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* Laboratoire de Biophysique Moléculaire, Cellulaire et Tissulaire (BioMoCeTi), Unité Mixte de Recherche, Centre National de la Recherche Scientifique 7033, Unité de Formation et de Recherche, Santé, Médecine et Biologie Humaine, Université Paris 13, 93017 Bobigny cedex, France;
Université Pierre et Marie Curie, Case 138, 75252 Paris cedex 05, France; and
Plate-forme Synthèse d'Oligonucléotides, Institut Pasteur, 75724 Paris cedex 15, France
Correspondence: Address reprint requests to J. Lacoste, Tel.: 33-1-48-38-73-91; Fax: 33-1-48-38-73-56; E-mail: jerl{at}ccr.jussieu.fr.
| ABSTRACT |
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| INTRODUCTION |
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It has been well known for a long time that, in vivo, traces of divalent metal ions are preferentially bound to reiterative DNA sequences (7
) and since such DNA sequences are essentially present in constitutive heterochromatin areas it was interesting to consider more precisely the properties of these sequences and their function, taking into account the presence of metal ions at some steps of the mitotic cycle.
Constitutive heterochromatin areas occupy identical positions in homologous chromosomes and were first distinguished from euchromatin areas on the basis of differential staining with banding techniques (8
). Heterochromatin is especially abundant at the centromeres and telomeres. It is composed of highly reiterated sequences called satellite DNA, characterized by their unusual base composition and nature. For example, in Drosophila melanogaster, heterochromatin accounts for an estimated 33.5% of the female genome with satellite repeats representing 21% of the genome (9
,10
). Progress has been made in the understanding of the sequence and molecular organization of Drosophila (9
,11
,12
) and human (13
) centromeres, yet our understanding of their higher structural organization and function is still very limited. Molecular and genetic properties that further distinguish heterochromatin from euchromatin include condensation throughout the cell cycle, late replicating during S phase, and faster replicating DNA leading to a good synchrony of its replication, transcriptional inactivity, sequence composition, and greater contents of metal ions (6
).
Among these metal ions, copper seems to play an important role in heterochromatin structure and function (2
,6
). The binding of Cu2+ to DNA appears to be highly cooperative and related to DNA denaturation. Moreover the Cu2+ binding is concentration dependent. At very low metal concentration Cu2+ binds nonspecifically to the phosphate groups like most other ions. Upon increasing concentration, the Cu2+ ions begin to reach the bases mostly by chelation with the N7 of guanine. When metal ion concentration reaches 0.7 atom/nucleotide, the double helix is opened, and DNA denaturation begins (2
,6
,14
,15
). Several models have been proposed to describe the Cu2+ binding to double-stranded DNA that we will not discuss here (7
,16
). Considering these properties, it is clear that Cu2+ binding to DNA can influence the structures and the functions of heterochromatic areas in vivo in various ways. For example Cu2+ can cause DNA helix-coil transition—thus facilitating replication, inducing errors during translation—or even be implicated in carcinogenesis (6
,7
). On the other hand, copper is known to be able, like other divalent cations, to promote and stabilize non-B DNA structures (5
,16
–18
) and even triple helices (19
).
A DNA triplex is formed upon binding of a pyrimidine or a purine single-stranded DNA to the major groove of a double helix, forming Hoogsteen or reverse-Hoogsteen hydrogen bonds with the purine strand of the duplex. Triplex DNA comes in three structural classes that differ in the base composition of the third strand, the relative orientation of the phosphodiester backbones, the sensitivity to pH and cations (4
,17
), and thermodynamic parameters (20
). They have been described as the (C, T) or pyrimidine motif, the (G, A) or purine motif, and the (G, T) motif. These motifs can form both intramolecularly, giving H DNA, and intermolecularly with triple helix-forming oligonucleotides (TFOs). In the pyrimidine motif, the third strand is composed of cytosines and thymines and binds parallel to the purine strand of the duplex by Hoogsteen hydrogen bonds, leading to the formation of T·A-T and C+·G-C triplets (21
,22
). (In the triple helix notation, the (·) represents the hydrogen bonds between the third strand and the target duplex; the (-) represents the Watson-Crick hydrogen bonds.) Formation of this motif requires slightly acidic conditions (21
,22
). In the purine motif, the third strand is composed of guanines and adenines and binds antiparallel to the purine strand of the duplex by reverse-Hoogsteen hydrogen bonds, leading to the formation of A·A-T and G·G-C triplets (21
–23
). This motif contains no protonated bases and its stability is therefore pH independent; however its formation generally requires divalent (Mg2+, Zn2+, Mn2+, etc.) (17
) or multivalent cations (spermine, spermidine) (22
). In the (G, T) motif the third strand is composed of guanines and thymines and binds parallel or antiparallel to the purine strand of the duplex, depending on the number of TpG steps in the third strand (24
–26
).
