From the W. A. Engelhardt Institute of Molecular Biology, Academy of Sciences of Russia, Vavilova, 32, Moscow B-334, 117984, Russia
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ABSTRACT |
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We have recently reported that certain core histone-DNA contacts are altered in nucleosomes during chromatin unfolding (Usachenko, S. I., Gavin I. M., and Bavykin, S. G. (1996) J. Biol. Chem. 271, 3831-3836). In this work, we demonstrate that these alterations are caused by a conformational change in the nucleosomal DNA. Using zero-length protein-DNA cross-linking, we have mapped histone-DNA contacts in isolated core particles at ionic conditions affecting DNA stiffness, which may change the nucleosomal DNA conformation. We found that the alterations in histone-DNA contacts induced by an increase in DNA stiffness in isolated core particles are identical to those observed in nucleosomes during chromatin unfolding. The change in the pattern of micrococcal nuclease digestion of linker histone-depleted chromatin at ionic conditions affecting chromatin compaction also suggests that the stretching of the linker DNA may alter the nucleosomal DNA conformation, resulting in a structural transition in the nucleosome which may play a role in rendering the nucleosome competent for transcription and/or replication.
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INTRODUCTION |
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The compaction of DNA into chromatin provides many obstacles for its functioning in eukaryotic nuclei (1). The current model of transcription and replication suggests that chromatin must be remodeled in at least two distinct steps (2-5). The first step involves decondensation of chromatin fibers facilitating the access of trans-acting factors to DNA. The second step implies either a reversible dissociation of the histone octamer from DNA or a structural transition of the nucleosome allowing transcription or replication to proceed (3, 6-11). A number of reports have suggested that the nucleosome structure in active chromatin is changed (12-15). Since only a few experiments have distinguished between transcriptionally competent and actively transcribed chromatin (3, 8), very little is known about the structural details of these changes. Transcriptionally active chromatin is unfolded and significantly depleted of linker histones (16), which play a key role in chromatin compaction (17, 18). Recently, we have reported that certain histone-DNA contacts in the nucleosome core are heavily attenuated during chromatin unfolding (19), indicating that the nucleosome structure is changed at the first step of chromatin activation, chromatin decondensation. These changes may facilitate the second step, which involves either remodeling or removal of the nucleosome.
The binding of histone H1 to linker DNA considerably reduces its electrostatic free energy which determines linker DNA bending during chromatin folding into the higher order structure (20). In contrast, in linker histone-depleted chromatin, the distance between the points where the linker DNA enters and leaves the nucleosome core may be increased by repulsion between adjacent linker DNA segments (17, 21-24) and thereby can affect the conformation of the nucleosome core DNA. To address the question of whether or not the alterations in histone-DNA contacts during chromatin unfolding, which we observed earlier (19), are caused by the changes in the nucleosome core DNA conformation, we have analyzed the histone-DNA contacts in isolated core particles under ionic conditions affecting DNA stiffness.
Several physical and biochemical studies have demonstrated that a reduction of the monovalent ion concentration below 10 mM has a significant effect on the nucleosome core structure (reviewed in Ref. 25). It has also been well documented that the loss of counter-ions at low ionic strengths increases the electrostatic repulsion of unneutralized DNA phosphate groups, resulting in an increase in DNA stiffness (26). This increase in the stiffness may cause stretching of the nucleosomal DNA that in turn may change the conformation of the nucleosome (27) and affect histone-DNA contacts. In the present paper, we show that the alterations in histone-DNA contacts in isolated core particles induced at low ionic strength are caused by a decrease in the neutralization of negative DNA charges and are identical to those observed in nucleosomes during chromatin unfolding (19). This suggests that the conformational changes in nucleosome core particles at low ionic strength and in nucleosomes in chromatin during chromatin unfolding are due to the stretching of the nucleosome core DNA. Based on these observations, we propose a model for the reversible structural transition yielding a new nucleosome conformation in an unfolded chromatin.
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EXPERIMENTAL PROCEDURES |
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Isolation of Nucleosome Core Particles and Histone-DNA Cross-linking-- Nucleosome core particles were isolated from chicken erythrocyte nuclei as described previously (28, 29). Protein-DNA cross-linking under various ionic conditions, purification, and histone-labeling of cross-linked complexes with 125I were performed as described (30, 31).
