than did
small liposomes. Aggregation could well prevent uniform mixture of DNA and lipid because some free lipid could be trapped inside the lipid
aggregates with the consequence that some free DNA is left in solution.
Generally, the conditions favorable for better mixing of DNA and lipid,
such as fast stirring during addition lipid to DNA, use of small
ultrasound treated liposomes, and ultrasound fragments of DNA, enhanced
formation of the thermostable complex. Fractionation of complexes by
centrifugation revealed that the thermostable component contained the
major proportion of lipid. The thermolabile fraction was relatively
enriched in DNA and contained a small amount of lipid (Figs. 5 and 6).
Although the simplest interpretation is that the thermolabile fraction
is essentially free DNA, given the present data, we cannot rule out
that it is a DNA-lipid complex with a different structure and much
higher DNA content than the thermostable complex. Presumably the excess of DNA did not interact with bulk of the lipid and remained in the
solution as free thermolabile DNA. Ultrastructural analyses revealed
that the thermostable fraction contained multilamellar structure with
periodicity of ~6 nm, which is close to the periodicity found early
by several methods of electron microscopy and by small angle x-ray
scattering (Rädler et al., 1997
; Huebner et al., 1999
; MacDonald
et al., 1999
). This periodic structure was very stable and was retained
at all temperatures involved in our experiments. Because this
multilamellar structure consists of parallel surfaces of bilayer
membranes alternating with monolayers of ordered DNA cylinders, then,
if the diameter of a DNA molecule,
DDNA = 2 nm, and the linear charge
density of DNA is LCDDNA = 0.17 nm/negative charge (i.e., 0.34 nm/bp), the projection of a DNA cylinder onto the
membrane surfaces is: S = 2DDNA
LCDDNA = 2 × 2 nm × 0.17 nm/negative charge = 0.68 nm2/negative
charge. Because the surface area of one EDOPC molecule is a few squared
Ångstroms larger than the surface area of a DOPC molecule and
approaches 0.7 nm2/mol (MacDonald, Momsen,
Brockman, unpublished results), the projection of one negative charge
of a DNA cylinder should be approximately equal to one positive charge
of one surface of an EDOPC membrane, hence a 1:1 stoichiometry would
imply that the DNA chains were essentially close packed. However, there
is interchain repulsion that holds the chains apart, so the
stoichiometry of the complex should be >1:1. In fact, based on the
plateau values of the DNA denaturation temperature (Figs. 1 and 3), the
stoichiometry of our complex with EDOPC was actually
R(±) = 1.5 to 2.0, which corresponds to an
intercylinder distance of: d = DDNA R(±) = 3.0 to
4.0 nm. This distance is, in fact, close to that found by small angle x-ray scattering and electron microscopy for other cationic lipid complexes (Rädler et al., 1997
; Lasic et al., 1997
; Battersby et
al., 1998
; Koltover et al., 1998
; Huebner et al., 1999
). It thus
appears that the thermostable complex with stoichiometry of
approximately R(±) = 1.5 to 2.0 corresponds to the known multilamellar periodic structure containing
ordered DNA molecules with fixed distances between axes of DNA cylinders.
In itself, the thermal stabilization of DNA by cationic lipids is not
unexpected, for many other cations are known to have this effect. For
example, mono- and bivalent metal cations can considerably increase the
temperature of DNA melting (Duguid et al., 1993
, 1995
). In general, the
stabilization of DNA by cations can be explained by electrostatic
interactions between positive charges and DNA phosphate oxygens, the
result of which is reduced coulombic repulsive forces between phosphates.
Although DNA stabilization by cationic lipids exhibits some resemblance
to that of water-soluble cations, there are also some very significant
differences. Indeed, these differences constitute some of the most
significant aspects of this study. The most obvious difference has to
do with concentration dependencies. Stabilization by cationic lipids is
characterized by a stoichiometric interaction in which the denaturation
temperature rises to a maximum and remains constant thereafter,
independent of the ratio of lipid to DNA. In contrast, metal cation
effects are highly concentration dependent with stabilization
increasing with concentration in the low and moderate ranges. Moreover,
in some cases (particularly transition metals), high metal ion
concentrations induce destabilization of the double helix by causing
improper base pairing and backbone disorder, and A-conformations and
even Z-form elements may appear (Anderson and Record, 1990
; Duguid et
al., 1993
, 1995
; Kornilova et al., 1997
; Andrushchenko et al., 1997
).
The only reported effect on DNA of a cationic lipid has been some small
changes in polar region that could be explained by partial dehydration
(Choosakoonkriang et al., 2001
). Our results revealed that the position
of Tm(stable) was not only largely
independent of R(±), but was also uninfluenced by conditions of sample preparation and buffer
composition. Furthermore, Tm(stable)
was approximately the same for both calf thymus and plasmid DNA (Fig.
4; Table 1).
These fundamental differences between the concentration-dependent DNA stabilization by metal cations and the highly cooperative step-like changes in the melting temperature induced by cationic lipids are explicable by the basic structural differences between the associated charges of lipid bilayers and the dispersed charges of the water soluble agents. One important characteristic of the self-assembled nature of the lipid bilayer is that its multiple charges are "preassociated" and need not undergo a large concentration increase (and an associated entropy decrease) to associate with DNA. This must significantly reduce the free energy barrier for DNA condensation and account for a considerable part of the high association constant of bilayer-forming cationic lipids with DNA (Pozharski and MacDonald, manuscript in preparation). The second important characteristic of the lipid bilayer has to do with the behavior of the two interacting surfaces. Once lipid is in excess, the DNA faces two cationic surfaces along its entire length, and dissociation is impossible without breaking large numbers of interactions simultaneously. Although there may be other influences, the two differences described appear to adequately explain the significant differences between DNA stabilization by lipids and those of dispersed cations.
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ACKNOWLEDGMENTS |
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This research was supported by the National Institutes of Health grant GM 52329 and Russian Foundation of Basic Investigations grants 00-04-48144; 00-15-97985. Many of the investigations made use of the Keck Biophysical Facility of Northwestern University, and we are grateful to the director, Katerina Spiegel, for assistance in many ways.
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FOOTNOTES |
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Received for publication 21 June 2001 and in final form 2 October 2001.
Address reprint requests to Robert C. MacDonald, Department of Biochemistry, Molecular Biology and Cell Biology, Northwestern University, Evanston, IL 60208. Tel.: 847-491-5062; Fax: 847-467-1380; E-mail: macd{at}northwestern.edu.
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REFERENCES |
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Biophys J, January 2002, p. 264-273, Vol. 82, No. 1
© 2002 by the Biophysical Society 0006-3495/02/01/264/10 $2.00
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