We have recently shown using electrophoretic mobility shift assay experiments that low concentrations of Cu2+ can promote the formation and stabilization of a pyrimidine triplex with D. melanogaster satellite repeats under nearly physiological condition (i.e., mostly neutral pH), bypassing the protonation requisite of the third strand cytosines (19
).
Fourier transform infrared (FTIR) spectroscopy has been widely used for investigating metals in interaction with DNA (15
,27
,28
) and is known to be an appropriate technique to evidence the formation of triple helical structures and to determine many of their characteristics (basepairing, sugar geometries, etc.) (29
,30
). In this work we investigate by FTIR and ultraviolet (UV) spectroscopies the in vitro formation of a pyrimidine triplex at neutral pH in presence of Cu2+ by the D. melanogaster satellite sequence (AAGAGAG)n=2. We then propose a mechanism by which the Cu2+ ions can overcome the protonation requisite for classical pyrimidine motif triple helices and promote the triple helix formation at neutral pH.
| MATERIALS AND METHODS |
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After evaporation to dryness, the oligonucleotides were desalted on a G10 Sephadex column and then purified twice by high-performance liquid chromatography (HPLC) on a reverse phase C18 column using gradient CH3CN in TEAAc buffer. The purified oligonucleotides were then exchanged into sodium salt on a Dowex Na+ column and lyophilized. Purity was checked by analytical HPLC, capillar electrophoresis, and matrix-assisted laser desorption ionization-time of flight. For vibrational spectroscopy three 14-mer deoxyoligonucleotides were synthesized with the following sequences:
Concentrations of oligonucleotides were estimated by UV absorption measurements at 85°C using a nearest-neighbor approximation for the absorption coefficients (32
). All concentrations are expressed in strand molarities.
UV spectroscopy
Absorbance versus temperature cooling and heating curves were obtained using a UVIKON 940 (Kontron, Paris, France) spectrophotometer as previously described (19
). The temperature of the bath was increased or decreased at a rate of 0.1°C/min, thus allowing complete thermal equilibrium of the cells. At each temperature, absorbance measurements were performed at 245, 260, and 330 nm (control wavelength). Data were extracted from the profiles recorded at 260 nm. Unless otherwise specified, all experiments were performed in 10 mM sodium cacodylate buffer (pH 6.0 or 7.2) containing 25 mM KCl and between 0 and 35 µM CuCl2 (0–0.5 copper ions/nucleotide). For triplex experiments strand concentrations were 1 µM for the duplex and 1.2 µM for the third strand. Tm was determined as described in Rougée et al. (33
). In all UV experiments, the extended target duplex was used shifting, as previously described (19
), the duplex melting toward higher temperatures to distinguish triplex from duplex transition.
Infrared spectroscopy
The 14RY duplexes were preformed and annealed at 95°C for 10 min. The desired amount of Cu2+ ions (CuCl2 solution) was then added. Finally an equimolecular amount of third strand (in the same buffer as the duplex) was added.
Samples were studied in H2O and in D2O solutions at a strand concentration around 10 µM. They were deposited between two ZnSe windows without spacer. Deuteration experiments were performed by drying the samples under nitrogen and redissolving them in identical volumes of D2O (>99.8% purity, Euriso-Top; CEA, Saclay, France). FTIR spectra were recorded using a Perkin Elmer 2000 spectrophotometer (Perkin Elmer, Foster City, CA) at a 1-cm–1 resolution. Five scans were accumulated. Data treatment was performed using the Perkin Elmer spectrum program.
| RESULTS AND DISCUSSION |
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At pH 6.0 in 25 mM KCl, for the equimolecular mixture of the 26RY duplex and the 14TC third strand a classical pyrimidine triple helix melting curve is obtained (Fig. 1, curve e). A first clear transition due to the separation of the TFO from the duplex is detected with a Tm value of 36°C, whereas the duplex transition exhibits a Tm value of 57°C (Table 1, column 1) at the same temperature as that measured for the duplex alone under similar conditions (Fig. 1, curve c). As expected, an increase in KCl ionic strength induces a stabilization of the duplex to 67°C (Table 1, columns 2 and 3), whereas the triplex Tm remains unchanged, as previously described in Horn et al. (19
).