Micrococcal Nuclease Digestion of Linker Histone-depleted Chromatin-- Linker histone-depleted chromatin prepared from chicken erythrocyte nuclei as described earlier (19) was digested with micrococcal nuclease (3 µg/1 mg of DNA) in 10 mM Tris-Cl, pH 8.0, and either 0.3 mM CaCl2 or 2 mM CaCl2 for the time course of 20, 40, and 80 min at 37 °C. The reaction was stopped by adding EDTA to a final concentration of 4 mM.
Gel Electrophoresis Analysis-- DNA from nucleosomes released by the micrococcal nuclease digestion of linker histone-depleted chromatin was analyzed in a 9% denaturing gel containing 7 M urea following digestion with Pronase (0.5 mg/ml) for 30 min at 37 °C (32).
Histone-DNA contacts were mapped by the "protein version" of two-dimentional gel electrophoresis of 125I-histone-labeled cross-linked complexes as described earlier (31). For the qualitative analysis of relative intensities of certain signals, the autoradiographs of two-dimensional gels from at least three sets of experiments were scanned in a SL-504-XL Zeineh soft laser scanning densitometer (Biomed Instruments Inc., Fullerton, CA). ![]() |
RESULTS |
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The Alterations in Histone-DNA Contacts in Isolated Core Particles
Induced by Low Ionic Strength Are Identical to Those Occurring during
Chromatin Unfolding--
To study the histone-DNA interactions in
isolated core particles under different ionic conditions, we used the
method of chemically induced zero-length protein-DNA cross-linking (31,
33). Cross-linking causes a single-stranded nick of the nucleosomal DNA
at the site of cross-linking such that only the 5-terminal DNA
fragment becomes attached to a histone molecule (33). Therefore, the
length of the DNA fragment cross-linked to a particular histone is the
precise distance of a protein cross-linking site from the 5
-end of the nucleosomal DNA and can be assessed by the two-dimensional gel electrophoresis. To map the histone-DNA contacts in nucleosome core
particles under different ionic conditions, we have used a protein
version of the two-dimensional gel electrophoresis system (31, 33). In
the denaturing first dimension SDS gel, the mobility of
125I-labeled histone-DNA cross-linked complexes depends on
the molecular weight of the histones and the size of the cross-linked
DNA fragment. After separation of cross-linked complexes in the first
dimension, the DNA is hydrolyzed directly in the gel according to a
modified Burton's procedure (31, 33, 34), and released
125I-labeled histones are separated in the second dimension
SDS gel (35) according to their size. In the first dimension, the
mobility of histones is decreased proportionally to the size of DNA
fragments cross-linked to a particular histone (33). As a result, in
the gel of the second dimension, the 125I-labeled histones
are arranged as spots on different horizontal lines (Figs.
1 and 2).
The position of these spots indicates the location of the DNA cross-linking site for a particular histone in the
nucleosome (33).
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The Structural Transition of Nucleosome Core Particles Induced by Low Ionic Strength Is Caused by the Change in the Nucleosomal DNA Conformation-- The elevation of salt concentration causes electrostatic blocking of DNA phosphate groups, which depends on the charge of cations (26). The experimentally measured persistence length of DNA increases rapidly when the concentration of monovalent cations is decreased below 10 mM, whereas the same effect for divalent cations was observed at concentrations below 0.1 mM (37). Consistent with this observation, our data, represented in Fig. 2, demonstrate a similar change in the relative intensities of the analyzed contacts after the addition of divalent cations at 2 orders of magnitude less concentrations than monovalent cations. The weak intensity of contacts H2B(129) and H4(66) in 5 mM HEPES (Fig. 2A) is noticeably increased upon addition of 0.1 mM CaCl2 (Fig. 2B). A further increase in the concentration of divalent cations up to 2 mM causes an additional increase in the intensities of contacts H2B(129) and H4(66) (Fig. 2C). The relative intensities of the analyzed contacts at 100 and 30 mM monovalent cations (Fig. 1, A and B) resemble those at 2 and 0.1 mM divalent cations, respectively (Fig. 2, B and C) confirming previous observations that monovalent cations affect the nucleosome structure at approximately 2 orders of magnitude higher concentrations than divalent cations (36, 38, 39). We also tested various monovalent and divalent cations, such as K+, Li+, Cs+, Mg2+, Zn2+ for their ability to change histone H4/H2B contacts, and as expected, different cations that have the same charge had an identical effect on the analyzed contacts at the same concentrations. Cross-linking analysis also reveals that anions have no impact on the conformational transition induced by low ionic strength (not shown). Obtained results suggest that the conformational transition, observed as alterations in relative intensities of histone H2B/H4-DNA contacts at low ionic strength, is caused by the repulsion of adjacent unneutralized negative charges of DNA phosphate groups resulting in an increase in DNA stiffness.
The Interaction of Core Histones with DNA Regions Entering and Leaving the Nucleosome-- The level of chromatin compaction induced by 1-2 mM divalent cations is similar to that observed at physiological concentrations of monovalent cations (17, 18). An increase in the salt concentration also results in folding of linker histone-depleted chromatin and bending of linker DNA (17, 40-43). To investigate how this salt-induced chromatin condensation might change the nucleosome conformation, we have analyzed the pattern of micrococcal nuclease digestion of linker histone-depleted chromatin at different concentrations of divalent cations (Fig. 3). The first time point in the course of digestion at 0.3 mM Ca2+ yields nucleosome core particles with 146-bp1 DNA represented in the gel by a single band (Fig. 3A, lane 1). These nucleosomes are further digested to the level of subnucleosomes (Fig. 3A, lanes 2 and 3). In contrast, the first time point at 2 mM Ca2+ yields a set of core particles and particles with 157- and 168-bp DNA (Fig. 3B, lane 1), which then turn into particles with 146-bp DNA (Fig. 3B, lane 3). The bending of linker DNA induced by 2 mM divalent cations (17, 43) facilitates the wrapping of an additional ~20-bp DNA around the histone octamer (21, 22, 24). This renders linker DNA regions less accessible to micrococcal nuclease yielding nucleosomes with 157- and 168-bp DNA (Fig. 3B). The interaction of core histones with the end regions of nucleosomal DNA in particles with 155- and 165-bp DNA at monovalent salt concentrations above 30 mM has been demonstrated by protein-DNA cross-linking in isolated chromatin (44), in nuclei (45), and in H1-depleted nucleosomes (46). In contrast, at concentrations of divalent cations below 0.3 mM, linker DNA is stretched (17) such that the end regions of the nucleosomal DNA become susceptible to micrococcal nuclease. As a result, nucleosomes with 157- and 168-bp DNA are not observed under these conditions (Fig. 3A). It has been shown that micrococcal nuclease activity is only slightly reduced in 0.3 mM Ca2+ compared with 2 mM Ca2+ (47), whereas the specificity of the enzyme remains the same (48). This indicates that the observed difference in micrococcal nuclease digestion pattern reflects the change in the chromatin structure rather than the activity of the micrococcal nuclease, which is supported by early studies where a similar effect was observed at various concentrations of monovalent cations (49, 50).
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DISCUSSION |
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The Change in Histone H2B/H4-DNA Contacts Induced by Low Ionic Strength Occurs in the Sharply Bent Regions of Nucleosomal DNA-- In the present work, we have demonstrated that a structural transition in isolated core particles induced by low concentrations of monovalent cations is caused by the change in the nucleosomal DNA conformation that alters the analyzed histone H2B/H4-DNA contacts. These altered contacts are located at sites ± 5.5 and ± 1 (Fig. 4), which are very close to the sharply bent regions of the nucleosomal DNA (51-55). Histone H4 cross-links to the sites around ± 1 mainly through the single highly basic domain (30, 56, 57), which may alter DNA structure in this region (57, 58). On the other hand, the change in nucleosomal DNA conformation induced by low ionic strength in isolated core particles or by the stretching of linker DNA during chromatin unfolding can in turn affect histone interactions with these DNA sites. Since the analyzed contacts are located close to the sharply bent DNA regions, they would be expected to be very sensitive to conformational changes in the nucleosomal DNA.