At pH 7.2 in 25 mM KCl when the 26RY duplex is mixed with the 14TC TFO, no transition due to the formation of a triple helix can be evidenced (Table 1, column 4). Under the same conditions and in presence of Cu2+ ions with a ratio of 0.15 and 0.33 Cu2+/nucleotide, still only monophasic melting curves are obtained, corresponding to the 26RY duplex transition (Table 1, columns 5 and 6, curves not shown). At a ratio of 0.5 Cu2+ ions/nucleotides a biphasic melting curve is recorded (Fig. 1, curve f). The first transition with a Tm value of 23°C can be assigned to the separation of the third strand from the duplex, whereas the second transition observed at 57°C corresponds to the melting of the 26RY duplex (Table 1, column 7). This latter transition is observed at the same temperature as for the 26RY duplex alone in presence of copper ions (Fig. 1, curve d). It should be noted that for curve 1 d, upon cooling, around 40°C a slight displacement of the curve is observed, reflecting the difficulty in reforming the duplex in presence of Cu2+ ions. A similar displacement, upon cooling, is observed for curve 1 f above the triplex Tm.
In presence of copper the triplex transition at 23°C appears perfectly reversible upon association (cooling) and dissociation (heating) (Fig. 1, curve f) in contrast with classical pyrimidine triplexes for which, at acidic pH, the dissociation is generally shifted toward higher temperatures as compared to the association curves (Fig. 1, curve e, and (19
,33
)). This reflects that the mechanism by which the triplex formation is achieved in presence of copper ions is clearly different from that occurring under acidic pH conditions.
Thus UV experiments show that Cu2+ ions are able to stabilize a triple helix formed by the (AAGAGAG)n=2 Drosophila satellite repeats at neutral pH. To further investigate the mechanism of this stabilization, we have studied this triple helix by vibrational spectroscopy, which allows us to probe different putative interaction sites in nucleic acid structures.
Vibrational spectroscopy
Binding of copper ions on the 14TC oligonucleotide
Fig. 2 presents the FTIR spectra of the 14TC oligonucleotide in absence (spectrum 2 a) and in presence of increasing amounts of Cu2+ ions (0.5 Cu2+/nucleotide, spectrum 2 b; 1 Cu2+/nucleotide, spectrum 2 c). The spectra are recorded in D2O solutions, and the spectral domain shown (1750–1450 cm–1) contains absorption bands due to in-plane double bond stretching vibrations of the bases. The base absorption bands of the 14TC spectrum can be assigned as follows (Table 2 column 3): 1693 cm–1 thymine C2=O2 stretching vibration; 1660 cm–1, thymine C4=O4 stretching vibration (band overlapping the 1653 cm–1 cytosine C2=O2 stretching vibration absorption); 1634 cm–1: thymine ring vibration; 1524 and 1506 cm–1: cytosine ring vibrations (30
,34
). The 1524 cm–1 band involves in particular the motions of the cytosine N3 atom (35
). Progressive addition of Cu2+ ions shifts this band to higher wavenumbers (1546 cm–1), reflecting the interaction of the copper ions on the N3 cytosine site. A similar shift of the 1524 cm–1 band to 1546 cm–1 is also observed upon addition of Cu2+ to dC14 or poly dC (spectra not shown). The 1506 cm–1 cytosine ring vibration is also affected by the addition of copper ions. It progressively disappears with increasing copper content and is replaced by an absorption located at 1518 cm–1. Binding of copper on the cytosine affects the electronic repartition of the ring and thus possibly the relative intensity of the 1506 cm–1 band. Earlier NMR (36
) and infrared (IR) (16
,37
) studies have shown that Cu2+ does not bind to thymidine. We notice that the addition of Cu2+ ions to the 14TC oligonucleotide does not alter the positions of the three thymine bands described above. In summary, the Cu2+ ions interact with the cytosines of the free 14TC third strand at the position of the N3 atoms.