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Models for the Conformational Transition of Nucleosomes-- Two models for the conformational transition of a nucleosome core caused by the straightening of the nucleosomal DNA have been proposed (27). In the model for a radial transition, the nucleosomal DNA straightening increases radius of gyration resulting in an oblate conformation of the nucleosome core. In the case of an axial transition, DNA straightens along the superhelical axis and thereby stretching the nucleosome core into the prolate form. Recent observations of the altered core particle shape to a prolate form (36) that have a decreased (36, 60) or unchanged (61) radius of gyration at concentrations of monovalent cations below 30 mM provide strong support for the second model. This model is also in agreement with the expected repulsion of adjacent superhelical turns of the nucleosomal DNA induced by low salt concentrations, which also tends to stretch the core particle in the direction of the superhelical axis. The axial straightening of DNA may also cause deformation of the histone octamer, which is consistent with the observed alteration in the histone octamer compaction with decreasing ionic strength from 30 to 10 mM NaCl (62).
Based on the results of this work and the observations of other investigators, we suggest a model for the structural transition of the nucleosome core that may occur during chromatin unfolding (Fig. 5). In condensed chromatin, the linker DNA is bent such that the histone octamer interacts with an additional 20 bp of DNA (Fig. 5A). In contrast, during chromatin decondensation after depletion or rearrangement of linker histones, stretching of the linker DNA may increase DNA tension along the polynucleosomal chain and change the nucleosome conformation in a way similar to that observed for isolated core particles at monovalent salt concentrations below 10 mM. This stretching would cause partial sliding of DNA off the histone octamer and make the additional 20-bp accessible to micrococcal nuclease (Fig. 5B). This model is also consistent with the observed salt-dependent release of nucleosomal DNA termini resulting in the change in the linking number of DNA in minichromosomes (21, 22) and in the altered nucleosome morphology in linker histone-depleted chromatin (21-24).
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Biological Relevance of the Conformational Transition of Nucleosomes during Chromatin Decondensation-- The association of the alterations in the analyzed histone H2B/H4-DNA contacts with the level of chromatin compaction and activity demonstrates the importance of these changes in chromatin structural/functional relationships (19). The alterations in the contacts formed by the highly basic histone domains may result in destabilization of the nucleosomes in unfolded chromatin facilitating nucleosome remodeling or/and removal during transcription and replication. This is strongly supported by the observation that a deletion of the histone H2B cross-linking domain changes the minichromosome topology in vivo, suggesting that this domain is required for the proper folding of DNA in the nucleosome (63). Deletion or substitution of a single amino acid in the cross-linking domain of histone H4 alters chromatin structure in vivo (63-66), decreases the ability of yeast to mate, increases the duration of S phase (67-70), and affects telomeric repression (71, 72) as well as expression of a large number of yeast genes (64, 65, 73-75). It should be mentioned also that the cross-linking domain of histone H4 contains sites for post-translational acetylation and phosphorylation (76) that may also be involved in the regulation of the interaction of this domain with DNA at different levels of chromatin activity and condensation rendering nucleosomes competent for transcription and/or replication.
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ACKNOWLEDGEMENTS |
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We thank Andrei Mirzabekov for the initial idea of this work. We are also grateful to Hugh Patterton for critical comments and Jodie Usachenko for help in the preparation of this manuscript.
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FOOTNOTES |
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* The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked "advertisement" in accordance with 18 U.S.C. Section 1734 solely to indicate this fact.
Present address: Dept. of Biochemistry and Molecular Biology,
Pennsylvania State University, University Park, PA 16802.
§ Present address: Dept. of Biological Chemistry, School of Medicine, University of California, Davis, CA 95616.
¶ Present address and to whom correspondence should be addressed: Center for Mechanistic Biology and Biotechnology, Argonne National Laboratory, 9700 S. Cass Ave., Bldg. 202, Argonne, IL 60439. Tel.: 630-252-3980; Fax: 630-252-3387; E-mail: sbavykin{at}everest.bim.anl.gov.
1 The abbreviations used are: bp, base pair(s).
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REFERENCES |
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