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Localization of the copper ions stabilizing the triple helix
The formation of the C·G-C base triplets is thus made possible by the presence of copper ions without protonation of the N3 atom. Different binding sites are possible for Cu2+ ions, enabling this binding of the third strand cytosine to the guanine of the target polypurine strand. The proposed binding model (Fig. 4 c) is supported by the following evidence.
In the first place, it can be seen that the C6=O6 guanine stretching band located at 1674 cm–1 in the duplex spectrum (Fig. 2 d) is still present when Cu2+ ions are added (Fig. 2 e) but is no longer observed in the spectra of the triplexes either at acidic pH (Fig. 5 c) or in presence of Cu2+ ions (Fig. 5, d and e). This reflects the formation of the Hoogsteen-type hydrogen bond between the C6=O6 guanine carbonyl and the N4H2 group of the third strand cytosine and does not involve binding of Cu2+ ions to the C6=O6 guanine carbonyl.
Second, in the spectrum of the triple helix formed at neutral pH in presence of Cu2+ ions (Fig. 5 d), an absorption band is detected at 1540 cm–1. We have seen in the previous sections that the emergence of this band reflected the interaction of copper at the N3 atom of cytosines.
The emergence of a band located at 1582 cm–1 is also detected in the spectrum of the triple helix formed in presence of Cu2+ ions (Fig. 5 d), reflecting an interaction at the guanine N7 atom. To confirm the existence of such an interaction, we have studied a triple helix incorporating a targeted purine strand with selectively deuterated guanines at the C8-H group (14D8R). Fig. 6 presents the spectra recorded in H2O solutions of the 14RY and 14D8RY duplexes (respectively, spectra 6, a and b). The band located at 1492 cm–1 (spectrum 6 a) contains a contribution assigned to the N7C8H bending vibration. Hydrogen-deuterium exchange shifts this component to lower wavenumbers: it is now observed at 1462 cm–1 (spectrum 6 b). Addition of copper ions shifts this band back to 1487 cm–1, reflecting the binding of copper at the N7 guanine site (spectrum 6 c).
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Thus, in the triple helix, the Cu2+ ions interact on one hand with the N3 atoms of cytosines and on the other with the N7 atoms of guanines. We propose therefore that they stabilize the formation of the triple helix at neutral pH (Fig. 4 c), replacing the protonation of the N3 atom used in classical pyrimidine motif triplexes formed at acidic pH (Fig. 4 b).
| CONCLUSION |
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Biological relevance of triplexes in heterochromatin
A question that arises here is: Can triple helices, or H-DNA, be formed in vivo in centromeric regions? Some studies have shown that TFOs can be hybridized in situ to nondenatured metaphase spreads and interphase nuclei (44
) and that triplex-forming DNAs in the human interphase nucleus can be visualized with DNA probes and anti-triplex antibodies (45
). Our results show that, in principle, the Drosophila AG-rich satellite is able to form a triple helix. Yet, a major restriction (the necessity of an acidic pH) could prevent the formation of this pyrimidine triple strand structure in vivo. We demonstrate in this study that pH dependence can be overcome by relatively low Cu2+ concentrations.
It is conceivable that some intracellular mechanisms can locally increase divalent metal ions concentrations to levels comparable with our experimental conditions. For example, it is known that metal ions are naturally present in in vivo DNA (18
) and concentrated in centromeric reiterated sequences (2
,7
). Thus, high local concentrations of divalent cations can be achieved via their natural binding to such sequences. Another mechanism by which the triplex-modulatory effects that we have observed with naked transition metal cations could be accomplished naturally in vivo is the interaction with a metal cation coordinated to a specialized peptide domain (46
) or by a conjugate such as iminodiacetic acid (47
) or glutamic acid (48
).
Our data have been obtained using a twice-repeated AAGAGAG target sequence of the D. melanogaster satellite DNA. In vivo the sequence is found repeated thousands of times. We have previously shown (19
) that an increase in the number of repeats drastically increases the triplex stability. Thus we can reasonably propose that the formation of a stable copper-induced triplex in vivo may be compatible with the environmental conditions naturally encountered by D. melanogaster (49
).
Thus the data presented herein support the concept that triplex-favorable local conditions of the micronuclear environment and therefore triple-stranded DNA can exist in vivo. The study of the effect of other metal ions on the stabilization of triple helices in D. melanogaster satellite repeats is now under progress.
| ACKNOWLEDGEMENTS |
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Submitted on October 23, 2006; accepted for publication December 8, 2006.
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